Examlex
The final step in delegation is:
Cleavage
The tendency of a mineral to break along flat, defined surfaces as a result of its crystal structure.
Axial Surfaces
Imaginary surfaces that divide a fold as evenly as possible, extending through the apex of each fold in stratified rock.
Folds
Structures formed by the bending and warping of rock layers under pressure during geological processes.
Metamorphic Rocks
Rocks that have undergone transformation in their mineral composition or texture due to high pressure and temperature, without melting.
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