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When two states decide to bargain:
Syncline
A fold, generally concave upward, with the youngest rocks in the center.
Cleavage
A property of minerals that describes their tendency to break along flat surfaces based on their crystalline structure.
Strike-Slip Fault
A type of fault where rocks on either side move horizontally past one another, typically a result of shear stress.
Oblique-Slip Faults
Faults that exhibit both vertical and horizontal movement, combining characteristics of strike-slip and dip-slip (normal or reverse) faults.
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