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  1. The former Montreal East City Hall suffered severe damage to the masonry cladding. Note that the structure is founded on 17 metres of clay and had suffered from excessive settlements prior to the earthquake. References. Drysdale, J. and Cajka, M., 1989. Intensity Report of the November 25, 1988 Saguenay, Quebec Earthquake. GSC Open File Report ...

  2. ABSTRACT. On Friday November 25, 1988 the largest earthquake in eastern North America in 53 years occurred 35 km south of Chicoutimi, Québec and 75 km north of the Charlevoix-Kamouraska earthquake zone. This earthquake, referred to as the Saguenay earthquake, was located in a relatively aseismic region, had a calculated magnitude of 5.9 mb, 6. ...

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  4. The Saguenay earthquake of 25 November 1988 occurred close to the southern margin of the Saguenay Graben in southern Quebec. It was caused by almost purely dip-slip faulting centered at a depth of 26 km with a P axis oriented northeast-southwest. This faulting mechanism is similar to those of the larger historical earthquakes in eastern North ...

    • Paul G. Somerville, James P. McLaren, Chandan K. Saikia, Donald V. Helmberger
    • 1990
  5. The November 25, 1988, moment magnitude 5.9 (M. w) Saguenay earthquake is one of the largest eastern Canadian earthquakes of the 20thcentury. It was preceded by a magnitude (M. N) 4.7 foreshock and followed by very few aftershocks considering the magnitude of the main shock. The largest aftershock was a magnitude (M.

  6. Felt reports and impact of the November 25, 1988, magnitude 5.9 Saguenay, Quebec earthquake sequence / M. Lamontagne, K.B.S. Burke, and L. Olson.: M183-2/8803E-PDF "The November 25, 1988, moment magnitude 5.9 (Mw) Saguenay earthquake is one of the largest eastern Canadian earthquakes of the 20th century.

    • Geological Survey of Canada, issuing body.
    • Series-View Master Record
    • [English]
    • Open file, 2816-7155 ; 8803
  7. Feb 1, 1991 · The November 25, 1988, Saguenay earthquake (m b 5.9) occurred at 23:46:04.5 U.T. outside previously known seismic source-zones in eastern Canada.The event is also peculiar due to its 29 km depth in the lower crust of the “stable” Precambrian craton of the Canadian Shield, its low aftershock activity (84 earthquakes over 6 months), its high Lg wave energy (m b Lg 6.5) and its extensive felt ...

  8. "The most significant earthquake in over fifty years in eastern North America took place on November 25, 1988. The event was centered north of Quebec City in the Province of Quebec, Canada. The purpose of this open file report is to present the strong motion data recorded from this event by the Eastern Canada Strong Motion Seismograph Network ...