Karst waters are subterranean watercourses that occur in karsted terrain.
In most regions, the groundwater is distributed over a large area. In principle, the groundwater flows as soon as there is a hydraulic gradient in the water-bearing layer. As a rule, however, there are no delimited veins, but rather an extensive pore space filled with groundwater.
This article or section needs to be revised. Details should be given on the talk page. Please help to improve it , and then remove this flag.
Important information is missing from this article or section. Help Wikipedia by researching and pasting it .
