a reverse fault
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.
When compression pushes rocks together, it creates a reverse fault. In a reverse fault, the hanging wall moves up relative to the footwall due to compression forces pushing the rocks together.
A reverse fault is a type of fault where the hanging wall moves up relative to the footwall due to compression forces in the Earth's crust. This type of fault is typically found in regions undergoing compression, such as at convergent plate boundaries where tectonic plates collide. Reverse faults are characterized by a steep fault plane and can result in uplift and mountain building.
A reverse fault occurs when compression forces push one side of the fault upward and the other side downward. This motion creates a steep incline in the fault plane, with the hanging wall moving up and the footwall moving down. Reverse faults are typically associated with convergent plate boundaries where compression forces are high.
A reverse fault is under compression. In a reverse fault, the hanging wall moves up relative to the footwall due to compression forces in the Earth's crust. This type of fault is common in areas with convergent tectonic plate boundaries.
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 normal fault.
A fault caused by compression forces is a reverse fault, where the hanging wall moves up relative to the footwall. This type of fault is commonly found in areas where tectonic plates are colliding, such as in mountain ranges. Reverse faults are associated with convergent plate boundaries.
When compression pushes rocks together, it creates a reverse fault. In a reverse fault, the hanging wall moves up relative to the footwall due to compression forces pushing the rocks together.
A reverse fault is a type of fault where the hanging wall moves up relative to the footwall due to compression forces in the Earth's crust. This type of fault is typically found in regions undergoing compression, such as at convergent plate boundaries where tectonic plates collide. Reverse faults are characterized by a steep fault plane and can result in uplift and mountain building.
A thrust fault is a type of reverse fault where the hanging wall moves up and over the footwall, resulting in compression and shortening of the crust. This type of fault is commonly associated with convergent plate boundaries where horizontal compression forces rocks to move vertically.
A reverse fault is a type of fault in which the hanging wall moves up relative to the footwall, resulting from compressional forces in the Earth's crust. This type of fault is common in regions undergoing compression, such as convergent plate boundaries. Reverse faults are characterized by steeply dipping fault planes and may result in the uplift of mountain ranges.
A reverse fault occurs when compression forces push one side of the fault upward and the other side downward. This motion creates a steep incline in the fault plane, with the hanging wall moving up and the footwall moving down. Reverse faults are typically associated with convergent plate boundaries where compression forces are high.
Probably reverse fault because folding is the result of compressional stres and reverse faults are caused by compression
compression :)