Jump to content

1935 Timiskaming earthquake

From Wikipedia, the free encyclopedia

This is an old revision of this page, as edited by Liz (talk | contribs) at 13:07, 10 January 2014 Category:Earthquakes in Quebec; ±Category:Earthquakes in Ontario using HotCat). The present address (URL) is a permanent link to this revision, which may differ significantly from the current revision.

1935 Temiskamingue earthquake
Lua error in Module:Location_map at line 526: Unable to find the specified location map definition: "Module:Location map/data/Quebec (conic)" does not exist.
UTC time??
Magnitude6.2 Mw
Depth200 km (124 mi)
Epicenter46°47′00″N 79°04′00″W / 46.78333°N 79.066667°W / 46.78333; -79.066667[1]
Areas affected Canada
Max. intensityVII - Very Strong

The 1935 Temiskamingue earthquake was a magnitude 6.2 earthquake that occurred on November 1, 1935 in the Abitibi-Témiscamingue region of Quebec. It is one of the major earthquakes that have occurred in the Western Quebec Seismic Zone.[2]

Earthquake

The earthquake had its epicentre on a thrust fault in the Ottawa-Bonnechere Graben, approximately 10 kilometres north east of Témiscamingue, and occurred at 1:03 a.m. ET. The earthquake was felt over a wide swath of North America, extending west to Fort William (now Thunder Bay), east to Fredericton, New Brunswick, north to James Bay and south as far as Kentucky and West Virginia. Occasional aftershocks were also reported for several months following the earthquake.

Damage

Although the most significant damage connected to the earthquake was to chimneys, both in the immediate area and as far south as North Bay and Mattawa, a railroad embankment near Parent, 300 km away, also collapsed as a result of the earthquake. Researcher E. A. Hodgson later concluded that the embankment slide was already imminent, and was merely hastened by the earthquake vibrations.[3] Some rockfalls and structural cracks were also reported, although there were few major structural collapses aside from the Parent embankment. The relative lack of major damage, despite the fact that it was a strong earthquake, has been attributed primarily to the sparseness of the area's population.

Other events

The 2000 Kipawa earthquake on January 1, with a magnitude of 5.2, had its epicentre at Lake Kipawa, very near the epicentre of the 1935 quake.

References

  1. ^ The Temiskamingue Earthquake of November 1, 1935. The Location of the Epicentre and Determination of Focal Depth. Hodgson, E. A. Journal of the Royal Astronomical Society of Canada, 1936, Vol. 30, pp.120
  2. ^ The Western Quebec Seismic Zone
  3. ^ Hodgson, Ernest A. (1937) "Progress Report on the Research Connected with the Timiskaming Earthquake of November 1, 1935" Earthquake Notes 8: p. 76
Sources
  • Adams, John; Vonk, Andrew (2009), The November 1, 1935, M 6.2 Timiskaming earthquake, its aftershocks, and subsequent seismicity (PDF), Open File 6207, Geological Survey of Canada