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HISTORICAL NEWS SEARCH - Government of British Columbia

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was a contorted track over which a bulldozer smoothed the way for traffic that gathered at either side <strong>of</strong> the break.<br />

Telephone lines and cables were a tangled mass, at some spots partially buried in the heaved-up ground. Power lines<br />

were stretched to a taut breaking point. Town Council declared the land immediately adjacent to the slide a disaster<br />

area. Residents were warned that they remained there at their own risk. For a time on April 14 and early April 15, the<br />

big refuse burner <strong>of</strong> the A.L. Patchett & Sons Ltd. mill was threatened. Slide debris that slowly oozed out over the flat<br />

area around the burner was being kept away by a bulldozer. However, at times it pushed to within 20 ft. (6 m) <strong>of</strong> the<br />

base <strong>of</strong> the burner.<br />

By April 15, the land movement was noticeably less. By April 17, the movement had stopped. Crews were<br />

busy improving the road around Dragon Lake to allow traffic to be detoured that way and easing pressure on the hill.<br />

By the time the slide action had finished, the cabin and garage looked down on the highway that was once considered<br />

above the dwelling site. Early estimates placed the damage as high as $300,000, including the cost <strong>of</strong> relocating power<br />

and telephone lines, emergency highway work and personal property damage.<br />

--------------------------<br />

*1) The area had long been a trouble spot and slides had frequently been experienced before but never at such a<br />

magnitude (Cariboo Observer).<br />

October 1, 1958<br />

Event type: Rockslide.<br />

Precipitation: Not applicable.<br />

Source: The Citizen, October 1, 1958; The Vancouver Sun, October 1, 1958.<br />

On October 1, rocks came down onto the PGE line 30 mi. (48 km) north <strong>of</strong> Prince George, delaying Premier<br />

W.A.C. Bennett’s north bound inaugural train for two hours. The train carrying Premier Bennett and members <strong>of</strong> his<br />

cabinet to Dawson Creek and Fort St. John for the opening <strong>of</strong> the northern extension. Another source put the location<br />

<strong>of</strong> the slide as 90 mi. (144 km) north <strong>of</strong> Prince George (The Citizen, October 1, 1958). Crews spend most <strong>of</strong> the day<br />

trying to clear the tracks. J.S. Broadbent, general manager <strong>of</strong> the PGE, said the slide was “a minor occurrence – it<br />

happens all the time.” *1)<br />

-------------------------<br />

*1) He used much the same words in 1956, when Bennett’s inaugural train was delayed for eight hours by rocks along<br />

Howe Sound during the opening <strong>of</strong> the southern extension between Squamish-Vancouver (The Citizen, October 1,<br />

1958; The Vancouver Sun, October 1, 1958).<br />

October 19, 1958<br />

Event type: Glacial outburst flood.<br />

Precipitation: Not applicable.<br />

Source: Mathews 1965 (pp. 46-52).<br />

On October 19, Strohn Lake suddenly drained. This was the first time a sudden draining <strong>of</strong> the lake at the<br />

head <strong>of</strong> the Bear River valley was recorded (Mathews 1965). *1)<br />

-------------------------<br />

*1) The lake drained again between October 26-28, 1959, and on October 6, 1960 (Mathews 1965).<br />

October 27-November 2, 1958<br />

Event type: Flooding.<br />

Precipitation: Prince Rupert M. Circ (184.9 mm/7 days), October 27-November 2, 1958; Terrace (188.2 mm/7 days),<br />

October 27-November 2, 1958; Falls River (361.2 mm/7 days), October 27-November 2, 1958; Kitimat (329.0 mm/7<br />

days), October 27-November 2, 1958; Kemano (123.2 mm/2 days), October 28-29, 1958; Sandspit A (90.1 mm/3<br />

days), October 28-30, 1958.<br />

Source: Kitimat Kemano Ingot, November 5, 1958; The Northern Sentinel, October 30, 1958; Northwest Hydraulic<br />

Consultants Ltd. 1987; B.C. Ministry <strong>of</strong> Transportation and Highways. Granite Creek Flooding, Lakelse Lake Area.<br />

B.C. Ministry <strong>of</strong> Transportation and Highways, Terrace; Lloyd Johnstone, pers. comm. September 1993.<br />

The Kitimat River flooded the access roads under the bridge and the dike on the east side. The eroding river<br />

washed out some <strong>of</strong> the 13,000-V poles <strong>of</strong> the power line to the Service Centre. The road connecting the plant with the<br />

Service Centre was threatened. The Anderson Creek reached high water levels. The road on the Haisla Hill was<br />

closed. Run<strong>of</strong>f water washed through the gravel under the newly laid drainage flume. On November 29, the highway<br />

bridge at the end <strong>of</strong> the pavement washed out.<br />

Lower Granite Creek piled up gravel and debris, blocking <strong>of</strong>f the flow into the North Granite Creek. As a<br />

result, bank overflow occurred on the south side above this point, and the lower portion <strong>of</strong> the road from Highway 25<br />

to the lake washed out. One car was lost in this road washout. The properties <strong>of</strong> the federal Department <strong>of</strong> Fisheries,<br />

Lot 4 and adjoining Lot 5, were greatly endangered and damaged. Lakelse Lake reached the highest water level since<br />

1935, making it the fourth highest level this century (L. Johnstone, pers. comm.). According to local resident D.L.<br />

71

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