Weathering crust and karren on exposed gypsum surfaces
The evolution of gypsum bare rock surfaces is the result both of volume changes of the outer rock layer and mass wasting by dissolutional processes. Some unusual weathering processes induce an increase in the volume of the outer gypsum layer, resulting in the development of a "weathering crust&...
Main Authors: | , |
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Format: | Article |
Language: | English |
Published: |
University of South Florida Libraries
1996-01-01
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Series: | International Journal of Speleology |
Online Access: | http://ijs.speleo.it/pdf/6.53.25_Macaluso.Sauro.pdf |