The November 3, 2002, M w 7.9 Denali Fault earthquake produced about 340 km of surface rupture along the Susitna Glacier Thrust Fault and the right-lateral, strike-slip Denali and Totschunda Faults. Major movements on the Hines Creek fault ceased by the Late Cretaceous, but local dip-slip movements continued into the Cenozoic. … The Denali fault line work and all points are based on Reed, B.L. Copyright © 2020 Elsevier B.V. or its licensors or contributors. The map offers zoom and scroll options, and multiple base map layers. By clicking “I agree” below, you consent to the use by us and our third-party partners of cookies and data gathered from your use of our platforms. The Denali fault system and the tectonic development of Southern Alaska. This content is currently not available in your region. An online map of United States Quaternary faults (faults that have been active in the last 1.6 million years) is available via the Quaternary Fault and Fold Database. Thus the fault system may mark a reactivated suture zone between continental rocks to the north and a late Paleozoic island arc to the south, as suggested by Richter and Jones (1973). Geologic line work on this map other than specified faults … Other colored lines indicate known regional and teleseismic earthquake times. Please enable cookies on your web browser in order to continue. On Sunday, November 3, 2002, at 3:12 p.m. (MST), a large (magnitude 7.9) earthquake occurred on the Denali fault … This publication updates previous fault maps of Oregon as a contribution to the larger U.S. Geological Survey effort to produce digital maps of active faults in the Pacific Northwest region. Present address: Union Oil Company of California Research Center, Brea, Calif. 92621 (U.S.A.). This is along the Denali Fault, a strike-slip fault line. During each, the axis of maximum compressive strain was subhorizontal and about north—south. The few remaining Native Americans in the area spoke of the earth shaking and ocean rising to consume the land. You’d be mistaken. ScienceDirect ® is a registered trademark of Elsevier B.V. ScienceDirect ® is a registered trademark of Elsevier B.V. Image courtesy of the USGS A trace of the Denali Fault runs … Over the centuries, earthquakes have hitched one part of the … Many tribes even left the region permanently. Digital photogrammetric methods were primarily used to create a 1:500-scale, three-dimensional surface rupture map… The Denali Fault cuts across Alaska in a line that on satellite photos looks like a canal dug through the Alaska Range. We use cookies and other technologies to customize your experience, perform analytics and deliver personalized advertising on our sites, apps and newsletters and across the Internet based on your interests. The Denali Fault and Earthquakes. Note the striking contrast in rock type and age on opposite sides of the fault. Minor Potential Faults: 2 feet lateral, 2 feet vertical. Figure 2 (bottom): Geologic map of part of the 2002 Denali Fault rupture near the Trans-Alaska Pipeline crossing in the Alaska Range. Donnelly Dome Fault: 3 feet lateral, 10 feet vertical. 40Ar/39Ar data from the Richardson mining district, Big … We map the 385-kilometer (km) long surface trace of the right-lateral, strike-slip Denali Fault between the Totschunda-Denali Fault intersection in Alaska, United States and the village of Haines Junction, … This model therefore supports the strike-slip fault consensus, while being able to visually explain events such as the Denali … The Castle Mountain fault trends northeasterly and is marked by a low, south-facing escarpment. A fault scarp is visible near Augustana Creek, Alaska. The Denali fault is an active intraplate dextral strike-slip fault. The upper reach­es of the Nenana flow out of the Nenana Glac­i­er and runs south then west into a wide glacial val­ley and the pri­ma­ry access for the upper Class II stretch is from the Denali High­way at mile 20.This is a geo­log­i­cal­ly inter­est­ing area as the riv­er runs into the trench of the Denali Fault Line… AD. By the time Lewis and Clark arrived on the West Coast in 1805, it had been 105 years since the Cascadia Subduction Zone last ruptured, sending a large portion of the Pacific Ocean roaring toward the coast. Note also, that Alaska is not behaving as one rigid plate. The main shock occurred about 80 km (50 miles) east of the Denali … Along the Denali Fault, lateral and vertical