Definition:
Masse de glace qui s’écoule le long d’une pente sous l’effet de la gravité (par déformation interne et/ou glissement à la base) tout en étant contrainte par des pressions internes et des frictions à la base et sur les côtés. Les glaciers sont entretenus par l’accumulation de neige en haute altitude, équilibrée par la fonte à basse altitude ou par l’écoulement dans la mer.
Source:
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Food and Agriculture Organization of the United Nations, AQUASTAT Web Site
Bates, B.C., Z.W. Kundzewicz, S. Wu and J.P. Palutikof, Eds. 2008. Climate change and water. Technical Paper VI of the Intergovernmental Panel on Climate Change. IPCC Secretariat, Geneva, 210 pp.