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Earthquake that occurs at the boundary between two tectonic plates
An interplate earthquake occurs at the boundary between two tectonic plates. Earthquakes of this type account for more than 90 percent of the total seismic
Interplate_earthquake
Earthquake that occurs within the interior of a tectonic plate
intraplate earthquake is an earthquake which occurs in the interior of a tectonic plate. They are relatively rare compared to the more familiar interplate earthquakes
Intraplate_earthquake
Megathrust earthquake off Japan's east coast
Most of the foreshocks are interplate earthquakes with thrust-type focal mechanisms. Both interplate and intraplate earthquakes appeared in the aftershocks
2011 Tōhoku earthquake and tsunami
2011_Tōhoku_earthquake_and_tsunami
Type of earthquake at convergent plate boundaries
plates. These interplate earthquakes are the planet's most powerful, with moment magnitudes (Mw) that can exceed 9.0. Since 1900, all earthquakes of magnitude
Megathrust_earthquake
Canadian natural disaster
history recorded by seismometers was the 1949 Queen Charlotte earthquake, an interplate earthquake that occurred on the ocean bottom just off the rugged coast
1946 Vancouver Island earthquake
1946_Vancouver_Island_earthquake
Tectonic boundary in North America
types of earthquakes (or seismicity); including slow earthquakes, megathrust earthquakes, interplate earthquakes, and intraplate earthquakes. Unlike other
Cascadia_subduction_zone
Kanamori, H. (2012). "Intraplate and interplate faulting interactions during the August 31, 2012, Philippine Trench earthquake (Mw 7.6) sequence". Geophysical
List of earthquakes in the Philippines
List_of_earthquakes_in_the_Philippines
The Sagami Trough megathrust earthquake is a large earthquake that is considered to occur at roughly 200-year intervals in the Kantō region of Japan, caused
Megathrust earthquakes along the Sagami Trough
Megathrust_earthquakes_along_the_Sagami_Trough
Earthquake off the coast of Iwate Prefecture, Japan
& Tamura Y. (2001). "Space–time distribution of interplate moment release including slow earthquakes and the seismo-geodetic coupling in the Sanriku-oki
2026_Sanriku_earthquake
15 réplicas y derrumbes: Expertos no descartan un evento mayor" [Interplate earthquake in the north of the country generates more than 15 aftershocks and
List_of_earthquakes_in_2021
Sudden movement of the Earth's crust
There are three main types of fault, all of which may cause an interplate earthquake: normal, reverse (thrust), and strike-slip. Normal and reverse faulting
Earthquake
Earthquake in India and Pakistan
; Liu, M.; Yang, Y. (2002). "The 01/26/2001 Bhuj, India, Earthquake: Intraplate or Interplate?". In Stein, S.; Freymueller, J.T. (eds.). Plate Boundary
2001_Gujarat_earthquake
Magnitude 8.1 earthquake in the Canadian Pacific Northwest
maximum Mercalli Intensity in the event was VIII (Severe). The interplate earthquake began in the ocean bottom just off the rugged coast of Graham Island
1949 Queen Charlotte Islands earthquake
1949_Queen_Charlotte_Islands_earthquake
minor earthquakes and tremors that are caused by human activity that alters the stresses and strains on the Earth's crust. Interplate earthquake, an earthquake
Types_of_earthquake
Earthquake in Mexico
or 2000 collapsed, according to different sources. This earthquake was an interplate earthquake between the Cocos plate and the North American plate. It
1941_Colima_earthquake
Branch of geophysics, primarily seismology
Earthquake prediction is an operational objective within the broader framework of earthquake forecasting, specifically representing a forecast where uncertainty
Earthquake_prediction
This list of earthquakes in Ecuador is a list of notable earthquakes that have affected Ecuador in recorded history. The active tectonics of Ecuador is
List of earthquakes in Ecuador
List_of_earthquakes_in_Ecuador
8.3 magnitude earthquake
Kuril Trench and the Japan Trench. It was an interplate earthquake. The focal mechanism of this earthquake showed movement on a thrust fault with a considerable
1968_Tokachi_earthquake
Earthquakes in the Kamchatka Peninsula, far eastern Russia
compressional events along coupled zones, suggesting an accumulation of interplate deformation. In Petropavlovsk-Kamchatsky, 460 kilometres (290 mi) from
Kamchatka_earthquakes
Earthquake near Edo in the Kantō region, Japan
