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 ]. [5] [6]
The zone exists within an Archaean Shield structure called the Yilgarn Block. [7] The identified geological subdivisions within this Precambrian structure do not show an obvious relation to the seismicity. [8]
The zone represents a significant seismic hazard to Perth. [2] More than six thousand earthquakes have occurred in the SWSZ in the years 1968 – 2002. [8] Meckering, Cadoux and Burakin earthquakes originated in the SWSZ. More recent events have occurred to the south in Lake Muir in 2018 [9] [10] [11] [12] and Arthur River in 2022. [13]
The zone and the explanation of it, has been titled Perthquake in the Catalyst programme on the ABC in 2001. [14]
Temporal variation of the events in the region have been analysed over time. [15] [16] In the 2000s, monitoring and instrumentation was developed in the region. [17] [18]
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 M6.8 Meckering earthquake in 1968. Since the SWSZ lies as close as ~150 km from the ~1.4 million population of the Perth region, it poses a distinct seismic hazard.
Mundaring is a suburb located 34 km east of Perth, Western Australia on the Great Eastern Highway. The suburb is located within the Shire of Mundaring.
The New Madrid seismic zone (NMSZ), sometimes called the New Madrid fault line, is a major seismic zone and a prolific source of intraplate earthquakes in the Southern and Midwestern United States, stretching to the southwest from New Madrid, Missouri.
The Yarrabubba impact structure is the eroded remnant of an impact crater, situated in the northern Yilgarn Craton near Yarrabubba Station between the towns of Sandstone and Meekatharra, Mid West Western Australia. With an age of 2.229 billion years, it is the oldest known impact structure on Earth.
The Australian plate is a major tectonic plate in the eastern and, largely, southern hemispheres. Originally a part of the ancient continent of Gondwana, Australia remained connected to India and Antarctica until approximately 100 million years ago when India broke away and began moving north. Australia and Antarctica had begun rifting by 96 million years ago and completely separated a while after this, some believing as recently as 45 million years ago, but most accepting presently that this had occurred by 60 million years ago.
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.
Lake Muir is a freshwater lake, with a larger surrounding wetlands area, that is located in the South West region of Western Australia. The lake lies near Muir Highway, north of Walpole and southeast of Manjimup.
The Yilgarn Craton is a large craton that constitutes a major part of the Western Australian land mass. It is bounded by a mixture of sedimentary basins and Proterozoic fold and thrust belts. Zircon grains in the Jack Hills, Narryer Terrane have been dated at ~4.27 Ga, with one detrital zircon dated as old as 4.4 Ga.
The geology of Australia includes virtually all known rock types, spanning a geological time period of over 3.8 billion years, including some of the oldest rocks on earth. Australia is a continent situated on the Indo-Australian Plate.
The Perth Basin is a thick, elongated sedimentary basin in Western Australia. It lies beneath the Swan Coastal Plain west of the Darling Scarp, representing the western limit of the much older Yilgarn Craton, and extends further west offshore. Cities and towns including Perth, Busselton, Bunbury, Mandurah and Geraldton are built over the Perth Basin.
The Australian Shield is a geological feature known as a shield that occupies more than half of the continent of Australia. The word shield is used because it refers to ancient, molten rock which has cooled and solidified.
Western Australia has the longest coastline of any state or territory in Australia, at 10,194 km or 12,889 km. It is a significant portion of the coastline of Australia, which is 35,877 km.
The New Hebrides plate, sometimes called the Neo-Hebridean plate, is a minor tectonic plate located in the Pacific Ocean. While most of it is submerged as the sea bottom of the North Fiji Basin, the island country of Vanuatu, with multiple arc volcanoes, is on the western edge of the plate. It is bounded on the south-west by the Australian plate, which is subducting below it at the New Hebrides Trench. The Vanuatu subduction zone is seismically active, producing many earthquakes of magnitude 7 or higher. To its north is the Pacific plate, north-east the Balmoral Reef plate and to its east the Conway Reef plate.
The South Bismarck plate is a small tectonic plate located mainly in the southern Bismarck Sea. The eastern part of New Guinea and the island of New Britain are on this plate. It is associated with high earthquake and volcanic activity as part of the New Britain subduction zone within the Pacific Ring of Fire.
Earthquakes have occurred in Western Australia (WA) on a regular basis throughout its geological 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.
On 22 January 1988, a sequence of destructive earthquakes measuring 6.2, 6.3, and 6.6 struck southwest of Tennant Creek, Australia which was felt as far north as Darwin and in other regions of the country. The largest event of the sequence was the largest earthquake ever recorded in mainland Australia since records began in 1800. An intensity of IX (Violent) was observed. Despite the large magnitude of the earthquakes and a close proximity to a town, in a country where earthquakes of this size are not common, damages were limited. Thousands of aftershocks were reported and felt across the Northern Territory.
Meghan S. Miller is a Canadian geoscientist based in Australia, who studies the structural and dynamical evolution of the Earth. She is a professor in the School of Earth Sciences at the Australian National University and the program leader of the AuScope Earth Imaging & Sounding program.