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How to Book a Hotel in Zion

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When a hotel search in Zion is done, please select the room type, the included meals and the suitable booking conditions (for example, "Deluxe double room, Breakfast included, Non-Refundable"). Press the "View Deal" ("Book Now") button. Make your booking on a hotel booking website and get the hotel reservation voucher by email. That's it, a perfect hotel in Zion is waiting for you!

Hotels of Zion

A hotel in Zion is an establishment that provides lodging paid on a short-term basis. Facilities provided may range from a basic bed and storage for clothing, to luxury features like en-suite bathrooms. Larger in Zion hotels may provide additional guest facilities such as a swimming pool, business centre, childcare, conference facilities and social function services. Hotel rooms in Zion are usually numbered (or named in some smaller hotels and B&Bs) to allow guests to identify their room. Some Zion hotels offer meals as part of a room and board arrangement. Hotel operations vary in size, function, and cost. Most Zion hotels and major hospitality companies that operate hotels in Zion have set widely accepted industry standards to classify hotel types. General categories include the following:

Upscale luxury hotels in Zion
An upscale full service hotel facility in Zion that offers luxury amenities, full service accommodations, on-site full service restaurant(s), and the highest level of personalized and professional service. Luxury Zion hotels are normally classified with at least a Four Diamond or Five Diamond status or a Four or Five Star rating depending on classification standards.

Full service hotels in Zion
Full service Zion hotels often contain upscale full-service facilities with a large volume of full service accommodations, on-site full service restaurant(s), and a variety of on-site amenities such as swimming pools, a health club, children's activities, ballrooms, on-site conference facilities, etc.

Historic inns and boutique hotels in Zion
Boutique hotels of Zion are smaller independent non-branded hotels that often contain upscale facilities of varying size in unique or intimate settings with full service accommodations. Zion boutique hotels are generally 100 rooms or less. Some historic inns and boutique hotels in Zion may be classified as luxury hotels.

Focused or select service hotels in Zion
Small to medium-sized hotel establishments that offer a limited amount of on-site amenities that only cater and market to a specific demographic of Zion travelers, such as the single business traveler. Most Zion focused or select service hotels may still offer full service accommodations but may lack leisure amenities such as an on-site restaurant or a swimming pool.

Economy and limited service hotels in Zion
Small to medium-sized Zion hotel establishments that offer a very limited amount of on-site amenities and often only offer basic accommodations with little to no services, these facilities normally only cater and market to a specific demographic of travelers, such as the budget-minded Zion traveler seeking a "no frills" accommodation. Limited service Zion hotels often lack an on-site restaurant but in return may offer a limited complimentary food and beverage amenity such as on-site continental breakfast service.

Guest houses and B&Bs in Zion
A bed and breakfast in Zion is a small lodging establishment that offers overnight accommodation and inclusive breakfast. Usually, Zion bed and breakfasts are private homes or family homes offering accommodations. The typical Zion B&B has between 4 and 11 rooms, with 6 being the average. Generally, guests are accommodated in private bedrooms with private bathrooms, or in a suite of rooms including an en suite bathroom. Some homes have private bedrooms with a bathroom which is shared with other guests. Breakfast is served in the bedroom, a dining room, or the host's kitchen. Often the owners of guest house themselves prepare the breakfast and clean the rooms.

Hostels in Zion
Zion hostels provide budget-oriented, sociable accommodation where guests can rent a bed, usually a bunk bed, in a dormitory and share a bathroom, lounge, and sometimes a kitchen. Rooms can be mixed or single-sex, although private rooms may also be available. Hostels are often cheaper for both the operator and occupants; many Zion hostels have long-term residents whom they employ as desk agents or housekeeping staff in exchange for experience or discounted accommodation.

Apartment hotels, extended stay hotels in Zion
Extended stay hotels are small to medium-sized Zion hotels that offer longer term full service accommodations compared to a traditional hotel. Extended stay hotels may offer non-traditional pricing methods such as a weekly rate that cater towards travelers in need of short-term accommodations for an extended period of time. Similar to limited and select service hotels, on-site amenities are normally limited and most extended stay hotels in Zion lack an on-site restaurant.

Timeshare and destination clubs in Zion
Zion timeshare and destination clubs are a form of property ownership also referred to as a vacation ownership involving the purchase and ownership of an individual unit of accommodation for seasonal usage during a specified period of time. Timeshare resorts in Zion often offer amenities similar that of a Full service hotel with on-site restaurant(s), swimming pools, recreation grounds, and other leisure-oriented amenities. Destination clubs of Zion on the other hand may offer more exclusive private accommodations such as private houses in a neighborhood-style setting.

