Weathering: Processes and Significance
Weathering is the action of elements of weather and climate over the earth’s materials. Several processes within weathering act either individually or together to affect the earth’s materials to reduce them to a fragmental state.
Weathering: Definition
Weathering is defined as the mechanical disintegration and chemical decomposition of rocks through the actions of various elements of weather and climate. As very little or no motion of materials takes place in weathering, it is an in-situ or on-site process. Weathering processes are conditioned by many complex geological, climatic, topographic, and vegetative factors. Climate is of particular importance. Not only do weathering processes differ from climate to climate, but also the depth of the weathering mantle.
Weathering| Class 11 Geography Notes
Weathering is the process of breaking down rocks, minerals, and other materials on the Earth’s surface. It is a natural process that is caused by a variety of factors, including wind, water, ice, temperature changes, and plants and animals. Weathering can occur in a variety of different environments, from deserts to mountains to oceans. Weathering is an important process because it helps to create soil, which is essential for plant growth. It also helps to shape the Earth’s surface by breaking down rocks and creating new landforms. Weathering can also have a negative impact on human activities, such as by causing erosion and damage to buildings and infrastructure.
Table of Content
- Weathering: Processes and Significance
- Weathering: Processes
- Chemical Weathering Processes
- Physical Weathering Processes
- Biological Activity