A fault-block mountain forms where the edges of two plates come together to create a fault. When one plate pushes up over the other one, the upper one can continue up until it is high enough to create a fault-block mountain.
Chat with our AI personalities
The surface of earth is in constant motion because of forces inside the planet. These forces cause sections of earth's surface, called plates, to move.
The Alpine Fault is a geological right-lateral strike-slip fault. It forms a transform boundary, so yes.
A lateral fault is when Shearing causes rock blocks to slide horizontally past each other.
A reverse fault forms when a hanging wall moves upward due to compressional forces. This type of fault occurs in areas where the crust is being pushed together, causing the hanging wall to move up and the footwall to move down.
A reverse fault can create a landform known as a fault scarp, which is a steep slope or cliff that forms when one block of rock is thrust up and over another along the fault line. This can result in noticeable elevation changes in the landscape.
In a normal fault, the hanging wall moves down relative to the footwall, resulting in extensional strain. This type of fault forms in response to tensional stress in the Earth's crust, such as the pulling apart of tectonic plates.