It is situated on the southwest flank of the Mont Blanc massif, flowing from Col de Bionnassay (3,892 m (12,769 ft) above sea level) into Val Veny. At around 10 km (6.2 mi) in length, it is Italy's longest glacier and also the largest debris-covered glacier in Europe. Approximately 5 km2 (1.9 sq mi) of its total area of ~11 km2 (4.2 sq mi) is covered in debris originating primarily in rockfall from surrounding walls and avalanching in accumulation areas of its four tributaries. Debris carried along within the glacier is also being exposed at increased rates due to accelerating thinning of the glacier tongue.
The number of sources of supraglacial debris as well as the unusual, mica schist-dominated lithology of the rock walls surrounding the glacier, makes for a varied debris lithology; debris cover becomes continuous at ~2,400 m (7,900 ft) above mean sea level (asl) and remains unbroken to the terminus. Patchy areas can occur, however, where crevasses or moulins occur. Debris thickness generally increases from a few centimetres at 2,400 m (7,900 ft) asl to over 1 metre (3 ft 3 in) at the terminus at ~1,775 m (5,823 ft) asl, although the spatial distribution of thicknesses is heterogeneous especially on parts of the northern terminal lobe.
Miage Lake is an ice-contact lake near the southern end of the Miage Glacier, located on the outside of the glacier's 90-degree bend eastwards. It is a popular tourist attraction due to the spectacular ice cliffs rising up to one side and its two-coloured appearance. The colours reflect varying sediment concentrations in the water which arise as a result of the filtering effect of the debris.
Huge ice blocks have been known to break off the glacier and fall into the lake, providing another major tourist attraction despite the low chance of such an event occurring. On August 7, 1996, a particularly large block, estimated to have had a volume of 7000-16000m3, fell into the lake causing an abnormally large wave that seriously injured several people.
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- Deline, P. (2009). "Interactions between rock avalanches and glaciers in the Mont Blanc massif during the late Holocene". Quaternary Science Reviews 28: 1070–1083. Bibcode:2009QSRv...28.1070D. doi:10.1016/j.quascirev.2008.09.025.
- Mihalcea, C.; Brock, B.; Diolaiuti, G.; Dagata, C.; Citterio, M.; Kirkbride, M.; Cutler, M.; Smiraglia, C. (2008). "Using ASTER satellite and ground-based surface temperature measurements to derive supraglacial debris cover and thickness patterns on Miage Glacier (Mont Blanc Massif, Italy)". Cold Regions Science and Technology 52: 341. doi:10.1016/j.coldregions.2007.03.004.
- Brock, B. W.; Mihalcea, C.; Kirkbride, M. P.; Diolaiuti, G.; Cutler, M. E. J.; Smiraglia, C. (2010). "Meteorology and surface energy fluxes in the 2005–2007 ablation seasons at the Miage debris-covered glacier, Mont Blanc Massif, Italian Alps". Journal of Geophysical Research 115: D09106. Bibcode:2010JGRD..11509106B. doi:10.1029/2009JD013224.
- "SwissEduc: Glaciers Online - Glacier du Miage". Swisseduc.ch. 2008-01-28. Retrieved 2010-09-13.
- Tinti, S.; Maramai, A.; Cerutti, A. (1999). "The Miage Glacier in the Valley of Aosta (Western Alps, Italy) and the extraordinary detachment which occurred on August 9, 1996". Physics and Chemistry of the Earth, Part A: Solid Earth and Geodesy 24 (2): 157. Bibcode:1999PCEA...24..157T. doi:10.1016/S1464-1895(99)00012-5.
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