Karst and Paleokarst
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Publication Date
January 2014
Abstract
Karst is a term used to describe the processes and products of the natural dissolution of soluble rocks, usually limestone. It produces a distinctive suite of surface geomorphological features on scales of millimeter to kilometer. Many karst landforms are intimately linked to underground drainage systems, or caves, which are an integral component of karst landscapes. Caves, and their contained sediments and precipitated minerals, form an invaluable and often dateable archive recording hydrological, climatic and landscape change.
Keywords
Cave, Dissolution, Geomorphology, Hydrology, Karren, Landform, Landscape, Limestone, Phreatic, Vadose
Document Type
Article
Identifier
SFS0057888_00001
Recommended Citation
Simms, M. J., "Karst and Paleokarst" (2014). KIP Articles. 3016.
https://digitalcommons.usf.edu/kip_articles/3016