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If an excess quantity of labor demanded exists in a free market, there is a tendency for
Horizontal Syncline
A fold in sedimentary rock layers where the youngest materials are located at the center of the fold, typically indicating compression.
Dip-Slip Fault
A type of fault where the movement is mainly vertical, caused by the two sides moving up or down relative to each other.
Strike-Slip Fault
A type of fault where two blocks of the Earth's crust move horizontally past each other, parallel to the fault plane.
Normal Fault
A type of fault where the hanging wall slides downward relative to the footwall due to tensional forces.
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