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On 2 June 1979 the second-most damaging earthquake in Western Australia's recorded history hit with a magnitude of 6.1. The epicentre was close to the town of Cadoux in the Wheatbelt region about 165 km (103 mi) north east of Perth, Western Australia. One person was injured and 25 buildings were damaged along with roads, railways and power ...
The South West seismic zone (also identified as SWSZ) is a major intraplate earthquake province located in the south west of Western Australia. [1] [2] [3]It was known earlier as the Yandanooka–Cape Riche Lineament, [4] including the physiographic boundary known as the Meckering Line, and also the junction between Swanland [clarification needed] and Salinaland [clarification needed].
1858 Hietsu earthquake (M~7) Awatere Fault: 200: South Island, New Zealand: Dextral strike-slip: Active: 1848 Marlborough (M7.5) Azores–Gibraltar transform fault: 2250: Azores to Strait of Gibraltar: Dextral strike-slip: Active: 1755 Lisbon earthquake (est. M7.7–9.0), 1969 Cape St. Vincent (M7.9), 1941 Gloria Fault (M8.0) Baikal Rift Zone ...
Western Australia: Canning Basin: 1975-10-03 6.2 Part of a sequence of c. 25 quakes of magnitude 5.0 or greater in the Canning Basin area of northern Western Australia between 1970 and 1982 [27] Victoria: Balliang: 1977-12-02 4.7 1 Felt strongly in Geelong and across the suburbs of Melbourne, caused minor damage in the Anakie area. [29] Western ...
Pages in category "Earthquakes in Western Australia" The following 8 pages are in this category, out of 8 total. This list may not reflect recent changes. ...
Category: Earthquakes in Europe by country. ... Earthquakes in the United Kingdom (1 C, 12 P) This page was last edited on 24 June 2020, at 04:03 (UTC). Text ...
The 2010 Kalgoorlie–Boulder earthquake was a 5.2 M w earthquake that occurred near the city of Kalgoorlie–Boulder, Western Australia on 20 April 2010, at approximately 8:17 am WST. [3] [4] [1] [5] The earthquake caused major damage to the historic buildings in Kalgoorlie–Boulder.
Earthquake epicenters 1963–98. In seismology, a seismic zone or seismic belt is an area of seismicity potentially sharing a common cause. It can be referred to as an earthquake belt as well. It may also be a region on a map for which a common areal rate of seismicity is assumed for the purpose of calculating probabilistic ground motions.