Severe, Multiple Seismic Events.
We are only posting this for general information.
We are not "Experts"
This is a lot of action all at once.
Stay Informed.
Updates here frequently.
It's really all about situational preparedness. What you have control over.
Cheers.
UPDATE: 7.1.2013
Update: 6.1.2013
We are only posting this for general information.
We are not "Experts"
This is a lot of action all at once.
Stay Informed.
Updates here frequently.
It's really all about situational preparedness. What you have control over.
Cheers.
UPDATE: 7.1.2013
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5.2 - Taiwan region
Severe // Earthquake | Japan |
less than minute ago / 0 Comments / Share | via feed / Source |
Update: 6.1.2013
M5.1 - 7km ESE of Palomares, Mexico 2013-01-06 18:24:45 UTC
Summary
Location and Magnitude contributed by: USGS, NEIC, Golden, Colorado (and predecessors)
General
Event Time
- 2013-01-06 18:24:45 UTC
- 2013-01-06 12:24:45 UTC-06:00 at epicenter
- 2013-01-06 12:24:45 UTC-06:00 system time
Location
17.135°N 94.994°W depth=65.3km (40.6mi)Nearby Cities
- 7km (4mi) ESE of Palomares, Mexico
- 28km (17mi) N of Matias Romero, Mexico
- 62km (39mi) N of San Jeronimo Ixtepec, Mexico
- 75km (47mi) NNW of Union Hidalgo, Mexico
- 505km (314mi) ESE of Mexico City, Mexico
M7.5 - 94km W of Craig, Alaska 2013-01-05 08:58:19 UTC
Summary
Location and Magnitude contributed by: USGS, NEIC, Golden, Colorado (and predecessors)
General
20 km
20 mi
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55.368°N, 134.621°W
Depth: 9.8km (6.1mi)
Depth: 9.8km (6.1mi)
Event Time
- 2013-01-05 08:58:19 UTC
- 2013-01-04 23:58:19 UTC-09:00 at epicenter
- 2013-01-05 02:58:19 UTC-06:00 system time
Location
55.368°N 134.621°W depth=9.8km (6.1mi)Nearby Cities
- 94km (58mi) W of Craig, Alaska
- 300km (186mi) WNW of Prince Rupert, Canada
- 326km (203mi) S of Juneau, Alaska
- 397km (247mi) WNW of Terrace, Canada
- 596km (370mi) S of Whitehorse, Canada
Tectonic Summary
The
January 5, 2013 M 7.5 earthquake off the west coast of southeastern
Alaska occurred as a result of shallow strike-slip faulting on or near
the plate boundary between the Pacific and North America plates. At the
location of this earthquake, the Pacific plate is moving approximately
northwestward with respect to the North America plate at a velocity of
51 mm/yr.
This earthquake is likely associated with relative motion across the Queen Charlotte fault system offshore of Alaska and British Columbia, Canada, which forms the major expression of the Pacific:North America plate boundary in this region. The surrounding area of the plate boundary has hosted 8 earthquakes of magnitude 6 or greater over the past 40 years; In 1949, a M 8.1 earthquake occurred close to the Pacific:North America plate boundary approximately 230 km to the south east of the January 5 earthquake, as a result of strike-slip faulting. In October of 2012, a M 7.8 earthquake occurred approximately 330 km to the south east of the January 5 event, slightly inboard of the plate boundary, and was associated with oblique-thrust faulting. The latter earthquake was likely an expression of the oblique component of deformation along this plate boundary system. The January 5, 2013 earthquake is related to that Haida Gwai earthquake three months previously, and is an expression of deformation along the same plate boundary system.
The January 5 event broke a fault approximately 50 km in length, and slipped 7-8 m. Aftershocks of the earthquake can be seen here.
This earthquake is likely associated with relative motion across the Queen Charlotte fault system offshore of Alaska and British Columbia, Canada, which forms the major expression of the Pacific:North America plate boundary in this region. The surrounding area of the plate boundary has hosted 8 earthquakes of magnitude 6 or greater over the past 40 years; In 1949, a M 8.1 earthquake occurred close to the Pacific:North America plate boundary approximately 230 km to the south east of the January 5 earthquake, as a result of strike-slip faulting. In October of 2012, a M 7.8 earthquake occurred approximately 330 km to the south east of the January 5 event, slightly inboard of the plate boundary, and was associated with oblique-thrust faulting. The latter earthquake was likely an expression of the oblique component of deformation along this plate boundary system. The January 5, 2013 earthquake is related to that Haida Gwai earthquake three months previously, and is an expression of deformation along the same plate boundary system.
The January 5 event broke a fault approximately 50 km in length, and slipped 7-8 m. Aftershocks of the earthquake can be seen here.
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