February 28th marks the anniversary of the Nisqually Earthquake. The earthquake had a magnitude of 6.8, a depth of 52 km, with a hypocenter about 17.8 km NE of Olympia, Washington. A clearinghouse with information about this earthquake can be found here.
The earthquake sequence that struck the city of Christchurch and surrounding Canterbury region in 2010-2011 has had unprecedented impacts in all spheres of New Zealand society. The Canterbury earthquake sequence had many geologically remarkable characteristics, with ramifications for all aspects of life in the region. To commemorate the anniversary of the most devastating, M6.3 Christchurch earthquake of February 22, 2011 CREW highlights some of the key lessons which can be found here.
The February 2014 issue of National Geographic magazine includes a story about plans to build a tsunami refuge at Ocosta Elementary School in Westport, Washington. The story includes quotes from CREW member John Schelling (State of Washington) and mapped evacuation-modeling results from CREW member Nathan Wood (USGS).
January 26, 2014 marked the 314-Year Anniversary of the last Cascadia Earthquake
SEATTLE— The last Cascadia Subduction Zone earthquake occurred one hundred years before Lewis and Clark saw the Pacific Ocean. It was a time when native traditions spoke of the ground shaking and the waters rising. There were no bridges to fall and no schools, hospitals and other critical infrastructure in tsunami inundation zones. It was a time when Cascadia was much more resilient than today. “The very advances that are the foundations of our modern communities create vulnerability along with convenience” said Michael Kubler, Cascadia Region Earthquake Workgroup (CREW) President. “The revised Cascadia scenario is a crucial tool for regional leaders to use in developing policies and plans for the next earthquake.”
Events over the last few years have expanded our understanding of earthquake science and the hazards faced by our region from a future Cascadia Subduction Zone earthquake. The Cascadia Subduction Zone extends along the coastlines of northern California, Oregon, Washington, and southern British Columbia. There’s no doubt that Cascadia is capable of producing earthquakes and tsunamis on the same scale as the magnitude 8.8 earthquake off Chile in 2010 and the magnitude 9.0 quake that devastated the east coast of Japan in 2011.
Cascadia’s last great earthquake occurred on January 26, 1700—stresses have been building on the fault ever since. While the full extent of the earthquake hazard was not realized until the 1980s, the Cascadia subduction zone is now one of the most closely studied and monitored regions in the world. “In 2005 CREW first published the Cascadia earthquake scenario, but so much new information has emerged that an update was needed” said Heidi Kandathil, CREW Executive Director. The newly updated Cascadia Scenario joins the list of other free products developed by CREW to help the region’s residents, schools, businesses, planners, and emergency managers prepare for future earthquakes. The Scenario and other materials are available online at http://tinyurl.com/m34v2ex.