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Council Meeting/Documents/Appendix: Seismic hazard investigations at select DND facilities
Appendix

Appendix: Seismic hazard investigations at select DND facilities

July 16, 2024Pages 201–2033 sections

Excerpts from a 2022 Geological Survey of Canada report investigating seismic risks in southwestern British Columbia.

1 CALL TO ORDER- Mayor Tobias called the meeting to order at 7:00 p.m.
Report authors: C. Paul and J.F. CassidyFocuses on subduction, in-slab, and crustal scenariosNotes that the proximity of the Leech River Valley fault to Greater Victoria yields the highest amplitude of shaking

GEOLOGICAL SURVEY OF CANADA OPEN FILE 8934

Page 201–203

Seismic hazard investigations at select DND facilities in southwestern British Columbia: subduction, in-slab, and crustal scenarios

C. Paul and J.F. Cassidy

2022


Page 201–203

Additional information for Notice of Motion

The Leech River fault line runs east / west, just 5 km south of Thetis Lake historic dam 3

Map of the Victoria region showing population density, GNSS velocity vectors, and active fault traces including the Leech River Fault (LRF), San Juan Fault (SJF), and Devil's Mountain Fault (DMF).
Map of the Victoria region showing population density, GNSS velocity vectors, and active fault traces including the Leech River Fault (LRF), San Juan Fault (SJF), and Devil's Mountain Fault (DMF).

The Leech River and Devil’s Mountain are connected

Map illustrating the continuous connection between the Leech River Valley Fault and the Devil's Mountain Fault across Vancouver Island and the Canada-U.S.A. border.
Map illustrating the continuous connection between the Leech River Valley Fault and the Devil's Mountain Fault across Vancouver Island and the Canada-U.S.A. border.

2022 report for the DND Page 16

“… the smallest magnitude event, the proximity to Greater Victoria yields the highest amplitude of shaking”

6.3 CRUSTAL

The Leech River Valley – Devil’s Mountain Fault scenario was the smallest magnitude of our three scenarios at $M_w$ 6.4. This scenario occurs along a shallow rupture plane (1 to 30 km deep) following the LRV-DMF trace offshore of Greater Victoria towards the Leech River Valley. The PGA map (Figure 14) shows that although it is the smallest magnitude event, the proximity to greater Victoria yields the highest amplitude of shaking (maximum PGA of 0.58g experienced in Langford). The ground-shaking drops off to modest shaking at ~75 km from the rupture plane and light shaking within 150 km. The quick attenuation of the shaking intensities means that only light shaking is experienced in most of Greater Vancouver and central Vancouver Island (including Comox). The amplification due to the soft soils of the Fraser River Delta generates modest shaking in Richmond.

Like the other two scenarios, we calculated the SA at differing periods (0.1, 0.2, 0.3, 0.5, 0.6, 1.0, 2.0, 5.0 and 10.0 seconds). Additionally, we calculated the Peak Ground Velocity (PGV). The hazard spectra display the extreme localization of shaking (Figure 15), as the peak amplitude in Victoria is five times that felt in Vancouver on similar soil and more than ten times that in Nanaimo.

Figure 14: Three-paneled map showing Peak Ground Acceleration (PGA) of the Leech River Valley-Devil’s Mountain Fault scenario earthquake, with a specific pointer to Thetis Lake Dam 3 and an intensity scale legend.
Figure 14: Three-paneled map showing Peak Ground Acceleration (PGA) of the Leech River Valley-Devil’s Mountain Fault scenario earthquake, with a specific pointer to Thetis Lake Dam 3 and an intensity scale legend.
PERCEIVED SHAKING Not felt Weak Light Moderate Strong Very strong Severe Violent Extreme
PEAK ACC.(%g) <0.05 0.3 2.8 6.2 12 22 40 75 >139
INSTRUMENTAL INTENSITY I II–III IV V VI VII VIII IX X+

Figure 14: Peak Ground Acceleration of the Leech River Valley-Devil’s Mountain Fault scenario earthquake. Highly localized extreme shaking. PGA to perceived shaking is modified from Worden et al. (2010).

Page 201–203
Extracted from: 2024 07 16 Council Agenda - Agenda - Pdf