Bremerton Earthquake Intensity Map

The following map is an attempt to display the felt-form data obtained by our Web forms responses. This map was generated by averaging the responses over all responses from one zip-code and using that average at the geographic center of the zip code (dots on the map) and then producing a smooth contour of those values. We plan to try and do a similar thing for the exact location of each response; however, it is quite difficult to obtain a geographic coordinate from a full address so this may take much longer.

About the isoseismal map:

The contours shown on this map represent equal strength of shaking and are known as isoseismal lines. The numbers (ranging from 3.3 to 5) are intensity values and should not be confused with earthquake magnitude. Earthquake magnitude is a measure of the relative size of the earthquake source and can be determined from seismographs often located far from the earthquake epicenter. In theory, each earthquake will have a single magnitude value. In practice, different ways of calculating magnitude and the use of different seismic instruments will cause some variation in the magnitude numbers. However, these variations are usually pretty small and the final magnitude calculations for the Bremerton earthquake all fall between 4.2 and 5.0. Earthquake intensities, in contrast to magnitude, always show considerable variation. The intensity is usually strongest near the earthquake epicenter and decreases with distance until eventually, at some point far away, the earthquake is no longer felt by anyone. Other factors such as the local geology beneath a particular site, the regional geology and the orientation of the earthquake fault can all affect intensities. Intensities are determined from the reports of individuals and assessments of damage caused by the earthquake. The numbers on the map represent relative shaking strength and can by qualitatively interpreted as follows: Some individual reports were for shaking stronger than this; however the map shows averages over a zip-code district and so will not represent the worst shaking in an area. Although there are no higher averages on the Bremerton map, other earthquakes are quite capable of producing stronger shaking. Higher values have the following general characteristics:

Descriptive text adapted from report by Lori Dengler of Humbolt State University

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University of Washington Dept. of Earth and Space Sciences, Box 351310 Seattle, WA, 98195-1310
This is file /SEIS/EQ_Special/WEBDIR_97062319131p/intensity.map.html; modified 6/27/97 - If you see any problems e-mail: seis_web@ess.washington.edu