The answer is a dip-slip fault, When a portion of rock moves upward leaving the other in place with a dip this is known as a dip-slip fault.
The answer is a dip-slip fault, When a portion of rock moves upward leaving the other in place with a dip this is known as a dip-slip fault.
parallel normal faults.
A fault called a normal fault occurs when tectonic plates pull apart and tensional stress causes the rock layers to break and move along the fault line. In a normal fault, the hanging wall moves down relative to the footwall due to the extensional forces acting on the rocks.
The San Gabriel Mountains formed at what is essentially a kink in the San Andreas Fault. Along this fault the Pacific Plate slides northward while the North American Plate slides southward. At the kink, a small portion of the North American Plate juts out north of part of the Pacific Plate. The motion of the two plates rams them together at this location, thrusting sections of rock upward to form the San Gabriel Mountains.
A thrust fault occurs when one portion of rock slides over the top of the other. This type of fault typically forms in compressional tectonic settings where horizontal pressures cause the rocks to be pushed over each other at a low angle.
A reverse fault occurs when a portion of rock moves upwards while the other portion moves downwards, forming a dip in the rock layers. This type of fault is typically associated with compressional forces in the Earth's crust.
A reverse fault occurs when a portion of rock moves upward and over the other with a steep dip angle. This type of fault occurs in compressional tectonic settings where the forces push the rocks together, causing one block to thrust over the other.
The answer is a dip-slip fault, When a portion of rock moves upward leaving the other in place with a dip this is known as a dip-slip fault.
That is called a fault. A fault is a fracture in the Earth's crust where movement has occurred along the fracture.
reverse
The answer is a dip-slip fault, When a portion of rock moves upward leaving the other in place with a dip this is known as a dip-slip fault.
A normal fault occurs when a portion of rock moves downward relative to the other in place. This type of fault is caused by tensional forces pulling the rock mass apart, resulting in the hanging wall moving down relative to the footwall.
parallel normal faults.
parallel normal faults.
parallel normal faults.
A strike-slip fault generally occurs at a transform boundary