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Vancouver, British Columbia, is one of the handful of major North American metropolises with no damaging earthquakes since modern seismic monitors were invented.
Without an earthquake record to provide insight into how the ground under the city shakes during quake, scientists aren't sure what will happen buildings in the City of Glass when a future earthquake strikes. Recent earthquakes in other cities, such as Christchurch, New Zealand, and Los Angeles, show that damage can concentrate in zones defined by buried geologic structures, such as sedimentary basins (lows or valleys filled by sediment). Basins increase shaking by focusing seismic energy, like a magnifying glass focuses light. Seismic waves can also ping-pong back and forth inside a basin, like waves sloshing inside a swimming pool.
A new study seeks to better understand how the big Georgia Basin surrounding Vancouver will fare in the next earthquake. The Georgia Basin is a shallow, wide bowl filled by silt, sand and glacial deposits. With computer simulations, researchers discovered that the city could see three to four times greater shaking during an earthquake than if the basin wasn't there. The findings were published today (Jan. 20) in the Bulletin of the Seismological Society of America.
"This is a worthwhile first step toward building better earthquake-hazard models," said lead study author Sheri Molnar, a seismic geologist at the University of British Columbia.
— Becky Oskin, LiveScience
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