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Critics of stabilization policy argue that
Thrust Faults
Thrust faults are a type of fault where the upper block, or hanging wall, moves up and over the lower block, or footwall, typically occurring at a low angle and often associated with mountain building.
Normal Faults
A geological fault in which the hanging wall moves down relative to the footwall, typically resulting from extensional forces.
Glacially Carved
Landforms shaped by the movement of glaciers, resulting in features such as U-shaped valleys and fjords.
Metamorphic Rocks
Rocks that have been transformed from their original state by heat, pressure, or chemically active fluids.
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