The breakdown of rocks results in the formation of soil over many thousands of years.
diagenesis
Clastic
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.
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The chemical breakdown of rocks is called weathering. This process involves the physical and chemical breakdown of rocks into smaller pieces due to exposure to elements such as water, wind, and temperature changes.
Clastic rocks are made from fragments of pre-existing rocks.
Mechanical erosion.
Clastic sedimentary rocks form from the breakdown of larger rocks through weathering and erosion. The resulting sediments are deposited and undergo compaction and cementation to form rocks like sandstone, shale, and conglomerate.
WEATHERING and EROSION
weathering
mechanical or physical weathering
Clastic sedimentary rocks form from the breakdown and erosion of larger rocks, through processes like weathering, transportation, and deposition. These sediments are then compacted and cemented together to form rocks like sandstone, shale, and conglomerates.