Weathering is the process by which rocks and minerals decay or change their shape. It is a fundamental terrestrial process that causes errosion and contributes to soil establishment.

There are two main types:

1. Physical Weathering (Mechanical Weathering): Physical Weathering includes the breaking of rocks into tinier pieces outside changing their synthetic arrangement. It usually results from material forces.

2. Chemical Weathering: Chemical Weathering includes the change of the synthetic arrangement of rocks and minerals, frequently developing new minerals and separated meanings.

Factors Influencing Weathering:

1. Climate: Temperature and storm levels influence the rate.

2. Rock Type: Different mineral and rock types weather at various rates.

3. Topography: Slope and countryside physiognomy influenced by what water and wind communicate accompanying rocks.

4. Biological Activity: Plants and microorganisms can enhance two together material and synthetic enduring.

Importance of Weathering:

1. Soil Formation: Weathering breaks rocks into more delicate pieces, donating to soil composition, which is critical for plant development.

2. Landscape Development: It shapes landforms by breaking down and redistributing rock fabrics.

3. Nutrient Cycling: Weathering releases essential vitamins from rocks into the soil, upholding environments.