Geomorphic character, age and distribution of rock glaciers in the Olympic Mountains, Washington
Rock glaciers are tongue-shaped or lobate masses of rock debris which occur below cliffs and talus in many alpine regions. They are best developed in continental alpine climates where it is cold enough to preserve a core or matrix of ice within the rock mass but insufficiently snowy to produce true...
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| Format: | Others |
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PDXScholar
1987
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| Online Access: | https://pdxscholar.library.pdx.edu/open_access_etds/3558 https://pdxscholar.library.pdx.edu/cgi/viewcontent.cgi?article=4565&context=open_access_etds |