Earthquakes have occurred in Western Australia (WA) on a regular basis throughout its geological history.
In 1849, the first earthquake following European settlement in WA was recorded. "On Saturday last, about a quarter past four o'clock a.m., several inhabitants of Perth were awoke by what they conceived to be a slight shock of an earthquake." [1] [2] [3]
The largest earthquake affecting Western Australia in modern times was an offshore earthquake in 2019, occurring 202 km west of Broome at a magnitude of 6.6 causing minor damage in the town itself. The strongest earthquake with its epicentre on land is the magnitude 6.5 Meckering earthquake of 1968, which caused injuries to at least 17 people and extensive property damage; it was the best-known earthquake in Western Australia the late twentieth century. The previous largest earthquake documented occurred in 1941, at Meeberrie, in the Murchison region. Like many earthquakes it remained little known, due to its lack of impact on urban areas. Initially reported at magnitude 7.2 – 7.3 it was eventually revised down to 6.3 by Geoscience Australia in 2016. The Meckering quake was also revised down from 6.9 to 6.5 in the same year but in the process overtook the Meeberrie quake in strength. [4]
Prior to scientific equipment being utilised to record earthquakes, newspaper reports appear to be the main source of historical information. [5] Perth Observatory was the recording location from 1923 to 1959, when the Mundaring Geophysical Observatory was operated by the Bureau of Mineral Resources between March 1959 and April 2000. [6] Subsequent to the closing of the Mundaring observatory, recording locations are more dispersed throughout the state. [7]
Western Australia's largest recorded onshore earthquake to date was at the Wheatbelt township of Meckering, in October 1968. See the separate section below. The Cadoux earthquake of 1979 with magnitude 6.1 caused surface rupturing, about 15 km (9.3 mi) long. [8]
The Meckering, Calingiri (several during 1970 and 1971) and Cadoux earthquakes led to the identification of a zone of seismicity known as the South West Seismic Zone. [9] This zone has now been significantly mapped and analysed and is the most active zone in Western Australia. [10]
The earthquake which occurred in 1906 about 400 km (250 mi) NW of Exmouth occurred before world earthquake monitoring had really developed. With an estimated magnitude of 7.5, it is probably the largest earthquake known to have occurred in the Australian region. [11] [12]
On 28 August 1917, tremor was reported near midnight in Kalgoorlie, which resulted in an underground rock fall, killing one miner and injuring several others. [9] Also in the 1990s further seismic activity required consideration of seismic activity. [13]
The second largest onshore earthquake to date in Western Australia was on 29 April 1941 at Meeberrie station at 01.35.39 am (Lat −26.90 and Long 115.80). It was initially reported with a magnitude of 7.3 (though some sources give 7.2) but was revised to 6.3 in 2016. [14] [15] [16] [17]
The Meeberrie earthquake was one of the largest to have occurred in Australia. Its Richter magnitude was 7.2 and it was felt over a wide area of Western Australia. Damage from the earthquake was small because of the low population in the epicentral region, but the shaking at Meeberrie homestead was very severe. All the walls of the homestead were cracked, several rainwater tanks burst, & widespread cracking of the ground occurred. Although questionnaires were distributed by the WA Government Astronomer, there has been scant updated information received on known damage. [18] [19]
On 20 April 1946 a magnitude 5.7 earthquake occurred near Yallingup at 9:13 pm on 19 April 1946 (5:13 local time on 20 April), which was felt at Kirup. A tremor was reported at 5:30 am at Caves House Yallingup and at Busselton on 30 April, which is probably the same event, reported on the wrong date. [9]
Gabalong, 30 August 1955, magnitude 5.8 Gabalong, a small community about 30 km (19 mi) east of Moora and 200 km (120 mi) NNE of Perth. The earthquake, at 9:52 pm local time, was felt at MM VI at Yericoin and Miling, and MM V in Moora. It was felt in Perth at intensities between MM II and MM IV, and at Dongara at MM II. It was preceded by a magnitude 5.3 earthquake at the same location at 2:09 pm on the same day. It was a SouthWest Seismic Zone earthquake, and because of the poor location capabilities at the time, may well be related to a series of earthquakes near Yericoin, which started with a magnitude 5.1 earthquake on 2 May 1949. [9]
A magnitude 5.0 earthquake occurred at 12:07 GMT on 3 October (8:07 pm local time) at 34.5 degrees south, 114.5 degrees east. It was felt at Busselton, Yallingup, Margaret River, Bunbury, Cape Naturaliste and Cape Leeuwin. [9]
18 January 1963 at Nourning Spring, approximately 20 km (12 mi) NE of Brookton and approximately 100 km (62 mi) ESE of Perth. It was felt at Intensity VII at Nourning Springs, VI at Brookton, and MM II at Perth. It occurred at 1:49 pm local time, and had a magnitude of 5.4, although it was given a magnitude of 4.9 originally. Many earthquake questionnaires were distributed for this event, and a good isoseismal map was prepared. [9]
On 14 October 1968 at 10:59 am, an earthquake registering 6.9 on the Richter scale occurred 100 km (62 mi) east of Perth in Meckering, Western Australia. [3] Injuring 20 people, causing over 2 million dollars in damage and felt in towns 650 km (400 mi) away, it is Western Australia's most destructive earthquake to date.
