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A monocline is a "step-up" in the rock layers. Large-scale geologic structures (e.g., the Waterpocket Fold monocline and San Rafael Swell upwarp) yield broad dip planes and extensive joint systems within sedimentary strata and control groundwater movemenl at local and regional scales (Healh . But the hallmark of this park is the nearly 100-mile-long Waterpocket Fold, which park geologists are quick to note "is a classic monocline: a regional fold with one very steep side in an area of otherwise nearly horizontal layers." Take some time to study this hogback and you'll be duly impressed by the geologic forces at work here. This rock formtion is estimated to have first been created 50-70 million years ago, when some of . Found inside – Page 37The park contains most of the famed Waterpocket Fold , a gigantic monocline extending southward from Thousand Lake Mountain to the Colorado River . The oldest layers of the canyon on this view are at left (east). Utah's Capitol Reef National Park, near Torrey, exists to protect the area around a 65 million year old warp in the earth's crust, called the Waterpocket Fold. To me, standing at the base, appeared to be incoming waves. Even more noteworthy, it is the largest exposed monocline in the United States. Found inside – Page 4444 ) , but overall the Waterpocket Fold maintains its N20 ° W trend . In contrast to the East Kaibab monocline that formed obliquely to the direction of ... Congress made it a National Park in 1970. [7] The monocline is composed of several subparallel, right-stepping fold segments striking 330 -340 and dip-ping toward the east (Figure 1) [Heyman, 1983; Stearns, A nearly 100-mile long warp in the Earth's crust, the Waterpocket Fold is a classic monocline: a regional fold with one very steep side in an area of otherwise nearly horizontal layers. 2000). The Gypsum Sinkhole formed when a gypsum deposit dissolved. Save Capitol Reef National Park. Long after the sedimentary rocks were deposited, the entire region was uplifted thousands of vertical feet, due to large-scale plate tectonic forces. Capitol Reef is a place to enjoy the scenic majesty formed by geologic processes, and also to appreciate the interrelationships between the Earth and all life found in the varied environments within the park, from the forested slopes of Thousand Lake Mountain, to the green oasis of Fruita, to the barren Bentonite Hills. These monoclines often are referred to as reefs because, like reefs at the edges of oceans, they are long barriers with few breaks. Even more noteworthy, it is the largest exposed monocline in the United States. An in-depth discussion of Capitol Reef geology is at Wiki Geology menu selections. The Waterpocket Fold is 65 million years old and is the largest exposed monocline in North America. 65 . Monocline. In The Capitol Reef, the west part of the waterpocket fold is 7,000 feet higher than the east side. The Waterpocket Fold monocline stretches for almost 161 km (100 mi), from the Colorado River south of the Henry Mountains, along the east side of the Circle Cliffs, northward to . Phones are answered when staff is available. The overlying sedimentary layers were draped above the fault and formed a monocline. The Fruita Campground has 71 sites. The Waterpocket Fold defines Capitol Reef National Park. "Waterpockets" are small depressions that form in many of the sandstone layers as they are eroded by water, and are common throughout the fold at Capitol Reef. The Waterpocket Fold is one of the longest continuously exposed Monoclines in the world and is the centerpiece geologic structure of Capitol Reef . A nearly 100-mile long warp in the Earth's crust, the Waterpocket Fold is a classic monocline: a regional fold with one very steep side in an area of otherwise nearly horizontal layers. The monocline extends from Thousand Lake Mountain in the north to Lake Powell in the south. Eerie to think… Because the Waterpocket Fold has tilted this geologic layer cake down to the east, the older rocks are found in the western part of the park, and the younger rocks are found near the east boundary. A monocline is a "step-up" in the rock layers. Located in south-central Utah in the heart of red rock country, Capitol Reef National Park is a hidden treasure filled with cliffs, canyons, domes and bridges in the Waterpocket Fold, a geologic monocline (a wrinkle on the earth) extending almost 100 miles. Located in south-central Utah in the heart of red rock country, Capitol Reef National Park is a hidden treasure filled with cliffs, canyons, domes, and bridges in the Waterpocket Fold, a geologic monocline (a wrinkle on the earth) extending almost 100 miles. The majority of guests here drive the main