21.12.2012 Views

HISTORICAL NEWS SEARCH - Government of British Columbia

HISTORICAL NEWS SEARCH - Government of British Columbia

HISTORICAL NEWS SEARCH - Government of British Columbia

SHOW MORE
SHOW LESS

You also want an ePaper? Increase the reach of your titles

YUMPU automatically turns print PDFs into web optimized ePapers that Google loves.

In July, heavy rainfall caused widespread landsliding over a large area <strong>of</strong> the northern Cordillera. The heavy<br />

rainfall resulted in numerous debris flows and related sediment-water flow processes that severed the Alaska Highway in<br />

three areas: Muncho Lake, B.C., Rancheria and Kluane, Y.T. The events paralysed travel in the region for several days<br />

(Evans and Clague 1989; Trenhaile1998).<br />

A major portion <strong>of</strong> the highway along the west shore <strong>of</strong> Kluane Lake was buried under a mountain slide. It took<br />

many days to dig the muck <strong>of</strong>f the road surface and to stabilise the hillside sufficiently to protect against further slides.<br />

Traffic again piled up at both ends <strong>of</strong> the blockage, although many escaped by driving around by way <strong>of</strong> Dawson City, the<br />

Top <strong>of</strong> the World Highway, and Richardson Highway in Alaska to Teslin Junction on the Alaska Highway (Coates 1992).<br />

In the vicinity <strong>of</strong> Muncho Lake, debris flows originating in the steep watersheds <strong>of</strong> the Sentinel Range <strong>of</strong> the<br />

Rocky Mountains severed the highway at six locations. At Kluane Lake, debris flows and debris avalanches severed the<br />

highway in numerous places. At one location, near the Slims River, a debris flow covered over 500 m <strong>of</strong> highway. The direct<br />

cost <strong>of</strong> restoring the Alaska Highway was in the order <strong>of</strong> $1.8 Million in 1988 dollars (Evans and Clague 1989). *1)<br />

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

*1) These events point out the vulnerability <strong>of</strong> transportation facilities in mountainous terrain where the location <strong>of</strong> routes<br />

necessarily involves the traversing <strong>of</strong> active geomorphic surfaces.<br />

August 1, 1988<br />

Event type: Glacial outburst flood.<br />

Precipitation: Not applicable.<br />

Source: Eero Karanka, pers. comm. February 21, 1994. Habitat Biologist, Department <strong>of</strong> Fisheries and Oceans, Prince<br />

Rupert.<br />

On August 1, the lower lake on the Tulsequah Glacier drained (Karanka, pers. comm.). *1)<br />

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

*1) There are two lakes on Tulsequah Glacier that drain by jökulhlaup; the one described by Marcus (1960) and<br />

another lake further up the glacier. The latter should not be confused with Upper Lake Tulsequah described by Marcus<br />

(1960) (Karanka, pers. comm.).<br />

September 16, 1988<br />

Event type: Glacial outburst flood.<br />

Precipitation: Not applicable.<br />

Source: Eero Karanka, pers. comm. February 21, 1994. Habitat Biologist, Department <strong>of</strong> Fisheries and Oceans, Prince<br />

Rupert.<br />

On September 16, the upper lake <strong>of</strong> the Tulsequah Glacier drained (Karanka, pers. comm.). *1)<br />

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

*1) Based on WSC data, other drainings may have occurred on August 17, 1989, July 19 and August 20, 1990. The<br />

drainings are detectable in the WSC data only since 1988, when the gauging station was moved from upstream to<br />

downstream <strong>of</strong> the Tulsequah River junction (Karanka, pers. comm.).<br />

September 26-29, 1988<br />

Event type: Flooding.<br />

Precipitation: Hartley Bay (357.2 mm/3 days), September 26-28, 1988; Prince Rupert (75.0 mm/1 day), September 27,<br />

1988; Pallant Creek (234.6 mm/2 days), September 27-28, 1988; Prince Rupert M. Circ (121.4 mm/2 days), September<br />

27-28, 1988; Falls River (180.2 mm/2 days), September 27-28, 1988; Kemano (114.4 mm/2 days), September 27-28,<br />

1988; Kildala (172.9 mm/2 days), September 27-28, 1988; Kitimat 2 (204.2 mm/2 days), September 27-28, 1988;<br />

Kitimat Townsite (180.5 mm/2 days), September 27-28, 1988; Bella Coola (149.8 mm/2 days), September 27-28,<br />

1988; Sewell Inlet (222.2 mm/2 days), September 27-28, 1988; Sandspit A (36.6 mm/1 day), September 28, 1988;<br />

Nass Camp (62.4 mm/1 day), September 28, 1988; Terrace (106.6 mm/1 day), September 28, 1988; Smithers A (59.4<br />

mm/2 days), September 28-29, 1988.<br />

Source: The Daily News, September 29, October 21, 1988; Northern Sentinel, September 29, 1988; The Coast<br />

Mountain Courier, October 5, November 30, 1988; The Terrace Standard, October 5 and 19, November 2, 1988; The<br />

Interior News, October 5, 1988; The Province, October 21, 1988; Environment Canada 1991; Initial Report by<br />

Ministry <strong>of</strong> Environment –Rivers Section File P88-6, Task 890895; Eurocan Pulp & Paper Co. Ltd., Annual Report<br />

1988 T.F.L. 41, Kitimat; Brent Smith, pers. comm. Skeena Cellulose, Terrace; Memorandum, October 4, 1988, Archie<br />

MacDonald (Skeena Cellulose, Terrace) to Ted Wilson (B.C. Min. For., Terrace); Pacific Northern Gas, Terrace)<br />

Repair Costs for Copper River; Letter, October 31, 1988, Ted Wilson (Engineering Assistant B.C. Min. For., Terrace)<br />

to Dean Moneray (Manager, Coastal Sector Provincial Emergency Program) Vancouver. Damage Report for<br />

September 29-30, 1988.<br />

On August 29 following heavy rains, severe flooding occurred in a number <strong>of</strong> watersheds in northwestern<br />

<strong>British</strong> <strong>Columbia</strong>. A two-day storm hit Terrace and Kitimat, with winds gusting up to 100 km/h. Kitimat reported 5.5<br />

in. (139.7 mm) <strong>of</strong> rain in 24 hours and Terrace reported 4 in. (101.6 mm) on September 28. The storm brought heavy<br />

155

Hooray! Your file is uploaded and ready to be published.

Saved successfully!

Ooh no, something went wrong!