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Qu'est-ce (qui) est roche moutonnee - définition
ROCK FORMATION CREATED BY THE PASSING OF A GLACIER
Roche mountainee; Rouche moutonnee; Sheepback; Roche Moutonnee; Roche Moutonnée; Roche moutonée; Roche moutonee; Roche moutoneé; Roche moutonnee; Roches moutonnée; Rôche moutonnée
![An oblique view of a roche moutonnée surface at [[Great Slave Lake]], [[Northwest Territories]], Canada; notice the contiguous, wavy rows of glaciated bedrock which resemble old-fashioned wigs as mentioned by Horace de Sassure](https://commons.wikimedia.org/wiki/Special:FilePath/Oblique view of roches moutonnees surface at Great Slave Lake, Nunavut, Canada.jpg?width=200 "An oblique view of a roche moutonnée surface at [[Great Slave Lake]], [[Northwest Territories]], Canada; notice the contiguous, wavy rows of glaciated bedrock which resemble old-fashioned wigs as mentioned by Horace de Sassure")
Roche moutonnee
·- ·see Sheepback.
Roche moutonnée
In glaciology, a roche moutonnée (or sheepback) is a rock formation created by the passing of a glacier. The passage of glacial ice over underlying bedrock often results in asymmetric erosional forms as a result of abrasion on the "stoss" (upstream) side of the rock and plucking on the "lee" (downstream) side.
roche moutonnee
[?r?. mu:'t?ne?]
¦ noun (plural roches moutonnees pronunciation same) Geology a small bare outcrop of rock shaped by glacial erosion, with one side smooth and gently sloping and the other steep, rough, and irregular.
Origin
C19: Fr., lit. 'fleecy rock'.
Wikipédia
Roche moutonnée
In glaciology, a roche moutonnée (or sheepback) is a rock formation created by the passing of a glacier. The passage of glacial ice over underlying bedrock often results in asymmetric erosional forms as a result of abrasion on the "stoss" (upstream) side of the rock and plucking on the "lee" (downstream) side. Some geologists limit the term to features on scales of a metre to several hundred metres: 324–326 and refer to larger features as crag and tail.