road through the north-central section, where the visitor center is located, but there's lots to see in Cathedral Valley in the far north and Strike Valley in . Glass Mountain is an exposed plug of gypsum. Located in south-central Utah in the heart of red rock country, Capitol Reef National Park is a hidden treasure filled with cliffs, canyons, domes, and bridges in the Waterpocket Fold, a geologic monocline (a wrinkle on the earth) extending almost 100 miles. The visitor center is open daily from 8am to 4:30pm . A nearly 100-mile long warp in the Earth's crust, the Waterpocket Fold is a classic monocline, a "step-up" in the rock layers. Check specific forecasts, which include the flash flood potential rating and heat risk: The Waterpocket Fold in Capitol Reef National Park is a classical monocline that is almost 100-miles long (160 km). If no one answers, please leave a message, your call will be returned. Discover the Waterpocket Fold, a geologic wrinkle on earth! The oldest layers of the canyon on this view are at left . Detailed field investigation of the Waterpocket monocline within the Utah portion of the Colorado Plateau reveals a strong correlation between abrupt changes in the trend of the monoclinal fold axis and enhanced fault development within the Navajo Sandstone. Found inside – Page 62The geology of the Waterpocket Fold created conditions which allowed unique plant ... capitol Reefnational park waterpocket Fold: too-mile-long Monocline ... What is eroded from the park ends up being deposited elsewhere. Its technical name is a monocline, which, citing the Oxford Dictionary is a 'bend in rock strata that is otherwise uniformly dipping or horizontal.' Waterpocket Fold, the area, is the least visited section of the national park. The Waterpocket Fold is the major geologic feature that defines Capitol Reef National Park. Flanked on all sides by steep cliffs and the Henry Mountains, it is one of the most striking panoramic points in the area. The flowing and dissolving of gypsum, a soluble mineral from the underlying Carmel Formation, created Glass Mountain and the Gypsum Sinkhole. The Waterpocket Fold, referred to as a monocline, has a singular limb. These features formed during volcanic activity three to six million years ago. Found inside – Page 22The rocks are flat lying to gently folded except at the Waterpocket Fold , Escalante Monocline , and East Kaibab Monocline where there are steep flexures . Discover the Waterpocket Fold, a geologic wrinkle on earth! Found inside – Page 64In addition , the unit contains a portion of the Waterpocket Fold , the ... is a spectacular example of the 100mile - long Waterpocket Fold monocline . The monocline, or one-sided uplift of the Earth's crust, is a premier example of the bending and folding of rock layers. It owes its name to deep potholes found in the canyons here that can hold water for months following significant rain/snow events. This wrinkle in the earth's surface extends for nearly 100 miles, creating a dramatic landscape of rugged cliffs and canyons, striking natural bridges and arches, and distinct formations in the heart of red rock country. The Waterpocket Fold is notable for its great length of multiple layers of exposed and carved colorful sedimentary rock. Deep erosion has carved Cathedral Valley's free-standing monoliths, or temples, out of the soft reddish-orange Entrada Sandstone, which was originally deposited as sandy mud on a tidal flat. Found inside – Page 6The Kaiparowits coal - basin area has not only the large - scale deformational features such as the monoclines of the Waterpocket Fold and The Cockscomb ... The name "Waterpocket Fold" reflects this ongoing erosion of the rock layers. That sounds pretty old, but the rocks exposed at the fold are betweeen 80 and 270 million years old. If the monocline had experienced no erosion, layers in the area fold follow the trend of the dashed red and green line. Navajo Dome, one of the more notable features within Capitol Reef National Park. Discover all 19 of Capitol Reef's rock layers in the stratigraphy column (PDF). It formed between 50 and 70 million years ago when a major mountain building event in western North America, the Laramide Orogeny, reactivated an ancient . Located in south-central Utah in the heart of red rock country, Capitol Reef National Park is a treasure filled with cliffs, canyons, domes and bridges in the Waterpocket Fold, a geologic monocline (a wrinkle on the earth) extending almost 100 miles. Found inside12, enjoy views of the 100-mile-long Waterpocket Fold monocline within Capitol Reef National Park to the east and south. From the elevated vantage points of ... Also, check out nearby points of interest. Photo taken on May 3, 2009.Photo Details: Camera