Motels in Zion
A Zion motel is a small-sized low-rise lodging establishment similar to that of a limited service hotel, but with direct access to individual rooms from the car park. Common during the 1950s and 1960s, motels were often located adjacent to a major road, where they were built on inexpensive land at the edge of towns or along stretches of highways. They are still useful in less populated areas of Zion for driving travelers, but the more populated an area becomes the more hotels fill the need. Many of Zion motels which remain in operation have joined national franchise chains, rebranding themselves as hotels, inns or lodges.

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Travelling and vacation in Zion

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Zion National Park
IUCN category II (national park)
Map showing the location of Zion National Park
Location Washington, Kane, and Iron counties, Utah
United States
Nearest city Springdale (south), Orderville, Utah (east) and Cedar City near Kolob Canyons entrance
Coordinates  / 37.20262; -112.98785  / 37.20262; -112.98785
Area 146,597 acres (229.058 sq mi; 59,326 ha; 593.26 km)
Established November 19, 1919
Visitors 4,295,128 (in 2016)
Governing body National Park Service
Website www.nps.gov/zion
Zion Canyon as seen from the top of Angels Landing at sunset

Zion National Park is located in the Southwestern United States, near Springdale, Utah. A prominent feature of the 229-square-mile (590 km) park is Zion Canyon, which is 15 miles (24 km) long and up to half a mile (800 m) deep, cut through the reddish and tan-colored Navajo Sandstone by the North Fork of the Virgin River. The lowest elevation is 3,666 ft (1,117 m) at Coalpits Wash and the highest elevation is 8,726 ft (2,660 m) at Horse Ranch Mountain. Located at the junction of the Colorado Plateau, Great Basin, and Mojave Desert regions, the park's unique geography and variety of life zones allow for unusual plant and animal diversity. Numerous plant species as well as 289 species of birds, 75 mammals (including 19 species of bat), and 32 reptiles inhabit the park's four life zones: desert, riparian, woodland, and coniferous forest. Zion National Park includes mountains, canyons, buttes, mesas, monoliths, rivers, slot canyons, and natural arches.

Human habitation of the area started about 8,000 years ago with small family groups of Native Americans; the semi-nomadic Basketmaker Anasazi (300 CE) stem from one of these groups. In turn, the Virgin Anasazi culture (500 CE) developed as the Basketmakers settled in permanent communities. A different group, the Parowan Fremont, lived in the area as well. Both groups moved away by 1300 and were replaced by the Parrusits and several other Southern Paiute subtribes. Mormons came into the area in 1858 and settled there in the early 1860s. In 1909 the President of the United States, William Howard Taft, named the area a National Monument to protect the canyon, under the name of Mukuntuweap National Monument. In 1918, however, the acting director of the newly created National Park Service changed the park's name to Zion, the name used by the Mormons. According to historian Hal Rothman: "The name change played to a prevalent bias of the time. Many believed that Spanish and Indian names would deter visitors who, if they could not pronounce the name of a place, might not bother to visit it. The new name, Zion, had greater appeal to an ethnocentric audience." The United States Congress established the monument as a National Park on November 19, 1919. The Kolob section was proclaimed a separate Zion National Monument in 1937, but was incorporated into the park in 1956.

The geology of the Zion and Kolob canyons area includes nine formations that together represent 150 million years of mostly Mesozoic-aged sedimentation. At various periods in that time warm, shallow seas, streams, ponds and lakes, vast deserts, and dry near-shore environments covered the area. Uplift associated with the creation of the Colorado Plateaus lifted the region 10,000 feet (3,000 m) starting 13 million years ago.

Zion Canyon near the park entrance

Zion National Park: Geography and climate

The park is located in southwestern Utah in Washington, Iron and Kane counties. Geomorphically, it is located on the Markagunt and Kolob plateaus, at the intersection of three North American geographic provinces: the Colorado Plateaus, the Great Basin, and the Mojave Desert. The northern part of the park is known as the Kolob Canyons section and is accessible from Interstate 15, exit 40.

The 8,726-foot (2,660 m) summit of Horse Ranch Mountain (photo) is the highest point in the park; the lowest point is the 3,666-foot (1,117 m) elevation of Coal Pits Wash, creating a relief of about 5,100 feet (1,600 m).

