4 Types of Mechanical Weathering

It is also known as physical weathering. The disintegration of rocks without any change in their chemical composition is known as mechanical weathering. Moisture, changes in temperature, frost action, and winds are the main actors of mechanical weathering. This kind of weathering usually occurs in hot deserts because of the wide ranges of temperature. There are four types of mechanical weathering:


Types of Mechanical Weathering


Block Disintegration: Rocks disintegrate because of repeated expansion (due to high temperature) and contraction (due to extremely low temperature).

Granular Disintegration: Agents of weathering reduce the rocks made of different minerals to small pieces and fragments.

Exfoliation: Sudden change in temperature may cause cracks and fissures in rocks. Weathering occurs when water percolates in these fissures. The sudden expansion and contraction of rocks result in the peeling of their outer layers or exfoliation.

Frost Action: In regions of a dry climate, the cracks in rocks get filled with water. During the night, the water freezes and expands. When this process is repeated several times, the rock eventually breaks.


YOU MAY READ

Weathering

Weathering is the gradual wearing and tearing of rocks on the surface of the Earth. The main agents of weathering are temperature, humidity, and precipitation. Read more

The Atmosphere

The blanket of air that surrounds the Earth is known as the atmosphere. It exists in several layers. The atmosphere is made of many gases and solid particles. Read more

Precipitation -Types and Causes

The water cycle includes the process of evaporation, condensation, and precipitation. The heat of the Sun evaporates the water resulting in the formation of water vapour. Read more

Our World

A large cluster or collection of stars held together by gravitational force along with gases and dust is known as a galaxy. Milky Way is the name of our galaxy. Read more

Discover more from Home of learning

Subscribe now to keep reading and get access to the full archive.

Continue reading

Scroll to Top