Sedimentory rocks form in several stages, which are: weathering, errosion, sedimentation, cementation and at the end lithification.
In case of formation of metamorphic rocks, rock of any origin altered in mineralogical composition, chemical composition, or structure by heat, pressure, and movement. Nearly all such rocks are crystalline.
If any kind of rock-igneous or sedimentary- is far enough beneath the surface, the pressure can change it into a metamorphic rock. Also heat - the effects differ. It doesn't have to be ever so deeply buried, geologically, since metamorphism is usually a orogenic process in the affected sedimentary rock.
Metamorphic rock differs from Igneous rock by, Metamorphic rock forms when sedimentary and igneous rocks change under heat and pressure. Igneous rocks form as lava cools and hardens.
Clastic rocks are composed of broken pieces of older rocks that have been broken up by the process of weathering and are therefore sedimentary in nature. The "clasts" (bits of older rock) may vary in size.
The sequences of sedimentary rocks in cratons are typically thin and are relatively undeformed or gently warped. The sequences in mountain belts, meanwhile, are thick and extensively folded and faulted.
IGNEOUS refers to rocks that originate in the interior of the Earth, and include the various volcanic types and the granite group of rocks. There is a 1:1 correspondence between the granite types of rock, and the volcanic ones - it depends upon whether they have been melted or not. Granites usually have well differentiated crystals, and are hard. SEDIMENTARY rocks are those that have result from the weathering of the above igneous rocks, and in general are deposited as fine-grained sediments at sea, and this will eventually form rocks. METAMORPHIC rocks are generally formed from sedimentary rocks that have been subjected to heat and pressure. Consequently, the mineral assembly will differ from that of the sedimentary, new minerals will be formed, and shear and folding are common. The degree of metamorphism varies depending on the burial pressure and temperatures. In the extreme of melting, then granites will result if the cooling is very slow, or volcanics will form if the rock is ejected in the molten state. Marble is a curious metamorphic rock in that it may be formed from the hard bodies of tiny marine animals, but with a low degree of metamorphism, often fossils may still be recognized. At extreme metamorphism, it will become a matrix mainly of CaCO3.
Sedimentory rocks form in several stages, which are: weathering, errosion, sedimentation, cementation and at the end lithification. In case of formation of metamorphic rocks, rock of any origin altered in mineralogical composition, chemical composition, or structure by heat, pressure, and movement. Nearly all such rocks are crystalline.
If any kind of rock-igneous or sedimentary- is far enough beneath the surface, the pressure can change it into a metamorphic rock. Also heat - the effects differ. It doesn't have to be ever so deeply buried, geologically, since metamorphism is usually a orogenic process in the affected sedimentary rock.
If any kind of rock-igneous or sedimentary- is far enough beneath the surface, the pressure can change it into a metamorphic rock. Also heat - the effects differ. It doesn't have to be ever so deeply buried, geologically, since metamorphism is usually a orogenic process in the affected sedimentary rock.
If any kind of rock-igneous or sedimentary- is far enough beneath the surface, the pressure can change it into a metamorphic rock. Also heat - the effects differ. It doesn't have to be ever so deeply buried, geologically, since metamorphism is usually a orogenic process in the affected sedimentary rock.
Metamorphic rock differs from Igneous rock by, Metamorphic rock forms when sedimentary and igneous rocks change under heat and pressure. Igneous rocks form as lava cools and hardens.
Clastic rocks are composed of broken pieces of older rocks that have been broken up by the process of weathering and are therefore sedimentary in nature. The "clasts" (bits of older rock) may vary in size.
Clastic rocks are composed of broken pieces of older rocks that have been broken up by the process of weathering and are therefore sedimentary in nature. The "clasts" (bits of older rock) may vary in size.
Igneous rock is formed by magma cooling and becoming solid. Metamorphic rock is the end result of a process called metamorphism (which means "change in form"). Sedimentary rock is formed by sedimentation of material at the Earth's surface and within bodies of water.
A high metamorphic grade
All three rocked differ most importantly in how they were formed. Igneous rock is formed in volcanic environments. Heated magma exits volcanoes, cools off rapidly or slowly (which also effects the type of rock produced) and forms igneous rock. Its appearance will be without organic particles or any stratification, and its grain is typically fine. Sedimentary rock is formed in layers referred to as stratification, as moving water carries particles ranging in size as well as organic material and deposits them on the ground floor depending on the speed of the water that is travelling. Its grains can range from fine to coarse and its colors are usually reddish due to iron content. Metamorphic rock is formed from the previous two types undergoing a process of compression. The molecular structures change under the heat and pressure of metamorphosis, thereby changing the color and properties of the rock. This process can be exemplified by the existence of coal, which is organic sediment that has been subjected to a metamorphic environment. It will typically be much more dense and usually has distorted layers and darker colors due to lack of oxygen.
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