what type of plate boundary caused the 1964 alaska earthquake

Deployment of tools like deep ocean pressure sensors (Deep-ocean Assessment and Reporting of Tsunamis or DART) are designed to ensure early detection of tsunamis and acquire data critical to real-time forecasts. These plates constantly move. In Alaska, the Pacific plate, relative to the North American plate, moves at a rate of ~5.5+ cm/yr (~2.2+ in/yr). The 1964 Alaska Earthquake and Tsunami lecture by George Plafker, USGS Geologist Emeritus. Regional uplift and subsidence occurred mainly in two nearly parallel elongate zones, together about 600 miles long and as much as 250 miles wide, that lie along the continental margin. It includes many lesser faults in addition to the San Andreas Fault. Youre now subscribed to NightLife updates. They washed away everything in their immediate path buildings, docks and people. In fact, West notes, four out of every five U.S. quakes occurs in this northernmost state. The data helped engineers develop earthquake-resistant structures to limit future casualties and property damage. When the fault finally slips, its like a rug flattening out. Then, as Alaskas shaking ceased, things got worse much worse. HISTORY.com works with a wide range of writers and editors to create accurate and informative content. Point Reyes National Seashore and Joshua Tree National Park have granitic magma-chamber rocks of the eroded arc, and Pinnacles National Park preserves volcanic rocks. In places, the waves towered as high as a 20-story building. NOAA Natural Hazards Image Database. Reports of residual water sloshing (seiches) came in from the U.S. Gulf Coast and as far away as Australia. Plate boundaries from The Plates Project, University of Texas Institute for Geophysics. Download the official NPS app before your next visit, Plate Tectonics and Our National ParksSite Index, Plate TectonicsThe Unifying Theory of Geology, Tectonic Settings of NPS SitesMaster List. Listing total number of features into an ArcGIS Online feature pop-up, Convergent boundaries: where two plates are colliding. You'll learn why earthquakes happen, how they've shaped the Bay Area, and what you can do to prepare for the next one. Parks in the Sierra Nevada, including Yosemite, Kings Canyon, and Sequoia national parks, contain granite-type rocks that cooled within magma chambers beneath ancient subduction zone volcanoes. Railroad tracks warped. Plafker, G., 1969, Tectonics of the March 27, 1964 Alaska earthquake: U.S. Geological Survey Professional Paper 543I, 74 p., 2 sheets, scales 1:2,000,000 and 1:500,000, https://pubs.usgs.gov/pp/0543i/. Through very complete mapping of vertical deformation and faulting and the application of tectonics, he was first to propose in 1965 that the source of the 1964 Alaska earthquake was a low-angle thrust fault. Tectonic setting. Animations explain the magnitude (Just how big is 9.2? Layers of ocean sediment were squeezed and contorted as they were caught in the vise of the converging plates at the ancient subduction zone. Such boundaries are called transform plate boundaries because they connect other plate boundaries in various combinations, transforming the site of plate motion. This happens because the oceanic plate is denser (heavier) than the continental plate. The friction between these massive plates means they dont move fast. It turned out that the ramps shape was very, very significant. The .gov means its official. The cards slip along their faces, forming a broad zone of shearing between your unaffected hands. It includes the crust and uppermost mantle.) Microplates are smaller fragments of tectonic plates that appear in plate boundary zones. Historically, the Alaska subduction zone is known for its large earthquakes, where the Pacific and North American plates scrape against each other violently as one slides suddenly over the other in the subduction zone. Get a new perspective on earthquakes with this rich collection of multimedia resources. About 200 million years ago, a large tectonic plate (called the Farallon Plate) started to subduct beneath the western edge of North America. As the plates move past each other, they sometimes get caught and pressure builds up. Oral presentations, poster sessions, exhibits, field trips, business meetings and social gatherings all provide participants the opportunity to meet and share with their peers. Scientists measured a wave runup of 220 feet in the Valdez Inlet. Convergent (Colliding): This occurs when plates move towards each other and collide. Ahead of the wave. Science News for Students. Afterwards, geologists realized subduction zonesareas where two tectonic plates (huge slabs