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Find the area of the surface of revolution , where
and
.
Normal Fault
A type of geological fault where the hanging wall has moved downward relative to the footwall, usually due to extensional forces.
Cleavage
In geology, the tendency of a mineral to break along flat, parallel surfaces determined by its crystal structure.
Hornfels
A hard, fine-grained metamorphic rock formed by the contact metamorphism of clay-rich or silicate rocks.
Thrust Fault
A type of fault in which the upper block, above the fault plane, moves up and over the lower block.
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