Capitol Reef National Park is a national park, in Utah's Canyon Country.
Capitol Reef National Park is a national park, in Utah's Canyon Country.
Capitol Reef is a National Park comprising 378 sq mi (980 km2) of sandstone canyons, ridges, buttes, and monoliths. The park is defined by the Waterpocket Fold, a 100 mi (160 km) long wrinkle in the earth's crust known as a monocline. The Fold extends from nearby Thousand Lakes Mountain to the Colorado River (now Lake Powell). Capitol Reef National Park was established to protect this grand and colorful geologic feature, as well as the unique natural and cultural history found in the area. The name was derived from the rounded sandstone buttes which resemble capitol domes and from the long line of rocky cliffs which are a barrier to travel, like a coral reef.
From the 9th to 15th centuries, Native Americans of the Fremont Culture lived in and near the Waterpocket Fold. They seem to have left the region around 1500 for unknown reasons. Later, nomadic Ute and Southern Paiute tribes inhabited the area. Explorer John C. Fremont passed through the northern part of what is now Capitol Reef in 1854. The Fremont River that runs through the park is named after him.
White settlement came late to the area, in the 1870s, Latter Day Saints (Mormon) settlers moved into the high plateau lands west of Capitol Reef and established communities based on short-season farming and grazing. In the 1880s Mormon settlers moved into Capitol Reef and established the community of Fruita along the banks of the Fremont River. These settlers planted the fruit orchards along the river that still exist today. No more than 10 families at any one time lived in the Fruita area.
National park in Utah, United States Capitol Reef National ParkIUCN category II (national park)Capitol Reef National ParkInteractive map of Capitol Reef National ParkLocationWayne, Garfield, Sevier, and Emery counties, Utah, United StatesNearest cityTorreyCoordinates38°12′N 111°10′W / 38.200°N 111.167°W / 38.200; -111.167Area241,904 acres (978.95 km2)670 acres (270 ha) privateEstablishedDecember 18, 1971; 54 years ago (1971-12-18)Visitors1,422,490 (in 2024)Governing bodyNational Park ServiceWebsitenps.gov/care Capitol Reef National Park is a national park of the United States in south-central Utah. The park is approximately 60 miles (100 km) long on its north–south axis and just 6 miles (10 km) wide on its east-west axis, on average. The park was established in 1971 to preserve 241,904 acres (377.98 sq mi; 97,895.08 ha; 978.95 km2) of desert landscape and is open all year, with May through September receiving the most visitors. Partially in Wayne County, Utah, the area was originally named "Wayne Wonderland" in the 1920s by local boosters Ephraim P. Pectol and Joseph S. Hickman. Capitol Reef National Park was designated a national monument on August 2, 1937, by President Franklin D. Roosevelt to protect the area's colorful canyons, ridges, buttes, and monoliths; however, it was not until 1950 that the area officially opened to the public. Road access was improved in 1962 with the construction of State Route 24 through the Fremont River Canyon. The majority of the nearly 100-mile-long (160-kilometer) up-thrust formation called the Waterpocket Fold—a rocky spine extending from Thousand Lake Mountain to Lake Powell—is preserved within the park. Capitol Reef is an especially rugged and spectacular segment of the Waterpocket Fold by the Fremont River. The park was named for its whitish Navajo Sandstone cliffs with dome formations—similar to the white domes often placed on capitol buildings—that run from the Fremont River to Pleasant Creek on the Waterpocket Fold. Locally, reef refers to any rocky barrier to land travel, just as ocean reefs are barriers to sea travel. Cathedral Valley
The area was called "Wayne Wonderland" in the 1920s by local boosters Ephraim P. Pectol and Joseph S. Hickman, and in 1937, President Franklin D. Roosevelt set aside a portion of Wayne Wonderland as a National Monument. Funds for the park were scarce, however, and it would be a long time before the first rangers would arrive. During the 1960s, a campground, visitor center and staff housing were built and a road through the park was paved. During this period, most of the farmers in the area left and sold their land to the Park Service. In 1968, a large amount of land was added to the park, increasing its size by almost 600%, and in 1971 the National Monument became Capitol Reef National Park.
Travellers to the park experience a dazzling landscape of rock formations. From colorful domes, high cliffs, and towering spires of sandstone to arches, natural bridges, and narrow slot canyons. The desert streams, such as the Fremont, wind through the Park, carving deep canyons and meandering through floodplains surrounded by narrow ribbons of greenery.
