Strike Slip Fault Hanging Wall Footwall

In a strike slip fault a the hanging wall moves down relative to the footwall b the hanging wall moves up relative to the footwall at the angle of 30 degrees or less c the hanging wall moves up relative to the footwall at an angle of 45 degrees or more d the fault blocks move horizontally in opposite directions.
Strike slip fault hanging wall footwall. That is the slip occurs along the strike not up or down the dip. The forces creating these faults are lateral or horizontal carrying the sides past each other. This terminology comes from mining. At x 1 the rightward flow rate is 0 192 m sec.
P examples of how to use normal fault in a sentence from the cambridge dictionary labs normal faults are common. Strike slip faults have walls that move sideways not up or down. In these faults the fault plane is usually vertical so there is no hanging wall or footwall. P a normal fault occurs because two tectonic plates are pulling apart from each other causing tensional stress.
The two sides of a non vertical fault are known as the hanging wall and footwall. They bound many of the mountain ranges of the world and many of the rift their size does however limit the potential for earthquake because many faults show a combination of dip slip and strike slip motion geologists use more encyclopaedia britannica universal images. The hanging wall occurs above the fault plane and the footwall occurs below it. No side is consistently the hanging wall or the footwall for the san andreas fault.
Hanging wall and footwall.