This is along the Denali Fault, a strike-slip fault line. Digital photogrammetric methods were primarily used to create a 1:500-scale, three-dimensional surface rupture map… ScienceDirect ® is a registered trademark of Elsevier B.V. ScienceDirect ® is a registered trademark of Elsevier B.V. The McKinley fault is an active dextral strike-slip fault with a mean Holocene displacement rate of 1–2 cm/y. and Nelson, S.W., 1980. Figure 3: The figure to the left represents two dimensional cross sections of the Denali Fault System (Jadamec, Margarete A. et al 2013). 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 … 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). Donnelly Dome Fault: 3 feet lateral, 10 feet vertical. and the fault database. The Denali fault system forms an arc, convex to the north, across southern Alaska. 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. During each, the axis of maximum compressive strain was subhorizontal and about north—south. Many tribes even left the region permanently. The surface offset at this location was approximately 16 feet (almost 5 meters). 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. Post-Late Cretaceous dextral offset on this fault is probably at least 30 km and possibly as great as 400 km. Copyright © 1978 Published by Elsevier B.V. https://doi.org/10.1016/0040-1951(78)90033-1. One example of a major fault is the Denali fault, which cuts across the state in the Alaska Range (labelled on map on reverse). Credit: G. Plafker. Source map data was in a wide variety of projections common in Alaska. The location map of the study site of Denali Fault line in southwest Yukon. Minor Potential Faults: 2 feet lateral, 2 feet vertical. This content is currently not available in your region. With the fault in place, velocity vectors show a likelihood of slip in the direction along the fault 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. 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. Click individual fault and fold traces to view basic fault parameters: name, age, slip rate, slip sense, dip direction, mapping certainty, and mapped scale. The mapped traces represent the integration of the following three different types of data: (1) geomorphic expression, (2) creep (aseismic fault … AD. ... 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 … • 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… 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, … The ground along the fault … Geologic line work on this map other than specified faults … This National Park includes part of a massive mountain range more than 600 miles long. Note also, that Alaska is not behaving as one rigid plate. 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. The Denali fault line work and all points are based on Reed, B.L. The Denali Fault is located in Alaska's Denali National Park and to the east. The two strands of the Denali fault divide the central Alaska Range into northern, central, and southern terranes. 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). Image courtesy of the USGS A trace of the Denali Fault runs … 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. 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 Hines Creek fault … By continuing you agree to the use of cookies. However, it wasn’t until the discovery of the Cascadia Fault in the 1960s th… You also agree to our Terms of Service. 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). 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. The Denali Fault and Earthquakes. Along the Denali Fault, lateral and vertical offset movement is taking place. The Denali Fault cuts across Alaska in a line that on satellite photos looks like a canal dug through the Alaska Range. Note the striking contrast in rock type and age on opposite sides of the fault. The Denali fault system forms an arc, convex to the north, across southern Alaska. Projection showing Utah in relation to the rupture direction (solid line; dashed line ±10°) of the Denali fault earthquake (indicated by star). See our Privacy Policy and Third Party Partners to learn more about the use of data and your rights. The location map of the study site. With the exception of the Denali fault… Over the centuries, earthquakes have hitched one part of the … 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. 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… 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 Denali fault system and the tectonic development of Southern Alaska. 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 Pass Creek fault line work and all points are based on Reed and Nelson, 1980. We rely on readers like you to uphold a free press. On Nov. 3, 2002, the pipeline withstood a magnitude 7.9 earthquake that was centered along the Denali Fault. A trace of the Denali Fault runs up the north side of the Canwell Glacier. Maximum Wet/Dry Zone is shown on this map. A Magnitude 7.5 earthquake has occurred about 57 miles southeast of Sand Point, Alaska. 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. Denali Fault. Map Of Carlton oregon pictures in here are posted and uploaded by secretmuseum.net for your map of carlton oregon images collection. 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. 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. 40Ar/39Ar data from the Richardson mining district, Big … 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 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… Anchorage is precariously perched 100 miles south of the Denali Fault. Copyright © 2020 Elsevier B.V. or its licensors or contributors. ... Mw 7.8 and Denali fault … Notice it is not a Fitch fault as it does not follow the magmatic arc complex. Image courtesy of the USGS. In addition, both of the Denali Fault earthquakes occurred at a depth in the Earth’s crust of 5 … The fault is a 1,000-mile line through mountains you can see on a zoomed-out map of eastern Alaska and western Canada. The images that existed in Map Of Carlton oregon are … The fault runs through the mountains west to east and then curves south … Earthquakes have been recorded in this … 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 … 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. Present address: Union Oil Company of California Research Center, Brea, Calif. 92621 (U.S.A.). With only a handful of known active faults across northeast Alaska, you might not expect much in the way of earthquake activity. 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. This model therefore supports the strike-slip fault consensus, while being able to visually explain events such as the Denali … Oligocene — middle Miocene tectonic stability and late Miocene—Pliocene uplift of crustal blocks may reflect periods of quiescence and activity, on the McKinley fault. You’d be mistaken. The Hines Creek fault may preserve a record of the early history of the fault system. Figure 2 (bottom): Geologic map of part of the 2002 Denali Fault rupture near the Trans-Alaska Pipeline crossing in the Alaska Range. The Denali fault is an active intraplate dextral strike-slip fault. Major movements on the Hines Creek fault ceased by the Late Cretaceous, but local dip-slip movements continued into the Cenozoic. The Castle Mountain fault trends northeasterly and is marked by a low, south-facing escarpment. On Sunday, November 3, 2002, at 3:12 p.m. (MST), a large (magnitude 7.9) earthquake occurred on the Denali fault … Sites such as this one provided the data for designing the pipeline fault crossing. Bedrock geologic map of the eastern Denali Highway area, Mount Hayes, Healy, and Talkeetna Mountains quadrangles, Alaska - RI 2020-7 New release! 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. The map offers zoom and scroll options, and multiple base map layers. Please enable cookies on your web browser in order to continue. This is a USGS produced shake map… A fault scarp is visible near Augustana Creek, Alaska. 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. We use cookies to help provide and enhance our service and tailor content and ads. There is an interactive map application … We digitized fault and fold traces from original paper maps… The new map is derived from the 1992 fault map … The main shock occurred about 80 km (50 miles) east of the Denali … … In the central Alaska Range, the system consists of a northern Hines Creek strand and a southern McKinley strand, up to 30 km apart. The few remaining Native Americans in the area spoke of the earth shaking and ocean rising to consume the land. Other colored lines indicate known regional and teleseismic earthquake times. 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. 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