Earthquake

What is an earthquake?

Earthquakes are the vibrations caused by rocks breaking under stress. The underground surface along which the rock breaks and moves is called a fault plane.

The focus, or “hypocentre”, of an earthquake is the point where it originated within the Earth. The point on the Earth's surface directly above the focus is called the earthquake epicentre.

The size or magnitude of earthquakes is determined by measuring the amplitude of the seismic waves recorded on a seismograph and the distance of the seismograph from the earthquake. These are put into a formula which converts them to a magnitude, which is a measure of the energy released by the earthquake. For every unit increase in magnitude, there is roughly a thirty-fold increase in the energy released. For instance, a magnitude 6.0 earthquake releases approximately 30 times more energy than a magnitude 5.0 earthquake, while a magnitude 7.0 earthquake releases approximately 900 times (30x30) more energy than a magnitude 5.0.

A magnitude 8.6 earthquake releases energy equivalent to about 10 000 atomic bombs of the type developed in World War II. Fortunately, smaller earthquakes occur much more frequently than large ones and most cause little or no damage.

Earthquake magnitude was traditionally measured on the Richter scale. It is often now calculated from seismic moment, which is proportional to the fault area multiplied by the average displacement on the fault.

The focus of an earthquake is the point where it originated within the Earth. The point on the Earth's surface directly above the focus is called the earthquake epicentre.

Where do earthquakes occur?

No part of Earth's surface is free from earthquakes, but some regions experience them more frequently. They are most common at tectonic plate boundaries where different plates meet. The largest events usually happen where two plates are colliding, or colliding and sliding past one another. They particularly occur around the edge of the Pacific Plate, for example in New Zealand, Vanuatu, the Solomon Islands, Papua New Guinea, Japan and the Americas, and in Indonesia, where the Indo-Australian Plate collides with the Eurasian Plate. The depths of focus in these collision zones can range from the surface-700 km.

Large shallow earthquakes also happen where two plates are pulling apart with the creation of new oceanic crust along mid-ocean ridges and on the transform faults that intersect them.

Shallow intraplate earthquakes occur in the relatively stable interior of continents away from plate boundaries. They are less common and do not follow easily recognisable patterns. This type of earthquake generally originates at shallow depths.

Although Australia is not on the edge of a plate, the continent experiences earthquakes because the Indo-Australian plate is being pushed north and is colliding with the Eurasian, Philippine and Pacific plates. This causes the build up of mainly compressive stress in the interior of the Indo-Australian plate which is released during earthquakes.

Australia's largest recorded earthquake was in 1988 at Tennant Creek in the Northern Territory, with an estimated magnitude 6.6, but it occurred in a sparsely populated area. A magnitude 6.5 earthquake at Meckering in 1968 caused extensive damage to buildings and was felt over most of southern Western Australia. Earthquakes of magnitude 4.0 or more are relatively common in Western Australia, with one occurring approximately every five years in the Meckering region.

Why do we get earthquakes in Australia?

Australia experiences considerably fewer earthquakes than other parts of the world near tectonic plate boundaries, where large earthquakes occur more frequently. However, there are on average 100 earthquakes of magnitude 3 or more in Australia each year. Earthquakes above magnitude 5.0, such as the destructive 1989 Newcastle earthquake, occur on average every one-to-two years; and about every ten years, Australia experiences a potentially damaging earthquake of magnitude 6.0 or more such as the Mw 6.5 Meckering earthquake in October 1968.

Although Australia is not on the edge of a plate, the Australian plate is the fastest moving continental land mass on Earth and is colliding into the Pacific plate to Australia's north and east, and the Eurasian Plate to the northwest. This causes mainly compressive stress in the interior of the Australian continent, that slowly builds up across the plate as it moves northeast about 7cm per year. Australia's earthquakes are caused by the sudden release of this stress when rocks deep underground break and move along a fault line. While some parts of the country are more likely to experience earthquakes than others, large earthquakes can occur anywhere across the continent, and without warning.

This video shows a short time lapse of earthquakes in Australia during 2014. For more information on historic earthquakes in Australia, see the earthquake story map.

What is Geoscience Australia's role in reducing risk to Australians from earthquakes?

