Valleys
Valleys are among the most common erosional landforms created by running water. They start as small and narrow rills, which gradually develop into long and wide gullies. Over time, these gullies deepen, widen, and lengthen, eventually forming valleys. There are different types of valleys, such as:
- Gorges: Deep valleys with very steep to straight sides, often found in hard rock areas.
- Canyons: Similar to gorges but wider at the top than at the bottom, canyons are characterized by steep step-like side slopes.
Erosional Landforms (Running water)| Class 11 Geography Notes
Erosional landforms created by running water are the result of water moving across the land, carving out valleys, shaping mountains, and creating a variety of other structures through processes of erosion and deposition. These landforms show us the path water takes as it travels over and through the earth.
This article will give you a detailed guide on Erosional landforms by running water, including their formation and the unique landscapes they create.
Table of Content
- Erosional Landforms of Running Water
- Valleys
- Potholes and Plunge Pools
- Incised or Entrenched Meanders
- River Terraces
- Difference between Erosional and Depositional Landforms