Hanging Wall Rises Relative To The Footwall

Fault that occurs when two tectonic plates collide.

Hanging wall rises relative to the footwall.

Thrust fault a dip slip fault in which the upper. Reverse faults occur in areas undergoing compression squishing. The terminology of normal and reverse comes from coal mining in england where normal faults are the most common. Eruption tends to be very explosive.

The hanging wall drops relative to the footwall reverse fault fault that occurs when two tectonic plates collide. The hanging wall rises relative to the footwall. Magma that has a high viscosity and high silica and gas content. Syncline underwater volcano whose top is eroded flat by waves 3.

A normal fault occurs when the crust is extended. Horst natural hot water on earth s surface containing many minerals 7. Caldera magma that filled the central vent that remains after the volcano has eroded 6. Reverse faults if the hanging wall rises relative to the footwall.

The hanging wall rises relative to the footwall. Fault that occurs when two tectonic plates collide. Alternatively such a fault can be called an extensional fault. The dip of a reverse fault is relatively steep greater than 45.

Fault that occurs when two tectonic plates are moving apart from each other. If the hanging wall rises relative to the footwall you have a reverse fault. Fault that occurs when two tectonic plates are moving apart from each other. A reverse fault is the opposite of a normal fault the hanging wall moves up relative to the footwall.

Seamount underwater volcano that never reaches above sea level 2. Reverse faults occur in areas undergoing compression squishing. Volcanic flow that contains a high concentration of gases ash and small rocks. This fault occurs when a hanging wall block has risen relative to its footwall block.

Hot spring on rolling hills this a dip between hills 4. If the hanging wall rises relative to the footwall you have a reverse fault. Cliff like landform created by a normal fault. The hanging wall rises relative to the footwall.

Cliff like landform created by a normal fault. Volcanic neck break between rocks where a hanging wall rises relative to a footwall 5. The hanging wall rises relative to the footwall. Another type of fault is the thrust fault where ground on one side of the fault moves up and over adjacent ground.

The hanging wall drops relative to the footwall. If you imagine undoing the motion of a reverse fault you will undo the compression and thus lengthen the horizontal distance between two points on either side of the fault. The hanging wall drops relative to the footwall. Graben a raised footwall block between normal fault creates.

Fault that occurs when two tectonic plates are moving apart from each other.