|Glacier du Giétro|
|Area||5.168 km2 (1.995 sq mi)|
|Length||4.45 km (2.77 mi)|
The Giétro Glacier or Giétroz Glacier (French: Glacier du Giétro) is a 4 km long valley glacier located in south-western Switzerland. The 1818 Giétro Glacier catastrophe, which led to lake outburst flood, is one of the most famous and most disastrous historical cases in the Swiss Alps.
The Giétro Glacier lies on the northern side of the Pennine Alps in the Swiss canton of Valais. It is located in the upper Bagnes Valley, south of Martigny and Verbier. The length of the glacier is 4.55 km (1979) and its area is 5.85 km2 (1979).
The glacier is fed by the snows of Mont Blanc de Cheilon (3,870 m) and La Ruinette (3,875 m). On the upper part, the glacier is relatively flat. It descends to the north on the side of Mont Rouge du Giétro and then curves to the west between Le Pleureur and Mont Rouge. On the lower part, the glacier reaches a steepness of 40% forming a large number of crevasses. The terminus is located at about 2,600 metres. Part of the glacier is linked to the Cheilon Glacier through the Col du Cheilon (3,243 m). The water generated by the glacier ends in the Lake Mauvoisin (artificial lake) and then reaches the Dranse de Bagnes, a tributary of the Rhone.
The Giétro Glacier is known to have caused many deaths in the valley during historical times. A first glacial lake outburst flood was recorded in 1595, causing 140 deaths. More recently in 1818 a similar lake outburst flood occurred killing 44 people. In the latter case a hole was drilled through the glacier to limit the level of waters.
After an increase of the glacier during the "Year Without a Summer", an ice cone started to form in 1816 in the valley. It was created by the accumulation of the falling seracs of the terminus. A lake was formed but it emptied on 27 May 1817 without causing any fatalities. In April 1818 the lake measured about 2 km in length. On 10 May 1818, the engineer Ignaz Venetz was called by the canton. To stop the rapid rise of waters, he decided to drill a hole through the ice. The work began one day later. A tunnel was drilled from the two sides, about 20 metres above the level of the lake. An avalanche of ice occurred on 18 May but without any casualties. A secondary tunnel was then drilled for safety reasons. A week later the level of the lake reached 10 metres below the tunnel. On 27 May an enormous piece of ice detached itself from the cone in the lake and floated to the surface while making terrible noise; everybody escaped. They went back to work two days later. The 198 metre-long hole was completed on 4 June. Other large pieces of ice detached from the cone and floated back. The waters finally reached the level of the hole on 13 June, 22:00. They continued to rise until 14 June, when the level of the lake began to fall because of the erosion of the hole by the waterfall. Some water also ran out from the base of the cone. Only two men stayed in place; Venetz warned the inhabitants of the valley of the danger. On the morning of 16 June, terrible noises and violent detonations were heard. The cone began to crack. A group of British tourists and a drawer from Lausanne visited the place with Venetz. In the afternoon, Venetz and the workers escaped to the heights of Fionnay.
Finally, at 16:30, the dam broke and 18 million m3 of water invaded the valley. Half an hour later the lake was empty. The flood reached the village of Bagnes 10 minutes later; the alert was given to Martigny before 18:00, but too late. The wave invaded Martigny-Bourg a few minutes later. The rise of the waters was observed along the Rhone, at 19:00 in Saint-Maurice and at 23:00 on Lake Geneva.