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

On December 9, Prince Rupert reported 3.86 in. (98.0 mm) of rain and 1.35 in. (34.3 mm) on December 10. The rail line sustained heavy damage, interrupting the rail traffic for over two weeks. The train passengers were held up for a week and some interior points were running short on food supplies. Many mudslides occurred along the railroad as far east as Moricetown. *1) The big slide at the hill cut at Mud Creek required pile driving over the full distance. On the east side, 300 ft. (100 m) of the hill went out. A pile bridge was erected and two steam shovels had to be brought in to widen the cuts several hundred feet. At the big cut at Duncanon, a few miles east of Hazelton, mudslides and several small slides occurred at the lower part of the railroad. On the Queen Charlotte Islands a slide blocked the Nadu road. It was cleared by the provincial government. The storm on the night of December 8 caused some damage. The gasoline launch Johnnie, belonging to the Tingley Bros., broke from its mooring. It sustained considerable damage after being blown across the lake to Ship Island. ----------------------- *1) To avoid the “gumbo” slides, the railway company considered abandoning the present grade in favour of the surveyed Old Copper River route (The Daily News, December 8, 1913). February 24-28, 1914 Event type: Flooding. Precipitation: Ikeda Bay (273.2 mm/5 days), February 24-28, 1914; Prince Rupert (133.0 mm/3 days), February 25-27, 1914; Prince Rupert (65.0 mm/1 day), February 26, 1914. Source: The Daily News, February 26, 1914; The Evening Empire, February 25, 26, and 27, 1914. Prince Rupert reported 1.81 in. (46.0 mm) of rain on February 25, 1.57 in. (39.9 mm) on February 26, and 1.38 in. (35.1 mm) on February 27. The excavation job on the new Post Office site was flooded out. November 20-25, 1914 Event type: Rain-on-snow flooding and landslides. Precipitation: Ikeda Bay (237.3 mm/5 days), November 20-24, 1914; Prince Rupert (116.8 mm/4 days), November 21- 24, 1914; Terrace (147.0 mm/4 days), November 22-25, 1914. Source: The Omineca Herald, November 27, 1914; The Interior News, November 28, 1914; Varley 1981 (pp. 134-136 and 223). As a result of incessant rains on November 22 and 23, trains were blocked by slides east and west of Smithers. The Bulkley River rose significantly, carrying large quantities of trees and driftwood. Old-timers claimed this “the biggest rain on record here at this season.” For the week ending November 25, Hazelton reported 2.55 in. (64.8 mm) of rain. The heavy snowfall turned into rain, causing slides a few miles east of New Hazelton. The train traffic was interrupted, delaying the westbound train for 36 hours. Very warm weather, combined with two days of heavy rain, a 25 ft.-(7.5 m) tide, and a full moon, caused heavy flood damage near Kitamaat Village. Roads and the Anderson ranch were flooded. *1) The water came so high that it flooded the valley for miles around. The Kitimat River cut a whole swath of timber from the Hallet and Mitchell logging operation, 2 mi. (3.2 km) upstream from the Anderson ranch. A big logjam formed at the head of Kouwthpega (Anderson’s) Creek. The water was running wild down the low land just upstream. The backed-up river directed its flow westward through Little Klupa Creek (Varley 1981). ----------------------- *1) The southwestern corner of the Anderson ranch has changed drastically since. By 1952, Kouwthpega Creek cut west as far as the corner of the front lawn and had taken the cabin, the barn, and the entire barnyard (Varley 1981). March 16-19, 1915 Event type: Mudslide. Precipitation: Prince Rupert (92.8 mm/4 days), March 16-19, 1915; Terrace (28.2 mm/1 day), March 17, 1915; Ikeda Bay (92.2 mm/2 days), March 17-18, 1915. Source: The Omineca Herald, March 19, 1915. On March 17, just east of New Hazelton, the spring’s first major mudslide occurred. The passenger train was held up for 24 hours. Two ditchers were involved in clearing the slide. Winter 1915-1916 Event type: Fatal snow avalanche. Precipitation: Not applicable. Source: Anthony L’Orsa, pers. comm. June 12, 1995. During the winter 1915-16, a snow avalanche on the southeastern shoulder of Mount Cronin killed a man carrying mail for the Cronin mine. *1) --------------------------- *1) Old-timers named the avalanche track “Dead Man’s Gulch”. March 6-10, 1916 11

On December 9, Prince Rupert reported 3.86 in. (98.0 mm) <strong>of</strong> rain and 1.35 in. (34.3 mm) on December 10.<br />