Aligning with Geoscience Australia’s Strategy 2028, Geoscience Australia provides earthquake risk information to help Australians understand the consequences of earthquakes, which contributes to more resilient communities now and in the future. Geoscience Australia’s capability spans the earthquake value chain from observations (through the Australian National Seismograph Network), to 24/7 monitoring and alerting (via the National Earthquake Alert Centre), to national hazard (through the National Seismic Hazard Assessment) and vulnerability (through earthquake damage models). Geoscience Australia collaborates with a range of stakeholders in Australia and through Australia’s overseas aid program to apply this value chain to develop actionable earthquake risk data and information to support evidence based decisions for disaster risk reduction. We do this by:

  • developing nationally consistent data, information and advice to enable informed decisions on preparedness and response to the impact of earthquakes
  • advancing our understanding of Australia’s earthquake hazard and vulnerability of the built environment to support mitigation and reduce the cost of disasters
  • providing ongoing real-time monitoring, analysis and advice on significant earthquakes and potentially tsunamigenic earthquakes to help safeguard Australian and Indian Ocean communities.

How do we record earthquakes?

Geoscience Australia monitors, analyses and reports on significant earthquakes to alert the Australian Government, State and Territory Governments and the public about earthquakes in Australia and overseas.

Earthquakes are detected by scientific instruments called seismometers. The word seismo originates from the Greek word seismos which means to shake or move violently and was later applied to the science and equipment associated with earthquakes. Seismographs, such as the Teledyne Geotech Helicorder, were used in the past to detect earthquake activity and relied on a mechanical system to record the seismic energy in the Earth onto paper. In contrast, modern seismometers such as the raspberry shake (pictured) detect and convert any small movement in the Earth into an electrical signal for use in computer systems, as shown in the digital seismogram image of seven seismic sensors which detected the magnitude 5.4 earthquake near Moe in Victoria on 19 June 2012.

Determining the location of an earthquake

The accurate locations of seismometers are stored in a database accessible by an earthquake monitoring computer system. The system also has access to crustal velocity models which provide approximate information on how fast the various earthquake waves travel through the different layers which make up the Earth in the area between the earthquake and the seismometers. The times at which the differing seismic waves arrive at various seismometers are identified by Seismic Analysts or by a computer system. The arrival times of the seismic waves at the seismometers, together with the locations of the seismometers and the speed at which the seismic waves travel to the seismometers are all used to determine the location of the earthquake. This location is also known as its focus or hypocentre which is represented by the latitude, longitude and depth below the surface.

How does Geoscience Australia monitor earthquakes?

Geoscience Australia monitors seismic data from more than 60 stations on the Australian National Seismograph Network and in excess of 300 stations worldwide in near real-time, 24 hours a day, seven days a week. Most of the 40 samples per second data are delivered within 30 seconds of being recorded at the seismometer to Geoscience Australia’s central processing facility in Canberra through various digital satellite and broadband communication systems.

Seismic data are also provided by overseas Governments which have national seismic networks. Geoscience Australia uses data provided by the Governments of New Zealand, Indonesia, Malaysia, Singapore and China and has access to data from global seismic networks provided by the USA, Japan, Germany and France. The Comprehensive Nuclear Test Ban Treaty Organisation’s International Monitoring System also provides seismic data for tsunami warning purposes.

The seismic data are collected and analysed automatically and immediately reviewed by Geoscience Australia’s Duty Seismologist.

As part of the Joint Australian Tsunami Warning Centre (JATWC), Duty Seismologists also are responsible for analysing and reporting within 10 minutes of the origin time, on earthquakes which have the potential to generate a tsunami. An earthquake alert is then sent to Geoscience Australia’s partner in the JATWC, the Australian Bureau of Meteorology, to determine tsunami advice and publish tsunami bulletins.

The parameters of all other earthquakes with a magnitude greater than 3.5 are generally computed within 20 minutes. The analysis includes its magnitude, origin time and date of the earthquake and the location of its hypocentre. Smaller earthquakes that are not detected by many seismometers are difficult to locate in real-time and, consequently, are located by Seismic Analysts.

What are the impacts of earthquakes?

The amplitude of the shaking caused by an earthquake depends on many factors, such as the magnitude, distance from the epicentre, depth of focus, topography and the local ground conditions.

In Australia, earthquakes with magnitudes of less than 3.5 seldom cause damage, and the smallest magnitude earthquake known to have caused fatalities is the magnitude Mw 5.4 (ML5.6) Newcastle earthquake in 1989. However, magnitude 4.0 earthquakes occasionally topple chimneys or result in other damage which could potentially cause injuries or fatalities.

