What is the difference between diastrophism and volcanism?
Diastrophism covers movement of solid (plastic) crust material, as opposed to movement of molten material which is covered by volcanism.
Diastrophism covers movement of solid (plastic) crust material, as opposed to movement of molten material which is covered by volcanism.
orogenic processes involving mountain building through severe folding and affecting long and narrow belts of the earth’s crust.epeirogenic processes involving uplift or warping of large parts of the earth’s crust. earthquakes involving local relatively minor movements.
In structural geology, a fold is a stack of originally planar surfaces, such as sedimentary strata, that are bent or curved during permanent deformation. A fault is a fracture in rock where there has been movement and displacement.
Weathering is often divided into the processes of mechanical weathering and chemical weathering. Biological weathering, in which living or once-living organisms contribute to weathering, can be a part of both processes.
Weathering is the breakdown of rocks at the Earth’s surface, by the action of rainwater, extremes of temperature, and biological activity. It does not involve the removal of rock material. There are three types of weathering, physical, chemical and biological.
Weathering, mass wasting, erosion, and deposition are the main exogenic processes. All the exogenic processes are covered under a general term- denudation, which means strip off or uncovers. The elements of nature capable of doing these exogenic processes are termed geomorphic agents (or exogenic geomorphic agents).
Weathering is a process in which rocks get disintegrated into smaller particles or get decomposed at or near the surface of the Earth. For example, biological weathering. Denudation is a long term process in which the wearing and tearing of the surface of the Earth takes place.
Answer: The sea waves deposit sediments along the seashores. This results in the formation of beaches.
Endogenic processes include tectonic movements of the crust, magmatism, metamorphism, and seismic activity (seeTECTONIC MOVEMENT; MAGMATISM; and METAMORPHISM).
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 .