Epeirogenic is the reverse of an orogenic process which involves mountain-building events like plate collision, resulting in the formation of mountain ranges.
Epeirogenic is the reverse of an orogenic process. Orogenic processes involve mountain-building events, such as the collision of lithospheric plates, leading to the formation of mountain ranges. In contrast, epeirogenic processes involve broad, regional uplift or subsidence of the Earth's crust without significant folding or faulting.
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