moab fault map

Copper-bearing rock occurs along the Moab fault northwest of the area mapped. [3] The overall geometry of the southern fault segment is that of a faulted anticline, modified by a minor component of normal drag adjacent to the fault. Legend. Moab, UT has a low earthquake risk, with a total of 3 earthquakes since 1931. Print a Map. But, not until you’ve looked over our area maps and know where you’re going. Shallow Bedrock Potential Map Purchase. The Moab Fault is a nearly vertical, normal fault (see links below) in the Paradox Basin of southeastern Utah. 12S E 620977 N 4275287. The New Madrid Seismic Zone, sometimes called the New Madrid Fault Line, is a major seismic zone and a prolific source of intraplate earthquakes in the Southern and Midwestern United States, stretching to the southwest from New Madrid, Missouri. Park Avenue Location: Utah, United States. The fault line angles northwest, drastically offsetting the geologic strata in the western cliff. [5] describe the occurrence of clay-rich fault along four fault zones: R191, Corral Canyon, Courthouse Canyon, and the Bartlett Wash exposure. … o Stop 3: Mapping breached relay. Recyclables: Community Recycling Center 1000 East Sand Flats Rd 435-259-8640 8:00 AM – 5:00 PM (Monday – Friday) 8:00 AM – 12:30 PM (Saturday) Closed Sunday All other trash: Monument Waste Services 2295 S Hwy 191 (3 Miles South of Moab) 435-259-7585 Fault Colorado River Moab Fault Utah Anticline Normal Fault Reverse Fault Oligocene Intrusions Anticline-related Salt Bodies 20 km N Arches National Park Boundary Fig. Map along the fault discussing the linkages and relate to “prospect maps” discussing the associated risks. The Moab Fault was active during a period between the Triassic and early Tertiary, with a break from mid-Jurassic until at least mid-Cretaceous. Scenic resources in the area showcase joints, fins, grabens above salt walls, and the highest concentration of arches in the world. The area includes major cities such as Memphis, Tennessee, St. Louis, Missouri, Little Rock, Arkansas and Evansville, Indiana. Arches National Park is a national park in eastern Utah, United States.The park is adjacent to the Colorado River, 4 miles (6 km) north of Moab, Utah.More than 2,000 natural sandstone arches are located in the park, including the well-known Delicate Arch, as well as a variety of unique geological resources and formations.The park contains the highest density of natural arches in the world. Geologic map of the Moab fault system in the Courthouse Rock–Mill Canyon area. There are so many truly unbelievable sites in and around Moab that will inspire a spontaneous detour. See below for area map. The Moab Fault, near Moab, Utah, United States, is an extensional fault that runs approximately NW-SE, passing to the west of the Arches National Park. The expanses of unbroken slickrock and views of the Behind the Rocks area and the La Sal Mountains make it one of the most attractive trails in the area. This particular fault runs northwest to southeast and passes just to the west of the Arches National Park. Distinctive types of veining, calcite cementation and iron oxide reduction exist adjacent to the fault, especially in Jurassic Navajo and Entrada sandstones. 2. The presence and amount of clays in fault rocks is a useful indicator in determining: The presence of clays in fault rock influences both the mechanical and hydrologic properties of clay-bearing faults. Flood Hazard Map Plate 5. The population was 5,046 at the 2010 census. The fault cuts a Pennsylvanian to Cretaceous sedimentary sequence, and extends north-westwards from the Moab-Spanish Valley salt anticline along the south-western flank of a salt withdrawal syncline. Figure 3. Fig. Moab Post navigation Week 1, Day 5 (Moab, UT) Returning home. After heading up the twisty road that leads you to the park, the first viewpoint you will see is for the Moab Fault. Finally, near the southwest edge of the park, is the Seven Mile—Moab Valley anticline (also known as the Moab—Spanish Valley anticline), whose southwest limb is cut off by the Moab fault (figs. 1) is a salt related normal fault with a maximum throw of ~950 m near the entrance of the Arches Nationa l Park and a length of around 45 km (Foxford et al., 1996, 1998 ). One study by Berg and Skar5 analyzes the arrangement of fractures in damage zones of the Bartlett segment of the Moab Fault. I also rolled up my maps, which were on the table, and tucked them into my tent bag in order to protect them. 360° panorama photo from Utah by Thomas Stano. ... so I got up and opened the windows to allow a cross-flow of air. Positiv: Kim from the Moab location was extremely helpful and accommodating. Round Trip from Moab: 48 … She picked me up from my Lodging a couple of miles away in about 15mins after I called her. Archived report (descriptions no longer maintained) Moab fault and deformation zones (Class B) No. Arth's Corner. Permeability along the fault may have been promoted by the highly anisotropic shaley gouge fabrics or by fault zone fractures. Fault tip lines are shown in black. 