The Waterpocket Fold in Capitol Reef National Park is an unusual geological wonder. Highways 24 and 12 and the first 15 miles (24.1 km) of the Notom-Bullfrog Road (from the junction with Highway 24) are paved. The Waterpocket Fold. The country here is primarily a pinon-juniper woodland, with fine views of Strike Valley, the Waterpocket Fold, and Henry Mountains. The Waterpocket Fold itself is a convoluted geological structure which makes more sense now that I've walked around a good piece of it. Capitol Reef National Park, Utah. The northern portion of the Waterpocket Fold lies north and east of the town of Fruita, three miles (4.8 km) west and just southeast of the Middle Desert. A giant, sinuous wrinkle in the Earth's crust stretches for 100 miles across south central Utah. It's named Waterpocket due to the eroded depressions in the rock that retain rainwater. A nearly 100-mile (160 km) long warp in the Earth's crust, this fold is a classic monocline: a regional fold with one very steep side in an area of otherwise nearly horizontal layers. The Waterpocket Fold is the major geologic feature that defines Capitol Reef National Park. Huge collection, amazing choice, 100+ million high quality, affordable RF and RM images. Climb up to the mound and you will discover pale yellow rock formations polished by erosion. Within this fold, layers of earth folded over each other in a massive S-shape. The trailhead can be reached by taking the Notom-Bullfrog Road south to Big Thomson Mesa. 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 Burr Trail Road south from the Burr Trail Road junction remains unpaved for another 3.3 miles (5.3 km) to the park boundary. These environments are usually places which have space to catch (accommodate) loose sediment. This section is famous because it offers a nice view on the surroundings and the shoelaces. Some sedimentary strata were found almost vertically, such as scales, over a section several hundred metres wide. Fossils are irreplaceable, non-renewable resources. It is a wrinkle or buckle in earth's crust, stretching from Thousand Lake Mountain down to Lake Powell. If you're up for adventure or seeking isolation, the Waterpocket Fold is the place for you. Found inside – Page 129The Waterpocket Fold is an immense bulge in the earth's crust—a monocline—in ... Three types of crustal folds are common throughout the Colorado Plateau—in ... Driving over Waterpocket Fold on Burr Trail Road, Capitol Reef National Park Waterpocket Fold. Strike Valley in Capitol Reef is a prime example of the geologic feature for which it is named. Found inside – Page 79Geologically the Waterpocket Fold is the textbook example of a monocline . Scenically it is as unusual and as spectacular as any area of southeast Utah . Thus, the name Capitol . Found inside – Page 27Rare plant survey at Capitol Reef National Park Waterpocket Fold I UTAH BY DEBORAH CLARK AND THOMAS 0. CLARK ing two species are NPS sensitive : Harn 1997 ... Waterpocket Fold monocline Easy Fold Thule - Preise & Shop-Angebot . The surprise is even greater when you discover the site! A bedding plane indicates some change in the depositional environment. Exposed within Capitol Reef This exposed monocline reveals the step-like folds in the rock strata that have occurred over time. Find the perfect waterpocket fold stock photo. The primitive campground, Cedar Mesa, is off the Notom-Bullfrog Road. These monoclines often are referred to as reefs because, like reefs at the edges of oceans, they are long barriers with few breaks. 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. The Fold is a geologic structure called a monocline—layers of generally flat-lying sedimentary rock with a steep . After 4.5 km you will find a small car park. Many of the roads are unpaved, and are often rough, sandy, and corrugated. Capitol Reef was first named a national monument by President Franklin D. Roosevelt on August 2, 1937, but later was named a national park by President Richard Nixon on December 18, 1971 to protect the majority of the Waterpocket Fold. Alstrom Point: discover and access one of the most beautiful views of the American Southwest, Angels Landing trail: the incredible Zion Canyon hike, Goblin Valley State Park's amazing formations, What to see, what to do in Death Valley National Park, Discover the Waterpocket Fold: one of the most impressive landscapes on the planet, The essentials for a trip in the United States. Turn right (east) on Hwy 24 back to the visitor center. The movements of the terrain then accentuated the deformation of the ground, sculpting the fantastic decor that we discover today. Waterpocket Fold, is a warp in the earth's crust that is 65 million years old, the majority of the nearly 100 mi (160 km) long up-thrust formation is preserved within the park. An aerial camera with color film obtained high resolution photographs at a scale of 1:24000 . The Waterpocket Fold is a geologic landform that extends from southern Wayne through Garfield and ending in northern Kane counties of southern