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The movement of seismic waves through the material of the mantle allows scientists to image Earth's interior, just as a medical ultrasound allows technicians to look inside a blood vessel

Mysterious deep-Earth seismic signature explained

Three water-filled maars, created by volcanic eruptions, in Germany’s Eifel region. Credit: Martin Schildgen/Wikimedia Commons

New evidence of long-term volcanic, seismic risks in northern Europe

A seismic mapping milestone

Ocean

Seismic study reveals huge amount of water dragged into Earth’s interior

seismic waves are essentially blind to a very common substance found throughout the Earth's interior: water.

Scientists find seismic imaging is blind to water

Rapid uplift of Southern Tibet

Geophysicist Helps Develop High-Res Map of Earth’s Magnetic Field

Earth

Study uses seismic noise to track water levels in underground aquifers

mosasaurs

The songs of fin whales offer new avenue for seismic studies...

Seismic study aims to map Earth’s interior in 3-D

Seismically active Katmandu region in store for larger earthquake

Drill ship Fugro Synergy

Drilling into the mysteries of seismic activity

This illustration shows how the changes in the electromagnetic properties of xenon, iron, and nickel under these intense pressures allow for the formation of XeFe3 and XeNi3.

Do you know where your xenon is?

The Mid-Atlantic Resource Imaging Experiment (MATRIX) collected reflection seismic data along more than 2000 km of trackline shown in yellow.

Seismic research cruise provides new data on US Atlantic margin gas...

Study details evidence for past large earthquakes in the Eastern Tennessee...

Model of a plant with one or several boreholes.

Optimized positioning of geothermal boreholes reduces seismicity

Marine Denolle (right) and her team, including Jiuxun Yin (left) and Brad Lipovsky, created numerical models to predict an earthquake’s final magnitude 10 to 15 seconds faster than today’s best algorithms. Credit: Stephanie Mitchell/Harvard Staff Photographer

Predicting the strength of earthquakes

Study reveals two seismic processes by which hydraulic fracturing induces tremors

Seismic recordings with bell ringing signals in four European locations to mark the passage of time: Lunas (France), Riolos (Greece), Sta. Marيa de Montmagastrell (Spain) y Oriolo (Italy). Each plot corresponds to one day. Each trace represents the same minute at every hour on that day. Time scale is in seconds. (Image: Jordi Dيaz, ICTJA-CSIC)

How seismometers record church bells ringing

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

Q&A: Creating a “Virtual Seismologist”

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