The Waterpocket Fold defines the park. A 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. A monocline is a "step-up" in the rock layers. The layers on the west side of the Fold have been lifted more than 7,000 ft (2,100 m) higher than those on the east. The park was established primarily to preserve the geologic features of the Waterpocket Fold, such as the scenic rock domes and narrow canyons. Capitol Reef is a geologist's paradise, with nearly 10,000 feet of sedimentary layers ranging from 270 million to 80 million years old. The Waterpocket Fold has tilted this geologic layer cake down to the east, with older rocks in the west and younger ones in the east. Rock layers in Capitol Reef reveal ancient environments as varied as rivers and swamps (Chinle Formation), Sahara-like deserts (Navajo Sandstone), and shallow oceans (Mancos Shale). These layers have been eroded by wind and especially water over the last 20 million years. The land forms are a result of different responses of various rock layers to these forces of erosion. Hard sandstone layers form cliffs, while softer shale layers form slopes and low hills. Black boulders found scattered throughout the park are volcanic rocks from the 20 to 30 million year old lava flows which cap the nearby mountains.
The most visible plant life in the park is found in the riparian corridors near Fruita. Along the rivers, you may see cottonwoods and willows as well as the invasive tamarisk. Pioneer orchards along the Fremont River sport apple, apricot, pear, peach, and cherry trees. In the dryer areas of the park, you may see sagebrush, Utah Juniper, various prickly pear cacti, and higher elevations may feature pinyon pine. The cacti, along with some desert wildflowers, bloom briefly in the early spring.
Like many parts of the Utah desert, the nearly barren ground is covered with a biological soil crust, also known as cryptobiotic soil. This collection of bacteria, moss and lichen helps to stabilize loose desert soils and retain precious moisture. These crusts are very fragile, however, and should never be walked or driven on as they may take centuries to regenerate. Do not leave established hiking trails, but if you must, walk in washes or on bare rock.
There are many animals in the park, but, like many desert creatures, they are far more active at night. The park is home to many species of lizards, and a number of snakes. Listen for the sound of Canyon Wrens in the narrow washes; they and many other birds make their home here. Vultures, hawks and the introduced Chukar are common sights in the park. You may be lucky enough to see some of the numerous bat species flying around Fruita in the evening. Deer are an extremely common sight in the orchards and picnic area. Though they may look tame, they are not. Do not feed them or any other animal. Other common large mammals include the Gray Fox, Raccoon, Ringtail, Badger, and Porcupine. The once common Desert Bighorn Sheep were reintroduced in the late 1990s and are thriving. Mountain Lions have also been reported in the park, but are rarely seen by visitors. If you do see one, do not approach it.
Summer temperatures often climb into the upper 90s(F), but nights cool down into the 50s(F) and 60s(F). The thunderstorm season from July through September brings cloudbursts, flash floods and lightning. Spring and fall are milder with highs generally in the 50s(F) and 60s(F). Daytime winter highs average less than 50(F). Snowfall is usually light, especially at lower elevations. Humidity is low all year.
Park website
Traveling westbound on Interstate 70 - Take Utah State Highway 24 west towards Hanksville (exit 149). Stay on Highway 24 for 95 miles to reach the park Visitor Center.
Traveling on Interstate 15 - Take US Highway 50 east at Scipio (exit 188) towards Salina for 30 miles. At the junction with Utah State Highway 89/259, turn right (south) and travel 8 miles. Turn left (east) onto Utah State Highway 24 towards Sigurd. Continue on Highway 24 for 82 miles to reach the park Visitor Center.
If you are OK with being way off the beaten track, you can reach the skinny south end of the park via the remote Burr Trail Road, which runs from Boulder in the west through some awe inspiring stretches of Grand Staircase-Escalante National Monument, and then runs southeast of the park to Bullfrog Marina in the desolate reaches of the Glen Canyon National Recreation Area. Be prepared that the road is not paved within the park, and the unavoidable gravelly ride down the Burr Trail Switchbacks is extremely steep, and not likely passable in rain or when wet.
The park and campgrounds are open year round. The Visitor Center is open daily (except for some major holidays) from 8AM-4:30PM with extended hours during the summer season.
Ripple Rock Nature Center is open from Memorial Day through Labor Day from 10AM-3PM Tuesday through Saturday, closed Sundays and Mondays.
The following entrance fees (updated as of 2020) are charged for traveling the park's Scenic Drive beyond the Fruita Campground and are valid for seven days:
$10 - Bicycle and Pedestrian
$15 - Motorcycle
$20 - Private Vehicle
$35 Capitol Reef Annual Pass
The America the Beautiful Pass, also called the Interagency Pass, provides entry to Capitol Reef National Park and all national parks, as well as some national monuments, national wildlife refuges, and national forests. A single pass applies for an entire group traveling together in a private vehicle, or up to four people on foot or bike. There are several pass types:
The Annual Pass (valid for twelve months from date of issue) can be purchased by anyone. $80 for U.S. citizens and residents, $250 for non-U.S. residents, $20 for U.S. citizens or permanent residents age 62 or over, and free for current military personnel (must show a Common Access Card (CAC) or Military ID).
