History of abrupt sinking of the Seal Beach Wetlands


A new collaborative study shows evidence of prior abrupt sinking of the wetlands within the Naval Weapons Station Seal Beach, caused by ancient earthquakes that shook the area at least three times in the past 2,000 years, according to researchers.

“Imagine a large earthquake — and it can happen again — causing the Seal Beach wetlands to sink abruptly by up to 3-feet. This would be significant, especially since the area already is at sea level,” said Dr. Matthew E. Kirby, Cal State Fullerton professor of geological sciences.

“Especially because the wetlands for the Seal Beach National Wildlife Refuge are a part of the naval weapons station, our staff will be closely evaluating the study, and will apply its findings in our future planning,” said Gregg Smith, public affairs officer for the base.

The paleoseismology study reveals that the wetlands at the National Wildlife Refuge Seal Beach, a nearly 500-acre area located within the Navy base, and next to the communities of Seal Beach and Huntington Harbor, are susceptible to rapid lowering in elevation during large — possibly more than 7.0 magnitude — earthquakes.

Former USGS geologist and CSUF alumnus Robert J. Leeper led the study with Kirby and Dr. Brady P. Rhodes, CSUF professor emeritus of geological sciences. Leeper’s master’s thesis is based on the research findings.

“These research findings have important implications in terms of seismic hazard and risk assessment in coastal Southern California and are relevant to municipal, industrial and military infrastructure in the region,” said Leeper.

The results may indicate more large events have occurred in the recent past (last 2,000 years) than has been assumed in other models, like the Uniform California Earthquake Rupture Forecast.

Located off the Pacific Coast Highway between Belmont Shore and Sunset Beach, the Seal Beach Wetlands likely formed due to complex, lateral movement of the Newport-Inglewood / Rose Canyon fault system, said Leeper.

The Wetlands straddle a segment of the fault system, which extends from Beverly Hills in the north to the San Diego region in the south. Should this Newport-Inglewood / Rose Canyon fault system all rupture in one earthquake, it could produce a magnitude 7.5 earthquake, and significantly impact communities along the entire coastline from Long Beach to San Diego.

The Seal Beach study reveals evidence for three earthquakes on the fault system over the past 2,000 years, noted Leeper, who earned his master’s degree in 2016 from Cal State Fullerton. According to Leeper, the last big quake to cause the land to abruptly drop occurred approximately 500 years ago.

According to Seal Beach Mayor Sandra Massa-Lavitt, “This is a continuing revelation of information concerning the faulty lines and potential seismic activity in the region. As technology becomes more sophisticated we will know even more. Taken together this information as well as previous knowledge reinforces what we already know. If ‘we get the big one,’ not many of us will be undamaged.”

Leeper, now a doctoral student in the earth sciences program at University of California at Riverside, is the lead author of the paper, and CSUF co-authors are Kirby; Rhodes; Dr. Joe Carlin, assistant professor of geological sciences; and 2016 geology graduate Angela Aranda, who for her master’s thesis analyzed sediment cores from the wetlands. Other collaborators and co-authors are Dr. Kate Scharer and Scott Starratt of the U.S. Geological Survey; Eileen Hemphill-Haley, consulting micropaleontologist; and Simona Avnaim-Katav and Glen MacDonald from UCLA.

The study, “Evidence for Coseismic Subsidence Events in a Southern California Coastal Saltmarsh,” is available at www.nature.com/articles/srep44615 in “Scientific Reports.”