|Title||Introduction to the Special Issue on the 2012 Haida Gwaii and 2013 Craig earthquakes at the Pacific-North America plate boundary (British Columbia and Alaska)|
|Author||James, T S; Cassidy, J F; Rogers, G C; Haeussler, P J|
|Source||Bulletin of the Seismological Society of America vol. 105, no. 2B, 2015 p. 1053-1057, https://doi.org/10.1785/0120150044|
|Alt Series||Earth Sciences Sector, Contribution Series 20140485|
|Publisher||Seismological Society of America|
|Media||paper; on-line; digital|
|File format||pdf; html|
|Province||Western offshore region|
|Area||Moresby Island; Queen Charlotte Terrace; Haida Gwaii; Alaska; Canada; United States|
|Lat/Long WENS||-136.0000 -130.0000 57.0000 51.5000|
|Subjects||tectonics; earthquakes; tectonic environments; plate tectonics; plate boundaries; crustal movements; Queen Charlotte fault|
|Program||Western Canada Geohazards Project, Public Safety Geoscience|
|Released||2015 04 07|
This is an overview article for a special issue on the 2012 Haida Gwaii and 2013 Craig earthquakes containing 19 original research papers.
|Summary||(Plain Language Summary, not published)|
The magnitude 7.8 earthquake of October 27, 2012 was the largest thrust earthquake ever recorded along the mainly strike slip margin to the west of Haida
Gwaii on the coast of British Columbia. It was followed by a magnitude 7.5 earthquake on the same plate boundary slightly more than 2 months later farther north in southeastern Alaska. This article summarizes 19 original research papers appearing in
a special issue focussing on these two earthquakes. It includes papers describing the geological setting, the characteristics of the earthquakes and their aftershocks, and other consequences of the earthquakes, such as intensity of ground shaking.
The research improves understanding of large thrust and strike-slip earthquakes and has applicability in other seismically-active regions of Canada.