Karst Springs: Difference between revisions
From MicrobeWiki, the student-edited microbiology resource
| Line 8: | Line 8: | ||
===References=== | ===References=== | ||
Picture | =Picture references:= | ||
1. International Association of Hydrogeologists | |||
http://www.iah.org/karst/karst_hydrogeology.html | http://www.iah.org/karst/karst_hydrogeology.html | ||
Revision as of 16:18, 27 March 2010
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 references:
1. International Association of Hydrogeologists http://www.iah.org/karst/karst_hydrogeology.html
