RIVER DEPOSITION AND LANDFORMS
River Deposition and Landforms
Welcome! This page explores river deposition—the process by which rivers deposit sediments—and the fascinating fluvial landforms that result. Whether you’re a student, educator, or enthusiast, you’ll find valuable information and an interactive quiz to test your knowledge.
What is River Deposition?
River deposition occurs when a river loses energy and drops the sediment it has been carrying. This usually happens when the river slows down, such as on the inside bends of meanders, at the base of mountains, or at the river’s mouth. Over time, these deposits form distinctive landforms.
Major Landforms Created by River Deposition
- Deltas: Formed at the mouth of a river where it meets a standing body of water, like the sea. Example: Ganges-Brahmaputra Delta.
- Floodplains: Flat areas alongside rivers, built up by sediments deposited during floods.
- Levees: Raised riverbanks formed by the deposition of heavier sediments during overbank flooding.
- Oxbow Lakes: U-shaped lakes formed when a meander is cut off from the main river.
- Alluvial Fans: Fan-shaped deposits at the base of mountains where a river spreads out and loses speed.
- Point Bars: Deposits on the inside bends of meandering rivers.

Image: Formation of meanders and oxbow lakes (Wikipedia)
Learn More
Quiz: Test Your Knowledge on River Deposition
Time Left: 10:00
Comments
Post a Comment