In Karst region the active erosional process of fluvial erosion is what?
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In Karst region, the active erosional process of fluvial erosion is produced by streams.
The Karst topography is characterized by dissolution of various rocks like gypsum, dolomite, and limestone. This area features underground drainage systems that have caves and sinkholes. Acidic water reacts with bedrock causing its breakdown and degradation by widening the cracks on it. This results in the formation of an underneath drainage system and enhance the karst formations that will be more erosive.
An exception to this is the Kegelkarst terrain that is more tropical in nature and does not feature strong fluvial erosion processes.
The Karst topography is characterized by dissolution of various rocks like gypsum, dolomite, and limestone. This area features underground drainage systems that have caves and sinkholes. Acidic water reacts with bedrock causing its breakdown and degradation by widening the cracks on it. This results in the formation of an underneath drainage system and enhance the karst formations that will be more erosive.
An exception to this is the Kegelkarst terrain that is more tropical in nature and does not feature strong fluvial erosion processes.
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