River Response to Melting Cryosphere Since Late Quaternary in the Pir Panjal Range of NW Himalaya
Rambiara River basin, a sub-basin of the Upper Indus, is dotted with fluvial and glacial geomorphic landforms.The presence of large number of glacial landforms like moraines, cirques, aretes, U-shaped valleys, etc.reflects the enormous erosive power of the past glaciers.During the Last Glacial Maximum (LGM), glaciers on average were 200 m thick and