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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On November 22, a derailment occurred at Mile 43 at the portal of the tunnel just east of New Hazelton. A ditcher was knocked off a flatcar, killing fireman W.J. Smith and injuring engineer G.H. Mogden. Both men were from Smithers. They were returning from clearing a slide on the main line in the Bulkley Canyon. The westbound passenger train was delayed for seven hours. The rail line reopened on November 25 after a two-day closure. On November 24, the Skeena River was reported to be at the June flood level. The Kispiox and Bulkley rivers reached high water levels. Two small 20-ft. (6 m) long bridges over the Kispiox River washed out and had to be replaced. A family at Mile 22 along the Kispiox River had to be evacuated because of the high water and some farm animals were lost. On November 25, the Bulkley River at Quick recorded a maximum daily discharge of 575 m 3 /s (Environment Canada 1991). In the Kalum District, roads and bridges were damaged. The Kalum Lake Road sustained heavy damage. Glacier Creek had dammed up and flooded the road at Mile 14. The road between Mile 14-Mile 16 was almost impassable. Kitsequecla bridge No. 61 was undermined again after temporary repairs had been made two weeks previous. The cost to replace Clear Creek bridge, which went out, was estimated at $250; the replacement cost of Cedar River bridge was estimated at $7,000-8,000. The Douglas Creek bridge No. 31 had to be rebuilt. Hall Creek bridge No. 173, with one end floating, was expected to go out with the next high water. The cutbank on the west side of Whiskey Creek was completely washed out. The road between Nash-Skeena Crossing was blocked. The cribbing at Porphyry Creek caved in. The filling was expected to take four to five days (A.A. McLean). In the Smithers-Telkwa area, some slides occurred on the Aveling Coal Road. The Telkwa River changed its course, requiring another 150 ft. (45 m) of cribbing. At the Smithers bridge about 600 lineal ft. (180 m) of cribbing was required on the Bulkley Hill on the Telkwa side across the river. -------------------------- *1) In November 1933, Terrace had an all-time record rainfall to date of 25.53 in. (648.5 mm) (The Daily News, December 2, 1933). November 23-December 2, 1933 Event type: Flooding and snow avalanches. Precipitation: Falls River (385.9 mm/9 days), November 23-December 1, 1933; Kitimat Mission (447.2 mm/10 days), November 23-December 2, 1933; Ocean Falls (145.3 mm/1 day), November 29, 1933; Swanson Bay (336.5 mm/3 days), November 29-December 1, 1933; Kitimat Mission (343.0 mm/5 days), November 29-December 2, 1933; Aiyansh (43.2 mm/1 day), November 30, 1933; Terrace (187.7 mm/2 days), November 30-December 1, 1933; Falls River (187.4 mm/2 days), November 30-December 1, 1933; Terrace (116.0 mm/1 day), December 1, 1933. Source: The Terrace News, December 6, 1933; The Omineca Herald, November 29 and December 6, 1933; The Daily News, December 1 and 2, 1933; Evening Empire, November 28 and 30, December 1 and 2, 1933. Heavy rain occurred all along the coast with unusual stormy weather on the Queen Charlotte Islands and snowstorms in Stewart and Anyox. The S.S. Catala reported experiencing squally weather all the way north. The winds were particularly strong on the west coast of the Queen Charlotte Islands. The vessel Beatrice H on her regular weekly trip had difficulty reaching the mining camps. Prince Rupert reported a record rainfall of 25.53 in. (648.5 mm) for November; Terrace received 15 in. (381.0 mm) during that month. The heavy rain caused flooding and property damage in the Terrace area. The Thornhill bridge on the Lakelse Road was flooded. A slide on the hill on Remo Road buried about half an acre of cultivated land on the Joe Cook Ranch. In Terrace, a plugged culvert on Lakelse Avenue caused the municipal reservoir to overflow and flood the street near the Public Works garage. The basement of the Philbert Hotel was flooded with 4 ft. (1.2 m) of water. On December 1, the telegraph lines east and west of Terrace and also the Anyox line went down, cutting the telegraphic communications. Lines were still down on December 2. A small culvert on the Kispiox road got plugged and flooded the road. On the rail line between Prince Rupert-Terrace, an eastbound train from Prince Rupert was delayed due to slide conditions on the lower Skeena River. On December 1, snowslides were reported on the line at Kwinitsa. The rail traffic was reported back to normal on December 2. December 18-20, 1933 Event type: Icejam flooding. Precipitation: Not applicable. Source: The Vancouver Daily Province, December 20, 1933. Overnight December 18-19, an icejam on the Nechako River caused the river to overflow in a number of places. Near Prince George, the CNR rail yard was flooded with 2 ft. (60 cm) of water and sections of roadbed washed out. The heavy ice created a dam near the mouth of the Nechako River. A number of families living in what was known as the railway cache, between the railway yards and the river, were marooned. The water rose so rapidly that their escape was cut off. A woman was marooned on the upper floor of a farmhouse on the north bank of the Nechako 26

