The Info List - Mont Blanc Glacier Flood

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The TêTE ROUSSE GLACIER (French : Glacier
de Tête Rousse) is a small but significant glacier located in the Mont Blanc massif within the French Alps
whose collapse in 1892 killed 200 people in the town of Saint-Gervais-les-Bains .


* 1 Geography * 2 1892 Mont Blanc
Mont Blanc
glacier flood * 3 Modern day risks * 4 Notes * 5 References * 6 External links


The glacier is located on the northwestern slopes of the Aiguille du Goûter , on the northern side of Mont Blanc
Mont Blanc
and 11 km upstream of the town of Saint-Gervais. It lies at an altitude of 3,300 metres, descending to a height of 3,100 metres, and is predominantly avalanche-fed from snows falling from the steep slopes of Aiguille du Goûter above. As at 2007, the glacier had a total area of 0.08 km² and a maximum thickness of 75 metres.

The glacier is frequently crossed by mountaineers on their way to the Tête Rousse mountaineering hut , which stands at the side of the glacier at an altitude of 3,167 metres. It is also crossed by many more climbers attempting the 'normal' route of ascent to the summit of Mont Blanc
Mont Blanc
via the Goûter route. The Tête Rousse Glacier
lies just above the considerably much larger Glacier
de Bionnassay, yet the build-up of large water pockets within this small glacier continues to pose a very serious risk to life to this day, and has been the subject of much research and disaster planning, with considerable investment in risk-reduction measures. The main risk to life comes from a repeat of the 1892 outburst flood which would impact upon those living in the valley below.


The Mont Blanc
Mont Blanc
glacier flood was a devastating outburst flood that occurred on 11 July 1892. The disaster took place at night-time when the Tête Rousse Glacier
suddenly released 200,000 cubic meters of water from large pockets of water which had accumulated within the structure of the glacier. The collapse of the glacier and sudden release of water completely destroyed the hamlet of Bionnay and flooded the bath house in the town of Saint-Gervais , reaching as far as the hamlet of Le Fayet. Contemporary accounts show that over 200 people lost their lives in the villages. Everything in the path of the rushing water, mud and boulders was swept away, leaving behind some 800,000 cubic metres of sediment.

Joseph Vallot (fr), the glaciologist and Director of the Mont Blanc Observatory at the time of the incident, published detailed accounts of his investigations into the Catastrophy of Saint Gervais. Measurements and photographs taken shortly afterwards showed that part of the glacier's snout (terminus ) had been torn away, revealing a cavity 40 metres in diameter and 20 metres above its base. From this a 3 metre high tube led back some 85 metres and at a 36° angle to an even larger second cavity, up to 40m high and 50 m wide. Maps drawn up shortly afterwards confirmed a depression in the centre of the glacier. It was estimated that 100,000 cubic metres of liquid water had drained away during the glacier's collapse, plus a further 100,000 cubic metres of broken ice. Together with the soil and rock broken away by the force of the rushing water, Vallot estimated that a weight of 500 million kilograms of material had borne down on the villages. He also warned that a repeat of water build-up was quite likely to occur, and that this would become more dangerous as time went on. He advocated the use of explosives to ensure a permanent flow of meltwater away from the glacier.

In 1904 a second water pocket was discovered within the glacier, and a hole was drilled to drain away 22,000 cubic metres.

Opinions have differed as to the precise mechanism by which water had built up in such quantity and then had suddenly been released with such devastating consequences. For many years the accepted explanation was that proposed by Joseph Vallot. It was believed that meltwater had drained through the glacier and become trapped as an intraglacial cavity, i.e. as an underground lake within a crevasse which itself had then become enlarged and widened by the water. However, recent re-analysis of historic photographs, accounts and contemporary meteorological precipitation data and field measurements, including radar analysis and magnetic resonance imaging, has presented an alternative and more plausible mechanism in which meltwater collected much closer to the surface (as a supraglacial lake ) in a period when the glacier had a negative mass balance (i.e. was experiencing year-on-year melting and retreat). Prior to 1878 the glacier would not have been well-visited, so any surface lake could have gone unnoticed, and after 1878 the glacier experienced a positive mass balance (i.e. year-on-year accumulation of snow and ice) which would have hidden the lake from view until the eventual outburst flood in 1892.


In July 2010 a pocket containing 50,000 cubic metres of water was detected in a glacial pocket, and some 48,000 cubic metres of water were pumped out. A siren warning system was installed to aid evacuation of those at risk in the valley below, and evacuation plan was put in place. The final section of the Mont Blanc
Mont Blanc
Tramway from St Gervais to Nid d'Aigle was closed for safety reasons for the rest of the operational season, as was the adjacent Nid d'Aigle mountain refuge .

In 2011 water levels within the glacier were predicted to refill the glacial cavity before summer, and a further 25,000 cubic metres of water was drained away. Further research was carried out to study and monitor the origin of the water.

