5 names of old fold mountains in each continent wise
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The Jura mountains – A series of sub-parallel mountainous ridges that formed by folding over a Triassic evaporite decollement due to thrust movements in the foreland of the Alps
The 'Simply Folded Belt' of the Zagros Mountains – A series of elongated anticlinal domes, mostly formed as detachment folds over underlying thrusts in the foreland of the Zagros collisional belt, generally above a basal decollement that formed in evaporite of the late Neoproterozoic to Early Cambrian Hormuz Formation
The Akwapim-Togo ranges in Ghana
The Ridge-and-Valley Appalachians in the eastern part of United States.
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