Streams in the area take rectangular paths because they follow jointing planes in the rocks. The stream gradient of the Virgin River, whose North Fork flows through Zion Canyon in the park, ranges from 50 to 80 feet per mile (9.5 to 15.2 m/km) (0.9–1.5%)-one of the steepest stream gradients in North America.

"Temples and Towers of the Virgin"

The road into Zion Canyon is 6 miles (9.7 km) long, ending at the Temple of Sinawava ("Sinawava" refers to the Coyote God of the Paiute Indians). At the Temple the canyon narrows and a foot-trail continues to the mouth of the Zion Narrows, a gorge as narrow as 20 feet (6 m) wide and up to 2,000 feet (610 m) tall. The Zion Canyon road is served by a free shuttle bus from early April to late October and by private vehicles the other months of the year. Other roads in Zion are open to private vehicles year-round.

The east side of the park is served by Zion-Mount Carmel Highway (SR-9), which passes through the Zion–Mount Carmel Tunnel and ends at Mount Carmel. On the east side of the park, notable park features include Checkerboard Mesa (photo) and the East Temple.

The Kolob Terrace area, west of Zion Canyon features The Subway, a slot canyon hike, and Lava Point, with a panoramic view of the entire area. The Kolob Canyons section, further west near Cedar City, features the world's second longest arch, Kolob Arch.

Zion rock formation, photo c. 1941 by Ansel Adams

Spring weather is unpredictable, with stormy, wet days being common, mixed with occasional warm, sunny weather. Precipitation is normally heaviest in March. Spring wildflowers bloom from April through June, peaking in May. Fall days are usually clear and mild; nights are often cool. Summer days are hot (95 to 110 °F; 35 to 43 °C), but overnight lows are usually comfortable (65 to 70 °F; 18 to 21 °C). Afternoon thunderstorms are common from mid-July through mid-September. Storms may produce waterfalls as well as flash floods. Autumn tree-color displays begin in September in the high country; in Zion Canyon, autumn colors usually peak in late October. Winter in Zion Canyon is fairly mild. Winter storms bring rain or light snow to Zion Canyon and heavier snow to the higher elevations. Clear days may become quite warm, reaching 60 °F (16 °C); nights are often 20 to 40 °F (−7 to 4 °C). Winter storms can last several days and make roads icy. Zion roads are plowed, except the Kolob Terrace Road which is closed when covered with snow. Winter driving conditions last from November through March.

Notable geographical features of the park include: Virgin River Narrows, Emerald Pools, Hidden Canyon (photo), Angels Landing (photo), The Great White Throne, Checkerboard Mesa (photo), The Three Patriarchs (photo) and Kolob Arch.

Zion National Park: History

Archaeologists have divided the long span of Zion's human history into three cultural periods: the Archaic, Protohistoric and Historic periods. Each period is characterized by distinctive technological and social adaptations.

Zion National Park: Archaic period

The first human presence in the region dates to 8,000 years ago when family groups camped where they could hunt or collect plants and seeds. About 2,000 years ago, some groups began growing corn and other crops, leading to an increasingly sedentary lifestyle. Later groups in this period built permanent villages called pueblos. Archaeologists call this the Archaic period and it lasted until about 500 CE. Baskets, cordage nets, and yucca fiber sandals have been found and dated to this period. The Archaic toolkits included flaked stone knives, drills, and stemmed dart points. The dart points were attached to wooden shafts and propelled by throwing devices called atlatls.

By 300 CE some of the archaic groups developed into an early branch of seminomadic Anasazi, the Basketmakers. Basketmaker sites have grass- or stone-lined storage cists and shallow, partially underground dwellings called pithouses. They were hunters and gatherers who supplemented their diet with limited agriculture. Locally collected pine nuts were important for food and trade.

Zion National Park: Protohistoric period

Kaun huts were used by Southern Paiute

Both the Virgin Anasazi and the Parowan Fremont disappear from the archaeological record of southwestern Utah by about 1300. Extended droughts in the 11th and 12th centuries, interspersed with catastrophic flooding, may have made horticulture impossible in this arid region.

Tradition and archaeological evidence hold that their replacements were Numic-speaking cousins of the Virgin Anasazi, such as the Southern Paiute and Ute. The newcomers migrated on a seasonal basis up and down valleys in search of wild seeds and game animals. Some, particularly the Southern Paiute, also planted fields of corn, sunflowers, and squash to supplement their diet. These more sedentary groups made brownware vessels that were used for storage and cooking.

