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Craig earthquake 2013

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Journal Article
Published: 14 April 2015
Bulletin of the Seismological Society of America (2015) 105 (2B): 1153–1164.
... and model fits for selected sites. On 5 January 2013 at 08:58 UTC, the Craig M w  7.5 earthquake occurred off the coast of Alaska about 113 km west of Craig and 114 km south of Port Alexander, as located by the Alaska Earthquake Center. The mainshock initiated at 10 km depth and was accompanied...
FIGURES | View All (7)
Journal Article
Published: 07 April 2015
Bulletin of the Seismological Society of America (2015) 105 (2B): 1143–1152.
...Stephen Holtkamp; Natalia Ruppert Abstract The M w 7.5 Craig, Alaska, earthquake on 5 January 2013 was the second largest earthquake on the Queen Charlotte fault ( QCF ) in 40 yrs, representing the transform plate boundary between the Pacific and North American plates. Earthquake hazard along...
FIGURES | View All (7)
Image
Published: 14 April 2015
Figure 7. Finite‐fault models for the 2013 Craig earthquake representing the preferred model with the least constrained (top) and the most constrained (bottom) fault geometry. Both models have a centered hypocenter of 15 km, with a rupture velocity of 4  km/s along the positive 333° strike and 1
Journal Article
Published: 14 April 2015
Bulletin of the Seismological Society of America (2015) 105 (2B): 1053–1057.
...Thomas S. James; John F. Cassidy; Garry C. Rogers; Peter J. Haeussler 6 February 2015 The 27 October 2012 M w  7.8 Haida Gwaii thrust earthquake and the 5 January 2013 M w  7.5 Craig strike‐slip earthquake are the focus of this special issue. They occurred along the transform...
FIGURES
Journal Article
Published: 14 April 2015
Bulletin of the Seismological Society of America (2015) 105 (2B): 1129–1142.
...Figure 7. Finite‐fault models for the 2013 Craig earthquake representing the preferred model with the least constrained (top) and the most constrained (bottom) fault geometry. Both models have a centered hypocenter of 15 km, with a rupture velocity of 4  km/s along the positive 333° strike and 1...
FIGURES | View All (8)
Journal Article
Published: 07 April 2015
Bulletin of the Seismological Society of America (2015) 105 (2B): 1219–1230.
... for amplification of surface waves observed at seismic stations in Alaska ( Gomberg, 2013 ) and may provide a potential link between this 2012 event and the 2013 Craig, Alaska, earthquake. Online Material: Figure of all relative source time functions used in directivity analysis. * Now at the School of Earth...
FIGURES | View All (10)
Journal Article
Published: 14 April 2015
Bulletin of the Seismological Society of America (2015) 105 (2B): 1165–1177.
... broadband stations in the Canadian National Seismograph Network and find that the 2012 M w 7.8 Haida Gwaii and 2013 M w 7.5 Craig, Alaska, earthquakes triggered long duration (>10 s), emergent tremor‐like signals near the southeastern portion of the EDF . In both cases, tremor coincides with the peak...
FIGURES | View All (10)
Journal Article
Journal: Geosphere
Published: 02 April 2020
Geosphere (2020) 16 (3): 712–722.
... in 1972. Many of the northern aftershocks locate east of the Queen Charlotte fault. This pattern is similar to aftershocks observed in the 2013 M w = 7.5 Craig, Alaska earthquake. Recent and pre-1971 (1925–1970) seismicity indicates that the regions where aftershocks clustered remained active through time...
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Image
Published: 07 April 2015
( Koehler, 2013 ). Active seismic stations are shown by black triangles, and population centers near the M w  7.5 Craig earthquake are shown by yellow squares and associated labels. Major earthquakes (stars), their aftershocks (circles), and estimated rupture zones are as follows: large white star, 1927
Image
Published: 14 April 2015
are using a shelf structure, and moment tensors for all earthquakes in the Global Centroid Moment Tensor (Global CMT) catalog between 1990 and 2013 are plotted on the right ( Ekström et al. , 2012 ). Small circles are aftershocks within 30 days of the Craig mainshock, and the largest fault used
Image
Published: 14 April 2015
Figure 1. Map view of the study region. Black lines indicate fault traces, gray dots indicate background seismicity during 2010–2013 from the Advanced National Seismic System earthquake catalog, gray triangles indicate AK network stations, and black triangles indicate CN network stations. Focal
Image
Published: 14 April 2015
Figure 1. Map view of the study region. Black lines indicate fault traces, gray dots indicate background seismicity during 2010–2013 from the Advanced National Seismic System earthquake catalog, gray triangles indicate AK network stations, and black triangles indicate CN network stations. Focal
Image
Published: 29 February 2024
Figure 1. Tectonic setting and surface topography of the present study region. Red dashed curves outline the Snake River plain (SRP) and the Rocky Mountain front (RMF). The red focal mechanism plot denotes the epicenter and fault‐plane solution of the 2013 M 4.8 Wyoming upper‐mantle earthquake
Image
Published: 07 April 2015
 7.8 earthquake. Times of offsets for the M w  7.8 Haida Gwaii (28 October 2012) and M w  7.5 Craig, Alaska (5 January 2013), events are shown by the vertical gray lines in (a) and (b).
Image
Published: 14 April 2015
Figure 1. Location map for the 2012 M w  7.8 Haida Gwaii and 2013 M w  7.5 Craig earthquakes, which occurred on the Pacific–North American plate boundary. Approximate rupture zones for the two events are shown in yellow, whereas other significant events on the plate boundary are depicted
Image
Published: 07 April 2015
Figure 1. Tectonic setting of the Haida Gwaii earthquake, including the trace of the Queen Charlotte fault ( QCF ). (a) The location of the 2012 mainshock (U.S. Geological Survey [USGS] focal mechanism) in relation to other large earthquakes in the region, including the 2012 M w  7.5 Craig
Image
Published: 07 April 2015
Figure 1. Tectonic setting of the Haida Gwaii earthquake, including the trace of the Queen Charlotte fault ( QCF ). (a) The location of the 2012 mainshock (U.S. Geological Survey focal mechanism) in relation to other large earthquakes in the region, including the 2012 M w  7.5 Craig, Alaska
Image
Published: 14 April 2015
Figure 6. Stations used in the finite‐fault slip inversion of the 2013 Craig earthquake. The map has the location of each station relative to the NEIC hypocenter, showing the good azimuthal coverage. The seismograms show P waves (left) and SH waves (right) with solid lines for the recorded
Image
Published: 14 April 2015
Figure 6. Stations used in the finite‐fault slip inversion of the 2013 Craig earthquake. The map has the location of each station relative to the NEIC hypocenter, showing the good azimuthal coverage. The seismograms show P waves (left) and SH waves (right) with solid lines for the recorded
Image
Published: 14 April 2015
by aftershocks for major historic earthquakes along the margin are indicated by dashed black outlines ( Plafker et al. , 1994 ). Aftershocks (circles) and focal mechanisms for the 2013 M w  7.5 Craig earthquake and the 2012 M w  7.8 Haida Gwaii earthquake are also included, along with a magnitude scale