
Barr Leadership Chair Boosts Caltech Center for Comparative Planetary Evolution
Gift from alumnus and family offers flexible funding for multidisciplinary studies of planets familiar and far away.
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Gift from alumnus and family offers flexible funding for multidisciplinary studies of planets familiar and far away.
Caltech alumnus and telecommunications pioneer Ronald Willens and his wife, JoAnne, support early-career faculty working across traditional boundaries.
When Richard Alvarez (BS ’57) worked at the Stanford Linear Accelerator Center, he helped a team fire an electron beam down 10,000 feet of three-quarter-inch tube to probe elementary particle physics. He was one of the people in the lab, he recalls, who understood the whole machine.
If a hydra breaks in two, each half of the ageless sea creature grows into a fully formed organism. Planarian worms, axolotls, sea stars, and certain geckos regrow lost body parts as well, but this select club excludes humans and other mammals. People can regenerate small pieces of tissue, but lost limbs are gone forever.
Behind almost every discovery, there is a team. Breakthroughs grow out of scientific collaborations among extraordinary investigators. And another type of partnership can drive new knowledge: backing from generous supporters. Such is the case for Sarkis Mazmanian, the Luis B. and Nelly Soux Professor of Microbiology and a Heritage Medical Research Institute Investigator at Caltech.
A gift to Break Through: The Caltech Campaign from trustee Richard Merkin establishes the Richard N. Merkin Institute for Translational Research.
In the case of Caltech’s Theodore Y. Wu Professorship, established with a generous gift from Li-San and Anne Hwang, the answer is 55 years of friendship.
When Caltech’s Nadia Lapusta creates computer models of earthquakes, she must integrate an astonishing range of data—on scales from thousands of kilometers down to microns and from millennia down to thousandths of a second. That’s because to understand the big and slow, she needs to understand the tiny and fast. “Large-scale earthquake ruptures—even those around 8 on the Richter scale—are ultimately happening in very narrow layers of granulated rock,” she says. In fact, where one side of a fault moves against the other, those layers are powdered so thin that a stack of a thousand grains would equal the thickness of a credit card. And although a fault can go eons between destructive quakes, the first slip that kicks off the shaking can take place in a blink.