When Roland Bürgmann started his PhD at Stanford in the Fall of 1989, he expected to build on his structural geology studies in Boulder, CO and Tübingen, Germany. He was thinking about how to map extinct faults and model how they formed, particularly up in the Sierras. “Then, two months after I arrived, the Loma Prieta earthquake destroyed our building” and gave him a different project. (By the time the Stanford Geology Corner reopened five years later, Bürgmann was already an assistant prof at UC Davis.) Geophysicist Paul Segall was an early adopter of GPS receivers, and he and a group of students “ran up to the Santa Cruz mountains and took measurements.” Tracking “post-earthquake transient deformations” and the mechanics of fault systems was a new capability, and it became the topic of a chapter of Bürgmann’s PhD thesis. He thinks this new research direction “ultimately led to me getting hired” by Earth & Planetary Sciences here at UC Berkeley. A combination of new technology, an earthquake, and Bürgmann happened at just the right time.
This compact origin story contains most of the features that Professor Bürgmann wants to get across. “Sometimes I’m a geophysicist, or a geologist, or maybe a geodesist,” depending on the problem at hand, “but I don’t want to be defined by the tools I use.” He picks up whatever he needs. Still, “without GPS and remote sensing satellite radar systems, I wouldn’t be where I am, right? I came at just the right time to partake in the revolution of being able to see the earth move with millimeter accuracy.”
