Shale is a detrital rock, meaning it is composed of fragments of other rocks and minerals. It forms from the compaction and cementation of silt and clay particles. There are organic-rich shales as well, but they are still considered detrital in nature.
Sedimentary rocks form through different processes: Detrital (Clastic) Rocks: Formed from the accumulation of fragments of pre-existing rocks, which are compacted and cemented together, like sandstone. Chemical Rocks: Formed from the precipitation of minerals from water, often due to evaporation, such as limestone. Organic Rocks: Formed from the accumulation of plant or animal debris, like coal, which originates from decomposed organic material. Examples include sandstone (detrital), limestone (chemical), and coal (organic).
The two main types of sedimentary rocks are clastic (detrital) rocks, which are made of pre-existing rock fragments cemented together, and chemical rocks, which form from minerals that precipitate out of solution.
The main sub-categories of sedimentary rocks are clastic, chemical, and organic. Clastic sedimentary rocks form from the accumulation and cementation of fragments of pre-existing rocks. Chemical sedimentary rocks form from the precipitation of minerals from water solutions. Organic sedimentary rocks form from the accumulation and compression of organic materials, such as plant or animal remains.
Sedimentary rocks are classified as either clastic (composed of fragments of pre-existing rocks), chemical (formed from mineral precipitation), or organic (derived from the remains of plants and animals). These classifications help to understand how the rock was formed and its origin.
Detrital, Chemical, and Organic.
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Shale is a detrital rock, meaning it is composed of fragments of other rocks and minerals. It forms from the compaction and cementation of silt and clay particles. There are organic-rich shales as well, but they are still considered detrital in nature.
Detrital rocks are composed of rock particles, chemical sedimentary rocks are composed of precipitated minerals.Examples:Detrital or clastic rocks:ConglomerateBrecciaSandstoneShaleChemical sedimentary rocks:Rock saltSome limestonesRock gypsumWhat_is_the_difference_between_detrital_and_chemical_sedimentary_rock
Sedimentary rocks form through different processes: Detrital (Clastic) Rocks: Formed from the accumulation of fragments of pre-existing rocks, which are compacted and cemented together, like sandstone. Chemical Rocks: Formed from the precipitation of minerals from water, often due to evaporation, such as limestone. Organic Rocks: Formed from the accumulation of plant or animal debris, like coal, which originates from decomposed organic material. Examples include sandstone (detrital), limestone (chemical), and coal (organic).
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The two main types of sedimentary rocks are clastic (detrital) rocks, which are made of pre-existing rock fragments cemented together, and chemical rocks, which form from minerals that precipitate out of solution.
Detrital- made of sediment grains Orgains- Made of fossils Chemical- from due to chemical reactions I hope this helped you enough :)
Detrital- made of sediment grains Orgains- Made of fossils Chemical- from due to chemical reactions I hope this helped you enough :)
They are rocks formed from pieces of pre-existing rocks or organic debris.
It can be. Some limestone is formed from the precipitation of calcite from saturated solutions, and is considered a chemical sedimentary rock. Other limestone that consists largely of the skeletal remains of marine organisms is considered bio-clastic, a cross between an organic and a detrital sedimentary rock. Typical detrital sedimentary rocks are those composed mostly of particles of pre-existing rock, although organic matter may be included; examples would be sandstone, shale, and conglomerate.
Lithic greywacke comprises more lithic fragments and feldspathic greywacke contains more feldspar