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Divergent faulting. That is to say the two oceanic crust are moving apart from each other.
Transform boundaries cause fault lines or faults.
Normal / extensional faulting creates horst and graben topography.
type of faulting depth frequency of shakin proximity of epicentre distance of earthquake focus magnitude
the circulation of convection cells in the mantle, which dragged against the lithosphere
Divergent faulting. That is to say the two oceanic crust are moving apart from each other.
The type of faulting that characterizes mid-ocean ridges is a transform fault. This type of faulting occurs because transform fault ridges stay in the same fixed location, thus the new ocean sea floor being created at the ridges is pushed away from the ridge.
Basin and Range faults
Strike-Slip Faulting
convergent boundaries
Transform boundaries cause fault lines or faults.
and what type of fault is created with each type of stress
Normal / extensional faulting creates horst and graben topography.
Normal faults are the result of tensile stresses.
strartified squamous epithelium
type of faulting depth frequency of shakin proximity of epicentre distance of earthquake focus magnitude
That's what I'm trying to find out. Can somebody please answer it.! D: