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keod3025upvoted (100.00%) @stevescully / official-challenge-to-scientists2024/08/29 15:15:30
keod3025upvoted (100.00%) @stevescully / official-challenge-to-scientists
2024/08/29 15:15:30
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}stevescullypublished a new post: official-challenge-to-scientists2024/08/11 19:32:54
stevescullypublished a new post: official-challenge-to-scientists
2024/08/11 19:32:54
| author | stevescully |
| body | It is the position of modern science that ammonites are fossils. However, the history of science labeling geological features as fossils has the example of the Eozoon canadense found in Canada that was initially believed to be a gigantic Foraminifera before it was recognized to be geological in origin. This challenge is to the longstanding assumption that has been made that ammonites are fossils. The challenge is simple. Here we have an ammonite in a stone known as a shaligram.  [Image Credits: Mangalam Jewelry](https://www.etsy.com/listing/1727918725/big-size-golden-narsimha-shaligram) In order to successfully refute the challenge, a refutation must <b>explain all features discussed below, not just some</b>. The challenge is to explain how the following features of this shaligram could result from fossilization. It is the position of the challenger that they <b>cannot</b>, as will be elaborated on at the conclusion of disclosing the details. ## Features of Pertinence This particular ammonite structure has several distinguishing characteristics that demonstrate irrefutably that ammonites <b>cannot be fossils</b> because the fossilization process <b>cannot explain how <i>all</i> these features are in the shaligram as a whole.</b> ### 1) The ammonite narrowing  While ammonites have been found to narrow and this feature <b>alone</b> would not distinguish that the ammonite cannot be a fossil, the many <b>elements</b> of the stone that relate to this make the ammonite distinguishably not a fossil. ### 2) The ammonite narrows to the middle height of the ammonite  This curious detail is of the ammonite shell specifically narrowing on <b>one side only</b> where the structure is shifted <b>wholly to the other side</b> would additionally require explanation. ### 3) The ammonite definitively narrows  As can be seen above, the ribs on the outside of the ammonite are visible on the top of the narrowed segment of the ammonite, thus the segment in question <b>is not broken in half so as to only <i>appear</i> like a narrowed section; the structure of the ammonite itself <i>actually is narrower</i> at this segment of the ammonite.</b> ### 4) The full structure of an ammonite is imprinted.  Up until this detail, it may appear like an ammonite's shell that narrowed at this segment would be adequate to explain the details. However, if the shell was truly the shape of ammonite as presently visible, it would not have had the <b>necessary boundary shapes to imprint the upper section of the shaligram by its contours since the contours would be those of the narrower segment.</b>  This further captures how the <b>full ammonite is imprinted.</b> How was this smaller ammonite shell able to imprint the structure below as if there was no difference in its shape? How did it imprint the above region? ### 5) The ammonite narrows in the middle of the ammonite and then continues as if nothing happened.  While it may not be immediately apparent, the left side of the ammonite is actually in the middle of the spiral outward from the center to the far boundary (right side). That means that the ammonite does not just do this <b>at the very terminal portion of its structure</b> but rather it abruptly has this feature in the middle of the ammonite. ### Challenge The author herein claims that ammonites <b>cannot be fossils because fossilization cannot explain these details.</b> Therefore, the challenge is thus to explain these details by conventional understanding of what we are looking at. If this is truly a fossil, how did an ammonite imprint a large structure in the stone while physically not having that structure? ### Conclusion It is the position of the author that ammonites are pseudofossils misclassified as fossils but are actually products of high energy eddy currents of water that propagated through materials of the Earth itself and shaped the materials, differentiated the materials, and took repetitive and regular shapes that appear like seashells to a point where they were misclassified, but are purely geological in origin and a product of high intensity water currents. Respectfully, Steve Scully [My website](https://cascadinguniverse.org) |
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"body": "It is the position of modern science that ammonites are fossils. However, the history of science labeling geological features as fossils has the example of the Eozoon canadense found in Canada that was initially believed to be a gigantic Foraminifera before it was recognized to be geological in origin. This challenge is to the longstanding assumption that has been made that ammonites are fossils.\n\nThe challenge is simple. Here we have an ammonite in a stone known as a shaligram.\n\n\n[Image Credits: Mangalam Jewelry](https://www.etsy.com/listing/1727918725/big-size-golden-narsimha-shaligram)\n\nIn order to successfully refute the challenge, a refutation must <b>explain all features discussed below, not just some</b>.\n\nThe challenge is to explain how the following features of this shaligram could result from fossilization. It is the position of the challenger that they <b>cannot</b>, as will be elaborated on at the conclusion of disclosing the details.\n\n## Features of Pertinence\nThis particular ammonite structure has several distinguishing characteristics that demonstrate irrefutably that ammonites <b>cannot be fossils</b> because the fossilization process <b>cannot explain how <i>all</i> these features are in the shaligram as a whole.</b>\n\n### 1) The ammonite narrowing\n\n\nWhile ammonites have been found to narrow and this feature <b>alone</b> would not distinguish that the ammonite cannot be a fossil, the many <b>elements</b> of the stone that relate to this make the ammonite distinguishably not a fossil.\n\n### 2) The ammonite narrows to the middle height of the ammonite\n\n\nThis curious detail is of the ammonite shell specifically narrowing on <b>one side only</b> where the structure is shifted <b>wholly to the other side</b> would additionally require explanation.\n\n### 3) The ammonite definitively narrows\n\n\nAs can be seen above, the ribs on the outside of the ammonite are visible on the top of the narrowed segment of the ammonite, thus the segment in question <b>is not broken in half so as to only <i>appear</i> like a narrowed section; the structure of the ammonite itself <i>actually is narrower</i> at this segment of the ammonite.</b>\n\n### 4) The full structure of an ammonite is imprinted.\n\n\nUp until this detail, it may appear like an ammonite's shell that narrowed at this segment would be adequate to explain the details. However, if the shell was truly the shape of ammonite as presently visible, it would not have had the <b>necessary boundary shapes to imprint the upper section of the shaligram by its contours since the contours would be those of the narrower segment.</b> \n\n\nThis further captures how the <b>full ammonite is imprinted.</b> How was this smaller ammonite shell able to imprint the structure below as if there was no difference in its shape? How did it imprint the above region?\n\n### 5) The ammonite narrows in the middle of the ammonite and then continues as if nothing happened.\n\n\nWhile it may not be immediately apparent, the left side of the ammonite is actually in the middle of the spiral outward from the center to the far boundary (right side). That means that the ammonite does not just do this <b>at the very terminal portion of its structure</b> but rather it abruptly has this feature in the middle of the ammonite.\n\n### Challenge\nThe author herein claims that ammonites <b>cannot be fossils because fossilization cannot explain these details.</b> Therefore, the challenge is thus to explain these details by conventional understanding of what we are looking at. If this is truly a fossil, how did an ammonite imprint a large structure in the stone while physically not having that structure?\n\n### Conclusion\nIt is the position of the author that ammonites are pseudofossils misclassified as fossils but are actually products of high energy eddy currents of water that propagated through materials of the Earth itself and shaped the materials, differentiated the materials, and took repetitive and regular shapes that appear like seashells to a point where they were misclassified, but are purely geological in origin and a product of high intensity water currents.\n\nRespectfully,\nSteve Scully\n[My website](https://cascadinguniverse.org)",
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}g1999upvoted (100.00%) @stevescully / shaligrams-are-not-fossils2024/07/06 06:41:36
g1999upvoted (100.00%) @stevescully / shaligrams-are-not-fossils
2024/07/06 06:41:36
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}stevescullypublished a new post: events-of-the-kt-boundary-part-22023/01/22 07:03:48
stevescullypublished a new post: events-of-the-kt-boundary-part-2
2023/01/22 07:03:48
| author | stevescully |
| body | [Events of the KT Boundary](https://steemit.com/science/@stevescully/events-at-the-kt-boundary) lists several major events at the K/T Boundary for consideration. Here is a continuation of the list. Additional geological events dated to ~66Ma: MORE impacts: After 1. Chicxulub Crater, 2. Nadir Crater, 3. Boltysh Crater, and 4. Shiva Crater, all discussed previously, 5. Tefe River Structure in Brazil dates to KT boundary: [Geophysical Evidence Of A Possible Impact Structure At The K-T Boundary Of The Solimões Basin, Brazil](https://www.earthdoc.org/content/papers/10.3997/2214-4609-pdb.215.sbgf220) [The Cretaceous-Tertiary boundary in the context of impact geology and sedimentary record-an analytical review of 10 years of researches in Brazil](https://www.researchgate.net/publication/325317164_The_Cretaceous-Tertiary_boundary_in_the_context_of_impact_geology_and_sedimentary_record-an_analytical_review_of_10_years_of_researches_in_Brazil) 6. The Silverpit Crater is controversially ~65-60Ma, and debated on whether it is an impact structure or a pull-apart basin: [A 20-km-diameter multi-ringed impact structure in the North Sea](https://www.nature.com/articles/nature00914) 7. Dumas Magnetic Anomaly in Canada, believed to be from a meteorite impact, formed late cretaceous, 70+/- 5Ma: [Magnetic Fields Associated with a Probable Late Cretaceous Astrobleme at Dumas, Saskatchewan](https://adsabs.harvard.edu/pdf/1978LPI.....9..433G) 8. The Jebel Hadid structure in Libya was formed after early Cretaceous and prior to late Miocene rivers and is compared to the Tin Bider impact crater in Algeria: [The Jebel Hadid structure (Al Kufrah Basin, SE Libya)—A possible impact structure and potential hydrocarbon trap?](https://www.researchgate.net/publication/248516714_The_Jebel_Hadid_structure_Al_Kufrah_Basin_SE_Libya-A_possible_impact_structure_and_potential_hydrocarbon_trap) 9. The Tin Bider Impact is poorly constrained to <66Ma by stratigraphy, the youngest geological unit affected by the event being ~66Ma limestones: [Shock-metamorphic microstructures in quartz grains from Albian sandstones from the Tin Bider impact structure, Algeria](https://onlinelibrary.wiley.com/doi/abs/10.1111/maps.13766) 10, 11. Kara/Ust-Kara twin impact structure dates variously to 60Ma-70Ma and has been considered as a possible K/T Boundary event: [The Kara/Ust-Kara twin impact structure; A Large-scale impact event in the Late Cretaceous](https://books.google.com/books?hl=en&lr=&id=naUIAQAAQBAJ&oi=fnd&pg=PA233&dq=ust-kara+crater&ots=-rdFZBbbCb&sig=uGqpK1cwuduM7ljUgFOlU5FfvyA#v=onepage&q=ust-kara%20crater&f=false) [The Kara and Ust-Kara impact structures (USSR) and their relevance to the K/T boundary event](https://ntrs.nasa.gov/api/citations/19890011970/downloads/19890011970.pdf) ***12.*** In D.R. Congo the age of the Omeonga structure can be constrained to the Late Cretaceous-Cenozoic, according to the youngest units in which the ring structure was formed: [Omeonga––A possible large impact structure on the Eastern Kasai Province(D.R. Congo)](https://onlinelibrary.wiley.com/doi/epdf/10.1111/j.1945-5100.2011.01296.x) That's right; there are at least 11 additional K/T boundary suspects or *confirmed* "impact craters." Coupled with what else was occurring on Earth, this strongly suggests the craters are the result of the Earth's own processes. # Additional Events at the K/T Boundary: A major step in Himalayas mountain formation process occurred; Trans-Tethyan subduction zone between India and Eurasia active 66-62Ma: [Paleocene latitude of the Kohistan–Ladakh arc indicates multistage India–Eurasia collision](https://www.pnas.org/doi/abs/10.1073/pnas.2009039117) Tibet's Dianzhong Formation 66-63Ma: [Origin of the volcanic rocks in Dianzhong Formation, central Lhasa Terrane, Tibet: implication for the genesis of syn-collisional magmatism and Neo-Tethyan slab roll-back](https://www.tandfonline.com/doi/abs/10.1080/00206814.2022.2031314) Mingshui Formation also dates ~66Ma: [Mesozoic–Cenozoic tectonic evolution and dynamics of the Songliao Basin, NE Asia: Implications for the closure of the Paleo-Asian Ocean and Mongol-Okhotsk Ocean and subduction of the Paleo-Pacific Ocean](https://www.sciencedirect.com/science/article/abs/pii/S0012825220305171) The Alps have several locations with apparent ages ~66Ma: [Preservation of sub-microscopic structural relicts in micas from the Gran Paradiso Massif (Western Alps): Implications for 40Ar–39Ar geochronology](https://www.sciencedirect.com/science/article/abs/pii/S001670371300330X) [Time constraints on the metamorphic and structural evolution of the southern Sesia-Lanzo Zone, Western Italian Alps](https://web.archive.org/web/20180604070412id_/http://www.minersoc.org/pages/Archive-MM/Volume_58A/58A-2-758.pdf) [Metamorphic evolution of the Sesia-Lanzo Zone, Western Alps: time constraints from multi-system geochronology](https://link.springer.com/article/10.1007/s004100050241) Late Cretaceous mixed sediments along the Argentine Margin indicate a change from gravity dominated deposition style along the margin to bottom current dominated 66Ma marking the cessation of mixed system due to bottom current intensification and transition to a pure contourite system: [A Late Cretaceous mixed (turbidite-contourite) system along the Argentine Margin: Paleoceanographic and conceptual implications](https://www.sciencedirect.com/science/article/pii/S0264817220305511) Moeraki Boulders, Koutu, and other large round boulders of New Zealand date to 66Ma: [Treasured Spheres Protecting New Zealand's Heritage of Spherical Concretions](https://www.researchgate.net/publication/261258771_Treasured_spheres_Protecting_New_Zealand%27s_heritage_of_spherical_concretions) What is believed to be [A Mega-Tsunami Deposit at the KT Boundary on Tora Coast of New Zealand](https://www.youtube.com/watch?v=3RI1QtF-Tuk&ab_channel=OutThereLearning) Central and western Solomon Islands are composed of exceptionally thick succession of Lower Cretaceous to Holocene rocks: [GEOLOGY OF THE CENTRAL AND WESTERN SOLOMON ISLANDS](https://spccfpstore1.blob.core.windows.net/digitallibrary-docs/files/8e/8ec636d7bd6de607fa100c7a12e79b69.pdf?sv=2015-12-11&sr=b&sig=ismMjrsPNaIieQLioVglWF9cUZe02Wi2v9HdfrY5lOA%3D&se=2023-06-26T16%3A31%3A43Z&sp=r&rscc=public%2C%20max-age%3D864000%2C%20max-stale%3D86400&rsct=application%2Fpdf&rscd=inline%3B%20filename%3D%22TR0043.pdf%22#page=108) Formation of the East Sikhote-Alin area of far east Russia included eruptions from 66Ma to 46Ma: [Late Cretaceous palaeomagnetic results from Sikhote Alin, far eastern Russia: tectonic implications for the eastern margin of the Mongolia Block](https://academic.oup.com/gji/article/152/1/202/702390) The Louisville Seamount Chain in the Pacific Ocean contains the Osbourn Seamount at the westernmost end of the chain which has rocks dated to ~66Ma: Seamounts, Islands, and Atolls, Volume 43 [Petrologic Evolution of the Louisville Seamount Chain](https://agupubs.onlinelibrary.wiley.com/doi/abs/10.1029/GM043p0235) [Isotopic Evidence for a Hotspot Origin of the Louisville Seamount Chain](https://www.researchgate.net/publication/258963769_Isotopic_Evidence_for_a_Hotspot_Origin_of_the_Louisville_Seamount_Chain) Cerro Quema and other Gold-Copper deposits throughout the world, especially around the Pacific Rim, were formed ~66Ma: [Cerro Quema (Azuero Peninsula, Panama): Geology, Alteration, Mineralization, and Geochronology of a Volcanic Dome-Hosted High Sulfidation Au-Cu Deposit](https://pubs.geoscienceworld.org/segweb/economicgeology/article-abstract/111/2/287/128817/Cerro-Quema-Azuero-Peninsula-Panama-Geology) Ore Deposits in Butte, Montana date to the 67-65Ma, and similar ages: [Two-event lode-ore deposition at Butte, USA: 40Ar/39Ar and U-Pb documentation of Ag-Au-polymetallic lodes overprinted by younger stockwork Cu-Mo ores and penecontemporaneous Cu lodes](https://www.sciencedirect.com/science/article/abs/pii/S0169136818300325) |
| json metadata | {"tags":["geology"],"links":["https://steemit.com/science/@stevescully/events-at-the-kt-boundary","https://www.earthdoc.org/content/papers/10.3997/2214-4609-pdb.215.sbgf220","https://www.researchgate.net/publication/325317164_The_Cretaceous-Tertiary_boundary_in_the_context_of_impact_geology_and_sedimentary_record-an_analytical_review_of_10_years_of_researches_in_Brazil","https://www.nature.com/articles/nature00914","https://adsabs.harvard.edu/pdf/1978LPI.....9..433G","https://www.researchgate.net/publication/248516714_The_Jebel_Hadid_structure_Al_Kufrah_Basin_SE_Libya-A_possible_impact_structure_and_potential_hydrocarbon_trap","https://onlinelibrary.wiley.com/doi/abs/10.1111/maps.13766","https://books.google.com/books?hl=en&lr=&id=naUIAQAAQBAJ&oi=fnd&pg=PA233&dq=ust-kara+crater&ots=-rdFZBbbCb&sig=uGqpK1cwuduM7ljUgFOlU5FfvyA#v=onepage&q=ust-kara%20crater&f=false","https://ntrs.nasa.gov/api/citations/19890011970/downloads/19890011970.pdf","https://onlinelibrary.wiley.com/doi/epdf/10.1111/j.1945-5100.2011.01296.x","https://www.pnas.org/doi/abs/10.1073/pnas.2009039117","https://www.tandfonline.com/doi/abs/10.1080/00206814.2022.2031314","https://www.sciencedirect.com/science/article/abs/pii/S0012825220305171","https://www.sciencedirect.com/science/article/abs/pii/S001670371300330X","https://web.archive.org/web/20180604070412id_/http://www.minersoc.org/pages/Archive-MM/Volume_58A/58A-2-758.pdf","https://link.springer.com/article/10.1007/s004100050241","https://www.sciencedirect.com/science/article/pii/S0264817220305511","https://www.researchgate.net/publication/261258771_Treasured_spheres_Protecting_New_Zealand%27s_heritage_of_spherical_concretions","https://www.youtube.com/watch?v=3RI1QtF-Tuk&ab_channel=OutThereLearning","https://spccfpstore1.blob.core.windows.net/digitallibrary-docs/files/8e/8ec636d7bd6de607fa100c7a12e79b69.pdf?sv=2015-12-11&sr=b&sig=ismMjrsPNaIieQLioVglWF9cUZe02Wi2v9HdfrY5lOA%3D&se=2023-06-26T16%3A31%3A43Z&sp=r&rscc=public%2C%20max-age%3D864000%2C%20max-stale%3D86400&rsct=application%2Fpdf&rscd=inline%3B%20filename%3D%22TR0043.pdf%22#page=108","https://academic.oup.com/gji/article/152/1/202/702390","https://agupubs.onlinelibrary.wiley.com/doi/abs/10.1029/GM043p0235","https://www.researchgate.net/publication/258963769_Isotopic_Evidence_for_a_Hotspot_Origin_of_the_Louisville_Seamount_Chain","https://pubs.geoscienceworld.org/segweb/economicgeology/article-abstract/111/2/287/128817/Cerro-Quema-Azuero-Peninsula-Panama-Geology","https://www.sciencedirect.com/science/article/abs/pii/S0169136818300325"],"app":"steemit/0.2","format":"markdown"} |
| parent author | |
| parent permlink | geology |
| permlink | events-of-the-kt-boundary-part-2 |
| title | Events of the KT Boundary: Part 2 |
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"body": "[Events of the KT Boundary](https://steemit.com/science/@stevescully/events-at-the-kt-boundary) lists several major events at the K/T Boundary for consideration. Here is a continuation of the list.\n\nAdditional geological events dated to ~66Ma:\n\nMORE impacts:\n\nAfter \n1. Chicxulub Crater, \n2. Nadir Crater, \n3. Boltysh Crater, and \n4. Shiva Crater, all discussed previously,\n\n5. Tefe River Structure in Brazil dates to KT boundary: [Geophysical Evidence Of A Possible Impact Structure At The K-T Boundary Of The Solimões Basin, Brazil](https://www.earthdoc.org/content/papers/10.3997/2214-4609-pdb.215.sbgf220)\n[The Cretaceous-Tertiary boundary in the context of impact geology and sedimentary record-an analytical review of 10 years of researches in Brazil](https://www.researchgate.net/publication/325317164_The_Cretaceous-Tertiary_boundary_in_the_context_of_impact_geology_and_sedimentary_record-an_analytical_review_of_10_years_of_researches_in_Brazil)\n\n6. The Silverpit Crater is controversially ~65-60Ma, and debated on whether it is an impact structure or a pull-apart basin: [A 20-km-diameter multi-ringed impact structure in the North Sea](https://www.nature.com/articles/nature00914)\n\n7. Dumas Magnetic Anomaly in Canada, believed to be from a meteorite impact, formed late cretaceous, 70+/- 5Ma: [Magnetic Fields Associated with a Probable Late Cretaceous Astrobleme at Dumas, Saskatchewan](https://adsabs.harvard.edu/pdf/1978LPI.....9..433G)\n\n8. The Jebel Hadid structure in Libya was formed after early Cretaceous and prior to late Miocene rivers and is compared to the Tin Bider impact crater in Algeria: [The Jebel Hadid structure (Al Kufrah Basin, SE Libya)—A possible impact structure and potential hydrocarbon trap?](https://www.researchgate.net/publication/248516714_The_Jebel_Hadid_structure_Al_Kufrah_Basin_SE_Libya-A_possible_impact_structure_and_potential_hydrocarbon_trap)\n\n9. The Tin Bider Impact is poorly constrained to <66Ma by stratigraphy, the youngest geological unit affected by the event being ~66Ma limestones: [Shock-metamorphic microstructures in quartz grains from Albian sandstones from the Tin Bider impact structure, Algeria](https://onlinelibrary.wiley.com/doi/abs/10.1111/maps.13766)\n\n10, 11. Kara/Ust-Kara twin impact structure dates variously to 60Ma-70Ma and has been considered as a possible K/T Boundary event: [The Kara/Ust-Kara twin impact structure; A Large-scale impact event in the Late Cretaceous](https://books.google.com/books?hl=en&lr=&id=naUIAQAAQBAJ&oi=fnd&pg=PA233&dq=ust-kara+crater&ots=-rdFZBbbCb&sig=uGqpK1cwuduM7ljUgFOlU5FfvyA#v=onepage&q=ust-kara%20crater&f=false)\n\n[The Kara and Ust-Kara impact structures (USSR) and their relevance to the K/T boundary event](https://ntrs.nasa.gov/api/citations/19890011970/downloads/19890011970.pdf)\n\n***12.*** In D.R. Congo the age of the Omeonga structure can be constrained to the Late Cretaceous-Cenozoic, according to the youngest units in which the ring structure was formed: [Omeonga––A possible large impact structure on the Eastern Kasai Province(D.R. Congo)](https://onlinelibrary.wiley.com/doi/epdf/10.1111/j.1945-5100.2011.01296.x)\n\nThat's right; there are at least 11 additional K/T boundary suspects or *confirmed* \"impact craters.\" Coupled with what else was occurring on Earth, this strongly suggests the craters are the result of the Earth's own processes.\n\n# Additional Events at the K/T Boundary:\n\nA major step in Himalayas mountain formation process occurred; Trans-Tethyan subduction zone between India and Eurasia active 66-62Ma: [Paleocene latitude of the Kohistan–Ladakh arc indicates multistage India–Eurasia collision](https://www.pnas.org/doi/abs/10.1073/pnas.2009039117)\n\nTibet's Dianzhong Formation 66-63Ma: [Origin of the volcanic rocks in Dianzhong Formation, central Lhasa Terrane, Tibet: implication for the genesis of syn-collisional magmatism and Neo-Tethyan slab roll-back](https://www.tandfonline.com/doi/abs/10.1080/00206814.2022.2031314)\n\nMingshui Formation also dates ~66Ma: [Mesozoic–Cenozoic tectonic evolution and dynamics of the Songliao Basin, NE Asia: Implications for the closure of the Paleo-Asian Ocean and Mongol-Okhotsk Ocean and subduction of the Paleo-Pacific Ocean](https://www.sciencedirect.com/science/article/abs/pii/S0012825220305171)\n\nThe Alps have several locations with apparent ages ~66Ma: [Preservation of sub-microscopic structural relicts in micas from the Gran Paradiso Massif (Western Alps): Implications for 40Ar–39Ar geochronology](https://www.sciencedirect.com/science/article/abs/pii/S001670371300330X)\n\n[Time constraints on the metamorphic and structural evolution of the southern Sesia-Lanzo Zone, Western Italian Alps](https://web.archive.org/web/20180604070412id_/http://www.minersoc.org/pages/Archive-MM/Volume_58A/58A-2-758.pdf)\n\n[Metamorphic evolution of the Sesia-Lanzo Zone, Western Alps: time constraints from multi-system geochronology](https://link.springer.com/article/10.1007/s004100050241)\n\nLate Cretaceous mixed sediments along the Argentine Margin indicate a change from gravity dominated deposition style along the margin to bottom current dominated 66Ma marking the cessation of mixed system due to bottom current intensification and transition to a pure contourite system: [A Late Cretaceous mixed (turbidite-contourite) system along the Argentine Margin: Paleoceanographic and conceptual implications](https://www.sciencedirect.com/science/article/pii/S0264817220305511)\n\nMoeraki Boulders, Koutu, and other large round boulders of New Zealand date to 66Ma: [Treasured Spheres Protecting New Zealand's Heritage of Spherical Concretions](https://www.researchgate.net/publication/261258771_Treasured_spheres_Protecting_New_Zealand%27s_heritage_of_spherical_concretions)\n\nWhat is believed to be [A Mega-Tsunami Deposit at the KT Boundary on Tora Coast of New Zealand](https://www.youtube.com/watch?v=3RI1QtF-Tuk&ab_channel=OutThereLearning)\n\nCentral and western Solomon Islands are composed of exceptionally thick succession of Lower Cretaceous to Holocene rocks: [GEOLOGY OF THE CENTRAL AND WESTERN SOLOMON ISLANDS](https://spccfpstore1.blob.core.windows.net/digitallibrary-docs/files/8e/8ec636d7bd6de607fa100c7a12e79b69.pdf?sv=2015-12-11&sr=b&sig=ismMjrsPNaIieQLioVglWF9cUZe02Wi2v9HdfrY5lOA%3D&se=2023-06-26T16%3A31%3A43Z&sp=r&rscc=public%2C%20max-age%3D864000%2C%20max-stale%3D86400&rsct=application%2Fpdf&rscd=inline%3B%20filename%3D%22TR0043.pdf%22#page=108)\n\nFormation of the East Sikhote-Alin area of far east Russia included eruptions from 66Ma to 46Ma: [Late Cretaceous palaeomagnetic results from Sikhote Alin, far eastern Russia: tectonic implications for the eastern margin of the Mongolia Block](https://academic.oup.com/gji/article/152/1/202/702390)\n\nThe Louisville Seamount Chain in the Pacific Ocean contains the Osbourn Seamount at the westernmost end of the chain which has rocks dated to ~66Ma: Seamounts, Islands, and Atolls, Volume 43 [Petrologic Evolution of the Louisville Seamount Chain](https://agupubs.onlinelibrary.wiley.com/doi/abs/10.1029/GM043p0235)\n\n[Isotopic Evidence for a Hotspot Origin of the Louisville Seamount Chain](https://www.researchgate.net/publication/258963769_Isotopic_Evidence_for_a_Hotspot_Origin_of_the_Louisville_Seamount_Chain)\n\nCerro Quema and other Gold-Copper deposits throughout the world, especially around the Pacific Rim, were formed ~66Ma: [Cerro Quema (Azuero Peninsula, Panama): Geology, Alteration, Mineralization, and Geochronology of a Volcanic Dome-Hosted High Sulfidation Au-Cu Deposit](https://pubs.geoscienceworld.org/segweb/economicgeology/article-abstract/111/2/287/128817/Cerro-Quema-Azuero-Peninsula-Panama-Geology)\n\nOre Deposits in Butte, Montana date to the 67-65Ma, and similar ages: [Two-event lode-ore deposition at Butte, USA: 40Ar/39Ar and U-Pb documentation of Ag-Au-polymetallic lodes overprinted by younger stockwork Cu-Mo ores and penecontemporaneous Cu lodes](https://www.sciencedirect.com/science/article/abs/pii/S0169136818300325)",
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}steemeggsent 0.001 STEEM to @stevescully- "Accumulate free upvotes on your posts every 6 hours! All you need to do is vote our witness account -> se-witness as one of your 30 witness votes. -> See actual rewards not just 0.001 every day. http..."2023/01/11 22:07:03
steemeggsent 0.001 STEEM to @stevescully- "Accumulate free upvotes on your posts every 6 hours! All you need to do is vote our witness account -> se-witness as one of your 30 witness votes. -> See actual rewards not just 0.001 every day. http..."
