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A normal fault.

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Mossie Auer

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3y ago

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Which type of fault is the result of tension and why?

Normal Fault


What type of FAULT is the result of compression forces?

a reverse fault


Which type of fault is the result of tension?

Normal faults are the result of tensile stresses.


Which type of fault is under tension?

Normal Thrust


Tension in earth crust can produce a normal fault which is?

A normal fault is a type of fault in which the hanging wall drops down relative to the footwall due to tensional forces in the Earth's crust. This type of fault is commonly associated with extensional tectonic settings, where the crust is being pulled apart.


Which mt form when forces pull from opposite direction?

The type of mountain that forms when forces pull from opposite directions is the fault-block mountain.


What type of fault in under tension?

A fault that is under tension is typically a normal fault. In a normal fault, the rock above the fault plane moves downward relative to the rock below, primarily due to extensional forces that pull the crust apart. This type of faulting is common in areas experiencing tectonic stretching, such as divergent boundaries or continental rift zones. The tension creates a landscape characterized by basins and elongated ridges.


What occurs when tension forces pull rocks apart?

When tension forces act on rocks, they can cause the rocks to stretch and eventually break. This type of stress can lead to the formation of faults, fractures, and rock rifts as the rocks are pulled apart. Over time, this can result in the creation of features like rift valleys or deep fractures in the Earth's crust.


What type of fault is tension associated with hanging wall?

the upper wall of an inclined fault


What type of fault usually occurs because tension?

normal


Which type of fault is caused by shearing forces?

A strike-slip fault


What type of fault moves because it is under tension?

A normal fault moves because of tension. In this type of fault, the hanging wall moves down relative to the footwall due to the stretching and pulling apart of the Earth's crust.