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Felsenmeer

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felsenmeer [′felz·ən‚mer]
(geology)
A flat or gently sloping veneer of angular rock fragments occurring on moderate mountain slopes above the timber line.

Felsenmeer 

vast placers of blocks of rock on the flat surfaces of mountain peaks, located above the treeline. They form as the result of the processes of frost weathering together with the phenomena of solifluction under conditions of a severe continental climate and the development of permafrost rock.



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2004, Felsenmeer persistence through glacial periods in the Torngat and Kaumajet Mountains, Quebec-Labrador, as determined by soil weathering and cosmogenic nuclide exposure dating: Canadian Journal of Earth Sciences, v.
The thick-bedded and massive members are fractured and frost-heaved into large slabs of felsenmeer that raft downhill for considerable distances and locally override the Lower Schist Unit.
 
 
 
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