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Clastic sediments are sediments that have particles or pieces of rock (clasts) in them. The clasts can be of igneous, metamorphic or sedimentary rock. Non-clastic sediments are made up of dissolved minerals or organic matter.
The rock cycle
clastic
It is clastic
Clastic and organic sedimentary rocks like conglomerate, coal, some limestones, and shale, are formed under pressure from overlying sediments.
Fragmentation clastic sedimentary rock is formed by the lithification of inorganic and/or organic sediments.
Non-clastic rocks are formed through chemical and organic processes. Chemical rocks like limestone are formed when minerals in water precipitate out and accumulate. Organic rocks like coal are formed from the remains of plants and animals that are buried and compacted over time. These processes occur without the transportation and deposition of sediments like in clastic rocks.
Weathering and erosion break down pre-existing rocks into sediments. Transportation of these sediments by water, wind, or ice to a new location. Deposition and compaction of the sediments to form layers, followed by cementation to create a solid clastic rock.
These rocks are called detrital or clastic.
None of the above. These terms describe sedimentary rocks. Granite is igneous.
Weathering produces rock and mineral fragments known as clastic sediments. The word clastic comes from the Greek word klastos, meaning "broken"
Weathering produces rock and mineral fragments known as clastic sediments. The word clastic comes from the Greek word klastos, meaning "broken"