地理学評論
Online ISSN : 2185-1719
Print ISSN : 0016-7444
ISSN-L : 0016-7444
大興安嶺地帯の地下凍結
千葉 徳爾
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ジャーナル フリー

1949 年 22 巻 8 号 p. 259-263

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At the border of permanent frozen soil region, its depth depends on plants, soil and water in soil. I measured some places at Great Ningan and saw that mass of frozen soil was formed by moor growing up to. forest, and it moved like glacier. In this district forest situated only north sidle of hills, other sides are grass because underground moisture is little. All of these cause different weathering.
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