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| amount | 0.001 STEEM |
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| memo | Accumulate free upvotes on your posts every 6 hours! All you need to do is vote our witness account -> se-witness as one of your 30 witness votes. -> See actual rewards not just 0.001 every day. https://steemlogin.com/sign/account-witness-vote?witness=se-witness&approve=1 |
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}jayleesteemupvoted (100.00%) @stevescully / events-at-the-kt-boundary2022/12/21 20:53:48
jayleesteemupvoted (100.00%) @stevescully / events-at-the-kt-boundary
2022/12/21 20:53:48
| author | stevescully |
| permlink | events-at-the-kt-boundary |
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}exnihilo.witnesssent 0.001 STEEM to @stevescully- "By casting your witness vote on @exnihilo.witness you will passively earn and be rewarded just for voting. More information : https://steemit.com/@exnihilo.witness"2022/12/21 20:34:45
exnihilo.witnesssent 0.001 STEEM to @stevescully- "By casting your witness vote on @exnihilo.witness you will passively earn and be rewarded just for voting. More information : https://steemit.com/@exnihilo.witness"
2022/12/21 20:34:45
| amount | 0.001 STEEM |
| from | exnihilo.witness |
| memo | By casting your witness vote on @exnihilo.witness you will passively earn and be rewarded just for voting. More information : https://steemit.com/@exnihilo.witness |
| to | stevescully |
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}stevescullypublished a new post: events-at-the-kt-boundary2022/12/21 20:34:21
stevescullypublished a new post: events-at-the-kt-boundary
2022/12/21 20:34:21
| author | stevescully |
| body | @@ -51,16 +51,56 @@ imeframe + of the Chicxulub crater and KT Boundary .%0A%0ANadir |
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}stevescullypublished a new post: events-at-the-kt-boundary2022/12/21 20:33:36
stevescullypublished a new post: events-at-the-kt-boundary
2022/12/21 20:33:36
| author | stevescully |
| body | A working list of what I've come across for this timeframe. Nadir Crater also occurred offshore of West Africa 66Ma: [The Nadir Crater offshore West Africa: A candidate Cretaceous-Paleogene impact structure](https://www.science.org/doi/pdf/10.1126/sciadv.abn3096?fbclid=IwAR0Y9YzBrvLIk79hTeTNuJpA-BGqomFPFkSW6I50gTaDdkTusXIrc3J9p08) The Boltysh Crater is dated to the 65.17 +/- 0.64Ma: [Boltysh, another end-Cretaceous impact](https://onlinelibrary.wiley.com/doi/pdfdirect/10.1111/j.1945-5100.2002.tb00875.x) The potential Shiva Crater is also dated to the same time frame: [SHIVA STRUCTURE: A POSSIBLE KT BOUNDARY IMPACT CRATER ON THE WESTERN SHELF OF INDIA](https://www.researchgate.net/publication/228719850_Shiva_structure_a_possible_KT_boundary_impact_crater_on_the_western_shelf_of_India) The Deccan Traps are dated in the general range of 66Ma, such as here: [40Ar-39Ar age of a lava flow from the Bhimashankar Formation, Giravali Ghat, Deccan Traps](https://www.ias.ac.in/article/fulltext/jess/113/04/0755-0758) Within the Deccan Traps, many plutonic complexes formed also in the general time frame: [Widespread silicic and alkaline magmatism synchronous with the Deccan 2 Traps flood basalts, India](https://www.sciencedirect.com/science/article/abs/pii/S0012821X20305604?fr=RR-2&ref=pdf_download&rr=77d35f5e3ab7d4f1) Mount Girnar dates to ~66Ma: [Mantle and Crustal Contributions to the Mount Girnar Alkaline Plutonic Complex and the Circum-Girnar Mafic-Silicic Intrusions of Saurashtra, Northwestern Deccan Traps](https://www.researchgate.net/publication/359368565_Mantle_and_crustal_contributions_to_the_Mount_Girnar_alkaline_plutonic_complex_and_the_circum-Girnar_mafic-silicic_intrusions_of_Saurashtra_northwestern_Deccan_Traps_2022) "Stratigraphy of Powder River and Bighorn basins adjacent to the Bighorn Mountains indicate that the main phase of uplift and exhumation of the range occurred in the latest Cretaceous-earliest Tertiary,": [Influence of crystal size on apatite (U-Th)/He thermochronology: an example from the Bighorn Mountains, Wyoming](https://www.geo.arizona.edu/~reiners/ReinersandFarley2001.pdf) The Labrador margin between Greenland and North America at 66Ma began sinistral faulting, uplifting, and spreading with major volcanics (Figure 3): [A new model for the Paleogene motion of Greenland relative to North America: Plate reconstructions of the Davis Strait and Nares Strait regions between Canada and Greenland](https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2011JB008942) The Trans Sahara Seaway environment changed from 72 to 66Ma, and last phases were through 56Ma: [Paleoenvironment and paleoclimate of the Late Cretaceous Ise Formation, Eastern Dahomey Basin.](https://assets.researchsquare.com/files/rs-1453685/v1/296ad01f-f7f5-4fba-bfa6-27dd6f855238.pdf?c=1648047902) Paleomagnetic inclination of Wrangellia indicates motion from 85-65Ma: [A Paleomagnetic Study of Three Granite Plutons Exposed in the Cascades Mountains, Washington](https://www.geology.cwu.edu/facstaff/nick/gBAJA/1973_Noson_MS_Thesis.pdf) Onset of dextral slip on northern splays of the Border Ranges fault system in the Cordilleran orogen considered a "gold event": [Orogenic gold and evolution of the Cordilleran orogen](https://www.researchgate.net/publication/235625951_Orogenic_gold_and_evolution_of_the_Cordilleran_orogen) Marine flooding in southern Wyoming from 65-63Ma: [Paleocene (65–63 and 58.5 ma) marine flooding and 62–60 ma sediment bypass in southern Wyoming, U.S.A.: Implications for Laramide sediment flux to the Gulf of Mexico](https://pubs.geoscienceworld.org/sepm/jsedres/article-abstract/92/10/859/617903/Paleocene-65-63-and-58-5-ma-marine-flooding-and-62) Regarding Panama, "With respect to the initiation of subduction-zone magmatism (66 Ma, see following), it is interesting to note that the accretion of seamounts from the Galapagos hotspot track (ocean-island basalts) commenced at 66 Ma (data compilation in Hoernle et al., 2004).": [Geochemical evolution of igneous rocks and changing magma sources during the formation and closure of the Central American land bridge of Panama](https://www.researchgate.net/publication/301673959_Magmatic_history_and_evolution_of_the_Central_American_Land_Bridge_in_Panama_since_Cretaceous_times) In the forming of the Caribbeans, "relative motion between North America and South America with at least a component of divergence continued until ~66Ma": [An integrative geologic, geochronologic and geochemical study of Gorgona Island, Colombia: Implications for the formation of the Caribbean Large Igneous Province](https://stri-apps.si.edu/docs/publications/pdfs/STRI-W_Jaramillo_2011_Serrano_Gorgona_Luca.pdf) Eolian dust was deposited on the Mid-Pacific Mountains from 112Ma-66Ma: ["Late Cretaceous History of Eolian Deposition in the Mid-Pacific Mountains, Central North Pacific Ocean," Rea and Janecek (1981)](https://deepblue.lib.umich.edu/bitstream/handle/2027.42/24203/0000462.pdf%3Bjsessionid%3D28E5C27D9E90ECBB0E3CAB8FC1D36396?sequence%3D1) The main island of New Caledonia, Grande Terre, was submerged between 75 and 60Ma: [Chapter 8 Palaeobiogeography of New Caledonia](https://www.lyellcollection.org/doi/10.1144/M51-2019-31) The mean age of oceanic crust is 64.2Ma: [A Global Data Set of Present-Day Oceanic Crustal Age and Seafloor Spreading Parameters](https://agupubs.onlinelibrary.wiley.com/doi/full/10.1029/2020GC009214) |
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"body": "A working list of what I've come across for this timeframe.\n\nNadir Crater also occurred offshore of West Africa 66Ma: [The Nadir Crater offshore West Africa: A candidate Cretaceous-Paleogene impact structure](https://www.science.org/doi/pdf/10.1126/sciadv.abn3096?fbclid=IwAR0Y9YzBrvLIk79hTeTNuJpA-BGqomFPFkSW6I50gTaDdkTusXIrc3J9p08)\n\nThe Boltysh Crater is dated to the 65.17 +/- 0.64Ma: [Boltysh, another end-Cretaceous impact](https://onlinelibrary.wiley.com/doi/pdfdirect/10.1111/j.1945-5100.2002.tb00875.x)\n\nThe potential Shiva Crater is also dated to the same time frame: [SHIVA STRUCTURE: A POSSIBLE KT BOUNDARY IMPACT CRATER ON THE WESTERN SHELF OF INDIA](https://www.researchgate.net/publication/228719850_Shiva_structure_a_possible_KT_boundary_impact_crater_on_the_western_shelf_of_India)\n\nThe Deccan Traps are dated in the general range of 66Ma, such as here: [40Ar-39Ar age of a lava flow from the Bhimashankar Formation, Giravali Ghat, Deccan Traps](https://www.ias.ac.in/article/fulltext/jess/113/04/0755-0758)\n\nWithin the Deccan Traps, many plutonic complexes formed also in the general time frame: [Widespread silicic and alkaline magmatism synchronous with the Deccan 2 Traps flood basalts, India](https://www.sciencedirect.com/science/article/abs/pii/S0012821X20305604?fr=RR-2&ref=pdf_download&rr=77d35f5e3ab7d4f1)\n\nMount Girnar dates to ~66Ma: [Mantle and Crustal Contributions to the Mount Girnar Alkaline Plutonic Complex and the Circum-Girnar Mafic-Silicic Intrusions of Saurashtra, Northwestern Deccan Traps](https://www.researchgate.net/publication/359368565_Mantle_and_crustal_contributions_to_the_Mount_Girnar_alkaline_plutonic_complex_and_the_circum-Girnar_mafic-silicic_intrusions_of_Saurashtra_northwestern_Deccan_Traps_2022)\n\n\"Stratigraphy of Powder River and Bighorn basins adjacent to the Bighorn Mountains indicate that the main phase of uplift and exhumation of the range occurred in the latest Cretaceous-earliest Tertiary,\": [Influence of crystal size on apatite (U-Th)/He thermochronology: an example from the Bighorn Mountains, Wyoming](https://www.geo.arizona.edu/~reiners/ReinersandFarley2001.pdf)\n\nThe Labrador margin between Greenland and North America at 66Ma began sinistral faulting, uplifting, and spreading with major volcanics (Figure 3): [A new model for the Paleogene motion of Greenland relative to North America: Plate reconstructions of the Davis Strait and Nares Strait regions between Canada and Greenland](https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2011JB008942)\n\nThe Trans Sahara Seaway environment changed from 72 to 66Ma, and last phases were through 56Ma: [Paleoenvironment and paleoclimate of the Late Cretaceous Ise Formation, Eastern Dahomey Basin.](https://assets.researchsquare.com/files/rs-1453685/v1/296ad01f-f7f5-4fba-bfa6-27dd6f855238.pdf?c=1648047902)\n\nPaleomagnetic inclination of Wrangellia indicates motion from 85-65Ma: [A Paleomagnetic Study of Three Granite Plutons Exposed in the Cascades Mountains, Washington](https://www.geology.cwu.edu/facstaff/nick/gBAJA/1973_Noson_MS_Thesis.pdf)\n\nOnset of dextral slip on northern splays of the Border Ranges fault system in the Cordilleran orogen considered a \"gold event\": [Orogenic gold and evolution of the Cordilleran orogen](https://www.researchgate.net/publication/235625951_Orogenic_gold_and_evolution_of_the_Cordilleran_orogen)\n\nMarine flooding in southern Wyoming from 65-63Ma: [Paleocene (65–63 and 58.5 ma) marine flooding and 62–60 ma sediment bypass in southern Wyoming, U.S.A.: Implications for Laramide sediment flux to the Gulf of Mexico](https://pubs.geoscienceworld.org/sepm/jsedres/article-abstract/92/10/859/617903/Paleocene-65-63-and-58-5-ma-marine-flooding-and-62)\n\nRegarding Panama, \"With respect to the initiation of subduction-zone magmatism (66 Ma, see following), it is interesting to note that the accretion of seamounts from the Galapagos hotspot track (ocean-island basalts) commenced at 66 Ma (data compilation in Hoernle et al., 2004).\": [Geochemical evolution of igneous rocks and changing magma sources during the formation and closure of the Central American land bridge of Panama](https://www.researchgate.net/publication/301673959_Magmatic_history_and_evolution_of_the_Central_American_Land_Bridge_in_Panama_since_Cretaceous_times)\n\nIn the forming of the Caribbeans, \"relative motion between North America and South America with at least a component of divergence continued until ~66Ma\": [An integrative geologic, geochronologic and geochemical study of Gorgona Island, Colombia: Implications for the formation of the Caribbean Large Igneous Province](https://stri-apps.si.edu/docs/publications/pdfs/STRI-W_Jaramillo_2011_Serrano_Gorgona_Luca.pdf)\n\nEolian dust was deposited on the Mid-Pacific Mountains from 112Ma-66Ma: [\"Late Cretaceous History of Eolian Deposition in the Mid-Pacific Mountains, Central North Pacific Ocean,\" Rea and Janecek (1981)](https://deepblue.lib.umich.edu/bitstream/handle/2027.42/24203/0000462.pdf%3Bjsessionid%3D28E5C27D9E90ECBB0E3CAB8FC1D36396?sequence%3D1)\n\nThe main island of New Caledonia, Grande Terre, was submerged between 75 and 60Ma: [Chapter 8 Palaeobiogeography of New Caledonia](https://www.lyellcollection.org/doi/10.1144/M51-2019-31)\n\nThe mean age of oceanic crust is 64.2Ma: [A Global Data Set of Present-Day Oceanic Crustal Age and Seafloor Spreading Parameters](https://agupubs.onlinelibrary.wiley.com/doi/full/10.1029/2020GC009214)",
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}stevescullypublished a new post: damodar-kund-the-shaligram-to-rule-them-all2022/10/04 14:37:21
stevescullypublished a new post: damodar-kund-the-shaligram-to-rule-them-all
2022/10/04 14:37:21
| author | stevescully |
| body | @@ -1,15 +1,11 @@ In -the remote m |
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| parent permlink | geology |
| permlink | damodar-kund-the-shaligram-to-rule-them-all |
| title | Damodar Kund: The Shaligram to rule them all |
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}stevescullypublished a new post: damodar-kund-the-shaligram-to-rule-them-all2022/10/04 14:05:18
stevescullypublished a new post: damodar-kund-the-shaligram-to-rule-them-all
2022/10/04 14:05:18
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| parent author | |
| parent permlink | geology |
| permlink | damodar-kund-the-shaligram-to-rule-them-all |
| title | Damodar Kund: The Shaligram to rule them all |
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}stevescullypublished a new post: damodar-kund-the-shaligram-to-rule-them-all2022/10/04 13:59:48
stevescullypublished a new post: damodar-kund-the-shaligram-to-rule-them-all
2022/10/04 13:59:48
| author | stevescully |
| body | @@ -3603,8 +3603,384 @@ fossils. +%0A%0A!%5Bimage.png%5D(https://cdn.steemitimages.com/DQmYfSVtK6nmXhoKMxjpFe3hFNK3QQomp2qMxuGh4899xyY/image.png)%0A%0ANotice how the two %22fossils%22 are coalesced and their structure is *dependent on the other*? This is the case for flowing energies, but not for shells in a rock matrix.%0A%0A!%5Bimage.png%5D(https://cdn.steemitimages.com/DQmYb9tuAPy79VgGVE7Cgz8Cfsz74Yx27ngf2CpmSCHtE9f/image.png) |
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| parent author | |
| parent permlink | geology |
| permlink | damodar-kund-the-shaligram-to-rule-them-all |
| title | Damodar Kund: The Shaligram to rule them all |
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"body": "@@ -3603,8 +3603,384 @@\n fossils.\n+%0A%0A!%5Bimage.png%5D(https://cdn.steemitimages.com/DQmYfSVtK6nmXhoKMxjpFe3hFNK3QQomp2qMxuGh4899xyY/image.png)%0A%0ANotice how the two %22fossils%22 are coalesced and their structure is *dependent on the other*? This is the case for flowing energies, but not for shells in a rock matrix.%0A%0A!%5Bimage.png%5D(https://cdn.steemitimages.com/DQmYb9tuAPy79VgGVE7Cgz8Cfsz74Yx27ngf2CpmSCHtE9f/image.png)\n",
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"title": "Damodar Kund: The Shaligram to rule them all"
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}stevescullypublished a new post: damodar-kund-the-shaligram-to-rule-them-all2022/10/04 13:56:33
stevescullypublished a new post: damodar-kund-the-shaligram-to-rule-them-all
2022/10/04 13:56:33
| author | stevescully |
| body | In the remote mountains of the Himalayas, [shaligrams](https://en.wikipedia.org/wiki/Shaligram) are found in the Gandaki River.  Tracing their path back to their source, shaligrams are said to come from Damodar Kund.  The terrain leading up to this lake is filled with signs of processes involved in the shaligram formation. While shaligrams are considered to be fossils of creatures called ammonites, Damodar Kund raises questions regarding whether or not the fossils are from creatures that once lived.  [En route](https://youtu.be/daKxy8EaPGw?t=363) Signs of sections of rock filled with complex designs are not limited to portable stones, but the same structures can be seen in larger-scale systems like hills and the mountainsides.   [Holes in stones](https://youtu.be/AHZVTr0shhI?t=451) These shapes and openings are reminiscent of shaligrams themselves:  Curiously, these lakes are separated by a divided center having light-colored stones in paths.  [Source](https://www.youtube.com/watch?v=Ij5pCCAxl1E&t=1136s)   [Google Maps](https://goo.gl/maps/RFybfh2qx85wR64E8) These lakes appear to be openings into the side of a shaligram.     As can be seen from the formation of shaligrams, they tend to create openings along the edge of the structure. Where the overall vortex is not cleanly stripped of rock, there are walls that stand but that become chemically modified as well as begin to contain larger holes in *along the edges* of the carved opening. Moreover, the region additionally has distinct chakras, as the spirals are termed in shaligrams, which are in an opening gouged into the ground.     Meanwhile, Damodar Kund itself appears like looking into a viewing chamber of a shaligram:   # Conclusion Shaligrams are not fossils. |
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| parent author | |
| parent permlink | geology |
| permlink | damodar-kund-the-shaligram-to-rule-them-all |
| title | Damodar Kund: The Shaligram to rule them all |
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"body": "In the remote mountains of the Himalayas, [shaligrams](https://en.wikipedia.org/wiki/Shaligram) are found in the Gandaki River.\n\n\n\n\nTracing their path back to their source, shaligrams are said to come from Damodar Kund.\n\n\n\nThe terrain leading up to this lake is filled with signs of processes involved in the shaligram formation. While shaligrams are considered to be fossils of creatures called ammonites, Damodar Kund raises questions regarding whether or not the fossils are from creatures that once lived.\n\n\n[En route](https://youtu.be/daKxy8EaPGw?t=363)\n\nSigns of sections of rock filled with complex designs are not limited to portable stones, but the same structures can be seen in larger-scale systems like hills and the mountainsides.\n\n\n[Holes in stones](https://youtu.be/AHZVTr0shhI?t=451) \n\nThese shapes and openings are reminiscent of shaligrams themselves:\n\n\nCuriously, these lakes are separated by a divided center having light-colored stones in paths.\n\n[Source](https://www.youtube.com/watch?v=Ij5pCCAxl1E&t=1136s)\n\n\n\n[Google Maps](https://goo.gl/maps/RFybfh2qx85wR64E8)\n\nThese lakes appear to be openings into the side of a shaligram.\n\n\n\n\n\n\nAs can be seen from the formation of shaligrams, they tend to create openings along the edge of the structure. Where the overall vortex is not cleanly stripped of rock, there are walls that stand but that become chemically modified as well as begin to contain larger holes in *along the edges* of the carved opening.\n\nMoreover, the region additionally has distinct chakras, as the spirals are termed in shaligrams, which are in an opening gouged into the ground.\n\n\n\n\n\n\n\n\n\nMeanwhile, Damodar Kund itself appears like looking into a viewing chamber of a shaligram:\n\n\n\n\n\n# Conclusion\nShaligrams are not fossils.",
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}stevescullypublished a new post: shaligrams-are-not-fossils2022/09/28 02:41:27
stevescullypublished a new post: shaligrams-are-not-fossils
2022/09/28 02:41:27
| author | stevescully |
| body | @@ -145,19 +145,16 @@ fossils -of that dat |
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| parent permlink | geology |
| permlink | shaligrams-are-not-fossils |
| title | Shaligrams Are Not Fossils |
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}stevescullypublished a new post: shaligrams-are-not-fossils2022/09/28 02:38:27
stevescullypublished a new post: shaligrams-are-not-fossils
2022/09/28 02:38:27
| author | stevescully |
| body | # Ten Shaligrams that demonstrate they are not fossils Historically, [shaligrams](https://en.wikipedia.org/wiki/Shaligram) have been considered fossils of that date to around 400Ma and became extinct in 66Ma. They are considered a specific variety of ammonite that is only found in the Gandaki River in Nepal. In Hindu philosophy, they are considered to generate positive energy and ["are worshipped as Lord Vishnu."](https://www.quora.com/What-is-the-significance-of-Shaligram-in-Hinduism) Special markings on the shaligram *"resemble Vishnu's paraphernalia such as mace, conch, lotus and disc (chakra)."* As these shaligram show, ***they are formed by energy flows*** involved in Earth processes rather than being fossils. ## 1. The Phantom Dancer This [first shaligram](https://www.etsy.com/listing/786695788/sacred-adwaitya-shweta-crystal-laxmi?click_key=775079af77e01c2cf87db1715721ea7de1aa549a%3A786695788&click_sum=332a2e1f&ref=rv_more-2-1&pro=1&frs=1) has a coherent and more typical "fossil" feature at the center, but the structure has an appearance of stopping while the outer edge, having a ridged structure, blends subtly into the side of the stone.    ## 2. The Core This [second shaligram](https://www.etsy.com/listing/830460411/hayagriva-shaligram-gandaki-river-nepal?click_key=10e20aecd23ac1401028a23a7a53365c333e33f1%3A830460411&click_sum=260ea94e&external=1&rec_type=ss&ref=landingpage_similar_listing_top-7&pro=1&frs=1) has a very distinct sphere where the upper and lower sections converge at the center, as if it formed a ***core.***     ## 3. The Triplet In [this shaligram's](https://www.etsy.com/listing/860352629/rare-sitarama-shaligram-shatchakra-sita?click_key=42857b6c5bc40358013d50d02a5bf85467f96a70%3A860352629&click_sum=dbdbf7fa&ref=rv_more-1-4&pro=1&frs=1) formation process, it has not one but three "fossils." The largest of the structures points perpendicular to the adjacent structure, suggestive of an energy flow relationship between the two.   ## 4. The Pile o' Shaligram Here, [a shaligram](https://www.etsy.com/listing/1134288830/sacred-adwaitya-shweta-laxmi?click_key=e4512dbad49c968823041d7ed4b2f20282c0d625%3A1134288830&click_sum=920d293f&ref=rv_more-2-3&pro=1&frs=1) is shown to have formed in a spiral that grows along a perpendicular axis into a "pile." The initial ridges are distinct and become smoother while the overall shape is maintained as the structure grew.       ## 5. The Crashing Waves In [this shaligram](https://www.etsy.com/listing/1019957360/kamdhenu-shaligram-shila-208-237gms?click_key=68939310724a3d0180b61802451bd9c60aa58f1a%3A1019957360&click_sum=a77a224a&ref=rv_more-2-18&frs=1&sts=1), it appears as if the rock was still molten when it collapsed inward into the "fossil" structure, causing it to take a wave appearance.   ## 6. Sixth Shaligram [This shaligram](https://www.etsy.com/listing/1150225089/shrirudram-kurma-shaligram-saligram?click_key=50a5faa6b904ba341ea96300d510b5714dbef155%3A1150225089&click_sum=3de2cc61&ref=rv_more-2-5&frs=1&sts=1) is    ## 7. Just Peachy [This peach shaped shaligram](https://www.etsy.com/listing/800568495/sacred-adwaitya-golden-chamunda-bhadra?click_key=13fbe467de6ae9cc2b6d3c6f0093d1962a0aaa4f%3A800568495&click_sum=e2a0610d&ref=rv_more-1-11&pro=1&frs=1)     ## 8. Double Decker [This stacked shaligram](https://www.etsy.com/listing/927584808/rare-kalki-shaligram-gandaki-river-nepal?click_key=52174ec44176421103e65e97f8207e3de98df548%3A927584808&click_sum=e9d4e766&ref=rv_more-1-8&pro=1&frs=1)    ## 9. The Window Glimmering like a star, [this shaligram's center](https://www.etsy.com/listing/927564956/rare-big-size-krishna-shaligram-santan?click_key=cce1903934a4f1ff6f9a5875bb669247a29d80fb%3A927564956&click_sum=7b70f900&ref=rv_more-1-17&pro=1&frs=1) provides an abrupt window into the side of the smooth surfaced stone.    ## 10. The Sphere Lastly, [this spherical shaligram](https://www.etsy.com/listing/1148411640/krishna-shaligram-bala-krishna-salagram?click_key=b2ba79977071cdec653aa4eb2a432157d2aaf503%3A1148411640&click_sum=65362dff&ref=rv_more-1-22&pro=1&frs=1) has a gateway into its internal structure.   ## Not "Biological" While shaligram have been considered fossils, they are the results of geological processes that imprint subtle variations in the conditions of their formation into the resultant stone. Each's unique *and* shared characteristics make each magnify particular traits of their formation process. For more information, check out my video exploring these stones and others, [Shaligrams Are Not Fossils](https://youtu.be/3hAno-h1HZk). |
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| parent author | |
| parent permlink | geology |
| permlink | shaligrams-are-not-fossils |
| title | Shaligrams Are Not Fossils |
