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Canada Earthquakes of the last 30 days (<= 500 km)
RegionMagnitudeDistance to
Epicenter		Local Time
6 km SE from Val-des-Bois,QC. Aftershoc 1.5 451 km (280 mi) 09/02/2010 9:15pm
15 km W from Fort-Coulonge,QC 1.6 369 km (229 mi) 09/02/2010 7:40pm
6 km SE from Val-des-Bois,QC. Aftershoc 1.7 451 km (280 mi) 09/02/2010 6:45pm
6 km SE from Val-des-Bois,QC. Aftershoc 1.2 451 km (280 mi) 09/02/2010 5:58pm
11 km NW from Saint-Andre-Avellin,QC 2.6 468 km (291 mi) 09/02/2010 10:21am
7 km S from Val-des-Bois,QC. Aftershock 1.3 446 km (277 mi) 08/26/2010 11:29pm
87 km NE from Mattawa,ON 3.3 433 km (269 mi) 08/23/2010 2:41am
10 km SE from Kemptville,ON 1.5 396 km (246 mi) 08/23/2010 1:31am
33 km SE from Fort Erie,ON 2.3 115 km (72 mi) 08/22/2010 4:41pm
15 km SE from Clarington,ON 1.1 128 km (79 mi) 08/22/2010 6:26am
17 km SE from Clarington,ON 2.4 129 km (80 mi) 08/21/2010 6:28am
95 km N from Deep River,ON 1.4 456 km (284 mi) 08/21/2010 6:04am
22 km S from Gananoque,ON 2.0 320 km (199 mi) 08/20/2010 7:32am
9 km SE from Val-des-Bois,QC,aftershoc 1.8 453 km (282 mi) 08/16/2010 2:02am
57 km NW from Maniwaki,QC 1.6 480 km (298 mi) 08/13/2010 4:38am
13 km SW from Les Coteaux,QC 1.8 491 km (305 mi) 08/12/2010 4:34am
3 km S from Temiscaming,QC 2.2 389 km (242 mi) 08/07/2010 10:29am
19 km S from Mont-Laurier,QC 1.4 486 km (302 mi) 08/06/2010 11:38am

In the last 30 days 18 earthquakes were recorded in the 500 km zone.

Natural Resources Canada

Canada Earthquakes of the last 30 days

Last 30 days Canadian Earthquake activity
Earthquake map legend

Natural Resources Canada


Random Weather Facts

Dew Point
The dew point is the temperature to which air must be cooled, at constant barometric pressure, for water vapor to condense into water. The condensed water is called dew. When the dew point temperature falls below freezing it is called the frost point, as the water no longer creates dew but instead creates frost. The dew point is associated with relative humidity. A high relative humidity indicates that the dew point is closer to the current air temperature. If the relative humidity is 100%, the dew point is equal to the current temperature. Given a constant dew point, an increase in temperature will lead to a decrease in relative humidity.