Zion National Park: Exploration and settlement by Euro-Americans

The Historic period begins in the late 18th century with the exploration of southern Utah by Padres Silvestre Vélez de Escalante and Francisco Atanasio Domínguez. The padres passed near what is now the Kolob Canyons Visitor Center on October 13, 1776, becoming the first people of European descent known to visit the area. In 1825, trapper and trader Jedediah Smith explored some of the downstream areas while under contract with the American Fur Company.

In 1847, Mormon farmers from the Salt Lake area became the first people of European descent to settle the Virgin River region. In 1851, the Parowan and Cedar City, Utah areas were settled by Mormons who used the Kolob Canyons area for timber, and for grazing cattle, sheep, and horses. They prospected for mineral deposits, and diverted Kolob water to irrigate crops in the valley below. Mormon settlers named the area Kolob-in Mormon scripture, the heavenly place nearest the residence of God.

A ranch located near the mouth of Zion Canyon

Settlements had expanded 30 miles (48 km) south to the lower Virgin River by 1858. That year, a Southern Paiute guide led young Mormon missionary and interpreter Nephi Johnson into the upper Virgin River area and Zion Canyon. Johnson wrote a favorable report about the agricultural potential of the upper Virgin River basin, and returned later that year to found the town of Virgin. In 1861 or 1862, Joseph Black made the arduous journey to Zion Canyon and was very impressed by its beauty.

The floor of Zion Canyon was settled in 1863 by Isaac Behunin, who farmed corn, tobacco, and fruit trees. The Behunin family lived in Zion Canyon near the site of today's Zion Lodge during the summer, and wintered in Springdale. Behunin is credited with naming Zion, a reference to a place of peace mentioned in the Bible. Two more families settled Zion Canyon in the next couple of years, bringing with them cattle and other domesticated animals. The canyon floor was farmed until Zion became a Monument in 1909.

The Powell Geographic Expedition entered the area in 1869 after their first trip through the Grand Canyon. John Wesley Powell visited Zion Canyon in 1872 and named it Mukuntuweap, under the impression that that was the Paiute name. Powell Survey photographers John K. Hillers and James Fennemore first visited the Zion Canyon and Kolob Plateau region in the spring of 1872. Hillers returned in April 1873 to add more photographs to the "Virgin River Series" of photographs and stereographs. Hillers described wading the canyon for four days and nearly freezing to death to take his photographs.

Zion National Park: Protection and tourism

Painting of Zion Canyon by Frederick Dellenbaugh (1903)

Paintings of the canyon by Frederick S. Dellenbaugh were exhibited at the Saint Louis World's Fair in 1904, followed by a glowing article in Scribner's Magazine the next year. That, along with previously created photographs, paintings, and reports, led to President William Howard Taft's proclamation on July 31, 1909 that created Mukuntuweap National Monument. In 1917, the acting director of the newly created National Park Service visited the canyon and proposed changing its name from the locally unpopular Mukuntuweap to Zion, a name used by the local Mormon community. The United States Congress added more land and established Zion National Park on November 19, 1919. A separate Zion National Monument, the Kolob Canyons area, was proclaimed on January 22, 1937, and was incorporated into the park on July 11, 1956.

Travel to the area before it was a national park was rare due to its remote location, lack of accommodations, and the absence of real roads in southern Utah. Old wagon roads were upgraded to the first automobile roads starting about 1910, and the road into Zion Canyon was built in 1917 leading to the Grotto, short of the present road that now ends at the Temple of Sinawava.

1938 poster of Zion National Park

Touring cars could reach Zion Canyon by the summer of 1917. The first visitor lodging in Zion Canyon, called Wylie Camp, was established that same year as a tent camp. The Utah Parks Company, a subsidiary of the Union Pacific Railroad, acquired Wylie Camp in 1923, and offered ten-day rail/bus tours to Zion, nearby Bryce Canyon, Kaibab, and the North Rim of the Grand Canyon. The Zion Lodge complex was built in 1925 at the site of the Wylie tent camp. Architect Gilbert Stanley Underwood designed the Zion Lodge (photo) in the "Rustic Style" and the Utah Parks Company funded the construction.

Zion National Park: Infrastructure improvements

Main article: Historical buildings and structures of Zion National Park

Work on the Zion Mount Carmel Highway started in 1927 to enable reliable access between Springdale and the east side of the park. The road opened in 1930 and park visit and travel in the area greatly increased. The most famous feature of the Zion-Mount Carmel Highway is the 1.1-mile (1.8 km) Zion-Mount Carmel Tunnel, which has six large windows cut through the massive sandstone cliff.

