U.S. Geological Survey Earthquake Hazards Program
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Our scientists study locations around the world. Learn about research conducted in our regional offices, regional seismic network monitoring, and local activities of interest.
Today’s Earthquake Fact
Among the most dramatic and visible creations of plate-tectonic forces are the lofty Himalayas, which stretch 2,900 km along the border between India and Tibet. This immense mountain range began to form between 40 and 50 million years ago, when two large landmasses, India and Eurasia, driven by plate movement, collided. Because both these continental landmasses have about the same rock density, one plate could not be subducted under the other. The pressure of the impinging plates could only be relieved by thrusting skyward, contorting the collision zone, and forming the jagged Himalayan peaks.
News & Highlights
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Significant Earthquakes
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Recent Earthquakes (M 2.5+)
- M 3.3, Southern California March 11, 2010 21:09:25 UTC
- M 5.8, Libertador General Bernardo O'higgins, Chile March 11, 2010 20:11:20 UTC
- M 5.5, Libertador General Bernardo O'higgins, Chile March 11, 2010 19:28:07 UTC
- M 3.4, Southern Alaska March 11, 2010 17:51:30 UTC
- M 5.1, Libertador General Bernardo O'higgins, Chile March 11, 2010 17:18:50 UTC
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Earthquake News
- USGS Scientists, Research Help Haiti Reconstruction March 5, 2010 18:22:34 UTC
- 2/23/10 - USGS Updates Assessment of Earthquake Hazard and Safety in Haiti and the Caribbean February 23, 2010 19:47:15 UTC
- Yellowstone Swarm Updates from Univ of Utah and YVO January 22, 2010 18:45:33 UTC
- USGS Issues Assessment of Aftershock Hazards in Haiti January 22, 2010 01:14:41 UTC
- Earthquakes Cause over 1700 Deaths in 2009 January 14, 2010 19:57:09 UTC
Featured Items
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Educational Slides for M8.8 Chile - M7.0 Haiti Earthquakes (24MB PDF)
Educational slides for the M8.8 Chile and M7.0 Haiti Earthquakes
Slides with Notes (7MB PDF) - USGS Updates Assessment of Earthquake Hazard and Safety in Haiti and the Caribbean
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Slab Models for Subduction Zones
Three-dimensional compilation of global subduction geometries separated into regional models for each major subduction zone.




