Ocean plate because it is more dence when an ocean plate and a continental plate collide which plate would be pushed into a subjection zone.
Hanging wall plate tectonics.
Top of the sign hangs flat bottom is at an angle.
Short side is half of the overall height.
The hanging wall is like a cliff with an overhang.
Theory of plate tectonics.
The footwall rests on its widest part.
In geology a fault is a planar fracture or discontinuity in a volume of rock across which there has been significant displacement as a result of rock mass movement.
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The tectonic plates can be made up of many faults.
Links theories of continental drift and ocean floor spreading.
Hanging wall the block of rock that forms the upper half of a fault.
The driving force that helps tectonic plates move.
Plate tectonics from the late latin.
Plate a section of the lithosphere that slowly moves over the asthenosphere carrying pieces of continental and oceanic crust.
Hanging wall goes down while footwall rises due to tension divergent boundaries hanging wall goes up wall foot wall sinks due to compression converngt boundary the two plates slide past each other.
The theory that explains how large pieces of the earth s outermost layer called tectonic plates move and change shape.
Large faults within the earth s crust result from the action of plate tectonic forces with the largest forming the boundaries between the plates such as subduction zones or transform faults.
Theory of plate tectonics earth s plates are in slow constant motion driven by convection currents in the mantle.
The one side is called the foot wall.
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The other is the hanging wall.
This makes two fault blocks.
A type of fault where the hanging wall slides downward relative to the foot wall caused by tension in the crust.
Closed bottom graphics include bottom panel.
Nasa sometimes the faults occur along an angle.
A hanging wall is the overhanging rock unit on the slant that separates the two slabs while the footwall is below the slant what is the modern theory for orogenesis mountain building.
Sea floor spreading and the theory of plate tectonics.