Aftershock, a smaller earthquake that occurs after a previous large earthquake, in the same area of the main shock.[1][2]
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Blind thrust earthquake, an earthquake which occurs along a thrust fault that does not show signs on the Earth's surface.[3]
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Cryoseism, a seismic event that may be caused by a sudden cracking action in frozen soil or rock saturated with water or ice.[4]
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Deep-focus earthquake, also called a plutonic earthquake, an earthquake with a depth exceeding 70 kilometres (43 mi).[5]
Doublet earthquake, an earthquake that consists of at least two or more mainshocks of nearly identical magnitude, separated by a period of time.[6]
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Earthquake swarm, events where a local area experiences sequences of many earthquakes striking in a relatively short period of time.[7]
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Foreshock, an earthquake that occurs before a larger seismic event (the mainshock) and is related to it in both time and space.[8]
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Harmonic tremor, a sustained release of seismic and infrasonic energy typically associated with the underground movement of magma, the venting of volcanic gases from magma, or both.[9]
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Induced seismicity, typically minor earthquakes and tremors that are caused by human activity that alters the stresses and strains on the Earth's crust.[10]
Megathrust earthquake, an earthquake occurring at subduction zones at destructive convergent plate boundaries, where one tectonic plate is forced underneath another.[14]
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Remotely triggered earthquakes, a result of the effects of other earthquakes at considerable distance, outside of the immediate aftershock zones.[15]
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Slow earthquake, a discontinuous, earthquake-like event that releases energy over a period of hours to months, rather than the seconds to minutes characteristic of a typical earthquake.[16]
Submarine earthquake, an earthquake that occurs underwater at the bottom of a body of water, especially an ocean.[17]
Supershear earthquake, an earthquake in which the propagation of the rupture along the fault surface occurs at speeds in excess of the seismic shear wave (S-wave) velocity, causing an effect analogous to a sonic boom.[18]
Tsunami earthquake, an earthquake that triggers a tsunami of a magnitude that is very much larger than the magnitude of the earthquake as measured by shorter-period seismic waves.[20]
^Mulroy, Clare (December 20, 2022). "What is an aftershock? Learn about the smaller earthquakes impacting Turkey and Syria". USA Today. Retrieved February 29, 2024.
^Moshou, Alexandra; Konstantaras, Antonios; Argyrakis, Panagiotis; Petrakis, Nikolaos S.; Kapetanakis, Theodoros N.; Vardiambasis, Ioannis O. (July 25, 2022). "Data Management and Processing in Seismology: An Application of Big Data Analysis for the Doublet Earthquake of 2021, 03 March, Elassona, Central Greece". Applied Sciences. 12 (15): 7446. doi:10.3390/app12157446. ISSN 2076-3417.
^"Earthquake Swarm". ScienceDirect. Retrieved March 1, 2024.
^Gates, A.; Ritchie, D. (2006). Encyclopedia of Earthquakes and Volcanoes. Infobase Publishing. p. 89. ISBN 978-0-8160-6302-4. Retrieved 29 November 2010.
^Montegrossi, Giordano; Farina, Angiolo; Fusi, Lorenzo; De Biase, Antonietta (October 8, 2019). "Mathematical model for volcanic harmonic tremors". Nature Publishing Group. 9: 14417. Bibcode:2019NatSR...914417M. doi:10.1038/s41598-019-50675-2. ISSN 2045-2322. PMC6783453. PMID 31594972.
^Kalkan, E.; Gurbuz, C.; Zor, E. (December 2014). "The Usage of Correlation Method for Micro-Earthquake Analysis at Salavatlı Geothermal Area, Aydın, Turkey". American Geophysical Union. 2014: S51A–4392. Bibcode:2014AGUFM.S51A4392K – via Astrophysics Data System.
^Bellam, Srigiri Shankar (August 2012). "Assessment of interplate and intraplate earthquakes" (PDF). Texas A&M University Libraries. Retrieved March 1, 2024.
^Iwata, Tomotaka; Asano, Kimiyuki (2011). "Characterization of the Heterogeneous Source Model of Intraslab Earthquakes Toward Strong Ground Motion Prediction". Pure and Applied Geophysics. 168 (1–2): 117–124. Bibcode:2011PApGe.168..117I. doi:10.1007/s00024-010-0128-7. S2CID 140602323.
^Senoa, Tetsuzo; Yoshida, Masaki (2004). "Where and why do large shallow intraslab earthquakes occur?". Physics of the Earth and Planetary Interiors. 141 (3): 183–206. Bibcode:2004PEPI..141..183S. doi:10.1016/j.pepi.2003.11.002.
^"Questions and Answers on Megathrust Earthquakes". Natural Resources Canada. Retrieved March 1, 2024.
^Hough, Susan E. (January 1, 2005). "Remotely Triggered Earthquakes Following Moderate Mainshocks (or, Why California Is Not Falling into the Ocean)". GeoScienceWorld. Retrieved March 1, 2024.
^Becker, Rachel (August 30, 2016). "Slow Earthquakes Are a Thing". Smithsonian Magazine. Retrieved March 1, 2024.
^Fryer, Gerard. "How do undersea earthquakes cause tsunamis?". Hawaii Institute of Geophysics and Planetology. Retrieved March 1, 2024.
^Levy D. (December 2, 2005). "A century after the 1906 earthquake, geophysicists revisit 'The Big One' and come up with a new model". Press release. Stanford University. Archived from the original on January 29, 2008. Retrieved June 12, 2008.
^Adams, Rick (August 2, 2019). "Earthquakes: What Is a Strike Slip Fault?". Spectrum News. Retrieved March 1, 2024.
^Sun, Lin (August 2020). "Relationships between tsunami size and earthquake magnitude improved by fault parameters". ScholarSpace. Retrieved February 29, 2024.