RENDZINA FORMATION ON BATHURST ISLAND1 1
Summary The identification of a Rendzina soil on Bathurst Island at 75° G45′ N, 99°30′ W, is believed to mark its northernmost known occurrence. The Rendzina soil is quite shallow, usually no more than 5 to 10 cm on for‐like limestone structures, but on the debris apron surrounding the base of the t...
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1977
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Online Access: | http://dx.doi.org/10.1111/j.1365-2389.1977.tb02260.x https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1365-2389.1977.tb02260.x http://onlinelibrary.wiley.com/wol1/doi/10.1111/j.1365-2389.1977.tb02260.x/fullpdf |
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crwiley:10.1111/j.1365-2389.1977.tb02260.x 2024-06-02T08:04:13+00:00 RENDZINA FORMATION ON BATHURST ISLAND1 1 TEDROW, J. C. F. WALTON, G. F. 1977 http://dx.doi.org/10.1111/j.1365-2389.1977.tb02260.x https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1365-2389.1977.tb02260.x http://onlinelibrary.wiley.com/wol1/doi/10.1111/j.1365-2389.1977.tb02260.x/fullpdf en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Journal of Soil Science volume 28, issue 3, page 519-525 ISSN 0022-4588 journal-article 1977 crwiley https://doi.org/10.1111/j.1365-2389.1977.tb02260.x 2024-05-03T11:22:12Z Summary The identification of a Rendzina soil on Bathurst Island at 75° G45′ N, 99°30′ W, is believed to mark its northernmost known occurrence. The Rendzina soil is quite shallow, usually no more than 5 to 10 cm on for‐like limestone structures, but on the debris apron surrounding the base of the tor, the soil may be as much as 30 cm or more in depth. Article in Journal/Newspaper Bathurst Island Wiley Online Library Bathurst Island ENVELOPE(-100.002,-100.002,75.752,75.752) Journal of Soil Science 28 3 519 525 |
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Open Polar |
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Wiley Online Library |
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crwiley |
language |
English |
description |
Summary The identification of a Rendzina soil on Bathurst Island at 75° G45′ N, 99°30′ W, is believed to mark its northernmost known occurrence. The Rendzina soil is quite shallow, usually no more than 5 to 10 cm on for‐like limestone structures, but on the debris apron surrounding the base of the tor, the soil may be as much as 30 cm or more in depth. |
format |
Article in Journal/Newspaper |
author |
TEDROW, J. C. F. WALTON, G. F. |
spellingShingle |
TEDROW, J. C. F. WALTON, G. F. RENDZINA FORMATION ON BATHURST ISLAND1 1 |
author_facet |
TEDROW, J. C. F. WALTON, G. F. |
author_sort |
TEDROW, J. C. F. |
title |
RENDZINA FORMATION ON BATHURST ISLAND1 1 |
title_short |
RENDZINA FORMATION ON BATHURST ISLAND1 1 |
title_full |
RENDZINA FORMATION ON BATHURST ISLAND1 1 |
title_fullStr |
RENDZINA FORMATION ON BATHURST ISLAND1 1 |
title_full_unstemmed |
RENDZINA FORMATION ON BATHURST ISLAND1 1 |
title_sort |
rendzina formation on bathurst island1 1 |
publisher |
Wiley |
publishDate |
1977 |
url |
http://dx.doi.org/10.1111/j.1365-2389.1977.tb02260.x https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1365-2389.1977.tb02260.x http://onlinelibrary.wiley.com/wol1/doi/10.1111/j.1365-2389.1977.tb02260.x/fullpdf |
long_lat |
ENVELOPE(-100.002,-100.002,75.752,75.752) |
geographic |
Bathurst Island |
geographic_facet |
Bathurst Island |
genre |
Bathurst Island |
genre_facet |
Bathurst Island |
op_source |
Journal of Soil Science volume 28, issue 3, page 519-525 ISSN 0022-4588 |
op_rights |
http://onlinelibrary.wiley.com/termsAndConditions#vor |
op_doi |
https://doi.org/10.1111/j.1365-2389.1977.tb02260.x |
container_title |
Journal of Soil Science |
container_volume |
28 |
container_issue |
3 |
container_start_page |
519 |
op_container_end_page |
525 |
_version_ |
1800748841201303552 |