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Anticlines
Upwardly convex folds in rock layers, typically formed through compression within the Earth's crust.
Synclines
Downward-curving folds in sedimentary strata, opposite of anticlines, which can also be indicators of oil and gas deposits.
Cleavage
In geology, the tendency of crystalline materials to split along definite crystallographic structural planes, creating flat, shiny surfaces.
Monocline
A geological feature where sedimentary layers are tilted or bent along a single axis.
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