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Foo Pass

Canton of Glarus geography stubsCanton of St. Gallen geography stubsGlarus–St. Gallen borderMountain passes of SwitzerlandMountain passes of the Alps
Mountain passes of the canton of GlarusMountain passes of the canton of St. Gallen
Foopass
Foopass

The Foo Pass (German: Foopass) is a mountain pass of the Glarus Alps, located on the border between the Swiss cantons of St. Gallen and Glarus, at an elevation of 2,223 m (7,293 ft). It crosses the col between the peaks of Foostock and Piz Sardona.The pass is traversed by a trail, which connects the village of Weisstannen, in the canton of St. Gallen at an elevation of 1,004 m (3,294 ft), with the village of Elm, in the canton of Glarus at an elevation of 977 m (3,205 ft). The trail forms part of the Alpine Pass Route, a long-distance hiking trail across Switzerland between Sargans and Montreux.The alpine pasture below the pass on the St Gallen side is notable for its marmot colony.

Excerpt from the Wikipedia article Foo Pass (License: CC BY-SA 3.0, Authors, Images).

Foo Pass
Krauchtalstrasse, Glarus Süd

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Geographical coordinates (GPS)

Latitude Longitude
N 46.942777777778 ° E 9.2381944444444 °
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Foopass

Krauchtalstrasse
8766 Glarus Süd
Glarus, Switzerland
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Rockslide of Elm
Rockslide of Elm

The rockslide of Elm (German: Der Bergsturz von Elm) was a mining disaster in Elm, Canton of Glarus, Switzerland which killed 115 people and destroyed 83 buildings on September 11, 1881. The catastrophe was partially caused by the mining of slate, beginning after 1870, by impoverished farmers who sought an additional source of income. Being inexperienced with proper mining techniques, they destabilized the rock face until the final catastrophe. The miners undercut the mountain face to a breadth of 180 m, and already in 1878 first rock movements occurred. A geological commission to examine the increasing number of rockfalls visited the scene shortly before the catastrophe, but did not find any indications of an impending disaster. The loud noise of the rockfalls, break-offs and fractures were already heard during the Sunday service on the morning of September 11, 1881. In spite of this, next to nobody left the dangerous area – in fact, many spectators went to the affected area or climbed to the nearby hamlet Düniberg on the opposing face of the valley in the hope of enjoying a better view of the spectacle. In the late afternoon, after two smaller rock slides, 10 million cubic meters (353 million cubic feet) of slate broke off, travelled 2 km (1.2 mi), and destroyed 90 hectares (220 acres) of land. The slate mine was also completely destroyed. The event and its causes were chronicled in the same year by the local priest Ernst Buss and the geologist Albert Heim in their publication "Der Bergsturz von Elm".