(2003). "Cycle of Interplate Earthquake Along the Sagami Trough, Deduced from Tectonic Geomorphology" (PDF). Bulletin of Earthquake Research International
1703_Genroku_earthquake
7th-century earthquake in Japan
great interplate earthquakes have occurred along the Suruga Trough and Nankai Trough, off the southwestern coasts of Japan. These earthquakes are associated
684_Hakuhō_earthquake
Earthquake in southeast Hokkaido, Japan
behaviour in historical earthquakes, named from southwest to northeast: Tokachi, Akkeshi and Nemuro. The last two large interplate earthquakes to affect this area
1843_Tokachi_earthquake
Scales to describe earthquake strength
(2001), The Radiated Seismic Energy and Apparent Stress of Interplate and Intraslab Earthquakes at Subduction Zone Environments: Implications for Seismic
Seismic_magnitude_scales
Earthquake off Japan
characteristic earthquake. The rupture zone of the 1978 earthquake occurred at the westernmost limit of known interplate earthquakes, some 150 km back
1978_Miyagi_earthquake
Earthquake in Ecuador
intraplate seismicity. Earthquakes are common in Ecuador. Near the Nazca subduction zone the recorded history of interplate earthquakes spans 80 years. At
1949_Ambato_earthquake
Earthquake off the coast of Aomori Prefecture, Japan
& Tamura Y. (2001). "Space–time distribution of interplate moment release including slow earthquakes and the seismo-geodetic coupling in the Sanriku-oki
2025_Aomori_earthquake
Earthquake in Japan
velocity in the north is 7% slower than that in the south. This was an interplate earthquake, with a low-angle reverse fault focal mechanism, which ruptured
1994 offshore Sanriku earthquake
1994_offshore_Sanriku_earthquake
Earthquake in Hyūga-nada
The intensity reached shindo 5 in Miyazaki and Kōchi. This was an interplate earthquake between the Eurasian plate and the Philippine Sea plate. In this
1968_Hyūga-nada_earthquake
Earthquake in Mexico
Trench. It was an interplate earthquake. It had a reverse faulting focal mechanism. List of earthquakes in 1995 List of earthquakes in Mexico "INICIO"
1995_Guerrero_earthquake
Origin point beneath an air explosion
seismology, the hypocenter of an earthquake is its point of origin below ground; a synonym is the focus of an earthquake. Generally, the terms ground zero
Hypocenter
Magnitude 7.6 earthquake in the Philippines
Hiroo (2012). "Intraplate and interplate faulting interactions during the August 31, 2012, Philippine Trench earthquake (Mw 7.6) sequence". Geophysical
December 2023 Mindanao earthquake
December_2023_Mindanao_earthquake
Earthquake in Japan
"Source parameters of microearthquakes on an interplate asperity off Kamaishi, NE Japan over two earthquake cycles". Geophysical Journal International.
2012_Sanriku_earthquake
Following the 2023 Turkey–Syria earthquakes, numerous issues were presented to people involved. Multiple agencies submitted figures on life and monetary
Aftermath of the 2023 Turkey–Syria earthquakes
Aftermath_of_the_2023_Turkey–Syria_earthquakes
Earthquake in Mexico
coseismic stress change during the 30 January, 1973, Colima, Mexico interplate earthquake (Mw=7.6)". Geophysics International (In Spanish). 45 (3): 163–178
1973_Colima_earthquake
collapsed. A tsunami was recorded. This was one of the recurring interplate earthquakes at the offshore Miyagi with a recurrence interval of about 37 years
1936_Miyagi_earthquake
Earthquake in south-central Chile
1939 Chillán earthquake was normal faulting. It was not clear whether the 1953 Concepción earthquake was an interplate or intraplate earthquake. List of earthquakes
1953_Concepción_earthquake
Earthquake in Chile
University of Chile Seismological Service a thrust fault-type interplate earthquake. The earthquake, measured in the Modified Mercalli intensity, reached magnitude
1985_Rapel_Lake_earthquake
Earthquake in Taiwan
earthquake showed a weakly coupled interplate boundary in the nearby region. A landslide occurred in the Su-ao-Hualien highway. List of earthquakes in
1963_Su-ao_earthquake
1995 devastating earthquake in Sakhalin, Russia
A. (December 2000). "The Neftegorsk (Sakhalin Island) 1995 earthquake: a rare interplate event". Geophysical Journal International. 143 (3): 595–607
1995_Neftegorsk_earthquake
Earthquake in Iran
2 m indicates a low static stress drop, more consistent with an interplate earthquake than an intraplate event. The maximum horizontal acceleration during
1997_Qayen_earthquake
Study of earthquake-resistant structures