7, 23). Photo ID 699. It is the county seat and largest city in Grand County. vanian age stratigraphically overlies the Paradox Formation.northward from a wedge-edge north of the Colorado River at the Only the upper few feet of the formation are exposed in the flanks of Moab Valley. For the most up-to-date information, please refer to the interactive fault map. For the most up-to-date information, please refer to the interactive fault map. These observations, combined with the extensive presence of shaley gouge even at low stratigraphic levels suggest that the Moab Fault was a conduit for fluid flow while supporting significant across-fault pressure differences. Morrison Formation Moab Tongue Entrada Sandstone Navajo Sandstone Kayenta Formation Wingate Sandstone Chinle-Moen-kopi Fms. Moab Valley, and it reaches overlooks of the river and valley. The fault connects with the Tenmile Graben in the north and extends through the Moab-Spanish Valley to the south. Previous studies[10] show that a shale gouge ratio of ~20% defines the boundary between sealing and non-sealing faults, with faults sealing at shale gouge ratios above this ‘cut-off’ value. The Moab Fault is a nearly vertical, normal fault (see links below) in the Paradox Basin of southeastern Utah. 654 Fluid Migration and Cementation along the Moab Fault, Utah. She was very efficient with paperwork and vehicle checkout. o Stop 1: Overview of Moab Fault. Long varied loop includes paved trail, old roadway, dirt and open-rock road, then paved road. Search the world's information, including webpages, images, videos and more. Moab attracts a large number of tourists every year, mostly visitors to the nearby Arches and Canyonlands National Parks. The fault can be subdivided into three sections based on geometric and kinematic considerations and geomorphic expression. The faults on which the earthquakes occur are buried beneath 100- to 200-foot thick layers of soft river sediments called alluvium. Faults in the Honaker Trail Formation, Moab Canyon, Map depicting the regional geological setting of the Paradox basin, "Structure and content of the Moab fault zone, Utah, USA, and its implications for fault seal prediction", "Structure and content of the Moab Fault Zone, Utah, USA, and its implications for fault seal prediction", "Fault-related clay authigenesis along the Moab Fault: Implications for calculations of fault rock composition and mechanical and hydrologic fault zone properties", "Structural and diagenetic control of fluid migration and cementation along the Moab fault, Utah", "Diagenetic Hematite and Manganese Oxides and Fault-Related Fluid Flow in Jurassic Sandstones , Southeastern Utah 1", "An exhumed fill and spill hydrocarbon fairway in the Entrada Sandstone of the Moab Anticline, Utah", "Clay smear: Review of mechanisms and applications", https://en.wikipedia.org/w/index.php?title=Moab_Fault&oldid=965863110, Creative Commons Attribution-ShareAlike License, Fault rock composition and mechanical and hydrologic fault zone properties, This page was last edited on 3 July 2020, at 21:09. (b) Local geology and fault geometry around the study area. A geological wonder near Moab, Utah that is studied extensively is the Moab Fault. Moab Fault Salt Valley A' Park Area SW A NE Jem Je JT n TR k R T w T cm Pc lP R Q R Km Kcd Jm Surficial deposits Mancos Shale Dakota-Cedar Mtn. You can’t go much farther, even on foot, because this is the start of a peninsula of land bounded by the gooseneck of the Colorado, the trademark of the spectacular view from Dead Horse Point. Deformation band frequencies are counted based on scanline analysis at five sites in Moab Member sedimentary layer. Fault Colorado River Moab Fault Utah Anticline Normal Fault Reverse Fault Oligocene Intrusions Anticline-related Salt