washington fault line map

This map gives an overview of geologically young faults and is intended to help in evaluation of the potential activity of faulting nationally. Photo by Steve Palmer. Please visit our Geologic Information Portal and Geologic Hazard Maps page for the most up-to-date listing of all of our hazard maps. In much of Washington, dense vegetation covers the land and makes finding faults very difficult. After a large earthquake it is common to have other large earthquakes for hours, days, and even weeks. Larger crustal faults, such as the Seattle fault and southern Whidbey Island fault zone, can produce earthquakes up to magnitude 7.5. Geologists are constantly trying to better understand the faults in our state. All of the following resources can also be found on our Publications and Maps page, through the For each increase in earthquake magnitude, there are about 10 times fewer earthquakes. HomePrograms and ServicesGeologyGeologic Hazards. Each of the earthquakes listed on the bottom of the screen is capable of significant damage. Hover over a cluster of earthquakes to learn about the different types in the Pacific Northwest. Faults running on the Snohomish County-Skagit County line and between Port Townsend and Whidbey Island point toward Vancouver Island. Identify and secure items in your home or work that could cause damage. Even when an earthquake happens on a fault that doesn’t reach the surface, the ground can still show signs of cracking. It is a qualitative scale that ranges from I–XI (1-11) and measures the amount of damage caused by an event. This was a problem because no two locations would agree on the size of the same earthquake. MORE FROM SEATTLEPI: Remembering when Mount St. Helens blew its top. The shaking can damage or destroy buildings and other infrastructure. The biggest faults in the world are those on the edges of tectonic plates. Hold on to any sturdy shelter until the shaking stops. Know what other hazards you might face. It is not yet possible to predict when a fault will have an earthquake. Coupeville, WA 98239, Camano Office Photo courtesy of Brian Sherrod. Faults can be grouped based on their relative movement into three types. These aftershocks can last for hours to weeks or months. Photo courtesy of MOHAI (neg. Many faults have not been studied enough to know if they are active. Even when the location of a fault is known, there is much additional work to determine how hazardous it may be. USA Earthquake Hazard Map. For some active faults, such as the Seattle fault or Cascadia subduction zone, we can also learn how often large earthquakes have happened in the past. In this sense, the shaking of the ground is the ‘sound’ of rocks breaking and moving deep within the Earth. This means that when the Seattle fault ruptures the south side of the fault moves up relative to the north side. The map also shows potentially active faults from a separate 2014 report (click here to download). Both types of faults can cause ground shaking during an earthquake and may cause permanent deformation of the ground. Will Washington know an earthquake is coming? Washington’s fault lines tend to sweep east-west. However, we can learn which faults are active and which are inactive. This is a direct result of the problems discussed above—our knowledge of faults beneath the earth’s surface, where earthquakes occur, is limited. When an earthquake happens there will not be time to google what you are supposed to do. Repeating Earthquakes on Mount Rainier - are glaciers the culprit? Cover your head and neck with your arms to protect against falling debris. Photo from, Liquefaction can be a big problem. Check out the gallery above for a look at where an earthquake will hit Seattle hardest. This earthquake caused parts of Restoration Point near on Bainbridge Island to be lifted 35 feet straight up. Aftershocks can be nearly as large as the main earthquake and can cause significant additional damage. Consider subscribing to our blog, Washington State Geology News, to receive notifications when new information is published. Throughout the world ‘shallow’ earthquakes generally refer to earthquakes that are less than ~45 miles deep. Most damage and loss of life in earthquakes is a result of ground shaking. It can also make landslides that are much bigger than expected. Coupeville, WA 98239, Main Line: These older faults do not have any evidence for recent activity, but the Earth is always changing. In Washington, the risk from earthquake-induced landslides is large. The new “Display Faults” tool is a great way for you to learn more about the geology of the Pacific Northwest, but before you start exploring the map, here are some final caveats: 1)   The faults shown are the ones we know about, and not all the faults that exist, 2)   Only the faults in Oregon and Washington are on the map, and. For example, if you take a bucket full of sand and push on the sides of the bucket, cracks will form in the sand. Most are too small to be felt or cause damage. The Seattle fault, which runs from Bainbridge Island, across the Puget Sound, and through West Seattle and Bellevue, is an example of a fault formed as a result of the Earth horizontally compressing. These large underwater slides only occur during very large earthquakes and are one way to learn about earthquakes that happened thousands of years ago. The map is from a 2007 report (click here to download) on seismic design categories in Washington. Unfortunately, both looking for faults in the field and LiDAR surveys have limitations. Charles Richter and Beno Gutenberg discovered that for every magnitude of earthquake, there are about ten times more earthquakes of the next lower magnitude. Visit our School Seismic Safety page for more information. Also, very large earthquakes were difficult to measure accurately. This map is from a 2007 report on the seismic design categories in Washington. Tsunamis triggered by earthquakes usually require at least a M7 event. 