The length of time that the sediments that compose the rocks are eroded causes the sediments in a conglomerate to become rounded.
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.
The protolith of metaconglomerate is a sedimentary rock called conglomerate. Conglomerate is composed of rounded gravel-sized clasts that are cemented together. Through the process of metamorphism, this sedimentary rock undergoes changes in temperature and pressure to form metaconglomerate.
Breccia is a type of sedimentary rock that is composed of angular rock fragments cemented together. It is formed through the process of sedimentation where broken pieces of pre-existing rocks are lithified and compacted into a new rock mass.
Breccia forms through the consolidation of broken rock fragments due to hydraulic fracturing, such as during landslides or faulting. Conglomerate forms by the deposition and lithification of rounded gravel-sized particles in a high-energy environment like a river or coastal shoreline.
The weathering, erosion, and deposition of the rock rhyolite could result in the compaction and cementation into sedimentary rock of different types: breccia, conglomerate, sandstone, mudstone, or shale. Which type depends on the degree of weathering and the distance from the point of origin of the original rhyolite.
If the process of cementation is volcanic you get a "tuff". If the cementation post sedimentation of rock clasts you get a sedimentary rock which may be a breccia or a conglomerate.
Conglomerate is a clastic sedimentary rock.
Pegmatite is a type of igneous rock that can have two different grain sizes of the same mineral present. This is due to the slow cooling process of the magma, allowing for the growth of large crystals (phenocrysts) within a finer-grained matrix.
They are known as Conglomerate.
A clump. Unless they have undergone compaction and cementation in a process known as lithification. Then they would be classified as a sedimentary rock, maybe conglomerate, breccia, or sandstone.
Breccia is a clastic sedimentary rock composed of various sized visible pieces of other rock, cemented together by the processes of lithification.The pieces of rock that are visible are angular fragments, meaning they have somewhat jagged edges. This means that the fragments in the breccia did not travel far before they were deposited. If they had traveled longer and further they would have become rounded, in which case the resulting sedimentary rock would have been called conglomerate.
Coarse sedimentary rocks like conglomerate and breccia are formed from the deposition and lithification of large fragments or particles such as pebbles, cobbles, or boulders. These fragments are often transported by fast-moving currents like rivers or avalanches, which deposit them in layers that later solidify into coarse sedimentary rocks through the process of compaction and cementation.
Lithification is the process by which loose sediment is transformed into solid rock through compaction and cementation. It involves the squeezing together of sediment grains and the binding of these grains by minerals dissolved in the groundwater, resulting in the formation of sedimentary rocks.
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.
The protolith of metaconglomerate is a sedimentary rock called conglomerate. Conglomerate is composed of rounded gravel-sized clasts that are cemented together. Through the process of metamorphism, this sedimentary rock undergoes changes in temperature and pressure to form metaconglomerate.
The type of sedimentary rock that forms when sediments stick together is called "clastic sedimentary rock." These rocks are created from the compaction and cementation of loose particles like sand, silt, and clay. Examples include sandstone, shale, and conglomerate.
If the process of cementation is volcanic you get a "tuff". If the cementation post sedimentation of rock clasts you get a sedimentary rock which may be a breccia or a conglomerate.