| Frank Slide |
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| natural disasters in alberta | |
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| 1903 natural disasters | |
| 1903 in canada | |
| provincial historic sites of alberta | |
| frank slide interpretive centre | |
| SHOPPER'S DELIGHT | |
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The Frank Slide is a natural Landslide feature in the southern Rocky Mountains of Canada , and a significant historical event in western Canada. Frank, Alberta is a coal mining town in the Crowsnest Pass , Alberta (formerly Northwest Territories ). On April 29, 1903, at 4:10 a.m., 82 million tonnes (30 million cubic meters) of limestone crashed from the summit of Turtle Mountain and covered approximately three square kilometers of the valley floor. The slide dammed the Crowsnest River and formed a small lake, covered 2km of the Canadian Pacific Railway, destroyed most of the coal mine's surface infrastructure, and buried seven houses on the outskirts of the sleeping town of Frank, as well as several rural buildings. Frank was home to approximately 600 people in 1903; of the roughly 100 individuals who lived in the path of the slide, more than 70 were killed. The town was evacuated, but people were soon allowed to return and both the mine and the railway were back in operation within a month. The town of Frank continued to grow, until a report on the mountain’s stability resulted in the province ordering the closure of the south part of the town in 1911. Studies and monitoring continue today. The Frank Slide was designated a Provincial Historical Resource in 1977, and in 1985 a major interpretive centre opened in the town of Frank that describes the slide and the coal-mining history of the area. GEOLOGY Turtle Mountain is an anticline of Paleozoic Rundle Group carbonates thrust over weaker Mesozoic clastics and coals. Summit fissures at the apex of the anticline likely allowed water to infiltrate and weaken the slightly-soluble carbonates within the mountain face, while the supporting underlying clastics were undermined by valley glaciation followed by erosion from the Crowsnest River. The slide removed the top of Turtle Mountain, leaving a present elevation of 2,109 metres (6,920 feet) for the north peak and 2,200 metres (7,217 feet) for the south peak. The primary cause of the slide was the mountain's unstable structure, although severe spring weather conditions, underground coal mining activity, and an earthquake on the Aleutian Islands in 1901 may have contributed. HISTORICAL NOTES
REFERENCES Anderson, Frank W. ''The Frank Slide Story''. Frontier Books, 1968. Kerr, J. W. ''Frank Slide''. Barker, 1990. ''Crowsnest and its People''. Crowsnest Pass Historical Society, 1979. ''On the Edge of Destruction'' National Film Board of Canada, ID 153C0103256, 2003. EXTERNAL LINKS
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