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Horst mountains form at large-scale normal faults where the footwall and hanging wall spread apart from each other. Horst mountains are created by blocks of the Earth's crust uplifting along the fault line, resulting in mountainous ridges or plateaus.

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Normal and reverse faults are characterized mainly by?

Normal faults are characterized by the hanging wall moving down relative to the footwall, while reverse faults are characterized by the hanging wall moving up relative to the footwall. Both faults are caused by compressional forces in the Earth's crust, but their movements are opposite in direction.


When the hanging wall moves up relative to the footwall it is a fault.?

Yes, when the hanging wall moves up relative to the footwall along a fault, it is known as a reverse fault. Reverse faults are caused by compressional forces in the Earth's crust, leading to the hanging wall moving up and over the footwall.


Compare normal faults to reverse faults?

Normal faults occur when the hanging wall moves down relative to the footwall due to extensional forces, while reverse faults occur when the hanging wall moves up relative to the footwall due to compressional forces. Normal faults are associated with divergent plate boundaries, while reverse faults are associated with convergent plate boundaries.


In a fault the hanging wall moves down relative to the footwall?

This is true of normal faults. In thrust or reverse faults, the hanging wall moves up relative to the footwall and in strike slip faults, it moves horizontally relative to the footwall.


What boundary creates fault-block mountains?

Fault-block mountains are created by tensional forces in the Earth's crust that cause blocks of rock to move up or down along faults. As these blocks move, they create a series of steep mountain ranges and valleys. This movement is typically associated with normal faults, where the hanging wall moves downward relative to the footwall.

Related Questions

Which mountains form at large-scale normal faults where the footwall and hanging wall spread apart from each other?

Fault-block mountains


What does normal faulting mean?

Normal faults are when you have hanging walls that slide down relative to and below the footwall. Dip-slip faults are normal faults.


What types of faults would you expect to find in these mountains?

Reverse faulting is found in the Himalayas. With a reverse fault, the hanging wall moves up relative to the footwall.


Normal and reverse faults are characterized mainly by?

Normal faults are characterized by the hanging wall moving down relative to the footwall, while reverse faults are characterized by the hanging wall moving up relative to the footwall. Both faults are caused by compressional forces in the Earth's crust, but their movements are opposite in direction.


What is a Reverse faults?

A reverse fault is a fault in which the hanging wall moves up relative to the footwall.


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.


What are the movements produced by the three types of faults?

-Normal Faults form when the hanging wall moves down. -Reverse Faults form when the hanging wall moves up. -Strike-Slip Faults have walls that moce sideways, instead of up or down.


When the hanging wall moves up relative to the footwall it is a fault.?

Yes, when the hanging wall moves up relative to the footwall along a fault, it is known as a reverse fault. Reverse faults are caused by compressional forces in the Earth's crust, leading to the hanging wall moving up and over the footwall.


What are the 3 types of fault?

Reverse faultNormal faultStrike-slip fault


Compare normal faults to reverse faults?

Normal faults occur when the hanging wall moves down relative to the footwall due to extensional forces, while reverse faults occur when the hanging wall moves up relative to the footwall due to compressional forces. Normal faults are associated with divergent plate boundaries, while reverse faults are associated with convergent plate boundaries.


In a fault the hanging wall moves down relative to the footwall?

This is true of normal faults. In thrust or reverse faults, the hanging wall moves up relative to the footwall and in strike slip faults, it moves horizontally relative to the footwall.


What does faults mean?

Normal faults are when you have hanging walls that slide down relative to and below the footwall. Dip-slip faults are normal faults.