of rock made of the earths crust and upper mantle) meet and one bends under the otherplayed a major role in creating the immense Alaskan quake. The movements of the plates help shape the geological features of our planet. Its like opening a sticky window or door. Short video (4 min) by Stephen Wessells, USGS relating how the largest quake in U.S. history had profound and lasting impacts on our lives. Although the school was destroyed, the nearby water tower was undamaged. Tomales Bay is the surface expression of the San Andreas Fault, seen in the photo below. There are three types of tectonic plate boundaries: Another large-scale feature is a hotspot, where a plate rides over a rising plume of hot mantle, creating a line of volcanoes on top of the plate. Plates beneath the oceans are much thinner than those under continents. Society for Science & the Public 20002023. A divergent boundary occurs when two tectonic plates move away from each other. These occur directly along subduction zones. Along with the NOAA Pacific Tsunami Warning Center located at Ford Island, Hawaii, the National Tsunami Warning Center monitors and warns for tsunami threats 24/7 throughout the year. IRIS video directed by Robert F. Butler explaining the science behind the earthquake. Contact Information, Menlo Park, Calif. Imagine that your left hand is the undeformed Pacific Plate, your right hand the intact North American Plate. Transform boundaries occur on the north and south sides of the Caribbean Plate. Earthquakes and tsunamis can happen along any coastline, at any time of the year, but Alaska is particularly prone to them because it sits on the convergence of two tectonic platesthe Pacific Plate and the North American Plate. The landscapes of our national parks, as well as geologic hazards such as earthquakes and volcanic eruptions, are due to the movement of the large plates of Earths outer shell. In Mexico, a combinatiion of divergent and transform plate boundary motion is opening the Gulf of California, causing the Baja Peninsula to separate from the rest of Mexico. Strong ground motion at Seward lasted 3-4 minutes. Updated: August 21, 2018 | Original: March 6, 2018. Remnants of the ancient volcanic mountain chain remain. Then suddenly, it pops open. CHISChannel Islands National Park, California [, CABRCabrillo National Monument, California[, GOGAGolden Gate National Recreation Area, California[, PINNPinnacles National Monument, California[, POREPoint Reyes National Seashore, California[, SAMOSanta Monica Mountains National Recreation Area, California[, BUISBuck Island Reef National Monument, U.S. Virgin Islands[, VIISVirgin Islands National Park, U.S. Virgin Islands[. The tidal wave had diminished by the time it hit Hawaii and Japan, causing little damage. The convergent boundary happens when two plates slide toward each other to form a subduction zone or a continental collision. The Virgin Islands are in a broad zone where the landscape is being sheared up as the Carribean Plate slides eastward past the oceanic part of the North American Plate. This uplift attained a measured maximum on land of 38 feet in a northwest-trending narrow belt less than 10 miles wide that is exposed on Montague Island in southwestern Prince William Sound. SSAs 2014 Annual Meeting will provide a stimulating exchange of research on a wide range of topics with colleagues from all over the world. Sunday: 11 am 5 pm As the tremors ended, local tsunamis sprung up almost immediately, leaving residents little to no time to flee for higher ground. When a continental plate meets an oceanic plate, the thinner, denser, and more flexible oceanic plate sinks beneath the thicker, more rigid continental plate. Both plates are capped by oceanic crust. Some had been up to 24 inches (61 centimeters) in diameter and as much as 101 feet (30.8 meters) above sea level. Special Earthquakes, Earthquake Sequences, and Fault Zones. Most had been killed by the tsunami waves that raked not just the coast of Alaska, but Oregon and California too. Thats a type of convergent plate boundary where one plate dives beneath another. This vehicle illustrates the force of the tsunami waves that had struck this truck, which had been 32 feet (9.8 meters) above sea level at the time of the quake. The major area of uplift trended northeast from southern Kodiak Island to Price William Sound and trended east-west to . Forty million years ago, a large tectonic plate, known as the Farallon Plate, was between the Pacific and North American plates. 