572 - Southern Whidbey Island fault zone First, these Seattle neighborhoods are most likely to see liquefaction in a major shaker. ​, * NOTE: Hazard maps for each jurisdiction will only be included if that jurisdiction is at risk to that hazard.​​, Copyright Island County. The Washington Geological Survey develops, produces, and publishes a large variety of maps and reports on the hazards faced by our state. It devastated the coast of the Pacific Northwest and sent an ‘orphan’ tsunami to Japan. Photo from Pacific Northwest Seismic Network Seismo Blog. Geothermal project starts soon. This means that a tsunami made by an earthquake on the Cascadia subduction zone will start to impact the Washington coast in less than 15 minutes. Within this rich oral history there are many references to events like earthquakes and tsunamis. Before modern record keeping, Native Americans lived in the Pacific Northwest for thousands of years. These maps are created by small planes that use a specific type of laser to measure the elevation of the ground. Washington’s faults: Where the Earth moves the Seattle area, https://www.seattlepi.com/seattlenews/article/Washington-s-faults-Where-the-earth-moves-the-12411552.php, HistoryLink, Washington’s online encyclopedia, described the discovery. The Cascadia subduction zone last ruptured over 300 years ago on January 26, 1700. Once a fault is located, it is important to know if it is active. Another complication is that faults can look different at depth than they do on the surface. The map is from a, This car was parked on sand during the 2011 earthquake in Christchurch, New Zealand. An earthquake can be a scary event. Stay away from glass, windows, outside doors and walls, and anything that could fall down. Another large plate-boundary fault is the San Andreas Fault, where two plates slide past each other rather that moving towards each other like in Cascadia. If a large earthquake happens, be prepared for many more earthquakes. By looking at maps made with LiDAR, scientists can identify faults that are not immediately obvious out in the field. Although we cannot predict exactly when the next earthquake will happen, we can predict the general distribution of earthquake sizes. Warm weather triggers snow avalanches at St. Helens, Seismic recordings of a gas explosion in North Bend, WA, Seismic signals generated by the March 22nd Oso Landslide, A New View On What's Shaking on the Cascade Volcanoes, Seismic Spectrograms - A new way to look at wiggles, Large Mount Baker debris Avalanche this fall, Peppy seismic swarm 20 km NW of Mount St Helens, Glacier outburst flood on Mount Baker recorded by the PNSN, Three new ways to view recent earthquakes in the Northwest, M3.5 event west of Tacoma early Sunday morning, Small swarm near Mount McLoughlin last night, Earthquake Early Warning Workshop Quick Report, The Last Cascadia Great Earthquake and Tsunami; 313 Years and Ticking, A flash in the sky, a thump in the ground, 4800 earthquakes in a mild 2012 in the Pacific Northwest, Historical Earthquakes in the Portland Area, Six-year drought of large Pacific Northwest earthquakes, UW Campus ShakeOut exercise Thursday, 10/18/2012. Sometimes Geologists can use the offset land surface to understand how much the fault moved during the earthquake. Ground shaking is a hazard near the epicenter of an earthquake and also in areas far from the earthquake where amplification occurs. Is the plague of great earthquakes this decade a sign of increased danger? Below you will find links to view and download hazard maps created for each jurisdiction included in the current mitigation planning process. This photo shows a fence that was offset about 8.5 feet during the 1906 Great San Francisco Earthquake on the San Andreas fault. When this happens, even a very small slope can cause the ground to slide. View Full Metadata. read more. As part of the Hazard Mitigation Planning process, mapping of the hazards that have the potential to affect the jurisdiction is performed using geographic information systems (GIS) software. It all pointed to a heretofore unknown fault line. The Northern Sangre de Cristo Fault. Oregon and Washington faults added to PNSN earthquake map, West Coast Earthquake Early Warning System on the Horizon, Slow Earthquake Trembles beneath Vancouver Island, Don’t be scared, be prepared: A response to the New Yorker article “The Really Big One”, Unusual earthquake swarm south of Bend, OR, PNW Earthquake Early Warning prototype goes live, Packers versus Seahawks game analysis -- too exciting, Seismology will again watch/help the Seahawk's playoff run. These faults and earthquakes occur in oceanic crust as it is subducted beneath the continent. Expect and help to extinguish fires. This movement happens because stress builds up as tectonic plates move. The last earthquake on the Seattle fault (about AD 950) triggered a landslide and seiche in Lake Washington. This uplift creates a very broad wave called a tsunami. A new analysis of the Seattle area’s risk during a major earthquake has found new locations at higher potential for violent shaking. This fault will have an earthquake in the future, but we cannot predict exactly when. Is Mount St. Helens seismicity increasing? Therefore the line drawn on the map from the surface expression may not represent where the fault is at depth. The map is from a 2007 report (click here to download) on seismic design categories in Washington. Stop as quickly as safety permits and stay in the vehicle. Finding faults and knowing how often they rupture is one of the most important tasks to keep society safe from these hazards. The buildings sank when ground shaking weakened the underlying sediments. The Arizona Geological Survey collates and serves geological information for Arizona and other states through its partnership with other state geological surveys.

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