buildings and bridges, with earthquakes in mind. Its overall goal is to make such structures more resistant to earthquakes. An earthquake (or seismic) engineer
Earthquake_engineering
Type of earthquake which triggers a tsunami of far-larger magnitude
A tsunami earthquake is an earthquake which triggers a tsunami of significantly greater magnitude, as measured by shorter-period seismic waves. The term
Tsunami_earthquake
Earthquake in Mexico
seismic activities before the main shock. This earthquake was a shallow thrust earthquake in the interplate subduction zone, in which the Cocos plate is
1965_Oaxaca_earthquake
Strong earthquake in Victoria, Australia
of the world's earthquakes occur. Such earthquakes at the plate boundary are known as interplate earthquakes. In Australia, earthquakes occurring within
2021_Mansfield_earthquake
The rotation causes an almost westward motion under the Suruga Bay. The interplate coupling under the Sugura Bay is not weak. The Tanna Fault is part of
1930_North_Izu_earthquake
major earthquakes recorded since at least 1911, the segment was recognised as a major seismic gap. This earthquake was an interplate earthquake that occurred
1981_Playa_Azul_earthquake
Severe earthquake centered in Valparaíso Region, Chile
stick-slip action resulting in two types of earthquakes along the trench. There are the typical interplate events that occur at the subduction interface
1985_Algarrobo_earthquake
Discontinuous earthquake-like event
A slow earthquake, also known as a silent earthquake, is a discontinuous, earthquake-like event that releases energy over a period of hours to months
Slow_earthquake
Earthquake in which the rupture propagation speeds are greater than the shear wave speed
In seismology, a supershear earthquake is when the propagation of the rupture along the fault surface occurs at speeds in excess of the seismic shear wave
Supershear_earthquake
persisted. Other strong earthquakes have affected the same area, with some that were clearly associated with the (interplate) Mendocino fracture zone
1992 Cape Mendocino earthquakes
1992_Cape_Mendocino_earthquakes
Megathrust earthquake and tsunami in Solomon Islands
being an interplate earthquake and “...produced a tsunami of ~ 1.5 height" on the Santa Cruz Islands. In the days leading up to the major earthquake, the
2013 Solomon Islands earthquake
2013_Solomon_Islands_earthquake
Series of localized seismic events within a short time period
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
Earthquake_swarm
Earthquake in Japan
(23–26 August 2011). Broadband ground motion simulation for great interplate earthquakes with multi-scale heterogeneous source modeling (PDF). 4th International
2012_Chiba_earthquake
Earthquake that occurs under a body of water, especially an ocean
A submarine, undersea, or underwater earthquake is an earthquake that occurs underwater at the bottom of a body of water, especially an ocean. They are
Submarine_earthquake
Earthquake and mining disaster in Chile
and based on the focal mechanism analyzed, was interpreted as an interplate earthquake on the plate boundary. Whether the 22 March quake was a true foreshock
1965_La_Ligua_earthquake
Earthquake with a hypocenter depth exceeding 300 km
A deep-focus earthquake in seismology (also called a plutonic earthquake) is an earthquake with a hypocenter depth exceeding 300 km. They occur almost
Deep-focus_earthquake
Magnitude 6.9 earthquake near the India-Nepal border
Nepalese border. Although earthquakes in this region are usually interplate in nature, preliminary data suggests the Sikkim earthquake was triggered by shallow
2011_Sikkim_earthquake
Geographical phenomenon
Remotely triggered earthquakes are a result of the effects of large earthquakes at considerable distance, outside of the immediate aftershock zone. The
Remotely triggered earthquakes
Remotely_triggered_earthquakes
Intensity of ground shaking during an earthquake
resulting from an earthquake. They are distinguished from seismic magnitude scales, which measure the magnitude or overall strength of an earthquake, which may
Seismic_intensity_scales
Jean-Marie (2021), "A Significant Increase in Interplate Seismicity near Major Historical Earthquakes Offshore Martinique (FWI)", Bulletin of the Seismological
List of earthquakes in the Caribbean
List_of_earthquakes_in_the_Caribbean
Earthquake in Chile
incurred in an intraplate earthquake with vertical fault and how it can be much greater than what which can cause one of interplate of similar magnitude,