Apart from causing shaking, earthquakes of magnitude 4.0 or greater can also trigger landslides, which can cause casualties. The larger the magnitude of the earthquake, the bigger the area over which landslides may occur.

In areas underlain by water-saturated sediments, large earthquakes, usually magnitude 6.0 or greater, may cause liquefaction. The shaking causes the wet sediment to become quicksand and flow. Subsidence from this can cause buildings to topple, and the sediment might erupt at the surface from craters and fountains.

Undersea earthquakes can cause a tsunami, or a series of waves which can cross an ocean and cause extensive damage to coastal regions.

The destruction from strong earthquake shaking can be worsened by fires caused by downed power lines and ruptured gas mains.

Earthquake effects, based on human observation, are rated using the Modified Mercalli (MM) intensity scale, which ranges from I (imperceptible) up to XII (total destruction) (see table below).

The Modified Mercalli Intensity (MMI) scale

Intensity Shaking Description/Damage
I Not felt Not felt except by a very few under especially favorable conditions.
II Weak Felt only by a few persons at rest,especially on upper floors of buildings.
III Weak Felt quite noticeably by persons indoors, especially on upper floors of buildings. Many people do not recognize it as an earthquake. Standing motor cars may rock slightly. Vibrations similar to the passing of a truck. Duration estimated.
IV Light Felt indoors by many, outdoors by few during the day. At night, some awakened. Dishes, windows, doors disturbed; walls make cracking sound. Sensation like heavy truck striking building. Standing motor cars rocked noticeably.
V Moderate Felt by nearly everyone; many awakened. Some dishes, windows broken. Unstable objects overturned. Pendulum clocks may stop.
VI Strong Felt by all, many frightened. Some heavy furniture moved; a few instances of fallen plaster. Damage slight.
VII Very strong Damage negligible in buildings of good design and construction; slight to moderate in well-built ordinary structures; considerable damage in poorly built or badly designed structures; some chimneys broken.
VIII Severe Damage slight in specially designed structures; considerable damage in ordinary substantial buildings with partial collapse. Damage great in poorly built structures. Fall of chimneys, factory stacks, columns, monuments, walls. Heavy furniture overturned.
IX Violent Damage considerable in specially designed structures; well-designed frame structures thrown out of plumb. Damage great in substantial buildings, with partial collapse. Buildings shifted off foundations.
X Extreme Some well-built wooden structures destroyed; most masonry and frame structures destroyed with foundations. Rails bent.

Source: Replicated from the USGS https://earthquake.usgs.gov/learn/topics/mercalli.php

Magnitude vs Intensity

  • Earthquake magnitude is related to the energy released over its ruptured fault area
  • The intensity of an earthquake refers to the level of ground-shaking at a given location
  • Earthquake intensity decreases with increasing distance away from an earthquake
  • The Modified Mercalli Intensity (MMI) scale is commonly used to describe the damage and felt effects of an earthquake at a given location
  • MMI is a qualitative assessment of earthquake effects on structures and people
  • Earthquake magnitude is a quantitative measure based on physical recordings made on seismometers

How does Geoscience Australia use earthquake data to communicate and reduce seismic risk?

Focus on earthquakes in Papua New Guinea

Papua New Guinea (PNG) is located at the edge of the Pacific “ring of fire” and is exposed to frequent large earthquakes and volcanic eruptions. Earthquakes in PNG, such as the 2018 New Guinea Highland event (Mw7.5), continue to cause loss of life and widespread damage to buildings and infrastructure. Geoscience Australia has a long history of partnering with the PNG Government, through the Australian Aid program.

Currently Geoscience Australia and PNG are working together on three earthquake related activities.

A low-cost seismic network for Papua New Guinea

The seismic network in PNG is currently very sparse and expansion of the network is cost prohibitive. Geoscience Australia is working with partners in PNG to expand the national earthquake monitoring network. We are doing this by deploying new seismic stations in currently unmonitored regions. As part of this work Geoscience Australia is trialling establishing a low-cost, community-based seismic network by deploying sensors such as the Raspberry Shake 4D seismograph.

