Identify the true statement.
Strike slip fault hanging wall.
Typically this occurs in the hanging wall for dipping faults but also occurs with strie slip faults.
The forces creating these faults are lateral or horizontal carrying the sides past each other.
The displacement of layer b shows that this is a thrust fault.
Moving the hanging wall up an inclined fault requires work to overcome friction on the fault and the downward pull of gravity.
The hanging wall occurs above the fault plane and the footwall occurs below it.
That means someone standing near the fault trace and looking across it would see the far side move to the right or to the left respectively.
The displacement of layer b shows that this is a strike slip fault.
This terminology comes from mining.
Some parts of it dip east while others dip west.
Shallow focus quakes do less damage than deep focus quakes.
In these faults the fault plane is usually vertical so there is no hanging wall or footwall.
The two sides of a non vertical fault are known as the hanging wall and footwall.
High angle 45 or more dip thrust fault.
Hanging wall up footwall down.
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.
True in a reverse fault the hanging wall block moves up relative to the footwall block.
When the hanging wall moves horizontally it s a strike slip earthquake.
No side is consistently the hanging wall or the footwall for the san andreas fault.
Rocks on either side move horizontally in opposite directions.
When working a tabular ore body the miner stood with the footwall under his feet and with the hanging wall above him.
Zones of crustal compression.
Strike slip faults are either right lateral or left lateral.
Strike slip fault also called transcurrent fault wrench fault or lateral fault in geology a fracture in the rocks of earth s crust in which the rock masses slip past one another parallel to the strike the intersection of a rock surface with the surface or another horizontal plane.
Normal faults form in response to horizontal tensional stresses that stretch or elongate the rocks.
Later we will see how faults are often linked to more distributed deformation and how how you define the boundaries of the fault zone can make a difference.
Zones of crustal compression.
Hanging wall and footwall.
Since the san andreas fault is a strike slip fault which blocks.
Block x is the hanging wall.