1719 N Street, N.W., Washington, D.C. 20036, People and animals sometimes team up to hunt for food, Pokmon evolution looks more like metamorphosis, These beetles drink water using their butts. Sometimes the valleys are partially filled with water, as at Point Reyes National Seashore, where Tomales Bay and Olema Valley follow the main trace of the San Andreas Fault. Afterward, the roots daily bathing for hours each day in salt water killed these trees. USGS.The 1964 Tsunami Strikes Valdez. Transoceanic tsunami waves swept across the Pacific and reached as far away as Hawaii and Japan. This material is also available as a free iBooks textbook and iTunes U course. Department of Homeland Security & Emergency Management.The 1964 Great Alaskan Earthquake and TsunamisA Modern Perspective and Enduring Legacies. This causes the crust to crack and form faults where earthquakes occur. NM = National Monument The San Andreas Fault is the transform plate boundary where a thin sliver of western California, as part of the Pacific Plate, slides north-northwestward past the rest of North America. For example, moving at about 2 inches (5 centimeters) per year, in our lifetime the Pacific Plate moves 10 to 15 feet (3 - 5 meters) past the North American Plate along the San Andreas Fault, a transform plate boundary in California. . Most earthquakes occur at the boundaries where the plates meet. Instead, blocks of crust are torn apart in a broad zone of shearing between the two plates. This stretch of road had been built partly atop mud from a tidal estuary and other unsecure soils. An official website of the United States government. Feb. 13, 2013. Along convergent boundaries, neighboring plates either collide head-on or a denser ocean plate dives beneath a lighter continental plate. These data are incompatible with a significant locked region in this segment of the plate boundary. They still had many questions to answer. Seismicity of the United States, 1568-1989 (Revised), The San Andreas Fault is one of the best examples of lateral plate motion. The long mountain ridges and narrow bays in the region surrounding U. S. Virgin Islands National Park are a product of compression due to the convergence, in addition to lateral motion due to shearing along the transform plate boundary. Quakes cause faraway sloshing. Science News for Students. Subduction causes deep ocean trenches to form, such as the one along the west coast of South America. All rights reserved. That motion was huge, West says. National Park Service sites in the Transverse Ranges include Santa Monica Mountains National Recreation Area and part of Joshua Tree National Park. Originating off the coast of southern Chile on May 22, 1960, the temblor caused substantial damage and loss of life both in that country andas a result of the tsunamis that it generatedin distant Pacific coastal areas. Along other, divergent boundaries, plates move away from each other. The three main types of plate movements include: Divergent (Spreading):This is where two plates move away from each other. These instruments detect and record earthquakes. This subduction zone landscape was later plucked from the edge of the North American Plate and transported nearly 200 miles northwestward along the San Andreas Fault. The epicenter of the 1964 quake occurred deep beneath the Chugach Mountains, shown here some time later. By midnight, 131 people were dead. When oceanic and continental plates meet, the denser oceanic plate moves under the less dense continental plate. Alaska's continental shelf and North American plate rose over 9 meters during the earthquake. (en Espaol). When the ground dropped 3 feet, the trees shallow roots ended up in the tidal zone. But Alaskas 1964 Great Quake led to a huge leap in their understanding. Nows a great time to start window-shopping at the. Before sharing sensitive information, make sure youre on a federal government site. Photo courtesy of the National Parks Conservation Association. the first to be generally understood by earth scientists as having occurred on a subduction zone interface: the slip was along the gently dipping boundary, or "megathrust fault," between the denser downgoing oceanic plate and the lighter overriding continental plate. (2) Intermediate depth seismicity (below 20 miles) occurs in the so-called Benioff Zone, where the subducting Pacific Plate descends towards the mantle beneath the North American Plate. They have been transported about 300 miles (500 kilometers) in a north-northwestward direction along the transform plate boundary. Richter scale Modified Mercalli scale the Centigrade scale the moment magnitude scale. As the plates collide, the oceanic plate is forced beneath the continental plate. The foreground shows a ditch (or graben) that opened up roughly 12 feet (or around 3.7 meters) deep. Is earthquake a