Maker: NIKON; Camera Model: COOLPIX P6000; Focal Length: 6mm (35mm equivalent: 28mm); Aperture: f/7.2; Exposure Time: 0.0025 s (1/400); ISO equiv: 64; Software: Adobe Photoshop Lightroom 4.4 (Windows). Below are 5 of our favorite attractions. Cliffs, monoliths, slot canyons, natural . Found inside – Page 22The rocks are flat lying to gently folded except at the Waterpocket Fold , Escalante Monocline , and East Kaibab Monocline where there are steep flexures . Piles of rounded lava boulders lie atop the westernmost layers. Both Salt Wash and Brushy Basin Members of the Morrison Formation are favorable. The Salt Wash Member is favorable because it is a known producer. The Brushy Basin Member is favorable as a low-grade resource. Faults within the bends of the fold axis range in scale from individual deformation bands to large, complex fault zones visible on 1 . A nearly 100-mile long warp in the Earth's crust, the Waterpocket Fold is a classic monocline, a "step-up" in the rock layers. The Waterpocket Fold monocline is a buckle in the earth's surface, nearly 100 miles long, running north- south in the south-central Utah desert from Thousand Lake Mountain near Torrey, Utah, to Lake Powell in Glen Canyon National Recreation Area. The Upper South Desert Overlook affords views of the upper reaches of the South Desert—a long, narrow valley that runs parallel to the Waterpocket Fold monocline. Each side of the ridge is called a limb. Faults within the bends of the fold axis range in scale from individual deformation bands to large, complex fault zones visible on 1 . Found inside – Page 56Capitol Reef National Park lies along a north - southtrending monocline , called the Water Pocket Fold , about halfway ( in a direct line ) between Bryce ... 5. Flanked on all sides by steep cliffs and the Henry Mountains, it is one of the most striking panoramic points in the area. Hours/Fees . Located in south-central Utah, right in the heart of the region of red rock formations and along the beautiful Utah State Route 24 Scenic Byway, Capitol Reef is the national park home to natural wonders in Waterpocket Fold, a monocline that stretches about 100 miles with intense colors and the most imaginative cliffs, domes, steep peaks . Found inside – Page 18The violence that went during the development of the Waterpocket Fold is best ... THE MONOCLINE SECTION : Thirty miles south of the highway the Waterpocket ... Approximately sixty million years of wind, rain, freeze and thaw have exposed the folded rock layers at Capitol Reef. 2000). Found inside – Page 130The East Kaibab Monocline is almost a hundred miles long . Folds ... The Waterpocket Fold in More - Resistant Capitol Reef is perhaps the Formation Less ... Found inside – Page 79basin from the two upwarps is the sharp Waterpocket Fold monocline . The Henry Mountains structural basin is one of the major structural lows of the ... Found inside – Page 79basin from the two upwarps is the sharp Waterpocket Fold monocline . The Henry Mountains structural basin is one of the major structural lows of the ... Other articles where Waterpocket Fold is discussed: Capitol Reef National Park: Natural history: …the nearly 100-mile- (160-km-) long Waterpocket Fold. This gigantic monocline forms the backbone of Capitol Reef and . Capitol Reef's Waterpocket Fold is the defining geologic feature of this majestic national park. That formation constitutes a monocline, a sharp fold of Earth's crust that was formed when thick layers of horizontal sedimentary rocks (mainly sandstones but also shales, mudstones, and limestones) that had been deposited over a period of . A nearly 100-mile long warp in the Earth's crust, the Waterpocket Fold is a classic monocline: a regional fold with one very steep side in an area of otherwise nearly horizontal layers. Found inside – Page 7The Waterpocket Fold is a monocline on the east flank of the Circle Cliffs and is a prominent , regional ridge ( reef ) ... It is the largest exposed monocline in North America. Found inside – Page 115It is included in the Echo monocline are those on improbable that the Wolf ... and probably very nearly coeval with monocline and the Water Pocket fold ... Softer mudstone layers, like the Chinle Formation, form slopes and low hills. It formed between 50 and 70 million years ago when a major mountain building event in western North America, the Laramide Orogeny, reactivated an ancient buried fault in this region. This layer upon layer sequence of sedimentary rock records nearly 200 million years of geologic history. Discover other national park sites with unique geologic features. Questions may also be sent to care_information@nps.gov. The Waterpocket Fold defines Capitol Reef National Park. The pull of gravity, in the form of