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
Heat loss by electromagnetic radiation & by convection
diffusion is occur when different concentration gradient is applied
The movement of crustal or lithospheric plates is a part of the theory of plate tectonics.
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It occurs in the intestines.
hi their people of this earth
Three mechanisms for crustal thickening are magmatic intrusion, sedimentation, and faulting.
Crustal plates have moved over time due to the process of plate tectonics. The plates interact at their boundaries, where they can move apart (divergent boundary), come together (convergent boundary), or slide past each other (transform boundary). These interactions create various geological features like mountains, volcanoes, and earthquakes as the plates shift and grind against each other.
Because of the plate tectonic
Western
Through the small intestine
tectonic plates
earthquakes and tsunamis
erosion
volcanoes,earthquakes,mountains
In the rectal region of the digestive system. Its the creation of fecal matter.