Karst Springs: Difference between revisions
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===Introduction=== | ===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. | |||
===Microbial Inhabitants=== | ===Microbial Inhabitants=== | ||
===References=== | ===References=== |