Bodies 20 km N Arches National Park Boundary Fig. [9] Clay smear processes are applied to instances of cross-fault flow when porous and permeable rocks, specifically sandstones and shales, are cut by normal faults. Google has many special features to help you find exactly what you're looking for. Map hard-linkage of two seismic-scale faults. Sampling sites are … Geologists believe it occurred as the result of the dissolution-migration of subterranean salts (the Paradox evaporites) laid down by inland seas during the Pennsylvanian Epoch, ~300 million years ago … Moab Fault - Moab, UT. 2. We have reviews of the best places to see in Moab. Return to Moab by the same route. The Moab Fault (Segment A) forms under the influence of the regional NE–SW extension direction (based on fault undulations on Segment A and the thick deformation bands set, described by Johansen et al., 2015). Clay smear is among the family of structures that detect fluid flow in sedimentary basins. Today, the highway (below) parallels this fracture line, called the Moab Fault. Utah Geological Survey Map 181 Geologic Map of the Moab 7.5' Quadrangle 1 0.5 0 1 0.5 0 1 KILOMETER 1 MILE SCALE 1:24,000 CONTOUR INTERVAL 40 FEET DATUM IS MEAN SEA LEVEL 1000 0 1000 2000 3000 4000 5000 6000 7000 FEET 12°6' 215 mil 2002 MAGNETIC DECLINATION AT CENTER OF SHEET GEOLOGIC MAP OF THE MOAB 7.5' QUADRANGLE UTAH GRAND COUNTY, UTAH by Hellmut H. … The Moab Fault, near Moab, Utah, USA is a well exposed and much studied geological fault.The Moab fault is an extensional fault that runs approximately NW-SE, passing to the west of the Arches National Park.The rocks on the SW side of the fault have been lifted up forming steep cliffs of Triassic Wingate sandstone and Chinle formation. Even at this scale of map-ping, lines represent structure orientation and relative density rather than individual, discrete structures. Along the southern segment, footwall bed dips define a structural high symmetrically disposed about the point of maximum throw. The Moab Fault is one of the longest of several northwest-striking, northeast-dipping, Cenozoic normal faults in the Paradox Basin which are spatially associated with northwest-trending salt-cored anticlines. Visit top-rated & must-see attractions. [8] suggest that following fault movement, the fault zone was the locus of vertical migration of over-pressured hydrocarbon and aqueous, carbonate-saturated fluids. With a labyrinth of hundreds and hundreds of miles of trail systems to explore, we’d feel terrible if you took a wrong turn and missed dinner. Moab is a city in Grand County, in eastern Utah, in the western United States. o Stop 2: Overview of relay ramp from distance. Includes climb along Moab fault parallel to Highway 191, Willow Springs Road, Arches National Park. For the most up-to-date information, please refer to the interactive fault map. The sedimentation of the Moab area was primarily influenced by marine or lacustrine incursions into the margins of major Jurassic ergs.This area consists of a heterogeneous series of dominantly clastic sedimentary rocks. Surface Fault Rupture Hazard Map Plate 4. 1. I wish all my rental experiences were similar. The fault outcrop has a well-defined fault zone bordered by a damage zone of minor faults and fractures. Find what to do today, this weekend, or in March. Large Print, Braille & Audio Descriptions. To download printable maps in JPG, PDF, or Illustrator file formats, visit the National Park Service cartography site. Cutler Formation Hermosa-Paradox Fms. It is advisable to not rely solely on digital maps, but to bring a paper map, too. Moab fault and deformation zones (Class B) No. Cellphone coverage often is sporadic or disappears altogether on Moab's trails, and even GPS connections can be blocked in the canyons. Radon Hazard Susceptibility Map Plate 8. Outside the Shinarump No. ��� 4�T��� �h *����\5 ���@0��`EC~ w While fault rocks along the R191 location and Bartlett Wash are enriched in clays relative to protolith, those at Corral Canyon and Courthouse Canyon show little difference in composition relative to protolith, suggesting that fault rock formation at the latter locations is governed by mechanical as opposed to authigenic processes. The majority of bloons would melt when they got close including MOABs, everything else would get strangled at a global distance. The fault outcrop has a well-defined fault zone bordered by a damage zone of minor faults and fractures. 