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Isoseismal Maps An isoseismal map shows the Modified Mercalli Intensities (MMI) reported from a particular earthquake. To use the metaphor of a lightbulb; an earthquake has a fixed magnitude (the Watt rating of the bulb), but the intensity varies with distance (the brightness of the light). By plotting intensities, we may learn more about the mechanisms for earthquakes in those areas. Isoseismal maps are derived from "felt reports" - accounts from people who felt the earthquake. We also ask people to fill in these reports when they are in the earthquake area and did not feel it, as this may reveal something about the local geology. Below are some isoseismal maps from earthquakes in our area of operation.
Although seismographs have been operated in Australia for over 100 years, until about 1960 these were optimised to record large distant earthquakes. They were too insensitive, and there were too few of them to record most local earthquakes. The locations and magnitudes of most Australian earthquakes before 1960 were estimated using earthquake intensity reports. Many of these have been summarised in one of three earthquake atlases published by the Australian Geological Survey Organisation. Atlas of Isoseismal Maps of Australian Earthquakes Part 1, 1982, BMR Bulletin 214, compiled by I.B. Everingham, A.J. McEwin and D. Denham.
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