It will continue as long as there is an atmosphere.
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Weathering can continue indefinitely, as long as there are external forces acting upon the rocks. However, certain factors such as environmental conditions and rock composition can influence the rate of weathering. In some cases, weathering may slow down or cease temporarily if conditions change.
The disintegration of rocks is called weathering. Weathering is the process by which rocks are broken down into smaller pieces through physical, chemical, or biological means.
The breakdown of sedimentary rocks is primarily caused by weathering processes such as physical (mechanical) weathering, chemical weathering, and biological weathering. Physical weathering involves the mechanical breakdown of rocks into smaller pieces, while chemical weathering involves the breakdown of rocks through chemical reactions. Biological weathering is the breakdown of rocks by living organisms such as plants and burrowing animals.
The four main types of weathering are mechanical weathering, chemical weathering, biological weathering, and physical weathering. Mechanical weathering involves the physical breakdown of rocks, chemical weathering involves the decomposition of rocks through chemical processes, biological weathering involves the actions of living organisms on rocks, and physical weathering involves the breaking down of rocks by natural forces such as wind or water.
When rocks undergo weathering, they can form sedimentary rocks. Weathering breaks down rocks into smaller sediments, which then get compacted and cemented together to form sedimentary rocks.
The three factors that affect weathering are mechanical weathering (physical breakdown of rocks), chemical weathering (chemical changes in rocks), and biological weathering (weathering caused by living organisms).