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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Source: Northern Sentinel, February 21, 1985; The Interior News, February 27, 1985; Jamieson and Geldsetzer 1996<br />
(p. 109; pp. 169-170); B.C. Ministry <strong>of</strong> Transportation and Highways 1980; Adam Charneski, pers. comm. July 1991,<br />
Line Foreman Alcan, Kitimat.<br />
At slide path Rockface, 69.6 km west <strong>of</strong> Terrace on February 18, a CNR train ran into a slide deposit at 50<br />
mph (80 km/h). The lights on the engine were broken and the train uncoupled.<br />
An avalanche wiped out a transmission tower between Kemano-Kitimat near the Kildala Pass, 24 km from<br />
Kemano on the south side <strong>of</strong> the Hanging Valley. *1) The slab type avalanche occurred at a steep 60% slope at the<br />
6,000 ft. (1,800 m) level. It jumped a ridge and spilled over and the windblast created by the massive snow flow<br />
knocked down the aluminum tower 124L. Pieces <strong>of</strong> the tower were carried away over a maximum horizontal distance<br />
<strong>of</strong> 950 ft. (285 m). The windblast also caused minor damage to steel members <strong>of</strong> adjacent towers 123R and 124R at an<br />
elevation <strong>of</strong> 740 m and knocked down trees on the uphill side <strong>of</strong> these towers (A. Charneski, pers. comm.). The single<br />
curcuit on the right was able to maintain the delivery <strong>of</strong> power. *2)<br />
In the five days prior to the avalanche, about 200 mm <strong>of</strong> precipitation had fallen in the area. This and<br />
previous snowfalls probably an approximately 190-cm deep unstable snowpack in the avalanche path. The avalanche<br />
starting zone, at 1,700 m, was on a northeast-facing slope with a 39 o incline and lee to the prevailing storm wind. After<br />
running down an open 31 o slope, the avalanche was deflected by a 50-m high ridge. It then moved over 400 m on<br />
gentle incline between 0-10 o along the opposite valley side, towards the powerline.<br />
Models <strong>of</strong> avalanche dynamics and the runout distance <strong>of</strong> the avalanche led to the conclusion that the<br />
avalanche speed at tower 124L was approximately 24 m/s (86.4 km/h). The avalanche snow was dry and probably had<br />
a deep powder component. The age <strong>of</strong> broken threes in the avalanche path suggested that an avalanche <strong>of</strong> similar<br />
magnitude had not occurred for close to 100 years. (Peter Schaerer In: Jamieson and Geldsetzer 1996).<br />
On February 22 at midnight, an avalanche on Onion Mountain near Smithers killed a snowmobiler. At just<br />
after midnight, it was snowing heavily. A number <strong>of</strong> snowmobilers were taking turns running up <strong>of</strong> one <strong>of</strong> its slopes.<br />
The victim, a 29-year old man, started up the slope and was traveling at high speed when hit by the avalanche. The<br />
slide was about 350 m wide and ran 400 m. Neither the victim nor his snowmobile were buried in the avalanche. But<br />
when the other members <strong>of</strong> the group found him, he had died <strong>of</strong> massive trauma. (Jamieson and Geldsetzer 1996).<br />
-----------------------------<br />
*1) For a distance <strong>of</strong> 15 km over Kildala Pass, the transmission line is split into two single, parallel circuits. The line<br />
on the right side (identified by R) is carried on steel lattice towers, and the line on the left (L) on towers built with<br />
aluminum tubing. The transmission line has a history <strong>of</strong> destructive avalanches. By January 26, 1955, avalanches had<br />
already destroyed three towers in Glacier Bowl at the south side <strong>of</strong> Kildala Pass on the line completed only the<br />
previous year. (Jamieson and Geldsetzer 1996).<br />
*2) In the following years, earth and steel deflectors were built at other exposed towers. On January 22, 1973, an<br />
avalanche destroyed tower 105L. Subsequently, placing strong steel breakers in front <strong>of</strong> them protected the legs <strong>of</strong><br />
towers 105L and 105R. On December 27, 1992, tower 113R near the top <strong>of</strong> Kildala Pass was damaged. (Jamieson and<br />
Geldsetzer 1996).<br />
March 1985<br />
Event type: Landslide potential.<br />
Precipitation: Not applicable.<br />
Source: Times Colonist, March 12, 1985.<br />
In March, Dinosaur Lake on the Peace River was closed to the public until further notice for all recreation<br />
and sport fishing. This followed a study on the movement <strong>of</strong> a landslide, which developed on the north-shore <strong>of</strong> the<br />
reservoir near the town <strong>of</strong> Hudson’s Hope. The slide had moved 5 m in the last four years. It was feared that if it would<br />
move rapidly into the water it could create waves in excess <strong>of</strong> 4 m. Depending on how fast the slide would move, the<br />
lake could be closed for up to five years.<br />
September 3-4, 1985<br />
Event type: Flooding.<br />
Precipitation: Prince Rupert M. Circ (57.4 mm/1 day), September 3, 1985; Prince Rupert A (52.2 mm/1 day),<br />
September 4, 1985.<br />
Source: The Daily News, September 12, 1985.<br />
Unusually heavy rains washed out the forms for the construction <strong>of</strong> the new Wolf Creek dam near Port<br />
Edward. Forms for the 5-m high and 13-m wide concrete dam had been set up and crews were ready to pour the<br />
concrete when the washout occurred. The forms lifted up and drifted against a tractor. Stikine Construction company<br />
lost about 62 man-hours as a result <strong>of</strong> the incident. Work on the project resumed on September 12.<br />
September 19-20, 1985<br />
Event type: Debris slides.<br />
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