HISTORICAL NEWS SEARCH - Government of British Columbia
HISTORICAL NEWS SEARCH - Government of British Columbia
HISTORICAL NEWS SEARCH - Government of British Columbia
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mm). The highest month <strong>of</strong> precipitation was in May 1948 with 7.32 in. (185.9 mm) (The Interior News, January 3,<br />
1957).<br />
April 30, 1957<br />
Event type: Landslide<br />
Precipitation: Not applicable.<br />
Source: The Interior News, May 2, 1957.<br />
On April 30, a slide occurred on a side hill along the rail line 4 mi. (6.4 km) east <strong>of</strong> Moricetown. Fill<br />
saturated from spring run<strong>of</strong>f slid out from underneath the track. The roadbed slid downhill, leaving a gap<br />
approximately 40 ft. (12 m) long and 30 ft. (9 m) deep. The slide delayed the eastbound passenger train for 24 hours.<br />
May 18-20, 1957<br />
Event type: Spring run<strong>of</strong>f flooding.<br />
Precipitation: Not available.<br />
Source: The Interior News, May 23, 1957.<br />
On May 18-19, heavy prolonged rain and melting <strong>of</strong> high-level snow caused flooding and washouts in the<br />
Smithers area. Washed our roads and bridges disrupted traffic on Highway 16 east and west <strong>of</strong> Smithers. District side<br />
roads also suffered with bridges and culverts reported out on the Smithers-Babine Lake Road and Driftwood Creek<br />
Road. Babine Road was closed to traffic. Near Perow, the approach to the Lund Creek bridge washed out on May 19.<br />
Following temporary repairs, traffic was able to get through. The bridge at Harvey Ranch on Driftwood Creek and the<br />
Chapman Lake bridge on Babine Road washed out.<br />
On May 20, further damage resulted into further disruption <strong>of</strong> traffic. Highway 16 between Smithers-Prince<br />
Rupert washed out in at least 10 places, six <strong>of</strong> which between Terrace-Prince Rupert. Smaller cars were unable to get<br />
through to Terrace from Smithers due to washouts with up to 2.5 ft. (75 cm) <strong>of</strong> water flowing across the highway near<br />
Usk and Cedarvale.<br />
For a time, the Bulkley and Telkwa rivers threatened to flood a road at Telkwa. The rainfall stopped on May<br />
19. By the afternoon <strong>of</strong> May 20, the water level at Telkwa had dropped 6-8 ft. (1.8-2.4 m). Debris drifting down the<br />
Bulkley River threatened to take out the temporary piling for the new bridge at Telkwa. *1) Though the structure was<br />
damaged, little disruption was expected on further work on the bridge.<br />
Around May 19, a 200-ft. (60 m) stretch <strong>of</strong> newly built rail line toppled into the Peace River near Taylor.<br />
Apparently undermined by high water, a 100 ac. (40 ha) area <strong>of</strong> land collapsed, destroying a section <strong>of</strong> grade and<br />
blocking the road for a distance <strong>of</strong> 1,000 ft. (300 m). According to construction <strong>of</strong>ficials, the line could not be fully<br />
restored until the ground would have settled.<br />
----------------------<br />
*1) During the winter 1956-57, drifting ice had taken out the temporary structure. (The Interior News, May 23, 1957)<br />
October 16, 1957<br />
Event type: Severe scour.<br />
Precipitation: Not applicable.<br />
Source: Prince George Citizen, October 18, 1957; Kelsey 1958 (p. 86); Cohen 1992 (pp. 72-75).<br />
In October 16, the north end <strong>of</strong> the Peace River bridge at Taylor Flats just south <strong>of</strong> Fort St. John collapsed. *1) The<br />
northern span <strong>of</strong> the multi-million dollar bridge tore from its moorings and crashed into the river. The centre portion <strong>of</strong> the<br />
collapsed span was badly warped out <strong>of</strong> shape. A sag in the 930-ft. centre span <strong>of</strong> the two-lane bridge aroused fears that it<br />
also could drop into the Peace River. Possible causes were give as a shift in the shale bed <strong>of</strong> the river or due to the intensive<br />
industrial traffic. The oil industry was one <strong>of</strong> those most acutely affected by the bridge’s collapse.<br />
Earlier in 1957, a water line, which was strung underneath the structure, ruptured sending high-pressure water into<br />
the river. This scoured out gravel once again from beneath the north abutment. *2)<br />
---------------------------<br />
*1) This bridge, completed in August 1943, was the longest bridge on the Alaska Highway, at 2,130 feet (639 m) costing<br />
approximately $3.5 million. Because <strong>of</strong> the importance <strong>of</strong> the bridge, after the collapse the government <strong>of</strong> <strong>British</strong> <strong>Columbia</strong><br />
rushed another, more substantial structure to completion in January 1960 (Cohen 1992).<br />
*2) Early in 1948, it was discovered that scouring water undermined the north pier <strong>of</strong> the bridge making immediate<br />
repairs necessary (Cohen 1992).<br />
November 2-4, 1957<br />
Event type: Rockslides and snow avalanches.<br />
Precipitation: Prince Rupert (93.2 mm/3 days), November 2-4, 1957.<br />
Source: Prince Rupert Daily News, November 2 and 4, 1957; Terrace Omineca Herald, November 7, 1957; J.<br />
Mekechuck, pers. comm. 1989. CN Railway, Edmonton, Alta.<br />
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