River after floodwaters completely surrounded the house. Alone at the time and though her cries for help could be heard across the river in central Fort George, she could not be located in the darkness. On December 20, ice jammed at Engen in the canyon forcing water to break through and flooding low lying land and the home of Harry Worthington. This family escaped with great difficulty to the schoolhouse 0.75 mile (1.2 km) away. A number of sheep, pigs and large cattle drowned. January 24-27, 1934 Event type: Rain-on-snow and icejam flooding. Precipitation: Ocean Falls (393.0 mm/3 days), January 24-26, 1934; Swanson Bay (288.6 mm/3 days), January 24-26, 1934; Falls River (207.0 mm/4 days), January 24-27, 1934; Prince Rupert (219.2 mm/2 days), January 25-26, 1934; Aiyansh (96.7 mm/2 days), January 25-26, 1934; Terrace (116.6 mm/2 days), January 25-26, 1934; Kitimat Mission (168.9 mm/3 days), January 25-27, 1934; Terrace (77.5 mm/1 day), January 26, 1934. Source: The Daily News, January 25, 26 and 27, 1934; The Omineca Herald, January 31, 1934; The Terrace News, January 31, 1934; Evening Empire, January 26, 27, 29 and 30, February 1, 1934; The Interior News, January 31, 1934. Near Prince Rupert, a slide came down from Mount Oldfield near Fairview during the night of January 27. Thousands of tons of debris buried 30 cords of stacked wood. Telegraphic communications and rail traffic between Prince Rupert-Terrace were interrupted by washouts, large slides, and damaged bridges. A mudslide blocked the rail line at North Pacific. After the slide had been cleared, a second slide came down at the same location. The Khyex River railroad bridge sustained minor damage by drifting ice and high water conditions. Between Pacific-Kwinitsa, eight to 10 snow and mudslides occurred, varying from 40- 600 ft. (12-180 m) long and 5-25 ft. (1.5-7.5 m) deep. A rotary plow was dispatched to clear the line. Rail traffic was interrupted for a week. A washout occurred east of Smithers, but its exact location was unknown. Just upstream from Terrace, big icejams in the Skeena River dammed the stream. The water was diverted to the south side of the river and almost completely washed away DL 374 Lot 107. Also a part of the old Copper City trail was washed away. On Kitselas Mountain, a large slide came down across the railway and frozen river. Heavy rains and mild weather caused “one of the worst tie-ups on the railroad in the [Smithers] district during the past 15 years.” Huge slides and washouts occurred at Kitwanga and the lower Skeena. For at least 10 days all trains from the west were cancelled. Serious washouts also occurred near Prince George. During a continuous series of west gales with snow, rain, and sleet, the Queen Charlotte Islands experienced the “worst weather known for several years.” The heavy rain and thaw combination caused floods and washouts that interrupted the traffic between Queen Charlotte City-Port Clements. January 30-31, 1934 Event type: Ice jam flooding. Source: The Daily Colonist, February 3, 1934; The Cariboo Observer, February 3, 1934. At the end of January, ice jams caused the “worst winter flood in the history of Quesnel.” Rain and mild weather caused an early thaw and break-up of river ice. On the afternoon of January 30, a large ice run came down the Fraser River and jammed about the mouth of the Quesnel River. Early next day, the river had completely jammed except for a small passage on the west side, and the water began to rise. About 6 p.m., the “auto camp,” in which a large number of families were living, was flooded as was the south portion of Quesnel. During the night of January 31, an ice jam occurred near Quesnel at the Forks, which backed up water in the Quesnel and Fraser rivers. Residents of houses bordering the banks of the two rivers both in Quesnel and West Quesnel had to leave their homes. Although during the spring runoff in 1894 there was more water on the flat on the west side and while ice jams are common, this one was the “worst in the memory of the old-timers.” Fraser River water levels rose to several feet above the high water mark, reaching to the windowsills of some houses along the river. The ice and trees were carried onto the front street at the lower end of town and against the piers of the Fraser River bridge to within 6 ft. (1.8 m) of the decking. On the west side, where a number of dwellings had been built the previous year, a larger area was flooded. About a dozen families hastily packed their belongings and moved across the bridge. Quesnel Light and Power Co.’s plant was isolated for several hours. The basement of Ernest Sealy’s cabin along the Quesnel River at the north portal of the Quesnel bridge was completely flooded. Water undermined its foundations and allowed the floor to settle. Sealy lost a number of personal belongings and five cords of his wood floated over the fence and down the river. Large chunks of ice piled on the banks uprooting trees. Under the Fraser River bridge, the ice piled up to only 6-8 ft. (1.8-2.4 m) from the spans on the west side. The water subsided almost as quickly as it had risen. August 18, 1934 Event type: Flooding. Precipitation: Stewart (54.1 mm/1 day), August 18, 1934. 27

