Stanford Earth scientist Scott Fendorf helped discover how trace amounts of arsenic were moving from sediments into groundwater aquifers in Southern California.
We can't journey to the center of the Earth, but that hasn't stopped us finding out what is down there. Associate Prof. Wendy Mao provides her perspective on studying Earth's interior.
Stanford School of Earth, Energy & Environmental Sciences
Research by Tiziana Vanorio finds that fiber-reinforced rocks beneath Italy’s dormant Campi Flegrei supervolcano are similar to a wonder-material used by the ancients to construct enduring structures such as the Pantheon, and may lead to improved building materials.
Stanford School of Earth, Energy & Environmental Sciences
A new Stanford study finds that, contrary to expectations, weathering rates over the past 2 million years have remained constant through glacial cycles.
Stanford School of Earth, Energy & Environmental Sciences
Stanford Earth researchers have devised a technique that transforms the tiny tremors generated by the everyday hustle and bustle of city life into a tool for probing the subsurface of Earth.
New research by Greg Asner illustrates a hidden tapestry of chemical variation across the lowland Peruvian Amazon, with plants in different areas producing an array of chemicals that changes across the region’s topography.
Stanford School of Earth, Energy & Environmental Sciences
New research by Jonathan Payne's lab refutes a hypothesis by the famed evolutionary biologist Stephen J. Gould that marine creatures underwent an “early burst” of functional diversity during the dawn of animal life.
Stanford School of Earth, Energy & Environmental Sciences
New Stanford research shows that animals tend to evolve toward larger body sizes over time. Over the past 542 million years, the mean size of marine animals has increased 150-fold.
A new way of determining the hydrogen content in mantle rocks could lead to improved estimates of Earth’s interior water and a better understanding of our planet’s early evolution.