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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August 25-26, 1950 Event type: Severe wind storm. Precipitation: Langara (71.7 mm/2 days), August 25-26, 1950; Falls River (39.6 mm/1 day), August 26, 1950; Prince Rupert (64.8 mm/1 day), August 26, 1950. Source: The Daily News, August 28, 1950; The Interior News, August 31, 1950. A rainstorm with winds of 60-70 mph (96.6-112.7 km/h) went through the Skeena Valley. The storm, which was described as “one of the worst storms known in the District,” was felt as far east as Burns Lake. Trees fell across the highway, railroad tracks and telephone lines. The highway 30 mi. (48 km) west of Terrace was blocked for a distance of 3 mi. (4.8 km). In Prince Rupert, many basements flooded and the telephone service was interrupted. There were three major breaks in the line. The railway dispatcher’s telephone line also went out. October 7-8, 1950 Event type: Severe storm. Precipitation: Not applicable. Source: Prince Rupert Daily News, October 10, 1950; The British Columbian, October 10, 1950. On October 7-8, southeast gales, the third storm within a week with winds reaching 65 mph (104 km/h), hit the Queen Charlotte Islands. A Davis raft, valued at over $1 million, was torn from its moorings at Alliford Bay and piled up on the shores of Queen Charlotte City. Barber’s float, used by fishermen and Queen Charlotte Airlines, parted and was scattered along the same shores. Several gillnet fishing vessels were badly damaged or lost. Attempts to tow to Queen Charlotte City the seiner Scrub, severely damaged in one of the earlier storms with the loss of two lives proved unsuccessful. Storms washed the vessel ashore at Sandspit where she broke up. November 2-4, 1950 Event type: Flooding. Precipitation: Aiyansh (38.9 mm/1 day), November 2, 1950; Namu (152.1 mm/2 days), November 2-3, 1950; Ocean Falls (293.1 mm/2 days), November 2-3, 1950; Falls River (64.8 mm/1 day), November 3, 1950; Bella Coola (180.3 mm/2 days), November 3-4, 1950. Source: Ocean Falls Reporter, November 11, 1950; Environment Canada 1991. Winds up to 50 mph (80 km/h) were reported from all across the Queen Charlotte Islands. In some places also fog and heavy rain occurred. The storms over the Queen Charlottes kept planes of Queen Charlotte Airlines grounded in Prince Rupert on November 2. On November 4, the Bella Coola River near Hagensborg recorded a maximum daily discharge of 813 m 3 /s (Environment Canada 1991). The recent flood at the South Bentick Logging Camp washed out some of the logging bridges. Cartwright, Public Works Engineer, was called to Bella Coola to look over the damage caused by the rampaging Bella Coola River. The flood isolated Hagensborg and the rest of the valley from the townsite. The plans of the new bridge crossing to Salloompt had to be altered because of the rise of the river. November 22-26, 1950 Event type: Icejam flooding. Precipitation: Not applicable. Source: Nanaimo Free Press, November 27, 1950; The British Columbian, November 28, 1950; The Interior News, November 30, 1950. On November 22, drift ice started jamming the Bulkley River in a bend of the river at the east end of the bridge near Smithers. Ice started building up to some point between Smithers-Telkwa. The river’s surface was frozen in a canyon 4 mi. (6.4 km) south of the Bulkley bridge. Water started backing up into an old slough. On November 22 at 3 a.m., the K. Vetterli family was evacuated when the lower part of the farm flooded. On November 26, the flood situation worsened. The river channel in the canyon near the airport, frozen across the top caused water to back up. An icejam 1 mi. (1.6 km) east of Smithers on the Bulkley River caused flooding of two farms with 3 ft. (90 cm) of water. The families of William Kidd and Carl Vetterli’s neighbouring 320ac. (128 ha) farm were forced to vacate their farms. Floodwaters damaged 25 tons of potatoes and a large volume of timothy seed stored in a root cellar at the Vetterli farm. Parts of the Northern Trans-Provincial Highway (Highway 16) were under 4-5 ft. (1.2-1.5 m) of water over an old part of the road. Water also covered a quarter-mile (400 m) section of the new highway, 0.5 mi. (800 m) from Smithers. By November 27, 10 in. (25 cm) of water was pouring across the main highway. School bus runs to Driftwood, Glentanna and Telkwa were temporary discontinued. December 1-4, 1950 Icejam flooding. Precipitation: Not applicable. 56

