KARST LANDFORMS
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YouTubeTHE GEOGRAPHIA
KARST LANDFORMS
Karst is a topography formed from the dissolution of soluble rocks such as limestone, dolomite, and gypsum. It is characterized by underground drainage systems with sinkholes and caves. It has also been documented for more weathering-resistant rocks, such as quartzite, given the right conditions. Subterranean drainage may limit surface water ...
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KARST TERRAIN Karst terrain refers to a distinctive type of landscape formed primarily from the dissolution of soluble rocks such as limestone, dolomite, and gypsum. This process creates unique landforms on the surface and underground, due to chemical weathering and erosion by slightly acidic water (mainly rainwater containing dissolved carbon dioxide). FEATURES OF KARST TERRAIN 1. SURFACE FEATURES (Exokarst): • Dolines (sinkholes): Depressions formed by collapse or dissolution. • Uvalas: Large
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KARST TERRAIN Karst terrain refers to a distinctive type of landscape formed primarily from the dissolution of soluble rocks such as limestone, dolomite, and gypsum. This process creates unique landforms on the surface and underground, due to chemical weathering and erosion by slightly acidic water (mainly rainwater containing dissolved carbon dioxide). FEATURES OF KARST TERRAIN 1. SURFACE FEATURES (Exokarst): • Dolines (sinkholes): Depressions formed by collapse or dissolution. • Uvalas: Large
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KARST TERRAIN Karst terrain refers to a distinctive type of landscape formed primarily from the dissolution of soluble rocks such as limestone, dolomite, and gypsum. This process creates unique landforms on the surface and underground, due to chemical weathering and erosion by slightly acidic water (mainly rainwater containing dissolved carbon dioxide). FEATURES OF KARST TERRAIN 1. SURFACE FEATURES (Exokarst): • Dolines (sinkholes): Depressions formed by collapse or dissolution. • Uvalas: Large
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