Crustal assimilation happens where some tectonic plates border on each other. These generally occur at deep ocean trenches where the oceanic crust (suducting oceanic lithosphere) is being pushed under the continental crust (continental lithosphere). Water and other volatiles are driven from suducting oceanic crust causing the mantle rock to melt and the resulting magma to rise and form a continental volcanic arc. The "ring of fire" around the Pacific Ocean is a good example of this. When the suducting oceanic lithosphere melts and rises it assimilates with other rocks causing granitic type igneous bodies to form.
its moving to the right of Indian
The term "assimilate" is best defined as the process of absorbing and integrating new information, ideas, or cultural practices into one's existing framework or identity. In a social context, it often refers to individuals or groups adopting the norms, values, and behaviors of a dominant culture, which can lead to a loss of original cultural identity. Assimilation can occur voluntarily or as a result of external pressures.
Heat loss by electromagnetic radiation & by convection
The movement of crustal or lithospheric plates is a part of the theory of plate tectonics.
diffusion is occur when different concentration gradient is applied
It occurs in the intestines.
hi their people of this earth
Three mechanisms for crustal thickening are magmatic intrusion, sedimentation, and faulting.
Molten magma from the mantle rises at the top oceanic ridge, cools and solidifies, continually forming a crustal plate. Hundreds to thousands of miles from the ridge the plate moves downward into the mantle at the contact with another plate and melts. The continuous process resembling a large "conveyor belt" moves the crustal plate a few centimeters each year.
Because of the plate tectonic
Western
Through the small intestine
earthquakes and tsunamis
tectonic plates
erosion
volcanoes,earthquakes,mountains
Crustal plate movement due to convection cells occurs in the asthenosphere, which is a semi-fluid layer beneath the lithosphere. The heat-driven convection currents in the asthenosphere cause the overlying crustal plates to move and interact with each other.