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《Journal of Glaciology and Geocryology》 1988-01
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Moraine Features and Ice Ages of the Quaternary in the Taibai Mountain

Ma Qiuhua He Yuanqing ( Lanzhou Institute of Glaciology and Geocryology, Chinese Academy of Sciences )  
Baxiantai ( the highest peak of the Taibai Mountain, 3767m a.s.l.)is located in the border among Taibai, Meixian and Zhouzhi counties.During earlier and later periods of tho Late Pleistocene, two glaciations occurred at Baxiantai, that is, the Sanyehai Ice Age and the Taibai Ice Age. In the Taibai lce Age two sub-ice ages can be divided. By excavating artificial sections the authors have confirmed that there are thfee moraines in the Eryehai glacial valley located in the southern slope of Taibai Mountain.Some cirques and other glaciation vestiges are also found, corresponding with above-mentioned Ice Ages.Because of the uplift of the Taibai Mountain and fluctuations of snow-lines, all cirques of the Taibai Ice Age developed on the basis of earlier cirques The remainder of earlier cirques were preserved at the shoulder on one side of the cirque or at mountain redges between two later cirques as glacier scale deccreased. Before the end of the "Last Ice Age", some small parasitic cirques, such as the Day-ehai cirque and Eryehai cirque, has formed with the rise of snowlines. These glacial landforms are controled in trend, location, shape and so on by tec-tonism.
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1 LI Yue-cong1, XU Qing-hai1,CAO Xian-yong1,YANG Xiao-lan2, LI Yi-yin3,ZHOU Li-ping3 (1.College of Resources and Environmental Sciences, Hebei Normal University, Shijiazhuang 050016,China; 2.Hebei Geography Institute, Hebei Academy of Sciences, Shijiazhuang 050011,China; 3.College of Environmental Sciences, Peking University, Beijing 100871,China);Pollen influx and surface pollen assemblage on the northern slope of Taibai Mountain[J];Geographical Research;2008-03
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