Much of the greater LA area is built on a giant pit of sand and debris that extends 30,000 feet down at its deepest point before hitting solid bedrock. That deep spot is just south of downtown and, until now, geologists and engineers believed that the deeper the underlying basin, the bigger the sway of a tall building during an earthquake. But the new study found that even buildings erected on relatively shallow areas are vulnerable to the energy generated by a big quake.
“We thought the amplifications would be south of downtown LA, but we didn’t see that,” Kohler says. “We saw them elsewhere, where the basin is not deep, in West LA and the San Fernando Valley.”West LA includes the Century City commercial and entertainment district and the Wilshire Corridor, home to dozens of high-rise condos and office buildings. The San Fernando Valley sits on a separate geological basin. “That’s of concern,” Kohler says about the new findings. “Because the [state of California] building code hasn’t taken into account whether you are built over a basin or not.”On the evening of July 5, 2019, a 7.1 magnitude earthquake struck near the town of Ridgecrest, about 124 miles north of Los Angeles. It was the main shock of a series of several related quakes that began on July 4 and continued for several days. The earthquake was so strong that it created massive cracks in the arid landscape, some as big as 15 feet wide, according to a study on the quake’s effects by the US Geological Survey and other experts. While the big Ridgecrest quake didn’t cause major damage in Los Angeles, people in buildings taller than 15 stories felt frightening swaying lasting up to two minutes, the study reported. Some felt nauseous, according to a report in The Los Angeles Times.
What Kohler and her colleagues wanted to know was where the swaying was the longest, and why. They looked at observations recorded by 560 ground‐level devices called accelerometers that measure how much an object moves back and forth. The sensors were part of a citizen science project called the Community Seismic Network and were placed in computer closets at Los Angeles County schools across the region. The accelerometers measured the vibrations from the earthquake 250 times per second, enough data to see how the quake’s force changed over time.Each building has something called a “resonant period,” which is the amount of time it takes to move back and forth along the horizontal plane during a quake. Buildings taller than 15 floors, suspension bridges, and big petroleum tanks often have a resonant period of more than three seconds. The study found that buildings with a long resonant period experienced more shaking from the Ridgecrest quake than those with shorter periods, and the amount of shaking wasn’t connected to how deep the basin is underneath.
When I asked Caltech geologist Brian Wernicke, a giant in the field of global geophysics, if it was possible that Faulds was paying too much attention to the Walker Lane, he replied, quickly and without irony: “Well, it's the most interesting place in the world.” In terms of understanding how continents deform and how seismic hazards relate to plate tectonics, he added, “it's an unparalleled natural laboratory.”.