The hypocentre occurred 7 km (4.3 mi) below the earth's surface in the Yandanooka/Cape Riche Lineamen region located east of Meckering. The fault trended on a 32 km (20 mi) north-south arc. Through strike-slip the eastern side of the arc shoved 2 m (6 ft 7 in) westward, 1.5 m (4 ft 11 in) upwards and 0.9 m (2 ft 11 in) in a southerly direction which left a distinct trench in its path. This intraplate earthquake is thought to be caused through east–west compressional force within the southwest seismic zone.
24 March 1970, magnitude 6.7 near Lake Tobin in the Canning Basin, was the first in a location which had many more earthquakes over the following years. In all, there were three earthquakes of magnitude 6.0 or more (24 March 1970, M 6.7, 16 July 1971, M6.4 and 3/10/75, M 6.2), and 25 earthquakes of magnitude 5.0 or more, the last of which occurred on 13 February 1982. [9]
An earthquake struck the Wheatbelt town of Calingiri on 10 March 1970 [20] with a magnitude of 5.9. No buildings were damaged despite the epicentre being 3 km (1.9 mi) from the town and the surface being uplifted as much as 30 cm (12 in). [21]
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-lines over an area of 4 ha (9.9 acres). The total amount of damage was around A$3.8 million. [22]
This earthquake, 10 August 1997, magnitude 6.3 just off the WA north coast in Collier Bay, was the largest Australian earthquake since the magnitude 6.7 earthquake near Tennant Creek, in the Northern Territory, in January 1988. [9]
Located near Cadoux (but not on the same physical feature) the Burakin event was named the most significant seismic activity in 40 years. [23]
This very large earthquake on 12 December 2001, magnitude 7.1 occurred about 1,000 km (620 mi) southeast of Albany. It was felt in Albany. It was an intraplate earthquake, as it occurred about 1,000 km (620 mi) north of the (constructive) boundary between the Indo-Australian and Antarctic plates. [9]
On 20 April 2010, a magnitude 5.0 earthquake occurred close to Kalgoorlie. [24] The quake caused damage to a number of hotels along Burt street in Boulder and an underpass also on Burt street collapsed. Work in the Superpit and many other mines around Kalgoorlie was also stopped. [25]
On 16 September 2018 a magnitude 5.7 earthquake occurred with its epicentre close to Lake Muir [26] in the South West region. On 13 October another earthquake with a magnitude of 4.7 was recorded [27] followed by a magnitude 5.4 earthquake on 9 November. [28]
A magnitude 6.6 earthquake struck just over 200 km west-southwest of Broome during the afternoon of the 14 July 2019 at a depth of 10 km. [29] While it is tied for largest earthquake in Australian waters and was felt widely across northern Western Australia the isolation of the quake meant only superficial damage was reported in Broome [30]
On 13 November 2021 a magnitude 5.4 earthquake stuck east of Marble Bar in the evening. The earthquake was 7.3 km deep and was widely felt across the Eastern Pilbara including in Newman, Port Hedland and various mining projects in the area. [31]
The region between Darkan and Wagin, centred on the hamlet of Arthur River has reported over 40 earthquakes since the first event on 5 January 2022, with the strongest so far a magnitude 4.7 on 25 January. It was reported as far away as Busselton and Albany with minor damage reported in Wagin. [32]
The Australian southwest seismic zone (SWSZ) is a north-south trending belt of intra-plate earthquake activity that occurs in the southwest of Western Australia, bounded by 30.5°S to 32.5°S and 115.5°E to 118°E. This is one of the most seismically active areas in Australia, with nine earthquakes over magnitude 5.0 occurring between 1968 and 2002, the largest of these was the M6.5 Meckering earthquake in 1968. Since the SWSZ lies as close as ~150 km (93 mi) from the ~1.4 million population of the Perth region, it poses a distinct seismic hazard.
In seismology, an earthquake swarm is a sequence of seismic events occurring in a local area within a relatively short period. The time span used to define a swarm varies, but may be days, months, or years. Such an energy release is different from the situation when a major earthquake is followed by a series of aftershocks: in earthquake swarms, no single earthquake in the sequence is obviously the main shock. In particular, a cluster of aftershocks occurring after a mainshock is not a swarm.