offset movement is taking place. Strong contrasts between juxtaposed lower Paleozoic rocks appear to require large dextral strike-slip or a combination of dipslip and strike-slip displacements along this fault. Post-Late Cretaceous dextral offset on this fault is probably at least 30 km and possibly as great as 400 km. Anchorage is precariously perched 100 miles south of the Denali Fault. The two strands of the Denali fault divide the central Alaska Range into northern, central, and southern terranes. We digitized fault and fold traces from original paper maps… While there’s a good chance this is the fault that ruptured, it’s too early to tell for sure until more data comes in. Notice it is not a Fitch fault as it does not follow the magmatic arc complex. With the exception of the Denali fault… In addition, both of the Denali Fault earthquakes occurred at a depth in the Earth’s crust of 5 … By clicking “I agree” below, you consent to the use by us and our third-party partners of cookies and data gathered from your use of our platforms. Northern California Area Faults Earthquake Fault Map Resources USGS Past Significant Earthquakes Archive Rodgers Creek, Healdsburg and Maacama Faults List of the strongest California earthquakes Fault Attributes Key NAME is an 80-character field for the name of the fault (including section name, i.e., Denali fault… The November 2002 earthquake had a magnitude of 7.9 and caused a surface rupture 325 km (~200 miles) long, mostly on the central Denali Fault (see red line on map … The Hines Creek fault … The fault runs through the mountains west to east and then curves south … We use cookies to help provide and enhance our service and tailor content and ads. Image courtesy of the USGS. However, it wasn’t until the discovery of the Cascadia Fault in the 1960s th… Map Of Carlton oregon pictures in here are posted and uploaded by secretmuseum.net for your map of carlton oregon images collection. Oregon Cascadia Earthquake Fault Map Resources USGS Significant Earthquakes Activity Tsunamis Evacuation Brochures and Apps List of earthquakes and tsunamis in the United States 1700 Cascadia earthquake Fault Attributes Key NAME is an 80-character field for the name of the fault (including section name, i.e., Denali fault… Active faults in the Alaska Range and adjacent areas include those of the Denali fault system, including the Totschunda fault and the McGinnis Glacier fault; inactive faults include the Hines Creek fault. The Denali fault system forms an arc, convex to the north, across southern Alaska. We rely on readers like you to uphold a free press. Figure 3: The figure to the left represents two dimensional cross sections of the Denali Fault System (Jadamec, Margarete A. et al 2013). • Little River fault Puget Sound Earthquake Fault Map Resources USGS 2014 Significant Earthquakes Archive The very strong 1700 Cascadia earthquake List of the strongest world earthquakes, Cascadia was one of them Fault Attributes Key NAME is an 80-character field for the name of the fault (including section name, i.e., Denali fault… In 2002, the M 7.9 earthquake ruptured a portion of the Denali fault east of the park to produce a horizontal offset of up to 8.8 m (29 feet). Earthquakes have been recorded in this … The map shows the seismic energy migrated back to the source, where it constructively interferes, imaging the source in space at the source time. The Pass Creek fault line work and all points are based on Reed and Nelson, 1980. There is an interactive map application … The location map of the study site of Denali Fault line in southwest Yukon. On Nov. 3, 2002, the pipeline withstood a magnitude 7.9 earthquake that was centered along the Denali Fault. Source map data was in a wide variety of projections common in Alaska. Patterns of early Tertiary folding and reverse faulting indicate that the McKinley fault was active at that time and suggest that this fault developed shortly after strike-slip activity ceased on the Hines Creek fault. The Hines Creek fault may preserve a record of the early history of the fault system. Thus, source data was imported or digitized in its native projection and reprojected to the database projection (for instance, NAD 27 UTM to GCS WGS 1984). During the Paleozoic—Mesozoic there is evidence for at least two episodes of compressive deformation in the northern terrane, four in the central terrane, and two in the southern. The