CANADA, AUGUST 23, 2011 (COMPUTERWORLD) By Sharon Gaudin - People turn to social networks as earthquake jolts D.C area, New York, New England .

Just moments after a 5.8 magnitude earthquake hit the East Coast on Tuesday afternoon, Twitter and Facebook lit up with the news.

The quake struck central Virginia at 1:51 p.m. Eastern time today and rocked the Washington area, according to the U.S. Geological Survey. The quake was felt as far away as New Jersey, New York and New England. It also disrupted cell phone service and closed two nuclear reactors, and many bridges and tunnels in East Coast cities

Various news services reported that parts of the Pentagon, the White House and the U.S. Capitol were evacuated as a precaution. The federal building in Newark, N.J., was also evacuated.

But before news could be reported on television or even on online news sites, the reports were lighting up social networking sites like Twitter and Facebook.

People were quick to turn to their favorite social networking sites to report the quake, with many tweeting or posting while the shaking was still going on.

A reporter in Maine read about the quake on Twitter before actually feeling the shock waves reach that far north.

"When I felt the house shake I ran outside to yell at whoever was tramping across my roof. Typical Brooklyn reaction. #earthquake," tweeted Computerworld feature editor Barbara Krasnoff.

And someone identified as zephoria tweeted, "Gotta love Twitter. The building shakes. Everyone immediately gets on Twitter to confirm that they're not hallucinating." While brianstelter, wrote, "Quake was so strong at my family home, 40 min north of D.C., that my mom rushed outside, thinking something had hit the house."

And CBS News reporter Norah O'Donnell tweeted, "#SecretService rushing people out of WH and into Lafayette Square. Most people calm. #quake"

People have been quick to take to social networking sites after other earthquakes, and after the tsunami in Japan and even during anti-government uprisings.

However, today's flash tweeting and Facebook postings are a reminder of what an intrinsic part of our lives the sites have become, said Zeus Kerravala, an analyst at Yankee Group.

"It again supports the theory that social networks are the fastest way to distribute information. They have become the 'send to' of life," said Kerravala. "It's become the de facto communication tool for anyone looking to reach all of their contacts because it's simple, fast and now ubiquitous. I don't need to put in an address in a "to" field. I just type it and hit enter."

Sharon Gaudin covers the Internet and Web 2.0, emerging technologies, and desktop and laptop chips for Computerworld. Follow Sharon on Twitter at @sgaudin, or subscribe to Sharon's RSS feed . Her email address is

Small quake has big reach By John Roach MSNBC.COM NEWS

Air, train traffic disrupted over wide area; some feared another 9/11

[PHOTO - Pablo Martinez Monsivais / AP One of the National Cathedral spires damaged in the quake is seen at left.]

People stand in a square outside the courthouse after an earthquake was felt in New York Tuesday, causing buildings to be evacuated. The Pentagon, the U.S. Capitol and Union Station in the nation's capital were all evacuated after the 5.9-magnitude quake, which was shallow with its epicenter only 0.6 miles (one kilometer) underground.

A magnitude-5.8 earthquake in Virginia Tuesday afternoon was felt across the U.S. East Coast, shaking offices and nerves from Washington D.C. to New York City and as far south as Chapel Hill, North Carolina. There are even reports of shaking as far west as Columbus, Ohio, and out on Martha's Vineyard.

That's a whole lot of shaking for what amounts to a medium-sized quake. The reason for its reach, according to the U.S. Geological Survey, is geology of the East Coast.

"The reason an earthquake in the high 5s is felt so far away is that it occurred in an area where the bedrock is solid, it's not really fractured or broken up by faults the way it would be, say, in California," Peter Powers, a geophysicist with the survey, told me today.

[PHOTO - People stand in a square outside the courthouse after an earthquake was felt in New York Tuesday, causing buildings to be evacuated. The Pentagon, the U.S. Capitol and Union Station in the nation's capital were all evacuated after the 5.9-magnitude quake, which was shallow with its epicenter only 0.6 miles (one kilometer) underground.Nicholas Kamm / AFP / Getty Images]

The seismic energy in areas with stable bedrock "stable continental craton" in geophysics speak can travel much farther than it can when broken up by young faults.

"Seismic energy attenuates very slowly on the East Coast," Powers said. "On the West Coast it attenuates much more rapidly because the bedrock is fractured and faulted and much more variable in its composition than on the East Coast."

Seismologist Dr. Lucy Jones joins Brian Williams from the United States Geological Survey headquarters in Pasadena, Calif.

The survey notes that earthquakes in the central and eastern U.S. are typically felt over a much broader region than those in the Western U.S., sometimes an area as much as ten time larger than similar magnitude earthquake on the West Coast.

"A magnitude 5.5 eastern U.S. earthquake usually can be felt as far as 300 miles from where it occurred, and sometimes causes damage as far away as 25 miles," the agency notes on its website.

Early reports indicated the depth of the earthquake is also quite shallow just 3.7 miles down in the Earth's crust. Powers said this would likely be revised deeper as time goes by and the data is further analyzed, but depth here isn't much of a factor in the shaking.

The earthquake today on the East Coast, Powers said, was large enough to be felt over a large area no matter if its depth is ultimately determined to be 3 miles or 15 miles deep. "At that point, the depth really isn't much of a factor."

Depth can be a factor In other regions, however, depth of an earthquake can make a difference.

Generally, the closer the epicenter of an earthquake is to the surface, the stronger the shaking on the surface and the more damage they cause, no matter what their size.

Conversely, when earthquakes rupture deeper in the crust they can rupture up to 500 miles deep more energy is lost as it races to the surface.

That's one reason why some relatively strong earthquakes, originating deep in the crust, cause little damage on the surface whereas some seemingly small earthquakes can cause massive damage.

The 7.0 magnitude earthquake in Haiti in January 2010 was 8.1 miles deep. The relatively shallow depth combined with subpar construction in Haiti caused massive damage there.

A pair of minor earthquakes in Spain this May ruptured just over half a mile below the ground, causing several deaths and damaging buildings in a part of the world with a tame seismic history.

The 9.0 magnitude earthquake hit Japan on March 11 began at a depth of 19.9 miles. Though devastating, it could have been worse had it been even shallower and had Japan's infrastructure not been among some of the most earthquake ready in the world.

John Roach is a contributing writer for Connect with the Cosmic Log community by hitting the "like" button on the Cosmic Log Facebook page or following's science editor, Alan Boyle, on Twitter (@b0yle).

NBC's Tom Costello reports from the earthquake epicenter in Mineral, Va., where the roof of the town hall collapsed in the quake.

An 5.8-magnitude earthquake in central Virginia was felt across much of the East Coast on Tuesday, causing light damage and forcing thousands of people to evacuate buildings in New York, Washington and other cities. NBC's Lester Holt reports.

Chief News Editor: Sol Jose Vanzi

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