The rock cycle
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In the lithification process, compaction is followed by cementation. It is the hardening and welding of clastic sediments by the precipitation of mineral matter.
Yes, sediment transport is a crucial process in the formation of clastic rocks. Clastic rocks are formed from the accumulation and lithification of sediments, which are typically derived from the weathering and erosion of pre-existing rocks. These sediments are transported by natural agents such as water, wind, or ice before being deposited in various environments, where they compact and cement over time to form clastic rock types, such as sandstone and shale.
Clastic and organic sedimentary rocks like conglomerate, coal, some limestones, and shale, are formed under pressure from overlying sediments.
No because Conglomerate is made by sediments that are eroded by other rock or by dead plants and animals. The sediments are pushed or smooshed together by the pressuer sitting on top of it. This process is called compacton. This process turns the sediments into clasti sedimentry rocks. So Conglomerate is a clastic sedimantary rock.
Fragmentation clastic sedimentary rock is formed by the lithification of inorganic and/or organic sediments.
Marble is neither clastic nor detrital; it is a metamorphic rock. It forms from the recrystallization of limestone or dolostone under heat and pressure. Clastic rocks are composed of fragments of other rocks, while detrital refers to sediments that are transported and deposited, which does not apply to marble's formation process.
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.
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"
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.