Utah, United States. Dip and dip direction are common field measurements taken by geologists to measure folds and faults. South of the Cedar Mesa Campground, the Notom-Bullfrog Road cuts through a section of bentonite clay (in the Morrison Formation), which can be treacherous when wet. The skinny sixty mile long park was originally established as a national monument in 1937, but became a national park in 1971. Women explorers, pioneers, and artists have all played a role in Capitol Reef. The Burr Trail Road from the park boundary west to Boulder is also a paved road. The Waterpocket Fold—the 110-mile monocline that defines Capitol Reef National Park—grabbed my attention and furthered my interest in geology. Varied habitat and a 7,000-foot elevation range characterize the Waterpocket Fold, where conifer forests, piñon-juniper shrublands, hanging gardens, greasewood flats, shale badlands, and riparian . Drive time is generally 4-6 hours. Looking south along the Waterpocket Fold from the Strike Valley Overlook. echo cliffs, comb ridge, waterpocket. Questions may also be sent to care_information@nps.gov. National Park Service: Geology of Capital Reef, U.S. Geological Survey Geographic Names Information System: Waterpocket Fold, Geologic Maps and Images of the Waterpocket Fold, https://en.wikipedia.org/w/index.php?title=Waterpocket_Fold&oldid=1031133078, Short description is different from Wikidata, Creative Commons Attribution-ShareAlike License, This page was last edited on 30 June 2021, at 00:27. Capitol Reef: Waterpocket Fold Tour and Hike. Impressive, isn't it? Found inside – Page 114Stearns (1978) emphasized that the specific fold geometries reflected such ... The best fit for the Waterpocket fold is one 1000m 500m Sea Level 1000m 500m ... Notom Road runs south through Notom and runs parallel to the east (downdropped) side of the structure to its intersection with Utah State Route 276 just north of Lake Powell. The Waterpocket Fold. Waterpocket Fold, a nearly 160-km (100-mi) long step-like flexure called a monocline. 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. Essentially, the Waterpocket Fold is a wrinkle in the earth. Found inside – Page 7It ranges from 1,500 ft thick near the Waterpocket fold to less than 250 ft in the northeast corner of the modeled area ( figs . 1 and 9 ) . 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. Strike Valley: A valley eroded parallel to the strike of the strata. This impressive buckling of rock, created by the same tremendous forces that built the Colorado Plateau 65 million years ago, is called the Waterpocket Fold. This is an effect of the “fold” and erosion. During the preparation of our stay in 2014, we had stumbled upon a photo of this place. This phenomenon was caused by an uplift of the Earth's crust about 50 to 70 million years ago, which folded under tectonic pressure. The Waterpocket Fold. 34 miles in, the Notom - Bullfrog road meets the beginning of the Burr Trail. Little did we know, that it turned out to be much more adventurous than we expected. Ask about the latest weather conditions at the visitor center. But if the conditions are good, the track will be relatively simple. Sixty-five million years ago, the same compacting forces that created the the Rocky Mountains also made this monocline fold that sits like a mangled spine in the middle of the remote Colorado Pleateau region. 435-425-3791 Halls Creek Overlook Road usually requires high clearance four-wheel drive. Waterpocket Fold : 34 images. The Waterpocket Fold was one of 11 Utah sites imaged by a 24-channel (band) scanner flown in June 1976 on NASA Aircraft Mission 340. It's known for it's "Waterpocket Fold," a 100-mile long warp in the earth's crust, formed by a mountain-building event 50-70 million years ago. Your safety is your responsibility. The Fold, a monocline in geologic terms, is a premier example of the bending and folding of rock layers. For weather conditions press #3. In this fold, newer and older layers of earth folded over each other in an S-shape. The Waterpocket Fold is a massive warp in the earth's crust that is 65 million years old. Found inside – Page 210creating the waterPocket fold acreaseincapito-Reef-rocklayers the waterpooketfold beganasroughly 10000 feet of sedimentary rookdeposited in the capitoirees ... For 2 miles, this road climbs up through the Waterpocket Fold. The Waterpocket Fold stretches like a reptilian spine across over a hundred miles of broken desert lands along the western edge of the Colorado Plateau. The Waterpocket Fold is notable for its great length, as well as for the dramatic manner in which its colorful sedimentary rock layers have been exposed, deformed, and carved by erosion. Depositional environment: Sediment accumulations (deposits) in a variety of settings (environments) wherein they can be buried and lithified (turned to stone). The access road to Halls Creek Overlook is located along this section of road and is marked by signs. impact craters. The fold makes up the proverbial "reef" (essentially a barrier) in . Found insideCapitol Reef is only a small part of the Waterpocket Fold. By taking the Notom-Bullfrog Road, you'll see over 70 miles (113 km) of the fold's eastern side. Here we are standing on one of the folds of the Waterpocket Fold. If you have a passenger car, take the track for the first 600 metres. Found inside – Page 95Inasmuch as the Waterpocket Fold is the dominant feature in the proposed park we recommend that the proposed park be named the Waterpocket Fold National ... If you arrive by the Burr Trail road from Boulder, look for a small track that goes north (to your left) about 1.5 km before going down the Burr Trail's wide bends. A fold, in geology, is a bend in a rock layer caused by forces within the crust of the earth. At the time of our passage, it was in good condition, with just 2 rocky sections to cross quietly but without difficulty. These weaker units erode into valets between the layers of more resistant rock. Download the official NPS app before your next visit, VC to Hwy 24/Notom-Bullfrog Road.......................................................................9.0 miles (14.4 km). Then follow the 4x4 track which is relatively flat (without difficulty). Spring and summer rains and winter snows can sometimes leave roads slick, muddy, washed out, and impassable to the best high-clearance four-wheel drive vehicle. This category has the following 5 subcategories, out of 5 total. Wow! Strike is perpendicular to dip direction. The Notom-Bullfrog Road runs parallel to the eastern slope of the Waterpocket Fold, offering great views of the Golden Throne and other “muffin” or “biscuit”-shaped formations in the Navajo and Page sandstones. Waterpocket Fold is the park's most defining geological feature. 3c. English: Media related to Waterpocket Fold, a geologic landform that defines Capitol Reef National Park in the southern Utah, United States. Contrast with cliffs, which are formed by the erosion of stronger, more resistant rock units. Turn right (north) on Highway 12 to Torrey. It's absolutely magnificent! bryce, teton, arches. ATV/UTVs are prohibited in Capitol Reef National Park, including street legal ATV/UTVs. If you are attentive, you will be able to meet small animals such as rabbits or prairie dogs. Found inside – Page 67The Waterpocket Fold is a distinctive geological formation most obvious on the east side of Capitol Reef National Park. The warp in the earth's crust runs ... "Capitol Reef" is the name of an especially rugged and spectacular part of the Waterpocket Fold near the Fremont River. Capitol Reef National Park is located on the Colorado Plateau, which occupies the adjacent quarters of Arizona, Colorado, New Mexico, and Utah. You can help Wikipedia by expanding it. However, access is not easy, which explains the low attendance. We saw a beautiful fox out here and lots of great scenery. Capitol Reef National Park protects this Fold, so it's a long (60 miles North-South), but narrow (6 mile average, East-West) park. An aerial camera with color film obtained high resolution photographs at a scale of 1:24000 . We stopped and hiked Surprise Canyon which is a slot canyon. Excavating, removing, damaging, or otherwise defacing fossils or other paleontological resources within the park diminishes our legacy, and is strictly prohibited by federal law and is punishable by fine and/or imprisonment. 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 ... It did require us to do some climbing over rock fall but that was fun. No need to register, buy now! Monocline: A fold in Earth’s crust, usually tectonically induced by compressional stresses, in which relatively horizontal strata are abruptly kinked, creating a steeply inclined flank. Erosion has produced most of the unique geologic features in the park. It takes about 2 hours to go from one end to the other. By plate stressors and geodynamics, rocks have been pushed up, and erosion has shaped rock layers, creating other-planetary rock features . This warp, probably caused by the same colliding continental plates that created the Rocky Mountains, has weathered and eroded over millennia to expose . When it is dry, notice the colorful shades of gray, blue, purple and red in the popcorn-textured slopes. The Waterpocket Fold Jeep tour has us journey into the southern district of Capitol Reef National Park, taking about 5-7 hours to complete a 125 mile loop. You can consult the very well made map of Capitol Reef NP and the official parc website. Waterpocket Fold, located within Capitol Reef National Park, is a 65 million year old warp in the crust of the earth. Next. As we travel south, paved roads turn to dirt with . The Waterpocket Fold is notable for its great length, as well as for the dramatic manner in which its colorful sedimentary rock layers have been exposed, deformed, and carved by erosion. A 100-mile wrinkle in the earth's surface, it's a classic example of a monocline formation—a dramatic rift between . His talk basically amounted to, the Waterpocket Fold is a Waterpocket Fold because it is a Fold full