The Lifetime Pass (valid for the life of the holder) is available for $80 to U.S. citizens or permanent residents age 62 or over, and free for veterans and Gold Star families (families of servicemembers who were killed in action). Applicants must provide documentation showing they are eligible. This pass also provides a 50% discount on some park amenities.
The Access Pass (valid for the life of the holder) is available for free to U.S. citizens or permanent residents with permanent disabilities. Applicants must provide documentation of citizenship and permanent disability. This pass also provides a 50% discount on some park amenities.
The Volunteer Pass is available for free to individuals who have volunteered 250 or more hours with federal agencies that participate in the Interagency Pass Program.
The free Annual 4th Grade Pass (valid for September to August of the 4th grade school year) allows entry to the bearer and any accompanying passengers in a private non-commercial vehicle. Registration at the Every Kid Outdoors website is required.
In 2026, the National Park Service offers free admission to all national parks on 10 days:
President's Day (February 16)
Memorial Day (May 25)
Flag Day (June 14)
Independence Day Weekend (July 3-5)
The National Park Service Birthday (August 25)
Constitution Day (September 17)
Theodore Roosevelt's birthday (October 27)
Veterans Day (November 11)
Entrance fee waivers: fee waivers are available for groups traveling the Scenic Drive for educational purposes. Fee waiver requests must be submitted two weeks prior to your visit.
Sites at the Fruita Campground are $10 per night. Senior and Access pass holders receive a 50% discount on their campsite.
Unlike the more popular parks in Utah, Capitol Reef does not have a bus system inside the park.
There are extensive roads running through the park, some paved, some not. A few roads require a four-wheel drive vehicle. During a strong storm some roads become impassable by any vehicle.
Biking is allowed only on established roads in order to protect the fragile high desert soil.
Orchards Along Highway 24 and the scenic drive are 22 orchards ranging from .5 acre to nearly 8 acres, with various fruits, including cherry, apricot, peach, pear, apple, and a few plum, mulberry, almond and walnut trees. Flowering season starts in early March and ends early May. Harvest season starts early June and ends in the middle of October, depending on the type of tree. You are allowed to enter any unlocked orchard and eat as much ripe fruit as you wish. Seeds are usually thrown on the ground, inside the orchard. Only during each fruit's individual harvest season are you allowed to carry out fruit. Usually one pound of fruit will cost $1.00 and a bushel $15–20. Ladders, picking tools, and plastic bags are provided.
Rim Overlook & Navajo Knobs trail (deviation from the Hickman Bridge trail located on Highway 24). Strenuous, with a fantastic 360° view from the summit.
Cohab Canyon (one trailhead lies right on the road outside the Fruita campground in a well-marked place, the other trailhead is on Highway 24 across the Hickman Bridge trailhead, also well-marked). One of the most popular trails, this one-way, 1 3/4 mile trail connects Highway 24 and the Fruita campground by way of a gorgeous canyon littered with side slot canyons and small holes in the rock, begging to be explored. At the campground trailhead there is a series of switchbacks for 1/4 mile, the most strenuous part of the hike. Halfway there is a side trail leading to a north and south overlook of Highway 24 and the nearby orchards. The north overlook rests on a sheer cliff hundreds of feet from the ground.
Hickman Bridge (self-guided nature trail) (trailhead right off Highway 24 connected to a small parking lot). Be sure to pick up a brochure at the trailhead ($0.50) and watch for numbered wooden poles. One of the attractions is a small clay enclosure tucked up into the fold of a rock once used by the Fremont tribe to store food. An easy 1 mile loop hike leads to the Hickman Natural Bridge.
Historic Gifford Farmhouse (One mile south of Visitor's Center along the Scenic Drive). Daily 9AM-4:30PM. There is a store inside the kitchen of this historic homestead that sells items handmade by local craftsmen, such as quilts, soap, candles and toys as well more typical souvenirs like books, and postcards. The highlight is the locally made foodstuff such as jams, pickles, and excellent homemade fruit pies.
The only food able to be purchased in the park is small snacks and drinks in the visitor center or from the Gifford Farmhouse. For sale are scones, loaves of artisan bread, freshly baked fruit pies, ice cream, many different types of salsa, jams, butters, and any other concoctions made in the nearby town of Torrey.
All of the running water near the visitor center and campground is safe to drink. In the backcountry it is possible to find shallow holes filled with water, but these are a last resort and must be thoroughly filtered and sanitized before drinking. Local wildlife use these small seasonal ponds for their daily consumption and it is irresponsible to disturb these micro habitats unless absolutely necessary.