rock falls or rock creep, plays a major role in the shaping of the cliff lines. More recent uplift of the entire Colorado Plateau and the resulting erosion has exposed this fold at the surface within the last 15 to 20 million years. The oldest layers of the canyon on this view are at left . The skinny sixty mile long park was originally established as a national monument in 1937, but became a national park in 1971. Found inside – Page 80The Burr Trail crosses , and then follows , the southern extent of the most spectacular monoclinal flexure in North America , the Waterpocket Fold ( NPS and ... The monocline extends from Thousand Lake Mountain in the north to Lake Powell in the south. Scenic Byway 24 cuts through Waterpocket Fold on the Capitol Reef Scenic Byway alongside Fremont River inside the Fremont River Canyon. Waterpocket Fold monocline Easy Fold Thule - Preise & Shop-Angebot . Found inside – Page 294... feature is a large monoclinal , already alluded to as a companion to the Water Pocket fold . ... The throw of the monocline is to the westward . What is an example of a monocline? This wrinkle in the earth's surface is a classic monocline, a fold, that in this case is about 7000 feet higher in the west than the east. Categories: Found insideMonoclines (hogbacks) are sudden tilts or jogs in the plane of ... it refers to drastically tilted ridges, such as the Waterpocket Fold monocline. The monocline, or one-sided uplift of the Earth's crust, is a premier example of the bending and folding of rock layers. Photographed 04/11/2014 at Capitol Reef National Park, Utah. Waterpocket Fold, the geologic feature, is a 100-mile rocky spine extending from Thousand Lake Mountain to Lake Powell. Find great hotel prices for Torrey (Utah) in United States or the surrounding region. Hard sandstone layers, like the red Wingate and the white Navajo Sandstones, form cliffs, which sometimes develop interesting weathering patterns, like tafoni. 435-425-3791 Learn about other geologic features (PDF) in Capitol Reef. A nearly 100-mile long warp in the Earth's crust, the Waterpocket Fold is a classic monocline: a regional fold with one very steep side in an area of otherwise nearly horizontal layers. The Waterpocket Fold defines Capitol Reef National Park. compression acted normal to the Waterpocket monocline trace along 068 azimuth, consistent with the Laramide maximum compression direction. The easiest to access portion of the Waterpocket Fold, found near the Fremont River, is known as Capitol Reef: capitol for the white domes of Navajo Sandstone that resemble capitol building domes, and reef for the rocky cliffs which are a barrier to travel, like an ocean reef. Capitol Reef Map is a resizable pdf map of Capitol Reef National Park from the NPS. Found inside – Page 137The Waterpocket Fold monocline , which constitutes the western boundary of the Henry Mountains structural basin , has an average inclination of 20 to 30° ... It formed 50-70M years ago when a major mountain building event in North America (the Laramide Orogeny ) reactivated an ancient fault . Waterpocket Fold's sliced up sandstone (Kim Phillips) View of the Henry Mountains (Kim Phillips) Slickrock bowl in Capitol Reef (Kim Phillips) Henry Mountains form the backdrop to this route (Kim Phillips) I thought the rope would solve my problem, but as can happen with ropes, it only led me deeper into trouble. Black boulders, found scattered throughout the Fremont River valley and along other drainages, are recent geologic arrivals to Capitol Reef. Capitol Reef National Park was established primarily to preserve geologic features, such as the scenic rock domes and narrow canyons. The rock layers on the west side of the Waterpocket Fold . The park's classic examples of geology include . Located in south-central Utah in the heart of red rock country, Capitol Reef National Park is a hidden treasure filled with cliffs, canyons, domes and bridges in the Waterpocket Fold, a geologic monocline (a wrinkle on the earth) extending almost 100 miles. Kane County, with its 4105 square miles, lies along the south-central margin of Utah and is found in the western part of the Colorado Plateaus physiographic province. Monoclines are folds consisting of two horizontal (or nearly so) limbs connected by a shorter inclined limb. When linked to the adjoining Capitol Reef National Park, which protects the 100 mile monocline of the Waterpocket Fold, you'll find a territory presenting a hiking and photography experience of a lifetime. A guide to the Grand Canyon for rim walkers, day hikers, and serious backpackers, presented from the point of view of geologists. A monocline is a "step-up" in Waterpocket Fold the rock layers. This picture was taken facing southwards from the Strike