River after floodwaters completely surrounded the house. Alone at the time and though her cries for help could be<br />

heard across the river in central Fort George, she could not be located in the darkness.<br />

On December 20, ice jammed at Engen in the canyon forcing water to break through and flooding low lying<br />

land and the home <strong>of</strong> Harry Worthington. This family escaped with great difficulty to the schoolhouse 0.75 mile (1.2<br />

km) away. A number <strong>of</strong> sheep, pigs and large cattle drowned.<br />

January 24-27, 1934<br />

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

Precipitation: Ocean Falls (393.0 mm/3 days), January 24-26, 1934; Swanson Bay (288.6 mm/3 days), January 24-26,<br />

1934; Falls River (207.0 mm/4 days), January 24-27, 1934; Prince Rupert (219.2 mm/2 days), January 25-26, 1934;<br />

Aiyansh (96.7 mm/2 days), January 25-26, 1934; Terrace (116.6 mm/2 days), January 25-26, 1934; Kitimat Mission<br />

(168.9 mm/3 days), January 25-27, 1934; Terrace (77.5 mm/1 day), January 26, 1934.<br />

Source: The Daily News, January 25, 26 and 27, 1934; The Omineca Herald, January 31, 1934; The Terrace News,<br />

January 31, 1934; Evening Empire, January 26, 27, 29 and 30, February 1, 1934; The Interior News, January 31, 1934.<br />

Near Prince Rupert, a slide came down from Mount Oldfield near Fairview during the night <strong>of</strong> January 27.<br />

Thousands <strong>of</strong> tons <strong>of</strong> debris buried 30 cords <strong>of</strong> stacked wood.<br />

Telegraphic communications and rail traffic between Prince Rupert-Terrace were interrupted by washouts,<br />

large slides, and damaged bridges. A mudslide blocked the rail line at North Pacific. After the slide had been cleared,<br />

a second slide came down at the same location. The Khyex River railroad bridge sustained minor damage by drifting<br />

ice and high water conditions. Between Pacific-Kwinitsa, eight to 10 snow and mudslides occurred, varying from 40-<br />