result of plate tectonics? The landscapes of Channel Islands National Park, Pinnacles National Park, Point Reyes National Seashore and many other NPS sites in California are products of such a broad zone of deformation, where the Pacific Plate moves north-northwestward past the rest of North America. Maximum indicated uplift in the Alaska and Aleutian Ranges to the north of the zone of subsidence was l feet. The movement releases stored-up 'elastic strain' energy in the form of seismic waves, which propagate through the Earth and cause the ground surface to shake. This was a great leap forward in resolving key mechanisms of the developing theory of plate tectonics. The lower portion (right center) is white from the dried out remains of shellfish that had lived on this rock when it was still part of the seafloor. The March 27, 1964, earthquake was accomp anied by crustal deformation-including warping, horizontal distortion, and faulting-over probably more than 110,000 square miles of land and sea bottom in south-central Alaska. Subduction zones occur when one or both of the tectonic plates are composed of oceanic crust. Transform boundaries - where plates slide passed each other. Finally, the transform boundary, that the San Andreas . Channel Islands National Park includes five islands that are the tops of a mostly-submerged portion of the Transverse Ranges. The earthquake rupture started approximately 25 km beneath the surface, with its epicenter about 6 miles (10 km) east of the mouth of College Fiord, 56 miles (90 km) west of Valdez and 75 miles (120 km) east of Anchorage. OfficeEarthquake Science Center A sudden unlocking could produce an earthquake every bit as big as the one that occurred in Alaska in 1964, when a similar subduction zone boundary snap occurred. The 16 feet (about 200 inches, or 5 meters) of offset along the fence line thus carries a powerful message. Southeast of Florida, the Caribbean Plate is sliding east-northeast about 0.8 inches (2 centimeters) per year relative to the North American Plate. Plate Tectonics and Our National Parks (2020), Text and Illustrations by Robert J. Lillie, Emeritus Professor of Geosciences, Oregon State University [E-mail]. Photos and illustrations above modified from Oregon's Island in the Sky: Geology Road Guide to Marys Peak, by Robert J. Lillie, Wells Creek Publishers, 75 pp., 2017, www.amazon.com/dp/1540611965. The demolished towns of Valdez and Chenega were rebuilt on higher ground, but not everyone was prudent about rebuilding on earthquake-prone land. Since neither plate is stronger than the other, they crumple and are pushed up. Other plates include continents, and some plates include both continents and ocean. Earths crust The outermost layer of Earth. So this was the first earthquake to be recorded around the world. In the days and weeks that followed, dozens of smaller earthquakes continued to rattle Alaska. Slight uplift inland from the major zones of deformation presumably was related to elastic strain changes resulting from the overthrusting; however, the data are insufficient to permit conclusions regarding its cause. At this boundary, the Pacific Plate slides beneath the North American Plate, causing the majority of Alaskas earthquakes, including the 1964 earthquake. Read more from USGS: The Great Alaska Earthquake and Tsunami of March 27, 1964, Teachers' questions: The quake that shook up geology. U.S. Geological Survey Professional Paper 1527, U.S. Geological Survey Point Reyes National Seashore, Golden Gate National Recreation Area, and Pinnacles National Park present landscapes affected by the main line of movement, the San Andreas Fault. The 1964 Alaska earthquake resulted from rupture along the thrust fault boundary bet- ween the downgoing Pacific Plate and the overriding North American Plate, causing widespread shaking and tectonic defor- mation. FOIA This opinion piece by USGS geologist Peter Haeussler, et al. The earthquake hit at 3:11 pm approximately 100 miles (160 km) off the coast of Chile . Fifty years later, it continues to shape Alaska, its people, and the science of earthquakes. Today, almost 60 years since the Great Alaska Earthquake, the Tsunami Warning Centers issue tsunami warnings in minutes, not hours, after a major earthquake occurs. Many transform boundaries are found on the sea floor, where they connect segments of diverging mid-ocean ridges. You can now see under the house to the yard beyond (center right of photo). The 1964 Great Alaska Quake caused several downtown areas of Anchorage to collapse. If a segment of the San Andreas Fault is locked for a century, then a large earthquake might result in 200 inches (2 inches/year x 