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《Journal of Glaciology and Geocryology》 1981-01
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PERIGLACIAL LANDFORMS OF THE CHANGBAI SHAN

Qiu Shanwen Li Fenghua Sui Xiulan ( Changchun Institute of Geography, Academia Sinica )  
Changbai Shan is one of the two large periglacial zone in Northeast China. The development of periglacial landforms is mainly conditioned by local relief and rocks together with other factors,such as the severe constructional cold climate in high moutains. The transformational force of periglacial landforms is chiefly by large scale of frost weathering and nivation, developing more than ten types of periglacial land-forms. Baitou Shan in the Changbai Shan is a big and high volcanic cone at 2749.2 m a.s.l.with a relative height of about 2000m.According to the data of Tianchi Meteorological Station, the annual mean temperature has been -7.3℃ for many years, the mean temperature of January -24. 0 ℃, and the yearly temperature difference reaches 50°-60℃.The climate is cold and wet, frost weathering proceeds strongly,and periglacial landform sufficiently develops. This district belongs to a vertical zone of high and cold periglacial environment at middle latitude. The lower limit of the periglacial zone might be set at the lower limit of the dark coniferous forest and generally coincides with the isotherm of 0℃ average temperature.
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【Co-citations】
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