600 ft. (12-180 m) long and 5-25 ft. (1.5-7.5 m) deep. A rotary plow was dispatched to clear the line. Rail traffic was<br />

interrupted for a week. A washout occurred east <strong>of</strong> Smithers, but its exact location was unknown.<br />

Just upstream from Terrace, big icejams in the Skeena River dammed the stream. The water was diverted to<br />

the south side <strong>of</strong> the river and almost completely washed away DL 374 Lot 107. Also a part <strong>of</strong> the old Copper City<br />

trail was washed away. On Kitselas Mountain, a large slide came down across the railway and frozen river.<br />

Heavy rains and mild weather caused “one <strong>of</strong> the worst tie-ups on the railroad in the [Smithers] district<br />

during the past 15 years.” Huge slides and washouts occurred at Kitwanga and the lower Skeena. For at least 10 days<br />

all trains from the west were cancelled. Serious washouts also occurred near Prince George.<br />

During a continuous series <strong>of</strong> west gales with snow, rain, and sleet, the Queen Charlotte Islands experienced<br />

the “worst weather known for several years.” The heavy rain and thaw combination caused floods and washouts that<br />

interrupted the traffic between Queen Charlotte City-Port Clements.<br />

January 30-31, 1934<br />

Event type: Ice jam flooding.<br />

Source: The Daily Colonist, February 3, 1934; The Cariboo Observer, February 3, 1934.<br />

At the end <strong>of</strong> January, ice jams caused the “worst winter flood in the history <strong>of</strong> Quesnel.” Rain and mild weather<br />

caused an early thaw and break-up <strong>of</strong> river ice. On the afternoon <strong>of</strong> January 30, a large ice run came down the Fraser River<br />

and jammed about the mouth <strong>of</strong> the Quesnel River. Early next day, the river had completely jammed except for a small<br />

passage on the west side, and the water began to rise. About 6 p.m., the “auto camp,” in which a large number <strong>of</strong> families<br />

were living, was flooded as was the south portion <strong>of</strong> Quesnel.<br />

During the night <strong>of</strong> January 31, an ice jam occurred near Quesnel at the Forks, which backed up water in the<br />

Quesnel and Fraser rivers. Residents <strong>of</strong> houses bordering the banks <strong>of</strong> the two rivers both in Quesnel and West Quesnel had<br />

to leave their homes. Although during the spring run<strong>of</strong>f in 1894 there was more water on the flat on the west side and while<br />

ice jams are common, this one was the “worst in the memory <strong>of</strong> the old-timers.”<br />

Fraser River water levels rose to several feet above the high water mark, reaching to the windowsills <strong>of</strong> some<br />

houses along the river. The ice and trees were carried onto the front street at the lower end <strong>of</strong> town and against the piers <strong>of</strong><br />

the Fraser River bridge to within 6 ft. (1.8 m) <strong>of</strong> the decking. On the west side, where a number <strong>of</strong> dwellings had been built<br />

the previous year, a larger area was flooded. About a dozen families hastily packed their belongings and moved across the<br />

bridge.<br />

Quesnel Light and Power Co.’s plant was isolated for several hours. The basement <strong>of</strong> Ernest Sealy’s cabin<br />

along the Quesnel River at the north portal <strong>of</strong> the Quesnel bridge was completely flooded. Water undermined its<br />

foundations and allowed the floor to settle. Sealy lost a number <strong>of</strong> personal belongings and five cords <strong>of</strong> his wood<br />

floated over the fence and down the river. Large chunks <strong>of</strong> ice piled on the banks uprooting trees. Under the Fraser<br />

River bridge, the ice piled up to only 6-8 ft. (1.8-2.4 m) from the spans on the west side. The water subsided almost as<br />

quickly as it had risen.<br />

August 18, 1934<br />

Event type: Flooding.<br />

Precipitation: Stewart (54.1 mm/1 day), August 18, 1934.<br />

27

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