vertical...
i think
The main types of faults that lead to earthquakes are normal faults, reverse faults, and strike-slip faults. Normal faults occur when the hanging wall drops down relative to the footwall, while reverse faults happen when the hanging wall moves up relative to the footwall. Strike-slip faults involve horizontal movement along the fault.
A break in the Earth's crust that can move up, down, or sideways is called a fault. Faults are classified based on the direction of movement, with different types including normal faults, reverse faults, and strike-slip faults. Movement along faults can result in earthquakes.
Reverse faultNormal faultStrike-slip fault
Fractures in bedrock along which movement has taken place are known as faults. These geological structures occur when stress on the Earth's crust exceeds the strength of the rock, causing it to break and move. Faults can lead to significant geological events, such as earthquakes, and can vary in size and type, including normal, reverse, and strike-slip faults. The movement along these fractures can result in displacement of the rock layers on either side.
The movement of the crust along a thrust fault is usually a reverse movement unlike the movement along a normal fault.
earthquakes
vertical... i think
Fractures in rocks where movement occurs are called faults. These are surfaces along which rocks have broken and moved in response to stress. Faults are commonly found at tectonic plate boundaries and can result in earthquakes when movement happens along them.
A fracture in rock along which movement occurs is called a fault. faults are caused by stress in the Earth's crust, and can result in earthquakes when the stored energy is released through movement along the fault plane.
The three different types of rock movement in earthquakes are normal (extensional) faulting, reverse (compressional) faulting, and strike-slip (lateral) faulting. Normal faulting occurs when rocks are pulled apart, reverse faulting involves rocks being pushed together, and strike-slip faulting involves horizontal movement along a fault line.
When movement occurs along a normal fault, the hanging wall moves down relative to the footwall. This type of faulting is caused by extensional stresses in the Earth's crust, where the crust is being pulled apart. Normal faults are common in areas of tectonic plate divergence or in regions experiencing crustal extension.
The main types of faults that lead to earthquakes are normal faults, reverse faults, and strike-slip faults. Normal faults occur when the hanging wall drops down relative to the footwall, while reverse faults happen when the hanging wall moves up relative to the footwall. Strike-slip faults involve horizontal movement along the fault.
It slips downward when movement occurs along a normal faultIt occurs when the fault is at an angle
It slips downward when movement occurs along a normal faultIt occurs when the fault is at an angle
A break in the Earth's crust along which there has been some movement is a fault. A fault is considered a planar fracture.
A break in the Earth's crust that can move up, down, or sideways is called a fault. Faults are classified based on the direction of movement, with different types including normal faults, reverse faults, and strike-slip faults. Movement along faults can result in earthquakes.
Reverse faultNormal faultStrike-slip fault