V.—Account of an Expedition to Greenland in the Year 1870

These holes in the ice filled with water are in no way connected with each other, and at the bottom of them we found everywhere, not only near the border, but in the most distant parts of the inland ice visited by us, a layer, some few millimetres thick, of grey powder, often conglomerated into smal...

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Published in:Geological Magazine
Main Author: Nordenskiöld, A. E.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1872
Subjects:
Online Access:http://dx.doi.org/10.1017/s0016756800465325
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0016756800465325
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spelling crcambridgeupr:10.1017/s0016756800465325 2024-09-09T19:43:17+00:00 V.—Account of an Expedition to Greenland in the Year 1870 Nordenskiöld, A. E. 1872 http://dx.doi.org/10.1017/s0016756800465325 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0016756800465325 en eng Cambridge University Press (CUP) https://www.cambridge.org/core/terms Geological Magazine volume 9, issue 98, page 355-368 ISSN 0016-7568 1469-5081 journal-article 1872 crcambridgeupr https://doi.org/10.1017/s0016756800465325 2024-06-19T04:04:35Z These holes in the ice filled with water are in no way connected with each other, and at the bottom of them we found everywhere, not only near the border, but in the most distant parts of the inland ice visited by us, a layer, some few millimetres thick, of grey powder, often conglomerated into small round balls of loose consistency. Under the microscope, the principal substance of this remarkable powder appeared to consist of white angular transparent grains. We could also observe remains of vegetable fragments; yellow, imperfectly translucent particles, with, as it appeared, evident surfaces of cleavage (felspar?); green crystals (augite) and black opaque grains, which were attracted by the magnet. The quantity of these foreign components is, however, so inconsiderable, that the whole mass may be looked upon as one homogeneous substance. Article in Journal/Newspaper Greenland Cambridge University Press Greenland Geological Magazine 9 98 355 368
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language English
description These holes in the ice filled with water are in no way connected with each other, and at the bottom of them we found everywhere, not only near the border, but in the most distant parts of the inland ice visited by us, a layer, some few millimetres thick, of grey powder, often conglomerated into small round balls of loose consistency. Under the microscope, the principal substance of this remarkable powder appeared to consist of white angular transparent grains. We could also observe remains of vegetable fragments; yellow, imperfectly translucent particles, with, as it appeared, evident surfaces of cleavage (felspar?); green crystals (augite) and black opaque grains, which were attracted by the magnet. The quantity of these foreign components is, however, so inconsiderable, that the whole mass may be looked upon as one homogeneous substance.
format Article in Journal/Newspaper
author Nordenskiöld, A. E.
spellingShingle Nordenskiöld, A. E.
V.—Account of an Expedition to Greenland in the Year 1870
author_facet Nordenskiöld, A. E.
author_sort Nordenskiöld, A. E.
title V.—Account of an Expedition to Greenland in the Year 1870
title_short V.—Account of an Expedition to Greenland in the Year 1870
title_full V.—Account of an Expedition to Greenland in the Year 1870
title_fullStr V.—Account of an Expedition to Greenland in the Year 1870
title_full_unstemmed V.—Account of an Expedition to Greenland in the Year 1870
title_sort v.—account of an expedition to greenland in the year 1870
publisher Cambridge University Press (CUP)
publishDate 1872
url http://dx.doi.org/10.1017/s0016756800465325
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0016756800465325
geographic Greenland
geographic_facet Greenland
genre Greenland
genre_facet Greenland
op_source Geological Magazine
volume 9, issue 98, page 355-368
ISSN 0016-7568 1469-5081
op_rights https://www.cambridge.org/core/terms
op_doi https://doi.org/10.1017/s0016756800465325
container_title Geological Magazine
container_volume 9
container_issue 98
container_start_page 355
op_container_end_page 368
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