Source: The Interior News, December 7, 1950. On December 1, cold weather caused icejams to form on the Skeena River near Terrace. “Authoritative sources” advised that the extensive ice jamming on the river were the worst since 1929. On December 1, 3 and 4, Smithers recorded temperatures of –20.8 o , -19.2 o and –21.7 o F (-29.3 o , -28.4 o and –29.8 o C), respectively. March 23-26, 1951 Event type: Rockslide. Precipitation: Falls River (98.3 mm/2 days), March 23-24, 1951; Prince Rupert (33.8 mm/2 days), March 24-25, 1951; Terrace (20.4 mm/2 days), March 25-26, 1951. Source: The Interior News, March 29, 1951. On March 26, a rockslide came down 5 mi. (8 km) west of Kwinitsa. The slide occurred just as a train was going by. It missed the engine but derailed the first two cars and overturned the rails. In addition to the bulldozers stationed as Kwinitsa, an extra crew was dispatched from Prince Rupert. It caused a nine-hour delay for the eastbound train out of Prince Rupert. An earlier slide at the same spot had taken out the wire services to Prince Rupert. Rail service was restored on March 27. Severe storms of early March made attempts by the Public Works Department to have the highway between Prince Rupert-Terrace open for traffic impossible. A series of new slides interfered with the attempts to open up the snow-blocked road. One such slide at the tunnel near Kwinitsa blocked the highway to a depth of 12 ft. (3.6 m). It slid out on the river ice for a distance of 150 ft. (45 m). It was expected that slides would continue to block the highway for some time to come. Spring 1951 Event type: Icejam flooding? Source: The Cariboo Observer, April 24, 1952. During the spring before the ice in the Quesnel River broke up, an ice jam developed, which extended well above the Fraser River bridge. April 4-5, 1951 Event type: Spring runoff flooding. Precipitation: Terrace (max. temp. 9.4 o C, 13.9 o C), April 4-5, 1951. Source: Omineca Herald, April 6, 1951; The Interior News, April 5, 1951; Files, B.C. Ministry of Transportation and Highways, Terrace. Around April 4-5, a major washout occurred at Dorreen, and the road was impassable at Copper River flats. Highway 16 between Usk-Terrace was closed. The highway was scheduled to reopen on April 7 at noon. May 10-12, 1951 Event type: Spring runoff flooding. Precipitation: Smithers (28.9 mm/2 days), May 10-11, 1951; Smithers A (17.2 mm/2 days), May 11-12, 1951. Source: The Interior News, May 17, 1951; The Daily Times, May 15, 1951; Environment Canada 1991; Files, B.C. Ministry of Transportation and Highways, Terrace. In the Bulkley Valley, steady rainfalls, together with warm weather, created flood conditions on the creeks flowing into the Bulkley River. The Bulkley River at Quick recorded a maximum daily discharge of 634 m 3 /s on May 13 (Environment Canada 1991). The worst situation occurred in the Forestdale-Houston area. Floodwaters threatened the new $140,000 Houston Hotel and several houses were surrounded by water. Mile 16 of the highway was under 2-3 ft. (60-90 cm) of water and a number of homes were threatened with evacuation (Daily Times, May 15, 1951). Flooding occurred at Houston, when the Buck River (Creek) flooded the highway. On May 12, numerous small washouts occurred because the culverts were too small to handle the abnormal runoff. The most serious washout was at a point 2 mi. (3.2 km) west of Forestdale. The highway was open to light traffic only. On May 14, the eastbound way freight was cancelled because of impassable track. Other freight traffic was delayed for 36 hours. On the evening of May 14, the high water started receding. June 4, 1951 Event type: Rockslide. Precipitation: Not applicable; Terrace (max. temp. 26.1 o C), June 3 and 4, 1951. Source: The Interior News, June 7, 1951. Early on June 4, a rockslide near Telegraph Point, 3 mi. (4.8 km) west of Kwinitsa, blocked the railway tracks. A 120-ft. (36 m) section of track was badly damaged and needed to be replaced, requiring drilling and blasting equipment. Late summer-early fall 1951 Event type: Rockslide. 57

Source: The Interior News, December 7, 1950.<br />

On December 1, cold weather caused icejams to form on the Skeena River near Terrace. “Authoritative<br />

sources” advised that the extensive ice jamming on the river were the worst since 1929. On December 1, 3 and 4,<br />

Smithers recorded temperatures <strong>of</strong> –20.8 o , -19.2 o and –21.7 o F (-29.3 o , -28.4 o and –29.8 o C), respectively.<br />

