Debris Slopes as Series
نویسندگان
چکیده
منابع مشابه
Ice-driven creep on Martian debris slopes
[1] Accumulations of rocky debris at the base of bedrock escarpments on Mars have mean inclinations of 20 , well below the angle of repose ( 35 ). These inclinations decrease with increasing latitude, suggesting a climatic influence. We present evidence that these low inclinations are the result of gravitational creep driven by repeated deposition and sublimation of ground ice. We estimate the ...
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ژورنال
عنوان ژورنال: Arctic and Alpine Research
سال: 1972
ISSN: 0004-0851,2325-5153
DOI: 10.1080/00040851.1972.12003653