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title = "Palaeoglaciation of Bayan Har Shan, northeastern Tibetan Plateau: glacial geology indicates maximum extents limited to ice cap and ice field scales", abstract = "Key locations within an extensive area of the northeastern Tibetan Plateau, centred on Bayan Har Shan, have been mapped to distinguish glacial from non-glacial deposits.

(2008). Central Bayan Har Shan with TCN samples and 10Be exposure ages. Analysed sample types and results for the four sediment depth profiles. The ages in the sample Key locations within an extensive area of the northeastern Tibetan Plateau, centred on Bayan Har Shan, have been mapped to distinguish glacial from non-glacial deposits. Prior work suggests palaeo-glaciers ranging from valley glaciers and local ice caps in the highest mountains to a regional or even plateau-scale ice sheet.

Bayan har shan

Zhou and Li (1998) presented a four-stage glacial reconstruction for the Bayan Har Shan based on mapped glacial landforms and sediments. The oldest Huang He ice sheet stage, during marine isotope stage (MIS)-16, was followed by a slightly smaller ice mass that existed during the Yematan glaciation of Fig. 1. Bayan Har Shan is a mountain belt approximately 500km long and 150km wide stretching in a NW–SE orientation on the northeasternTibetanPlateau.Thestudyarea,centredonBayan Har Shan, encompasses the headwaters of the Huang He (Yellow River) in the north and is delimited in the southwest by the valley gorge of the Chang Jiang (Yangtze River) (Fig This study concerns the palaeoglaciation of the northeastern Tibetan Plateau, with emphasis on the Bayan Har Shan (Shan = Mountain) in the headwaters of Huang He (Yellow River). To reconstruct past glacier development multiple techniques, including remote sensing, field investigations, cosmogenic exposure dating, and numerical modelling have been employed. Key locations within an extensive area of the northeastern Tibetan Plateau, centred on Bayan Har Shan, have been mapped to distinguish glacial from non‐glacial deposits. Prior work suggests palaeo‐glaciers ranging from valley glaciers and local ice caps in the highest mountains to a regional or even plateau‐scale ice sheet. In conclusion, the glacial geology examined in the Bayan Har Shan region is consistent with paleo-glaciers of varying extent restricted to elevated mountain areas.

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of the northeastern Tibetan Plateau, with emphasis on the Bayan Har Shan (Shan = Mountain) in the headwaters of Huang He (Yellow River). To reconstruct

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In conclusion, the glacial geology examined in the Bayan Har Shan region is consistent with paleo-glaciers of varying extent restricted to elevated mountain areas. Even though extensive icefields/ice caps were centred on discrete mountain areas, there is no indication that these ice masses merged but rather that they were separated from each other by unglaciated plateau areas. Palaeoglaciation of Bayan Har Shan, northeastern Tibetan Plateau: glacial geology indicates maximum extents limited to ice cap and ice field scales Heyman, Jakob Stroeven, Arjen P. We here present a paleoglaciological reconstruction for the Bayan Har Shan region, NE Tibetan Plateau, which could serve as a working model to investigate other poorly investigated regions.
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