what is diastropism?
Answers
Answer:
Diastrophism, also called tectonism, large-scale deformation of earth's crust by natural processes, which leads to the formation of continents and ocean basins, mountain systems, plateaus, Rift valleys, and other features by mechanisms such as lithospheric plate movement (that is, plate tectonics), volcanic loading, or folding.
Diastrophism covers movement of solid (plastic) crust material, as opposed to movement of molten material which is covered by volcanism. Movement causes rock to be bent or broken. The most obvious evidence of disastrophic movement can be seen where sedimentary rocks have been bent, broken or tilted. Such non-horizontal strata provide visual proof of movement.
Diastrophic movement can be classified as two types, folding and faulting, tilted beds usually are part of a larger syncline or anticline. Diastrophic movement is often called orogenic as it is associated with mountain building.
Explanation:
the process of movement and deformation of the earth's crust that gives rise to large-scale features such as continents, ocean basins, and mountain.
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