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What is the difference between siliciclastic and chemical or biochemical sedimentary rocks?
Wiki User
∙ 10y ago
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.
Wiki User
∙ 10y ago
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What type of sedimentary rock is chalk clastic chemical or biochemical?
Chalk is a biochemical sedimentary rock.
What are examples of biochemical sedimentary rocks and evaporates?
Biochemical sedimentary rocks: limestone, coal, chalk. Evaporative chemical sedimentary rocks: rock salt, gypsum.
Describe the requirements for a material to be classified as a sedimentary rock?
Sedimentary rocks have three main types that reflect their origins: Detrital chemical and biochemical.
How are detrital chemical and biochemical sedimentary rocks different?
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
Are stalactites and stalagmites igneous or sedimentary?
They are chemicAL Sedimentary rock
What type of sedimentary rock is chalk clastic chemical or biochemical?
Chalk is a biochemical sedimentary rock.
What are examples of biochemical sedimentary rocks and evaporates?
Biochemical sedimentary rocks: limestone, coal, chalk. Evaporative chemical sedimentary rocks: rock salt, gypsum.
Describe the requirements for a material to be classified as a sedimentary rock?
Sedimentary rocks have three main types that reflect their origins: Detrital chemical and biochemical.
Which describes breccia?
A. a clastic sedimentary rock with angular particles B. a chemical sedimentary rock C. a biochemical sedimentary rock D. a clastic sedimentary rock with large, rounded particles answer is a
What the types of sediments that often create sedimentary rocks?
There are four types of sediments that create sedimentary rocks. The fours types of rocks are sandstone, mudrocks, biochemical and chemical.
What is the or-gin of sedimentary rocks?
weathering of preexisting rocks form clastic sedimentary rocks, Oversaturated water basins form chemical sedimentary rocks after the water evaporates and dead sea organisms settle at the bottom forming biochemical sedimentary rocks.
What are the three main types of sedimentary rock?
The three main types of sedimentary rocks are clastic, chemical and biochemical. Clastic rocks are made of minerals and rocks including quartz, mica and feldspar. Chemical rocks are created when water precipitates from ground water, lakes or the ocean. Biochemical rocks can be found in the ocean. This sedimentary rock comes from plants or living organisms which helps to build tissue.
How do biochemical sedimentary rocks form?
Chemical sedimentary rocks form from solutions (water with something in it).
What is the difference between eco-friendlly colors and chemical colors?
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.
What is the difference between detrital and chemical sedimentary rocks?
Detrital- made of sediment grains Orgains- Made of fossils Chemical- from due to chemical reactions I hope this helped you enough :)
How are detrital chemical and biochemical sedimentary rocks different?
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
What do biochemical do?
biochemical cycles connect biological, geological, and chemical aspects of the biosphere.
