Karst Springs

From MicrobeWiki, the student-edited microbiology resource
Diagram of a Karst Formation. (29)

Introduction

A Karst topography is formed when rock (often limestone) is dissolved, causing small fissures within the surface structure. This fissures channel water, leading to subsurface flow within cave-like structures. Karst springs are formed when water exits the subterranean matrix and forms surface pools.

Microbial Inhabitants

References

Picture reference: International Association of Hydrogeologists http://www.iah.org/karst/karst_hydrogeology.html