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1989 Ungava earthquake

From Wikipedia, the free encyclopedia

1989 Ungava earthquake
UTC time1989-12-25 14:24:34
ISC event384953
Local date25 December 1989 (1989-12-25)
Local time09:24:34
Magnitude6.3 Ms, 6.0 Mw
Depth<5 km
Epicenter60°07′N 73°36′W / 60.12°N 73.60°W / 60.12; -73.60
Areas affectedCanada
Max. intensityIV (Light)
Foreshocks5.1 mb(PDE)  1989-12-25 04:25

The 1989 Ungava earthquake occurred at 09:24 local time (14:24 UTC) on 25 December to the north of Lac Bécard in a remote part of the Ungava Peninsula in northern Quebec.[1] It had a magnitude of 6.3 on the surface wave magnitude scale and 6.2–6.5 on the moment magnitude scale and a maximum felt intensity of only IV (Light) on the Mercalli intensity scale, due to its remoteness from any inhabited areas.[2] The mainshock was preceded by a magnitude 5.1 foreshock ten hours earlier. It was the first earthquake in eastern North America known to be associated with ground rupture.[1]

Tectonic setting

The northern part of Quebec lies mainly on the Minto block of the Superior craton. The earthquake occurred within the Utsalik domain, which consists mainly of Archean granitic and granodioritic rocks.[3] A number of northerly trending brittle faults zones have been recognized in the domain. The area has been tectonically quiescent since the Archean. However, like most of the Canadian shield, it is currently experiencing post-glacial rebound.[4]


The mainshock was preceded by a series of foreshocks, starting with a M 5.1 event about ten hours earlier. The hypocentral depth was very shallow, less than five kilometers.[1]

Modelling of seismic waveforms shows that the earthquake was caused by two sub-events, a thrust event followed almost immediately by a strike-slip event.[5] The surface offsets show consistent thrust faulting over a distance of 8.5 km, with a maximum displacement of 1.8 m near the centre of the zone. The fault zone has a strike of N 038° E.[1] There is no evidence of previous rupture along the fault zone.[5]

The NW-SE orientation of the maximum horizontal stress derived from the observed focal mechanism is at a high angle to the regional stress field for North America. It has been suggested that this compression is a result of the area being in a 'saddle zone' between two centres of post-glacial uplift.[4]


  1. ^ a b c d Natural Resources Canada (7 November 2011). "The Lac Turquoise Fault Scarp". Retrieved 3 December 2011.
  2. ^ Lamontagne, M.; Halchuk, S.; Cassidy, J.F.; Rogers G.C. (2007). Significant Canadian Earthquakes 1600–2006. Open File. 5539. Geological Survey of Canada.
  3. ^ Percival, J.A.; Skulski, T.; Nadeau, L. (1997). Reconnaissance geology of the Pelican-Nantais belt, northeastern Superior Province, Quebec. Open File. 3525. Geological Survey of Canada.
  4. ^ a b Muir-Wood, R. (2000). "Deglaciation Seismotectonics: a principal influence on intraplate seismogenesis at high latitudes". Quaternary Science Reviews. 19 (14–15): 1399–1411. Bibcode:2000QSRv...19.1399M. doi:10.1016/S0277-3791(00)00069-X.
  5. ^ a b Bent, A.L. (1994). "The 1989 (MS 6.3) Ungava, Quebec, earthquake: a complex intraplate event". Bulletin of the Seismological Society of America. 84 (4): 1075–1088. Retrieved 3 December 2011.

External links

This page was last edited on 15 June 2020, at 21:40
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