Karst Springs: Difference between revisions

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===References===
===References===


=Picture references:=
Picture references:
1. International Association of Hydrogeologists
1. International Association of Hydrogeologists
http://www.iah.org/karst/karst_hydrogeology.html
http://www.iah.org/karst/karst_hydrogeology.html

Revision as of 16:19, 27 March 2010

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 references: 1. International Association of Hydrogeologists http://www.iah.org/karst/karst_hydrogeology.html