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The type of force found in a strike slip fault is lateral force.

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13y ago

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The type of stress force that produces a strike-slip fault is transform stress. This stress occurs when two tectonic plates slide past each other horizontally, causing displacement along a fault line. Strike-slip faults are often associated with transform plate boundaries, such as the San Andreas Fault in California.

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AnswerBot

9mo ago
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Shear forces and hence stresses are generated at a strike-slip fault boundary.

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14y ago
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tension or compression, or strike-slip

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12y ago
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Landslide

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11y ago
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shear

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13y ago
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Shear force

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14y ago
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Q: The type of stress force that produces a strike-slip fault is?
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Continue Learning about Earth Science

The bending and buckling of rocks under great force produces a fold a fault a rift a epicenter?

The bending and buckling of rocks under great force produces a fold.


How frictional resistance along a fault affect the force released during an earthquake?

Higher frictional resistance along a fault can inhibit the fault from slipping smoothly, causing stress to accumulate over time. When this stress is eventually released as an earthquake, the force released can be higher if the resistance was greater. Conversely, lower frictional resistance can allow the fault to slip more easily, potentially leading to a lower force released during an earthquake.


What type of force causes a normal fault to form?

Tensional stress from divergent plate boundaries causes a normal fault to form. This stress pulls rocks apart along a fault line, causing the hanging wall to drop relative to the footwall.


What force causes a strike slip fault?

Strike-slip faults are caused by horizontal shear stress along the fault plane, which results in horizontal movement of the rocks on either side of the fault. The movement can be either left-lateral (sinistral) or right-lateral (dextral), depending on the direction of the shear stress.


What force causes rocks on either side of a fault to slide past each other?

The force that causes rocks on either side of a fault to slide past each other is the built-up stress along the fault line, which is released as the two sides move in opposite directions. This stress can accumulate due to tectonic plate movements, leading to the sudden release of energy in the form of an earthquake.