Earthquakes
The head of Iran's Crisis Management organization, Hassan Qadami, confirmed the initial 30 casualties to IRNA. However, Bushehr's Governor, Fereydoon Hasanvand, updated the figure to 45 on Thursday night. He added that 'total calm' had settled in the area.
Fars news agency placed the death toll higher, at eight, adding that helicopters would be posted to the area on Friday to assess the extent of the damage.
"There were some houses and electricity poles damaged. Rescue teams have been dispatched," local governor Alireza Khorani told Fars before full news of the wounded emerged.
Tremors were registered at a depth of 16.4 kilometers and some 14 kilometers from the nearest city of Borazjan in Bushehr Province.
While USGS measured the quake at 5.6, the local Seismological Center of Tehran University's Geophysics Institute has said that the earthquake measured 5.7 on the Richter scale.
In the introduction the ZAMG writes:
If one compares the temperature development of the last 15 years to the simulations from the new climate model generation, then one sees a substantial deviation between reality and model: the so-called temperature hiatus."Air temperature is the preferred parameter that experts use to gauge climate change. On the hiatus the ZAMG writes, "In the last 15 years there has been a clear weakening in the global temperature rise; only 3 of 114 climate model simulations account for it (Figure 1)."
It says the quake struck at 2-27 a.m. on Monday (0627 GMT), about 195 miles southeast of the Falklands' capital, Stanley, and 545 miles east of Ushuaia, Argentina. The depth was a shallow 6.2 miles.
The Falklands are a British territory that is claimed by Argentina.
The USGS says the quake followed four others that all measured more than 5.0, over a two-hour period leading up to the big quake. It says such quakes are uncommon in the region. Only 15 quakes of more than magnitude 5.0 had been measured in the region in the previous 40 years.
2013-11-25 06:27:33 UTC
2013-11-25 02:27:33 UTC-04:00 at epicenter
Location
53.881°S 54.882°W depth=10.0km (6.2mi)
Nearby Cities
314km (195mi) SE of Stanley, Falkland Islands
877km (545mi) E of Ushuaia, Argentina
998km (620mi) ESE of Rio Gallegos, Argentina
1031km (641mi) SE of Puerto Deseado, Argentina
314km (195mi) SE of Stanley, Falkland Islands
Technical details
Additional commentary
The November 25, 2013 M7.0 earthquake (06:27:33 UTC) southwest of the Falkland Islands in the South Atlantic Ocean occurred as the result of strike slip faulting, on either a left-lateral fault striking ENE-WSW, or a right-lateral structure striking NNW-SSE. The location of the earthquake, near the ENE-WSW trending plate boundary between the South America and Scotia tectonic plates, suggests it is likely associated with left-lateral faulting along this margin. At the location of this earthquake, the Scotia plate moves ENE with respect to South America at a rate of approximately 9.5 mm/yr.
The November 25, 06:27:33 earthquake was the largest of 5 M5+ events that occurred in a similar area over an approximate 2-hour period, including a M5.6 earthquake 24 seconds prior to the M7.0 mainshock. Though this region experiences moderate-sized earthquakes relatively frequently - 15 M5+ events have occurred within 250 km of the November 25 earthquake over the past 40 years - large events are fairly uncommon. The largest nearby earthquake over the same time period was a M6.6 event in September 1993, 210 km to the east of the November 25 earthquake.
2013-11-25 06:27:09 UTC
2013-11-25 02:27:09 UTC-04:00 at epicenter
Location
53.987°S 54.923°W depth=15.1km (9.4mi)
Nearby Cities
321km (199mi) SE of Stanley, Falkland Islands
872km (542mi) E of Ushuaia, Argentina
997km (620mi) ESE of Rio Gallegos, Argentina
1036km (644mi) SE of Puerto Deseado, Argentina
321km (199mi) SE of Stanley, Falkland Islands
Technical Details
2013-11-23 07:48:32 UTC
2013-11-22 19:48:32 UTC-12:00 at epicenter
2013-11-23 08:48:32 UTC+01:00 system time
Location
17.097°S 176.562°W depth=377.1km (234.3mi)
Nearby Cities
322km (200mi) WNW of Neiafu, Tonga
438km (272mi) E of Lambasa, Fiji
469km (291mi) NNW of Nuku'alofa, Tonga
542km (337mi) ENE of Suva, Fiji
628km (390mi) SW of Apia, Samoa
Technical details
There were no reports of damage, though both ODNR and the Athens County Emergency Management Agency received dozens of calls about the quake. "(Southeast Ohio) is not really a seismically active area," said Tim Leftwich, a seismologist at ODNR. "It's not noted to be an earthquake prone area of the state."
Calls from as far as Charleston, W.Va. were reporting shaking, Leftwich said. Though the county is hundreds of miles from the nearest tectonic plate boundary - in the middle of the Atlantic Ocean - a small fault line runs through the northern part of Athens County, said Doug Green, a geophysicist at Ohio University who studies earthquakes.
"It's consistent, the location of the earthquake (and) the approximate depth are consistent with a structural weak point in the Earth's crust," Green said. The U.S. Geological Survey placed the quake's depth at 7.9 km - too deep to be triggered by a fracking injection well, said Green, who is currently studying drilling's effects on seismic activity.
2013-11-19 13:32:54 UTC
2013-11-19 22:32:54 UTC+09:00 at epicenter
Location
2.647°N 128.402°E depth=63.6km (39.5mi)
Nearby Cities
110km (68mi) NNE of Tobelo, Indonesia
232km (144mi) NNE of Ternate, Indonesia
236km (147mi) NNE of Kota Ternate, Indonesia
382km (237mi) ENE of Bitung, Indonesia
850km (528mi) SW of Koror Town, Palau
Technical details
The U.S. Geological Survey reports that a 5.7 magnitude earthquake has struck Japan 25 kilometers southeast of Toba, releasing the following tweet:
Strong earthquake, NEAR S. COAST OF HONSHU, JAPAN, Nov-18 19:10 UTC, 0 #quake tweets/min, http://t.co/jAAXkTfU5k












