Earthquake Hazards Mapping of Greater Victoria
Hard Copies are available from Crown
Publications in Victoria
To view any of the following
maps at full size (in JPG format), click on the small map images. To
download or view in PDF format, you require Adobe
Reader. The PDF files for each of the earthquake
hazard maps have been created in a high resolution format to maximize their legibility and
are best viewed by downloading and using the zoom functions in Adobe or by
generating large-format hard copy output, e.g., E-size plots (36" x 48").
Related publications:
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Composite Relative
Earthquake Hazard Map of Greater Victoria (Geoscience Map 2000-1): The objective
of this map is to show areas of Greater Victoria where the earthquake hazard is likely to
be increased due to the presence of potentially unstable slopes, and soils susceptible to
amplification of ground motion and/or liquefaction. This map has been compiled from three
other maps: a relative liquefaction hazard map, a relative amplification of ground motion
hazard map, and an earthquake-induced slope instability hazard map.
Composite Map (PDF
3.9 MB)
Composite Map (details viewable) (PDF
9.7 MB)
Legend:
PDF version (1.6
MB), or HTML version
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Relative Amplification
of Ground Motion Hazard Map of Greater Victoria (Geoscience Map 2000-3, Sheet 3B): This
map shows areas where the earthquake hazard is increased due to amplification of ground
motion. The amplification of ground motion hazard has been estimated on the basis of
the National Earthquake Hazard Reduction Program (NEHRP) site classes for the
susceptibility to amplification of ground motion (Building Seismic Safety Council, 1994),
which are based on the average response of various types of soils.
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Relative Liquefaction
Hazard Map of Greater Victoria (Geoscience Map 2000-3, Sheet 3A): This map
shows areas of Greater Victoria in which the earthquake hazard is potentially increased
due to the presence of soils susceptible to liquefaction. Liquefaction is the
transformation that occurs when earthquake shaking (or other disturbance) causes a
saturated granular soil to lose its strength and behave like a liquid and can be one of
the major causes of damage during an earthquake. The susceptibility of a site to
liquefaction depends on the depth to water table and the density, grain size and age of
the underlying deposits. This map was prepared by assigning a hazard rating to each
geological map unit based on these criteria and quantitative analyses.
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Seismic Slope
Stability Map of Greater Victoria (Geoscience Map 2000-3, Sheet 3C): Seismic
slope hazard mapping is intended to show relative susceptibility to earthquake-induced
slope failures. The seismic slope hazard map is based on a compilation of existing
subsurface data, previous slope stability assessments, bedrock geology and surficial
geology maps, topographic data, and airphoto interpretation. Stability analyses were
conducted on twelve different slope models including typical or simplified slopes found
throughout the Victoria area as well as specific, complex slope models where more detailed
information was available. The stability analyses determined both the static factor
of safety and the yield acceleration (the intensity of seismic motions that would cause a
slope failure).
Seismic Slope Stability Map (PDF
2.0 MB)
Legend |
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Quaternary Geological
Map of Greater Victoria (Geoscience Map 2000-2): This map shows the
thickness and distribution of the Quaternary stratigraphic units in Greater
Victoria. It is intended to provide the geological basis for the assessment of the
earthquake hazards shown on companion maps which depict the liquefaction and amplification
of ground motion in Greater Victoria (Geoscience Maps 2000-3a and 2000-3b; Monahan et
al., 2000b and c). The geological units shown here are defined in part to reflect
these hazards.
Quaternary Geological Map (PDF
1.9 MB)
Legend:
PDF version (183
KB), or HTML version
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