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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October 26-27, 1976; Stewart A (112.7 mm/2 days), October 26-27, 1976; Kemano (158.5 mm/2 days), October 26-27,<br />
1976; Hartley Bay (162.0 mm/3 days), October 26-28, 1976; Ocean Falls (192.0 mm/2 days), October 27-28, 1976.<br />
Source: The Herald, October 27, November 3, 1976; The Daily News, October 27, 1976.<br />
Prince Rupert reported 110 mm <strong>of</strong> rain in 24 hours with 46-mph (74.0 km/h) winds. Two power transmission<br />
lines were damaged by slides, causing a 24-hour power blackout in Prince Rupert. A mudslide near Oliver Lake took<br />
out three power poles. The slide also stripped part <strong>of</strong> the hillside from the top <strong>of</strong> the mountain to across the road 1,500<br />
ft. (450 m) below. The October 29 issue <strong>of</strong> The Daily News shows a photograph <strong>of</strong> the slide at Oliver Lake.<br />
In Prince Rupert, the Senior Highschool sustained $5,000 damage. Its basement boiler room was submerged<br />
under 4 ft. (1.2 m) <strong>of</strong> water. The Kindergarten room in the King Edward Elementary School was flooded. The Seal<br />
Cove School lost two furnaces as a result <strong>of</strong> water damage. Basements in homes were flooded because <strong>of</strong> poor<br />
drainage and backed-up run<strong>of</strong>f ditches. The Mountain View trailer court was flooded with water at “mid calf height.”<br />
The road along the lower areas <strong>of</strong> the town was under water. On Conrad Street, a small slide occurred in Mrs. Bond’s<br />
yard. Approximately 60 ft. (18 m) <strong>of</strong> yard, including a reinforced rock and concrete wall, slid down to the street<br />
below.<br />
In Port Edward, a slide cut <strong>of</strong>f the electric power and the main water supply. Parts <strong>of</strong> Port Edward were<br />
without power on October 26. On October 27, a slide came down just before the Cassiar Cannery, cutting <strong>of</strong>f power to<br />
some 50 people. Falls River reported 447.0 mm in the 10 days between October 25-November 3 (Environment Canada<br />
1991). In Terrace, Spring Creek flooded near Dutch Valley. The water rose above the footbridge just below the<br />
logjam.<br />
November 1-3, 1976<br />
Event type: Flooding and debris slides.<br />
Precipitation: Hartley Bay (101.1 mm/2 days), November 1-2, 1976; Tasu Sound (234.2 mm/3 days), November 1-3,<br />
1976; Sewell Inlet (261.4 mm/3 days), November 1-3, 1976; Falls River (117.1 mm/2 days), November 2-3, 1976;<br />
Prince Rupert M. Circ (129.0 mm/2 days), November 2-3, 1976; Terrace (36.0 mm/2 days), November 2-3, 1976;<br />
Stewart A (153.9 mm/2 days), November 2-3, 1976; Sandspit A (42.2 mm/1 day), November 3, 1976; Prince Rupert<br />
(69.9 mm/1 day), November 3, 1976.<br />
Source: The Daily News, November 3, 4 and 5, 1976; The Sentinel, November 12, 1976.<br />
In Prince Rupert, a heavy rainstorm with over 4 in. (101.6 mm) in 24 hours caused severe erosion and flood<br />
damage. The recently completed Comox Mobile Home Park was flooded with up to 1 ft. (30 cm) <strong>of</strong> water. An area<br />
covering about 5,000 ft. 2 (465 m 2) , including at least three trailer pads, was under water. On November 3, two debris<br />
slides came down on the Port Edward Cannery Road. One slide happened at Phelan and the second one just north <strong>of</strong><br />
the old Inverness Cannery Road.<br />
On November 2, an eastbound freight train hit a rockslide 1 mi. (1.6 km) west <strong>of</strong> Usk. Ten cars derailed and<br />
one <strong>of</strong> the three engines went into the Skeena River. There were no injuries.<br />
The Stewart-Meziadin road was closed by extensive flood damage. The bridges across the Hanna and<br />
Tintina creeks were restricted to 50% weight load. In Stewart, the downtown area was flooded with 1 ft. (30 cm) <strong>of</strong><br />
water. Many residents had their basements flooded with up to 4 ft. (1.2 m) <strong>of</strong> water; others had their property<br />
completely inundated.<br />
Between November 1-3, slides occurred in the Rennell Sound area. The weather station at Gospel Point<br />
recorded 197.6 mm <strong>of</strong> rain in three days. On November 3, MacMillan Bloedel reported about 10 slides at Dinan Bay.<br />
The weather station at Sewall Masset Inlet recorded 17.8 mm <strong>of</strong> rain in the previous 24 hours and a total <strong>of</strong> 138.7 mm<br />
during the previous 10 days. On November 3, Crown Forest Products reported a slide near Sandspit. During the<br />
previous 24 hours, Sandspit had recorded 42.2 mm <strong>of</strong> rain and a total <strong>of</strong> 141.7 mm during the previous 10 days.<br />
December 1976<br />
Event type: Slide potential.<br />
Precipitation: Not applicable.<br />
Source: The Vancouver Sun, December 4 and 16, 1976.<br />
On December 3, BC Hydro chairman Robert Bonner reported that an enormous slide, 80 % bigger than the<br />
Downie slide on the <strong>Columbia</strong> River, was creeping into the reservoir behind the W.A.C. Bennett Dam. BC Hydro<br />
engineers noted that “safety cannot be guaranteed.” According to Larry Peterson <strong>of</strong> Fort St. John, spokesman for the<br />
Peace Valley Environmental Association and speaking for concerned Peace River farmers, the Brantham Ridge slide,<br />
located above a failure zone 20 mi. (32 km) upstream from the dam, contains an estimated 1.8 billion cubic yards (1.38<br />
billion m 3 ) <strong>of</strong> material. *1)<br />
Peterson said that the situation was particularly critical in view <strong>of</strong> BC Hydro’s intention to divert the<br />
McGregor River from the Fraser drainage system to flow north into 410,000-ac. (164,000 ha) Williston Lake. The<br />
McGregor diversion would put 20% more water in the reservoir and add to the pressure on the slide area. *2)<br />
A report by the hydro-electric design division, dated July, 1974, said that the monitoring <strong>of</strong> the unstable<br />
Brantham Ridge area showed the slide, which extends for 4 mi. (6.4 km) along the shore <strong>of</strong> Williston Lake, had moved<br />
2 ft. (60 cm) closer to the reservoir since 1968.<br />
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