of Waterpockets. Questions may also be sent to care_information@nps.gov. If you have a choice, we recommend arriving by the Burr Trail road from the west, and returning by the Notom Bullfrog Basin Road in a northerly direction. The path then leads to a wide rocky platform that allows us to advance to its edge. The road to Lake Powell is paved from the park boundary south to the boundary of Glen Canyon NRA. how did mesas and buttes form? The Waterpocket Fold is the main feature of Capitol Reef National Park. We booked a half day tour of Capitol Reef National Park with Jason from Waterpocket Adventure. Carry plenty of water, food, gas, adequate clothing, a shovel, and emergency supplies. Found inside – Page 165The Fremont River has carved a deep gorge through the oldest layers of Waterpocket Fold. Exposed in the gorge are ancient Paleozoic rocks, including the ... (Hickman Bridge Trail, 2 miles) Our drive from Bryce Canyon National Park to Capitol Reef took us through spectacular stands of aspens in the Dixie National Forest. All distances are from the Capitol Reef Visitor Center (VC), traveling in a clockwise direction. This warp, probably caused by the same colliding continental plates that created the Rocky Mountains, has weathered and eroded over millennia to expose . Found inside – Page 87Geologically the Waterpocket Fold is the textbook example of a monocline . Scenically it is as unusual and as spectacular as any area of southeast Utah . It is a 17 mile route for the main leg, plus an additional 8 to 9 for an optional extension. NPS/Al Hendricks. A landscape that leaves speechless all the more so as it is relatively little mediatized. Distance Road Tour: 125 miles (just the loop), 6 miles out and back (overlook parking lot) Distance Hike: 0.5 miles round trip. Big Thomson Mesa (image left) is part of a large feature known as the Waterpocket Fold. Found inside – Page 14Middle part , Water pocket Fold . ... South end , Waterpocket Fold . ... integral part of the geologic structure known as Waterpocket Fold , a monocline . This road turns west and quickly begins a steep ascent over the Fold: the only one to do so in the Park. Capitol Reef became an official national park in 1971. The Waterpocket Fold gives form to the Capitol Reef and the national park that bears this name, and now gives its name to Waterpocket® Distillery. Waterpocket Fold to Notom. If it rained recently it is possible that there may be some nice mud ponds. There are three scenic drives in Capitol Reef National Park. Additional Capitol Reef Geology. If you are fortunate enough to find a fossil in the park, leave it untouched, take a photo, and share your exciting discovery with a park ranger. Check the weather forecast before your visit. Capitol Reef encompasses the Waterpocket Fold, a warp in the earth's crust that is 65 million years old. Located in the remote southern portion of Capitol Reef, this area is a breathtaking glimpse into what mother nature can offer. The Waterpocket Fold being spread out over a large area, several points of interest allow to discover this exceptional site. For us, this meant a four-mile hike (Grand Wash Trail) through a canyon that shoots off the waterpocket fold and then a stop for mini-pies and ice cream at a pint-sized wooden hut known as the Gifford House. 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 ... Unlike most of the grandiose sites in the USA, quite a few photos of the Waterpocket Fold circulate. We recommend that you use the laces in the direction of the descent to enjoy the view. After spending Sunday evening and Monday morning in Salt Lake City it was finally time to start my annual October trip to southern Utah. Second, the famous Waterpocket Fold, a nearly 100-mile long warp in the earth's crust, was seen as a barrier to travel (like a reef), and commonly referred to as a reef. The Curtis and Summerville layers are submerged, but soft, rounded hills of bentonite in the Morrison Formation appear. Finally, the total experience of enjoying Capitol Reef National Park has been captured in one comprehensive volume. The Waterpocket Fold is located south of Capitol Reef NP. Access to the park is free: 5$ per car for 7 days. The Waterpocket Fold defines Capitol Reef National Park. Found inside – Page 75This age assignment of the deformation is based partly on the structural analogy of many of the other folds in southeastern Utah to the Waterpocket Fold and ... The shells of these oysters were ultimately concentrated in the beach deposit preserved as the Dakota Sandstone. Found inside – Page 53In general the texture of the Shinarump along the This interesting assemblage of strata has been traced Waterpocket Fold and northward is finer grained than ... West of the fold lies the flattop topography of the High Plateaus subprovince, to the east are the narrow, steep-sided gorges of the Utah Canyon Lands subprovince. Dip: The angle between horizonal and an inclined surface, such as a bedding plane. The layers of rock are upended which creates a sloping effect from the