There is no lodging other than camping in the park, the nearby towns of Torrey, Caineville and Hanksville have a selection of hotels, motels, B&Bs, etc.
Fruita Campground (one mile south of the visitor's center on the main road). 71 sites. 58 sites can be reserved in advance, 13 sites are first-come, first-served. There are nearby bathrooms with running water, picnic table, fire pit, RV dump station, a nearby amphitheater with Ranger talks almost every night in the summer season, and a bordering apple and pear tree grove. When the trees are bearing fruit, deer will wander into the grove every night and eat fallen fruit. Campers can safely view the wild animals at a distance, but it is not recommended to go any closer than 30 feet, as mothers can charge humans if they perceive a threat. It is open year-round. From March through October, campsites are able to be reserved on www.recreation.gov. From November through February, campsites are filled on a first-come, first-served basis. Maximum of 7 people per site. $20 per site (2020 rates). (updated Jun 2020)
There are two primitive camping spots in the park, each offering a picnic table, fire grate, and pit toilet. Neither site has running water or other amenities. Both are first-come, first-served and do not require a fee.
Cathedral Campground (on the Cathedral Valley Loop Road about 36 miles (57.9 km) from the visitor center). This primitive, first-come, first-served, no-fee campground has six sites, each with a picnic table and fire grate. There is a pit toilet, but no water available. The campground is open year-round; however, visitors should check road conditions with the Capitol Reef Visitor Center prior to planning an overnight stay. The campground is at ~7,000 feet (2,133 m) in elevation. Free. (updated Jun 2020)
Cedar Mesa Campground (approximately 23 miles (37.0 km) south of Utah State Highway 24 on the Notom-Bullfrog Road). This primitive, first-come, first-served, no-fee campground has five sites, each with a picnic table and fire grate. There is also a pit toilet, but no water is available. The campground is open year-round, but visitors should check with the Capitol Reef Visitor Center for road conditions prior to planning an overnight stay. It is located at 5,500 feet (1,676 m) in elevation. Free. (updated Jun 2020)
It is recommended to camp at least 1/2 mile away from an established trail or road. Open fires are not allowed. Cooking must be done with a portable stove. A free backcountry permit must be acquired from the visitor center. Rangers at the visitor center can also help plan a trip and recommend favorite camping spots.
Flash floods can occur in the park without warning. The danger is especially high when walking in narrow slot canyons such as Grand Wash. Although rainstorms in the park are beautiful, it's not a safe time to be on the trails. Flood waters originate upstream, so a flood may occur from a storm that is miles away. If you are in a narrow canyon and the water begins to rise even slightly or the wash begins to get muddy, begin looking for higher ground.
Heading west out of the park and about 40 miles south on the incredibly scenic Highway 12 will take you to the town of Boulder, Utah, home of Anasazi State Park which details the historic Native American tribes of Southern Utah. Travelling another 60 miles south on Hwy 12 will bring you to Bryce Canyon National Park.
Heading East on Hwy 24 and South on Hwy 95, (about 80 miles) will bring you to Glen Canyon National Recreation Area. Alternately, the adventurous can reach Bullfrog marina in Glen Canyon NRA by driving south on the unimproved Notom Road, but check road conditions at the Visitor Center.
Travelling east on Hwy 24 and North on Hwy 95 about 55 miles will bring you to the turn off to Goblin Valley State Park.
[edit] Park map Capitol Reef encompasses the Waterpocket Fold, a warp in the Earth's crust that is 65 million years old. It is the largest exposed monocline in North America. In this fold, newer and older layers of earth folded over each other in an S-shape. This warp, probably caused by the same colliding continental plates that created the Rocky Mountains, has weathered and eroded over millennia to expose layers of rock and fossils. The park is filled with brilliantly colored sandstone cliffs, gleaming white domes, and contrasting layers of stone and earth. The area was named for a line of white domes and cliffs of Navajo Sandstone, each of which looks somewhat like the United States Capitol building, that run from the Fremont River to Pleasant Creek on the Waterpocket Fold. The fold forms a north-to-south barrier that has barely been breached by roads. Early settlers referred to parallel impassable ridges as "reefs", from which the park gets the second half of its name. The first paved road through the area was constructed in 1962. State Route 24 cuts through the park traveling east-and-west between Canyonlands National Park and Bryce Canyon National Park, but few other paved roads exist in the rugged landscape. The park is filled with canyons, cliffs, towers, domes, and arches. The Fremont River has cut canyons through parts of the Waterpocket Fold, but most of the park is arid desert.
