June-October 1881, Cruise of the Corwin, Part II Image 178
and thaws follow each other night and morning, cloudy and sunny days, etc. The depth of tundra, humus, vegetation and earth mineral above the ice varies from 2 feet to 8 or ten, though perhaps the average is not more than 3 or 4, judging from cross-sections, front sections, and holes that I dug. The...
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ftunivpacificdc:oai:scholarlycommons.pacific.edu:jmj-all-3179 2023-08-27T04:12:24+02:00 June-October 1881, Cruise of the Corwin, Part II Image 178 Muir, John 1881-06-01T07:52:58Z image/jpeg https://scholarlycommons.pacific.edu/jmj-all/2180 https://scholarlycommons.pacific.edu/context/jmj-all/article/3179/type/native/viewcontent/fullsize.jpg eng eng Scholarly Commons https://scholarlycommons.pacific.edu/jmj-all/2180 https://scholarlycommons.pacific.edu/context/jmj-all/article/3179/type/native/viewcontent/fullsize.jpg To view additional information on copyright and related rights of this item, such as to purchase copies of images and/or obtain permission to publish them, click here to view the Holt-Atherton Special Collections policies . All John Muir Journals John Muir journals drawings writings travel journaling naturalist text 1881 ftunivpacificdc 2023-08-07T21:03:44Z and thaws follow each other night and morning, cloudy and sunny days, etc. The depth of tundra, humus, vegetation and earth mineral above the ice varies from 2 feet to 8 or ten, though perhaps the average is not more than 3 or 4, judging from cross-sections, front sections, and holes that I dug. The ice is as hard at top as at bottom of the cliff. A curious result of the shaking up, airing, and draining of the tundra soil is seen on the face of the cliff slopes, where the tundra material being undermined it rolls down and frequently, after being well shaken, comes to rest upside down as if turned by a plow, while there can be no stagnant water held in it, as it flows freely down the ice-slope on which the soil rests. On this soil, so curiously cultivated, there https://scholarlycommons.pacific.edu/jmj-all/3179/thumbnail.jpg Text Tundra University of the Pacific: Scholarly Commons |
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University of the Pacific: Scholarly Commons |
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English |
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John Muir journals drawings writings travel journaling naturalist |
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John Muir journals drawings writings travel journaling naturalist Muir, John June-October 1881, Cruise of the Corwin, Part II Image 178 |
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John Muir journals drawings writings travel journaling naturalist |
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and thaws follow each other night and morning, cloudy and sunny days, etc. The depth of tundra, humus, vegetation and earth mineral above the ice varies from 2 feet to 8 or ten, though perhaps the average is not more than 3 or 4, judging from cross-sections, front sections, and holes that I dug. The ice is as hard at top as at bottom of the cliff. A curious result of the shaking up, airing, and draining of the tundra soil is seen on the face of the cliff slopes, where the tundra material being undermined it rolls down and frequently, after being well shaken, comes to rest upside down as if turned by a plow, while there can be no stagnant water held in it, as it flows freely down the ice-slope on which the soil rests. On this soil, so curiously cultivated, there https://scholarlycommons.pacific.edu/jmj-all/3179/thumbnail.jpg |
format |
Text |
author |
Muir, John |
author_facet |
Muir, John |
author_sort |
Muir, John |
title |
June-October 1881, Cruise of the Corwin, Part II Image 178 |
title_short |
June-October 1881, Cruise of the Corwin, Part II Image 178 |
title_full |
June-October 1881, Cruise of the Corwin, Part II Image 178 |
title_fullStr |
June-October 1881, Cruise of the Corwin, Part II Image 178 |
title_full_unstemmed |
June-October 1881, Cruise of the Corwin, Part II Image 178 |
title_sort |
june-october 1881, cruise of the corwin, part ii image 178 |
publisher |
Scholarly Commons |
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1881 |
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https://scholarlycommons.pacific.edu/jmj-all/2180 https://scholarlycommons.pacific.edu/context/jmj-all/article/3179/type/native/viewcontent/fullsize.jpg |
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Tundra |
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Tundra |
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All John Muir Journals |
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https://scholarlycommons.pacific.edu/jmj-all/2180 https://scholarlycommons.pacific.edu/context/jmj-all/article/3179/type/native/viewcontent/fullsize.jpg |
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To view additional information on copyright and related rights of this item, such as to purchase copies of images and/or obtain permission to publish them, click here to view the Holt-Atherton Special Collections policies . |
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