The stages leading to the formation of a detrital sedimentary rock are weathering, erosion, transportation, deposition, compaction, and lithification. Compaction and lithification occur in the final stages of detrital sedimentary rock formation.
Detrital Sedimentary Rocks (also known as clastic sedimentary rocks) are created by the accumulation of rock and mineral fragments that have been weathered from pre-existing rocks, transported by wind, water, or ice, and then cemented together by mineral cement that precipitates from groundwater.
The Stages Leading to the Formation of a Detrital Sedimentary
Rock Weathering The first stage in the development of a detrital sedimentary rock is weathering. Weathering is the decomposition of rocks that occurs as a result of physical, chemical, or biological processes.
Erosion The second step is erosion, which occurs as a result of the transport of weathered rock particles by wind, water, or ice.
Transportation The third step is transportation. The movement of weathered rock particles by water, wind, or ice to a site where deposition can occur.
Deposition The fourth step is deposition, where weathered rock particles are deposited in layers by water, wind, or ice in a specific location.
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