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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Spring run<strong>of</strong>f caused the Fraser River at Prince George to rise to a record level <strong>of</strong> 25 ft. causing the city to<br />
flood. According to water level taken by J. Simonson, in 1911 the gauge at South Fort George reached a high mark <strong>of</strong><br />
18 ft. (Prince George Citizen, May 31, 1928).<br />
June 11, 1913<br />
Event type: Spring run<strong>of</strong>f flooding.<br />
Precipitation: Not applicable.<br />
Source: The Vancouver World, July 16, 1911.<br />
On June 11, Tète Jaune flooded due to the sudden rise <strong>of</strong> the Fraser River. Heavy rains during the previous few<br />
days caused a sharp rise in the water levels. In Main Street, the water was 6 ft. (1.8 m) deep and still rising. (The Vancouver<br />
World).<br />
March 31-April 2, 1912<br />
Event type: Severe storm.<br />
Precipitation: Ikeda Bay (68.6 mm/2 days), March 31-April 1, 1912; Swanson Bay (189.3 mm/2 days), March 31-April<br />
2, 1912; Prince Rupert (117.1 mm/2 days), April 1-2, 1912.<br />
Source: The Daily News, April 2, 3, and 4, 1912; The Evening Empire, April 1, 2, and 3, 1912.<br />
On April 1, Prince Rupert recorded 2.04 in. (51.8 mm) <strong>of</strong> rain and 3.18 in. (80.8 mm). On April 4, a<br />
“blizzard” dumped 7.5 in. (19.1 cm) <strong>of</strong> snow on Prince Rupert. The Vancouver-bound S.S. Chelohsin was badly<br />
damaged during the heavy gale. The ship was driven on the rocks in the Skeena Slough south <strong>of</strong> Prince Rupert.<br />
October 1-2, 10-11, 1913<br />
Event type: Landslide.<br />
Precipitation: Bella Coola (55.4 mm/2 days), October 1-2, 1913; Bella Coola (66.0 mm/2 days), October 10-11, 1913.<br />
Source: Bella Coola Courier, October 4 and 18, 1913.<br />
Bella Coola recorded a total rainfall <strong>of</strong> 8.11 in. (206.0 mm) for September. A landslide occurred 35 mi. (56<br />
km) up the valley above the Gibson Ranch during the first half <strong>of</strong> October. It damaged a portion <strong>of</strong> the wagon road,<br />
cutting <strong>of</strong>f the upper valley.<br />
October 29-November 3, 1913<br />
Event type: Rain-on-snow flooding.<br />
Precipitation: Bella Coola (58.7 mm/1 day), October 22, 1913; Masset (47.0 mm/1 day), November 3, 1913.<br />
Source: The Daily News, November 3, 1913; The Omineca Herald, November 7, 1913; The Morning Sun, November 3,<br />
1913.<br />
Three days <strong>of</strong> rain caused several large snowslides on Rocher de Boule near New Hazelton.<br />
In the Bella Coola area, incessant rains on snow caused the “most serious flood that the oldest settlers have<br />
ever known.” On October 29, the Neeleetsconnoy River and other streams started rising rapidly. By 3 p.m., large<br />
streams <strong>of</strong> water were running down the main streets. The river, which peaked at 6 p.m., seemed to have changed its<br />
course running through town at a depth <strong>of</strong> over 2 ft. (60 cm). The stream carried a horse and wagon engaged in rescue<br />
operations for 40 yd. (36 m) before becoming jammed in a pile <strong>of</strong> logs. Only with great difficulty the men and horse<br />
were extricated (Bella Coola Courier In: The Daily News).<br />
November 30-December 3, 1913<br />
Event type: Rain-on-snow flooding.<br />
Precipitation: Ikeda Bay (282.4 mm/4 days), November 30-December 3, 1913; Terrace (157.0 mm/3 days), December<br />
1-3, 1913.<br />
Source: The Omineca Herald, December 5, 1913; Varley 1981 (pp. 132-133).<br />
Debris slides and washouts interrupted the rail traffic between Terrace-Smithers. The train passengers were<br />
transferred to a special train. Foley, Welch & Stewart’s derrick and crew cleared a big landslide at Mile 125, 5 mi. (8<br />
km) east <strong>of</strong> Pacific. The slide was several feet high. Other damage consisted <strong>of</strong> a washout at Woodcock, a big slide<br />
just west <strong>of</strong> Sealy, and six small slides west and a big slide just east <strong>of</strong> the big tunnel between New Hazelton-Bulkley<br />
Canyon.<br />
Heavy rains caused the Kitimat River to flood roads near Kitamaat Village. The Anderson’s ranch along the<br />
west side <strong>of</strong> Kouwthpega (Anderson’s) Creek had its landing and boathouse carried downstream. (Varley 1981).<br />
December 8-9, 1913<br />
Event type: Debris flows.<br />
Precipitation: Ikeda Bay (247.0 mm/4 days), December 6-9, 1913; Prince Rupert (112.3 mm/1 day), December 8,<br />
1913; Terrace (38.1 mm/1 day), December 8, 1913.<br />
Source: The Daily News, December 8 and 9, 1913; The Omineca Herald, December 5, 12 and 19, 1913; Queen<br />
Charlotte Islander, December 10 and 17, 1913; The Interior News, December 13 and 20, 1913.<br />
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