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The May 2022 Canadian derecho was a high-impact derecho [5] event that affected the Quebec City-Windsor Corridor, Canada's most densely populated region, on May 21, 2022.. Described by meteorologists as a historic derecho and one of the most impactful thunderstorms in Canadian history, [6] [7] winds up to 190 km/h (120 mph) as well as around four tornadoes caused widespread and extensive ...
2022 January 13 2022 Ottawa Eastway tank explosion Fire Ottawa, Ontario: Eastern and Central Canada 6 2 Industrial explosion [47] [48] [49] 2022 September 23–24 Hurricane Fiona: Hurricane Atlantic Canada: Eastern Canada 3 $660 million in insured damage making Fiona the most costly storm to hit Canada [50] [51] 2023 February 13 2023 East ...
Pages in category "Landslides in 2022" The following 21 pages are in this category, out of 21 total. This list may not reflect recent changes. 0–9. 2022 Africa floods;
Using laser scans and GPS cameras, accurate down to one inch, the U.S. Geological Survey has so far mapped more than 600 landslides caused by Hurricane Helene.
A landslide in which the sliding surface is located within the soil mantle or weathered bedrock (typically to a depth from few decimeters to some meters) is called a shallow landslide. Debris slides and debris flows are usually shallow. Shallow landslides can often happen in areas that have slopes with high permeable soils on top of low ...
Historical maps of the ancient landslide complex, ... Phipps notes that the area is still shifting about 88 times faster than it was in October 2022, when he was measuring movement on the order of ...
Pages in category "Landslides in Canada" The following 15 pages are in this category, out of 15 total. This list may not reflect recent changes. C.
The landslide was caused by the presence of pre-existing tectonic structures (faults and shear zones) within the southwestern slope of Johnson Ridge. [14] The lower parts of the slide scar are underlain by felsite sheets (which may have failed first) while the upper parts of the slide scar are underlain by highly jointed Paleozoic greenstone beds. [3]