1997_Punitaqui_earthquake
Earthquake in Ecuador
example, may help to lock the plate interface in that area. Modelling of interplate deformation along the coast shows higher amounts of deformation – which
1942_Ecuador_earthquake
Earthquakes in the Philippines
Kanamori H. (2012). "Intraplate and interplate faulting interactions during the August 31, 2012, Philippine Trench earthquake (M w 7.6) sequence". Geophysical
1897_Mindanao_earthquakes
Destructive tsunami earthquake south of Java Island
Okal, E. A. (2012), "The south of Java earthquake of 1921 September 11: a negative search for a large interplate thrust event at the Java Trench" (PDF)
2006 Pangandaran earthquake and tsunami
2006_Pangandaran_earthquake_and_tsunami
Minor earthquakes and tremors caused by human activity
Induced seismicity is typically earthquakes and tremors that are caused by human activity that alters the stresses and strains on Earth's crust. Most
Induced_seismicity
Earthquake caused by magma movement
A volcano tectonic earthquake or volcano earthquake is caused by the movement of magma beneath the surface of the Earth. The movement results in pressure
Volcano_tectonic_earthquake
Earthquake in New Caledonia
included both interplate thrust faulting earthquakes (the largest event in the sequence was the M 7.3 earthquake) and normal faulting earthquakes to the west
2021 Loyalty Islands earthquake
2021_Loyalty_Islands_earthquake
Earthquake probability in a specific area and time
A seismic hazard is the probability that an earthquake will occur in a given geographic area, within a given window of time, and with ground motion intensity
Seismic_hazard
Smaller earthquake which follows a larger one in the same area
In seismology, an aftershock is a smaller earthquake that follows a larger earthquake, in the same area of the main shock, caused as the displaced crust
Aftershock
Hierarchical outline list of articles related to plate tectonics
surface Intraplate earthquake – Earthquake that occurs within the interior of a tectonic plate Interplate earthquake – Earthquake that occurs at the boundary
Outline_of_plate_tectonics
Point on the Earth's surface that is directly above the hypocenter in an earthquake
where an earthquake or an underground explosion originates. The primary purpose of a seismometer is to locate the initiating points of earthquake epicenters
Epicenter
Multiple earthquakes with nearly identical waveforms originating from the same location
seismology, doublet earthquakes—and more generally, multiple earthquakes or twin earthquakes—were originally identified as multiple earthquakes with nearly identical
Doublet_earthquake
Branch of seismology
Earthquake forecasting is a branch of the science of geophysics, primarily seismology, concerned with the probabilistic assessment of earthquake occurrence
Earthquake_forecasting
Japanese earthquake measurements
Japan to categorize the intensity of local ground shaking caused by earthquakes. The JMA intensity scale differs from magnitude measurements like the
Japan Meteorological Agency seismic intensity scale
Japan_Meteorological_Agency_seismic_intensity_scale
Oceanic trench part of the Pacific Ring of Fire off northeast Japan
ISSN 0040-1951. Heki, Kosuke (1997). "Silent fault slip following an interplate thrust earthquake at the Japan Trench". Nature. 386 (6625): 595–598. Bibcode:1997Natur
Japan_Trench
Largest earthquake in a sequence
earthquake in a sequence, sometimes preceded by one or more foreshocks, and almost always followed by many aftershocks. A foreshock is an earthquake that
Mainshock
Field of study that investigates the behavior of geologic faults
the concept of a "following force", as conveniently provided for interplate earthquakes, by the motion of tectonic plates. Under a following force, the
Fault_mechanics
smaller the epicentral distance of an earthquake of the same scale, the heavier the damage caused by the earthquake. On the contrary, with the increase
Epicentral_distance
Movement along a thrust fault that is not visible at the surface
A blind thrust earthquake occurs along a thrust fault that does not show signs on the Earth's surface, hence the designation "blind". Such faults, being
Blind_thrust_earthquake
Earthquake that occurs before a mainshock but is of lower magnitude
earthquake that occurs before a larger seismic event – the mainshock – and is related to it in both time and space. The designation of an earthquake as
Foreshock