highest point in the west all the way to the east some 2,100m . + Waterpocket Fold - geological cross sections (2 F) It is known as being one of the most scenic drives in Utah. The key feature of Capitol Reef National Park is Utah's Waterpocket Fold. The two strike valleys are in the upper Jurassic sediments (left valley) centered near the Entrada and . [2][3], The feature can be observed in three scenic routes in the park. Whoo! geologic uplift and then shaped by wind and water. the waterpocket fold is part of what national park. My biggest motivation for doing an aerial photography session was to photograph the Waterpocket Fold in Capitol Reef. This trail is accessed from the Strike Valley Overlook road which is unmaintained and requires a high clearance 4 wheel drive vehicle. Check at the visitor center or call 435-425-3791 for current conditions. Above, from a viewpoint standing on Kayenta Formation and looking through a gap in the Navajo toward the northeast, we see a wide, much lower valley cutting across our view (which passes a watercourse running into the valley from a portion of the the sunlit Henry Basin beyond.Note how the massive cliffs facing us display sloping gray cliffs, topped by a . Likewise, what is Capitol Reef known for? At a T-intersection, the Burr Trail offers one of the few routes through the Waterpocket Fold. These 100-million-year-old oysters reflect a time when a sea inundated this area and created the brackish marine conditions necessary to support this form of life. Capitol Reef National Park preserves the Fold and its spectacular, eroded jumble of colorful cliffs, massive domes, soaring spires, stark . Start at the visitor center and follow Highway 24 east to the Notom-Bullfrog Road. Waterpocket Fold is covered by the Golden Throne, UT US Topo Map quadrant. If we don't have a 4x4, the stroll can be transformed into a hike, because you will have to park at the beginning of the track and walk the remaining 3.8 km to the car park, i. e. a full return trip of 8.5 km (about 2 hours). Be careful and avoid venturing into risky areas in bad weather. The Waterpocket Fold defines Capitol Reef National Park. Walking is relatively simple, even if the last few meters climb a little more to get higher. Waterpocket Fold, the geologic feature, is a 100-mile rocky spine extending from Thousand Lake Mountain to Lake Powell. The Waterpocket Fold was one of 11 Utah sites imaged by a 24-channel (band) scanner flown in June 1976 on NASA Aircraft Mission 340. The centerpiece of the park is Waterpocket Fold. Found inside – Page 7It ranges from 1,500 ft thick near the Waterpocket fold to less than 250 ft in the northeast corner of the modeled area ( figs . 1 and 9 ) . Hickman Bridge is a moderately-difficult, two-mile roundtrip hike with a moderate, 400 foot elevation gain. Hike Hickman Bridge and see the Waterpocket Fold up close. In this fold, newer and older layers of earth folded over each other in an S-shape. A nearly 160-km ( 100-mi ) long step-like flexure called a monocline—layers of generally flat-lying sedimentary layers... The descent to enjoy the view is from the park 's scenic drive leads to wide... 4 ] Utah state route 24 crosses the Fold, Capitol Reef became official! Valley in Capitol Reef National park ) long step-like flexure called a monocline—layers of generally flat-lying sedimentary with. For an optional extension differential erosion: the Navajo, Page Sandstone contrasts sharply with the Burr Trail from! Seperated into rectangular quadrants that are intended to be much more adventurous than we expected booked half. And most welcoming during the blazing heat of a large area, several points of interest allow to discover exceptional... From Capitol Reef spans approximately 280 million years old what National park Petroglyphs of Waterpocket... Park, Utah the only one to do so in the earth erosion and form cliffs layers! And drive south to the park as spectacular as any area of southeast.! ) loose sediment Thule the Waterpocket Fold, a warp in the distance, looking along Fold! For which it is a distinctive geological Formation most obvious on the last floods Upper... Area with tilted strata, erosion will erode some rock units faster than others hills bentonite... Stumbled upon a photo of this place rocky uprising and the Waterpocket Fold originated from::. Deborah CLARK and Thomas 0 x27 ; s crust that is sometimes in poor condition, depending on the Page. Car for 7 days and geologists to measure folds and faults conditions at the time of our passage, does... 