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"body": "# Ten Shaligrams that demonstrate they are not fossils\nHistorically, [shaligrams](https://en.wikipedia.org/wiki/Shaligram) have been considered fossils of that date to around 400Ma and became extinct in 66Ma.\n\nThey are considered a specific variety of ammonite that is only found in the Gandaki River in Nepal.\n\nIn Hindu philosophy, they are considered to generate positive energy and [\"are worshipped as Lord Vishnu.\"](https://www.quora.com/What-is-the-significance-of-Shaligram-in-Hinduism) Special markings on the shaligram *\"resemble Vishnu's paraphernalia such as mace, conch, lotus and disc (chakra).\"* \n\nAs these shaligram show, ***they are formed by energy flows*** involved in Earth processes rather than being fossils.\n\n## 1. The Phantom Dancer\nThis [first shaligram](https://www.etsy.com/listing/786695788/sacred-adwaitya-shweta-crystal-laxmi?click_key=775079af77e01c2cf87db1715721ea7de1aa549a%3A786695788&click_sum=332a2e1f&ref=rv_more-2-1&pro=1&frs=1) has a coherent and more typical \"fossil\" feature at the center, but the structure has an appearance of stopping while the outer edge, having a ridged structure, blends subtly into the side of the stone.\n\n\n\n\n## 2. The Core\nThis [second shaligram](https://www.etsy.com/listing/830460411/hayagriva-shaligram-gandaki-river-nepal?click_key=10e20aecd23ac1401028a23a7a53365c333e33f1%3A830460411&click_sum=260ea94e&external=1&rec_type=ss&ref=landingpage_similar_listing_top-7&pro=1&frs=1) has a very distinct sphere where the upper and lower sections converge at the center, as if it formed a ***core.***\n\n\n\n\n\n## 3. The Triplet\nIn [this shaligram's](https://www.etsy.com/listing/860352629/rare-sitarama-shaligram-shatchakra-sita?click_key=42857b6c5bc40358013d50d02a5bf85467f96a70%3A860352629&click_sum=dbdbf7fa&ref=rv_more-1-4&pro=1&frs=1) formation process, it has not one but three \"fossils.\" The largest of the structures points perpendicular to the adjacent structure, suggestive of an energy flow relationship between the two.\n\n\n\n## 4. The Pile o' Shaligram\nHere, [a shaligram](https://www.etsy.com/listing/1134288830/sacred-adwaitya-shweta-laxmi?click_key=e4512dbad49c968823041d7ed4b2f20282c0d625%3A1134288830&click_sum=920d293f&ref=rv_more-2-3&pro=1&frs=1) is shown to have formed in a spiral that grows along a perpendicular axis into a \"pile.\" The initial ridges are distinct and become smoother while the overall shape is maintained as the structure grew.\n\n\n\n\n\n\n\n## 5. The Crashing Waves\nIn [this shaligram](https://www.etsy.com/listing/1019957360/kamdhenu-shaligram-shila-208-237gms?click_key=68939310724a3d0180b61802451bd9c60aa58f1a%3A1019957360&click_sum=a77a224a&ref=rv_more-2-18&frs=1&sts=1), it appears as if the rock was still molten when it collapsed inward into the \"fossil\" structure, causing it to take a wave appearance.\n\n\n\n## 6. Sixth Shaligram\n[This shaligram](https://www.etsy.com/listing/1150225089/shrirudram-kurma-shaligram-saligram?click_key=50a5faa6b904ba341ea96300d510b5714dbef155%3A1150225089&click_sum=3de2cc61&ref=rv_more-2-5&frs=1&sts=1) is\n\n\n\n\n## 7. Just Peachy\n[This peach shaped shaligram](https://www.etsy.com/listing/800568495/sacred-adwaitya-golden-chamunda-bhadra?click_key=13fbe467de6ae9cc2b6d3c6f0093d1962a0aaa4f%3A800568495&click_sum=e2a0610d&ref=rv_more-1-11&pro=1&frs=1)\n\n\n\n\n\n## 8. Double Decker\n[This stacked shaligram](https://www.etsy.com/listing/927584808/rare-kalki-shaligram-gandaki-river-nepal?click_key=52174ec44176421103e65e97f8207e3de98df548%3A927584808&click_sum=e9d4e766&ref=rv_more-1-8&pro=1&frs=1)\n\n\n\n\n## 9. The Window\nGlimmering like a star, [this shaligram's center](https://www.etsy.com/listing/927564956/rare-big-size-krishna-shaligram-santan?click_key=cce1903934a4f1ff6f9a5875bb669247a29d80fb%3A927564956&click_sum=7b70f900&ref=rv_more-1-17&pro=1&frs=1) provides an abrupt window into the side of the smooth surfaced stone. \n\n\n\n\n## 10. The Sphere\nLastly, [this spherical shaligram](https://www.etsy.com/listing/1148411640/krishna-shaligram-bala-krishna-salagram?click_key=b2ba79977071cdec653aa4eb2a432157d2aaf503%3A1148411640&click_sum=65362dff&ref=rv_more-1-22&pro=1&frs=1) has a gateway into its internal structure.\n\n\n\n## Not \"Biological\"\nWhile shaligram have been considered fossils, they are the results of geological processes that imprint subtle variations in the conditions of their formation into the resultant stone. Each's unique *and* shared characteristics make each magnify particular traits of their formation process.\n\nFor more information, check out my video exploring these stones and others, [Shaligrams Are Not Fossils](https://youtu.be/3hAno-h1HZk).",
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"parent_permlink": "geology",
"permlink": "shaligrams-are-not-fossils",
"title": "Shaligrams Are Not Fossils"
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}stevescullypublished a new post: on-the-non-random-distribution-of-impact-craters2022/09/27 15:01:06
stevescullypublished a new post: on-the-non-random-distribution-of-impact-craters
2022/09/27 15:01:06
| author | stevescully |
| body | @@ -868,17 +868,16 @@ r, again -, alike t |
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| parent author | |
| parent permlink | geology |
| permlink | on-the-non-random-distribution-of-impact-craters |
| title | On the non-random distribution of "Impact Craters" |
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"author": "stevescully",
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"parent_permlink": "geology",
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"title": "On the non-random distribution of \"Impact Craters\""
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}stevescullypublished a new post: on-the-non-random-distribution-of-impact-craters2022/09/27 15:00:51
stevescullypublished a new post: on-the-non-random-distribution-of-impact-craters
2022/09/27 15:00:51
| author | stevescully |
| body | @@ -876,29 +876,31 @@ , al -so like Nadir crater, +ike to one another, the Chi |
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| parent author | |
| parent permlink | geology |
| permlink | on-the-non-random-distribution-of-impact-craters |
| title | On the non-random distribution of "Impact Craters" |
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}stevescullypublished a new post: on-the-non-random-distribution-of-impact-craters2022/09/27 04:45:33
stevescullypublished a new post: on-the-non-random-distribution-of-impact-craters
2022/09/27 04:45:33
| author | stevescully |
| body | @@ -6839,18 +6839,20 @@ re are t -wo +hree separat |
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| parent permlink | geology |
| permlink | on-the-non-random-distribution-of-impact-craters |
| title | On the non-random distribution of "Impact Craters" |
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}stevescullypublished a new post: on-the-non-random-distribution-of-impact-craters2022/09/27 00:12:42
stevescullypublished a new post: on-the-non-random-distribution-of-impact-craters
2022/09/27 00:12:42
| author | stevescully |
| body | @@ -879,16 +879,30 @@ lso like + Nadir crater, Chicxul @@ -903,21 +903,16 @@ hicxulub -, the crater |
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| parent author | |
| parent permlink | geology |
| permlink | on-the-non-random-distribution-of-impact-craters |
| title | On the non-random distribution of "Impact Craters" |
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"author": "stevescully",
"body": "@@ -879,16 +879,30 @@\n lso like\n+ Nadir crater,\n Chicxul\n@@ -903,21 +903,16 @@\n hicxulub\n-, the\n crater \n",
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alexmove.witnesssent 0.001 STEEM to @stevescully- "Please support me @alexmove.witness as witness on site https://steemitwallet.com/~witnesses. I send daily Witness vote STEEM reward and voted for some posts of those who voted. Your vote is very impor..."
2022/09/26 23:11:06
| amount | 0.001 STEEM |
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| to | stevescully |
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}stevescullypublished a new post: on-the-non-random-distribution-of-impact-craters2022/09/26 23:10:12
stevescullypublished a new post: on-the-non-random-distribution-of-impact-craters
2022/09/26 23:10:12
| author | stevescully |
| body | @@ -728,16 +728,140 @@ craters. + Notably, the Boltysh Crater formed simultaneously and is also considered by Nicholson et al. as a binary or triple impact. %0A%0AHoweve |
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| parent author | |
| parent permlink | geology |
| permlink | on-the-non-random-distribution-of-impact-craters |
| title | On the non-random distribution of "Impact Craters" |
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"body": "@@ -728,16 +728,140 @@\n craters.\n+ Notably, the Boltysh Crater formed simultaneously and is also considered by Nicholson et al. as a binary or triple impact.\n %0A%0AHoweve\n",
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}stevescullypublished a new post: on-the-non-random-distribution-of-impact-craters2022/09/26 23:00:57
stevescullypublished a new post: on-the-non-random-distribution-of-impact-craters
2022/09/26 23:00:57
| author | stevescully |
| body | ### The Trifecta With the recent discovery of the [Nadir Crater](https://www.science.org/doi/pdf/10.1126/sciadv.abn3096?fbclid=IwAR0Y9YzBrvLIk79hTeTNuJpA-BGqomFPFkSW6I50gTaDdkTusXIrc3J9p08) off the southwestern coast of northern Africa, at the Guinea Terrace, the question of the proximity of craters to the edge of the continental shelf arises.  Like the Chicxulub crater, the stratigraphic analysis suggests that the crater formed at or near the Cretaceous-Paleogene boundary, ~66Ma.<sup>1</sup> As a result, the authors considered whether it was associated with the Chicxulub crater as binary impact craters. However, again, also like Chicxulub, the crater was found generally proximal to the edge of the continental shelf:  While alone this is an odd curiosity, their relatively simultaneous nature makes the proximity to the edge of the continental shelf notable. Then, also considered to have formed in ***the same time frame*** of 66Ma is the [Shiva Crater](https://www.researchgate.net/publication/228719850_Shiva_structure_a_possible_KT_boundary_impact_crater_on_the_western_shelf_of_India)<sup>2</sup>, positioned at the edge of continental shelf as well, making three simultaneous craters formed at the edges of continental shelf:  ### *Moar* Craters They are not the only craters found near the edge of the continental shelf. Running along the eastern coast of North America, the [Chesapeake Bay Crater, Toms Canyon Crater, and Montagnais Craters](https://craterexplorer.ca/chesapeake-impact-crater-2/) each are considered to have formed 35.7Ma, 35.7Ma, and 51Ma, respectively.<sup>3</sup> More, the Montagnais crater is curiously positioned *at* a bend in the edge of the continental shelf.  [Impacts near coast](https://craterexplorer.ca/chesapeake-impact-crater-2/) Then, off the coast of San Diego, [large enigmatic crater structures were discovered in bathymetry data<sup>4</sup>](https://academic.oup.com/gji/article/159/2/803/2067497):  [Figure 2 of Legg et al.](https://academic.oup.com/gji/article/159/2/803/2067497) As described by Legg et al.: > "...data reveal large, distinct near-circulate crater structures in the Inner Continental Borderland offshore southern California. Two have maximum crater diameters that exceed 30 km and a third has a crater diameter of approximately 12 km. All three features exhibit the morphology of large complex craters (raised outer rim, ring moat and central uplift) yet their exact origin remains a mystery...Timing of crater formation post-dates the initial rifting and rotation of the western Transverse Ranges, and appears to predate major right slip along the San Clemente and San Diego Trough fault systems--or approximately 18 to 16 Ma." Significantly, they describe that "the craters lie ***entirely within*** the Inner Borderland Rift," strongly suggestive of a ***relationship*** between the craters and the local processes both before and after their formations. The [Woodleigh Crater](https://en.wikipedia.org/wiki/Woodleigh_crater), the largest crater in Australia, can be found relatively near to the edge of the continental shelf, compared to its diameter:  The [Mjølnir Crater](https://en.wikipedia.org/wiki/Mj%C3%B8lnir_crater), considered to have formed ~150 Ma, appears to be in line with the direction the energy was propagating when the North America and Europe were severed around 200-150 Ma. Though it is not as close to the edge of the continental shelf as the others, it appears to be suggestive of a possible mechanism or contributing cause to the structures--energy propagating in the region being caused to funnel through particular channels.   [Source](https://observatorio.info/1999/06/mjlnir-crter-de-impacto/) Similarly, the [Popigai crater](https://en.wikipedia.org/wiki/Popigai_crater) is positioned near where continental shelf and the propagating fracture meet and the continent experienced a force:  More, Popigai is considered to have formed ~35.7 Ma, making it the same age as the Chesapeake Bay and Toms Canyon craters discussed above, and it has been considered for [links between the formation of the craters](https://onlinelibrary.wiley.com/doi/10.1111/j.1945-5100.2006.tb00985.x),<sup>5</sup> similarly producing another *trifecta* of simultaneous *continental shelf coastal* "impact craters" being formed. Its positioning and the shape of the continental shelf is suggestive of a larger polygonal structure that the Popigai crater lies along:      The structure carving through the polygon towards it's heart, from the southwestern region, is reminiscent of Mount Girnar's also southwestern fracture line that is at a 90 degree angle relative to the ridge branching from the central mountain:  Popigai polygon region  Mount Girnar ### What Is Really Going On? In a sense, these "impact craters" are like blow-out valves in the structure of the Earth itself that allowed energy accumulating in regions to be expelled through point locations. As there are two separate sets of trinary craters all on edges of continental shelf and both distributed globally and more locally, these are not *random* and thus cannot be impact craters from outer space as traditionally viewed. Rather, they can only be similar structures from internal impact processes caused by the Earth itself. This energy propagating through regions being the result of a [vortex weapon used on Ancient Dwarka that caused the Earth to expand....](https://www.youtube.com/watch?v=qRriWdNTUKY) 1. [Nicholson et al., The Nadir Crater offshore West Africa: A candidate Cretaceous-Paleogene impact structure, Science Advances, Vol. 8, No. 33, Aug 2022.](https://www.science.org/doi/10.1126/sciadv.abn3096) 2. [Chatterjee et al., "Shiva structure: a possible KT boundary impact crater on the western shelf of India, Special Publications, Museum Texas Tech University, January 2006](https://www.researchgate.net/publication/228719850_Shiva_structure_a_possible_KT_boundary_impact_crater_on_the_western_shelf_of_India) 3. [Poag et al., Ancient impact strucutres on modern continental shelves: The Chesapeake Bay, Montagnais, and Toms Canyon craters, Atlantic margin of North America, December 2002, Deep Sea Research Part II Topical Studies in Oceanography 49(6):1081-1102](https://www.researchgate.net/publication/248417154_Ancient_impact_structures_on_modern_continental_shelves_The_Chesapeake_Bay_Montagnais_and_Toms_Canyon_craters_Atlantic_margin_of_North_America) 4. [Mark R. Legg, Craig Nicholson, Chris Goldfinger, Randall Milstein, Marc J. Kamerling, Large enigmatic crater structures offshore southern California, Geophysical Journal International, Volume 159, Issue 2, November 2004, Pages 803–815](https://academic.oup.com/gji/article/159/2/803/2067497) 5. [DEUTSCH, A. and KOEBERL, C. (2006), Establishing the link between the Chesapeake Bay impact structure and the North American tektite strewn field: The Sr-Nd isotopic evidence. Meteoritics & Planetary Science, 41: 689-703.](https://onlinelibrary.wiley.com/doi/10.1111/j.1945-5100.2006.tb00985.x) |
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| parent author | |
| parent permlink | geology |
| permlink | on-the-non-random-distribution-of-impact-craters |
| title | On the non-random distribution of "Impact Craters" |
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"body": "### The Trifecta\nWith the recent discovery of the [Nadir Crater](https://www.science.org/doi/pdf/10.1126/sciadv.abn3096?fbclid=IwAR0Y9YzBrvLIk79hTeTNuJpA-BGqomFPFkSW6I50gTaDdkTusXIrc3J9p08) off the southwestern coast of northern Africa, at the Guinea Terrace, the question of the proximity of craters to the edge of the continental shelf arises. \n\n\n\nLike the Chicxulub crater, the stratigraphic analysis suggests that the crater formed at or near the Cretaceous-Paleogene boundary, ~66Ma.<sup>1</sup> As a result, the authors considered whether it was associated with the Chicxulub crater as binary impact craters.\n\nHowever, again, also like Chicxulub, the crater was found generally proximal to the edge of the continental shelf:\n\n\nWhile alone this is an odd curiosity, their relatively simultaneous nature makes the proximity to the edge of the continental shelf notable. Then, also considered to have formed in ***the same time frame*** of 66Ma is the [Shiva Crater](https://www.researchgate.net/publication/228719850_Shiva_structure_a_possible_KT_boundary_impact_crater_on_the_western_shelf_of_India)<sup>2</sup>, positioned at the edge of continental shelf as well, making three simultaneous craters formed at the edges of continental shelf:\n\n\n\n### *Moar* Craters\nThey are not the only craters found near the edge of the continental shelf.\n\nRunning along the eastern coast of North America, the [Chesapeake Bay Crater, Toms Canyon Crater, and Montagnais Craters](https://craterexplorer.ca/chesapeake-impact-crater-2/) each are considered to have formed 35.7Ma, 35.7Ma, and 51Ma, respectively.<sup>3</sup> More, the Montagnais crater is curiously positioned *at* a bend in the edge of the continental shelf.\n\n\n[Impacts near coast](https://craterexplorer.ca/chesapeake-impact-crater-2/)\n\nThen, off the coast of San Diego, [large enigmatic crater structures were discovered in bathymetry data<sup>4</sup>](https://academic.oup.com/gji/article/159/2/803/2067497):\n\n[Figure 2 of Legg et al.](https://academic.oup.com/gji/article/159/2/803/2067497)\n\nAs described by Legg et al.:\n> \"...data reveal large, distinct near-circulate crater structures in the Inner Continental Borderland offshore southern California. Two have maximum crater diameters that exceed 30 km and a third has a crater diameter of approximately 12 km. All three features exhibit the morphology of large complex craters (raised outer rim, ring moat and central uplift) yet their exact origin remains a mystery...Timing of crater formation post-dates the initial rifting and rotation of the western Transverse Ranges, and appears to predate major right slip along the San Clemente and San Diego Trough fault systems--or approximately 18 to 16 Ma.\"\n\nSignificantly, they describe that \"the craters lie ***entirely within*** the Inner Borderland Rift,\" strongly suggestive of a ***relationship*** between the craters and the local processes both before and after their formations.\n\nThe [Woodleigh Crater](https://en.wikipedia.org/wiki/Woodleigh_crater), the largest crater in Australia, can be found relatively near to the edge of the continental shelf, compared to its diameter:\n\n\n\nThe [Mjølnir Crater](https://en.wikipedia.org/wiki/Mj%C3%B8lnir_crater), considered to have formed ~150 Ma, appears to be in line with the direction the energy was propagating when the North America and Europe were severed around 200-150 Ma. Though it is not as close to the edge of the continental shelf as the others, it appears to be suggestive of a possible mechanism or contributing cause to the structures--energy propagating in the region being caused to funnel through particular channels.\n\n\n\n[Source](https://observatorio.info/1999/06/mjlnir-crter-de-impacto/)\n\nSimilarly, the [Popigai crater](https://en.wikipedia.org/wiki/Popigai_crater) is positioned near where continental shelf and the propagating fracture meet and the continent experienced a force:\n\n\nMore, Popigai is considered to have formed ~35.7 Ma, making it the same age as the Chesapeake Bay and Toms Canyon craters discussed above, and it has been considered for [links between the formation of the craters](https://onlinelibrary.wiley.com/doi/10.1111/j.1945-5100.2006.tb00985.x),<sup>5</sup> similarly producing another *trifecta* of simultaneous *continental shelf coastal* \"impact craters\" being formed.\n\nIts positioning and the shape of the continental shelf is suggestive of a larger polygonal structure that the Popigai crater lies along:\n\n\n\n\n\n\nThe structure carving through the polygon towards it's heart, from the southwestern region, is reminiscent of Mount Girnar's also southwestern fracture line that is at a 90 degree angle relative to the ridge branching from the central mountain:\n\n\nPopigai polygon region\n\n\nMount Girnar\n\n### What Is Really Going On?\n\nIn a sense, these \"impact craters\" are like blow-out valves in the structure of the Earth itself that allowed energy accumulating in regions to be expelled through point locations.\n\nAs there are two separate sets of trinary craters all on edges of continental shelf and both distributed globally and more locally, these are not *random* and thus cannot be impact craters from outer space as traditionally viewed. Rather, they can only be similar structures from internal impact processes caused by the Earth itself.\n\nThis energy propagating through regions being the result of a [vortex weapon used on Ancient Dwarka that caused the Earth to expand....](https://www.youtube.com/watch?v=qRriWdNTUKY)\n\n1. [Nicholson et al., The Nadir Crater offshore West Africa: A candidate Cretaceous-Paleogene impact structure, Science Advances, Vol. 8, No. 33, Aug 2022.](https://www.science.org/doi/10.1126/sciadv.abn3096)\n2. [Chatterjee et al., \"Shiva structure: a possible KT boundary impact crater on the western shelf of India, Special Publications, Museum Texas Tech University, January 2006](https://www.researchgate.net/publication/228719850_Shiva_structure_a_possible_KT_boundary_impact_crater_on_the_western_shelf_of_India)\n3. [Poag et al., Ancient impact strucutres on modern continental shelves: The Chesapeake Bay, Montagnais, and Toms Canyon craters, Atlantic margin of North America, December 2002, Deep Sea Research Part II Topical Studies in Oceanography 49(6):1081-1102](https://www.researchgate.net/publication/248417154_Ancient_impact_structures_on_modern_continental_shelves_The_Chesapeake_Bay_Montagnais_and_Toms_Canyon_craters_Atlantic_margin_of_North_America)\n4. [Mark R. Legg, Craig Nicholson, Chris Goldfinger, Randall Milstein, Marc J. Kamerling, Large enigmatic crater structures offshore southern California, Geophysical Journal International, Volume 159, Issue 2, November 2004, Pages 803–815](https://academic.oup.com/gji/article/159/2/803/2067497)\n5. [DEUTSCH, A. and KOEBERL, C. (2006), Establishing the link between the Chesapeake Bay impact structure and the North American tektite strewn field: The Sr-Nd isotopic evidence. Meteoritics & Planetary Science, 41: 689-703.](https://onlinelibrary.wiley.com/doi/10.1111/j.1945-5100.2006.tb00985.x)",
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}stevescullypublished a new post: dattatreya-peak2022/09/21 17:31:12
stevescullypublished a new post: dattatreya-peak
2022/09/21 17:31:12
| author | stevescully |
| body | @@ -3368,16 +3368,111 @@ 9.JPG)%0A%0A +!%5B9.JPG%5D(https://cdn.steemitimages.com/DQmRViZy2UzCazH2HgPaLj6nCC3qgaD6yDo3DzUxUH7ZF4G/9.JPG)%0A%0A Sources: @@ -4721,8 +4721,125 @@ -2p6_jU) +%0A%5BGirnar Parvat darshan LIVE %E0%A4%B8%E0%A4%AE%E0%A5%8D%E0%A4%AA%E0%A5%82%E0%A4%B0%E0%A5%8D%E0%A4%A3 %E0%A4%97%E0%A4%BF%E0%A4%B0%E0%A4%A8%E0%A4%BE%E0%A4%B0 %E0%A4%AA%E0%A4%B0%E0%A5%8D%E0%A4%B5%E0%A4%A4 %E0%A4%A6%E0%A4%B0%E0%A5%8D%E0%A4%B6%E0%A4%A8 %E0%A4%AF%E0%A4%BE%E0%A4%A4%E0%A4%BE %F0%9F%99%8F Part 1%5D(https://www.youtube.com/watch?v=X7WROwixQog) |
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| parent author | |
| parent permlink | geology |
| permlink | dattatreya-peak |
| title | Dattatreya Peak |
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}stevescullypublished a new post: dattatreya-peak2022/09/21 16:22:48
stevescullypublished a new post: dattatreya-peak
2022/09/21 16:22:48
| author | stevescully |
| body | @@ -2839,16 +2839,545 @@ c.JPG)%0A%0A +%0A!%5BDattatreya 1.png%5D(https://cdn.steemitimages.com/DQmaUfXvnJHhqEvmD3FQXbCEY5uqhsVMbM8a6Spx71kcMfU/Dattatreya%25201.png)%0A%0A!%5BDattatreya 2.png%5D(https://cdn.steemitimages.com/DQmf8t6UqYcZM7f3NyNxTg7kmadykwCYdN7ruDB9NwubzG4/Dattatreya%25202.png)%0A%0A%0A!%5B9.JPG%5D(https://cdn.steemitimages.com/DQmVGZSqmYqsX9RJRGQE4ocYQqZZrdSzk4sJ3izrAZtRbpy/9.JPG)%0A%0A!%5B13.JPG%5D(https://cdn.steemitimages.com/DQma6ixjitd5vERjdx213xGaPhoZ1XHFwxGp1LGe4c5iDiD/13.JPG)%0A%0A!%5B19.JPG%5D(https://cdn.steemitimages.com/DQmahMghkBtxEUEgW8eQh9uiq5BUyNWj8WDNsciDFQsuAdy/19.JPG)%0A%0A Sources: @@ -4515,8 +4515,119 @@ xLI8_-0) +%0A%5BEverest of Gujarat : Girnar Hills : Older Than Sacred Himalayas%5D(https://www.youtube.com/watch?v=O34O-2p6_jU) |
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| parent author | |
| parent permlink | geology |
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}stevescullypublished a new post: mount-girnar-the-catalyst2022/09/21 02:15:18
stevescullypublished a new post: mount-girnar-the-catalyst
2022/09/21 02:15:18
| author | stevescully |
| body | @@ -2096,17 +2096,95 @@ in Tibet -. +, and it means %5B%22crystal.%22%5D(https://www.ahymsin.org/docs2/News/1111Nov/01.html) Kailas |
