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