In 1896, local rancher John Winder improved the Native American footpath up Echo Canyon, which later became the East Rim Trail. Entrepreneur David Flanigan used this trail in 1900 to build cableworks that lowered lumber into Zion Canyon from Cable Mountain. More than 200,000 board feet (470 m) of lumber were lowered by 1906. The auto road was extended to the Temple of Sinawava, and a trail built from there 1 mile (1.6 km) to the start of the Narrows. Angel's Landing Trail was constructed in 1926 and two suspension bridges were built over the Virgin River. Other trails were constructed by the Civilian Conservation Corps during the 1930s.

Zion National Park: More recent history

Zion Canyon from the trail to Observation Point

Zion Canyon Scenic Drive provides access to Zion Canyon. Traffic congestion in the narrow canyon was recognized as a major problem in the 1990s and a public transportation system using propane-powered shuttle buses was instituted in the year 2000. As part of its shuttle fleet, Zion has two electric trams each holding up to 36 passengers. Usually from early April through late October, the scenic drive in Zion Canyon is closed to private vehicles and visitors ride the shuttle buses.

On April 12, 1995, heavy rains triggered a landslide that blocked the Virgin River in Zion Canyon. Over a period of two hours, the river carved away part of the only exit road from the canyon, trapping 450 guests and employees at the Zion Lodge. A one-lane, temporary road was constructed within 24 hours to allow evacuation of the Lodge. A more stable - albeit temporary - road was completed on May 25, 1995 to allow summer visitors to access the canyon. This road was replaced with a permanent road during the first half of 1996.

The Zion–Mount Carmel Highway can be travelled year-round. Access for oversized vehicles requires a special permit, and is limited to daytime hours, as traffic through the tunnel must be one way to accommodate large vehicles. The 5-mile (8.0 km)-long Kolob Canyons Road was built to provide access to the Kolob Canyons section of the park. This road often closes in the winter.

In March 2009, President Barack Obama signed into law the Omnibus Public Land Management Act of 2009, which designated and further protected 124,406 acres (50,345 ha) of park land as the Zion Wilderness.

In September 2015, flooding trapped a party of seven in Keyhole Canyon, a slot canyon in the park. The flash flood killed all seven members of the group, whose remains were located after a search lasting several days.

Virgin River after a snowstorm

Zion National Park: Geology

Main article: Geology of the Zion and Kolob canyons area
The Three Patriarchs in Zion Canyon are made of Navajo Sandstone

The nine known exposed geologic formations in Zion National Park are part of a super-sequence of rock units called the Grand Staircase. Together, these formations represent about 150 million years of mostly Mesozoic-aged sedimentation in that part of North America. The formations exposed in the Zion area were deposited as sediment in very different environments:

  • The warm, shallow (sometimes advancing or retreating) sea of the Kaibab and Moenkopi formations;
  • Streams, ponds, and lakes of the Chinle, Moenave, and Kayenta formations;
  • The vast desert of the Navajo and Temple Cap formations; and
  • The dry near-shore environment of the Carmel Formation.
The Kolob Canyons are a set of finger canyons cut into the Kolob Plateau

Uplift affected the entire region, known as the Colorado Plateaus, by slowly raising these formations more than 10,000 feet (3,000 m) higher than where they were deposited. This steepened the stream gradient of the ancestral Virgin and other rivers on the plateau.

The faster-moving streams took advantage of uplift-created joints in the rocks. Eventually, all Cenozoic-aged formations were removed and gorges were cut into the plateaus. Zion Canyon was cut by the North Fork of the Virgin River in this way. During the later part of this process, lava flows and cinder cones covered parts of the area.

High water volume in wet seasons does most of the downcutting in the main canyon. These flood events are responsible for transporting most of the 3 million short tons (2.7 million metric tons) of rock and sediment that the Virgin River transports yearly. The Virgin cuts away its canyon faster than its tributaries can cut away their own streambeds, so tributaries end in waterfalls from hanging valleys where they meet the Virgin. The valley between the peaks of the Twin Brothers is a notable example of a hanging valley in the canyon.

