Permafrost properties, patterns and processes in the Transantarctic Mountains region

Iain B. Campbell and Graeme G. C. Claridge

Permafrost and Periglacial Processes, 2006, vol. 17, issue 3, 215-232

Abstract: The properties, distribution patterns and thermal processes that influence the active layer and permafrost in the Transantarctic Mountains region of Antarctica, as deduced from our soil investigations since 1964 and drilling investigations since 1990, are outlined. The active layer depth varies from around 80 cm thick in coastal areas to

Date: 2006
References: Add references at CitEc
Citations:

Downloads: (external link)
https://doi.org/10.1002/ppp.557

Related works:
This item may be available elsewhere in EconPapers: Search for items with the same title.

Export reference: BibTeX RIS (EndNote, ProCite, RefMan) HTML/Text

Persistent link: https://EconPapers.repec.org/RePEc:wly:perpro:v:17:y:2006:i:3:p:215-232

Access Statistics for this article

More articles in Permafrost and Periglacial Processes from John Wiley & Sons
Bibliographic data for series maintained by Wiley Content Delivery ().