what is the texture of all inorganic land derived sedimentary rocks
what is the texture of all inorganic land derived sedimentary rocks
Inorganic rock refers to a type of rock that is not derived from living organisms. These rocks are formed through geological processes such as cooling and solidification of magma or compaction and cementation of sediment particles. Examples include igneous rocks like granite and basalt, as well as sedimentary rocks like sandstone and limestone.
Rocks are classified as inorganic because they are composed of minerals and do not contain carbon-based molecules associated with living organisms. Organic materials, on the other hand, are derived from living organisms and typically consist of carbon and other elements.
Limestone or Sandstone are two examples of sedimentary rocks. Two examples of sedimentary rocks are slate (fine silt) and chalk (shell remains of sea creatures).
what is the texture of all inorganic land derived sedimentary rocks
what is the texture of all inorganic land derived sedimentary rocks
Examples of organic sedimentary rocks include coal, which forms from the accumulation and compaction of plant remains, and limestone, which can contain organic debris such as shells and coral. Organic sedimentary rocks are derived from the remains of living organisms.
Inorganic rock refers to a type of rock that is not derived from living organisms. These rocks are formed through geological processes such as cooling and solidification of magma or compaction and cementation of sediment particles. Examples include igneous rocks like granite and basalt, as well as sedimentary rocks like sandstone and limestone.
Rocks are classified as inorganic because they are composed of minerals and do not contain carbon-based molecules associated with living organisms. Organic materials, on the other hand, are derived from living organisms and typically consist of carbon and other elements.
Rocks that are categorized as sedimentary rocks include sandstone, breccia shale, limestone and selenite. Sedimentary rocks are classified by their grain size.
Limestone or Sandstone are two examples of sedimentary rocks. Two examples of sedimentary rocks are slate (fine silt) and chalk (shell remains of sea creatures).
Sedimentary rocks are not directly derived from igneous rocks. Sedimentary rocks are formed from the accumulation and cementation of sediments, such as sand, mud, and organic material, through processes like erosion, deposition, and lithification. Igneous rocks, on the other hand, are formed from the cooling and solidification of magma or lava.
Chalk and coal are examples of biochemical sedimentary rocks. Biochemical sedimentary rocks are formed from the accumulation and compression of organic remains such as shells, coral, or plant material.
Rocks formed from sand, rocks, and shells are known as sedimentary rocks. Sandstones, mudstones, and limestone are common examples of sedimentary rocks that can be formed from these materials.
Chemical
Detrital sedimentary rocks are made from weathered rocks.