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| parent permlink | geology |
| permlink | mount-girnar-the-catalyst |
| title | Mount Girnar: The Catalyst |
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}stevescullypublished a new post: angles-of-the-world2022/09/20 21:45:51
stevescullypublished a new post: angles-of-the-world
2022/09/20 21:45:51
| author | stevescully |
| body | This is a compilation of my best attempts to earnestly find angles of edges of continental shelf as formed due to the Earth's expansion process (see my previous works for details). In the process, when there were straight edges for a distance followed by a bend and then straight edges, each side of the angle is ultimately aligned ~with the portions that are straight and not the curved sections. These numbers are important as they relate to crystalline structures. These further provide evidence of the expansion of the Earth, as discussed in my previous works in detail, having followed precise geometric processes. To people offended because, well, plate tectonics: Obviously this can be construed as cherry picking data. I would direct your attention to the sheer quantity of near identical specific angles at places like the many 120 degree angles around Africa and the string of 135 degree angles along the Australian coast. If this is happening, wouldn't it benefit us to analyze it further and determine if there is a REASON the angles TEND to be certain angles, especially in the places where sudden turns occur? Do not just dismiss it as trivial when there are in fact far more places sharing the same angles on Earth than would be the case if it was more "random." This is more than just some angles overlaying google maps. It is indicative of the geometric nature of how the continental crust, which was a single landmass with no oceanic crust between whatsoever, fractured sufficiently for the Earth to grow to a new radius. The ocean beds were formed in this process, much of the water on Earth's surface was released from within the planet. The angles contain the record of how it occurred written in stone. # The Curious Case of 120 Degrees ## Africa        ## Asia   ## Australia   ## North America   ## South America   # 135 Degrees As the first 5 images are all one after another along the Australian coast, that they closely approach 135 degree angles is anomalous, being 180-45 suggestive of a "cleavage" process at 45 degree angles when the Earth's crust fractured from a single landmass.        # 60 Degrees      # 90 Degrees    |
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| parent author | |
| parent permlink | geology |
| permlink | angles-of-the-world |
| title | Angles of the World |
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"author": "stevescully",
"body": "This is a compilation of my best attempts to earnestly find angles of edges of continental shelf as formed due to the Earth's expansion process (see my previous works for details). \n\nIn the process, when there were straight edges for a distance followed by a bend and then straight edges, each side of the angle is ultimately aligned ~with the portions that are straight and not the curved sections. These numbers are important as they relate to crystalline structures.\n\nThese further provide evidence of the expansion of the Earth, as discussed in my previous works in detail, having followed precise geometric processes.\n\nTo people offended because, well, plate tectonics: Obviously this can be construed as cherry picking data. I would direct your attention to the sheer quantity of near identical specific angles at places like the many 120 degree angles around Africa and the string of 135 degree angles along the Australian coast. If this is happening, wouldn't it benefit us to analyze it further and determine if there is a REASON the angles TEND to be certain angles, especially in the places where sudden turns occur? Do not just dismiss it as trivial when there are in fact far more places sharing the same angles on Earth than would be the case if it was more \"random.\" \n\nThis is more than just some angles overlaying google maps. It is indicative of the geometric nature of how the continental crust, which was a single landmass with no oceanic crust between whatsoever, fractured sufficiently for the Earth to grow to a new radius. The ocean beds were formed in this process, much of the water on Earth's surface was released from within the planet. The angles contain the record of how it occurred written in stone.\n\n# The Curious Case of 120 Degrees\n## Africa\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n## Asia\n\n\n\n\n\n## Australia\n\n\n\n\n\n## North America\n\n\n\n\n\n\n## South America\n\n\n\n\n\n# 135 Degrees\nAs the first 5 images are all one after another along the Australian coast, that they closely approach 135 degree angles is anomalous, being 180-45 suggestive of a \"cleavage\" process at 45 degree angles when the Earth's crust fractured from a single landmass.\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n# 60 Degrees\n\n\n\n\n\n\n\n\n\n\n\n# 90 Degrees\n\n\n\n\n\n\n",
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"permlink": "angles-of-the-world",
"title": "Angles of the World"
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}stevescullypublished a new post: angles-of-mount-girnar2022/09/19 23:36:33
stevescullypublished a new post: angles-of-mount-girnar
2022/09/19 23:36:33
| author | stevescully |
| body | @@ -595,24 +595,153 @@ %2520NW.JPG)%0A%0A +!%5B60 degrees 1 NW.JPG%5D(https://cdn.steemitimages.com/DQmZm7GL8Axdct6wPqDSTVtnoK1Ab5rc6sWvZ7VHikfzc4Z/60%2520degrees%25201%2520NW.JPG)%0A%0A !%5BCentral Mo |
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| parent permlink | girnar |
| permlink | angles-of-mount-girnar |
| title | Angles of Mount Girnar |
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}stevescullypublished a new post: angles-of-mount-girnar2022/09/19 22:56:27
stevescullypublished a new post: angles-of-mount-girnar
2022/09/19 22:56:27
| author | stevescully |
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| parent author | |
| parent permlink | girnar |
| permlink | angles-of-mount-girnar |
| title | Angles of Mount Girnar |
| Transaction Info | Block #67837286/Trx 2f2b822d1e46db6f2ff2f85f22b6ef66e1ba5c38 |
View Raw JSON Data
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"parent_author": "",
"parent_permlink": "girnar",
"permlink": "angles-of-mount-girnar",
"title": "Angles of Mount Girnar"
}
],
"op_in_trx": 0,
"timestamp": "2022-09-19T22:56:27",
"trx_id": "2f2b822d1e46db6f2ff2f85f22b6ef66e1ba5c38",
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}stevescullypublished a new post: angles-of-mount-girnar2022/09/19 22:53:42
stevescullypublished a new post: angles-of-mount-girnar
2022/09/19 22:53:42
| author | stevescully |
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| parent author | |
| parent permlink | girnar |
| permlink | angles-of-mount-girnar |
| title | Angles of Mount Girnar |
| Transaction Info | Block #67837232/Trx d416ea937c9bafac87ae1bb1aaef9918874b0c27 |
View Raw JSON Data
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"timestamp": "2022-09-19T22:53:42",
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}stevescullypublished a new post: angles-of-mount-girnar2022/09/19 22:52:36
stevescullypublished a new post: angles-of-mount-girnar
2022/09/19 22:52:36
| author | stevescully |
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| parent author | |
| parent permlink | girnar |
| permlink | angles-of-mount-girnar |
| title | Angles of Mount Girnar |
| Transaction Info | Block #67837210/Trx 30acdb9ca6c92b57b86ab2f2e61e441ff10718a5 |
View Raw JSON Data
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}stevescullypublished a new post: angles-of-mount-girnar2022/09/19 22:48:39
stevescullypublished a new post: angles-of-mount-girnar
2022/09/19 22:48:39
| author | stevescully |
| body |                                  |
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}stevescullypublished a new post: dattatreya-peak2022/09/19 21:54:57
stevescullypublished a new post: dattatreya-peak
2022/09/19 21:54:57
| author | stevescully |
| body | @@ -1,31 +1,4 @@ -A compilation of images of Datt @@ -8,18 +8,20 @@ eya Peak --- + is the high @@ -29,14 +29,15 @@ st p -eak at +oint on Mou @@ -49,34 +49,37 @@ rnar --- + and -the surrounding area +has many unique features . S |
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| parent author | |
| parent permlink | geology |
| permlink | dattatreya-peak |
| title | Dattatreya Peak |
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}stevescullypublished a new post: dattatreya-peak2022/09/19 21:53:15
stevescullypublished a new post: dattatreya-peak
2022/09/19 21:53:15
| author | stevescully |
| body | @@ -35,18 +35,52 @@ eya Peak -, +--the highest peak at Mount Girnar-- and the @@ -99,21 +99,8 @@ area -, from videos . S |
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| parent permlink | geology |
| permlink | dattatreya-peak |
| title | Dattatreya Peak |
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}stevescullypublished a new post: dattatreya-peak2022/09/19 21:49:24
stevescullypublished a new post: dattatreya-peak
2022/09/19 21:49:24
| author | stevescully |
| body | A compilation of images of Dattatreya Peak, and the surrounding area, from videos. Sources at bottom.                      Sources: [Girnar Ropeway | Girnar Mountain | Junagadh](https://www.youtube.com/watch?v=wO4-3YR-Ayg&t=35s) [Girnar Vlog | Girnar part-2 | Dattatrey Temple | Monsoon Trip | 2022](https://www.youtube.com/watch?v=L7w1ln3MW0o) [Safar Saurashtra Ni | Girnar & Girnar Ropeway | Ft. Purva Mehta | Junagadh | Aapdu Junagadh](https://www.youtube.com/watch?v=8Zq-R9K8HAU) [Junagadh and its Glory | Happy Independence Day | Junagadh | Aapdu Junagadh](https://www.youtube.com/watch?v=RW2PBW6jKek) [ચોમાસામાં સ્વર્ગ બની જતું,જૂનાગઢવાસીઓનું ફેવરિટ પ્લેસ |Jata Shankar| Best Place to Visit in Junagadh](https://www.youtube.com/watch?v=KCHcDK8HJws) [વરસાદ પહેલાંના અને પછીના જૂનાગઢના આ દ્રશ્યો ખરેખર અદ્દભુત છે! | The time lapse of Junagadh | Girnar](https://www.youtube.com/watch?v=wAZMesuPfbQ) [girnar vlog Girnar darshan #girnar # girnardarshan](https://www.youtube.com/watch?v=SSKWkz_dMfI) [गिरनार पर्वत संपूर्ण माहिती | दत्तगुरूचे दर्शन | ROPEWAY | GIRNAR HILLS | MY FIRST MARATHI VLOG](https://www.youtube.com/watch?v=hKclts4vkSE) [EP 3 Junagadh Tour | Girnar Hills, Dam visit, Kumbhkaran Thali | Saurashtra Tour](https://www.youtube.com/watch?v=MC8wxLI8_-0) |
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| parent author | |
| parent permlink | geology |
| permlink | dattatreya-peak |
| title | Dattatreya Peak |
| Transaction Info | Block #67835954/Trx 396bb61f5006385edaf56617e6dc027063a2ee39 |
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"body": "A compilation of images of Dattatreya Peak, and the surrounding area, from videos. Sources at bottom.\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\nSources:\n[Girnar Ropeway | Girnar Mountain | Junagadh](https://www.youtube.com/watch?v=wO4-3YR-Ayg&t=35s)\n[Girnar Vlog | Girnar part-2 | Dattatrey Temple | Monsoon Trip | 2022](https://www.youtube.com/watch?v=L7w1ln3MW0o)\n[Safar Saurashtra Ni | Girnar & Girnar Ropeway | Ft. Purva Mehta | Junagadh | Aapdu Junagadh](https://www.youtube.com/watch?v=8Zq-R9K8HAU)\n[Junagadh and its Glory | Happy Independence Day | Junagadh | Aapdu Junagadh](https://www.youtube.com/watch?v=RW2PBW6jKek)\n[ચોમાસામાં સ્વર્ગ બની જતું,જૂનાગઢવાસીઓનું ફેવરિટ પ્લેસ |Jata Shankar| Best Place to Visit in Junagadh](https://www.youtube.com/watch?v=KCHcDK8HJws)\n[વરસાદ પહેલાંના અને પછીના જૂનાગઢના આ દ્રશ્યો ખરેખર અદ્દભુત છે! | The time lapse of Junagadh | Girnar](https://www.youtube.com/watch?v=wAZMesuPfbQ)\n[girnar vlog Girnar darshan #girnar # girnardarshan](https://www.youtube.com/watch?v=SSKWkz_dMfI)\n[गिरनार पर्वत संपूर्ण माहिती | दत्तगुरूचे दर्शन | ROPEWAY | GIRNAR HILLS | MY FIRST MARATHI VLOG](https://www.youtube.com/watch?v=hKclts4vkSE)\n[EP 3 Junagadh Tour | Girnar Hills, Dam visit, Kumbhkaran Thali | Saurashtra Tour](https://www.youtube.com/watch?v=MC8wxLI8_-0)",
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}jayleesteemupvoted (100.00%) @stevescully / mount-girnar-rocks2022/09/16 22:02:48
jayleesteemupvoted (100.00%) @stevescully / mount-girnar-rocks
2022/09/16 22:02:48
| author | stevescully |
| permlink | mount-girnar-rocks |
| voter | jayleesteem |
| weight | 10000 (100.00%) |
| Transaction Info | Block #67750260/Trx 49336297db8a34f9c9864578b0d9370e01d0a09e |
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}stevescullypublished a new post: mount-girnar-rocks2022/09/16 21:37:48
stevescullypublished a new post: mount-girnar-rocks
2022/09/16 21:37:48
| author | stevescully |
| body | # A compilation of some interesting features of Mount Girnar. These images are taken from several videos from YouTube documenting Girnar. Sources at bottom.  Figure 1: The sharp angle of the rock (bottom right of the rock) is nearly exactly 120 degrees. Hexagons are a common theme of Mount Girnar.  Figure 2: Another rock with an ~120 degree angle and sharp edges.  Figure 3: More sharp edges.  Figure 4: Top, middle rock has a "sort of" hexagonal shape to the top, like it formed with some aspects.  Figure 5: More sharp edges.  Figure 6: Gorankhnath Tunk  Figure 7a: Wall showing tendrils from energy flows in mountain formation.  Figure 7b: Closer view.  Figure 7c: Different angle.  Figure 8: Dattatreya Peak with smooth steps in the rock face (visible especially middle, right side of image).  Figure 9: Rock with cavities.  Figure 10a: Microcosm three-peaked rock.  Figure 10b: Closer image.  Figure 10c: Closer image again.  Figure 11: Dattatreya Peak  Figure 12a: Side of a peak.  Figure 12b: Lower segment.  Figure 13: More sharp edged rocks.  Figure 14: More sharp edged rocks.  Figure 15: View of terrain.  Figure 16: Mount Girnar.  Figure 17: Mount Girnar.  Figure 18: Mount Girnar.  Figure 19: Mount Girnar.  Figure 20: River of Mount Girnar with distinct rocks.  Figure 21: Mount Girnar.  Figure 22: Mount Girnar.  Figure 23: Mount Girnar.  Figure 24: River rocks.  Figure 25: River rocks.  Figure 26: River rocks.  Figure 27: River rocks.  Figure 28: River rocks.  Figure 29: Temple built around stream  Figure 30: Mount Girnar.  Figure 31: Mount Girnar.  Figure 32: Peaks of Girnar.  Figure 33: Mount Girnar with Bhavnath Temple visible where Shivaling is said to have emerged of its own intention.  Figure 34: Dattatreya Peak.  Figure 35: Mountain peaks. Sources: Figures 1-8: [Girnar Vlog | Girnar part-2 | Dattatrey Temple | Monsoon Trip | 2022](https://www.youtube.com/watch?v=L7w1ln3MW0o) Rest of images from Aapdu Junagadh: [Junagadh and its Glory | Happy Independence Day | Junagadh | Aapdu Junagadh](https://www.youtube.com/watch?v=RW2PBW6jKek) [વરસાદ પહેલાંના અને પછીના જૂનાગઢના આ દ્રશ્યો ખરેખર અદ્દભુત છે! | The time lapse of Junagadh | Girnar](https://www.youtube.com/watch?v=wAZMesuPfbQ) [ચોમાસામાં સ્વર્ગ બની જતું,જૂનાગઢવાસીઓનું ફેવરિટ પ્લેસ |Jata Shankar| Best Place to Visit in Junagadh](https://www.youtube.com/watch?v=KCHcDK8HJws) [Safar Saurashtra Ni | Girnar & Girnar Ropeway | Ft. Purva Mehta | Junagadh | Aapdu Junagadh](https://www.youtube.com/watch?v=8Zq-R9K8HAU) |
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| parent author | |
| parent permlink | girnar |
| permlink | mount-girnar-rocks |
| title | Mount Girnar Rocks |
| Transaction Info | Block #67749763/Trx 72caa36cb52772f74f0a2060f30ce4abba5341fe |
View Raw JSON Data
{
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"author": "stevescully",
"body": "# A compilation of some interesting features of Mount Girnar.\n\nThese images are taken from several videos from YouTube documenting Girnar. Sources at bottom.\n\nFigure 1: The sharp angle of the rock (bottom right of the rock) is nearly exactly 120 degrees. Hexagons are a common theme of Mount Girnar.\n\n\nFigure 2: Another rock with an ~120 degree angle and sharp edges.\n\n\nFigure 3: More sharp edges.\n\n\nFigure 4: Top, middle rock has a \"sort of\" hexagonal shape to the top, like it formed with some aspects.\n\n\nFigure 5: More sharp edges.\n\n\n\nFigure 6: Gorankhnath Tunk\n\n\nFigure 7a: Wall showing tendrils from energy flows in mountain formation.\n\n\nFigure 7b: Closer view.\n\n\nFigure 7c: Different angle.\n\n\nFigure 8: Dattatreya Peak with smooth steps in the rock face (visible especially middle, right side of image).\n\n\nFigure 9: Rock with cavities.\n\n\nFigure 10a: Microcosm three-peaked rock.\n\n\nFigure 10b: Closer image.\n\n\nFigure 10c: Closer image again.\n\n\nFigure 11: Dattatreya Peak\n\n\n\nFigure 12a: Side of a peak.\n\n\nFigure 12b: Lower segment.\n\n\nFigure 13: More sharp edged rocks.\n\n\nFigure 14: More sharp edged rocks.\n\n\nFigure 15: View of terrain.\n\n\nFigure 16: Mount Girnar.\n\n\nFigure 17: Mount Girnar.\n\n\nFigure 18: Mount Girnar.\n\n\nFigure 19: Mount Girnar.\n\n\nFigure 20: River of Mount Girnar with distinct rocks.\n\n\nFigure 21: Mount Girnar.\n\n\nFigure 22: Mount Girnar.\n\n\nFigure 23: Mount Girnar.\n\n\nFigure 24: River rocks.\n\n\nFigure 25: River rocks.\n\n\nFigure 26: River rocks.\n\n\nFigure 27: River rocks.\n\n\nFigure 28: River rocks.\n\n\nFigure 29: Temple built around stream\n\n\nFigure 30: Mount Girnar.\n\n\nFigure 31: Mount Girnar.\n\n\nFigure 32: Peaks of Girnar.\n\n\nFigure 33: Mount Girnar with Bhavnath Temple visible where Shivaling is said to have emerged of its own intention.\n\n\nFigure 34: Dattatreya Peak.\n\n\nFigure 35: Mountain peaks.\n\nSources: \nFigures 1-8: [Girnar Vlog | Girnar part-2 | Dattatrey Temple | Monsoon Trip | 2022](https://www.youtube.com/watch?v=L7w1ln3MW0o)\nRest of images from Aapdu Junagadh:\n[Junagadh and its Glory | Happy Independence Day | Junagadh | Aapdu Junagadh](https://www.youtube.com/watch?v=RW2PBW6jKek)\n[વરસાદ પહેલાંના અને પછીના જૂનાગઢના આ દ્રશ્યો ખરેખર અદ્દભુત છે! | The time lapse of Junagadh | Girnar](https://www.youtube.com/watch?v=wAZMesuPfbQ)\n[ચોમાસામાં સ્વર્ગ બની જતું,જૂનાગઢવાસીઓનું ફેવરિટ પ્લેસ |Jata Shankar| Best Place to Visit in Junagadh](https://www.youtube.com/watch?v=KCHcDK8HJws)\n[Safar Saurashtra Ni | Girnar & Girnar Ropeway | Ft. Purva Mehta | Junagadh | Aapdu Junagadh](https://www.youtube.com/watch?v=8Zq-R9K8HAU)",
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"parent_author": "",
"parent_permlink": "girnar",
"permlink": "mount-girnar-rocks",
"title": "Mount Girnar Rocks"
}
],
"op_in_trx": 0,
"timestamp": "2022-09-16T21:37:48",
"trx_id": "72caa36cb52772f74f0a2060f30ce4abba5341fe",
"trx_in_block": 0,
"virtual_op": 0
}stevescullyreceived 0.041 STEEM, 0.045 SP author reward for @stevescully / sacred-geometry-of-mount-girnar2022/09/12 04:07:39
stevescullyreceived 0.041 STEEM, 0.045 SP author reward for @stevescully / sacred-geometry-of-mount-girnar
2022/09/12 04:07:39
| author | stevescully |
| permlink | sacred-geometry-of-mount-girnar |
| sbd payout | 0.000 SBD |
| steem payout | 0.041 STEEM |
| vesting payout | 73.841206 VESTS |
| Transaction Info | Block #67614226/Virtual Operation #5 |
View Raw JSON Data
{
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"op": [
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{
"author": "stevescully",
"permlink": "sacred-geometry-of-mount-girnar",
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"vesting_payout": "73.841206 VESTS"
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"op_in_trx": 0,
"timestamp": "2022-09-12T04:07:39",
"trx_id": "0000000000000000000000000000000000000000",
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}stevescullypublished a new post: mount-girnar-the-catalyst2022/09/12 02:52:15
stevescullypublished a new post: mount-girnar-the-catalyst
2022/09/12 02:52:15
| author | stevescully |
| body | @@ -8524,12 +8524,9 @@ 63.6 - %C2%B1 +- 56.2 |
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| parent permlink | geology |
| permlink | mount-girnar-the-catalyst |
| title | Mount Girnar: The Catalyst |
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}stevescullypublished a new post: mount-girnar-the-catalyst2022/09/12 02:49:18
stevescullypublished a new post: mount-girnar-the-catalyst
2022/09/12 02:49:18
| author | stevescully |
| body | # Introduction Positioned in the midst of the Deccan Traps, Mount Girnar rises out of the plains of Kathiawar. Considered to be an intrusion formed around the Cretaceous-Paleogene boundary, the formation is unlike any other on Earth.  Figure 1: *View of Mount Girnar from Bhavnath in Junagadh city of Gujarat, India* # What Is In a Name? The formation is known by many names. By Jains it is known as Mount Neminath, where Lord Neminatha is said to have obtained nirvana. It is also believed to be the location where the *next* twenty-four [tirthankaras](https://en.wikipedia.org/wiki/Tirthankara) *will* obtain nirvana. Girnar comes from the root sanskrit words of [*gir*](https://www.wisdomlib.org/definition/gir), meaning *"addressing; invoking; invocation, praise, song; a mountain"*, and [*nar*](https://www.wisdomlib.org/definition/nar), meaning *"a man; husband; hero; the primordial Man; a lion-hearted man."* It is also known as *Girinagar*, [*giri*](https://www.wisdomlib.org/definition/giri) meaning *"mountain; hill"* and [*nagar*](https://www.wisdomlib.org/definition/nagar) meaning *"city; town."* Additionally the mountain is known as Revatak Parvata. [Revata](https://www.wisdomlib.org/definition/revata) means *"a boar; a bamboo cane;* **a whirlwind"** and [*parvata*](https://www.wisdomlib.org/definition/parvata) means *"a mountain, hill; a rock; an artificial mountain or heap; the number 'seven', a tree, a kind of vegetable, a cloud (mountain-like)."* Anciently it was known as *Raivatagiri* and *Ujjayantagiri*, where [*raivata*](https://www.wisdomlib.org/definition/raivata) means *"brilliant, rich, wealthy, plentiful, splendid, beautiful,"* and [*ujjayanta*](https://www.wisdomlib.org/definition/ujjayanta) refers to a temple/building. Its [first names](http://junagadhgirnar.com/18-girnar-names/) were Kailashgiri and Svarnagiri. *Kailasa* refers to a type of temple, and is associated with a mountain in Tibet. Kailasa is also the name of the temple *carved into a mountain* at the Ellora Caves in Maharashtra, India. [*Svarna*](https://www.wisdomlib.org/definition/svarna) means *"gold."*  Figure 2: *[Kailasa Temple](https://en.wikipedia.org/wiki/Kailasa_Temple,_Ellora), Ellora Caves, India* Additional names attributed to Mount Girnar have been *Girinarayana, Giriraj, Urjayat, Gomanta, Raivatari, Vastrapatha, Lingakara, Kanchana, Grimunga, Girinayara, Pushpagiri, Highland of St. John, Girnal, Karnal, Killa-e-Girnar, Devagiri,* and more. For additional information on its many names, see [Girinagar: Junagadh and Mount Girnar - One of the Most Ancient and Sacred Sites of India](http://junagadhgirnar.com/18-girnar-names/) And yet, it is also known as Girnar *Hill.* Standing at 3,672 feet at the highest point of this five-peaked mountain, when we compare it to the many other options of places to study geologically, it does not stand first by any historical metric of comparing geological features on Earth. Mount Everest, by comparison, is 29,032 feet tall--nearly *eight times the elevation of Mount Girnar.* For another comparison, Mount Everest is [also known](https://education.nationalgeographic.org/resource/mount-everest) by Tibetans as Chomolungma, meaning *"Mother Goddess of the World,"* and by Nepalese as Sagarmatha, [*"Goddess of the Sky."*](https://www.montana.edu/everest/facts/naming.html) Where Girnar's list of names is nonexhaustive, this appears to be the full extent of alternative names for the tallest mountain in the world. If a rose by any other name would smell as sweet, would a mountain by many other names indicate its importance over lesser *named* geological features? Then, there is the fact that it sits alone in the plains of the Deccan Traps. With a 9 mile radius, it pales in comparison to the vast expanse of mountain chains like the Andes, which run *4,300 miles (7,000 kilometers)* along the entire western stretch of South America with an *average elevation in the range of 13,000 feet.* The Rockies, the Alps, the Himalayas. *These* are *mountains.* As described by [Cucciniello et al.<sup>1</sup>](https://www.researchgate.net/profile/Hetu-Sheth/publication/359368565_Mantle_and_crustal_contributions_to_the_Mount_Girnar_alkaline_plutonic_complex_and_the_circum-Girnar_mafic-silicic_intrusions_of_Saurashtra_northwestern_Deccan_Traps_2022/links/6237f839be72d414dad0e821/Mantle-and-crustal-contributions-to-the-Mount-Girnar-alkaline-plutonic-complex-and-the-circum-Girnar-mafic-silicic-intrusions-of-Saurashtra-northwestern-Deccan-Traps-2022.pdf), as of *2022*: >*"most of the studies relating to the plutonic complex and the silicic ring dyke are dated, whereas the circum-Girnar mafic intrusions...have been practically unstudied."