What are the effects of earthquakes?

Earthquake effects can include strong ground shaking, ground failure and tsunami.

The intensity of shaking at a given location depends upon several factors:

bulletThe magnitude of the quake
bulletDistance from the focus
bulletType of soil underlying the site

Because of these factors, the damage caused by a quake will vary from one area to another. Earthquakes are most destructive when they are located near cities. Since about 70 per cent of B.C.'s population lives in earthquake prone southwestern B.C., there is an obvious need for emergency planning and earthquake research.

LARGE EARTHQUAKES IN THE PAST
Year Region Magnitude Comment
1872 Washington-B.C. border 7.4 Widely felt in B.C.
1899 Yukon-Alaska border 8.0 Widely felt in northwestern B.C.
1918 Vancouver Island 7.0 Widely felt, minor damage.
1929 Queen Charlotte Islands 7.0 Widely felt, minor damage.
1946 Vancouver Island 7.3 Widely felt, most damaging quake in western Canada.
1949 Queen Charlotte Islands 8.1 Largest quake in Canada, one of the world's great quakes.
1949 Washington 7.0 Much damage in Washington and felt in southwestern B.C.
1958 Alaska-B.C. border 7.9 Damage in Alaska, widely felt in northwestern B.C.
1964 Alaska 9.2 Tsunami damage on Vancouver Island.
1970 Queen Charlotte Islands 7.4 Widely felt.

The 1946 Quake!

We can learn important lessons about how earthquakes will affect us by examining past events, such as the 1946 Vancouver Island earthquake.

This earthquake, one of the most damaging in B.C.'s history, had a magnitude of 7.3 and an epicentre located northwest of Courtenay. It was felt widely throughout B.C. Luckily, damage was restricted because there were no heavily populated areas near the epicentre, where the violent shaking occurred.

 

'46 Quake: location of damage
Map of central Vancouver Island showing locations of soil failures and landslide concentration. (Adapted from the Canadian Geotechnical Journal 1980, volume 17, page 124 and Bulletin of the Seismological Society of America 1979, volume 69, page 446).

It is interesting to note, that some of the areas most affected by this earthquake were not necessarily those closest to the epicentre. Several sites on Vancouver Island suffered damage due to ground amplification, liquefaction and landslides. The distribution of liquefaction sites and ground failures was influenced by the type of soil or rock underlying the site. Liquefaction sites occurred on both sides of the Strait of Georgia and near lake and river basins where areas were underlain by saturated sand and clay. Some of the highest intensities of shaking were observed in areas with saturated and loose soils. Likewise, landslides were distinctly concentrated in the coastal mountains where slopes are steep and unstable.

 

'46 Quake: location of damage
Isoseismal contours of approximately equal levels of shaking intensity resulting from the 1946 Vancouver Island earthquake. (Adapted from the Canadian Geotechnical Journal 1980, volume 17, page 123).

 

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Earthquakes in British Columbia was originally produced as Information Circular 1991-6 by the BC Geological Survey of the B.C. Ministry of Energy, Mines and Petroleum Resources, in cooperation with the B.C. Ministry of Environment, the B.C. Provincial Emergency Program and with the assistance of the Geological Survey of Canada. It has been amended and updated in this WWW version.

Copies are available from:

Publications Office
BC Geological Survey
Ministry of Energy, Mines, and Petroleum Resources
P.O. Box 9333. Stn Prov Gov't
Victoria, B.C.
V8W 9N3

 

  This page was last updated Wednesday, March 08, 2006