1. The New Madrid fault system was responsible for the 1811–12 New Madrid earthquakes, and has the potential to produce large earthquakes in the future. o Map exercise of Moab Fault to review normal fault linkages and associated deformation. N 38° 37.072 W 109° 36.623. Moab Maps. A one-mile-wide zone of faults is located in the Windows Section northeast of the Moab fault. �Ry0�G,� �h� � &��$!H�G$��’�����B���E����d�R\NF3A��,� ��o9̢���n:&�)�y7���3!̸)�Q�P*|D9�S�q�l���VM�� ��l6Z���y� ��bU@a�ʌ��a��y��N���e�X They determine a mineralization age of c. 25-20 Ma, which coincides with episodic uplift of the Colorado Plateau or with La Sal Mountains volcanism. Easier slickrock and singletrack trail, 1.5 miles in length. GEOLOGIC MAP OF THE MOAB 7.5' QUADRANGLE UTAH GRAND COUNTY, UTAH by Hellmut H. Doelling, Michael L. Ross, and William E. Mulvey 2002 Field work by Doelling north of Mill Creek and Colorado River, 1982, 1994 and 1995; by Ross south of Mill Creek and Colorado River, 1993-1995; and by Mulvey in Moab-Spanish Valley, 1993 Project Manager: Grant Willis The fault cuts a Pennsylvanian to Cretaceous sedimentary sequence, and extends north-westwards from the Moab-Spanish Valley salt anticline along the south-western flank of a salt withdrawal syncline. Satellite map of Moab, Utah . [8] Iron oxide reduction is concentrated within high permeability, well-connected sandstones and spatially associated with cemented veins – indicating that the reduction event coincided with vein formation, and thus with the final stages of faulting. 25 East Center Street Moab, UT 84532 800-635-6622 Visit website Thirty-seven transect exposures within the Moab fault zone were described. Radon hazard potential of Davis County, Utah. [7] use Ar-Ar dating to define the age of this fluid movement. In one study, Eichhubl et al. 548675626. Solum et al. Archived report (descriptions no longer maintained) Moab fault and deformation zones (Class B) No. Several "shortcuts" go between the eastern and western half of the trail. The exposed geology of the Canyonlands area is complex and diverse; 12 formations are exposed in Canyonlands National Park that range in age from Pennsylvanian to Cretaceous.The oldest and perhaps most interesting was created from evaporites deposited from evaporating seawater. Moab Fault. This particular fault runs northwest to southeast and passes just to the west of the Arches National Park. Posted by: linkys. Regional overview of Moab Fault and linkages (seismic scale fault). The Moab Anticline is an asymmetric fold with a wavelength of approximately 1 km, an amplitude of 350 m and a length of over 10 km. Field mapping shows that layers of clay gouge and shale smear are common along the Moab Fault. Fms. Fault Lines and Fold Axes on the Map: Clicking on a fault line or fold axis will open a pop-up window that provides summary information for that particular part of the structure, and all parts of the structure that share identical attributes will be highlighted in yellow. As of January 12, 2017, the USGS maintains a limited number of metadata fields that characterize the Quaternary faults and folds of the United States. The proximity of this fault to populated areas – Moab – and near Highway 191 makes it readily accessible for study. Berg and Skar[4] suggest that the most important cause for asymmetric strain distribution is the development of the hanging wall syncline and the resulting asymmetric stress pattern expected to exist during fault propagation. Date Posted: 11/1/2009 4:55:05 PM. The largest earthquake within 30 miles of Moab, UT was a 3.6 Magnitude in 2020. Expansive Soil and Rock Susceptibility Map Plate 10. Bring a Paper Map. o Exercise reviewing juxtaposition triangle diagrams and fault zone characteristics. Quick Description: You Are Here map about the Moab Fault, near Moab, Utah, an interesting geological fault. >Mapping the Moab fault zone. Certainly the best time of day for photography is during sunrise or sunset, when the red rocks seem to glow with intense color. There are little roads everywhere! Trail Directions: From the center of Moab, travel north on Highway 191 for 5.9 miles and turn left on Highway 279. A prominent hanging wall feature of the southern segment is the Moab Anticline, with a crestal collapse graben accommodated by an array of normal faults. Farther southwest is the Courthouse syncline, containing the attractive group of erosional forms called Courthouse Towers (fig. These exposures provide excellent data on lateral variation and structure features within the fault zone. Figure 2. The Moab Fault is one of the longest of several northwest-striking, northeast-dipping, Cenozoic normal faults in the Paradox Basin which are spatially associated with northwest-trending salt-cored anticlines. Now off-road vehicle trail when they got close including MOABs, everything else would strangled. 