100 years) of movement along the fault in less than a minute. N Pres = National Preserve. uplift A upward shift in some section of Earths surface due to tectonic activity along a fault. Fracking wastes and quakes. Science News for Students. National Park Service sites in the San Francisco Bay Area reveal a sheared-up, ancient subduction zone landscape developed along the San Andreas Fault. Tsunami waves can hit with the devastating force of a powerful tornado. USGS circular published one month after the earthquake by Arthur Grantz, George Plafker, and Reuben Kachadoorian detailing their scientific investigations of the quake. Oreo cookies are a fun way to demonstrate the three types of plate boundaries and a hotspot. Retriangulation over roughly 25,000 square miles of the deformed region in and around Prince William Sound shows that vertical movements there were accompanied by horizontal distortion, involving systematic shifts of about 64 feet in a relative seaward direction. Map showing ground motion and shaking intensity based on instrumental measurements of shaking along with information about local geology and the earthquakes location and magnitude. The megathrust boundary between the plates results in both the 4,000-km-long Aleutian Trench and in the arc of active volcanoes that lie subparallel to the trench. Massive landslides were triggered by the quake near downtown Anchorage and several residential areas, damaging or destroying about 30 blocks of dwellings and commercial buildings. Virgin Islands National Park in the U. S. Virgin Islands is located on another transform plate boundary, where the Caribbean Plate is sliding past the oceanic part of the North American Plate. Tsunamis trek traced in the sky. Science News for Students. Most of Alaskas mainland felt the magnitude 9.2 earthquake, which wobbled Seattles Space Needle some 1,200 miles away. Coastal trees, here near the Port of Valdez, were snapped off. This is known as subduction. The Australian plate is a continental plate and the Pacific plate is an oceanic plate. seismograph (also known as aseismometer) An instrument that detects and measures tremors (known as seismic waves) as they pass through Earth. The 1964 Alaska Earthquake taught coastal citizens to run for higher ground at the first sign of strong tremors. The map shows the epicenter of the 1964 Alaska Earthquake (red star), caused when the Pacific Plate lurched northward underneath the North American Plate. Where tectonic plates slip horizontally past one another, lithosphere is neither created nor destroyed. lithosphereThe upper layer of Earth, which includes its thin brittle crust and upper mantle. What are the boundary types? From Montague Island, the faults and related belt of maximum uplift may extend southwestward on the Continental Shelf to the vicinity of the Kodiak group of islands. East to west, nearly 960 kilometers (600 miles) of fault had ruptured at once. Sometimes a sub-surface cave becomes too weak to support the ground above it. This Story map combines an interactive map with historic photos of the earthquake. For more earthquake and tsunami data, images, and educational materials, visit NCEIs Natural Hazards website . What are the three types of convergent boundaries? (For example, the 2011 magnitude-9.0 earthquake off the eastern coast of Japan that unleashed a huge tsunami also was a megathrust earthquake.) By definition, intraplate earthquakes do not occur near plate boundaries, but along faults in the normally stable interior of plates. There are three types of plate boundaries, convergent, divergent, and transform. UAF is an AA/EO employer and educational institution and prohibits illegal discrimination against any individual: If you have difficulty accessing the information on this website due to a disability, please contact the web administrator by email at uaf-aec@alaska.edu or by phone at 907-474-7320. At spreading zones, molten rock rises, pushing two plates . Images above modified from Earth: Portrait of a Planet, by S. Marshak, 2001, W. W. Norton & Comp., New York. Hes a geophysicist with the USGS who recently co-authored a study looking back at the 1964 earthquake. Meanwhile, land near the coast just above the fault rose when the fault slipped. The Pacific Plate slides north-northwestward past the North American Plate along the San Andreas Transform Plate Boundary. According to the United States Geological Survey, The 1964 earthquake was giant because of the large area of the fault that slipped during the earthquake and the large amount of slip, or relative motion, between opposite sides of the earthquake fault..

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