About this document
Understanding Karst Topography by chatterjeevai is a document available to read on EtoBox.
Karst topography is formed by the dissolution of soluble bedrock like limestone by groundwater. It is characterized by features like sinkholes, caves, and underground drainage systems. For full karst topography development, the landscape requires soluble carbonate rock like limestone at or near the surface, permeable bedrock with fractures, adequate rainfall, and flowing groundwater. Mildly acidic water dissolves the bedrock along fractures and joints, enlarging them over time and creating distinctive karst
- Author
- chatterjeevai
- Language
- EN