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《Journal of Glaciology and Geocryology》 1981-04
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Periglacial Landforms and Region-alization in Northeast China

Xie Youyu (Institute of Geography, Academia Sinica)  
According to the action of exogenetic force, the types of periglacial landforms and sediments in Northeast China can be divided as follows: ( 1 ) Frost-heaving action: pingos, polygons, small non-sortednet, involutions, sand wedge, etc. (2) Thawing action: thaw lakes, thaw depression. (3) Frost-creeping action: solifluction fan, solifluction step, etc. (4) Nivation action: nivation hollow-scree cone, nivation hollow-so-lifluction fans. (5) Frost weathering-gravity action: rock field, block slope, scree-cone, talus etc. ( 6 ) Fluvial action: flat-bottom valley, asymmetric dale and hill. ( 7 ) Wind action: dune, reaction dune, eolation hollow, orientation lake, periglacial loess. The periglacial zone of this region is divided into two types: latitudinal periglacial zone and altitudinal periglacial zone. The latitudinal zone includes three regions: I . The region of Northern Da Hinggan Ling with wet and rather cold climate and strongly developed periglacial landform including(1) (2) (3) ( 5 ) of the above-mentioned types. II . The region of the western slope of Da Hinggan Ling with semi-arid and cold climate and moderately developed periglacial landforms including ( 5 ) ( 7 ) of the above-mentioned types. III . The region of the eastern slope of Dax hinggan Ling and Xiao Hinggan Ling wifh semi-wet and cold climate and moderately developed periglacial land-forms including( 2 )( 4 )( 6 ) of the above-mentioned types The altitudinal periglacial zone is divided into two regions. I . The region of Changbai Shan with wet and cold climate and well developed periglacial landforms including (4)(3)(5) of the above-mentioned types. II . The region of Huangganliang with semiarid and cold climate, and moderately developed periglacial landforms including (7) (5) (4) of the above-mentioned types.
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【References】
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