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Everest

Nepal expedition to remeasure height of Everest

hydraulic fracturing for shale gas

Damaging Sichuan earthquakes linked to fracking operations

earthquake monitoring

Crowdsourcing speeds up earthquake monitoring

San Andreas Fault

California’s current earthquake hiatus is an unlikely pause

San Andreas Fault

Signs of 1906 earthquake revealed in mapping of offshore northern San...

Deep below the Earth in the Tonga-Fiji region of the South Pacific, one enormous earthquake triggered another.

Massive earthquakes provide new insight into deep Earth

The Washington coast is geologically complex.

Hundreds of bubble streams link biology, seismology off Washington’s coast

A map of Japan showing locations for the epicenter of the 2011 Tohoku earthquake (✩),Kamioka (K), Matsushiro (M) and seismic survey instruments used (△ and ●). Credit: 2019 Kimura Masaya

A new way to sense earthquakes could help improve early warning...

Scientists used the model to calculate seismic risk in the L.A. Basin

Fast, simple new assessment of earthquake hazard

Roman monuments, including the Colosseum

Seemingly dormant geologic fault damaged famous Roman buildings 1,500 years ago

Graphic showing the Transition Zone inside the Earth Princeton seismologist Jessica Irving worked with then-graduate student Wenbo Wu and another collaborator to determine the roughness at the top and bottom of the transition zone, a layer within the mantle, using scattered earthquake waves. They found that the top of the transition zone, a layer located 410 kilometers down, is mostly smooth, but the base of the transition zone, 660 km down, in some places is much rougher than the global surface average. “In other words, stronger topography than the Rocky Mountains or the Appalachians is present at the 660-km boundary,” said Wu. NOTE: This graphic is not to scale. Credit: Kyle McKernan, Office of Communications

Massive Bolivian earthquake reveals mountains 660 kilometers below our feet

Indonesia’s devastating 2018 earthquake was a rare supershear, UCLA study finds

On the area map on the left, the colored background is the ground displacement induced by the Palu earthquake and the thin black line is the fault, both derived from satellite radar images. The black dot is the city of Palu. The circles are spots that radiated waves during the earthquake; their color indicates time (blue at the beginning, red at the end). The right figure shows the timing and position of these earthquake radiators. Their alignment indicates a steady earthquake speed of about 4.1 km/s Credit: © Han Bao et al., Nature Geoscience

Earthquake with magnitude 7.5 in Indonesia—an unusual and steady speed

Floating seismometers dubbed MERMAIDs -- Mobile Earthquake Recording in Marine Areas by Independent Divers -- reveal that Galapagos volcanoes are fed by a mantle plume reaching 1,900 km deep. By letting their nine MERMAIDs float freely for two years, an international team of researchers created an artificial network of oceanic seismometers that could fill in one of the blank areas on the global geologic map, where otherwise no seismic information is available. Drifting a mile below the surface, MERMAIDs cover a large area. The red circles show where a MERMAID picked up a seismic signal. Credit: Courtesy of the researchers

MERMAIDs reveal secrets from below the ocean floor

Where plates collide: The main frontal thrust (red line) extends over the entire length of the Himalayas. Credit: NASA Earth Observatory

Waiting for the complete rupture

Drilling deep for clues on earthquakes

New computer modeling approach could improve understanding of megathrust earthquakes

Map of the locations and depths of the deep low-frequency (DLF) earthquakes beneath the Laacher See Volcano ("Lake Laach Volcano") in Germany. Brittle earthquakes are marked as circles, DLF events as stars. Credit: Hensch et al.

Deep low-frequency earthquakes indicate migration of magmatic fluids beneath Laacher See...

A snapshot of seismic data taken at a single station during the peak of an aftershock sequence

Q&A: Creating a “Virtual Seismologist”

Transportable Array station P19K is one of the closest stations to the Iniskin earthquake origin. Solar panels power the station, and the seismometer is buried in a specially drilled borehole to insulate it from surface noise. Photo taken in 2017 during a service site visit by Incorporated Research Institutions for Seismology (IRIS). IRIS manages the Transportable Array station installation and maintenance. Credit: Doug Bloomquist, IRIS

Alaska earthquakes offer new insight into improving hazard assessment

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