In 2012 results of research were presented showing that two water pockets existed within the glacier. On 17 August 2012 part of the glacier's surface collapsed inwards. This created a large hole through which a glacial lake could be seen. Paths across the glacier were diverted, including that used to reach the Gouter Hut and thence the summit of Mont Blanc.

At 1:47am on 29 July 2013 during a heavy storm, the alarm system on the glacier triggered, alerting the authorities to a serious flood risk. 95 firefighters and 70 soldiers of the gendarmerie were mobilised, and an evacuation plan put into effect, involving the townspeople of St Gervais, Sallanches and Passy Domanc gathering at pre-arranged assembly points. Inspection of the glacier revealed that no collapse had taken place and the warning notice was lifted at 4:30am the same night. Studies revealed that between 35,000 and 50,000 cubic metres of water were present in the glacier.

By 2014 another build-up of a water pocket was discovered, and the Mayor of St. Gervais reported that, since its rediscovery, a total of 6 million euros had been spent in monitoring and pumping out water from the Tête Rousse glacier to protect the 3,000 inhabitants in the valley below.


* ^ A contemporary account by J Vallot, cited here, states over 200 deaths, although modern publications repeat a figure of only 175.


* ^ A B C D Vincent, C. (2010). "Origin of the Outburst flood from the Glacier
de Tete Rousse in 1892" (PDF). Journal of Glaciology. Retrieved 19 February 2016. * ^ Moran, Martin (July 2012). The 4000m Peaks of the Alps. The Alpine Club. p. 266. ISBN 9780900523663 . * ^ Griffin, Lindsay (1990). Mont Blanc
Mont Blanc
Massif Volume 1. London: Alpine Club. p. 22. ISBN 0900523573 . * ^ A B Peillex, Jean-Marc (December 2013). "Projections: Le journal d\'informations municipales des Saint-Gervolains" (PDF). www.saintgervais.com. Retrieved 24 February 2016. * ^ A B Vallot, Joseph (20 August 1892). "La Catastrophe de Saint-Gervais (12–13 Juillet 1892)". La Nature (1003). Retrieved 28 February 2016. * ^ A B C " France
drains lake under Mont Blanc
Mont Blanc
glacier". www.bbc.co.uk. 25 August 2010. Retrieved 28 February 2016. * ^ A B "Tête Rousse glacier collapses". www.chamonix.net. 17 August 2012. Retrieved 18 February 2016. * ^ LeRoux, Marc (13 August 1892). "La Catastrophe de Saint-Gervais : Théorie de l\'accident". La Science Illustrée (246). Retrieved 28 February 2016. * ^ A B Vincent, C.; Legchenko, A.; Descloitres, M.; Garambois, S. "Subglacial lake in the glacier of Tete Rousse ( Mont Blanc
Mont Blanc
area, France)" (PDF). www.risknat.org. Retrieved 28 February 2016. * ^ A B Legchenko, A.; Vincent, C.; Baltassat, J.M.; Girard, J.F.; Thibert, E.; Gagliardini, O.; Descloitres, M.; Gilbert, A.; Garambois, S.; Chevalier, A.; Guyard, H. (2014). "Monitoring water accumulation in a glacier using magnetic resonance imaging" (PDF). The Cryosphere. 8: 155–166. Bibcode :2014TCry....8..155L. doi :10.5194/tc-8-155-2014 . Retrieved 28 February 2016. * ^ "Poche d\'Eau du Glacier
de Tete Rousse". www.saintgervais.com. Retrieved 28 February 2016. * ^ "Catastrophes, avalanches, poches d\'eau". www.glaciers-climat.fr. Retrieved 23 February 2016. * ^ Clark, Tim (4 August 2010). "Flood risk in French Alps
after water pocket discovered under Mont Blanc
Mont Blanc
glacier". Daily Mail Online. Retrieved 23 February 2016. * ^ " Glacier
de Tête Rousse : la poche est réduite.. mais déjà pleine!". www.ledauphine.com. 17 July 2012. Retrieved 28 February 2016. * ^ "Press release (in French)" (PDF). www.haute-savoie.gouv.fr. 29 July 2013. Retrieved 24 February 2016. * ^ "Poche d\'Eau du Glacier
de Tete Rousse". www.saintgervais.com. January 2014. Retrieved 24 February 2016. * ^ Grassaud, Franck (3 July 2014). "Mont-Blanc: a new water pocket Tête Rousse glacier in Saint-Gervais (in French)". france3-regions.francetvinfo.fr. Retrieved 19 February 2016. * ^ Menegaux, Charlotte (20 August 2010). "La vallée de Saint-Gervais menacée par une poche d\'eau". www.lefigaro.fr. Retrieved 29 February 2016.


* Tête