Moving Towards Resilient Building Design

Geoscience Australia partnered with PNG to revise the PNG Probabilistic Seismic Hazard Assessment in 2019. For this revision a new seismotectonic model for PNG was developed, which includes 18 earthquake fault models, to give a more detailed understanding of earthquake hazard in PNG.

Geoscience Australia is now working with the PNG Government to update the Building Code in PNG to incorporate the new seismic hazard information that has been generated.

Communication of Earthquake Hazard

Communicating hazard to the PNG Government and the community is an area that requires further effort in PNG. Geoscience Australia will work with PNG partners to improve this in a number of ways. Development of automated earthquake bulletins and near real time products such as Shakemap will provide improved communication of earthquake hazard immediately after events in PNG.

Earthquake Impact and Risk Assessment for Perth and Supporting infrastructure (EIRAPSI)

Geoscience Australia is collaborating with four Western Australian government partners and the Global Earthquake Model Foundation (GEM) in Pavia, Italy, to develop an understanding of earthquake risk in the Perth region. Earthquake hazard has been largely ignored for most of Australia’s settled history, resulting in a significant legacy of vulnerable infrastructure, and this project is examining the implications of this. The WA partners are the Department of Fire and Emergency Services (DFES), Main Roads WA, Western Power and Water Corporation.

The two and half year project commenced in January 2017, with the six partner collaboration bringing together best earthquake risk science and industry expertise to generate actionable analysis that can inform risk management, including mitigation investment. The project is using the latest understanding of Australian earthquake hazard developed by Geoscience Australian in the 2018 National Seismic Hazard Assessment. This collaborative work is also utilising an asset exposure database (NEXIS), which is the most detailed developed by Geoscience Australia to date for a major city.

The project has included the modelling of earthquake scenario events to assist emergency managers in understanding the consequences of credible events that have not been experienced to date, thus informing better planning of response preparedness. This scenario modelling work underpinned the ‘2018 East Asia Summit: International Disaster Assistance Workshop’ (May 2018) which has informed Australian arrangements for accessing regional assistance following a catastrophic disaster.

Infrastructure facilities have been a key focus, with the influence of vulnerable components being assessed from a system disruption perspective using Geoscience Australia’s analytical tool SIFRA (System or Infrastructure Facility Resilience Analysis). This analysis will provide a body of actionable information for industry for consideration in targeted mitigation investments.

Finally, the project is providing insights on the resilience of communities and their recovery needs after a major earthquake. This research is utilising research in the Bushfire and Natural Hazards CRC, led by the University of New England, that has developed a local scale resilience index called the Australian Disaster Resilience Index (ANDRI).

The EIRAPSI project has been co-funded by the Global Earthquake Model Foundation and Geoscience Australia.

Earthquake Mitigation Case Study for Regional Town of York, WA

Geoscience Australia is collaborating with the University of Adelaide, the University of Western Australia, the WA Department of Fire and Emergency Services (DFES) and the Shire of York, WA, in a project developing information to inform the retrofit of buildings with a high risk to earthquake in Western Australia’s oldest inland town.

Earthquake hazard was largely ignored in the design of Australian buildings up to the mid 1990’s. As a result, some buildings in Australian communities have a high vulnerability to earthquake. This is particularly the case for unreinforced masonry (URM) buildings, which have inherent vulnerability and have been severely damaged in historical earthquakes (Adelaide, 1954; Meckering, 1968; Newcastle, 1989; and Kalgoorlie 2009). This issue is of particular concern for the WA town of York, which has a predominance of older heritage value URM buildings and a high earthquake hazard by Australian standards.

As part of this project the entire town has been surveyed along with its businesses. Six URM building types common in the community have been identified from the building inventory. The vulnerability of these buildings with and without earthquake retrofit is being assessed utilising research from the associated Bushfire and Natural Hazards CRC project entitled Cost-effective mitigation strategy for building-related earthquake risk.

Using the latest understanding of Australian earthquake hazard developed by Geoscience Australia in the 2018 National Seismic Hazard Assessment, the cost effectiveness of various levels of strengthening investment are being assessed for a range of building uses. This information will support future incentive schemes by the Shire of York and the WA government to make communities like York more resilient to earthquake hazard.

The project is co-funded by the Bushfire and Natural Hazards CRC and Geoscience Australia.

National Seismic Hazard Assessment (NSHA)

For information on the NSHA, see https://www.ga.gov.au/about/projects/safety/nsha.