Newly discovered fault line running underneath the Saanich Peninsula could be catastrophic for southern Vancouver Island
To the untrained eye, it’s nothing more than a tiny bump in the trail that surrounds Elk Lake. For Theron Finley, a PhD candidate at the University of Victoria in the earthquake geology department, it’s much more.
“The side that we’re on was pushed up overtop of that side,” said Finley.
It runs beneath Elk Lake, over Cordova Ridge and into Cordova Bay.
“The fault line actually runs right along the edge of this slope,” said Finley as he pointed to the lump in the trail.
It’s a newly discovered crustal fault line with the potential of causing a massive amount of damage.
“We know that the damage and the shaking would be quite severe, especially close to the fault,” said Nick Harrichhausen, researcher with the Centre National de la Recherche Scientifique in France.
A quake here could topple buildings and cause billions of dollars in damage.
It’s a scenario that researchers believe played out roughly 3,000 years ago.
“We estimate it to be a 6.1 to 7.6 magnitude earthquake,” said Finley.
The fault line was discovered through LiDAR data gathered by the province. LiDAR uses lasers to scan an area from the air, removing foliage and buildings in the process.
LiDAR data shows the fault line running through the Saanich Peninsula. “We had access to this LiDAR,” said Harrichhausen.
This data exposed the fault line to the UVic researchers, and that’s when the team dug deeper into the findings.
“Not only did we dig, but we also did geophysical surveys,” said Harrichhausen,
That work confirmed that yes, this is a fault line, and helped put a timeline on its last seismic movement as well as the power behind the earthquake it caused.
The big question remains: how long does this newly discovered fault line span?
“It’s a bit of an open question,” said Finley. “We have roughly a five-kilometre stretch here that we are very confident ruptured in an earthquake.”
LiDAR scanning cannot penetrate water, but evidence suggests the fault extends for 72 kilometres out underneath the Haro Strait.
With current findings only pinpointing one earthquake in the past, researchers now need to continue searching for more evidence of other shakes caused by the fault. As well, researchers need to measure how fast the fault is moving beneath our feet.
“With that data we can do a better job of calculating the probability that this type of rupture will happen within, say the next 500 years,” said Harrichhausen.
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