McKinley fault is an active dextral strike-slip fault with a mean Holocene displacement rate of 1–2 cm/y. The purpose of this map is to show the location of and evidence for recent movement on active fault traces within the Hayward Fault Zone, California. This map also shows the regulatory tsunami inundation line (Oregon Revised Statutes 455.446 and 455.447), commonly known as the Senate Bill 379 line. In the central Alaska Range, the system consists of a northern Hines Creek strand and a southern McKinley strand, up to 30 km apart. Maximum Wet/Dry Zone is shown on this map. One example of a major fault is the Denali fault, which cuts across the state in the Alaska Range (labelled on map on reverse). This is a USGS produced shake map… Click individual fault and fold traces to view basic fault parameters: name, age, slip rate, slip sense, dip direction, mapping certainty, and mapped scale. In the central Alaska Range, the system consists of a northern Hines Creek strand and a southern McKinley strand, up to 30 km apart. A Magnitude 7.5 earthquake has occurred about 57 miles southeast of Sand Point, Alaska. This pattern suggests a Paleozoic and Mesozoic setting dominated by plate convergence, despite the possible large pre-Late Cretaceous lateral movement on the Hines Creek fault. See our Privacy Policy and Third Party Partners to learn more about the use of data and your rights. A trace of the Denali Fault runs up the north side of the Canwell Glacier. By continuing you agree to the use of cookies. Bedrock geologic map of the eastern Denali Highway area, Mount Hayes, Healy, and Talkeetna Mountains quadrangles, Alaska - RI 2020-7 New release! Copyright © 1978 Published by Elsevier B.V. https://doi.org/10.1016/0040-1951(78)90033-1. The Denali fault system forms an arc, convex to the north, across southern Alaska. Credit: G. Plafker. This National Park includes part of a massive mountain range more than 600 miles long. Denali Fault. Projection showing Utah in relation to the rupture direction (solid line; dashed line ±10°) of the Denali fault earthquake (indicated by star). The surface offset at this location was approximately 16 feet (almost 5 meters). The ground along the fault … With the fault in place, velocity vectors show a likelihood of slip in the direction along the fault line. Tips/Special Features: The Denali Fault provides a natural travel corridor through the high peaks and valleys of the unit from Foggy Pass in the eastern side to Easy Pass at the western end.Large and … You also agree to our Terms of Service. See our, Read a limited number of articles each month, You consent to the use of cookies and tracking by us and third parties to provide you with personalized ads, Unlimited access to washingtonpost.com on any device, Unlimited access to all Washington Post apps, No on-site advertising or third-party ad tracking. ... Mw 7.8 and Denali fault … The new European data protection law requires us to inform you of the following before you use our website: We use cookies and other technologies to customize your experience, perform analytics and deliver personalized advertising on our sites, apps and newsletters and across the Internet based on your interests. With only a handful of known active faults across northeast Alaska, you might not expect much in the way of earthquake activity. The images that existed in Map Of Carlton oregon are … The location map of the study site. Sites such as this one provided the data for designing the pipeline fault crossing. and Nelson, S.W., 1980. ... New findings of earthquake recurrence on the Denali Fault line in southwest Yukon are helping researchers get closer to pinpointing when the next big one … and the fault database. The Denali Fault is located in Alaska's Denali National Park and to the east. The Cenozoic pattern of faulting and folding appears compatible with a plate tectonic model of (1) rapid northward movement of the Pacific plate relative to Alaska during the early Tertiary; (2) slow northwestward movement of the Pacific plate during the Oligicene and (3) rapid northwestward movement of the Pacific plate from the end of the Oligocene to the present. The new map is derived from the 1992 fault map … Oligocene — middle Miocene tectonic stability and late Miocene—Pliocene uplift of crustal blocks may reflect periods of quiescence and activity, on the McKinley fault. 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