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Residual soil is the soil formed from the weathering of the bedrock.
If you are asking for the name of such soils, they are soils formed in residuum, or residual soils. Typically, the soil profile grades into a degraded bedrock called saprolite, with depth, before hiyting hard bedrock.
Short spans of geologic time
Short spans of geologic time
According to the website of the New York State Geological Survey (see related link), the majority of sedimentary bedrock in New York State was deposited in a 160 million year period in the early to middle Paleozoic era from approx. 520 to 360 million years ago.
silurian
erosion
Bedrock is formed when the molten rock of the mantle cools.
Tug Hill Plateau and St. Lawrence Lowlands
Residual soil is the soil formed from the weathering of the bedrock.
When the soil above it formed from the bedrock below.
When the molten rock of the mantle cools it is called Bedrock.
If you are asking for the name of such soils, they are soils formed in residuum, or residual soils. Typically, the soil profile grades into a degraded bedrock called saprolite, with depth, before hiyting hard bedrock.
it is formed by weathering
it is formed by weathering
it is formed by weathering
no