March 23-26, 1951<br />

Event type: Rockslide.<br />

Precipitation: Falls River (98.3 mm/2 days), March 23-24, 1951; Prince Rupert (33.8 mm/2 days), March 24-25, 1951;<br />

Terrace (20.4 mm/2 days), March 25-26, 1951.<br />

Source: The Interior News, March 29, 1951.<br />

On March 26, a rockslide came down 5 mi. (8 km) west <strong>of</strong> Kwinitsa. The slide occurred just as a train was<br />

going by. It missed the engine but derailed the first two cars and overturned the rails. In addition to the bulldozers<br />

stationed as Kwinitsa, an extra crew was dispatched from Prince Rupert. It caused a nine-hour delay for the eastbound<br />

train out <strong>of</strong> Prince Rupert. An earlier slide at the same spot had taken out the wire services to Prince Rupert. Rail<br />

service was restored on March 27.<br />

Severe storms <strong>of</strong> early March made attempts by the Public Works Department to have the highway between<br />

Prince Rupert-Terrace open for traffic impossible. A series <strong>of</strong> new slides interfered with the attempts to open up the<br />

snow-blocked road. One such slide at the tunnel near Kwinitsa blocked the highway to a depth <strong>of</strong> 12 ft. (3.6 m). It slid<br />

out on the river ice for a distance <strong>of</strong> 150 ft. (45 m). It was expected that slides would continue to block the highway<br />

for some time to come.<br />

Spring 1951<br />

Event type: Icejam flooding?<br />

Source: The Cariboo Observer, April 24, 1952.<br />

During the spring before the ice in the Quesnel River broke up, an ice jam developed, which extended well<br />

above the Fraser River bridge.<br />

April 4-5, 1951<br />

Event type: Spring run<strong>of</strong>f flooding.<br />

Precipitation: Terrace (max. temp. 9.4 o C, 13.9 o C), April 4-5, 1951.<br />

Source: Omineca Herald, April 6, 1951; The Interior News, April 5, 1951; Files, B.C. Ministry <strong>of</strong> Transportation and<br />

Highways, Terrace.<br />

Around April 4-5, a major washout occurred at Dorreen, and the road was impassable at Copper River flats.<br />

Highway 16 between Usk-Terrace was closed. The highway was scheduled to reopen on April 7 at noon.<br />

May 10-12, 1951<br />

Event type: Spring run<strong>of</strong>f flooding.<br />

Precipitation: Smithers (28.9 mm/2 days), May 10-11, 1951; Smithers A (17.2 mm/2 days), May 11-12, 1951.<br />

Source: The Interior News, May 17, 1951; The Daily Times, May 15, 1951; Environment Canada 1991; Files, B.C.<br />

Ministry <strong>of</strong> Transportation and Highways, Terrace.<br />

In the Bulkley Valley, steady rainfalls, together with warm weather, created flood conditions on the creeks<br />

flowing into the Bulkley River. The Bulkley River at Quick recorded a maximum daily discharge <strong>of</strong> 634 m 3 /s on May<br />

13 (Environment Canada 1991). The worst situation occurred in the Forestdale-Houston area. Floodwaters threatened<br />

the new $140,000 Houston Hotel and several houses were surrounded by water. Mile 16 <strong>of</strong> the highway was under 2-3<br />

ft. (60-90 cm) <strong>of</strong> water and a number <strong>of</strong> homes were threatened with evacuation (Daily Times, May 15, 1951).<br />

Flooding occurred at Houston, when the Buck River (Creek) flooded the highway. On May 12, numerous small<br />

washouts occurred because the culverts were too small to handle the abnormal run<strong>of</strong>f. The most serious washout was<br />

at a point 2 mi. (3.2 km) west <strong>of</strong> Forestdale. The highway was open to light traffic only. On May 14, the eastbound<br />

way freight was cancelled because <strong>of</strong> impassable track. Other freight traffic was delayed for 36 hours. On the evening<br />

<strong>of</strong> May 14, the high water started receding.<br />

June 4, 1951<br />

Event type: Rockslide.<br />

Precipitation: Not applicable; Terrace (max. temp. 26.1 o C), June 3 and 4, 1951.<br />

Source: The Interior News, June 7, 1951.<br />

Early on June 4, a rockslide near Telegraph Point, 3 mi. (4.8 km) west <strong>of</strong> Kwinitsa, blocked the railway<br />

tracks. A 120-ft. (36 m) section <strong>of</strong> track was badly damaged and needed to be replaced, requiring drilling and blasting<br />

equipment.<br />

Late summer-early fall 1951<br />

Event type: Rockslide.<br />

57

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