Seismic

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Seismic waves are waves that travel through or over Earth. They are usually generated by movements of the Earth's tectonic plates (earthquakes) but may also be caused by explosions, volcanoes and landslides. They can tell us much about the Earth's structure.

Seismic facies are "mappable, three dimensional seismic units composed of groups of reflections whose parameters differ from those of ...

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Find out about the various types of waves. What types of waves are sound, electromagnetic, brain, seismic, mechanical, and surface waves.

Use a smartphone or GPS device to navigate to the provided coordinates. Visitors to EarthCaches can see how our planet has been shaped by geological processes, how we manage its resources, and how scientists gather evidence to learn about the Earth.

20 Cool Facts about the New Madrid Seismic Zone—Commemorating the bicentennial of the New Madrid earthquake sequence, December 1811–February 1812

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When an earthquake occurs, the shockwaves of released energy that shake the Earth and temporarily turn soft deposits, such as clay, into jelly (liquefaction) are called seismic waves, from the Greek ‘seismos’ meaning ‘earthquake’. Seismic waves are usually generated by movements of the Earth’s tectonic plates but may also be caused by explosions, volcanoes and landslides.