Appalachian Studies
Synclines are geological formations characterized by a downward-curving fold in rock layers, creating a trough-like structure. They typically form as a result of tectonic forces that cause the Earth's crust to bend and compress, leading to the alignment of younger rock layers at the core and older rock layers on the flanks. Understanding synclines is important for recognizing patterns of landforms and assessing natural resources within regions like the Ridge-and-valley system.
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