Cool rocks and hot flow
The collision of India with southern Asia in the past 50 million years has produced a mountain system of great diversity and immense size, with the Himalaya, Karakoram and the Tibetan plateau being the direct result. All of the world's 8000-metre peaks lie in the Himalaya-Tibet-Karakoram mounta...
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2005
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ftnerc:oai:nora.nerc.ac.uk:7844 2023-05-15T14:05:16+02:00 Cool rocks and hot flow Parrish, Randall R 2005 text http://nora.nerc.ac.uk/id/eprint/7844/ https://nora.nerc.ac.uk/id/eprint/7844/1/471%5B1%5D.pdf http://www.bgs.ac.uk/magazine/download.html en eng British Geological Survey https://nora.nerc.ac.uk/id/eprint/7844/1/471%5B1%5D.pdf Parrish, Randall R. 2005 Cool rocks and hot flow. Earthwise. 20-21. Earth Sciences Publication - Article NonPeerReviewed 2005 ftnerc 2023-02-04T19:25:12Z The collision of India with southern Asia in the past 50 million years has produced a mountain system of great diversity and immense size, with the Himalaya, Karakoram and the Tibetan plateau being the direct result. All of the world's 8000-metre peaks lie in the Himalaya-Tibet-Karakoram mountain system, and the structure, relative timescale and dimensions of this great range have strongly evolved. It is now reasonably well established that the rise of the range caused significant changes in the Earth's climate ini the past 40 million years, culminating in extensive glaciatin in the northern hemisphere and Antarctica. Article in Journal/Newspaper Antarc* Antarctica Natural Environment Research Council: NERC Open Research Archive |
institution |
Open Polar |
collection |
Natural Environment Research Council: NERC Open Research Archive |
op_collection_id |
ftnerc |
language |
English |
topic |
Earth Sciences |
spellingShingle |
Earth Sciences Parrish, Randall R Cool rocks and hot flow |
topic_facet |
Earth Sciences |
description |
The collision of India with southern Asia in the past 50 million years has produced a mountain system of great diversity and immense size, with the Himalaya, Karakoram and the Tibetan plateau being the direct result. All of the world's 8000-metre peaks lie in the Himalaya-Tibet-Karakoram mountain system, and the structure, relative timescale and dimensions of this great range have strongly evolved. It is now reasonably well established that the rise of the range caused significant changes in the Earth's climate ini the past 40 million years, culminating in extensive glaciatin in the northern hemisphere and Antarctica. |
format |
Article in Journal/Newspaper |
author |
Parrish, Randall R |
author_facet |
Parrish, Randall R |
author_sort |
Parrish, Randall R |
title |
Cool rocks and hot flow |
title_short |
Cool rocks and hot flow |
title_full |
Cool rocks and hot flow |
title_fullStr |
Cool rocks and hot flow |
title_full_unstemmed |
Cool rocks and hot flow |
title_sort |
cool rocks and hot flow |
publisher |
British Geological Survey |
publishDate |
2005 |
url |
http://nora.nerc.ac.uk/id/eprint/7844/ https://nora.nerc.ac.uk/id/eprint/7844/1/471%5B1%5D.pdf http://www.bgs.ac.uk/magazine/download.html |
genre |
Antarc* Antarctica |
genre_facet |
Antarc* Antarctica |
op_relation |
https://nora.nerc.ac.uk/id/eprint/7844/1/471%5B1%5D.pdf Parrish, Randall R. 2005 Cool rocks and hot flow. Earthwise. 20-21. |
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1766277084222586880 |