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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oom on the top floor <strong>of</strong> the residence <strong>of</strong> Frank Morris were torn out. “Everything was over in less than a second,”<br />
Morris said. At about 3 p.m., Imperial Oil Co.’s large tanker R.J. Hanna broke loose from its moorings.<br />
It appeared that most <strong>of</strong> the damage was not done by the direct force <strong>of</strong> the “sou’wester” but by a series <strong>of</strong><br />
whirlwinds. The sidewalk between the Post Office and Glennie’s store was blown across the street in a direct easterly<br />
direction. The sidewalks on 2 nd Avenue near the B.C. Undertakers were hurled in a westerly direction, while the<br />
overhead crossing at the railway station was blown directly north. This would lead to suppose the storm was cyclonic<br />
in nature, the centre being some distance from Prince Rupert (The Daily News, February 11, 1924).<br />
August 23-26, 1924<br />
Event type: Flooding.<br />
Precipitation: Bella Coola (196.7 mm/4 days), August 23-26, 1924.<br />
Source: The Daily News, August 27, 1924; Kopas 1970 (p. 266).<br />
In 1924, there was a series <strong>of</strong> three floods on the Bella Coola River. Kopas (1970) notes the first one<br />
occurred in August, which “contrary to all laws <strong>of</strong> nature, tore up the town. The Bella Coola River flooded, and the<br />
Necleetsconnoy brought down huge batteries <strong>of</strong> trees and rocks which it hurled agaist the bridges, buildings and<br />
roads.” (Kopas 1970). Starting August 24, floodwaters washed out a number <strong>of</strong> buildings, leaving many <strong>of</strong> the settlers<br />
isolated. After one <strong>of</strong> the bridges washed away, access to the wharf was cut <strong>of</strong>f.<br />
Only a short time earlier, there had been a flood that did much damage in the valley. At that time it was<br />
suggested that the village should be moved to the other side <strong>of</strong> the river. This was to prevent future isolation, as the<br />
bridge was likely to be washed out at any time when the water would rise again.<br />
December 9-13, 1924<br />
Event type: Flooding.<br />
Precipitation: Ocean Falls (238.4 mm/5 days), December 9-13, 1924; Aiyansh (24.4 mm/1 day), December 10, 1924;<br />
Bella Coola (159.8 mm/3 days), December 11-13, 1924.<br />
Source: Kopas 1970 (p. 266); Tempest 1974.<br />
According to records kept by the B.C. Ministry <strong>of</strong> Transportation and Highways, a moderate flood occurred<br />
on the Bella Coola River (Tempest 1974).<br />
This was probably the third <strong>of</strong> a series <strong>of</strong> floods on the Bella Coola River that Kopas mentions in his book<br />
“Bella Coola.” (Kopas 1970)<br />
December 2-7, 1925<br />
Event type: Flooding.<br />
Precipitation: Ocean Falls (430.9 mm/4 days), December 2-5, 1925; Terrace (53.1 mm/1 day), December 5, 1925;<br />
Anyox (188.0 mm/3 days), December 4-6, 1925; Aiyansh (154.2 mm/4 days), December 4-7, 1924;<br />
Source: File 35-40-14 Letter January 12, 1926, C. L. Dimock (Ass. Dist. Eng. Smithers) to G. C. Mackay (Dist. Eng.<br />
Prince Rupert). B.C. Ministry <strong>of</strong> Transportation and Highways, Terrace, B.C.<br />
Early December extreme high water took out the Cedar River bridge No. 40. The crib on the north side<br />
became undermined and the rock fill washed out.<br />
January, 1926<br />
Event type: Glacial outburst flood.<br />
Precipitation: Not applicable.<br />
Source: Marcus 1960.<br />
In January, a glacial outburst flood occurred on Tulsequah Lake. The unusual winter outburst flood was<br />
attributed to an exceptionally warm winter preceded by heavy autumn rains. An early prospector reported it to George<br />
Bacon <strong>of</strong> Tulsequah. The prospector stated that floodwaters rose 12 ft. (3.6 m) and that huge ice blocks were carried<br />
many miles downstream. It was not known whether this was a true glacial outburst flood, but climatic data seem to<br />
corroborate the statement. The normally small winter discharge and/or frozenness <strong>of</strong> the Taku River also lend<br />
credence to the story (Marcus 1960).<br />
February 8-10, 1926<br />
Event type: Flooding and landslides.<br />
Precipitation: Terrace (106.4 mm/3 days) February 8-10, 1926; Prince Rupert (36.1 mm/2 days), February 8-9, 1926.<br />
Source: The Terrace News, February 8-9, 1926; File 35-90-34 Letter, March 12, 1926, Dist. Eng. Prince Rupert to C.<br />
L. Dimock (Ass. Dist. Eng.). B.C. Ministry <strong>of</strong> Transportation and Highways, Terrace.<br />
Recent heavy rains caused damage to roads in the Terrace-Kitwanga area. Slides occurred on the Hodkin’s<br />
Road and on the hill at Terrace.<br />
Ca. 1927-1930<br />
Event type: Glacial outburst flood.<br />
19