Table of formations exposed in Zion National Park

Zion-Nationalpark-Gesteinsschichten.svg

Rock layer Appearance Location Deposition Rock type Photo
Dakota Formation Cliffs Top of Horse Ranch Mountain Streams Conglomerate and sandstone Dakota Sandstone
Carmel Formation Cliffs Mount Carmel Junction Shallow sea and coastal desert Limestone, sandstone and gypsum Carmel Formation
Temple Cap Formation Cliffs Top of West Temple Desert Sandstone Temple Cap Formation atop Navajo Sandstone
Navajo Sandstone Steep cliffs 1,600 to 2,200 ft (490 to 670 m)

thick; red lower layers are colored by iron oxides

Tall cliffs of Zion Canyon; highest exposure is West Temple. Cross-bedding shows well at Checkerboard Mesa (photo) Desert sand dunes covered 150,000 sq mi (390,000 km). Shifting winds during deposition created cross-bedding Sandstone Navajo Sandstone showing its two tones
Kayenta Formation Rocky slopes Throughout canyon Streams Siltstone and sandstone Kayenta Formation
Moenave Formation Slopes and ledges Lower red cliffs seen from Zion Human History Museum Streams and ponds Siltstone and sandstone Moenave Formation
Chinle Formation Purplish slopes Above Rockville Streams Shale, loose clay and conglomerate Chinle Formation
Moenkopi Formation Chocolate cliffs with white bands Rocky slopes from Virgin to Rockville Shallow sea Shale, siltstone, sandstone, mudstone, and limestone Moenkopi Formation
Kaibab Limestone Cliffs Hurricane Cliffs along I-15 near Kolob Canyons Shallow sea Limestone Hurricane Cliffs/Kaibab Limestone

Zion National Park: Biology

Taylor Creek with Horse Ranch Mountain in background. Desert, riparian, woodland, and coniferous forest habitats are all visible.

The Great Basin, Mojave Desert, and Colorado Plateau converge at Zion and the Kolob canyons. This, along with the varied topography of canyon–mesa country, differing soil types, and uneven water availability, provides diverse habitat for the equally diverse mix of plants and animals that live in the area. The park is home to 289 bird, 79 mammals, 28 reptiles, 7 fish, and 6 amphibian species. These organisms make their homes in one or more of four life zones found in the Park: desert, riparian, woodland, and coniferous forest.

Desert conditions persist on canyon bottoms and rocky ledges away from perennial streams. Sagebrush, prickly pear cactus, and rabbitbrush, along with sacred datura and Indian paintbrush, are common. Utah penstemon and golden aster can also be found. Milkvetch and prince's plume are found in pockets of selenium-rich soils.

Sacred datura grows on the canyon floor and blooms at night.

Common daytime animals include mule deer, rock squirrels, pinyon jays, and whiptail and collared lizards (photo). Desert cottontails, jackrabbits, and Merriam's kangaroo rats come out at night. Cougars, bobcats, coyotes, badgers, gray foxes, and ring-tail cats are the top predators.

Cooler conditions persist at mid-elevation slopes, from 3,900 to 5,500 feet (1,200 to 1,700 m). Stunted forests of pinyon pine and juniper coexist here with manzanita shrubs, cliffrose, serviceberry, scrub oak, and yucca. Stands of ponderosa pine, Gambel oak, manzanita and aspen populate the mesas and cliffs above 6,000 feet (1,800 m).

Desert bighorn sheep are often visible near the roadway in the park.

Golden eagles, red-tailed hawks, peregrine falcons, and white-throated swifts can be seen in the area.Desert bighorn sheep were reintroduced in the park in 1973. California condors were reintroduced in the Arizona Strip and in 2014 the first successful breeding of condors in the park was confirmed. Nineteen species of bat also live in the area.

Boxelder, Fremont cottonwood, maple, and willow dominate riparian plant communities. Animals such as bank beavers, flannel-mouth suckers, gnatcatchers, dippers, canyon wrens, the virgin spinedace, and water striders all make their homes in the riparian zones.

Zion National Park: Activities

Zion Canyon
Entrance to the Subway from the bottom

Guided horseback riding trips, nature walks, and evening programs are available from late March to early November. The Junior Ranger Program for ages 6 to 12 is active from Memorial Day to Labor Day at the Zion Nature Center. Rangers at the Zion Canyon Visitor Center and the smaller Kolob Canyons Visitor Center can help visitors plan their stay. A bookstore attached to the Zion Canyon Visitor Center, run by the Zion Natural History Association, offers books, maps, and souvenirs for sale, with proceeds benefiting the park. The Grotto in Zion Canyon, the Visitor Center, and the viewpoint at the end of Kolob Canyons Road have the only designated picnic sites.