* Standard metrics for ascertaining the significance of a mountain are all based on sheer size. Mountains can be arranged by their [*prominence*](https://en.wikipedia.org/wiki/List_of_mountain_peaks_by_prominence)--their elevation above the local terrain--or [by their elevation above sea level.](https://en.wikipedia.org/wiki/List_of_highest_mountains_on_Earth) Mount Everest sits atop both of these lists and Mount Girnar does not *fit in* to this method of analysis. As a result, it pales in comparison to other mountains when analyzed by basic metrics. While the mountain has received very little attention from the geological community, it has been ascribed with a long list of honorary titles. The reverence and love for Girnar has brought it to be the home to over 800 Hindu and Jain Temples. But its unique geological nature has not gone entirely unnoticed. In ["Magmatic Differentiation in Mount Girnar,"<sup>2</sup>](https://www.journals.uchicago.edu/doi/epdf/10.1086/623314) by Mathur et al. from The Journal of Geology in 1926, they explain: >*"The Girnar Hills form an imposing and characteristic land mass in the plains of Kathiawar. Considerable importance attaches to them from a religious and archaeological point of view, and the shrines on the top of the hill are visited by a large number of pilgrims every year. **Geologically, they are no less important, yet so far little information exists about the interesting varieties of rocks they contain, or the structure of the hill ranges.**"* Here, Mathur et al. compare the importance of the geological structures of Mount Girnar to its religious importance, calling the geology of Mount Girnar ***"no less important."*** # The Geology of Mount Girnar Mount Girnar's position in the heart of the [Deccan Traps](https://en.wikipedia.org/wiki/Deccan_Traps) makes it a curious anomaly. The Deccan Traps are a [large igneous province](https://en.wikipedia.org/wiki/Large_igneous_province) considered to be the result of a wide-spread eruption ~66Ma (million years ago). Notably, this coincides with the formation of the Chicxulub crater and the [K-Pg boundary layer](https://en.wikipedia.org/wiki/Cretaceous%E2%80%93Paleogene_boundary). They are a solidified flood basalt that is over 2,000 meters thick and 500,000 square kilometers. As described by Mathur et al.: >*"The quaquaversal dip in the surrounding basalt and the topographic features are possibly suggestive of a volcano, but there is little doubt that the rocks constitute a plutonic intrusion in the form of a laccolith, with a large number of differentiated types, which is probably* ***unique*** *in being the first of its kind studied in India."*  Figure 3: *[Google Earth](https://earth.google.com/) depicting Mount Girnar with surrounding basalt having a quaquaversal (directed outward from a common center towards all points of the compass) dip in its elevations.* In 1926, Mathur et al.<sup>2</sup> considered Girnar to have intruded during *"late Cretaceous, or early Eocene;"* 66 - 55 Ma. It has been established to have begun its formation process near the time of the K-Pg Boundary formation. Given a date of 65.3 ± 1.3 Ma in 1973 <sup>3</sup>, it is considered to *belong* to the Deccan Traps. Based on whole rock K/Ar ratios, Girnar has been dated with large error bars to 63.6 ± 56.2 Ma<sup>4</sup>. The geology of Saurashtra, India has two differing features from the bulk of the Deccan Traps<sup>1</sup>: 1) *Numerous plutonic complexes* dominated by gabbros and granophyres with diorite and monzonite important to Mount Girnar, and 2) *A wide range of rock types.*  Figure 4: [Saurashtra Region map](https://en.wikipedia.org/wiki/Saurashtra_%28region%29)  Figure 5: *Mount Girnar is seen as the "eye of the bird" of Saurashtra.* As shown by Mathur et al.<sup>2</sup>,where the map was updated by Cucciniello et al.<sup>1</sup>, Girnar is highly complex in its differentiation. Sections of the mountain are composed of specific materials and void of the materials of other sections. Separately, the intrusion was found to have segments of basalt, granophyre, olivine-gabbro, and diorite/monzonite:  Figure 6: *Cucciniello et al. updated map of Mathur et al.* Magmatic differentiation is the process by which chemically different igneous rocks, such as basalt and granite, can form from the same initial magma. On Girnar, the central mountain has peaks which run west to east, composed generally of diorite and monzonite. The mountain can be separated into four geological components<sup>2</sup>: 1) *The circular outer ranges of hills,* 2) *The central mountain,* 3) *Radial ridges joining the central mountain to the outer hills; and* 4) *Low plains occupying the intervening area.* The circular outer range of hills is, generally speaking, deeply escarped on the inner faces with gentler outer slopes. It is composed of *granophyre*, which is **restricted** to the outer hills, intruded through basalt.  Figure 7: *Steeply escarped granophyre intrusions with gentler slopes on outer faces.* These form a ring that is most pronounced in the South and diminishes in the East and Northeast directions of the mountain, *"but its continuity underground can be traced by veins too small to be shown on the map."* <sup>2</sup>  Figure 8: *[Topographic map of Mount Girnar](https://en-us.topographic-map.com/maps/bxn/India/)* This ring lies in a large **hexagonal** basaltic border to the mountain, as is especially apparent from the mountain's physical appearance shown above in Figure 3. This first hexagon of basalt has a ***second, smaller hexagonal slab*** of gabbro and olivine-gabbro--partly covered by alluvium and intrusions--as is visible in Figure 6. Similar to the ring of granophyre surrounding the mountain within the larger hexagonal basalt, the second hexagon of gabbro has a ring within it of basalt:  Figure 9: *Zoom in on the second hexagon overlaid with alluvium and a basalt ring.* All of which is generally centered on the inner mountain of Girnar which is composed of diorite, monzonite, and biotite<sup>1,2</sup>. The biotite is especially restricted to the periphery of the central mountain and the junction with the surrounding olivine-gabbro. The radial ridges projecting outward from the central mountain to the surrounding ring of dikes are principally composed of olivine-gabbro, except at the junctions with the central mountain where biotite is prevalent<sup>2</sup>. Their structure can be seen in Figure 3, and the topography:  Figure 10: *[A zoomed in topographical map of Mount Girnar](https://en-us.topographic-map.com/maps/bxn/India/) showing the four ridges branching out from the central mountain to the surrounding circular dikes.* They dissect the region between the central mountain and outer ring into numerous ravines where plains of basalt on their outer margins and gabbro nearer the mountain, at times overlaid with deposits of alluvium from flowing streams, are enclosed.  Figure 11: *[A view of Dattatreya Peak and the central mountain in the forefront, with the surrounding dikes and ravines visible.](https://www.gujarattourism.com/saurashtra/junagadh/girnar-hill.html)* As a result of the rich geological nature of Mount Girnar, it has been considered a unique opportunity to study magmatic differentiation. As stated by Mathur et al.<sup>2</sup>: >*"From the description of the rock types and their close relationship in the field...., it is clear that this unique assemblage can only be regarded as one petrological unit derived from a common magma."* >*"The separation of a magma into two immiscible phases in the liquid condition has been regarded as one of the possible causes of differentiation. ...It is possible that the conditions which may bring about the separation of two liquid phases in a silicate melt* ***did not exist*** *in this reservoir."* >*"The facts of the case appear to be in better accord with the scheme of crystallization differentiation suggested by Bowen."* In short, the process discussed by Bowen is one in which volatiles play an important part in the separation of the magma. As Mathur et al. state: >*"It is probable that in most granite batholiths the volatiles are distributed more or less evenly throughout the mass, whereas the actual concentration at any one place is not sufficiently high to effect the dissociation and separation of the alkali magma by the process contemplated [by Bowen]."* Evidence strongly suggests the separation process to have occurred, thus, due to the presence of volatiles and conditions capable of separating magma intrusions by crystallizations of different materials at different stages from a single source magma. Further discussed by Cucciniello et al.<sup>1</sup>, there are what appear to be radially arranged, with respect to the plutonic complex of Mount Girnar, intrusions of dikes and sills, which are referred to as *circum-Girnar intrusions:*  Figure 12: *[Cucciniello et al.](https://www.researchgate.net/profile/Hetu-Sheth/publication/359368565_Mantle_and_crustal_contributions_to_the_Mount_Girnar_alkaline_plutonic_complex_and_the_circum-Girnar_mafic-silicic_intrusions_of_Saurashtra_northwestern_Deccan_Traps_2022/links/6237f839be72d414dad0e821/Mantle-and-crustal-contributions-to-the-Mount-Girnar-alkaline-plutonic-complex-and-the-circum-Girnar-mafic-silicic-intrusions-of-Saurashtra-northwestern-Deccan-Traps-2022.pdf) map of dykes and mafic intrusions especially prevalent east of Mount Girnar's plutonic complex.* Their study shows that some of the intrusions assimilated crustal material. The central mass has **negligible assimilation** of crustal material in the genesis of the most evolved materials of the mountain, but the surrounding dykes and sill, as well as the granophyre ring, all demonstrate degrees of assimilation of crust. Thus, it has been suggested that the central region had significantly thinner ancient crust than the surroundings. Notably, they further conclude the granophyre ring to be unrelated structurally to the plutonic complex of the mountain, though this seems unlikely. This stems from both their distance away from the center, as well as the genetics of the rocks being so varied. # Ancient Dwarka While the mountain is heavily covered with temples, as well as 9,999 stairs to the highest peak, and positioned in ancient lands, the first evidence of civilization at the mountain is only from 150 CE. The Junagadh rock inscription of Rudradaman has been dated to far more recent times than the mountain may otherwise warrant. Was it unnoticeable historically? Or did it ***not even exist yet at all?*** Evidence strongly suggests that Mount Girnar [emerged in a vortex of energy due to a weapon attack on Ancient Dwarka](https://www.youtube.com/watch?v=qRriWdNTUKY); that the whole of the Deccan Traps were caused by this weapon. Indeed, that the whole Earth fractured apart and a global flood ensued. And as a result of the process, Mount Girnar was ***emitted from the center of the Earth in a whirlwind of energy.*** Today, the mountain is circumambulated yearly during the Lili Parikrama:  Figure 13: *[Girnar Parikrama Route Map](https://blog.yatradham.org/girnar-parikrama-route-map-girnar-parvat-yatra-girnar-mountain-dattatreya/).* Due to the vortex of energy in the formation of the mountain, there are distinct characteristics of [Sacred Geometry in the energy flows creating Mount Girnar](https://steemit.com/geology/@stevescully/sacred-geometry-of-mount-girnar). The presence of the hexagonal sheets of basalt and olivine-gabbro discussed above further supports the vortices involved in the formation of the mountain. Indeed, Dattatreya Peak is imprinted with the process:  Figure 14: [*Dattatreya peak in a spiral formation.*](https://youtu.be/wO4-3YR-Ayg?t=35) # Conclusion Truly, this mountain is from heaven.  Figure 15: *[Bhutanese thangka of Mount Meru and the Buddhist universe](https://en.wikipedia.org/wiki/Mount_Meru)* Additional links: [Dwarka: The Lost City of Krishna](https://steemit.com/philosophy/@stevescully/dwarka-the-lost-city-of-krishna) [The Geopolitical Impact of the Discovery of Ancient Dwarka](https://steemit.com/history/@stevescully/the-geopolitical-impact-of-the-discovery-of-ancient-dwarka) [Ancient Dwarka: Tales in the Land](https://steemit.com/science/@stevescully/ancient-dwarka-tales-in-the-land) [Ancient Dwarka: The Chicxulub Connection](https://steemit.com/science/@stevescully/ancient-dwarka-the-chicxulub-connection) References: 1. ["Mantle and Crustal Contributions to the Mount Girnar Alkaline Plutonic Complex and the Circum-Girnar Mafic-Silicic Intrusions of Saurashtra, Northwestern Deccan Traps," Cucciniello et al., Journal of Petrology, 2022, Vol. 63, No. 3, 1–30](https://www.researchgate.net/profile/Hetu-Sheth/publication/359368565_Mantle_and_crustal_contributions_to_the_Mount_Girnar_alkaline_plutonic_complex_and_the_circum-Girnar_mafic-silicic_intrusions_of_Saurashtra_northwestern_Deccan_Traps_2022/links/6237f839be72d414dad0e821/Mantle-and-crustal-contributions-to-the-Mount-Girnar-alkaline-plutonic-complex-and-the-circum-Girnar-mafic-silicic-intrusions-of-Saurashtra-northwestern-Deccan-Traps-2022.pdf) 2. ["Magmatic Differentiation in Mount Girnar," Mathur et al., The Journal of Geology, Volume XXXIV, No.4, 1926.](https://www.journals.uchicago.edu/doi/epdf/10.1086/623314) 3. [Kaneoka, I. & Haramura, H. (1973). K/Ar ages of successive lava flows from the Deccan Traps, India. Earth and Planetary Science Letters 18, 229–236.](https://www.researchgate.net/publication/248410542_KAr_ages_of_successive_lava_flows_from_the_Deccan_Traps_India) 4. [Paul et al. (1977). Geochemical and petrogenetic study of the Girnar igneous complex, Deccan volcanic province, India. Geological Society of American Bulletin 88, 227–234.](https://pubs.geoscienceworld.org/gsa/gsabulletin/article-abstract/88/2/227/202067/Geochemical-and-petrogenetic-study-of-the-Girnar) |
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| parent author | |
| parent permlink | geology |
| permlink | mount-girnar-the-catalyst |
| title | Mount Girnar: The Catalyst |
| Transaction Info | Block #67612667/Trx 58b375ea2a034b3e98198c98623e3364132bcaf9 |
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"body": "# Introduction\nPositioned in the midst of the Deccan Traps, Mount Girnar rises out of the plains of Kathiawar. Considered to be an intrusion formed around the Cretaceous-Paleogene boundary, the formation is unlike any other on Earth.\n\n\nFigure 1: *View of Mount Girnar from Bhavnath in Junagadh city of Gujarat, India*\n\n# What Is In a Name?\nThe formation is known by many names. \n\nBy Jains it is known as Mount Neminath, where Lord Neminatha is said to have obtained nirvana. It is also believed to be the location where the *next* twenty-four [tirthankaras](https://en.wikipedia.org/wiki/Tirthankara) *will* obtain nirvana.\n\nGirnar comes from the root sanskrit words of [*gir*](https://www.wisdomlib.org/definition/gir), meaning *\"addressing; invoking; invocation, praise, song; a mountain\"*, and [*nar*](https://www.wisdomlib.org/definition/nar), meaning *\"a man; husband; hero; the primordial Man; a lion-hearted man.\"*\n\nIt is also known as *Girinagar*, [*giri*](https://www.wisdomlib.org/definition/giri) meaning *\"mountain; hill\"* and [*nagar*](https://www.wisdomlib.org/definition/nagar) meaning *\"city; town.\"*\n\nAdditionally the mountain is known as Revatak Parvata. [Revata](https://www.wisdomlib.org/definition/revata) means *\"a boar; a bamboo cane;* **a whirlwind\"** and [*parvata*](https://www.wisdomlib.org/definition/parvata) means *\"a mountain, hill; a rock; an artificial mountain or heap; the number 'seven', a tree, a kind of vegetable, a cloud (mountain-like).\"*\n\nAnciently it was known as *Raivatagiri* and *Ujjayantagiri*, where [*raivata*](https://www.wisdomlib.org/definition/raivata) means *\"brilliant, rich, wealthy, plentiful, splendid, beautiful,\"* and [*ujjayanta*](https://www.wisdomlib.org/definition/ujjayanta) refers to a temple/building.\n\nIts [first names](http://junagadhgirnar.com/18-girnar-names/) were Kailashgiri and Svarnagiri. *Kailasa* refers to a type of temple, and is associated with a mountain in Tibet. Kailasa is also the name of the temple *carved into a mountain* at the Ellora Caves in Maharashtra, India. [*Svarna*](https://www.wisdomlib.org/definition/svarna) means *\"gold.\"*\n\n\nFigure 2: *[Kailasa Temple](https://en.wikipedia.org/wiki/Kailasa_Temple,_Ellora), Ellora Caves, India*\n\nAdditional names attributed to Mount Girnar have been *Girinarayana, Giriraj, Urjayat, Gomanta, Raivatari, Vastrapatha, Lingakara, Kanchana, Grimunga, Girinayara, Pushpagiri, Highland of St. John, Girnal, Karnal, Killa-e-Girnar, Devagiri,* and more. For additional information on its many names, see [Girinagar: Junagadh and Mount Girnar - One of the Most Ancient and Sacred Sites of India](http://junagadhgirnar.com/18-girnar-names/)\n\nAnd yet, it is also known as Girnar *Hill.* Standing at 3,672 feet at the highest point of this five-peaked mountain, when we compare it to the many other options of places to study geologically, it does not stand first by any historical metric of comparing geological features on Earth.\n\nMount Everest, by comparison, is 29,032 feet tall--nearly *eight times the elevation of Mount Girnar.* \n\nFor another comparison, Mount Everest is [also known](https://education.nationalgeographic.org/resource/mount-everest) by Tibetans as Chomolungma, meaning *\"Mother Goddess of the World,\"* and by Nepalese as Sagarmatha, [*\"Goddess of the Sky.\"*](https://www.montana.edu/everest/facts/naming.html) Where Girnar's list of names is nonexhaustive, this appears to be the full extent of alternative names for the tallest mountain in the world. \n\nIf a rose by any other name would smell as sweet, would a mountain by many other names indicate its importance over lesser *named* geological features?\n\nThen, there is the fact that it sits alone in the plains of the Deccan Traps. With a 9 mile radius, it pales in comparison to the vast expanse of mountain chains like the Andes, which run *4,300 miles (7,000 kilometers)* along the entire western stretch of South America with an *average elevation in the range of 13,000 feet.* The Rockies, the Alps, the Himalayas. *These* are *mountains.*\n\nAs described by [Cucciniello et al.<sup>1</sup>](https://www.researchgate.net/profile/Hetu-Sheth/publication/359368565_Mantle_and_crustal_contributions_to_the_Mount_Girnar_alkaline_plutonic_complex_and_the_circum-Girnar_mafic-silicic_intrusions_of_Saurashtra_northwestern_Deccan_Traps_2022/links/6237f839be72d414dad0e821/Mantle-and-crustal-contributions-to-the-Mount-Girnar-alkaline-plutonic-complex-and-the-circum-Girnar-mafic-silicic-intrusions-of-Saurashtra-northwestern-Deccan-Traps-2022.pdf), as of *2022*: \n>*\"most of the studies relating to the plutonic complex and the silicic ring dyke are dated, whereas the circum-Girnar mafic intrusions...have been practically unstudied.\"*\n\nStandard metrics for ascertaining the significance of a mountain are all based on sheer size. Mountains can be arranged by their [*prominence*](https://en.wikipedia.org/wiki/List_of_mountain_peaks_by_prominence)--their elevation above the local terrain--or [by their elevation above sea level.](https://en.wikipedia.org/wiki/List_of_highest_mountains_on_Earth) Mount Everest sits atop both of these lists and Mount Girnar does not *fit in* to this method of analysis. As a result, it pales in comparison to other mountains when analyzed by basic metrics.\n\nWhile the mountain has received very little attention from the geological community, it has been ascribed with a long list of honorary titles. The reverence and love for Girnar has brought it to be the home to over 800 Hindu and Jain Temples.\n\nBut its unique geological nature has not gone entirely unnoticed.\n\nIn [\"Magmatic Differentiation in Mount Girnar,\"<sup>2</sup>](https://www.journals.uchicago.edu/doi/epdf/10.1086/623314) by Mathur et al. from The Journal of Geology in 1926, they explain:\n>*\"The Girnar Hills form an imposing and characteristic land mass in the plains of Kathiawar. Considerable importance attaches to them from a religious and archaeological point of view, and the shrines on the top of the hill are visited by a large number of pilgrims every year. **Geologically, they are no less important, yet so far little information exists about the interesting varieties of rocks they contain, or the structure of the hill ranges.**\"*\n\nHere, Mathur et al. compare the importance of the geological structures of Mount Girnar to its religious importance, calling the geology of Mount Girnar ***\"no less important.\"***\n\n# The Geology of Mount Girnar\nMount Girnar's position in the heart of the [Deccan Traps](https://en.wikipedia.org/wiki/Deccan_Traps) makes it a curious anomaly. The Deccan Traps are a [large igneous province](https://en.wikipedia.org/wiki/Large_igneous_province) considered to be the result of a wide-spread eruption ~66Ma (million years ago). Notably, this coincides with the formation of the Chicxulub crater and the [K-Pg boundary layer](https://en.wikipedia.org/wiki/Cretaceous%E2%80%93Paleogene_boundary). They are a solidified flood basalt that is over 2,000 meters thick and 500,000 square kilometers.\n\nAs described by Mathur et al.:\n>*\"The quaquaversal dip in the surrounding basalt and the topographic features are possibly suggestive of a volcano, but there is little doubt that the rocks constitute a plutonic intrusion in the form of a laccolith, with a large number of differentiated types, which is probably* ***unique*** *in being the first of its kind studied in India.\"*\n\n\nFigure 3: *[Google Earth](https://earth.google.com/) depicting Mount Girnar with surrounding basalt having a quaquaversal (directed outward from a common center towards all points of the compass) dip in its elevations.*\n\nIn 1926, Mathur et al.<sup>2</sup> considered Girnar to have intruded during *\"late Cretaceous, or early Eocene;\"* 66 - 55 Ma.\n\nIt has been established to have begun its formation process near the time of the K-Pg Boundary formation. Given a date of 65.3 ± 1.3 Ma in 1973 <sup>3</sup>, it is considered to *belong* to the Deccan Traps.\n\nBased on whole rock K/Ar ratios, Girnar has been dated with large error bars to 63.6 ± 56.2 Ma<sup>4</sup>.\n\nThe geology of Saurashtra, India has two differing features from the bulk of the Deccan Traps<sup>1</sup>:\n1) *Numerous plutonic complexes* dominated by gabbros and granophyres with diorite and monzonite important to Mount Girnar, and\n2) *A wide range of rock types.*\n\n\nFigure 4: [Saurashtra Region map](https://en.wikipedia.org/wiki/Saurashtra_%28region%29)\n\n\nFigure 5: *Mount Girnar is seen as the \"eye of the bird\" of Saurashtra.*\n\nAs shown by Mathur et al.<sup>2</sup>,where the map was updated by Cucciniello et al.<sup>1</sup>, Girnar is highly complex in its differentiation. Sections of the mountain are composed of specific materials and void of the materials of other sections. \n\nSeparately, the intrusion was found to have segments of basalt, granophyre, olivine-gabbro, and diorite/monzonite:\n\nFigure 6: *Cucciniello et al. updated map of Mathur et al.*\n\nMagmatic differentiation is the process by which chemically different igneous rocks, such as basalt and granite, can form from the same initial magma.\n\nOn Girnar, the central mountain has peaks which run west to east, composed generally of diorite and monzonite.\n\nThe mountain can be separated into four geological components<sup>2</sup>:\n1) *The circular outer ranges of hills,*\n2) *The central mountain,*\n3) *Radial ridges joining the central mountain to the outer hills; and*\n4) *Low plains occupying the intervening area.*\n\nThe circular outer range of hills is, generally speaking, deeply escarped on the inner faces with gentler outer slopes. It is composed of *granophyre*, which is **restricted** to the outer hills, intruded through basalt.\n\n\nFigure 7: *Steeply escarped granophyre intrusions with gentler slopes on outer faces.*\n\nThese form a ring that is most pronounced in the South and diminishes in the East and Northeast directions of the mountain, *\"but its continuity underground can be traced by veins too small to be shown on the map.\"* <sup>2</sup>\n\n\nFigure 8: *[Topographic map of Mount Girnar](https://en-us.topographic-map.com/maps/bxn/India/)*\n\nThis ring lies in a large **hexagonal** basaltic border to the mountain, as is especially apparent from the mountain's physical appearance shown above in Figure 3. This first hexagon of basalt has a ***second, smaller hexagonal slab*** of gabbro and olivine-gabbro--partly covered by alluvium and intrusions--as is visible in Figure 6.\n\nSimilar to the ring of granophyre surrounding the mountain within the larger hexagonal basalt, the second hexagon of gabbro has a ring within it of basalt:\n\n\nFigure 9: *Zoom in on the second hexagon overlaid with alluvium and a basalt ring.*\n\nAll of which is generally centered on the inner mountain of Girnar which is composed of diorite, monzonite, and biotite<sup>1,2</sup>. The biotite is especially restricted to the periphery of the central mountain and the junction with the surrounding olivine-gabbro.\n\nThe radial ridges projecting outward from the central mountain to the surrounding ring of dikes are principally composed of olivine-gabbro, except at the junctions with the central mountain where biotite is prevalent<sup>2</sup>. Their structure can be seen in Figure 3, and the topography:\n\n\nFigure 10: *[A zoomed in topographical map of Mount Girnar](https://en-us.topographic-map.com/maps/bxn/India/) showing the four ridges branching out from the central mountain to the surrounding circular dikes.*\n \nThey dissect the region between the central mountain and outer ring into numerous ravines where plains of basalt on their outer margins and gabbro nearer the mountain, at times overlaid with deposits of alluvium from flowing streams, are enclosed.