Here you will find general information on the science behind tsunami generation, computer animations of tsunamis, and summaries of past field studies.
Learn More
Background information and links to our other tsunami research projects.
The scope of tsunami research within the USGS, however, is broader than the topics covered here. USGS researchers have also provided critical research toward understanding how sediments are transported during tsunami runup and deciphering the geologic record of prehistoric tsunamis. The USGS collaborates closely with the NOAA Center for Tsunami Research.
As part of the National Tsunami Hazard Mitigation Program, the USGS has also upgraded the seismograph network and communication functions of the U.S. Tsunami Warning Center.
Soon after the devastating tsunami in the Indian Ocean on December 26, 2004 many people have asked, “Could such a tsunami happen in the United States?” As a starting point, read “Could It Happen Here?”
Starting points:
- Could It Happen Here?
- Life of a Tsunami
- Local Tsunamis in the Pacific Northwest
-
- Not all tsunamis are generated by earthquakes
- Tsunamis can be caused by volcanoes, landslides, and even atmospheric disturbances
- Data from tide gauges can help unravel the complex physics of these sources
Tsunami events:
March 11, 2011, Japan
- Preliminary simulations of the tsunami
- Notes from the field: International Tsunami Team visits Japan before (2010) and after (May 2011);
plus eyewitness accounts from California on March 11
September 29, 2009, Samoa
- Preliminary analysis of the tsunami
- USGS scientists in Samoa and American Samoa studying impacts of tsunami
April 1, 2007, Solomon Islands
March 28, 2005, Sumatra
- Analysis and comparison of the December 2004 and March 2005 tsunamis
- Field study of the effects of the December 2004 and March 2005 earthquakes and tsunamis - April 2005
December 26, 2004, Sumatra-Andaman Islands
- Tsunami generation from the 2004 M=9.1 Sumatra-Andaman earthquake
- Initial findings on tsunami sand deposits, damage, and inundation in Sumatra - January 2005
- Initial findings on tsunami sand deposits, damage, and inundation in Sri Lanka - January 2005
June 23, 2001, Peru
- Preliminary analysis of the tsunami generated by the earthquake
- Preliminary analysis of sedimentary deposits from the tsunami
July 17, 1998, Papua New Guinea
Below are current tsunami studies and tsunami education materials.
PubTalk 1/2017 — Unusual sources of tsunamis
A presentation on "Unusual Sources of Tsunamis From Krakatoa to Monterey Bay" by Eric Geist, USGS Research Geophysicist
- Not all tsunamis are generated by earthquakes.
- Tsunamis can be caused by volcanoes, landslides, and even atmospheric disturbances
- Data from tide gauges can help unravel the complex physics of these sources
Below are USGS publications on a wide variety of topics related to tsunamis.
Far field tsunami simulations of the 1755 Lisbon earthquake: Implications for tsunami hazard to the U.S. East Coast and the Caribbean
The great Lisbon earthquake of November 1st, 1755 with an estimated moment magnitude of 8.5-9.0 was the most destructive earthquake in European history. The associated tsunami run-up was reported to have reached 5-15??m along the Portuguese and Moroccan coasts and the run-up was significant at the Azores and Madeira Island. Run-up reports from a trans-oceanic tsunami were documented in the Caribbe
Chapter 3 - Phenomenology of tsunamis: Statistical properties from generation to runup
Probabilistic tsunami hazard assessment at Seaside, Oregon, for near-and far-field seismic sources
Tsunami: wave of change
Triggering of tsunamigenic aftershocks from large strike‐slip earthquakes: Analysis of the November 2000 New Ireland earthquake sequence
[1] The November 2000 New Ireland earthquake sequence started with a Mw = 8.0 left‐lateral main shock on 16 November and was followed by a series of aftershocks with primarily thrust mechanisms. The earthquake sequence was associated with a locally damaging tsunami on the islands of New Ireland and nearby New Britain, Bougainville, and Buka. Results from numerical tsunami‐propagation models of the
Geophysics: The size and duration of the Sumatra-Andaman earthquake from far-field static offsets
Rapid tsunami models and earthquake source parameters: Far-field and local applications
Large-scale deformation related to the collision of the Aleutian Arc with Kamchatka
Application of continuum models to deformation of the Aleutian Island Arc
Continuum models were constructed to describe large‐scale deformation of the Aleutian Island Arc over the past 5 m.y. These models consider the island arc as a continuum in the horizontal plane with the velocity boundary condition at the Pacific edge stated as a fraction of Pacific plate convergence transferred to the arc. First, a simple model of uniformly distributed strain is formulated to illu
Below are news stories about tsunamis.
Below are FAQs associated with tsunamis.
