Miage Glacier
Debris-covered lower slopes of Miage Glacier in 2009
Map showing the location of Miage Glacier
Map showing the location of Miage Glacier
Miage Glacier
Glacier's location in the Alps
Map showing the location of Miage Glacier
Map showing the location of Miage Glacier
Miage Glacier
Miage Glacier (Northern Italy)
LocationSouthern slopes of the Mont Blanc massif
Coordinates45°48′15″N 6°50′26″E / 45.80417°N 6.84056°E / 45.80417; 6.84056
Area11 square kilometres (4.2 sq mi)
Length10 km (6.2 mi)

The Miage Glacier (French: Glacier du Miage; Italian: Ghiacciaio del Miage) is a debris-covered glacier in the upper Aosta Valley, in northwestern Italy.

Description

It is situated on the southwest flank of the Mont Blanc massif, flowing from the Col de Bionnassay (3,892 m (12,769 ft) above sea level) in a generally southerly direction towards Val Veny. Its most northerly arm or tributary is the Glacier de Bionnassay Italien, which arises from a cirque between the south eastern side of the Aiguille de Bionnassay, the Col de Bionnassay and the Calotte des Aiguille Grises. This descends for 2.5 km below the Col Infranchissible then turns south-east to merge with other glaciers, thence continuing as the Glacier du Miage (Ghiacciaio del Miage).

At around 10 km (6.2 mi) in length, the Miage Glacier is Italy's longest glacier and also the largest debris-covered glacier in Europe.[1][2] 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[3] and avalanching in accumulation areas of its four tributaries.[4] Debris carried along within the glacier is also being exposed at increased rates due to accelerating thinning of the glacier tongue.[4]

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.[4] 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.[5]

Miage Lake

View of Miage Lake from the west, summer 2010

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.[6] 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.[7]

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.[8] The incident was caught on camera by at least one tourist.

References

  1. ↑ "Miage Glacier, Italy". earth.esa.int. European Space Agency. Retrieved 10 November 2015.
  2. ↑ Deline, P. (2005). "Change in surface debris cover on Mont Blanc massif glaciers after the 'Little Ice Age' termination". The Holocene. 15 (2): 302. Bibcode:2005Holoc..15..302D. doi:10.1191/0959683605hl809rr.
  3. ↑ 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.
  4. 1 2 3 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.
  5. ↑ 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" (PDF). Journal of Geophysical Research. 115: D09106. Bibcode:2010JGRD..11509106B. doi:10.1029/2009JD013224.
  6. ↑ Masetti, M.; Diolaiuti, G.; D’agata, C.; Smiraglia, C. (2009). "Hydrological Characterization of an Ice-Contact Lake: Miage Lake (Monte Bianco, Italy)". Water Resources Management. 24 (8): 1677. doi:10.1007/s11269-009-9519-x.
  7. ↑ "SwissEduc: Glaciers Online - Glacier du Miage". Swisseduc.ch. 2008-01-28. Retrieved 2010-09-13.
  8. ↑ 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.
This article is issued from Wikipedia. The text is licensed under Creative Commons - Attribution - Sharealike. Additional terms may apply for the media files.