\n\n\nFigure 11: *[A view of Dattatreya Peak and the central mountain in the forefront, with the surrounding dikes and ravines visible.](https://www.gujarattourism.com/saurashtra/junagadh/girnar-hill.html)*\n\n\nAs a result of the rich geological nature of Mount Girnar, it has been considered a unique opportunity to study magmatic differentiation. As stated by Mathur et al.<sup>2</sup>:\n>*\"From the description of the rock types and their close relationship in the field...., it is clear that this unique assemblage can only be regarded as one petrological unit derived from a common magma.\"*\n\n>*\"The separation of a magma into two immiscible phases in the liquid condition has been regarded as one of the possible causes of differentiation. ...It is possible that the conditions which may bring about the separation of two liquid phases in a silicate melt* ***did not exist*** *in this reservoir.\"*\n\n>*\"The facts of the case appear to be in better accord with the scheme of crystallization differentiation suggested by Bowen.\"*\n\nIn short, the process discussed by Bowen is one in which volatiles play an important part in the separation of the magma. As Mathur et al. state:\n>*\"It is probable that in most granite batholiths the volatiles are distributed more or less evenly throughout the mass, whereas the actual concentration at any one place is not sufficiently high to effect the dissociation and separation of the alkali magma by the process contemplated [by Bowen].\"*\n\nEvidence strongly suggests the separation process to have occurred, thus, due to the presence of volatiles and conditions capable of separating magma intrusions by crystallizations of different materials at different stages from a single source magma.\n\nFurther discussed by Cucciniello et al.<sup>1</sup>, there are what appear to be radially arranged, with respect to the plutonic complex of Mount Girnar, intrusions of dikes and sills, which are referred to as *circum-Girnar intrusions:*\n\n\nFigure 12: *[Cucciniello et al.](https://www.researchgate.net/profile/Hetu-Sheth/publication/359368565_Mantle_and_crustal_contributions_to_the_Mount_Girnar_alkaline_plutonic_complex_and_the_circum-Girnar_mafic-silicic_intrusions_of_Saurashtra_northwestern_Deccan_Traps_2022/links/6237f839be72d414dad0e821/Mantle-and-crustal-contributions-to-the-Mount-Girnar-alkaline-plutonic-complex-and-the-circum-Girnar-mafic-silicic-intrusions-of-Saurashtra-northwestern-Deccan-Traps-2022.pdf) map of dykes and mafic intrusions especially prevalent east of Mount Girnar's plutonic complex.*\n\nTheir study shows that some of the intrusions assimilated crustal material. The central mass has **negligible assimilation** of crustal material in the genesis of the most evolved materials of the mountain, but the surrounding dykes and sill, as well as the granophyre ring, all demonstrate degrees of assimilation of crust. Thus, it has been suggested that the central region had significantly thinner ancient crust than the surroundings.\n\nNotably, they further conclude the granophyre ring to be unrelated structurally to the plutonic complex of the mountain, though this seems unlikely. This stems from both their distance away from the center, as well as the genetics of the rocks being so varied.\n\n# Ancient Dwarka\nWhile the mountain is heavily covered with temples, as well as 9,999 stairs to the highest peak, and positioned in ancient lands, the first evidence of civilization at the mountain is only from 150 CE. The Junagadh rock inscription of Rudradaman has been dated to far more recent times than the mountain may otherwise warrant. Was it unnoticeable historically?\n\nOr did it ***not even exist yet at all?*** \n\nEvidence strongly suggests that Mount Girnar [emerged in a vortex of energy due to a weapon attack on Ancient Dwarka](https://www.youtube.com/watch?v=qRriWdNTUKY); that the whole of the Deccan Traps were caused by this weapon. Indeed, that the whole Earth fractured apart and a global flood ensued.\n\nAnd as a result of the process, Mount Girnar was ***emitted from the center of the Earth in a whirlwind of energy.***\n\nToday, the mountain is circumambulated yearly during the Lili Parikrama:\n\nFigure 13: *[Girnar Parikrama Route Map](https://blog.yatradham.org/girnar-parikrama-route-map-girnar-parvat-yatra-girnar-mountain-dattatreya/).*\n\nDue to the vortex of energy in the formation of the mountain, there are distinct characteristics of [Sacred Geometry in the energy flows creating Mount Girnar](https://steemit.com/geology/@stevescully/sacred-geometry-of-mount-girnar).\n\nThe presence of the hexagonal sheets of basalt and olivine-gabbro discussed above further supports the vortices involved in the formation of the mountain. Indeed, Dattatreya Peak is imprinted with the process:\n\n\nFigure 14: [*Dattatreya peak in a spiral formation.*](https://youtu.be/wO4-3YR-Ayg?t=35)\n\n# Conclusion\nTruly, this mountain is from heaven.\n\n\nFigure 15: *[Bhutanese thangka of Mount Meru and the Buddhist universe](https://en.wikipedia.org/wiki/Mount_Meru)*\n\n\nAdditional links:\n[Dwarka: The Lost City of Krishna](https://steemit.com/philosophy/@stevescully/dwarka-the-lost-city-of-krishna)\n[The Geopolitical Impact of the Discovery of Ancient Dwarka](https://steemit.com/history/@stevescully/the-geopolitical-impact-of-the-discovery-of-ancient-dwarka)\n[Ancient Dwarka: Tales in the Land](https://steemit.com/science/@stevescully/ancient-dwarka-tales-in-the-land)\n[Ancient Dwarka: The Chicxulub Connection](https://steemit.com/science/@stevescully/ancient-dwarka-the-chicxulub-connection)\n\nReferences:\n1. [\"Mantle and Crustal Contributions to the Mount Girnar Alkaline Plutonic Complex and the Circum-Girnar Mafic-Silicic Intrusions of Saurashtra, Northwestern Deccan Traps,\" Cucciniello et al., Journal of Petrology, 2022, Vol. 63, No. 3, 1–30](https://www.researchgate.net/profile/Hetu-Sheth/publication/359368565_Mantle_and_crustal_contributions_to_the_Mount_Girnar_alkaline_plutonic_complex_and_the_circum-Girnar_mafic-silicic_intrusions_of_Saurashtra_northwestern_Deccan_Traps_2022/links/6237f839be72d414dad0e821/Mantle-and-crustal-contributions-to-the-Mount-Girnar-alkaline-plutonic-complex-and-the-circum-Girnar-mafic-silicic-intrusions-of-Saurashtra-northwestern-Deccan-Traps-2022.pdf)\n2. [\"Magmatic Differentiation in Mount Girnar,\" Mathur et al., The Journal of Geology, Volume XXXIV, No.4, 1926.](https://www.journals.uchicago.edu/doi/epdf/10.1086/623314)\n3. [Kaneoka, I. & Haramura, H. (1973). K/Ar ages of successive lava flows from the Deccan Traps, India. Earth and Planetary Science Letters 18, 229–236.](https://www.researchgate.net/publication/248410542_KAr_ages_of_successive_lava_flows_from_the_Deccan_Traps_India)\n4. [Paul et al. (1977). Geochemical and petrogenetic study of the Girnar igneous complex, Deccan volcanic province, India. Geological Society of American Bulletin 88, 227–234.](https://pubs.geoscienceworld.org/gsa/gsabulletin/article-abstract/88/2/227/202067/Geochemical-and-petrogenetic-study-of-the-Girnar)",
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"title": "Mount Girnar: The Catalyst"
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}gruntbetaupvoted (100.00%) @stevescully / mount-girnar-the-catalyst2022/09/12 00:00:12
gruntbetaupvoted (100.00%) @stevescully / mount-girnar-the-catalyst
2022/09/12 00:00:12
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}gruntomegaupvoted (100.00%) @stevescully / mount-girnar-the-catalyst2022/09/11 23:59:39
gruntomegaupvoted (100.00%) @stevescully / mount-girnar-the-catalyst
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}gruntprimeupvoted (100.00%) @stevescully / mount-girnar-the-catalyst2022/09/11 23:59:06
gruntprimeupvoted (100.00%) @stevescully / mount-girnar-the-catalyst
2022/09/11 23:59:06
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}stevescullypublished a new post: mount-girnar-the-catalyst2022/09/11 23:54:54
stevescullypublished a new post: mount-girnar-the-catalyst
2022/09/11 23:54:54
| author | stevescully |
| body | # Introduction Positioned in the midst of the Deccan Traps, Mount Girnar rises out of the plains of Kathiawar. Considered to be an intrusion formed around the Cretaceous-Paleogene boundary, the formation is unlike any other on Earth.  Figure 1: *View of Mount Girnar from Bhavnath in Junagadh city of Gujarat, India* # What Is In a Name? The formation is known by many names. By Jains it is known as Mount Neminath, where Lord Neminatha is said to have obtained nirvana. It is also believed to be the location where the *next* twenty-four [tirthankaras](https://en.wikipedia.org/wiki/Tirthankara) *will* obtain nirvana. Girnar comes from the root sanskrit words of [*gir*](https://www.wisdomlib.org/definition/gir), meaning *"addressing; invoking; invocation, praise, song; a mountain"*, and [*nar*](https://www.wisdomlib.org/definition/nar), meaning *"a man; husband; hero; the primordial Man; a lion-hearted man."* It is also known as *Girinagar*, [*giri*](https://www.wisdomlib.org/definition/giri) meaning *"mountain; hill"* and [*nagar*](https://www.wisdomlib.org/definition/nagar) meaning *"city; town."* Additionally the mountain is known as Revatak Parvata. [Revata](https://www.wisdomlib.org/definition/revata) means *"a boar; a bamboo cane;* **a whirlwind"** and [*parvata*](https://www.wisdomlib.org/definition/parvata) means *"a mountain, hill; a rock; an artificial mountain or heap; the number 'seven', a tree, a kind of vegetable, a cloud (mountain-like)."* Anciently it was known as *Raivatagiri* and *Ujjayantagiri*, where [*raivata*](https://www.wisdomlib.org/definition/raivata) means *"brilliant, rich, wealthy, plentiful, splendid, beautiful,"* and [*ujjayanta*](https://www.wisdomlib.org/definition/ujjayanta) refers to a temple/building. Its [first names](http://junagadhgirnar.com/18-girnar-names/) were Kailashgiri and Svarnagiri. *Kailasa* refers to a type of temple, and is associated with a mountain in Tibet. Kailasa is also the name of the temple *carved into a mountain* at the Ellora Caves in Maharashtra, India. [*Svarna*](https://www.wisdomlib.org/definition/svarna) means *"gold."*  Figure 2: *[Kailasa Temple](https://en.wikipedia.org/wiki/Kailasa_Temple,_Ellora), Ellora Caves, India* Additional names attributed to Mount Girnar have been *Girinarayana, Giriraj, Urjayat, Gomanta, Raivatari, Vastrapatha, Lingakara, Kanchana, Grimunga, Girinayara, Pushpagiri, Highland of St. John, Girnal, Karnal, Killa-e-Girnar, Devagiri,* and more. For additional information on its many names, see [Girinagar: Junagadh and Mount Girnar - One of the Most Ancient and Sacred Sites of India](http://junagadhgirnar.com/18-girnar-names/) And yet, it is also known as Girnar *Hill.* Standing at 3,672 feet at the highest point of this five-peaked mountain, when we compare it to the many other options of places to study geologically, it does not stand first by any historical metric of comparing geological features on Earth. Mount Everest, by comparison, is 29,032 feet tall--nearly *eight times the elevation of Mount Girnar.* For another comparison, Mount Everest is [also known](https://education.nationalgeographic.org/resource/mount-everest) by Tibetans as Chomolungma, meaning *"Mother Goddess of the World,"* and by Nepalese as Sagarmatha, [*"Goddess of the Sky."*](https://www.montana.edu/everest/facts/naming.html) Where Girnar's list of names is nonexhaustive, this appears to be the full extent of alternative names for the tallest mountain in the world. If a rose by any other name would smell as sweet, would a mountain by many other names indicate its importance over lesser *named* geological features? Then, there is the fact that it sits alone in the plains of the Deccan Traps. With a 9 mile radius, it pales in comparison to the vast expanse of mountain chains like the Andes, which run *4,300 miles (7,000 kilometers)* along the entire western stretch of South America with an *average elevation in the range of 13,000 feet.* The Rockies, the Alps, the Himalayas. *These* are *mountains.* As described by [Cucciniello et al.<sup>1</sup>](https://www.researchgate.net/profile/Hetu-Sheth/publication/359368565_Mantle_and_crustal_contributions_to_the_Mount_Girnar_alkaline_plutonic_complex_and_the_circum-Girnar_mafic-silicic_intrusions_of_Saurashtra_northwestern_Deccan_Traps_2022/links/6237f839be72d414dad0e821/Mantle-and-crustal-contributions-to-the-Mount-Girnar-alkaline-plutonic-complex-and-the-circum-Girnar-mafic-silicic-intrusions-of-Saurashtra-northwestern-Deccan-Traps-2022.pdf), as of *2022*: >*"most of the studies relating to the plutonic complex and the silicic ring dyke are dated, whereas the circum-Girnar mafic intrusions...have been practically unstudied."* Standard metrics for ascertaining the significance of a mountain are all based on sheer size. Mountains can be arranged by their [*prominence*](https://en.wikipedia.org/wiki/List_of_mountain_peaks_by_prominence)--their elevation above the local terrain--or [by their elevation above sea level.](https://en.wikipedia.org/wiki/List_of_highest_mountains_on_Earth) Mount Everest sits atop both of these lists and Mount Girnar does not *fit in* to this method of analysis. As a result, it pales in comparison to other mountains when analyzed by basic metrics. While the mountain has received very little attention from the geological community, it has been ascribed with a long list of honorary titles. The reverence and love for Girnar has brought it to be the home to over 800 Hindu and Jain Temples. But its unique geological nature has not gone entirely unnoticed. In ["Magmatic Differentiation in Mount Girnar,"<sup>2</sup>](https://www.journals.uchicago.edu/doi/epdf/10.1086/623314) by Mathur et al. from The Journal of Geology in 1926, they explain: >*"The Girnar Hills form an imposing and characteristic land mass in the plains of Kathiawar. Considerable importance attaches to them from a religious and archaeological point of view, and the shrines on the top of the hill are visited by a large number of pilgrims every year. **Geologically, they are no less important, yet so far little information exists about the interesting varieties of rocks they contain, or the structure of the hill ranges.**"* Here, Mathur et al. compare the importance of the geological structures of Mount Girnar to its religious importance, calling the geology of Mount Girnar ***"no less important."*** # The Geology of Mount Girnar Mount Girnar's position in the heart of the [Deccan Traps](https://en.wikipedia.org/wiki/Deccan_Traps) makes it a curious anomaly. The Deccan Traps are a [large igneous province](https://en.wikipedia.org/wiki/Large_igneous_province) considered to be the result of a wide-spread eruption ~66Ma (million years ago). Notably, this coincides with the formation of the Chicxulub crater and the [K-Pg boundary layer](https://en.wikipedia.org/wiki/Cretaceous%E2%80%93Paleogene_boundary). They are a solidified flood basalt that is over 2,000 meters thick and 500,000 square kilometers. As described by Mathur et al.: >*"The quaquaversal dip in the surrounding basalt and the topographic features are possibly suggestive of a volcano, but there is little doubt that the rocks constitute a plutonic intrusion in the form of a laccolith, with a large number of differentiated types, which is probably* ***unique*** *in being the first of its kind studied in India."*  Figure 3: *[Google Earth](https://earth.google.com/) depicting Mount Girnar with surrounding basalt having a quaquaversal (directed outward from a common center towards all points of the compass) dip in its elevations.* In 1926, Mathur et al.<sup>2</sup> considered Girnar to have intruded during *"late Cretaceous, or early Eocene;"* 66 - 55 Ma. It has been established to have begun its formation process near the time of the K-Pg Boundary formation. Given a date of 65.3 ± 1.3 Ma in 1973 <sup>3</sup>, it is considered to *belong* to the Deccan Traps. Based on whole rock K/Ar ratios, Girnar has been dated with large error bars to 63.6 ± 56.2 Ma<sup>4</sup>. The geology of Saurashtra, India has two differing features from the bulk of the Deccan Traps<sup>1</sup>: 1) *Numerous plutonic complexes* dominated by gabbros and granophyres with diorite and monzonite important to Mount Girnar, and 2) *A wide range of rock types.*  Figure 4: [Saurashtra Region map](https://en.wikipedia.org/wiki/Saurashtra_%28region%29)  Figure 5: *Mount Girnar is seen as the "eye of the bird" of Saurashtra.* As shown by Mathur et al.<sup>2</sup>,where the map was updated by Cucciniello et al.<sup>1</sup>, Girnar is highly complex in its differentiation. Sections of the mountain are composed of specific materials and void of the materials of other sections. Separately, the intrusion was found to have segments of basalt, granophyre, olivine-gabbro, and diorite/monzonite:  Figure 6: *Cucciniello et al. updated map of Mathur et al.* Magmatic differentiation is the process by which chemically different igneous rocks, such as basalt and granite, can form from the same initial magma. On Girnar, the central mountain has peaks which run west to east, composed generally of diorite and monzonite. The mountain can be separated into four geological components<sup>2</sup>: 1) *The circular outer ranges of hills,* 2) *The central mountain,* 3) *Radial ridges joining the central mountain to the outer hills; and* 4) *Low plains occupying the intervening area.* The circular outer range of hills is, generally speaking, deeply escarped on the inner faces with gentler outer slopes. It is composed of *granophyre*, which is **restricted** to the outer hills, intruded through basalt.  Figure 7: *Steeply escarped granophyre intrusions with gentler slopes on outer faces.* These form a ring that is most pronounced in the South and diminishes in the East and Northeast directions of the mountain, *"but its continuity underground can be traced by veins too small to be shown on the map."* <sup>2</sup>  Figure 8: *[Topographic map of Mount Girnar](https://en-us.topographic-map.com/maps/bxn/India/)* This ring lies in a large **hexagonal** basaltic border to the mountain, as is especially apparent from the mountain's physical appearance shown above in Figure 3. This first hexagon of basalt has a ***second, smaller hexagonal slab*** of gabbro and olivine-gabbro--partly covered by alluvium and intrusions--as is visible in Figure 6. Similar to the ring of granophyre surrounding the mountain within the larger hexagonal basalt, the second hexagon of gabbro has a ring within it of basalt:  Figure 9: *Zoom in on the second hexagon overlaid with alluvium and a basalt ring.* All of which is generally centered on the inner mountain of Girnar which is composed of diorite, monzonite, and biotite<sup>1,2</sup>. The biotite is especially restricted to the periphery of the central mountain and the junction with the surrounding olivine-gabbro. The radial ridges projecting outward from the central mountain to the surrounding ring of dikes are principally composed of olivine-gabbro, except at the junctions with the central mountain where biotite is prevalent<sup>2</sup>. Their structure can be seen in Figure 3, and the topography:  Figure 10: *[A zoomed in topographical map of Mount Girnar](https://en-us.topographic-map.com/maps/bxn/India/) showing the four ridges branching out from the central mountain to the surrounding circular dikes.* They dissect the region between the central mountain and outer ring into numerous ravines where plains of basalt on their outer margins and gabbro nearer the mountain, at times overlaid with deposits of alluvium from flowing streams, are enclosed.  Figure 11: *[A view of Dattatreya Peak and the central mountain in the forefront, with the surrounding dikes and ravines visible.](https://www.gujarattourism.com/saurashtra/junagadh/girnar-hill.html)* As a result of the rich geological nature of Mount Girnar, it has been considered a unique opportunity to study magmatic differentiation. As stated by Mathur et al.<sup>2</sup>: >*"From the description of the rock types and their close relationship in the field...., it is clear that this unique assemblage can only be regarded as one petrological unit derived from a common magma."* >*"The separation of a magma into two immiscible phases in the liquid condition has been regarded as one of the possible causes of differentiation. ...It is possible that the conditions which may bring about the separation of two liquid phases in a silicate melt* ***did not exist*** *in this reservoir."* >*"The facts of the case appear to be in better accord with the scheme of crystallization differentiation suggested by Bowen."* In short, the process discussed by Bowen is one in which volatiles play an important part in the separation of the magma. As Mathur et al. state: >*"It is probable that in most granite batholiths the volatiles are distributed more or less evenly throughout the mass, whereas the actual concentration at any one place is not sufficiently high to effect the dissociation and separation of the alkali magma by the process contemplated [by Bowen]."* Evidence strongly suggests the separation process to have occurred, thus, due to the presence of volatiles and conditions capable of separating magma intrusions by crystallizations of different materials at different stages from a single source magma. Further discussed by Cucciniello et al.<sup>1</sup>, there are what appear to be radially arranged, with respect to the plutonic complex of Mount Girnar, intrusions of dikes and sills, which are referred to as *circum-Girnar intrusions:*  Figure 12: *[Cucciniello et al.](https://www.researchgate.net/profile/Hetu-Sheth/publication/359368565_Mantle_and_crustal_contributions_to_the_Mount_Girnar_alkaline_plutonic_complex_and_the_circum-Girnar_mafic-silicic_intrusions_of_Saurashtra_northwestern_Deccan_Traps_2022/links/6237f839be72d414dad0e821/Mantle-and-crustal-contributions-to-the-Mount-Girnar-alkaline-plutonic-complex-and-the-circum-Girnar-mafic-silicic-intrusions-of-Saurashtra-northwestern-Deccan-Traps-2022.pdf) map of dykes and mafic intrusions especially prevalent east of Mount Girnar's plutonic complex.* Their study shows that some of the intrusions assimilated crustal material. The central mass has **negligible assimilation** of crustal material in the genesis of the most evolved materials of the mountain, but the surrounding dykes and sill, as well as the granophyre ring, all demonstrate degrees of assimilation of crust. Thus, it has been suggested that the central region had significantly thinner ancient crust than the surroundings. Notably, they further conclude the granophyre ring to be unrelated structurally to the plutonic complex of the mountain, though this seems unlikely. This stems from both their distance away from the center, as well as the genetics of the rocks being so varied. # Ancient Dwarka While the mountain is heavily covered with temples, as well as 9,999 stairs to the highest peak, and positioned in ancient lands, the first evidence of civilization at the mountain is only from 150 CE. The Junagadh rock inscription of Rudradaman has been dated to far more recent times than the mountain may otherwise warrant. Was it unnoticeable historically? Or did it ***not even exist yet at all?*** Evidence strongly suggests that Mount Girnar [emerged in a vortex of energy due to a weapon attack on Ancient Dwarka](https://www.youtube.com/watch?v=qRriWdNTUKY); that the whole of the Deccan Traps were caused by this weapon. Indeed, that the whole Earth fractured apart and a global flood ensued. And as a result of the process, Mount Girnar was ***emitted from the center of the Earth in a whirlwind of energy.*** Today, the mountain is circumambulated yearly during the Lili Parikrama:  Figure 13: *[Girnar Parikrama Route Map](https://blog.yatradham.org/girnar-parikrama-route-map-girnar-parvat-yatra-girnar-mountain-dattatreya/).* Due to the vortex of energy in the formation of the mountain, there are distinct characteristics of [Sacred Geometry in the energy flows creating Mount Girnar](https://steemit.com/geology/@stevescully/sacred-geometry-of-mount-girnar). The presence of the hexagonal sheets of basalt and olivine-gabbro discussed above further supports the vortices involved in the formation of the mountain. Indeed, Dattatreya Peak is imprinted with the process:  Figure 14: [*Dattatreya peak in a spiral formation.*](https://youtu.be/wO4-3YR-Ayg?t=35) # Conclusion Truly, this mountain is from heaven.  Figure 15: *[Bhutanese thangka of Mount Meru and the Buddhist universe](https://en.wikipedia.org/wiki/Mount_Meru)* Additional links: [Dwarka: The Lost City of Krishna](https://steemit.com/philosophy/@stevescully/dwarka-the-lost-city-of-krishna) [The Geopolitical Impact of the Discovery of Ancient Dwarka](https://steemit.com/history/@stevescully/the-geopolitical-impact-of-the-discovery-of-ancient-dwarka) [Ancient Dwarka: Tales in the Land](https://steemit.com/science/@stevescully/ancient-dwarka-tales-in-the-land) [Ancient Dwarka: The Chicxulub Connection](https://steemit.com/science/@stevescully/ancient-dwarka-the-chicxulub-connection) References: 1. ["Mantle and Crustal Contributions to the Mount Girnar Alkaline Plutonic Complex and the Circum-Girnar Mafic-Silicic Intrusions of Saurashtra, Northwestern Deccan Traps," Cucciniello et al., Journal of Petrology, 2022, Vol. 63, No. 3, 1–30](https://www.researchgate.net/profile/Hetu-Sheth/publication/359368565_Mantle_and_crustal_contributions_to_the_Mount_Girnar_alkaline_plutonic_complex_and_the_circum-Girnar_mafic-silicic_intrusions_of_Saurashtra_northwestern_Deccan_Traps_2022/links/6237f839be72d414dad0e821/Mantle-and-crustal-contributions-to-the-Mount-Girnar-alkaline-plutonic-complex-and-the-circum-Girnar-mafic-silicic-intrusions-of-Saurashtra-northwestern-Deccan-Traps-2022.pdf) 2. ["Magmatic Differentiation in Mount Girnar," Mathur et al., The Journal of Geology, Volume XXXIV, No.4, 1926.](https://www.journals.uchicago.edu/doi/epdf/10.1086/623314) 3. [Kaneoka, I. & Haramura, H. (1973). K/Ar ages of successive lava flows from the Deccan Traps, India. Earth and Planetary Science Letters 18, 229–236.](https://www.researchgate.net/publication/248410542_KAr_ages_of_successive_lava_flows_from_the_Deccan_Traps_India) 4. [Paul et al. (1977). Geochemical and petrogenetic study of the Girnar igneous complex, Deccan volcanic province, India. Geological Society of American Bulletin 88, 227–234.](https://pubs.geoscienceworld.org/gsa/gsabulletin/article-abstract/88/2/227/202067/Geochemical-and-petrogenetic-study-of-the-Girnar) |
