![]() |
| Chris Goldfinger Photo Credit: Courtesy of Oregon State University |
Two fault systems on North America’s West Coast – the Cascadia subduction zone and the San Andreas fault – may be synchronized, with earthquakes on one fault potentially triggering seismic events on the other, a new study.
“We’re used to hearing the ‘Big One’ – Cascadia – being this catastrophic huge thing,” said Chris Goldfinger Link is external, a marine geologist at Oregon State University and lead author of the study. “It turns out it’s not the worst-case scenario.”
Goldfinger and a team of researchers drilled deep-sea sediment cores representing 3,100 years of geologic history, and analyzed layers known as turbidites that are deposited by underwater landslides often triggered by earthquakes. They compared turbidite layers in cores from both fault systems and found similarities in timing and structure, suggesting the seismic synchronization between the faults.
In most cases, it’s difficult to determine the time separation between the Cascadia subduction zone and northern San Andreas fault ruptures, but Goldfinger said there are three instances in the past 1,500 years, including a most recent one from 1700, when the researchers believe the ruptures were just minutes to hours apart.
.jpg)


.jpg)

.jpg)
_MoreDetail-v3_x2_2200x1200.jpg)

_RealPhoto-v3_x2_1932x828.jpg)
