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Earthquake
Ground Shaking Levels for the Wasatch Front
2003 International Building Code, 0.2 and 1 second spectral response
acceleration maps
These maps are intended for use by
building officials and engineers to
illustrate earthquake ground-shaking levels.
Salt Lake County (pdf)
Utah County (pdf)
Davis County (pdf)
Weber County (pdf)
The Utah Seismic Safety Commission compiled a series of eight maps
showing 0.2 and 1 second spectral response acceleration contours
for Weber, Davis, Salt Lake, and Utah Counties.
These maps were created by the Utah Geological Survey (UGS) using
the gridded data from the 2003 International Building Code (IBC)
Seismic Design Parameters CD-ROM, prepared by the U.S. Geological
Survey. The maps show values for an IBC site class B, so adjustments
to map values must be made depending on the actual site class as
outlined in the IBC.
Generalized site class maps for Salt Lake Valley and the Wasatch
Front are available as UGS Open-File Report 424 (CD) and Report
of Investigation 248, respectively, at the Natural
Resources Map and Bookstore.
These maps are intended for use by building officials and engineers
to illustrate earthquake ground-shaking levels, but are not for
use in building design. The IBC Seismic Design Parameters CD-ROM
included with the IBC (available from International Code Council;
www.iccsafe.org) should be
used for design.
The following information is for those other than building officials
and engineers who are interested in viewing these maps to understand
relative ground shaking hazards.
Larger values shown on contour lines in the maps indicate relatively
greater levels of ground shaking expected during a given period
of time, in this case, 2,500 years (equivalent to a 2% probability
of exceedance in 50 years).
The Ss (0.2 second) maps indicate levels of ground
shaking at high frequencies (or short periods) that are particularly
damaging to 1-2 story structures such as houses. The S1
(1.0 second) maps indicate levels of ground shaking at lower frequencies
(or longer periods) that are more damaging to tall structures (around
10 stories or more).
For example, if you are interested in the relative ground-shaking
hazard to houses in Salt Lake Valley, the Ss (0.2 second)
maps indicate that the hazard (relative strength of ground shaking)
is highest in the East Bench area (1.7-1.8), and relatively lower
along the west side of Salt Lake Valley (1.1-1.3).
Keep in mind these maps do not take into account local geologic
conditions at a site, which may either amplify or dampen the motions
shown on the map.
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