Terrestrial cosmogenic nuclide dating
The mountain landscapes, however, are also the consequence of profound erosion by glaciers and rivers, mass movement (slope) processes and weathering.Defining how quickly the Himalaya and Tibet are uplifting and eroding has been one of the great challenges in geomorphology over their many decades of study and is important for helping to quantify tectonic and geomorphic models.Created by the author of the page containing this file. Sampling river sands in the Beas Valley of the Greater Himalaya of Northern India to determine the concentrations of terrestrial cosmogenic nuclides to calculate rates of catchment wide erosion.
Recently, global positioning systems have been used to determine short-term (years-decades) rates of surface displacement.
The mountain mass contains the entire world's 8000-m-high peaks and spans climates ranging monsoonal to arid.