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 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.
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 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.
A strike-slip fault generally occurs at a transform boundary
If a fault occurs in an area where rock layers have been folded, the type of fault it is likely to be is thrust faulting. This type of fault will have the ground on one side of the fault, move up and over adjacent ground.
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.
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.
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.
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.
parallel normal faults.
parallel normal faults.
parallel normal faults.
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.
A strike-slip fault generally occurs at a transform boundary
thrust A+
sliding friction.