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| parent author | |
| parent permlink | geology |
| permlink | mount-girnar-the-catalyst |
| title | Mount Girnar: The Catalyst |
| Transaction Info | Block #67609199/Trx c24bee39ee692f4751d52b632dca50c5b67b13fa |
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"body": "# Introduction\nPositioned in the midst of the Deccan Traps, Mount Girnar rises out of the plains of Kathiawar. Considered to be an intrusion formed around the Cretaceous-Paleogene boundary, the formation is unlike any other on Earth.\n\n\nFigure 1: *View of Mount Girnar from Bhavnath in Junagadh city of Gujarat, India*\n\n# What Is In a Name?\nThe formation is known by many names. \n\nBy Jains it is known as Mount Neminath, where Lord Neminatha is said to have obtained nirvana. It is also believed to be the location where the *next* twenty-four [tirthankaras](https://en.wikipedia.org/wiki/Tirthankara) *will* obtain nirvana.\n\nGirnar comes from the root sanskrit words of [*gir*](https://www.wisdomlib.org/definition/gir), meaning *\"addressing; invoking; invocation, praise, song; a mountain\"*, and [*nar*](https://www.wisdomlib.org/definition/nar), meaning *\"a man; husband; hero; the primordial Man; a lion-hearted man.\"*\n\nIt is also known as *Girinagar*, [*giri*](https://www.wisdomlib.org/definition/giri) meaning *\"mountain; hill\"* and [*nagar*](https://www.wisdomlib.org/definition/nagar) meaning *\"city; town.\"*\n\nAdditionally the mountain is known as Revatak Parvata. [Revata](https://www.wisdomlib.org/definition/revata) means *\"a boar; a bamboo cane;* **a whirlwind\"** and [*parvata*](https://www.wisdomlib.org/definition/parvata) means *\"a mountain, hill; a rock; an artificial mountain or heap; the number 'seven', a tree, a kind of vegetable, a cloud (mountain-like).\"*\n\nAnciently it was known as *Raivatagiri* and *Ujjayantagiri*, where [*raivata*](https://www.wisdomlib.org/definition/raivata) means *\"brilliant, rich, wealthy, plentiful, splendid, beautiful,\"* and [*ujjayanta*](https://www.wisdomlib.org/definition/ujjayanta) refers to a temple/building.\n\nIts [first names](http://junagadhgirnar.com/18-girnar-names/) were Kailashgiri and Svarnagiri. *Kailasa* refers to a type of temple, and is associated with a mountain in Tibet. Kailasa is also the name of the temple *carved into a mountain* at the Ellora Caves in Maharashtra, India. [*Svarna*](https://www.wisdomlib.org/definition/svarna) means *\"gold.\"*\n\n\nFigure 2: *[Kailasa Temple](https://en.wikipedia.org/wiki/Kailasa_Temple,_Ellora), Ellora Caves, India*\n\nAdditional names attributed to Mount Girnar have been *Girinarayana, Giriraj, Urjayat, Gomanta, Raivatari, Vastrapatha, Lingakara, Kanchana, Grimunga, Girinayara, Pushpagiri, Highland of St. John, Girnal, Karnal, Killa-e-Girnar, Devagiri,* and more. For additional information on its many names, see [Girinagar: Junagadh and Mount Girnar - One of the Most Ancient and Sacred Sites of India](http://junagadhgirnar.com/18-girnar-names/)\n\nAnd yet, it is also known as Girnar *Hill.* Standing at 3,672 feet at the highest point of this five-peaked mountain, when we compare it to the many other options of places to study geologically, it does not stand first by any historical metric of comparing geological features on Earth.\n\nMount Everest, by comparison, is 29,032 feet tall--nearly *eight times the elevation of Mount Girnar.* \n\nFor another comparison, Mount Everest is [also known](https://education.nationalgeographic.org/resource/mount-everest) by Tibetans as Chomolungma, meaning *\"Mother Goddess of the World,\"* and by Nepalese as Sagarmatha, [*\"Goddess of the Sky.\"*](https://www.montana.edu/everest/facts/naming.html) Where Girnar's list of names is nonexhaustive, this appears to be the full extent of alternative names for the tallest mountain in the world. \n\nIf a rose by any other name would smell as sweet, would a mountain by many other names indicate its importance over lesser *named* geological features?\n\nThen, there is the fact that it sits alone in the plains of the Deccan Traps. With a 9 mile radius, it pales in comparison to the vast expanse of mountain chains like the Andes, which run *4,300 miles (7,000 kilometers)* along the entire western stretch of South America with an *average elevation in the range of 13,000 feet.* The Rockies, the Alps, the Himalayas. *These* are *mountains.*\n\nAs described by [Cucciniello et al.<sup>1</sup>](https://www.researchgate.net/profile/Hetu-Sheth/publication/359368565_Mantle_and_crustal_contributions_to_the_Mount_Girnar_alkaline_plutonic_complex_and_the_circum-Girnar_mafic-silicic_intrusions_of_Saurashtra_northwestern_Deccan_Traps_2022/links/6237f839be72d414dad0e821/Mantle-and-crustal-contributions-to-the-Mount-Girnar-alkaline-plutonic-complex-and-the-circum-Girnar-mafic-silicic-intrusions-of-Saurashtra-northwestern-Deccan-Traps-2022.pdf), as of *2022*: \n>*\"most of the studies relating to the plutonic complex and the silicic ring dyke are dated, whereas the circum-Girnar mafic intrusions...have been practically unstudied.\"*\n\nStandard metrics for ascertaining the significance of a mountain are all based on sheer size. Mountains can be arranged by their [*prominence*](https://en.wikipedia.org/wiki/List_of_mountain_peaks_by_prominence)--their elevation above the local terrain--or [by their elevation above sea level.](https://en.wikipedia.org/wiki/List_of_highest_mountains_on_Earth) Mount Everest sits atop both of these lists and Mount Girnar does not *fit in* to this method of analysis. As a result, it pales in comparison to other mountains when analyzed by basic metrics.\n\nWhile the mountain has received very little attention from the geological community, it has been ascribed with a long list of honorary titles. The reverence and love for Girnar has brought it to be the home to over 800 Hindu and Jain Temples.\n\nBut its unique geological nature has not gone entirely unnoticed.\n\nIn [\"Magmatic Differentiation in Mount Girnar,\"<sup>2</sup>](https://www.journals.uchicago.edu/doi/epdf/10.1086/623314) by Mathur et al. from The Journal of Geology in 1926, they explain:\n>*\"The Girnar Hills form an imposing and characteristic land mass in the plains of Kathiawar. Considerable importance attaches to them from a religious and archaeological point of view, and the shrines on the top of the hill are visited by a large number of pilgrims every year. **Geologically, they are no less important, yet so far little information exists about the interesting varieties of rocks they contain, or the structure of the hill ranges.**\"*\n\nHere, Mathur et al. compare the importance of the geological structures of Mount Girnar to its religious importance, calling the geology of Mount Girnar ***\"no less important.\"***\n\n# The Geology of Mount Girnar\nMount Girnar's position in the heart of the [Deccan Traps](https://en.wikipedia.org/wiki/Deccan_Traps) makes it a curious anomaly. The Deccan Traps are a [large igneous province](https://en.wikipedia.org/wiki/Large_igneous_province) considered to be the result of a wide-spread eruption ~66Ma (million years ago). Notably, this coincides with the formation of the Chicxulub crater and the [K-Pg boundary layer](https://en.wikipedia.org/wiki/Cretaceous%E2%80%93Paleogene_boundary). They are a solidified flood basalt that is over 2,000 meters thick and 500,000 square kilometers.\n\nAs described by Mathur et al.:\n>*\"The quaquaversal dip in the surrounding basalt and the topographic features are possibly suggestive of a volcano, but there is little doubt that the rocks constitute a plutonic intrusion in the form of a laccolith, with a large number of differentiated types, which is probably* ***unique*** *in being the first of its kind studied in India.\"*\n\n\nFigure 3: *[Google Earth](https://earth.google.com/) depicting Mount Girnar with surrounding basalt having a quaquaversal (directed outward from a common center towards all points of the compass) dip in its elevations.*\n\nIn 1926, Mathur et al.<sup>2</sup> considered Girnar to have intruded during *\"late Cretaceous, or early Eocene;\"* 66 - 55 Ma.\n\nIt has been established to have begun its formation process near the time of the K-Pg Boundary formation. Given a date of 65.3 ± 1.3 Ma in 1973 <sup>3</sup>, it is considered to *belong* to the Deccan Traps.\n\nBased on whole rock K/Ar ratios, Girnar has been dated with large error bars to 63.6 ± 56.2 Ma<sup>4</sup>.\n\nThe geology of Saurashtra, India has two differing features from the bulk of the Deccan Traps<sup>1</sup>:\n1) *Numerous plutonic complexes* dominated by gabbros and granophyres with diorite and monzonite important to Mount Girnar, and\n2) *A wide range of rock types.*\n\n\nFigure 4: [Saurashtra Region map](https://en.wikipedia.org/wiki/Saurashtra_%28region%29)\n\n\nFigure 5: *Mount Girnar is seen as the \"eye of the bird\" of Saurashtra.*\n\nAs shown by Mathur et al.<sup>2</sup>,where the map was updated by Cucciniello et al.<sup>1</sup>, Girnar is highly complex in its differentiation. Sections of the mountain are composed of specific materials and void of the materials of other sections. \n\nSeparately, the intrusion was found to have segments of basalt, granophyre, olivine-gabbro, and diorite/monzonite:\n\nFigure 6: *Cucciniello et al. updated map of Mathur et al.*\n\nMagmatic differentiation is the process by which chemically different igneous rocks, such as basalt and granite, can form from the same initial magma.\n\nOn Girnar, the central mountain has peaks which run west to east, composed generally of diorite and monzonite.\n\nThe mountain can be separated into four geological components<sup>2</sup>:\n1) *The circular outer ranges of hills,*\n2) *The central mountain,*\n3) *Radial ridges joining the central mountain to the outer hills; and*\n4) *Low plains occupying the intervening area.*\n\nThe circular outer range of hills is, generally speaking, deeply escarped on the inner faces with gentler outer slopes. It is composed of *granophyre*, which is **restricted** to the outer hills, intruded through basalt.\n\n\nFigure 7: *Steeply escarped granophyre intrusions with gentler slopes on outer faces.*\n\nThese form a ring that is most pronounced in the South and diminishes in the East and Northeast directions of the mountain, *\"but its continuity underground can be traced by veins too small to be shown on the map.\"* <sup>2</sup>\n\n\nFigure 8: *[Topographic map of Mount Girnar](https://en-us.topographic-map.com/maps/bxn/India/)*\n\nThis ring lies in a large **hexagonal** basaltic border to the mountain, as is especially apparent from the mountain's physical appearance shown above in Figure 3. This first hexagon of basalt has a ***second, smaller hexagonal slab*** of gabbro and olivine-gabbro--partly covered by alluvium and intrusions--as is visible in Figure 6.\n\nSimilar to the ring of granophyre surrounding the mountain within the larger hexagonal basalt, the second hexagon of gabbro has a ring within it of basalt:\n\n\nFigure 9: *Zoom in on the second hexagon overlaid with alluvium and a basalt ring.*\n\nAll of which is generally centered on the inner mountain of Girnar which is composed of diorite, monzonite, and biotite<sup>1,2</sup>. The biotite is especially restricted to the periphery of the central mountain and the junction with the surrounding olivine-gabbro.\n\nThe radial ridges projecting outward from the central mountain to the surrounding ring of dikes are principally composed of olivine-gabbro, except at the junctions with the central mountain where biotite is prevalent<sup>2</sup>. Their structure can be seen in Figure 3, and the topography:\n\n\nFigure 10: *[A zoomed in topographical map of Mount Girnar](https://en-us.topographic-map.com/maps/bxn/India/) showing the four ridges branching out from the central mountain to the surrounding circular dikes.*\n \nThey dissect the region between the central mountain and outer ring into numerous ravines where plains of basalt on their outer margins and gabbro nearer the mountain, at times overlaid with deposits of alluvium from flowing streams, are enclosed.\n\n\nFigure 11: *[A view of Dattatreya Peak and the central mountain in the forefront, with the surrounding dikes and ravines visible.](https://www.gujarattourism.com/saurashtra/junagadh/girnar-hill.html)*\n\n\nAs a result of the rich geological nature of Mount Girnar, it has been considered a unique opportunity to study magmatic differentiation. As stated by Mathur et al.<sup>2</sup>:\n>*\"From the description of the rock types and their close relationship in the field...., it is clear that this unique assemblage can only be regarded as one petrological unit derived from a common magma.\"*\n\n>*\"The separation of a magma into two immiscible phases in the liquid condition has been regarded as one of the possible causes of differentiation. ...It is possible that the conditions which may bring about the separation of two liquid phases in a silicate melt* ***did not exist*** *in this reservoir.\"*\n\n>*\"The facts of the case appear to be in better accord with the scheme of crystallization differentiation suggested by Bowen.\"*\n\nIn short, the process discussed by Bowen is one in which volatiles play an important part in the separation of the magma. As Mathur et al. state:\n>*\"It is probable that in most granite batholiths the volatiles are distributed more or less evenly throughout the mass, whereas the actual concentration at any one place is not sufficiently high to effect the dissociation and separation of the alkali magma by the process contemplated [by Bowen].\"*\n\nEvidence strongly suggests the separation process to have occurred, thus, due to the presence of volatiles and conditions capable of separating magma intrusions by crystallizations of different materials at different stages from a single source magma.\n\nFurther discussed by Cucciniello et al.<sup>1</sup>, there are what appear to be radially arranged, with respect to the plutonic complex of Mount Girnar, intrusions of dikes and sills, which are referred to as *circum-Girnar intrusions:*\n\n\nFigure 12: *[Cucciniello et al.](https://www.researchgate.net/profile/Hetu-Sheth/publication/359368565_Mantle_and_crustal_contributions_to_the_Mount_Girnar_alkaline_plutonic_complex_and_the_circum-Girnar_mafic-silicic_intrusions_of_Saurashtra_northwestern_Deccan_Traps_2022/links/6237f839be72d414dad0e821/Mantle-and-crustal-contributions-to-the-Mount-Girnar-alkaline-plutonic-complex-and-the-circum-Girnar-mafic-silicic-intrusions-of-Saurashtra-northwestern-Deccan-Traps-2022.pdf) map of dykes and mafic intrusions especially prevalent east of Mount Girnar's plutonic complex.*\n\nTheir study shows that some of the intrusions assimilated crustal material. The central mass has **negligible assimilation** of crustal material in the genesis of the most evolved materials of the mountain, but the surrounding dykes and sill, as well as the granophyre ring, all demonstrate degrees of assimilation of crust. Thus, it has been suggested that the central region had significantly thinner ancient crust than the surroundings.\n\nNotably, they further conclude the granophyre ring to be unrelated structurally to the plutonic complex of the mountain, though this seems unlikely. This stems from both their distance away from the center, as well as the genetics of the rocks being so varied.\n\n# Ancient Dwarka\nWhile the mountain is heavily covered with temples, as well as 9,999 stairs to the highest peak, and positioned in ancient lands, the first evidence of civilization at the mountain is only from 150 CE. The Junagadh rock inscription of Rudradaman has been dated to far more recent times than the mountain may otherwise warrant. Was it unnoticeable historically?\n\nOr did it ***not even exist yet at all?*** \n\nEvidence strongly suggests that Mount Girnar [emerged in a vortex of energy due to a weapon attack on Ancient Dwarka](https://www.youtube.com/watch?v=qRriWdNTUKY); that the whole of the Deccan Traps were caused by this weapon. Indeed, that the whole Earth fractured apart and a global flood ensued.\n\nAnd as a result of the process, Mount Girnar was ***emitted from the center of the Earth in a whirlwind of energy.***\n\nToday, the mountain is circumambulated yearly during the Lili Parikrama:\n\nFigure 13: *[Girnar Parikrama Route Map](https://blog.yatradham.org/girnar-parikrama-route-map-girnar-parvat-yatra-girnar-mountain-dattatreya/).*\n\nDue to the vortex of energy in the formation of the mountain, there are distinct characteristics of [Sacred Geometry in the energy flows creating Mount Girnar](https://steemit.com/geology/@stevescully/sacred-geometry-of-mount-girnar).\n\nThe presence of the hexagonal sheets of basalt and olivine-gabbro discussed above further supports the vortices involved in the formation of the mountain. Indeed, Dattatreya Peak is imprinted with the process:\n\n\nFigure 14: [*Dattatreya peak in a spiral formation.*](https://youtu.be/wO4-3YR-Ayg?t=35)\n\n# Conclusion\nTruly, this mountain is from heaven.\n\n\nFigure 15: *[Bhutanese thangka of Mount Meru and the Buddhist universe](https://en.wikipedia.org/wiki/Mount_Meru)*\n\n\nAdditional links:\n[Dwarka: The Lost City of Krishna](https://steemit.com/philosophy/@stevescully/dwarka-the-lost-city-of-krishna)\n[The Geopolitical Impact of the Discovery of Ancient Dwarka](https://steemit.com/history/@stevescully/the-geopolitical-impact-of-the-discovery-of-ancient-dwarka)\n[Ancient Dwarka: Tales in the Land](https://steemit.com/science/@stevescully/ancient-dwarka-tales-in-the-land)\n[Ancient Dwarka: The Chicxulub Connection](https://steemit.com/science/@stevescully/ancient-dwarka-the-chicxulub-connection)\n\nReferences:\n1. [\"Mantle and Crustal Contributions to the Mount Girnar Alkaline Plutonic Complex and the Circum-Girnar Mafic-Silicic Intrusions of Saurashtra, Northwestern Deccan Traps,\" Cucciniello et al., Journal of Petrology, 2022, Vol. 63, No. 3, 1–30](https://www.researchgate.net/profile/Hetu-Sheth/publication/359368565_Mantle_and_crustal_contributions_to_the_Mount_Girnar_alkaline_plutonic_complex_and_the_circum-Girnar_mafic-silicic_intrusions_of_Saurashtra_northwestern_Deccan_Traps_2022/links/6237f839be72d414dad0e821/Mantle-and-crustal-contributions-to-the-Mount-Girnar-alkaline-plutonic-complex-and-the-circum-Girnar-mafic-silicic-intrusions-of-Saurashtra-northwestern-Deccan-Traps-2022.pdf)\n2. [\"Magmatic Differentiation in Mount Girnar,\" Mathur et al., The Journal of Geology, Volume XXXIV, No.4, 1926.](https://www.journals.uchicago.edu/doi/epdf/10.1086/623314)\n3. [Kaneoka, I. & Haramura, H. (1973). K/Ar ages of successive lava flows from the Deccan Traps, India. Earth and Planetary Science Letters 18, 229–236.](https://www.researchgate.net/publication/248410542_KAr_ages_of_successive_lava_flows_from_the_Deccan_Traps_India)\n4. [Paul et al. (1977). Geochemical and petrogenetic study of the Girnar igneous complex, Deccan volcanic province, India. Geological Society of American Bulletin 88, 227–234.](https://pubs.geoscienceworld.org/gsa/gsabulletin/article-abstract/88/2/227/202067/Geochemical-and-petrogenetic-study-of-the-Girnar)",
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}remlaps1upvoted (16.00%) @stevescully / sacred-geometry-of-mount-girnar2022/09/10 15:12:06
remlaps1upvoted (16.00%) @stevescully / sacred-geometry-of-mount-girnar
2022/09/10 15:12:06
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}remlaps-liteupvoted (50.00%) @stevescully / sacred-geometry-of-mount-girnar2022/09/10 15:12:03
remlaps-liteupvoted (50.00%) @stevescully / sacred-geometry-of-mount-girnar
2022/09/10 15:12:03
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}remlapsupvoted (50.00%) @stevescully / sacred-geometry-of-mount-girnar2022/09/10 15:11:51
remlapsupvoted (50.00%) @stevescully / sacred-geometry-of-mount-girnar
2022/09/10 15:11:51
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}stevescullypublished a new post: sacred-geometry-of-mount-girnar2022/09/05 04:07:39
stevescullypublished a new post: sacred-geometry-of-mount-girnar
2022/09/05 04:07:39
| author | stevescully |
| body | # Sacred Geometry of Mount Girnar  [Mount Girnar](https://en.wikipedia.org/wiki/Girnar) is extremely unique, comprising many formations unlike those found elsewhere on Earth. This is because [it was formed due to a vortex of energy that imprinted the resultant sacred geometry of the process in the mountain itself.](https://www.youtube.com/watch?v=qRriWdNTUKY) From above, we can see it has a hexagonal outline:  This further is layered with a square topographical mapping of the mountain and where the whole mountain is wrapped in a circular band:  The hexagon is not limited to the outer ring, but is also a common shape for the mountain's terrain to have formed:  The Dattatreya Temple sits atop formations of hexagonal shapes as well as a section having a flat-faced wall, as pictured here:  The formation itself is part of a larger structure surrounding the peak that spirals alike to a phi spiral:   Side shot of the formation:  [Another view of the formation](https://youtu.be/L7w1ln3MW0o?t=377) shows the layering angles of the phi ratio growth of the peak in its formation:   The mountain itself is shaped like a heart:   Energy flows settled into regions representative of the sacred geometry values:  The two lakes in the top right are positioned at 1 positions, as depicted below. The lake at the 8 position is fed by an outlet flow from the mountain that exits at a 1 position. Two additional lakes are positioned along lines involving the 1 value. A last lake is positioned at the 9 value opposite to the defined hexagonal point of the mountain and where the population of the region is most localized--making it, in a sense, a 0 position. And thus the low points of the region also are where low values in the sacred geometry pattern occur:  The [Bhavnath Mahadeva Shivling](https://en.wikipedia.org/wiki/Bhavnath) on the mountain is said "to have emerged of its own divine intention."  In conclusion, Mount Girnar is amazing.  |
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"body": "# Sacred Geometry of Mount Girnar\n\n\n[Mount Girnar](https://en.wikipedia.org/wiki/Girnar) is extremely unique, comprising many formations unlike those found elsewhere on Earth. This is because [it was formed due to a vortex of energy that imprinted the resultant sacred geometry of the process in the mountain itself.](https://www.youtube.com/watch?v=qRriWdNTUKY)\n\nFrom above, we can see it has a hexagonal outline:\n\n\nThis further is layered with a square topographical mapping of the mountain and where the whole mountain is wrapped in a circular band:\n\n\nThe hexagon is not limited to the outer ring, but is also a common shape for the mountain's terrain to have formed:\n\n\nThe Dattatreya Temple sits atop formations of hexagonal shapes as well as a section having a flat-faced wall, as pictured here:\n\n\nThe formation itself is part of a larger structure surrounding the peak that spirals alike to a phi spiral:\n\n\n\n\nSide shot of the formation:\n\n\n[Another view of the formation](https://youtu.be/L7w1ln3MW0o?t=377) shows the layering angles of the phi ratio growth of the peak in its formation:\n\n\n\n\nThe mountain itself is shaped like a heart:\n\n\n\n\nEnergy flows settled into regions representative of the sacred geometry values:\n\n\nThe two lakes in the top right are positioned at 1 positions, as depicted below. The lake at the 8 position is fed by an outlet flow from the mountain that exits at a 1 position. Two additional lakes are positioned along lines involving the 1 value. A last lake is positioned at the 9 value opposite to the defined hexagonal point of the mountain and where the population of the region is most localized--making it, in a sense, a 0 position. And thus the low points of the region also are where low values in the sacred geometry pattern occur:\n\n\nThe [Bhavnath Mahadeva Shivling](https://en.wikipedia.org/wiki/Bhavnath) on the mountain is said \"to have emerged of its own divine intention.\"\n\n\nIn conclusion, Mount Girnar is amazing.\n",
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}trx-steemsent 0.001 STEEM to @stevescully- "hello, I am an automated Swapping service between TRX / STEEM -> Send 15 or more Tron to >>> TUep3qrvP4QwqHtoXJjdQ6Q7JRQdyuaJQH <<< put your steem username NO @ symbol in the memo on your trx trans..."2022/06/24 19:02:15
trx-steemsent 0.001 STEEM to @stevescully- "hello, I am an automated Swapping service between TRX / STEEM -> Send 15 or more Tron to >>> TUep3qrvP4QwqHtoXJjdQ6Q7JRQdyuaJQH <<< put your steem username NO @ symbol in the memo on your trx trans..."