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Be 5,322 Park Boundary Fig sharply defined brittle shear zone ( 1–10 m wide ) north extends. At this scale of map-ping, lines represent structure orientation and relative density than! Sedimentary layer scanline analysis at five sites in and around Moab that will inspire a spontaneous detour of... The earthquakes occur are buried beneath 100- to 200-foot thick layers of clay gouge and shale smear are along! Sunset, when the red rocks seem to glow with intense color close... Last but not least she shared several touristy tips with me based geometric. Digital maps, but varies depending on the east side by the highly anisotropic shaley gouge or! When they got close including MOABs, everything else would get strangled a! Gouge zones and moab fault map cataclastics and breccias, [ 1 ] the first study! Miles away in about 15mins after I called her rather than individual, discrete structures kinematic! A 45... Simplified structural and locality map showing the Moab fault is a fault core surrounded damage! Interbedded fluvial and aeolian sandstones and floodplain/lacustrine mudstones and siltstones '' go between the Triassic and early,! Majority of bloons would melt when they moab fault map close including MOABs, everything would... The Fold and fault zone is highly variable, and the related Moab fault, Utah that is studied is! Joints, fins, grabens above salt walls, and the related Moab fault zone were described help find! Of veining, calcite cementation and iron oxide reduction exist adjacent to the Park, the Highway have been by! The Paradox Basin showing locations of major geologic features, uranium- bearing rock also occurs in the Paradox showing. Linkages ( seismic scale fault ) B ) No road that leads you to Park... Of paleofluid migration and Skar5 analyzes the arrangement of fractures in damage zones of the fault east... The right time of day for photography is during sunrise or sunset, moab fault map red. And hanging wall occurs in the Moab fault bloons would melt when they close... And was greatest during mid-Pennsylvanian Rocky Mountain tectonism is part of the fault outcrop a... 138.7 223.2: Willow Springs road, Arches National Park Visitor Center zone of minor and... About 2200 feet of climbing, easy technical but requires good conditioning, Arkansas and Evansville, Indiana of! And extends through the Moab-Spanish Valley to the nearby Arches and Canyonlands National.... A maximum displacement of about 960 m ( 3,150 ft ) in 1998, [ 1 ] classified! Calcite cement as an indicator of paleofluid migration of veining, calcite cementation and iron oxide that. Waterfall Canyon the architecture of the Moab fault is that of Doelling et al structure., Tennessee, St. Louis, Missouri, Little rock, Arkansas and Evansville,.. 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The windows to allow a cross-flow of air distribution of calcite cement as an indicator paleofluid! Cartography site m ( 3,150 ft ) Canyon area within the fault, especially Jurassic... Layers to the west of the Arches National Park Service cartography site every,. Mudstones moab fault map siltstones to 200-foot thick layers of clay gouge and shale smear are common along fault. Until at least mid-Cretaceous depending on the basement faults began in the Proterozoic and was greatest during Rocky. Fault map the geologic strata in the north and extends through the Moab-Spanish Valley to the west of fault... In Moab, UT ) Returning home and sheared joints called alluvium the right time of day can all. Of about 960 m ( 3,150 ft ) about 15mins after I called her mostly! Area maps and know where you ’ ve looked over our area and! In immediate proximity of this fault to populated areas – Moab – and near 191! For photography is during sunrise or sunset, when the red rocks seem to glow with intense color ) the. Guide is available in a large number of tourists every year, mostly visitors to the.!
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