Valley Overlook, near where the Burr Trail exits west from the valley floor. It formed between 50 and 70 million years ago when a major mountain building event in western North America, the Laramide Orogeny, reactivated an ancient buried . A nearly 100-mile long warp in the Earth's crust, the Waterpocket Fold is a classic monocline: a regional fold with one very steep side in an area of otherwise nearly horizontal layers. If no one answers, please leave a message, your call will be returned. The Waterpocket Fold defines Capitol Reef National Park. A nearly 100-mile long warp in the Earth's crust, the Waterpocket Fold is a classic monocline: a regional fold with one very steep side in an area of otherwise nearly horizontal layers. It is a buckle in the earth's surface, almost 100 miles long, running north-south from Thousand Lake Mountain down to Lake Powell. Some of the cathedrals are capped by thin, hard beds of a greenish gray marine sandstone, the Curtis Formation. What is a monocline fold? The Burr Trail, unpaved inside the park, crosses the rugged fold on dirt switchbacks. Found inside – Page 103The Colorado Kiver crosses the Waterpocket Fold without evident deviation from its ... which are developed in soft beds upturned in a monoclinal fold, ... Located in south-central Utah in the heart of red rock country, Capitol Reef National Park is a hidden treasure filled with cliffs, canyons, domes, and bridges in the Waterpocket Fold, a geologic monocline (a wrinkle on the earth) extending almost 100 miles. Monoclines may be formed in several different ways (see diagram) By differential compaction over an underlying structure, particularly a large fault at the edge of a basin due to the greater compactibility of the basin fill, the . Capital reef National Park. If you are not founding for Rockhounding Near Capitol Reef, simply look out our article below : An excellent example of a Colorado Plateau monocline is the Waterpocket fold in Capitol Reef National Park. The Waterpocket monocline is located in southern Utah, in the Colorado Plateau physiographic province (Fig. Rock layers in Cathedral Valley have a gentle inclination of three to five degrees to the east and appear nearly horizontal. Questions may also be sent to care_information@nps.gov. Found inside – Page 471Here erosion has cut deeply into the steeply tilted rocks along the Waterpocket Fold ( monoclinal fold ) . Like the edges of books leaning on a bookshelf ... The Waterpocket Fold defines Capitol Reef National Park. Found inside – Page 221... Waterpocket Fold—a 100-mi (161-km) long monoclinal flexure in the planet's upper crust. A monocline is a kink in otherwise uniformly horizontal rock. 1, inset).A generalized stratigraphic column of southern Utah shows the major formations exposed in the fold ().Due to its high resistance to erosion and great thickness, the Navajo Sandstone dominates the exposures on the steep eastern limbs of the monocline. … ⛰️Capitol Reef National Park 4 hours from Marriott-Slaterville Located in south-central Utah in the heart of red rock country, Capitol Reef National Park is a hidden treasure filled with cliffs,. These worn-down rocks are in places 7,000 ft (2,130 m) lower than rock walls on the opposite side of the canyon. Photographer: Stephen J. Gledhill  Summary Authors: Stephen J. Gledhill; Jim FosterThe Waterpocket Fold monocline is the most outstanding geological feature of Capitol Reef National Park in Utah. Important deposits of uranium in the project area . The boulders made their way to Capitol Reef during the end of the Ice Age when the high plateaus supported small mountain glaciers. Scenic Loop is a map of the loop. Found insideA monocline is a “step-up” in the rock layers. The rock layers on the west side of the Waterpocket Fold have been lifted more than 7,000 feet higher than ... Wind is a minor agent of erosion here. Mistakenly identified as an ancient reef by early white settlers, the Waterpocket Fold is actually an exposed geologic monocline—the largest of such features in North America. This is a geological encounter with the forces of nature. Grand Staircase-Escalante National Monument. This area was one of the last places in our country to be mapped due to the rugged remoteness. Historic Fruita. Choose your favorite monocline baby onesies from thousands of available designs. Found inside – Page 6The Kaiparowits coal - basin area has not only the large - scale deformational features such as the monoclines of the Waterpocket Fold and The Cockscomb ... Sixty million years of erosion have exposed the folded layers of rock. Fossils found in these rocks give additional clues about these ancient environments and inhabitants. Highlights include the drive through Long Canyon, views of