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 :)
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.
Organic sedimentary rocks are formed from the remains of plant and animal life. Chemical sedimentary rocks are formed from the precipitation of minerals in a solution.
A sedimentary organic rock is living or was once living like a coral. Chemical is chemically made and is usually man cut.
Chemical sedimentary rocks precipitate from solution. Organic is a subsection of chemical and includes limestone and coal, detrital, or clastic, are detritus, or fragments, of other rocks (e.g., sandstone). ChaCha on!
There sedimentary igneous and metemorphic
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1) Chemical and biological sedimentary rocks are produced by chemical weathering instead of the siliciclastic sediments which are created by physical weathering. Because physical weathering is much more often than the chemical weathering there are 10 times more clastic sediments in the earth's crust than chemical and biological sediments.
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The difference between a rice crispy treat and sedimentary rock is that you can enjoy eating the treat than having to chew on some dirt and rock. Put that in your juice box and Suck It!
Different clastic sediments have different textures based on the size, shape, and sorting of the grains they are composed of. The composition of a clastic sedimentary rock will vary depending on the mineralogy of the grains present in the rock. Factors such as the source rock, transportation distance, and depositional environment can all contribute to the differences in texture and composition between clastic sedimentary rocks.