M 3.1, Oklahoma

In this case, the assessment reports have been reviewed by the seismologist. Depth6 km (3.7 miles) (poorly limited) Distances35 km (20 miles) ENE OKLAHOMA CITY, Oklahoma
40 km (25 miles) SE Guthrie, Oklahoma
40 km (25 miles) NW Shawnee, Oklahoma
45 km (30 miles) North and between Norman, Oklahoma
ParametersNST = 14, 18, Nph = DMin = 39 km, Rmss = 0,85 sec, Gp 68 ° =
M-type = "Nuttli magnitude of surface-Wave" (mbLg), version = 6 you can feel it?Report by shaking and damage your location. You can also view report and other accumulated data show map.

CONTINENTAL STABLE REGION EARTHQUAKES
Most of the North America East of the Rocky Mountains rare earthquakes. here and earthquakes are more numerous, for example, the new Madrid seismic zone Southeast Missouri Eastern Quebec, New England, New York-Philadelphia-Wilmington and the rest of the cities when verifying the Kamouraska seismic zone in the middle of the big Rapids. However, the majority of the huge range of Rockies Atlantic to go without large enough and several u.s. States never reported adverse earthquake earthquake year.Earthquakes that occur at irregular intervals in any strike action.

Earthquakes located on the East side of the Rocky Mountains, although less frequently than West, generally felt much wider range.Rockies, located on the East side of an earthquake can be felt even ten times greater than that of the dumping margin, the earthquake on the West Coast area.Order of magnitude 4.0 US eastern earthquake, as a general rule, can the effects of a 100 km (60 mi), intended for planting, other than in many places where it occurred, and it is rarely close to its source.Order of magnitude 5.5 US eastern earthquake, as a general rule, can the effects of a 500 km from where it occurred (300 mi), and sometimes cause damage in so far as the 40 km (25 mi).

BUGS
Earthquakes occur usually miles across the deep bedrock, faults. most of the bedrock of the region was established several generations in the mountains, as a result of increased and were down again last billion or so over the years.

The unconscious of the plate edges as California San Andreas fault system is often scientists set name, which is responsible for a specific fault earthquake. instead, the Rocky Mountains on the East side of the so rarely. maximum range of all parts are far away from the nearest plate boundaries, which in the United States, are in the center of the South Atlantic Ocean to the East of the Caribbean Sea and to the West in California and offshore from Washington and Oregon. known bugs with the region laced but a large number of smaller or deeply buried faults. While most known bugs are poorly earthquake depths. Consequently, a number of earthquakes located on the East side of the Rockies can be linked to a designated faults. it is difficult to determine whether there is a known fault still active and may, on the basis of the packing slip and cause an earthquake. in most areas on the East side of the Rockies is the best guide to earthquake hazards is actually the earthquakes.

Oklahoma information earthquake