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THE CYBER CENTER Glacier alpin
Glacier issu de l’accumulation et de la compaction de la neige éternelle des hautes montagnes, et dont le mouvement est surtout dicté par la pente des flancs et la formation des vallées.

Aujourd'hui, on observe un recul de la majorité des glaciers alpins dans le monde. Multimedia Gallery Your Testimonies There's currently no testimony. Submit your own testimony!Your Suggested Documents There's currently no suggested document. Submit your document!Your Suggested Links There's currently no suggested link. Submit a link!Return to the Cyber-Encyclopedia Home Page
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