Discovery of Quaternary glacial evidence of Snow Mountain in Taiwan, China  

作　　者：CUI Zhijiu YANG Jianfu LIU Gengnian WANG Xin SONG Guocheng 

机构地区：[1]Department of Geography,Peking University,Beijing 100871,China [2]Department of Geography,Taiwan University,Taibei,China [3]Department of Earth Science,Chenggong University,Tainan,China

出　　处：《Chinese Science Bulletin》2000年第6期566-571,共6页

摘　　要：There are glacial remains of three different periods on the main peak of Snow Mountain in Taiwan province, including cirque lake, crosswall, polished surface, striation, moraine ete. These three different periods were called, respectively, Shanzhuang ((44.25 ± 3.72) kaBP), Shuiyuan ((18.26 ± 1.52) kaBP), and Xueshan glacial stages (the late period of last glaciation). it is characterized by the earlier glacier broad in scale.There are glacial remains of three different periods on the main peak of Snow Mountain in Taiwan province, including cirque lake, crosswall, polished surface, striation, moraine etc. These three different periods were called, respectively, Shanzhuang ((44.25 ±3.72) kaBP), Shuiyuan ((18.26 ±1.52) kaBP), and Xueshan glacial stages (the late period of last glaciation). It is characterized by the earlier glacier broad in scale.

关 键 词：SNOW MOUNTAIN peak last GLACIATION three GLACIER REMAINS evidence. 

分 类 号：P343.6[天文地球—水文科学]