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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ftunivportsmpubl:oai:researchportal.port.ac.uk:publications/432daa2f-b403-42ba-a2d4-640833c8d785 2023-05-15T13:41:17+02:00 Cool rocks and hot flow Parrish, Randall Richardson 2005 https://researchportal.port.ac.uk/portal/en/publications/cool-rocks-and-hot-flow(432daa2f-b403-42ba-a2d4-640833c8d785).html http://core.ac.uk/download/pdf/381417.pdf eng eng info:eu-repo/semantics/restrictedAccess Parrish , R R 2005 , ' Cool rocks and hot flow ' Earthwise , vol 22 , pp. 20-21 . /dk/atira/pure/core/subjects/earthsci Earth Sciences article 2005 ftunivportsmpubl 2017-09-28T19:36:05Z 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 University of Portsmouth: Portsmouth Research Portal |
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Open Polar |
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University of Portsmouth: Portsmouth Research Portal |
op_collection_id |
ftunivportsmpubl |
language |
English |
topic |
/dk/atira/pure/core/subjects/earthsci Earth Sciences |
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/dk/atira/pure/core/subjects/earthsci Earth Sciences Parrish, Randall Richardson Cool rocks and hot flow |
topic_facet |
/dk/atira/pure/core/subjects/earthsci 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 Richardson |
author_facet |
Parrish, Randall Richardson |
author_sort |
Parrish, Randall Richardson |
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 |
publishDate |
2005 |
url |
https://researchportal.port.ac.uk/portal/en/publications/cool-rocks-and-hot-flow(432daa2f-b403-42ba-a2d4-640833c8d785).html http://core.ac.uk/download/pdf/381417.pdf |
genre |
Antarc* Antarctica |
genre_facet |
Antarc* Antarctica |
op_source |
Parrish , R R 2005 , ' Cool rocks and hot flow ' Earthwise , vol 22 , pp. 20-21 . |
op_rights |
info:eu-repo/semantics/restrictedAccess |
_version_ |
1766148620169510912 |