Earthquakes
The quake hit at 4.55 am (7.55am AEDT today) 95 kilometres east-southeast of the city of Padangsidempuan in North Sumatra at a relatively deep 213km, USGS said.
Saturday, November 20, 2010 at 19:06:35 UTC
Saturday, November 20, 2010 at 01:06:35 PM at epicenter
Time of Earthquake in other Time Zones
Location:
35.319°N, 92.303°W
Depth:
4.5 km (2.8 miles)
Region:
ARKANSAS
Distances:
3 km (2 miles) ESE (102°) from Guy, AR
10 km (6 miles) SW (228°) from Quitman, AR
11 km (7 miles) E (89°) from Twin Groves, AR
29 km (18 miles) NNE (28°) from Conway, AR
65 km (40 miles) N (2°) from Little Rock, AR
411 km (255 miles) SSW (207°) from St. Louis, MO

A day after the earthquake, a young woman climbs over shopping carts and the rubble of a collapsed store on January 13, 2010 in Port-au-Prince, Haiti.
To geologists, it's good to see Haitians on such heightened alert. Most scientists believe the western hemisphere's poorest country is hardly out of the seismic woods - and after studying the Haiti quake data for the past 10 months, they're more convinced than ever that Haitians can expect another major quake sooner rather than later. That's largely because they've found, according to a new study by 10 prominent geologists, that the lion's share of the January temblor occurred not along the fault line they originally suspected, known as the Enriquillo - Plantain Garden fault zone, but on a previously unknown fault. (Faults separate plates in the earth's crust, which cause quakes when stress makes them collide.) As a result, says Falk Amelung, a University of Miami geologist and one of the report's authors, "the prospects of another serious event may be rather worse than we first thought."
When Amelung and other geologists started poring over information from the earthquake's satellite-radar images last January, they were flummoxed by a variety of features. One was the vertical motion the quake exhibited - unusual because the Enriquillo, which runs across Haiti's southern peninsula just below Port-au-Prince, is a strike-slip fault, the kind that almost exclusively displays horizontal motion when it ruptures. At the same time, the quake's horizontal movement was partly north-south, another anomaly for a strike-slip fault. "Those were the two important smoking guns" that made scientists question their early assumptions about the quake, says Eric Calais, a Purdue University geologist who is in Haiti as a science adviser to the U.N. Development Program and is a lead author of the study, which was published last month in Nature Geoscience.(See more about the January earthquake that devastated Haiti.)
The quake occurred at 7:02 a.m. CST about three miles underground and registered a preliminary magnitude of 3.3, the USGS said.
Platte County emergency services director Tim Hofbauer and the sheriff's office said there were no reports of injuries or damage.
Lennie Hiltner, Schuyler police chief, said he had stopped by a car dealership when he heard a loud noise but didn't feel anything shake. He and others at Reinecke Motor Co. quickly inspected the building but found no damage.
Several people called the police department to report hearing the noise.
A mild earthquake was felt in northern Israel early Tuesday, many residents reported. The Geophysical Institute reported an earthquake measuring 3.6 on the Richter Scale was felt in the Moshav Avivim area at 4:32 am. No injuries or damage were reported.
Yael of Safed said the quake caused her to wake up as she felt her house move. "I got up and felt the bed literally shaking under my stomach, actually moving. I can't fall back to sleep I'm so afraid."
Yael noted that some of her neighbors also woke up and added no damage was caused.
But, earthquake swarms happen, even in places that are not normally known for seismic activity. What's unusual about this particular group of earthquakes?
In this case, it seems that the vast majority of the quakes are happening at almost exactly a depth of 10 kilometers; over 20 earthquakes have occurred at that depth since the swarm began. I'm no statistician, but that seems like a pretty exceptionally unlikely scenario, especially when the region was entirely quiet in terms of seismic activity as of yesterday. It would definitely be interesting to see what real geologists make of it.
The quake struck 155 kilometers (95 miles) southeast of the nation's capital, Santo Domingo, at about 12:35 a.m. Saturday (11:35 p.m. Friday ET).
Wednesday, November 10, 2010 at 04:05:24 UTC
Wednesday, November 10, 2010 at 10:05:24 AM at epicenter
Time of Earthquake in other Time Zones
Location:
45.538°S, 96.394°E
Depth:
10.7 km (6.6 miles)
Region:
SOUTHEAST INDIAN RIDGE
Distances:
2250 km (1400 miles) SW of PERTH, Western Australia, Australia
Wednesday, November 03, 2010 at 23:34:44 UTC
Thursday, November 04, 2010 at 12:34:44 PM at epicenter
Time of Earthquake in other Time Zones
Location:
20.440°S, 174.290°W
Depth:
33.2 km (20.6 miles)
Region:
TONGA
Distances:
120 km (75 miles) NE of NUKU'ALOFA, Tonga
200 km (125 miles) S of Neiafu, Tonga
460 km (285 miles) E of Ndoi Island, Fiji
2100 km (1310 miles) NNE of Auckland, New Zealand
Wednesday, November 03, 2010 at 11:18:16 UTC
Wednesday, November 03, 2010 at 08:18:16 PM at epicenter
Time of Earthquake in other Time Zones
Location:
4.614°S, 134.040°E
Depth:
14.8 km (9.2 miles) set by location program
Region:
NEAR THE SOUTH COAST OF PAPUA, INDONESIA
Distances:
130 km (80 miles) N of Dobo, Kepulauan Aru, Indonesia
270 km (170 miles) WSW of Enarotali, Papua, Indonesia
930 km (580 miles) NNE of DARWIN, Northern Territory, Australia
3015 km (1870 miles) E of JAKARTA, Java, Indonesia