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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Published in:Journal of Soil Science
Main Authors: TEDROW, J. C. F., WALTON, G. F.
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 1977
Subjects:
Bathurst Island
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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spelling 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
institution Open Polar
collection Wiley Online Library
op_collection_id 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
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