[edit] Native Americans and Mormons[edit] Petroglyph in Capitol Gorge Fremont-culture Native Americans lived near the perennial Fremont River in the northern part of the Capitol Reef Waterpocket Fold around the year 1000. They irrigated crops of maize and squash and stored their grain in stone granaries (in part made from the numerous black basalt boulders that litter the area). In the 13th century, all of the Native American cultures in this area underwent sudden change, likely due to a long drought. The Fremont settlements and fields were abandoned. Many years after the Fremont left, Paiutes moved into the area. These Numic-speaking people named the Fremont granaries moki huts and thought they were the homes of a race of tiny people or moki. In 1872 Almon H. Thompson, a geographer attached to United States Army Major John Wesley Powell's expedition, crossed the Waterpocket Fold while exploring the area. Geologist Clarence Dutton later spent several summers studying the area's geology. None of these expeditions explored the Waterpocket Fold to any great extent. Following the American Civil War, officials of the Church of Jesus Christ of Latter-day Saints in Salt Lake City sought to establish missions in the remotest niches of the Intermountain West. In 1866, a quasi-military expedition of Mormons in pursuit of natives penetrated the high valleys to the west. In the 1870s, settlers moved into these valleys, eventually establishing Loa, Fremont, Lyman, Bicknell, and Torrey. Fruita School House Mormons settled the Fremont River valley in the 1880s and established Junction (later renamed Fruita), Caineville, and Aldridge. Fruita prospered, Caineville barely survived, and Aldridge died. In addition to farming, lime was extracted from local limestone, and uranium was extracted early in the 20th century. In 1904, the first claim to a uranium mine in the area was staked. The resulting Oyler Mine in Grand Wash produced uranium ore. By 1920 no more than ten families at one time were sustained by the fertile flood plain of the Fremont River, and the land changed ownership over the years. The area remained isolated. The community was later abandoned, and later still some buildings were restored by the National Park Service. Kilns once used to produce lime still exist in Sulphur Creek and near the campgrounds on Scenic Drive. Early protection efforts[edit] Local Ephraim Portman Pectol organized a "booster club" in Torrey in 1921. Pectol pressed a promotional campaign, furnishing stories to be sent to periodicals and newspapers. In his efforts, he was increasingly aided by his brother-in-law, Joseph S. Hickman, who was the Wayne County High School principal. In 1924, Hickman extended community involvement in the promotional effort by organizing a Wayne County–wide Wayne Wonderland Club. That same year, Hickman was elected to the Utah State Legislature. In 1933, Pectol was elected to the presidency of the Associated Civics Club of Southern Utah, successor to the Wayne Wonderland Club. The club raised $150 (equivalent to $3,731 in 2025) to interest a Salt Lake City photographer in taking a series of promotional photographs. For several years, the photographer, J. E. Broaddus, traveled and lectured on "Wayne Wonderland". In 1933, Pectol was elected to the legislature and almost immediately contacted President Franklin D. Roosevelt and asked for the creation of "Wayne Wonderland National Monument" out of the federal lands comprising the bulk of the Capitol Reef area. Federal agencies began a feasibility study and boundary assessment. Meanwhile, Pectol guided the government investigators on numerous trips and escorted an increasing number of visitors. The lectures of Broaddus were having an effect. Capitol Gorge Roosevelt signed a proclamation creating Capitol Reef National Monument on August 2, 1937. In Proclamation 2246, President Roosevelt set aside 37,711 acres (15,261 ha) of the Capitol Reef area. This comprised an area extending about two miles (3 km) north of present State Route 24 and about 10 mi (16 km) south, just past Capitol Gorge. The Great Depression years were lean ones for the National Park Service (NPS), the new administering agency. Funds for the administration of Capitol Reef were nonexistent; it was a long time before the first rangers arrived. Administration of the monument[edit] Administration of the new monument was placed under the control of Zion National Park. A stone ranger cabin and the Sulphur Creek bridge were built and some road work was performed by the Civilian Conservation Corps and the Works Progress Administration. Historian and printer Charles Kelly came to know NPS officials at Zion well and volunteered to watchdog the park for the NPS. Kelly was officially appointed custodian-without-pay in 1943. He worked as a volunteer until 1950, when