M. Ellis G. King 1990 Large localized uplift is commonly observed in continental regions undergoing extension. These observations can be modelled by planar, high-angle normal faulting of an elastic upper crust overlying an inviscid lower crust. Isostasy provides the necessary driving force. The model quantifies the role of flexural rigidity, density variations in the crust, and erosion and deposition of sediment. application/pdf 10.1038/348689a0 en Springer Nature The origin of large local uplift in extensional regions article