Difference between revisions of "Karst"
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| − | [[File:Microkarst-01_ICOMOS.jpg|thumb|Microkarst]] | + | [[File:Microkarst-01_ICOMOS.jpg|thumb|Microkarst<br>Photo credit: B. Fitzner]] |
== Description == | == Description == | ||
A topographic term for the landscape and structures formed in soluble bedrock by the effects of solution weathering. Karst regions are characterized by subterranean caverns, sinkholes, and dolines. Karst typically results from the action of mildly acidic water percolating through [[limestone]], [[gypsum]], or [[dolomite]]. As the rock dissolves, it becomes more porous and underground drainage systems develop. | A topographic term for the landscape and structures formed in soluble bedrock by the effects of solution weathering. Karst regions are characterized by subterranean caverns, sinkholes, and dolines. Karst typically results from the action of mildly acidic water percolating through [[limestone]], [[gypsum]], or [[dolomite]]. As the rock dissolves, it becomes more porous and underground drainage systems develop. | ||
| − | [[File:Microkarst-02_ICOMOS.jpg|thumb|Microkarst]] | + | [[File:Microkarst-02_ICOMOS.jpg|thumb|Microkarst<br>]] |
== Synonyms and Related Terms == | == Synonyms and Related Terms == | ||
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karst (Fr., Port.); carso (Port.) | karst (Fr., Port.); carso (Port.) | ||
| − | == | + | ==Resources and Citations== |
| + | * ICOMOS-ISCS: [http://www.international.icomos.org/publications/monuments_and_sites/15/pdf/Monuments_and_Sites_15_ISCS_Glossary_Stone.pdf Illustrated glossary on stone deterioration patterns] | ||
| − | * | + | * José Delgado Rodrigues, LNEC, Submitted information, 2009. |
| − | * Wikipedia | + | * Wikipedia: Karts topography (accessed March 2010) |
[[Category:Materials database]] | [[Category:Materials database]] | ||
Latest revision as of 13:54, 21 September 2022
Description
A topographic term for the landscape and structures formed in soluble bedrock by the effects of solution weathering. Karst regions are characterized by subterranean caverns, sinkholes, and dolines. Karst typically results from the action of mildly acidic water percolating through Limestone, Gypsum, or Dolomite. As the rock dissolves, it becomes more porous and underground drainage systems develop.
Synonyms and Related Terms
karst (Fr., Port.); carso (Port.)
Resources and Citations
- ICOMOS-ISCS: Illustrated glossary on stone deterioration patterns
- José Delgado Rodrigues, LNEC, Submitted information, 2009.
- Wikipedia: Karts topography (accessed March 2010)