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western quebec and southern ontario - Department of Geology

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Figure 3.2: Number <strong>of</strong> stations used versus frequency <strong>of</strong> the events <strong>and</strong> their cumulativenumber.Figure 3.3 shows the map distribution <strong>of</strong> the studied events (N=50) from 1992 to2010. The events are not uniformly distributed, but instead appear to be concentrated inseveral discrete areas. Among the 50 events studied here only 12 events (m>3.5) occurredin <strong>southern</strong> Ontario, <strong>and</strong> 38 <strong>of</strong> them occurred in <strong>western</strong> Quebec. Most <strong>of</strong> the earthquakesin <strong>western</strong> Quebec are concentrated along the Ottawa River <strong>and</strong> Montreal-Maniwakiregion with a strong NNW-NW trend, transverse to the Appalachians <strong>and</strong> the St.Lawrence River valley. There is no obvious concentration <strong>of</strong> earthquake epicentres in thenorth<strong>western</strong> part <strong>of</strong> the <strong>western</strong> Quebec (Figure 3.3). A similar relative absence <strong>of</strong>earthquakes is also present in the historical data (Chapter 2, Figure 2.3). In <strong>southern</strong>Ontario the earthquakes are concentrated either south <strong>of</strong> Lake Erie or in <strong>western</strong> LakeOntario <strong>and</strong> there is only one event in Georgian Bay (Figure 3.3).28

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