Seven trails with round-trip times of half an hour (Weeping Rock) to 4 hours (Angels Landing) are found in Zion Canyon. Two popular trails, Taylor Creek (4 hours round trip) and Kolob Arch (8 hours round trip), are in the Kolob Canyons section of the park, near Cedar City. Hiking up into The Narrows from the Temple of Sinawava is popular in summer. However, hiking beyond Big Springs requires a permit. The entire Narrows from Chamberlain's Ranch is a 16-mile one way trip that typically takes 12 hours of strenuous hiking. A shorter alternative is to enter the Narrows via Orderville Canyon. Both Orderville and the full Narrows require a back country permit. Entrance to the Parunuweap Canyon section of the park downstream of Labyrinth Falls is prohibited. Other often-used backcountry trails include the West Rim and LaVerkin Creek. The more primitive sections of Zion include the Kolob Terrace and the Kolob Canyons.

The final ascent at the top of the Angels Landing Trail

Zion is a center for rock climbing, with short walls like Touchstone, Moonlight Buttress, Spaceshot, and Prodigal Son being very popular.

Lodging in the park is available at Zion Lodge, located halfway through Zion Canyon. Zion Lodge is open year-round and has motel units and cabins, as well as a restaurant, café, and gift shop, but rooms fill up fast. Three campgrounds are available: South and Watchman at the far southern side of the park, and a primitive site at Lava Point in the middle of the park off Kolob Terrace Road. Watchman is the only campground in the park that takes reservations. Lava Point has only primitive facilities and is usually open from June to October. Overnight camping in the backcountry requires permits.

Zion Canyon IMAX in Springdale offers many interesting documentaries about the natural history of Zion Canyon and the American Southwest.

Lodging, food, and entertainment are also offered on the east side of the park along the Zion–Mount Carmel Highway and in Mount Carmel Junction.

Adjacent to the park on the south is the town of Springdale, Utah, which offers services such as lodging, food, and entertainment.

Driving through the east side of Zion to U.S. Route 89 allows access to Bryce Canyon National Park in the north or to the north rim of the Grand Canyon in the south. Due to the narrowness of the Zion–Mount Carmel Tunnel, RVs and buses must obtain a special pass and can only drive through the tunnel during limited hours.

