An uplifted terrane is a region of the Earth’s crust that has been elevated due to tectonic forces, often resulting in the exposure of older rocks that were previously buried. This geological feature is significant in tectonics and geomorphology for understanding the processes of mountain building, crustal deformation, and the evolution of landscapes.
Reference: Coney, P. J., Jones, D. L., & Monger, J. W. H. (1980). “Cordilleran Suspect Terranes.” Nature, 288(5789), 329-333.