The 1989 Newcastle earthquake was an intraplate earthquake that occurred in Newcastle, New South Wales on Thursday 28 December. The shock measured 5.6 on the Richter scale and was one of Australia's most serious natural disasters, killing 13 people and injuring more than 160. The damage bill has been estimated at A$4 billion, including an insured loss of about $1 billion.
Calingiri is a town located north-east of Perth, near New Norcia in Western Australia. It is in the Shire of Victoria Plains.
Cadoux is a town in the northeastern Wheatbelt region of Western Australia. It is about 180 kilometres (112 mi) northeast of Perth, within the Shire of Wongan-Ballidu.
Meckering is a town 130 kilometres (80.8 mi) east of Perth, Western Australia along the Great Eastern Highway. Meckering is located within the Shire of Cunderdin.
The 1935 Temiskamingue earthquake occurred on November 1 with a moment magnitude of 6.1 and a maximum Mercalli intensity of VII. The event took place in the Western Quebec Seismic Zone in the Abitibi-Témiscamingue region of Quebec.
The 2009 Dusky Sound earthquake was a Mw 7.8 earthquake that struck a remote region of Fiordland, New Zealand, on 15 July at 21:22 local time. It had an initially–reported depth of 12 km (7.5 mi), and an epicentre near Dusky Sound in Fiordland National Park, which is 160 km (99 mi) north-west of Invercargill. It was the country's largest earthquake magnitude since the 1931 Hawke's Bay earthquake, but caused only minor damage and there were no casualties. A tsunami accompanied the event and had a maximum measured run-up of 230 cm (91 in).
The South West Seismic Zone is a major intraplate earthquake province located in the south west of Western Australia.
The 2010 Kalgoorlie–Boulder earthquake was a 5.2 Mw earthquake that occurred near the city of Kalgoorlie–Boulder, Western Australia on 20 April 2010, at approximately 8:17 am WST.
The 2010 Central Canada earthquake occurred with a moment magnitude of 5.0 in Central Canada on 23 June at about 13:41:41 EDT and lasted about 30 seconds. The epicentre was situated approximately 56 kilometres (35 mi) north of Ottawa, Ontario, in the municipality of Val-des-Bois, Quebec. Canada's capital, Ottawa, declared this earthquake as being its most powerful in 65 years.
The 1967 Mudurnu earthquake or more correctly, the 1967 Mudurnu Valley earthquake occurred at about 18:57 local time on 22 July near Mudurnu, Bolu Province, north-western Turkey. The magnitude 7.4 Mw earthquake was one of a series of major and intermediate quakes that have occurred in modern times along the North Anatolian Fault since 1939.
The 2011 Lorca earthquake was a moderate 5.1 Mw earthquake that occurred 6:47 p.m. CEST on 11 May 2011, near the town of Lorca, causing significant localized damage in the Region of Murcia, Spain, and panic among locals, and displacing many from their homes. The quake was preceded by a magnitude 4.4 foreshock at 17:05, that inflicted substantial damage to many older structures in the area, including the historical Espolón Tower of Lorca Castle, the Hermitage of San Clemente and the Convent of Virgen de Las Huertas. Three people were killed by a falling cornice. A total of nine deaths have been confirmed, while dozens are reported injured. The earthquake was the worst to hit the region since a 5.0 Mw tremor struck west of Albolote, Granada in 1956.
The 2014 Orkney earthquake occurred at 12:22:33 SAST on 5 August, with the epicentre near Orkney, a gold mining town in the Klerksdorp district in the North West province of South Africa. The shock was assigned a magnitude of 5.5 on the Richter scale by the Council for Geoscience (CGS) in South Africa, making it the biggest earthquake in South Africa since the 1969 Tulbagh earthquake, which had a magnitude of 6.3 on the Richter scale. The United States Geological Survey (USGS) estimated a focal depth of 5.0 km (3.1 mi). The CGS reported 84 aftershocks on 5 August and 31 aftershocks on 6 August, with a magnitude of 1.0 to 3.8 on the Richter scale. According to the CGS, the earthquake is the biggest mining-related earthquake in South African history.
The Western Australian town of Meckering was struck by an earthquake on 14 October 1968. The earthquake occurred at 10:58:52 local time, with a moment magnitude of 6.5 and a maximum Mercalli intensity of IX (Violent). Total damage amounted to $2.2 million with 20–28 injured.
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An earthquake struck approximately 53 kilometres SSE of the town of Mansfield, in the Victorian Alps of Australia on 22 September 2021, at 09:15 local time. The earthquake measured 5.9 on the moment magnitude scale. The earthquake caused minor structural damage in parts of Melbourne and left one person injured. The earthquake was also felt in New South Wales, Australian Capital Territory, South Australia and Tasmania. The earthquake was substantially stronger than the 1989 Newcastle earthquake that measured 5.6 and killed 13 people.
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