difference between clastic sediments and chemical sediments
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Clastic sedimentary layers are formed by erosion and the accumulation of small broken bits of rock. Chemical sedimentary layers and organic sedimentary layers are not the result of erosion. Chemical sedimentary layers are the accumulation of precipitates of organic material.
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Organic sedimentary rocks are made of mineral crystals. All sedimentary rocks contain weathered rock and sediment. Stalagmites and stalactites are examples of chemical sedimentary rock. Peat and coal are examples of clastic sedimentary rock.
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Clastic sedimentary layers are formed by erosion and the accumulation of small broken bits of rock. Chemical sedimentary layers and organic sedimentary layers are not the result of erosion. Chemical sedimentary layers are the accumulation of precipitates of organic material.
Clastic sedimentary layers are formed by erosion and the accumulation of small broken bits of rock. Chemical sedimentary layers and organic sedimentary layers are not the result of erosion. Chemical sedimentary layers are the accumulation of precipitates of organic material.
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