Decoding earthquake history: How geologists find fossilized clues in sediment
Twenty years ago this Sunday, the Nisqually earthquake rattled the region. It registered 6.8 on the Richter scale and shook for 40 seconds. The damage was significant. Bricks flew. It caused cracks in the Capitol dome in Olympia and sealed the fate of Seattle’s Alaskan Way Viaduct as well as many older buildings in Pioneer Square. But it was nowhere near as drastic as some of the other possible geological scenarios that could lead to truly devastating shaking.
KNKX environment reporter Bellamy Pailthorp wanted to learn more about the geological context of that quake two decades ago … and how these scientists piece together the clues that unlock answers to some of the earth’s deepest mysteries.
She joined retired USGS geologist Brian Atwater at a favorite spot on Seattle’s Duwamish River that he likes to explore at low tide. And she spoke with Seattle Times science writer Sandi Doughton about her book, "Full-Rip 9.0: The Next Big Earthquake in the Pacific Northwest," as well as the latest on preparedness in the region.