The rail line sustained heavy damage, interrupting the rail traffic for over two weeks. The train passengers were held<br />

up for a week and some interior points were running short on food supplies. Many mudslides occurred along the<br />

railroad as far east as Moricetown. *1) The big slide at the hill cut at Mud Creek required pile driving over the full<br />

distance. On the east side, 300 ft. (100 m) <strong>of</strong> the hill went out. A pile bridge was erected and two steam shovels had to<br />

be brought in to widen the cuts several hundred feet. At the big cut at Duncanon, a few miles east <strong>of</strong> Hazelton,<br />

mudslides and several small slides occurred at the lower part <strong>of</strong> the railroad.<br />

On the Queen Charlotte Islands a slide blocked the Nadu road. It was cleared by the provincial government.<br />

The storm on the night <strong>of</strong> December 8 caused some damage. The gasoline launch Johnnie, belonging to the Tingley<br />

Bros., broke from its mooring. It sustained considerable damage after being blown across the lake to Ship Island.<br />

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

*1) To avoid the “gumbo” slides, the railway company considered abandoning the present grade in favour <strong>of</strong> the<br />

surveyed Old Copper River route (The Daily News, December 8, 1913).<br />

February 24-28, 1914<br />

Event type: Flooding.<br />

Precipitation: Ikeda Bay (273.2 mm/5 days), February 24-28, 1914; Prince Rupert (133.0 mm/3 days), February 25-27,<br />

1914; Prince Rupert (65.0 mm/1 day), February 26, 1914.<br />

Source: The Daily News, February 26, 1914; The Evening Empire, February 25, 26, and 27, 1914.<br />

Prince Rupert reported 1.81 in. (46.0 mm) <strong>of</strong> rain on February 25, 1.57 in. (39.9 mm) on February 26, and<br />

1.38 in. (35.1 mm) on February 27. The excavation job on the new Post Office site was flooded out.<br />

November 20-25, 1914<br />

Event type: Rain-on-snow flooding and landslides.<br />

Precipitation: Ikeda Bay (237.3 mm/5 days), November 20-24, 1914; Prince Rupert (116.8 mm/4 days), November 21-<br />

24, 1914; Terrace (147.0 mm/4 days), November 22-25, 1914.<br />

Source: The Omineca Herald, November 27, 1914; The Interior News, November 28, 1914; Varley 1981 (pp. 134-136<br />

and 223).<br />

As a result <strong>of</strong> incessant rains on November 22 and 23, trains were blocked by slides east and west <strong>of</strong><br />

Smithers. The Bulkley River rose significantly, carrying large quantities <strong>of</strong> trees and driftwood. Old-timers claimed<br />

this “the biggest rain on record here at this season.” For the week ending November 25, Hazelton reported 2.55 in.<br />

(64.8 mm) <strong>of</strong> rain. The heavy snowfall turned into rain, causing slides a few miles east <strong>of</strong> New Hazelton. The train<br />

traffic was interrupted, delaying the westbound train for 36 hours.<br />

Very warm weather, combined with two days <strong>of</strong> heavy rain, a 25 ft.-(7.5 m) tide, and a full moon, caused<br />

heavy flood damage near Kitamaat Village. Roads and the Anderson ranch were flooded. *1) The water came so high<br />

that it flooded the valley for miles around. The Kitimat River cut a whole swath <strong>of</strong> timber from the Hallet and Mitchell<br />

logging operation, 2 mi. (3.2 km) upstream from the Anderson ranch. A big logjam formed at the head <strong>of</strong> Kouwthpega<br />

(Anderson’s) Creek. The water was running wild down the low land just upstream. The backed-up river directed its<br />

flow westward through Little Klupa Creek (Varley 1981).<br />

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

*1) The southwestern corner <strong>of</strong> the Anderson ranch has changed drastically since. By 1952, Kouwthpega Creek cut<br />

west as far as the corner <strong>of</strong> the front lawn and had taken the cabin, the barn, and the entire barnyard (Varley 1981).<br />

March 16-19, 1915<br />

Event type: Mudslide.<br />

Precipitation: Prince Rupert (92.8 mm/4 days), March 16-19, 1915; Terrace (28.2 mm/1 day), March 17, 1915; Ikeda<br />

Bay (92.2 mm/2 days), March 17-18, 1915.<br />

Source: The Omineca Herald, March 19, 1915.<br />

On March 17, just east <strong>of</strong> New Hazelton, the spring’s first major mudslide occurred. The passenger train was<br />

held up for 24 hours. Two ditchers were involved in clearing the slide.<br />

Winter 1915-1916<br />

Event type: Fatal snow avalanche.<br />

Precipitation: Not applicable.<br />

Source: Anthony L’Orsa, pers. comm. June 12, 1995.<br />

During the winter 1915-16, a snow avalanche on the southeastern shoulder <strong>of</strong> Mount Cronin killed a man<br />

carrying mail for the Cronin mine. *1)<br />

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

*1) Old-timers named the avalanche track “Dead Man’s Gulch”.<br />

March 6-10, 1916<br />

11

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