HIMALDOC 4 records found  Search took 0.01 seconds. 
Year: 2009
Muztag Ata and Kongur Shan massifs represent a significant area of anomalously high topography at the northwestern end of the Tibetan Plateau, rising to > 7500 m above sea-level (asl) from the plateau that has an average elevation of ~ 3500 m asl
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Year: 2008
Glacial geological evidence from throughout the Himalayan–Tibetan orogen is examined to determine the timing and extent of late Quaternary glaciation in this region and its relation to similar changes on a global scale
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Year: 2001
The authors used cosmogenic 10Be to measure erosion rates over 10 k
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HIMALDOC 4 records found  Search took 0.01 seconds. 
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R. C. Finkel in TERI