US East Coast Shook By Strongest Earth Quake In 67 years UPDATES magnitude; Map locates the epicenter of an earthquake in Virginia. US East Coast was hit by a 5.8-magnitude earth quake at 1:51 p.m. Eastern Time, Tuesday. The epicenter was 5 miles (8 kilometers) from Mineral, Virginia, and 84 miles (135 kilometers) away from Washington, D.C. People ran out of their houses, tall buildings and offices. Parts of the White House, Capitol and Pentagon were evacuated. Some people did not know that was an earth quake and thought that it was an explosion, a bomb or a terrorist attack on their buildings. The quake was felt as far north as Toronto, as far west as Indiana and Kentucky and as far south as Atlanta and Savannah, Ga. Richmond Times-Dispatch, Bob Brown - Members of the public and staff stand outside the Virginia State Capitol in Richmond, Va., Tuesday, Aug. 23, 2011, after an earthquake caused evacuation of many structures in the city. (AP Photo/Richmond Times-Dispatch, Bob Brown) Civilians and military personnel evacuate the Pentagon in Washington after an earthquake was felt on Tuesday, Aug. 23, 2011. (AP Photo/U.S. Navy, Mass Communication Specialist 2nd Class Jason Graham) US Park Service helicopter patrols over the White House in Washington, Tuesday, Aug. 23, 2011, as a member of the Secret Service walks across the roof of the White House following an earthquake in the Washington area. The 5.9 magnitude earthquake centered northwest of Richmond, Va., shook much of Washington, D.C., and was felt as far north as Rhode Island and New York City. (AP Photo/Pablo Martinez Monsivais) People who came out on the street after an earthquake look up at a window that cracked during the quake on Market Street in Philadelphia, Tuesday, Aug. 23, 2011. (AP Photo/Alex Brandon) A worker with Baltimore Gas and Electric walks past a square where workers wait for word to re-enter their office buildings after an earthquake was felt in Baltimore on Tuesday, Aug. 23, 2011. Downtown office buildings were cleared and workers were waiting for clearance to re-enter. (AP Photo/Patrick Semansky) A worker with Baltimore Gas and Electric walks past a square where workers wait for word to re-enter their office buildings after an earthquake was felt in Baltimore on Tuesday, Aug. 23, 2011. (AP Photo/Patrick Semansky) Debris covers the floor of the Miller's Mart food store in Mineral, Va., a small town northwest of Richmond near the earthquake's epicenter, Tuesday, Aug. 23, 2011. The most powerful earthquake to strike the East Coast in 67 years shook buildings and rattled nerves from South Carolina to Maine. (AP Photo/Steve Helber) People crowd Pennsylvania Avenue in Washington, Tuesday, Aug. 23, 2011, as buildings were evacuated following an earthquake in the Washington area. (AP Photo/Charles Dharapak) The sun sets behind a quake damaged building in Mineral, Va., a small town close to the epicenter, Tuesday, Aug. 23, 2011. (AP Photo/Steve Helber) Share this:Click to share on Facebook (Opens in new window)Click to share on Twitter (Opens in new window)Click to email a link to a friend (Opens in new window)Click to print (Opens in new window)Like this:Like Loading... Related Author: Ahmad Ali Karim Blogger. Official Ambassador at Muafakat Pendidikan Johor (MPJ). Columnist at Utusan Malaysia. Secretary at Pertubuhan Permuafakatan Pendidikan Malaysia (ME'DIDIK). View all posts by Ahmad Ali Karim
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Plate tectonics is a scientific theory which describes the large scale motions of Earth’s lithosphere. The theory builds on the older concepts of continental drift, developed during the first decades of the 20th century, and was accepted by the majority of the geoscientific community when the concepts of seafloor spreading were developed in the late 1950s and early 1960s. The lithosphere is broken up into what are called tectonic plates. In the case of the Earth, there are currently seven or eight major (depending on how they are defined) and many minor plates. The lithospheric plates ride on the asthenosphere. These plates move in relation to one another at one of three types of plate boundaries: convergent, or collisional boundaries; divergent boundaries, also called spreading centers; and conservative transform boundaries. Earthquakes, volcanic activity, mountain-building, and oceanic trench formation occur along these plate boundaries. The lateral relative movement of the plates varies, though it is typically 0–100 mm annually.
Dear Mr. Micheal H. Miller,
Thank you for the information.
I wish I can have a book that explains about earthquakes for kids with illustrations.
I have a few books about volcano.
Please visit my blog again ☻