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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. Want to thank TFD for its existence? Tell a friend about us, add a link to this page, add the site to iGoogle, or visit the webmaster's page for free fun content. |
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