Article Title
Abstract
The current research on the dissolution of carbonate rocks in the Karst of Trieste indicates that the average degradation of surfaces exposed to atmospheric agents is 0.028 mm/year with an average rainfall of 1350 mm. The maximum levels (0.031 mm/year) correspond to micro-crystalline limestones, the minimum values (0.014 mm/year) to dolomites.
DOI
http://dx.doi.org/10.5038/1827-806X.16.3.6
Recommended Citation
Cucchi, Franco; Fabio Forti; and Furio Finocchiaro.
1987.
Carbonate surface solution in the classical karst.
International Journal of Speleology,
16: 125-138.
Available at:
https://digitalcommons.usf.edu/ijs/vol16/iss3/6
