词条 | Nivation |
释义 |
Weathered particles are moved downslope by creep, solifluction and rill wash.[1] Over time, this leads to the formation of nivation hollows which, when enlarged, can be the beginnings of a cirque.[1] References1. ^1 2 {{cite book |title=Surface Processes and Landforms |isbn=0-13-860958-6 |last=Easterbrook |first=Don J. |authorlink=Don Easterbrook |edition=2nd |page=334 |year=1999 |publisher=Prentice Hall |location=New Jersey}} {{Periglacial enviroment}}2. ^{{cite journal |title=Do periglacial landscapes evolve under periglacial conditions?|first=Marie-Françoise |last=André|year=2002|number=52|volume=1-2|pages=149–164|journal=Geomorphology|doi=10.1016/S0169-555X(02)00255-6}} 3. ^{{citation |url=http://www.nps.gov/archive/crla/notes/vol15b.htm#3 |title=Nivation |first=Franklin C. |last=Potter |date=September 1949 |volume=XV |number=1 |journal=Crater Lake Nature Notes}} 2 : Erosion|Snow |
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