This translates to an uplift rate of about 0.01-0.02 inches (0.2-0.5 millimeters) per year, the researchers estimated. The geological process responsible for this phenomenon is known as isostatic ...
That translates to an uplift rate of roughly 0.2 to 0.5mm annually. The geological process at work, they said, is called isostatic rebound. It involves the rise of land masses on Earth’s crust ...
That translates to an uplift rate of roughly 0.2 to 0.5mm per year. The geological process at work, they said, is called isostatic rebound. It involves the rise of land masses on Earth’s crust ...
tectonic uplift or subsidence, and glacial isostatic adjustment. The latter references the uplift of land and crustal deformation in response to the loss of ice sheet mass loading as they melt.