Intro; Preface; Acknowledgements; Contents; About the Author; 1 Method; 1.1 Preliminary Methodological Remarks; 1.2 Methods in the Sense of Working Techniques; References; 2 Research Areas; 2.1 The Glaciation of the Pangong Co Area in WSW Tibet; 2.2 The High Glacial Outlet Glacier of the Shyok Valley in Connection with the Pangong Co Outlet Glacier on the Western Margin of Tibet; 2.2.1 Theory on the Accumulation of Till: A Digression in Order to Understand the Example of the Shyok Valley Outlet Glacier.

2.2.2 Continuation of the Reconstruction of the High Glacial Shyok Valley Outlet Glacier in Connection with the Pangong Co Outlet Glacier on the Western Margin of Tibet2.2.2.1 The High Glacial Shyok Outlet Glacier Between the Junction of the Nubra Glacier and the Gorge Section of Yagulung; 2.2.2.2 Summary of Sects. 2.1 and 2.2: The High Glacial (LGP) Glaciations of the Pangong Co Area in WSW Tibet and the Connected Shyok Outlet Glacier from the Western Margin of Tibet Down to the Valleys of the Karakorum.

The Classification of a Dating of Lake Terraces as Well as the Results in the Older Literature2.3 The High Glacial Indus Glacier in the Central Indus Valley at the Western Margin of Tibet; 2.3.1 The Late Glacial Phyang Chu Glacier as an Example of a Tributary Orographic Right Side Glacier of the Indus Parent Glacier and Its ELA Depressions; 2.3.2 More on the Reconstruction of the High Glacial Indus Glacier in the Central Indus Valley at the Western Margin of Tibet; 2.3.3 Summary of Sect. 2.3: The High Glacial Indus Glacier in the Central Indus Valley.

2.4 The Current, Historical, Neoglacial, and Late Glacial to High Glacial Glaciation of Central Tibet2.4.1 The Current, Historical to Neoglacial Glaciations of the Chongce Shan I-South Slope; 2.4.2 The Late Glacial to High Glacial Glaciation of West-Central Tibet Between the Chongce Shan I-South Slope and the Himalaya SW of Pangong Co; 2.4.3 The Present, Historical, Neoglacial (Holocene), and Late to High Glacial Glaciation of the Muggargoibo Massif in Central Tibet as a Further Representative Example.

2.4.4 The Current, Historical to Neoglacial (Holocene) Glaciation of the Nyainqentanglha Shan in Central Tibet2.4.4.1 Summary of the Present, Historical to Neoglacial (Holocene) Glaciation of the Nyainqentanglha Shan in Central Tibet; 2.4.5 The Late Glacial to High Glacial Glaciations of the Nyainquentanglha Shan in Central Tibet; 2.4.5.1 The Late to High Glacial Glaciation of the Nyainqentanglha Shan and the Nam Co Basin in Central Tibet; 2.4.5.1.1 Summary of the Historical to High Glacial Glaciations of the Nyainquentanglha Shan and the Nam Co Basin in Central Tibet.