Stanford University
Grand Prismatic Spring, Yellowstone National Park

Geophysics

Understanding Earth. Benefitting Society.

Photo by Hailun Ni

There's only one Earth: We should know how it works

Geophysicists study Earth and planetary processes through laboratory experiments, computational and theoretical modeling, remote imaging, and direct observation. At Stanford, our teaching and research focus on understanding systems critical to the future of civilization. Students apply expertise to fundamental research sustaining life on Earth, combining underlying science with studies of Earth’s environment and resource needs. Such breadth of exposure is highly sought after and leads to careers in academia, industry, and government.

 

Today's Earth science is data driven

The satellite and supercomputer are the tools of modern geoscientists whose work spans from climate change projections to earthquake simulations and energy resources optimization. Stanford Earth scientists are as likely to be in front of an electronic screen, analyzing torrents of remote-sensing data as they are to be drilling ice cores in Antarctica.

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Geophysics-related news

Read the latest school highlights and research news in geophysics

School focused on climate and sustainability moves forward

A school focused on climate and sustainability, announced last May, is beginning to take shape. Leaders anticipate blueprints for the school’s academic structure by winter quarter.

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Letter to the community: Voting is a civic duty

Dean Stephan Graham co-authored an op-ed with the deans of the School of Humanities and Sciences and the School of Engineering urging readers to "vote for the party and candidate of your choice, but by all means vote."

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New Stanford seed grants create pathways to sustainability

The sustainability initiative that arose out of the Long-Range Vision has awarded 17 seed grants providing one year of funding to faculty pursuing groundbreaking ideas for sustainability solutions.

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How earthquake swarms arise

A new fault simulator maps out how interactions between pressure, friction and fluids rising through a fault zone can lead to slow-motion quakes and seismic swarms.

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