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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Bibliographic Details
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
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http://onlinelibrary.wiley.com/wol1/doi/10.1111/j.1365-2389.1977.tb02260.x/fullpdf
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Summary: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.

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