Sunday, 18 January 2015

Wellington, Washington avalanche









The Wellington avalanche was the worst avalanche, measured in terms of lives lost, in the history of the United States.



For nine days at the end of February 1910, the little town of Wellington, Washington was assailed by a terrible blizzard. Wellington was aGreat Northern Railway stop high in the Cascades, on the west side of the old Cascade Tunnel, under Stevens Pass. As much as a foot ofsnow fell every hour, and, on the worst day, 11 feet (340 cm) of snow fell. Two trains, a passenger train and a mail train, both bound fromSpokane to Seattle, were trapped in the depot. Snow plows were present at Wellington and others were sent to help, but they could not penetrate the snow accumulations and repeated avalanches along the stretch of tracks between Scenic and Leavenworth.
Late on February 28, the snow stopped and was replaced by rain and a warm wind. Just after 1 a.m. on March 1, as a result of a lightning strike, a slab of snow broke loose from the side of Windy Mountain during a violent thunderstorm. A ten-foot high mass of snow, half a mile long and a quarter of a mile wide, fell toward the town. A forest fire had recently ravaged the slopes above the town, leaving very little to impede the avalanche.
The avalanche missed the Bailets Hotel (which also housed the town's general store and post office), but hit the railroad depot. Most of the passengers and crew were asleep aboard their trains. The impact threw the trains 150 feet downhill and into the Tye River valley. Ninety six people were killed, including 35 passengers, 58 Great Northern employees on the trains, and three railroad employees in the depot. Twenty-three passengers survived; they were pulled from the wreckage by railroad employees who immediately rushed from the hotel and other buildings where they had been staying. The work was soon abandoned; it was not until 21 weeks later, during late July, that it was possible for the last of the bodies to be retrieved. This was not the only avalanche in the region that winter. Three days later, 63 railroad workers were killed in an avalanche nearby in British Columbia.

 Frank Slide


The Frank Slide was a rockslide that buried part of the mining town of Frank, Northwest Territories,[nb 1] Canada, on the morning of April 29, 1903. It occurred at 4:10 am, when over 82 million tonnes (90 million tons) of limestone rock slid down Turtle Mountain within 100 seconds, obliterating the eastern edge of Frank, the Canadian Pacific Railway line and the coal mine. It was one of the largestlandslides in Canadian history and remains the deadliest, as between 70 and 90 of the town's residents were killed, most of whom remain buried in the rubble. Multiple factors led to the slide. Turtle Mountain's formation left it in a constant state of instability, leading area Native tribes to call it, "the mountain that moves". Coal mining operations may have weakened the mountain's internal structure, as did a wet winter and cold snap on the night of the slide

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