Karst Springs

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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. 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