Plate motions produce stress in Earths crust that leads to faults, mountain building, and earthquakes.
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Compression and tension can indeed affect the thickness of the Earth's crust. Compression can thicken the crust by folding and faulting, while tension can cause stretching and thinning of the crust through processes like rifting and faulting. These tectonic forces play a significant role in shaping the Earth's crust over geological time scales.
The Earths crust is approximately 650 km deep.
The sudden vibration in the plates inside the crust causes the earths crust to rise & fall.
convection currents in the mantle provide the basic driving forces for plate motions.
mantle
The earth's crust is not stress
The movement of crustal or lithospheric plates is a part of the theory of plate tectonics. The geological theory is called plate tectonics.
Rotation and Revolution.
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Seismology is the study of the motions of the Earth's crust.
half of earths layer