Zion National Park: See also

  • Angels Landing

Zion National Park: References

  • This article incorporates public domain material from websites or documents of the National Park Service.
  • This article incorporates public domain material from websites or documents of the United States Geological Survey.
  1. "Listing of acreage as of December 31, 2012". Land Resource Division, National Park Service. Retrieved March 31, 2013.
  2. "Zion-Mt. Carmel Highway and Tunnel". National Park Service. Retrieved March 31, 2013.
  3. "NPS Annual Recreation Visits Report". National Park Service. Retrieved February 8, 2017.
  4. , p. 45
  5. Rothman, Hal (1989). Preserving Different Pasts: The American National Monuments. University of Illinois Press. p. 99. ISBN 978-0-252-01548-9.
  6. , p. 43
  7. , How to get here
  8. , Accessibility
  9. , p. 33
  10. , p. 29
  11. Alexander, Charles P (January 1948). "Records and Descriptions of North American Crane-Flies (Diptera). Part VII. The Tipuloidea of Utah". American Midland Naturalist. The University of Notre Dame. 39 (1): 1–82. doi:10.2307/2421428. JSTOR 2421428.
  12. , Zion Narrows (archive Archived December 30, 2008, at the Wayback Machine.)
  13. , Freestanding Arches
  14. , Weather and Climate
  15. "UT Zion NP". National Oceanic and Atmospheric Administration. Retrieved November 3, 2013.
  16. "Zion National Park, Utah". Western Regional Climate Center. Retrieved 3 Nov 2013.
  17. , History and Culture
  18. , Archeology (archive Archived December 28, 2008, at the Wayback Machine.)
  19. , People
  20. , Human History (archive Archived December 30, 2008, at the Wayback Machine.)
  21. , p. 457
  22. Arrington, Leonard J. (1994), "Colonization of Utah", Utah History Encyclopedia, Salt Lake City, Utah: University of Utah Press, retrieved December 6, 2012
  23. NPS contributors (2009), 2009 Centennial Newspaper, Washington, D.C.: National Park Service, retrieved December 6, 2012
  24. Powell, Allen Kent (1994), "Zion National Park", in Powell, Allan Kent, Utah History Encyclopedia, Salt Lake City, Utah: ISBN 0-87480-425-6, OCLC 30473917 Retrieved on January 1, 2009.
  25. USGS contributors. Stoffer, Phil, ed. Virgin River Canyons: Historic 3D Photographs of Powell Survey in the Zion National Park Area. Washington, D.C.: United States Geological Survey. Archived from the original on 1 Jun 2008. Retrieved 18 January 2009 – via web.archive.org. (public domain text)
  26. Albright, Horace M.; Schenck, Marian Albright; Utley, Robert M. (1999). "18 - Exploring a New World of Parks, 1917" (PDF). Creating the National Park Service: The Missing Years (PDF). University of Oklahoma Press, Norman Publishing. p. 243. Retrieved 18 January 2009.
  27. "Appendix C". Leave No Trace Principles. Washington, D.C.: National Park Service.
  28. Cape Royal Road (PDF). Washington, D.C.: National Park Service. c. 1968. p. 4. HAER AZ-40. Retrieved 18 January 2009.
  29. • The Zion–Mount Carmel Tunnel
  30. ZNHA contributors. A Guide to the Trails: Zion National Park. Springdale, Utah: Zion Natural History Association. p. 10. Retrieved 18 January 2009.
  31. , p. 465
  32. , Green Transit - The Zion Shuttle
  33. "Zion Traffic Mitigation Report, Department of Transportation". United States Department of Transportation, Federal Highway Administration. Retrieved December 19, 2009.
  34. Mentz, Kevin M.; Worrell, Eric; Zanetell, F. Dave (1997). "Park Project Is a Paragon of Partnership". Public Roads. Federal Highway Administration, United States Department of Transportation. 60 (4). Retrieved 18 January 2009.
  35. Kona, Srividya. "Zion National Park, Utah". Travel. Texas Tech University. Retrieved 1 January 2009.
  36. Mims, Bob (17 September 2015). "7 dead in Zion National Park flash flood". CNN.com. Retrieved 29 January 2016.
  37. , p. 461
  38. , p. 42
  39. NPS contributors. "Geology Fieldnotes: Zion National Park". Washington, D.C.: National Park Service. Retrieved January 1, 2009. (public domain text and table)
  40. , Home page
  41. NPS contributors. "Wilderness Stewardship Plan Handbook" (doc). Washington, D.C. p. 31. Retrieved 20 Dec 2008.
  42. , p. 39
  43. , Plants (subpages)
  44. , Wildflowers
  45. , Animals (subpages)
  46. , Bird list
  47. Utah Division of Wildlife Resources, Department of Natural Resource: - Utah Bighorn Sheep Statewide Management Plan,
  48. National Park Service: Zion National Park – Biologists Catch First Glimpse of Condor Chick in Utah, July 15, 2014
  49. , Mammal list
  50. , p. 40
  51. , Outdoor Activities
  52. , For Kids
  53. , Commercial Tours
  54. , Day Hiking (archive Archived February 1, 2009, at the Wayback Machine.)
  55. , Zion Narrows
  56. NPS contributors (2008). Backcountry Planner (PDF). Washington, D.C.: National Park Service. p. 10. Retrieved 18 January 2009.
  57. "Mountain Project".
  58. , Backcountry Reservations and Permits (archive Archived 2009-01-24 at the Wayback Machine.)
  59. , Campgrounds
  60. , Backpacking
  61. , Fees & Reservations

Zion National Park: Bibliography

Sunset at Lava Point
  • Harris, Ann G.; ISBN 0-7872-5353-7.
  • Kiver, Eugene P.; Harris, David V. (1999). Geology of U.S. Parklands (5th ed.). New York City: ISBN 0-471-33218-6.
  • Leach, Nicky (2007). Zion National Park: Sanctuary in the Desert (6th ed.). Mariposa, California: Sierra Press. ISBN 1-58071-020-4.
  • NPS contributors. "Zion National Park, official website". Washington, D.C.: National Park Service. (public domain text)
  • Schneider, Stuart (2001). Kolob Canyons Road Guide. Zion Natural History Association. ISBN 0-915630-28-1.
  • Tufts, Lorraine Salem (1998). Secrets in The Grand Canyon, Zion and Bryce Canyon National Parks (3rd ed.). North Palm Beach, Florida: National Photographic Collections. ISBN 0-9620255-3-4.
  • Woodbury, Angus M. (July–October 1944). A History of Southern Utah and Its National Parks. XII. Utah State Historical Society.
  • National Park Service
  • Maps
  • Zion Natural History Association

Zion National Park: Further reading

Source of information: Wikipedia, the free encyclopedia. We're not responsible for the content of this article and your use of this information. Disclaimer
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