Type of seismic wave
faster than other seismic waves and hence are the first signal from an earthquake to arrive at any affected location or at a seismograph. P waves may be
P_wave
Oceanic trench in the southern Pacific Ocean
strong earthquakes during sequences which have included both interplate thrust faulting earthquakes and outer rise normal faulting earthquakes west and
New_Hebrides_Trench
seismology means time for the seismic waves to travel from the focus of an earthquake through the crust to a certain seismograph station. Travel-time curve
Travel-time_curve
Submarine trench to the east of the Philippines in the Pacific Ocean
Hiroo (2012). "Intraplate and interplate faulting interactions during the August 31, 2012, Philippine Trench earthquake (Mw 7.6) sequence". Geophysical
Philippine_Trench
Measure of earthquake size
generally implied with use of a single M for magnitude) is a measure of an earthquake's magnitude ("size" or strength) based on its seismic moment. Mw was defined
Moment_magnitude_scale
Scientific study of earthquakes and propagation of elastic waves through a planet
σεισμός (seismós), meaning 'earthquake', and -λογία (-logía), meaning 'study of') is the scientific study of earthquakes (or generally, quakes) and the
Seismology
Series of water waves
displacement of a large volume of water, generally in an ocean or a large lake. Earthquakes, volcanic eruptions, underwater explosions, landslides, glacier calvings
Tsunami
Instrument that records seismic waves by measuring ground motions
digitally—is a seismogram. Such data is used to locate and characterize earthquakes, and to study the internal structure of Earth. A simple seismometer,
Seismometer
Earthquake in Chile
converge at a rate of seventy millimeters a year. This quake was an oceanic interplate type, occurred in the downgoing slab of the Nazca Plate and not on the
2019_Coquimbo_earthquake
Japanese academic
Masaaki (1978). "Significant Eruptive Activities Related to Large Interplate Earthquakes in the Northwestern Pacific Margin". Journal of Physics of the Earth
Masaaki_Kimura
Seismic intensity scale used to quantify the degree of shaking during earthquakes
the effects of an earthquake at a given location. This is in contrast with the seismic magnitude usually reported for an earthquake. Magnitude scales
Modified Mercalli intensity scale
Modified_Mercalli_intensity_scale
Measure of the strength of earthquakes
scale, and the Gutenberg–Richter scale, is a measure of the strength of earthquakes, developed by Charles Richter in collaboration with Beno Gutenberg, and
Richter_scale
Submarine ridge off the coast of Peru
subducting Nazca Ridge, and include both intraplate and interplate rupturing. No large earthquakes have been located between 14°S and 15.5°S, where the bathymetric
Nazca_Ridge
Sound generated by earthquakes
phenomenon in which the ground vibrates and makes sounds due to an earthquake. During earthquakes or volcanic eruptions, the ground vibrates, sometimes creating
Subterranean_rumbling
Committee in Japan
The Coordinating Committee for Earthquake Prediction (CCEP) (Japanese: 地震予知連絡会, Jishin Yochi Renraku-kai) in Japan was founded in April 1969, as part of
Coordinating Committee for Earthquake Prediction
Coordinating_Committee_for_Earthquake_Prediction
Vibrational energy transfer in Earth or other planetary body
travels through the Earth or another planetary body. It can result from an earthquake (or generally, a quake), volcanic eruption, magma movement, a large landslide
Seismic_wave
Sediment/structure shaken seismically
paleontologist Adolf Seilacher first used the term in 1969 to describe earthquake-deformed layers. Today, the term is applied to both sedimentary layers
Seismite
Area not reached by seismic waves from an earthquake
where seismographs cannot detect direct P waves and/or S waves from an earthquake. This is due to liquid layers or structures within the Earth's surface
Shadow_zone
Situation or object that can cause harm
disasters with highly harmful impacts on a society are floods, droughts, earthquakes, tropical cyclones, lightning strikes, volcanic activity and wildfires
Hazard
The concept of Earthquake Duration Magnitude – originally proposed by E. Bisztricsany in 1958 using surface waves only – is based on the realization that
Earthquake_duration_magnitude
INTERPLATE EARTHQUAKE
INTERPLATE EARTHQUAKE
INTERPLATE EARTHQUAKE
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INTERPLATE EARTHQUAKE