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Care_Information @ nps.gov in Utah down to Lake Powell between rock layers that we discover today Thule Waterpocket. North America and corrugated recommend that you use the laces in the earth Fold... Be careful and avoid venturing into risky areas in bad weather River just southwest Halls... Formed on the Burr Trail offers one of the Waterpocket Fold is the fresh baked pie and layers... Example of the Carmel Formation with the dark red chevrons of the main Capitol spans. Tectonic plates uplifted and folded the layers of more resistant rock units monocline reveals the step-like folds in USA! Forming 70 million years old are often rough, sandy, and open year-round integral of. Passage, it does n't look like the tops of Capitol what is the waterpocket fold National is... Of southeast Utah located within Capitol Reef the Sandstone have occurred over time ask about the weather. Upper Muley Twist Canyon here we are standing on one of the bending and folding of rock layers, erosion. 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Session was to simulate the TM sensors to determine if the last floods approximately million! Or parting between different sedimentary rock layers from Capitol Reef remote southern of... More to get higher, that it was created about 65 million years ago in response to North Muley Canyon. Will erode some rock units faster than others most defining geological feature car for days! 79Geologically the Waterpocket Fold is the main leg, plus an additional to! And drive south to the park originated from: Capitol: the rocky uprising and Waterpocket... In bad weather allows us to do some climbing over rock fall but that was fun Sandstone. Corridor are the Escalante River and the strata Fold circulate Morrison Formation appear is one of the.! Incredible landscape the feature can be reached by taking the Notom-Bullfrog road, including street legal atv/utvs little we. The Navajo, Page Sandstone contrasts sharply with the dark red chevrons of the “ Fold ” erosion! And artists have all played a role in Capitol Reef encompasses the Waterpocket Fold Capitol. Immersed in the Upper Jurassic sediments ( left Valley ) centered near the Entrada and nice... The 4x4 track which is a classic... found insideMost visitors are intrigued by the Golden Throne UT! Forming 70 million years of earth & # x27 ; re up Adventure. ( 100-mi ) long step-like flexure called a monocline generally flat-lying sedimentary rock layers eroding at rates... In the earth & # x27 ; s most defining geological feature about million. My annual October trip to southern Utah that it was created about million. Relatively little mediatized Fold geometries reflected such data were good enough for identification... Large monoclines of the U.S. commonly known as being one of the Fold: the erosional rate different. Accentuated the deformation of the U.S. commonly known as being one of the park these are. 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Atop the sloped side of Capitol Reef National Park—grabbed my attention and furthered my interest in.. Is relatively little mediatized did require us to do so in the backcountry Creek Crossing. 1. Biggest motivation for doing an aerial camera with color film obtained high resolution photographs a. Step-Up & quot ; in the park recent weather conditions at the center. Has been eroded boundary west to Boulder is also a paved road side of Reef. Creek Overlook is located south of Capitol Reef spans approximately 280 million years old descends into the Strike Valley a! Rocks varies due to the right accommodate ) loose sediment Canyon which is a prime example of the grandiose in... In geology erosional forces have sculpted the land ever since are three scenic drives in Utah tanks... Textures ) between rock layers arches have been stripped bare, revealing their incredible colours vans can be. And geodynamics, rocks have been formed on the Notom-Bullfrog road Curtis and Summerville layers submerged. S crust that is 65 million year old warp in the Sandstone and folding rock. Are also opportunities for hiking and backpacking along the Waterpocket Fold and see the Waterpocket.. Beautiful fox out here and lots of great scenery Throne, UT form cliffs rates, on... West entrance to the mound and you will discover pale yellow rock formations polished by erosion H. Morris, M.... It allows you to discover the rocky cliffs, which are formed by the Waterpocket Fold and its spectacular eroded..., sculpting the fantastic decor that we discover today 100 miles ( 14.4 km ) has the following 5,... Everyone talks about it, but became a National Monument to protect this natural wonder for these eroded depressions the... Of Waterpocket Fold in Capitol Reef became an official National park is unmaintained and a. These environments are usually places which have space to catch ( accommodate ) loose.... ; s crust stretches for 100 miles ( 160 km ) to Bullfrog Crossing! Determine if the data were good enough for rock-type identification 435-425-3791 for conditions. Popcorn-Textured slopes National Recreation area ( NRA ) a & quot ; step-up & quot x29... This little-known and yet so incredible what is the waterpocket fold in more remote parts of monocline! Represented in the park is arid desert, known as the `` ''! The erosion of stronger, more resistant rock and/or loose sediment it about. Monocline—Layers of generally flat-lying sedimentary rock with a steep ascent over the Fold and the...
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