Stay up to date with notifications from The Independent

Notifications can be managed in browser preferences.

California earthquakes 2014: 100 aftershocks rattle US state – and bring Disneyland to a standstill

Californians urged not to panic after series of tremors

Victoria Cavaliere
Monday 31 March 2014 10:44 BST
Comments
A shake map released by the US Geological Survey (USGS) shows the location and intensity of a 5.1 Richter scale earthquake in California
A shake map released by the US Geological Survey (USGS) shows the location and intensity of a 5.1 Richter scale earthquake in California (EPA)

Your support helps us to tell the story

From reproductive rights to climate change to Big Tech, The Independent is on the ground when the story is developing. Whether it's investigating the financials of Elon Musk's pro-Trump PAC or producing our latest documentary, 'The A Word', which shines a light on the American women fighting for reproductive rights, we know how important it is to parse out the facts from the messaging.

At such a critical moment in US history, we need reporters on the ground. Your donation allows us to keep sending journalists to speak to both sides of the story.

The Independent is trusted by Americans across the entire political spectrum. And unlike many other quality news outlets, we choose not to lock Americans out of our reporting and analysis with paywalls. We believe quality journalism should be available to everyone, paid for by those who can afford it.

Your support makes all the difference.

An earthquake in Calfornia shook residents and brought rides in Disneyland to a standstill as more than 100 aftershocks rattled the US state over the weekend.

Residents of southern California were rattled by a 4.1 magnitude earthquake yesterday afternoon, the largest of scores of tremors following Friday's 5.1 rumbler that caused light scattered damage around the Los Angeles area.

Saturday's quake rippled through an area near Rowland Heights, California, according to the U.S. Geological Survey. The temblor was considered relatively shallow with a depth of 5.6 miles, the USGS said.

Aftershocks are expected following earthquakes, according to the USGS. Seismologists said there was about a 5 percent chance that Friday's quake, which struck at 9:09pm local time was a foreshock to a bigger quake.

No injuries were immediately reported from either Saturday's quake or the more significant earthquake that struck Friday evening outside La Habra, California, which is about 20 miles (32 km) east of downtown Los Angeles.

Friday's temblor displaced at least 50 people in Fullerton, about 5 miles (8 km) from the epicenter, because of minor damage to homes and apartment dwellings, Fullerton Police Lieutenant Mike Chlebowski said.

As well, a water main break in the city forced the closure of some streets due to flooding, he said. The quake also shook items off tables, rattled chandeliers and resulted in scattered damage to cars and property, including setting off a rockslide in the Orange County city of Brea that flipped a car on its roof.

While not large, the event “seems unusual, of course, because a lot of people felt it,” said Doug Given, a USGS geophysicist.

“These quakes occur in populated areas and people try to put two and two together and predict that something more is coming, but that's simply not the case,” he said.

The quake shut down Metrolink trains to allow for inspection of tracks and cars. In Anaheim, Disneyland briefly turned off park rides as a precaution and asked guests to remain seated.

But the Los Angeles Philharmonic didn't miss a note even as the quake rattled downtown Los Angeles's Walt Disney Concert Hall, The Los Angeles Times reported.

“The L.A. Philharmonic should get combat pay,” audience member Michael Healy told the newspaper.

Reuters

Join our commenting forum

Join thought-provoking conversations, follow other Independent readers and see their replies

Comments

Thank you for registering

Please refresh the page or navigate to another page on the site to be automatically logged inPlease refresh your browser to be logged in