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joint does not show any relative movement as fault does

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What is the main difference between a dip slip fault and a strike slip fault?

The main difference between a dip-slip fault and a strike-slip fault is the direction of movement. In a dip-slip fault, the movement is primarily vertical along the dip direction of the fault plane, either up or down. In a strike-slip fault, the movement is primarily horizontal along the strike direction of the fault plane, either to the left or right.


What is the difference between a crack in the earths crust and a fault?

A crack in the Earth's crust is a fracture where rocks have pulled apart, whereas a fault is a fracture where there has been movement along the fracture plane. In other words, a fault is a type of crack in the Earth's crust that has undergone displacement.


What is the difference between a transform and a transverse fault?

A transform fault is a general term to describe a plate boundary where the lithosphere is not destroyed or created. A transverse fault is a type of transform fault also known as a strike-slip fault.


What is the difference between a reverse and normal fault and how does stress relate to the formation of each?

In a reverse fault, the hanging wall moves up relative to the footwall due to compressional stress. This type of fault occurs in convergent plate boundary settings. Conversely, in a normal fault, the hanging wall moves down relative to the footwall due to extensional stress, which is typically associated with divergent plate boundaries. Stress plays a crucial role in determining the type of fault that forms in response to the tectonic forces acting on the rock.


What is a joint fault?

Joint fault is an extense shear joint in basalt flows, dominantly layer-parallel and probably generated initially by the differential inertial movements inside the cooling lava flow of portions with different melt-viscosities. Their planar part is probably conditioned by the isotherms distribution, while curved segments may be related to brittle-ductile fissure propagations along their edges.

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