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.
thrust A+
A reverse fault occurs when compression forces push one side of the fault upward and the other side downward. This type of fault is associated with convergent plate boundaries where tectonic forces cause crustal rocks to be pushed together.
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.
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 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.
reverse
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.
thrust A+
A reverse fault occurs when rock above the fault moves upward at the fault line. This type of fault is associated with compressional stress where the hanging wall moves up relative to the footwall. Reverse faults are common in regions undergoing compression, such as convergent plate boundaries.
A reverse fault occurs when compression forces push one side of the fault upward and the other side downward. This type of fault is associated with convergent plate boundaries where tectonic forces cause crustal rocks to be pushed together.
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.