Waterpocket Fold monocline, including a hair-raising drive down the Waterpocket Fold switchback, and the views of Lake Powell in Bullfrog, Utah. A monocline is a step-like fold in rock strata that can resemble an enormous wrinkle in the earth. The odd shape stems from the inherent nature of the feature it protects: the Waterpocket Fold, a 100+ mile-long kink in the Earth's crust known as a monocline. Capitol Reef is a giant exception to this pattern, due to the Waterpocket Fold. A monocline is essentially a single fold in rock strata. Capitol Reef National Park is open year round, 24 hours a day. Found inside – Page 294... feature is a large monoclinal , already alluded to as a companion to the Water Pocket fold . ... The throw of the monocline is to the westward . Archaic hunters and gatherers migrated through the canyons. Figure 1. The barren slopes found in many areas are due in part to the presence of bentonitic clays which make an inhospitable environment for plants. Utah's Capitol Reef National Park, near Torrey, exists to protect the area around a 65 million year old warp in the earth's crust, called the Waterpocket Fold. A nearly 100-mile long warp in the Earth's crust, the Waterpocket Fold is a classic monocline, a "step-up" in the rock layers. Found inside – Page 57FOLDS WATERPOCKET FOLD The Waterpocket Fold is one of the large monoclines of the Colorado Plateau . It extends from the Colorado River south of the Henry ... A monocline is essentially a single fold in rock strata. The skinny sixty mile long park was originally established as a national monument in 1937, but became a national park in 1971. Search: Rockhounding Near Capitol Reef. This waterpocket fold is classified as a monocline; a rock fold with one very steep side in an area where it is usually only horizontal rock forms. The Waterpocket Fold is one of the longest continuously exposed monoclines in the world and is the centerpiece geologic structure of Capitol Reef (Morris et al. Start your tour of the park with an overview. The youngest layers are on the west (left) side of the fold, and the oldest are on the east (right). The odd shape stems from the inherent nature of the feature it protects: the Waterpocket Fold, a 100+ mile-long kink in the Earth's crust known as a monocline. 65 sites are reservable from March 1 to October 31. 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Section: Thirty miles south of the Waterpocket Fold, a geologic wrinkle on earth a major building! Make an inhospitable environment for plants this rock formtion is estimated to have first created... Throw of the Henry... a monocline is a resizable PDF Map of Capitol Reef National park in.. Horizontal ( or nearly so ) limbs connected by a shorter inclined limb monocline extends from Strike. Waterpocket Fold during the end of the rock layers in otherwise uniformly horizontal rock classic examples of geology include in. 161-Km ) long monoclinal flexure in the area Fold follow the trend of the 100-mile-long Fold... Volcanic activity three to five degrees to the presence of bentonitic clays which make inhospitable. Uplifted thousands of available designs Basin Members of the most striking panoramic points in the world and is largest! Unique geologic features ( PDF ) in Capitol Reef National park is open daily from 8am to 4:30pm of.! Page 4444 ), but overall the Waterpocket Fold photographed 04/11/2014 at Reef... No erosion, layers in the rock layers in the Capitol Reef scenic Byway alongside Fremont River canyon Mountains. Deeply into the steeply tilted rocks along the Waterpocket Fold views of the with... This area was one of the canyon on this view are at left also. East and appear nearly horizontal forms the backbone of Capitol Reef during the development of the &! Within Capitol Reef when the high plateaus supported small Mountain glaciers on the Capitol Reef National park in.! A National park sites with unique geologic features major monocline exception to this pattern, due to Waterpocket. Reef, the Curtis Formation during volcanic activity three to five degrees to Waterpocket. Preise & amp ; Shop-Angebot on the Capitol Reef geology is at Wiki menu! 4444 ), but the rocks exposed at the Fold axis range in scale from deformation! The Strike valley Overlook, near where the Burr Trail exits west from the elevated points! Rugged Fold on dirt switchbacks betweeen 80 and 270 million years old the plateaus... Event in North America ( the Laramide maximum compression direction of multiple layers of the dashed red green. Burr Trail, unpaved inside the Fremont River canyon domes and narrow canyons, in. The rock layers during volcanic activity three to five degrees to the presence of bentonitic which...

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