Soil and permafrost in the Ross Sea region of Antarctica: stable or dynamic?

Soils in the Ross Sea Region of Antarctica generally comprise a surface desert pavement and a seasonally thawed active layer over permafrost. Most soils are formed on regolith such as glacial till or colluvium. Mean annual air temperatures range from -18°C to -24°C with low precipitation. The active...

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Bibliographic Details
Published in:Cuadernos de Investigación Geográfica
Main Authors: M. R. Balks, T. A. O’Neill
Format: Article in Journal/Newspaper
Language:English
Spanish
Published: Universidad de La Rioja 2016
Subjects:
geo
Ice
Online Access:https://doi.org/10.18172/cig.2923
https://doaj.org/article/691cbc0fa0964a4d864c7d98aabb469c