Tilting and folding of rock layers due sinking, uplifting, stretching, or compression of the crust usually from plate movement.
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∙ 15y agoAnticlines and Synclines typically form during crustal deformation as the result of compression that accompanies orogenic mountain building.
compression
anticlines and synclines
anticlines, synclines, and monoclines
anticlines and synclines
Anticlines and Synclines typically form during crustal deformation as the result of compression that accompanies orogenic mountain building.
The most common of these are anticlines and synclines; anticlines are the "crests", while synclines are the "troughs".
compression
yes
yes
anticlines, synclines, and monoclines
anticlines and synclines
anticlines, synclines, and monoclines
anticlines and synclines
anticlines and synclines
synclines, anticlines, folded mountains, fault-block mountains, and plateaus
its the circulation of the rock and when it pushes together