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The change from one system to another is typically called a transition or migration. It involves moving data, processes, and resources from one system to another in order to upgrade or replace the existing system.
In clastic (or detrital) sedimentary rock:Weathering of an existing body of igneous, metamorphic, or sedimentary rock by natural mechanical or chemical means.Erosion of the weathered particles by wind, water, ice, and gravity.Deposition of the particles after transportation.Compaction of the particles by the weight of overlying sediments.Cementation of the particles by mineral precipitation from surrounding fluids.
In order to get an igneous rock from a sedimentary rock, the sedimentary rock must be melted and then that melt must crystallize.
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No, it doesn't.
Lithification, burial, compaction, cementation, recrystallization, and metamorphism can change one sedimentary rock into another sedimentary rock. These processes involve the physical and chemical alteration of sediment grains through pressure, heat, and other factors.
For metamorphic rock to change into sedimentary rock, it must undergo weathering and erosion to break down its minerals into sediments. These sediments are then transported, deposited, and lithified through processes like compaction and cementation to form sedimentary rock.
The change from one system to another is typically called a transition or migration. It involves moving data, processes, and resources from one system to another in order to upgrade or replace the existing system.
Yes, rocks can skip the sedimentary stage in the rock cycle by transforming directly from one type of rock to another through processes like metamorphism or melting and solidification. This can happen when rocks are subjected to high temperatures and pressures that alter their composition and characteristics without going through the sedimentary stage of being weathered, eroded, and deposited.
Yes, rocks can change from one kind to another through processes like metamorphism (changing due to heat and pressure) or weathering (breaking down into smaller particles). The rock cycle illustrates how rocks can continuously change from one type to another in any order.
Igneous rock can become sedimentary rock through the processes of weathering, erosion, transportation, deposition, and lithification. Weathering breaks down the igneous rock into smaller particles, which are then transported by wind, water, or ice to be deposited in a new location. Over time, these particles are compacted and cemented together to form sedimentary rock.
The process of forming sedimentary rock begins with weathering and erosion of existing rocks. The eroded material is then transported by water, wind, or ice to a new location where it is deposited as sediment. Over time, the sediment undergoes compaction and cementation to form sedimentary rock.
The correct order of processes involved in sedimentary rock formation is weathering, erosion, deposition, compaction, and cementation. Weathering breaks down rock into smaller pieces, erosion moves the sediments, deposition deposits the sediments into layers, compaction squeezes the sediments together, and cementation binds the sediments into rock.
The correct order of processes for the formation of sedimentary rocks is weathering, erosion, transportation, deposition, compaction, and cementation. Weathering breaks down rocks into smaller pieces, erosion transports the sediment, deposition leads to the settling of the sediment, compaction squeezes the sediment together, and cementation binds the sediment particles together to form rock.
In clastic (or detrital) sedimentary rock:Weathering of an existing body of igneous, metamorphic, or sedimentary rock by natural mechanical or chemical means.Erosion of the weathered particles by wind, water, ice, and gravity.Deposition of the particles after transportation.Compaction of the particles by the weight of overlying sediments.Cementation of the particles by mineral precipitation from surrounding fluids.
In clastic (or detrital) sedimentary rock:Weathering of an existing body of igneous, metamorphic, or sedimentary rock by natural mechanical or chemical means.Erosion of the weathered particles by wind, water, ice, and gravity.Deposition of the particles after transportation.Compaction of the particles by the weight of overlying sediments.Cementation of the particles by mineral precipitation from surrounding fluids.
In order to get an igneous rock from a sedimentary rock, the sedimentary rock must be melted and then that melt must crystallize.