the NPS offered him a civil-service appointment as the first superintendent. During the 1950s, Kelly was deeply troubled by NPS management acceding to demands of the U.S. Atomic Energy Commission that Capitol Reef National Monument be opened to uranium prospecting. He felt that the decision had been a mistake and destructive of the long-term national interest. It turned out that there was not enough ore in the monument to be worth mining. In 1958, Kelly got additional permanent help in protecting the monument and enforcing regulations; Park Ranger Grant Clark transferred from Zion. The year Clark arrived, fifty-six thousand visitors came to the park, and Charlie Kelly retired for the last time. During the 1960s (under the program name Mission 66), NPS areas nationwide received new facilities to meet the demand of mushrooming park visitation. At Capitol Reef, a 53-site campground at Fruita, staff rental housing, and a new visitor center were built, the latter opening in 1966. Visitation climbed dramatically after the paved, all-weather State Route 24 was built in 1962 through the Fremont River canyon near Fruita. State Route 24 replaced the narrow Capitol Gorge wagon road about 10 miles (16 km) to the south that frequently washed out. The old road has since been open only to foot traffic. In 1967, 146,598 persons visited the park. The staff was also growing. During the 1960s, the NPS purchased private land parcels at Fruita and Pleasant Creek. Almost all private property passed into public ownership on a "willing buyer-willing seller" basis. Preservationists convinced President Lyndon B. Johnson to set aside an enormous area of public lands in 1968, just before he left office. In Presidential Proclamation 3888, an additional 215,056 acres (87,030 ha) were placed under NPS control. By 1970, Capitol Reef National Monument comprised 254,251 acres (102,892 ha) and sprawled southeast from Thousand Lake Mountain almost to the Colorado River. The action was controversial locally, and NPS staffing at the monument was inadequate to properly manage the additional land. National park status[edit] Navajo Dome formation Tower and rock layers at Capitol Reef One of the Twin Rocks in Capitol Reef National Park. The vast enlargement of the monument and diversification of the scenic resources soon raised another issue: whether Capitol Reef should be a national park, rather than a monument. Two bills were introduced into the United States Congress. A House bill (H.R. 17152) introduced by Utah Congressman Laurence J. Burton called for a 180,000-acre (72,800 ha) national park and an adjunct 48,000-acre (19,400 ha) national recreation area where multiple use (including grazing) could continue indefinitely. In the United States Senate, meanwhile, Senate bill S. 531 had already passed on July 1, 1970, and provided for a 230,000-acre (93,100 ha) national park alone. The bill called for a 25-year phase-out of grazing. In September 1970, United States Department of Interior officials told a house subcommittee session that they preferred about 254,000 acres (103,000 ha) be set aside as a national park. They also recommended that the grazing phase-out period be 10 years, rather than 25. They did not favor the adjunct recreation area. It was not until late 1971 that Congressional action was completed. By then, the 92nd United States Congress was in session and S. 531 had languished. A new bill, S. 29, was introduced in the Senate by Senator Frank E. Moss of Utah and was essentially the same as the defunct S. 531 except that it called for an additional 10,834 acres (4,384 ha) of public lands for a Capitol Reef National Park. In the House, Utah Representative K. Gunn McKay (with Representative Lloyd) had introduced H.R. 9053 to replace the dead H.R. 17152. This time, the House bill dropped the concept of an adjunct Capitol Reef National Recreation Area and adopted the Senate concept of a 25-year limit on continued grazing. The Department of Interior was still recommending a national park of 254,368 acres (102,939 ha) and a 10-year limit for grazing phase-out. S. 29 passed the Senate in June and was sent to the House, which dropped its own bill and passed the Senate version with an amendment. Because the Senate was not in agreement with the House amendment, differences were worked out in Conference Committee. The Conference Committee issued its report on November 30, 1971, and the bill passed both houses of Congress. The legislation—"An Act to Establish The Capitol Reef National Park in the State of Utah"—became Public Law 92-207 when it was signed by President Richard Nixon on December 18, 1971.
[edit] The Milky Way at Capitol ReefIn April 2015, Capitol Reef National Park was designated a "Gold Tier" Dark Sky Park due to its remote location and minimal use of artificial lighting.
