Related topics: earthquake

Faults in oceanic crust contribute to slow seismic waves

The natural structure of the rigid oceanic crust that forms a shell around Earth contains cracks and faults. These fissures are hydrothermal pathways for heat, water, and chemical solutions to move between the ocean and the ...

Unearthing the cause of slow seismic waves in subduction zones

In modern subduction zones—regions around the world that have one tectonic plate sliding past another—one area can act like molasses for seismic waves. These anomalous areas are called low-velocity zones, or LVZs. In ...

Slow slips offer insights into earthquakes

Significant earthquakes, from gentle shaking to devastating tremors, are hazards caused by a sudden release of stress that has built up in geological faults. More subtle events called slow slips are attracting increasing ...

To track elephants, scientists keep an ear to the ground

The "mini earthquakes" that elephants make by both walking and vocalizing are not only a way to communicate with each other but can be used to track their movements, according to a study published Wednesday.

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