The primary cause of erosion in Chambal valley is Gully erosion, which is caused by the continuous action of running water.
Gully Erosion in Chambal Valley
- Rainwater Runoff: During heavy rains, water flows over the land surface, cutting into the loose soil.
- Formation of Small Channels: Over time, small streams or rills develop as water continues to erode the surface.
- Deepening of Gullies: With repeated erosion, these rills expand into deep gullies, removing large amounts of topsoil.
- Expansion into Ravines: As erosion continues unchecked, the gullies widen and deepen, eventually forming ravines, which are a characteristic feature of the Chambal Valley.