[edit] According to the Köppen climate classification system, the Capitol Reef Visitor Center has a cold semi-arid climate (BSk). Climate data for Capitol Reef National Park, Utah, 1991–2020 normals, extremes 1938–present Month Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec Year Record high °F (°C) 69(21) 72(22) 80(27) 91(33) 97(36) 104(40) 104(40) 102(39) 99(37) 91(33) 77(25) 69(21) 104(40) Mean maximum °F (°C) 54.1(12.3) 59.7(15.4) 71.8(22.1) 80.3(26.8) 87.9(31.1) 97.0(36.1) 99.2(37.3) 96.0(35.6) 91.0(32.8) 81.6(27.6) 65.3(18.5) 55.0(12.8) 99.7(37.6) Mean daily maximum °F (°C) 40.6(4.8) 46.8(8.2) 57.3(14.1) 64.7(18.2) 74.3(23.5) 86.4(30.2) 91.2(32.9) 87.8(31.0) 79.7(26.5) 65.9(18.8) 51.0(10.6) 40.2(4.6) 65.5(18.6) Daily mean °F (°C) 30.5(−0.8) 36.2(2.3) 45.4(7.4) 51.9(11.1) 61.3(16.3) 72.3(22.4) 78.2(25.7) 75.3(24.1) 67.2(19.6) 54.5(12.5) 40.7(4.8) 30.4(−0.9) 53.7(12.1) Mean daily minimum °F (°C) 20.5(−6.4) 25.7(−3.5) 33.6(0.9) 39.2(4.0) 48.3(9.1) 58.2(14.6) 65.2(18.4) 62.8(17.1) 54.7(12.6) 43.1(6.2) 30.4(−0.9) 20.6(−6.3) 41.9(5.5) Mean minimum °F (°C) 8.6(−13.0) 14.3(−9.8) 22.5(−5.3) 28.5(−1.9) 36.2(2.3) 46.4(8.0) 56.9(13.8) 55.5(13.1) 43.1(6.2) 30.0(−1.1) 18.4(−7.6) 10.2(−12.1) 6.8(−14.0) Record low °F (°C) −9(−23) −7(−22) 10(−12) 18(−8) 28(−2) 35(2) 44(7) 42(6) 30(−1) 12(−11) 5(−15) −8(−22) −9(−23) Average precipitation inches (mm) 0.56(14) 0.50(13) 0.46(12) 0.52(13) 0.65(17) 0.35(8.9) 1.03(26) 1.12(28) 0.95(24) 0.87(22) 0.50(13) 0.37(9.4) 7.88(200) Average snowfall inches (cm) 3.8(9.7) 1.5(3.8) 1.7(4.3) 0.2(0.51) 0.0(0.0) 0.0(0.0) 0.0(0.0) 0.0(0.0) 0.0(0.0) 0.0(0.0) 1.5(3.8) 2.2(5.6) 10.9(28) Average precipitation days (≥ 0.01 in) 3.3 3.7 3.6 4.5 4.9 3.3 7.7 8.1 5.3 4.5 2.7 2.9 54.5 Average snowy days (≥ 0.1 in) 1.9 1.3 0.8 0.3 0.1 0.0 0.0 0.0 0.0 0.0 0.7 1.8 6.9 Source: NOAA
[edit] Main article: Geology of the Capitol Reef area Waterpocket Fold from the ISS The area including the park was once the edge of a shallow sea that invaded the land in the Permian, creating the Cutler Formation. Only the sandstone of the youngest member of the Cutler Formation, the White Rim, is exposed in the park. The deepening sea left carbonate deposits, forming the Kaibab Limestone, the same formation that rims the Grand Canyon to the southwest. During the Triassic, streams deposited reddish-brown silt that later became the siltstone of the Moenkopi Formation. Uplift and erosion followed. Conglomerate, followed by logs, sand, mud, and wind-transported volcanic ash, then formed the uranium-containing Chinle Formation. The members of the Glen Canyon Group were all laid down in the middle- to late-Triassic during a time of increasing aridity. They include: Wingate Sandstone: sand dunes on the shore of an ancient sea Kayenta Formation: thin-bedded layers of sand deposited by slow-moving streams in channels and across low plains Navajo Sandstone: huge fossilized sand dunes from a massive Sahara-like desert. The Golden Throne. Though Capitol Reef is famous for white domes of Navajo Sandstone, this dome's color is a result of a lingering section of yellow Carmel Formation carbonate, which has stained the underlying rock. The San Rafael Group consists of four Jurassic-period formations; from oldest to youngest, they are: the Carmel Formation: gypsum, sand, and limey silt laid down in what may have been a graben that was periodically flooded by sea water; the Entrada Sandstone: sandstone from barrier islands/sand bars in a near-shore environment; the Curtis Formation: made from conglomerate, sandstone, and shale; and the Summerville Formation: reddish-brown mud and white sand deposited in tidal flats. Streams once again laid down mud and sand in their channels, on lakebeds, and in swampy plains, creating the Morrison Formation. Early in the Cretaceous, similar non-marine sediments were laid down and became the Dakota Sandstone. Eventually, the Cretaceous Seaway covered the Dakota, depositing the Mancos Shale. Only small remnants of the Mesaverde Group are found, capping a few mesas in the park's eastern section. Near the end of the Cretaceous period, a mountain-building event called the Laramide orogeny started to compact and uplift the region, forming the Rocky Mountains and creating monoclines such as the Waterpocket Fold in the park. Ten to fifteen million years ago, the entire region was uplifted much further by the creation of the Colorado Plateau. This uplift was very even. Igneous activity in the form of volcanism and dike and sill intrusion also occurred during this time. The drainage system in the area was rearranged and steepened, causing streams to downcut faster and sometimes change course. Wetter times during the ice ages of the Pleistocene increased the rate of erosion.