Here you will find general information on the science behind tsunami generation, computer animations of tsunamis, and summaries of past field studies.
Learn More
Background information and links to our other tsunami research projects.
The scope of tsunami research within the USGS, however, is broader than the topics covered here. USGS researchers have also provided critical research toward understanding how sediments are transported during tsunami runup and deciphering the geologic record of prehistoric tsunamis. The USGS collaborates closely with the NOAA Center for Tsunami Research.
As part of the National Tsunami Hazard Mitigation Program, the USGS has also upgraded the seismograph network and communication functions of the U.S. Tsunami Warning Center.
Soon after the devastating tsunami in the Indian Ocean on December 26, 2004 many people have asked, “Could such a tsunami happen in the United States?” As a starting point, read “Could It Happen Here?”
Starting points:
- Could It Happen Here?
- Life of a Tsunami
- Local Tsunamis in the Pacific Northwest
-
- Not all tsunamis are generated by earthquakes
- Tsunamis can be caused by volcanoes, landslides, and even atmospheric disturbances
- Data from tide gauges can help unravel the complex physics of these sources
Tsunami events:
March 11, 2011, Japan
- Preliminary simulations of the tsunami
- Notes from the field: International Tsunami Team visits Japan before (2010) and after (May 2011);
plus eyewitness accounts from California on March 11
September 29, 2009, Samoa
- Preliminary analysis of the tsunami
- USGS scientists in Samoa and American Samoa studying impacts of tsunami
April 1, 2007, Solomon Islands
March 28, 2005, Sumatra
- Analysis and comparison of the December 2004 and March 2005 tsunamis
- Field study of the effects of the December 2004 and March 2005 earthquakes and tsunamis - April 2005
December 26, 2004, Sumatra-Andaman Islands
- Tsunami generation from the 2004 M=9.1 Sumatra-Andaman earthquake
- Initial findings on tsunami sand deposits, damage, and inundation in Sumatra - January 2005
- Initial findings on tsunami sand deposits, damage, and inundation in Sri Lanka - January 2005
June 23, 2001, Peru
- Preliminary analysis of the tsunami generated by the earthquake
- Preliminary analysis of sedimentary deposits from the tsunami
July 17, 1998, Papua New Guinea
Below are current tsunami studies and tsunami education materials.
PubTalk 1/2017 — Unusual sources of tsunamis
A presentation on "Unusual Sources of Tsunamis From Krakatoa to Monterey Bay" by Eric Geist, USGS Research Geophysicist
- Not all tsunamis are generated by earthquakes.
- Tsunamis can be caused by volcanoes, landslides, and even atmospheric disturbances
- Data from tide gauges can help unravel the complex physics of these sources
Below are USGS publications on a wide variety of topics related to tsunamis.
Far field tsunami simulations of the 1755 Lisbon earthquake: Implications for tsunami hazard to the U.S. East Coast and the Caribbean
The great Lisbon earthquake of November 1st, 1755 with an estimated moment magnitude of 8.5-9.0 was the most destructive earthquake in European history. The associated tsunami run-up was reported to have reached 5-15??m along the Portuguese and Moroccan coasts and the run-up was significant at the Azores and Madeira Island. Run-up reports from a trans-oceanic tsunami were documented in the Caribbe
Chapter 3 - Phenomenology of tsunamis: Statistical properties from generation to runup
Probabilistic tsunami hazard assessment at Seaside, Oregon, for near-and far-field seismic sources
Tsunami: wave of change
Triggering of tsunamigenic aftershocks from large strike‐slip earthquakes: Analysis of the November 2000 New Ireland earthquake sequence
[1] The November 2000 New Ireland earthquake sequence started with a Mw = 8.0 left‐lateral main shock on 16 November and was followed by a series of aftershocks with primarily thrust mechanisms. The earthquake sequence was associated with a locally damaging tsunami on the islands of New Ireland and nearby New Britain, Bougainville, and Buka. Results from numerical tsunami‐propagation models of the
Geophysics: The size and duration of the Sumatra-Andaman earthquake from far-field static offsets
Rapid tsunami models and earthquake source parameters: Far-field and local applications
Large-scale deformation related to the collision of the Aleutian Arc with Kamchatka
Application of continuum models to deformation of the Aleutian Island Arc
Continuum models were constructed to describe large‐scale deformation of the Aleutian Island Arc over the past 5 m.y. These models consider the island arc as a continuum in the horizontal plane with the velocity boundary condition at the Pacific edge stated as a fraction of Pacific plate convergence transferred to the arc. First, a simple model of uniformly distributed strain is formulated to illu
Below are news stories about tsunamis.
Below are FAQs associated with tsunamis.