How does the water cycle change the earth's surface?

In geology, there are two types of forces: external and internal. One type of external force that tries to erode soil and deposit soil in coastal areas (beaches) is rainfall (precipitation).

In areas that are filled with soil particles (alluvium), like delta areas, water droplets carry soil particles that are prone to erosion through surface runoff.

As a result, the water cycle—particularly precipitation—tends to erode soil in higher elevations and deposit it in lower elevations.

The water cycle changes the Earth's surface by influencing erosion, shaping landforms through processes like weathering and deposition, contributing to the formation of bodies of water such as rivers, lakes, and oceans, and impacting vegetation patterns and distribution.

The water cycle changes the Earth's surface through various processes such as erosion, deposition, weathering, and transportation of sediment. Water from precipitation can wear away rocks and soil through erosion, shaping the landscape over time. It can also carry sediment from one place to another, depositing it in new locations. Additionally, water can break down rocks and minerals through weathering, contributing to the formation of soil. Overall, the water cycle plays a significant role in shaping the Earth's surface through these processes.