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Agnes Bogan

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What is a trench between two parallel faults in earth's crust called?

A trench between two parallel faults in the earth's crust is called a graben. Grabens are formed by the downward movement of blocks of land between normal faults.


What are the similarities of active and inactive faults?

Active and inactive faults are both types of fractures in the Earth's crust where movement has occurred in the past. They both have the potential to generate earthquakes when stress is released along the fault line. Additionally, both types of faults can be identified through geological mapping, remote sensing techniques, and geophysical surveys. The main difference between active and inactive faults is that active faults are currently experiencing tectonic movement, while inactive faults have not shown any recent movement but still have the potential to generate earthquakes in the future.


What is the relationship between faults and volcanoes?

Volcanoes are usually found near convergent an divergent plate boundaries, which are themselves major faults and usually create minor faults. Minor faults can also provide a pathway for magma to reach the surface.


What are symmetrical faults?

A three-phase symmetrical fault exists when all three line conductors are short-circuited, sometimes to earth (ground). An unsymmetrical fault occurs when only one or two of the three lines are involved.


What are the types of faults that lead to earthquakes?

The main types of faults that lead to earthquakes are normal faults, reverse faults, and strike-slip faults. Normal faults occur when the hanging wall drops down relative to the footwall, while reverse faults happen when the hanging wall moves up relative to the footwall. Strike-slip faults involve horizontal movement along the fault.