[edit] There are more than 840 species of plants that are found in the park, and over 40 of those species are classified as rare and endemic.
[edit] The closest town to Capitol Reef is Torrey, about 11 miles (18 km) west of the visitor center on Highway 24, slightly west of its intersection with Highway 12. Its 2020 population was less than 300. Torrey has a few motels and restaurants and functions as a gateway town to the park. Highway 12 and a partially unpaved scenic backway named the Burr Trail provide access from the west through the Grand Staircase–Escalante National Monument and the town of Boulder.
[edit] A variety of activities are available to tourists, both ranger-led and self-guided, including auto touring, hiking, backpacking, camping, bicycling (on paved and unpaved roads only; no trails), horseback riding, canyoneering, and rock climbing. The orchards planted by Mormon pioneers are maintained by the National Park Service. From early March to mid-October, various fruit—cherries, apricots, peaches, pears, or apples—can be harvested by visitors for a fee. Hiking and backpacking[edit] A hiking-trail guide is available at the visitor center for both day hikes and backcountry hiking. Backcountry access requires a free permit. Hickman Natural Bridge Numerous trails are available for hiking and backpacking in the park, with fifteen in the Fruita District alone. The following trails are some of the most popular in the park: Cassidy Arch Trail: a very steep, strenuous, 3.5-mile (5.6 km) round trip that leads into the Grand Wash to an overlook of the Cassidy Arch. Grand Wash Trail: a popular easy trail providing access to the Narrows area of the wash. Accessible both from Rt. 24 and from the end of Grand Wash Road, off of the Scenic Drive. Hickman Bridge Trail: a 2-mile (3.2 km) round trip leading to the natural bridge. Frying Pan Trail: an 8.8-mile (14.2 km) round trip that passes the Cassidy Arch, Grand Wash, and Cohab Canyon. Brimhall Natural Bridge: a popular, though strenuous, 4.5-mile (7.2 km) round trip with views of Brimhall Canyon, the Waterpocket Fold, and Brimhall Natural Bridge. Halls Creek Narrows: 22 miles (35 km) long and considered strenuous, with many side canyons and creeks; typically hiked as a 2-3 day camping trip. Auto touring[edit] Visitors may explore several of the main areas of the park by private vehicle: Scenic Drive: a 7.9-mile (12.7 km) paved road winds through the middle of the park, passing the major points of interest; the road is accessible from the visitor center to approximately 2 miles (3.2 km) into the Capitol Gorge. Notom-Bullfrog Road: traverses the eastern side of the Waterpocket Fold, along 10 miles (16 km) of paved road, with the remainder unpaved. Cathedral Road: an unpaved road through the northern areas of the park, that traverses Cathedral Valley, passing the Temples of the Sun and Moon. Camping[edit] The primary camping location is the Fruita campground, with 71 campsites (no water, electrical, or sewer hookups), and restrooms without bathing facilities. The campground also has group sites with picnic areas and restrooms. Two primitive, free camping areas are also available. Canyoneering[edit] Taken from the top of the first rappel of the Cassidy Arch route. Canyoneering is growing in popularity in the park. It is a recreational sport that takes one through slot canyons. It involves rappelling and may require swimming and other technical rope work. Day-pass permits are required for canyoneering in the park and can be obtained for free from the visitor center or through email. Each route requires its own permit. If one is planning on canyoneering for multiple days, then passes are required for each day. Overnight camping as part of the canyoneering trip is permitted, but a free backcountry pass must be requested from the visitor center. It is imperative to plan canyoneering trips around the weather. The Colorado Plateau is susceptible to flash flooding during prime rainy months. Because canyoneering takes place through slot canyons, getting caught in a flash flood could be lethal. Visitors are advised to consult reliable weather sources. The Weather Atlas shows charts with the monthly average rainfall in inches. Extreme heat during the summer months presents a danger to visitors, who can find weather warnings on the National Weather Service website. The heat levels are detailed by a color and numerical scale (0–4). One of the most popular canyoneering routes in Capitol Reef National Park is Cassidy Arch Canyon. A paper by George Huddart details the park's commitment to working with citizens to maintain the route as well as the vegetation and rocks. The canyon route is approximately 2.3 miles (3.7 km) long (0.4 miles (0.64 km) of technical work), consisting of 8 different rappels, and takes between 2.5 and 4.5 hours to complete. The first rappel is 140 feet (43 m) and descends below the famous Cassidy Arch.