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HISTORICAL NEWS SEARCH - Government of British Columbia

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Precipitation: Nass Camp (38.6 mm/1 day), December 7, 1980; Stewart A (163.7 mm/5 days), December 7-11, 1980;<br />

Falls River (265.6 mm/6 days), December 7-12, 1980; Salvus Camp (209.0 mm/4 days), December 7-10, 1980; Falls<br />

River (190.8 mm/3 days), December 8-10, 1980; Ocean Falls (251.0 mm/2 days), December 9-10, 1980; Bella Coola<br />

(320.4 mm/7 days), December 9-15, 1980; Prince Rupert (184.1 mm/3 days), December 8-10, 1980; Kitimat 2 (424.4<br />

mm/8 days), December 8-15, 1980; Tasu Sound (173.4 mm/5 days), December 10-14, 1980; Sewell Inlet (258.9 mm/5<br />

days), December 10-14, 1980; Hartley Bay (511.8 mm/6 days), December 10-15, 1980; Pallant Creek (176.8 mm/5<br />

days), December 10-14, 1980; Ocean Falls (363.4 mm/3 days), December 13-15, 1980; Kemano (93.1 mm/2 days),<br />

November 14-15, 1980.<br />

Source: Terrace-Kitimat Daily Herald, December 17, 1980; Northern Sentinel, December 11 and 18, 1980; The<br />

Province, December 18 and 19, 1980; January 7, 1981; Times Colonist, December 15 and 17, 1980; B.C. Ministry <strong>of</strong><br />

Transportation and Highways 1982 (p. 339); Environment Canada 1988; Environment Canada 1991.<br />

In mid-December a heavy snowfall <strong>of</strong> over 1,000 (100 cm?) cm occurred in a 24-hour period near Stewart. It<br />

resulted in avalanches releasing and covering about 2 km <strong>of</strong> highway in the Bear Pass area. Single-lane traffic was<br />

restored after a 10-hour closure. (B.C. Ministry <strong>of</strong> Transportation and Highways, Terrace, 1982)<br />

The Bella Coola area was hit with severe flooding caused by a combination <strong>of</strong> heavy rains and unseasonably<br />

warm temperatures melting snowcaps <strong>of</strong>f mountains on either side <strong>of</strong> the valley. Late on December 9, the area’s only<br />

airstrip, 21 km east <strong>of</strong> Bella Coola at Hagensborg, was submerged.<br />

Preliminary estimates put the damage at up to $5 million. According to Highways minister Alex Fraser, this<br />

included about $1 million damage to watercourses, and “$500,000 or better” to the highway system. Damage to homes<br />

was estimated at up to $3 million. The damage estimate for repair and bank protection work was estimated at<br />

$500,000. Environment minister Stephen Rogers promised financial aid to residents affected by flooding. Two nearby<br />

logging camps sustained an additional estimated damage <strong>of</strong> $1 million. *1)<br />

On December 9, the Bella Coola River broke its banks, carving out new channels in several locations. Over<br />

60 families had to leave their homes in the low-lying subdivisions east <strong>of</strong> Bella Coola. Thirty homes sustained flood<br />

damage and one house was swept away. Elsewhere it was reported that more than 40 families were evacuated and 46<br />

homes flooded, 10 <strong>of</strong> which severely.<br />

Highway 20, the only highway link to the remote community, sustained an estimated $1 million and was<br />

closed. Three bridges were closed and a fourth was teetering. The Bella Coola airport, closed due to mass flooding,<br />

reopened on December 17.<br />

The Nusatsum River flooded the rock dyke that was built in September 1980 and wiped out a house. The<br />

river cut a new channel through the Satterwhite home to a depth <strong>of</strong> about 2 m. The dyke had been built after a previous<br />

flood submerged the main floor <strong>of</strong> the house.<br />

On December 16, the Bella Coola River above Burnt Bridge Creek recorded a maximum instantaneous<br />

discharge <strong>of</strong> 725 m 3 /s and a maximum daily discharge <strong>of</strong> 701 m 3 /s. On the same day the Salloompt River near<br />

Hagensborg recorded a maximum instantaneous discharge <strong>of</strong> 241 m 3 /s and a maximum daily discharge <strong>of</strong> 141 m 3 /s,<br />

both these being extremes for the period <strong>of</strong> record (Environment Canada 1991). With colder temperatures on<br />

December 17, water levels receded dramatically. Though still beyond its banks, the Bella Coola River was expected to<br />

be in it original channel on December 18.<br />

For Isabel Edwards, 75, who had lived in the Bella Coola River valley for 48 years, this was just another in a<br />

long series <strong>of</strong> floods. *2) Her house, built in 1910, miraculously escaped damage. But floodwaters took out her<br />

driveway, all the topsoil <strong>of</strong> the just plowed hayfield, and left her with a debris-covered lawn.<br />

Two logging camps near Owikeno Lake, 145 km south <strong>of</strong> Bella Coola, were wiped out when the lake level in<br />

the lake rose 6 m. On December 16, Owikeno Lake at Rivers Inlet recorded a maximum instantaneous water level <strong>of</strong><br />

5.074 m and an estimated maximum daily water level <strong>of</strong> 4.870 m (Environment Canada 1988). The Owikeno Indian<br />

Reserve, a community <strong>of</strong> 55 inhabitants was threatened. One family was evacuated.<br />

According to preliminary findings, the December 1980 flooding caused a loss <strong>of</strong> at least 50% <strong>of</strong> the salmon<br />

in the Kitimat River. (The Province, January 7, 1981).<br />

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

*1) The provincial government agreed to provide $2 million for homes damaged by the flooding and $1 million to<br />

repair watercourses and $500,000 to repair Highway 20. Cabinet also earmarked $500,000 to cover flood damage<br />

elsewhere in the province.<br />

*2) The previous peak flood had occurred in 1968.<br />

December 16-17, 1980<br />

Event type: Icejam flooding.<br />

Precipitation: Not applicable.<br />

Source: The Citizen, December 17, 18 and 19, 1980; The Province, December 18, 1980; Times Colonist, December 19, 1980.<br />

On December 17, a 5-km long icejam in the Fraser River near Penny, about 90 km east <strong>of</strong> Prince George,<br />

backed up the water and caused flooding. Ice flows plugged sloughs and creeks and began to build up on gravel banks.<br />

The flooding started during early morning with the river rising 30 cm an hour.<br />

139

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