2022/06/24 19:02:15
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| to | stevescully |
| Transaction Info | Block #65344706/Trx ed6727e0518050e4122395e07ae2763243d66ac2 |
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}stevescullypublished a new post: the-golden-ratio-formation-of-the-earth-s-crust2022/06/15 23:30:30
stevescullypublished a new post: the-golden-ratio-formation-of-the-earth-s-crust
2022/06/15 23:30:30
| author | stevescully |
| body | The Earth's crust formed in a golden ratio spiral. The spiral, which has its nucleus in Africa, continues outward.  Next in the spiral is South America which was cradled along the western side of the continent by Central America, which wrapped around the continent. And then it extended through North America and through Europe, Asia, Australia, and Antarctica.  The Earth used to be a single landmass, undivided. Pangaea had no oceans. Continents were fractured apart when the Earth expanded. This did not arbitrarily occur but rather did so according to the phi ratio growth pattern of the Earth. The Pacific Ocean formed at the overall weakest region in the structural integrity of the crust of the Earth--the region between North America, Australia, Antarctica, and Asia. This is because it was where the golden ratio growth of the Earth spiraled around and wrapped on itself. Boundaries are locations most susceptible to current flows. For more information, see [Ancient Dwarka: The Secrets of Mount Girnar](https://www.youtube.com/watch?v=qRriWdNTUKY) |
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| parent permlink | physics |
| permlink | the-golden-ratio-formation-of-the-earth-s-crust |
| title | The Golden Ratio Formation of the Earth's Crust |
| Transaction Info | Block #65092234/Trx fa2d6456e283acecbbbe38bd7778cf64b7011068 |
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"body": "The Earth's crust formed in a golden ratio spiral. The spiral, which has its nucleus in Africa, continues outward.\n\n\n\n\nNext in the spiral is South America which was cradled along the western side of the continent by Central America, which wrapped around the continent. And then it extended through North America and through Europe, Asia, Australia, and Antarctica.\n\n\n\n\n\nThe Earth used to be a single landmass, undivided. Pangaea had no oceans. Continents were fractured apart when the Earth expanded. This did not arbitrarily occur but rather did so according to the phi ratio growth pattern of the Earth. The Pacific Ocean formed at the overall weakest region in the structural integrity of the crust of the Earth--the region between North America, Australia, Antarctica, and Asia. This is because it was where the golden ratio growth of the Earth spiraled around and wrapped on itself. Boundaries are locations most susceptible to current flows.\n\nFor more information, see [Ancient Dwarka: The Secrets of Mount Girnar](https://www.youtube.com/watch?v=qRriWdNTUKY)",
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}exnihilo.witnesssent 0.001 STEEM to @stevescully- "By casting your witness vote on @exnihilo.witness you will passively earn and be rewarded just for voting. More information : https://steemit.com/@exnihilo.witness"2022/06/12 16:29:12
exnihilo.witnesssent 0.001 STEEM to @stevescully- "By casting your witness vote on @exnihilo.witness you will passively earn and be rewarded just for voting. More information : https://steemit.com/@exnihilo.witness"
2022/06/12 16:29:12
| amount | 0.001 STEEM |
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| memo | By casting your witness vote on @exnihilo.witness you will passively earn and be rewarded just for voting. More information : https://steemit.com/@exnihilo.witness |
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}stevescullypublished a new post: ancient-dwarka-the-secrets-of-mount-girnar2022/06/12 16:28:09
stevescullypublished a new post: ancient-dwarka-the-secrets-of-mount-girnar
2022/06/12 16:28:09
| author | stevescully |
| body | This is the most important work I've ever done, including the theory of everything. [Ancient Dwarka: The Secrets of Mount Girnar](https://youtu.be/qRriWdNTUKY) |
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| parent permlink | truth |
| permlink | ancient-dwarka-the-secrets-of-mount-girnar |
| title | Ancient Dwarka: The Secrets of Mount Girnar |
| Transaction Info | Block #64997968/Trx be0af84a758682f0889e8309978c3472a193d7d5 |
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}stevescullyreceived 4.821 SBD, 18.993 SP author reward for @stevescully / ancient-dwarka-tales-in-the-land2022/06/08 16:05:42
stevescullyreceived 4.821 SBD, 18.993 SP author reward for @stevescully / ancient-dwarka-tales-in-the-land
2022/06/08 16:05:42
| author | stevescully |
| permlink | ancient-dwarka-tales-in-the-land |
| sbd payout | 4.821 SBD |
| steem payout | 0.000 STEEM |
| vesting payout | 30928.894550 VESTS |
| Transaction Info | Block #64882897/Virtual Operation #5 |
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}stevescullypublished a new post: ancient-dwarka-the-chicxulub-connection2022/06/06 20:58:45
stevescullypublished a new post: ancient-dwarka-the-chicxulub-connection
2022/06/06 20:58:45
| author | stevescully |
| body | @@ -13617,13 +13617,178 @@ *on*** Earth +, like two dimensions of the universe having their fabrics pushing against one another where one actually is able to cross the boundary and be in the other's reality . |
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| parent author | |
| parent permlink | science |
| permlink | ancient-dwarka-the-chicxulub-connection |
| title | Ancient Dwarka: The Chicxulub Connection |
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"body": "@@ -13617,13 +13617,178 @@\n *on*** Earth\n+, like two dimensions of the universe having their fabrics pushing against one another where one actually is able to cross the boundary and be in the other's reality\n .\n",
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"title": "Ancient Dwarka: The Chicxulub Connection"
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"timestamp": "2022-06-06T20:58:45",
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}stevescullypublished a new post: ancient-dwarka-the-chicxulub-connection2022/06/06 20:56:36
stevescullypublished a new post: ancient-dwarka-the-chicxulub-connection
2022/06/06 20:56:36
| author | stevescully |
| body | @@ -12509,19 +12509,32 @@ to the -pol +location that th e South @@ -12549,16 +12549,27 @@ Anomaly + is heading ? Seems @@ -12685,16 +12685,945 @@ le%2520motion.PNG) +%0A%0AAs the South Atlantic Anomaly moves into the position of Mt. Girnar's antipode, a second smaller system is distinctly separating from the anomaly, demonstrating the mechanics of particles splitting on a different scale. %0A%0A# Mt. Girnar%0AMount Girnar is nothing short of literal Heaven on Earth. The vortex storm that was sent into Dwarka, the Gateway TO Heaven, led to an equal and opposite response FROM Heaven of the positive vortex storm that formed Mt. Girnar. The South Atlantic Anomaly is like the negative pole of a magnet, being composed of a stable vacuum particle. Mt. Girnar, on the other hand, is the positive pole--composed of dense, solid material. So much so that it is causing the Earth's magnetic poles to merge on it's position as a single unified pole opposite to the South Atlantic Anomaly's end position off the western coast of South America. %0A%0AAs a result, Mount Girnar ***is*** heaven ***on*** Earth. |
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| parent author | |
| parent permlink | science |
| permlink | ancient-dwarka-the-chicxulub-connection |
| title | Ancient Dwarka: The Chicxulub Connection |
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"body": "@@ -12509,19 +12509,32 @@\n to the \n-pol\n+location that th\n e South \n@@ -12549,16 +12549,27 @@\n Anomaly\n+ is heading\n ? Seems\n@@ -12685,16 +12685,945 @@\n le%2520motion.PNG)\n+%0A%0AAs the South Atlantic Anomaly moves into the position of Mt. Girnar's antipode, a second smaller system is distinctly separating from the anomaly, demonstrating the mechanics of particles splitting on a different scale. %0A%0A# Mt. Girnar%0AMount Girnar is nothing short of literal Heaven on Earth. The vortex storm that was sent into Dwarka, the Gateway TO Heaven, led to an equal and opposite response FROM Heaven of the positive vortex storm that formed Mt. Girnar. The South Atlantic Anomaly is like the negative pole of a magnet, being composed of a stable vacuum particle. Mt. Girnar, on the other hand, is the positive pole--composed of dense, solid material. So much so that it is causing the Earth's magnetic poles to merge on it's position as a single unified pole opposite to the South Atlantic Anomaly's end position off the western coast of South America. %0A%0AAs a result, Mount Girnar ***is*** heaven ***on*** Earth.\n",
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}stevescullypublished a new post: ancient-dwarka-the-chicxulub-connection2022/06/06 20:22:24
stevescullypublished a new post: ancient-dwarka-the-chicxulub-connection
2022/06/06 20:22:24
| author | stevescully |
| body | @@ -4180,16 +4180,394 @@ 1361s)%0A%0A +Ejecta from Chicxulub include tektites which are spherical particles having vacuum nuclei. This is further evidence of the ethereal vortex producing stable vacuum particles having shells.%0A%0A!%5BVacuum bubbles Tektites.PNG%5D(https://cdn.steemitimages.com/DQmZhBFENEeuGKjDMb6dvpQkSBwFbZVEXnEVfJenXwLJ4SR/Vacuum%2520bubbles%2520Tektites.PNG)%0A%5BSource%5D(https://youtu.be/bdOledzfaXk?t=936)%0A%0A Moreover |
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| permlink | ancient-dwarka-the-chicxulub-connection |
| title | Ancient Dwarka: The Chicxulub Connection |
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}stevescullycustom json: notify2022/06/06 19:52:42
stevescullycustom json: notify
2022/06/06 19:52:42
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| Transaction Info | Block #64830032/Trx d4c26fb413a141fd4f4a70ef9168ea0afe7cd237 |
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}stevescullypublished a new post: ancient-dwarka-the-chicxulub-connection2022/06/06 19:45:06
stevescullypublished a new post: ancient-dwarka-the-chicxulub-connection
2022/06/06 19:45:06
| author | stevescully |
| body | @@ -4724,33 +4724,44 @@ , then between N -A +orth America and Africa, as @@ -4773,16 +4773,38 @@ as N -A and SA +orth America and South America . T @@ -5406,17 +5406,28 @@ caused S -A +outh America and Ant @@ -6819,17 +6819,28 @@ etween N -A +orth America and Afr @@ -7921,17 +7921,28 @@ across N -A +orth America into As |
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| parent permlink | science |
| permlink | ancient-dwarka-the-chicxulub-connection |
| title | Ancient Dwarka: The Chicxulub Connection |
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}stevescullypublished a new post: ancient-dwarka-the-chicxulub-connection2022/06/06 19:41:51
stevescullypublished a new post: ancient-dwarka-the-chicxulub-connection
2022/06/06 19:41:51
| author | stevescully |
| body | @@ -3923,16 +3923,210 @@ rent. %0A +%0A!%5BBirkeland Current Magnetic Anomalies Chicxulub.PNG%5D(https://cdn.steemitimages.com/DQmasy1JQFHUmjkxc79hqWeawDCvPQ5W4C6K6QrD8gYNBUH/Birkeland%2520Current%2520Magnetic%2520Anomalies%2520Chicxulub.PNG)%0A%0A %5BSource%5D @@ -4587,201 +4587,8 @@ G)%0A%0A -!%5BBirkeland Current Magnetic Anomalies Chicxulub.PNG%5D(https://cdn.steemitimages.com/DQmasy1JQFHUmjkxc79hqWeawDCvPQ5W4C6K6QrD8gYNBUH/Birkeland%2520Current%2520Magnetic%2520Anomalies%2520Chicxulub.PNG)%0A%0A We c |
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| permlink | ancient-dwarka-the-chicxulub-connection |
| title | Ancient Dwarka: The Chicxulub Connection |
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}stevescullypublished a new post: ancient-dwarka-the-chicxulub-connection2022/06/06 19:35:57
stevescullypublished a new post: ancient-dwarka-the-chicxulub-connection
2022/06/06 19:35:57
| author | stevescully |
| body | @@ -2273,34 +2273,34 @@ ipodal position -t o +f Mt. Girnar to t |
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| parent author | |
| parent permlink | science |
| permlink | ancient-dwarka-the-chicxulub-connection |
| title | Ancient Dwarka: The Chicxulub Connection |
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}gruntprimeupvoted (100.00%) @stevescully / ancient-dwarka-the-chicxulub-connection2022/06/06 19:33:54
gruntprimeupvoted (100.00%) @stevescully / ancient-dwarka-the-chicxulub-connection
2022/06/06 19:33:54
| author | stevescully |
| permlink | ancient-dwarka-the-chicxulub-connection |
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}stevescullypublished a new post: ancient-dwarka-the-chicxulub-connection2022/06/06 19:33:54
stevescullypublished a new post: ancient-dwarka-the-chicxulub-connection
2022/06/06 19:33:54
| author | stevescully |
| body | @@ -2558,17 +2558,137 @@ es North -. +, which is generally associated with Mecca. %5BGolden Ratio of Earth%5D(https://www.goldennumber.net/golden-ratio-of-earth/) %0A%0AThis m |
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| parent author | |
| parent permlink | science |
| permlink | ancient-dwarka-the-chicxulub-connection |
| title | Ancient Dwarka: The Chicxulub Connection |
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}gruntupvoted (100.00%) @stevescully / ancient-dwarka-the-chicxulub-connection2022/06/06 19:33:18
gruntupvoted (100.00%) @stevescully / ancient-dwarka-the-chicxulub-connection
2022/06/06 19:33:18
| author | stevescully |
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}stevescullypublished a new post: ancient-dwarka-the-chicxulub-connection2022/06/06 19:32:51
stevescullypublished a new post: ancient-dwarka-the-chicxulub-connection
2022/06/06 19:32:51
| author | stevescully |
| body | @@ -2167,20 +2167,16 @@ e Earth -was followed @@ -2176,16 +2176,32 @@ ollowed +energy flows of sacred g @@ -2456,24 +2456,125 @@ nates.PNG)%0A%0A +These coordinates are very close to the golden ratio latitude of the Earth of 21.246 degrees North.%0A%0A This means t |
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| permlink | ancient-dwarka-the-chicxulub-connection |
| title | Ancient Dwarka: The Chicxulub Connection |
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}gruntalphaupvoted (100.00%) @stevescully / ancient-dwarka-the-chicxulub-connection2022/06/06 19:32:48
gruntalphaupvoted (100.00%) @stevescully / ancient-dwarka-the-chicxulub-connection
2022/06/06 19:32:48
| author | stevescully |
| permlink | ancient-dwarka-the-chicxulub-connection |
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}stevescullypublished a new post: ancient-dwarka-the-chicxulub-connection2022/06/06 19:28:33
stevescullypublished a new post: ancient-dwarka-the-chicxulub-connection
2022/06/06 19:28:33
| author | stevescully |
| body | For context: [Dwarka: The Lost City of Krishna](https://steemit.com/philosophy/@stevescully/dwarka-the-lost-city-of-krishna) [The Geopolitical Impact of the Discovery of Ancient Dwarka](https://steemit.com/history/@stevescully/the-geopolitical-impact-of-the-discovery-of-ancient-dwarka) [Ancient Dwarka: Tales of the Land](https://steemit.com/science/@stevescully/ancient-dwarka-tales-in-the-land) [When the Earth Expanded](https://steemit.com/science/@stevescully/when-the-earth-expanded) [When the Earth Expanded (Part 2)](https://steemit.com/science/@stevescully/when-the-earth-expanded-part-2) [When the Earth Expanded (Part 3)](https://steemit.com/science/@stevescully/when-the-earth-expanded-part-3) [Theory of Everything](https://www.cascadinguniverse.org/) # Intro Evidence shows the Earth expanded by fracturing from Eastern Mediterranean westward, along eastern North America southward, between North America and South America, to western South America where a vortex ether storm passing through the Earth from a weapon used on Dwarka was applying pressure & caused the opposite side of the Earth to explode. I know. ## Discussion This explosion caused the antipodal position of Chicxulub and the land of Central America to be, due to torque of the vortex, twisted as it broke free so as to push against South America as the lands split apart, causing mountains of NW South America and islands of the Caribbean.  Mount Girnar is at 21.53N, 70.53E:  And the location of the rupture is at ~21.53S, 70.53W, which pushed up the Andes. The ocean floor tells us South America and Africa were still conjoined and the pressure of the explosion pushed outward into what would become the Pacific Ocean.  The whole explosion of the Earth was followed sacred geometry so well that the location of Chicxulub moved from the antipodal position to Mt. Girnar to the SAME LATITUDE NORTH.  This means that the harmonic resonance of the Earth was transformed to a different energy state, alike to how levitated water is influenced by sound: [Shape oscillation of a levitated drop in an acoustic field](https://www.youtube.com/watch?v=4z4QdiqP-q8&t=60s) The Iridium Anomaly of the K-Pg boundary found related to Chicxulub matches the process, as Iridium is only found in the core of the Earth. If a vortex of ethereal energy flowed from Dwarka, through the core, and impacted Chicxulub, the energy flow could transport material. Impacts require large periods of time, but radiometric dating is known to be seasonally dependent and is therefore not a reliable method of determining absolute ages. It can only be used for relative ages in sequences of events.  [Evidence for Correlations Between Nuclear Decay Rates and Earth-Sun Distance](https://arxiv.org/pdf/0808.3283.pdf) The history of the Earth as told by our ancestors has fundamentally important and actual truths of what occurred within. Chicxulub shows many magnetic anomalies indicative of a Birkeland Current. [Source](https://www.youtube.com/watch?v=bdOledzfaXk&t=1361s) Moreover, the angle formed the fracture location, where a curiously straight line is, is ~120 degrees--that of a hexagon's corner. Mount Girnar is surrounded by a distinct hexagonal pattern, which is tied to a physical rotation of energy in a vortex.   We can look at the ocean floor crustal age to see the flow of the Earth's fracturing. The oldest ocean crust is in the Mediterranean, then between NA and Africa, as well as NA and SA. Then there is a large CIRCLE in the Pacific from the Earth's explosion.  The explosion sent shockwaves throughout the region of the Pacific in all directions, causing the Ring of Fire because of the presence of water, which has explosive expansive properties under high pressure and temperatures, in the process.  When the pressures caused SA and Antarctica to separate, they did so violently sending a shockwave of energy that pushed up mounds of material along the path and a volcanic island arc.  The explosive force directed into the direction that *would become* the Pacific Ocean was so immense that it shoved Asia and Australia apart and created the Indonesian Archipelago.  When the Archipelago blocked the westward propagating energy from passing through the channel, it reflected with such fierceness as to create the Mariana Trench.  Energy reflected was separated by its density and the more subtle energies stopped first while the denser energies traveled further, creating two distinct imprints of the energy's flow. This is alike to how gamma rays pass through material further, and how quasars are born.  While the Earth was still at its previous radius, but fracturing from eastern Mediterranean and between NA and Africa, magma began to seep from the gaping fracture in the crust, creating the Central Atlantic Magmatic Province.  As can be seen, the CAMP was limited by the Appalachians from going further westward, which were formed by the propagation of the fracturing fault line across the circumference of the Earth. The direction the energy propagated is shown by the mountains.  Water and other material began to sweep westward across the globe as it was gushing from the Earth as well. But the explosive force in the Pacific caused a collision of energies leading to mountains between.  As the Earth rotated, the waters continued to flow westward and north along the mountains. This caused a body of water to be directed across NA into Asia.  As the waters accumulated from this process, they flowed with greater force as they moved towards the outlets into newly forming ocean beds. As it swept into Asia, it pushed up a mound of material in front of it from the weight of the water, creating the Himalayas.  The mountain chain was unable to hold the force of the water and it crumbled, creating a separation between the Himalayas and eastern mountains formed with them. This spilled down into the land below, changing topography and resulting greenery of the land.  Other portions of the water went around western Himalayas and spilled down across the Middle East. At this stage, the material was more and more stripped of nutrients and becoming more purely sand.  The currents that made it through all the way to Africa without finding an ocean bed swept across the northern country, largely void of nutrients, and left behind the Sahara desert.  This was where the currents spilled out into the Atlantic Ocean, newly being formed, Cape Verde and Canary Islands were created as can be seen by the flows still imprinted into African sands.   The vortex storm traveled through India and produced the Deccan Traps by allowing cosmic energies to reach the surface and transform it. The eye of the storm physically traveled from Dwarka through the Gulf of Kunch to the Gulf of Khambhat.  As it moved, it applied a downward pressure onto the planet that then flowed outward, carving the Gulf of Kunch into the land. The eye of the storm traveled over a region of land that was solid enough to not be drilled into and, instead, left a scorched imprint of its path.  The storm created a stable void nucleus that is effectively an electron on a different scale. It's negative energy sent such magnitudes of lightning as to scar the land nearest to its travel. Until it suddenly discharged in the direction of Mt. Girnar.  The energy flowed into Mt. Girnar with such influence as to produce a distinct hexagonal corner pointing in the direction of the discharge.  This discharge caused the ocean seamount to be imprinted with the storm's band as well, leaving evidence of a phi ratio storm on Earth in the structure of the seamount chain.  This caused the void particle to be ejected away from the Earth where it now is pushing into our magnetic field, creating a depression known as the South Atlantic Anomaly.  The anomaly is moving towards the antipodal position to Mt. Girnar, while the North and South Poles of Earth are converging near India. Are they actually headed for Mt. Girnar to merge as a single pole opposite to the pole South Atlantic Anomaly? Seems likely.  |
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| parent author | |
| parent permlink | science |
| permlink | ancient-dwarka-the-chicxulub-connection |
| title | Ancient Dwarka: The Chicxulub Connection |
| Transaction Info | Block #64829552/Trx 6b3452c1004f40d69545a007ba99f762fbd36f14 |
View Raw JSON Data
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"block": 64829552,
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"author": "stevescully",
"body": "For context:\n[Dwarka: The Lost City of Krishna](https://steemit.com/philosophy/@stevescully/dwarka-the-lost-city-of-krishna)\n[The Geopolitical Impact of the Discovery of Ancient Dwarka](https://steemit.com/history/@stevescully/the-geopolitical-impact-of-the-discovery-of-ancient-dwarka)\n[Ancient Dwarka: Tales of the Land](https://steemit.com/science/@stevescully/ancient-dwarka-tales-in-the-land)\n[When the Earth Expanded](https://steemit.com/science/@stevescully/when-the-earth-expanded)\n[When the Earth Expanded (Part 2)](https://steemit.com/science/@stevescully/when-the-earth-expanded-part-2)\n[When the Earth Expanded (Part 3)](https://steemit.com/science/@stevescully/when-the-earth-expanded-part-3)\n[Theory of Everything](https://www.cascadinguniverse.org/)\n\n\n\n# Intro\nEvidence shows the Earth expanded by fracturing from Eastern Mediterranean westward, along eastern North America southward, between North America and South America, to western South America where a vortex ether storm passing through the Earth from a weapon used on Dwarka was applying pressure & caused the opposite side of the Earth to explode.\n\nI know.\n\n## Discussion\nThis explosion caused the antipodal position of Chicxulub and the land of Central America to be, due to torque of the vortex, twisted as it broke free so as to push against South America as the lands split apart, causing mountains of NW South America and islands of the Caribbean.\n\n\n\nMount Girnar is at 21.53N, 70.53E:\n\n\nAnd the location of the rupture is at ~21.53S, 70.53W, which pushed up the Andes. The ocean floor tells us South America and Africa were still conjoined and the pressure of the explosion pushed outward into what would become the Pacific Ocean. \n\n\n\nThe whole explosion of the Earth was followed sacred geometry so well that the location of Chicxulub moved from the antipodal position to Mt. Girnar to the SAME LATITUDE NORTH.\n\n\nThis means that the harmonic resonance of the Earth was transformed to a different energy state, alike to how levitated water is influenced by sound: [Shape oscillation of a levitated drop in an acoustic field](https://www.youtube.com/watch?v=4z4QdiqP-q8&t=60s)\n\nThe Iridium Anomaly of the K-Pg boundary found related to Chicxulub matches the process, as Iridium is only found in the core of the Earth. If a vortex of ethereal energy flowed from Dwarka, through the core, and impacted Chicxulub, the energy flow could transport material. \n\nImpacts require large periods of time, but radiometric dating is known to be seasonally dependent and is therefore not a reliable method of determining absolute ages. It can only be used for relative ages in sequences of events.\n\n\n[Evidence for Correlations Between Nuclear Decay Rates and Earth-Sun Distance](https://arxiv.org/pdf/0808.3283.pdf)\n\nThe history of the Earth as told by our ancestors has fundamentally important and actual truths of what occurred within. Chicxulub shows many magnetic anomalies indicative of a Birkeland Current. \n[Source](https://www.youtube.com/watch?v=bdOledzfaXk&t=1361s)\n\nMoreover, the angle formed the fracture location, where a curiously straight line is, is ~120 degrees--that of a hexagon's corner. Mount Girnar is surrounded by a distinct hexagonal pattern, which is tied to a physical rotation of energy in a vortex. \n\n\n\n\n\nWe can look at the ocean floor crustal age to see the flow of the Earth's fracturing. The oldest ocean crust is in the Mediterranean, then between NA and Africa, as well as NA and SA. Then there is a large CIRCLE in the Pacific from the Earth's explosion.\n\n\n\nThe explosion sent shockwaves throughout the region of the Pacific in all directions, causing the Ring of Fire because of the presence of water, which has explosive expansive properties under high pressure and temperatures, in the process. \n\n\n\nWhen the pressures caused SA and Antarctica to separate, they did so violently sending a shockwave of energy that pushed up mounds of material along the path and a volcanic island arc.\n\n\n\nThe explosive force directed into the direction that *would become* the Pacific Ocean was so immense that it shoved Asia and Australia apart and created the Indonesian Archipelago. \n\n\n\nWhen the Archipelago blocked the westward propagating energy from passing through the channel, it reflected with such fierceness as to create the Mariana Trench.\n\n\n\nEnergy reflected was separated by its density and the more subtle energies stopped first while the denser energies traveled further, creating two distinct imprints of the energy's flow. This is alike to how gamma rays pass through material further, and how quasars are born. \n\n\n\nWhile the Earth was still at its previous radius, but fracturing from eastern Mediterranean and between NA and Africa, magma began to seep from the gaping fracture in the crust, creating the Central Atlantic Magmatic Province.\n\n\n\nAs can be seen, the CAMP was limited by the Appalachians from going further westward, which were formed by the propagation of the fracturing fault line across the circumference of the Earth. The direction the energy propagated is shown by the mountains.\n\n\n\nWater and other material began to sweep westward across the globe as it was gushing from the Earth as well. But the explosive force in the Pacific caused a collision of energies leading to mountains between. \n\n\n\nAs the Earth rotated, the waters continued to flow westward and north along the mountains. This caused a body of water to be directed across NA into Asia.\n\n\n\nAs the waters accumulated from this process, they flowed with greater force as they moved towards the outlets into newly forming ocean beds. As it swept into Asia, it pushed up a mound of material in front of it from the weight of the water, creating the Himalayas. \n\n\n\nThe mountain chain was unable to hold the force of the water and it crumbled, creating a separation between the Himalayas and eastern mountains formed with them. This spilled down into the land below, changing topography and resulting greenery of the land.\n\n\n\nOther portions of the water went around western Himalayas and spilled down across the Middle East. At this stage, the material was more and more stripped of nutrients and becoming more purely sand.\n\n\n\nThe currents that made it through all the way to Africa without finding an ocean bed swept across the northern country, largely void of nutrients, and left behind the Sahara desert. \n\n\n\nThis was where the currents spilled out into the Atlantic Ocean, newly being formed, Cape Verde and Canary Islands were created as can be seen by the flows still imprinted into African sands.\n\n\n\n\n\nThe vortex storm traveled through India and produced the Deccan Traps by allowing cosmic energies to reach the surface and transform it. The eye of the storm physically traveled from Dwarka through the Gulf of Kunch to the Gulf of Khambhat.\n\n\n\nAs it moved, it applied a downward pressure onto the planet that then flowed outward, carving the Gulf of Kunch into the land. The eye of the storm traveled over a region of land that was solid enough to not be drilled into and, instead, left a scorched imprint of its path. \n\n\nThe storm created a stable void nucleus that is effectively an electron on a different scale. It's negative energy sent such magnitudes of lightning as to scar the land nearest to its travel. Until it suddenly discharged in the direction of Mt. Girnar.\n\n\n\nThe energy flowed into Mt. Girnar with such influence as to produce a distinct hexagonal corner pointing in the direction of the discharge. \n\n\nThis discharge caused the ocean seamount to be imprinted with the storm's band as well, leaving evidence of a phi ratio storm on Earth in the structure of the seamount chain.\n\n\n\nThis caused the void particle to be ejected away from the Earth where it now is pushing into our magnetic field, creating a depression known as the South Atlantic Anomaly.\n\n\n\nThe anomaly is moving towards the antipodal position to Mt. Girnar, while the North and South Poles of Earth are converging near India. Are they actually headed for Mt. Girnar to merge as a single pole opposite to the pole South Atlantic Anomaly? Seems likely.\n\n",
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}stevescullypublished a new post: ancient-dwarka-tales-in-the-land2022/06/02 16:00:45
stevescullypublished a new post: ancient-dwarka-tales-in-the-land
2022/06/02 16:00:45
| author | stevescully |
| body | @@ -2441,80 +2441,68 @@ t. -And, becaus +On th e +o the - Earth has this feature, it is not natural for the Earth +r hand, it may be that the Earth itself is unable to @@ -2564,12 +2564,252 @@ y. +The Earth's greatest forces rip it asunder and caused mountains, yet all were within the *dimension* of the Earth. On this scale, phi ratios could only occur by a sudden influx of focused spiraling ether from the cosmos into one location. And - yet |
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| parent author | |
| parent permlink | science |
| permlink | ancient-dwarka-tales-in-the-land |
| title | Ancient Dwarka: Tales in the Land |
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}stevescullypublished a new post: ancient-dwarka-tales-in-the-land2022/06/02 15:53:30
stevescullypublished a new post: ancient-dwarka-tales-in-the-land
2022/06/02 15:53:30
| author | stevescully |
| body | @@ -1535,16 +1535,18 @@ ting in +a linear d |
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| parent permlink | science |
| permlink | ancient-dwarka-tales-in-the-land |
| title | Ancient Dwarka: Tales in the Land |
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}ace108upvoted (13.00%) @stevescully / ancient-dwarka-tales-in-the-land2022/06/02 15:00:45
ace108upvoted (13.00%) @stevescully / ancient-dwarka-tales-in-the-land
2022/06/02 15:00:45
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}happydolphinupvoted (11.00%) @stevescully / ancient-dwarka-tales-in-the-land2022/06/02 14:58:48
happydolphinupvoted (11.00%) @stevescully / ancient-dwarka-tales-in-the-land
2022/06/02 14:58:48
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}stevescullypublished a new post: ancient-dwarka-tales-in-the-land2022/06/02 03:45:30
stevescullypublished a new post: ancient-dwarka-tales-in-the-land
2022/06/02 03:45:30
| author | stevescully |
| body | @@ -1535,17 +1535,22 @@ ting in -a +linear directi @@ -1610,25 +1610,43 @@ om a - golden ratio arc +n arc produced by spiraling energy, in @@ -1683,16 +1683,64 @@ the ends + and the whole arc has a focal point like a lens , as is @@ -2042,16 +2042,161 @@ ng flow. + Rather than a linear projection of energy, the signatures left on the Earth of a spiraling vortex would be materially different in their shape. A vort |
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| parent permlink | science |
| permlink | ancient-dwarka-tales-in-the-land |
| title | Ancient Dwarka: Tales in the Land |
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}stevescullypublished a new post: the-geopolitical-impact-of-the-discovery-of-ancient-dwarka2022/06/02 03:19:48
stevescullypublished a new post: the-geopolitical-impact-of-the-discovery-of-ancient-dwarka
2022/06/02 03:19:48
| author | stevescully |
| body | @@ -6838,8 +6838,149 @@ Dwarka. +%0A%0AFor more information, read: %5BAncient Dwarka: Tales in the Land%5D(https://steemit.com/science/@stevescully/ancient-dwarka-tales-in-the-land). |
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| permlink | the-geopolitical-impact-of-the-discovery-of-ancient-dwarka |
| title | The Geopolitical Impact of the Discovery of Ancient Dwarka |
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}stevescullypublished a new post: ancient-dwarka-tales-in-the-land2022/06/02 03:02:06
stevescullypublished a new post: ancient-dwarka-tales-in-the-land
2022/06/02 03:02:06
| author | stevescully |
| body | @@ -8130,12 +8130,535 @@ ts creation. +%0A%0AMoreover, the vortex spirals out over the land. Could the storm have transformed the region known as the Deccan Traps? Indeed, Mount Girnar is a lone mountain in the expansive terrains of the Deccan Traps.%0A%0A%0A!%5Bimage.png%5D(https://cdn.steemitimages.com/DQmYeXQJ12PDvebwdn53nYekk8baTqiC3jBqgEme5R4LeBh/image.png)%0A%5BSource%5D(http://www.mantleplumes.org/Deccan.html)%0A%0A!%5Bimage.png%5D(https://cdn.steemitimages.com/DQmcJZbGRfZ5tUfYRarbDVaBFDfjzp14aH2sq4P7YDDU5rG/image.png)%0A%5BSource%5D(https://en.wikipedia.org/wiki/Geology_of_India) |
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stevescullypublished a new post: ancient-dwarka-tales-in-the-land
2022/06/01 18:17:24
| author | stevescully |
| body | @@ -7380,17 +7380,16 @@ e.png)%0A%0A -%0A It is po |
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| title | Ancient Dwarka: Tales in the Land |
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}stevescullypublished a new post: ancient-dwarka-tales-in-the-land2022/06/01 18:09:12
stevescullypublished a new post: ancient-dwarka-tales-in-the-land
2022/06/01 18:09:12
| author | stevescully |
| body | @@ -7523,16 +7523,519 @@ ttacked. + Notably, the spiral of energy moving down the coast seems to have dissipated sufficiently to stop moving mountains in the region of Gujarat. If the storm was functionally a negative source of energy and the Earth brought forth a positive counter to the energy, it is likely it would do it in a position generally perpendicularly inland from the negative charge of the storm. The discharge of the equal and opposite positive energy would have allowed for equilibrium to be, at least in part, induced. %0A%0AIn the |
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| parent permlink | science |
| permlink | ancient-dwarka-tales-in-the-land |
| title | Ancient Dwarka: Tales in the Land |
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"body": "@@ -7523,16 +7523,519 @@\n ttacked.\n+ Notably, the spiral of energy moving down the coast seems to have dissipated sufficiently to stop moving mountains in the region of Gujarat. If the storm was functionally a negative source of energy and the Earth brought forth a positive counter to the energy, it is likely it would do it in a position generally perpendicularly inland from the negative charge of the storm. The discharge of the equal and opposite positive energy would have allowed for equilibrium to be, at least in part, induced.\n %0A%0AIn the\n",
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}stevescullypublished a new post: ancient-dwarka-tales-in-the-land2022/06/01 17:58:18
stevescullypublished a new post: ancient-dwarka-tales-in-the-land
2022/06/01 17:58:18
| author | stevescully |
| body | @@ -3435,16 +3435,325 @@ related. + In other words, if the vortex of energy focused at Dwarka were to move to the continental shelf and follow the edge of the continental shelf, it could also produce the mountain range in the Arabian Sea. This is suggestive that the nucleus of the vortex did just that and the outcome was the mountain range. %0A%0AMoreov |
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