Abstract
Detailed explanation of hydrogeological characteristics of gypsum aquifers is given in various situations: deep-seated karst-confined conditions, subjacent, entrenched and denuded karst types-semi-confined, phreatic and vadose conditions. The hydrogeological evolution of barren exposed gypsum karst and flow velocities in gypsum karst aquifers is also discussed.
DOI
http://dx.doi.org/10.5038/1827-806X.25.3.6
Recommended Citation
Klimchouk, Alexander.
1996.
Hydrogeology of gypsum formations.
International Journal of Speleology,
25: 83-89.
Available at:
https://digitalcommons.usf.edu/ijs/vol25/iss3/6
