Zion National Park is located in the Southwestern United States, near Springdale, Utah. A prominent feature of the 229-square-mile (590 km2) 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.
Cabover Style C22 RV - UTAH
5 6ft 7in
Cabover Style C22 RV - UTAH V4
5 6ft 7in
Mighway, by TH2, allows you to rent your vehicle to discerning travellers when you’re not on the road, earning money and sharing the experience. At Mighway, you choose your level of service and we take good care of the rest. That means comprehensive insurance coverage, customer vetting, security deposits, payment processing and round the clock customer support for renters. It’s a bit like renting out a vacation home, with Mighway beside you all the way.LEARN MORE
The Narrows is the narrowest section of Zion Canyon. This gorge, with walls a thousand feet tall and the river sometimes just twenty to thirty feet wide, is one of the most popular areas in Zion National Park. You can see The Narrows by hiking along the paved, wheelchair accessible Riverside Walk for one mile from the Temple of Sinawava. If you wish to see more, you will be walking in the Virgin River. This can involve wading upstream for just a few minutes or it can be an all day hike. **Park at Zion Canyon Visitor Center and take the shuttle to it's final stop.
(1.2 mile / 1.9 km round-trip). Trailhead is across the highway from the Zion Lodge. This is an easy paved trail that leads to the lower pool, just below the middle pools.
Babylon Arch won’t put a ton of miles on your hiking boots, but it will put a smile on your face as you wind your way through the sandy red rock trail and pass through its beautiful formation. You have to keep a wary eye out for the arch, though. This particular hike has another nice addition besides the arch, and that is the Virgin River. Your final destination is the slow moving Virgin River, and it makes for a great way to cool down depending on the time of year.
(5.4 mile / 8.7 km round-trip). Trailhead is at the Grotto. A steep, strenuous hike up the West Rim Trail to the Angels Landing Trail, which is a half mile / 0.8 km spur. The trail follows a steep, narrow ridge with chains added to provide handholds. This spectacular trail ends at a magnificent overlook of Zion Canyon and the Virgin River. For those in good physical condition and not afraid of heights, this hike is a must. Those afraid of heights can stop and turn around at '''Scout Overlook''' where the final vertiginous ascent to Angel's landing starts. The hike to Scout Overlook only is strenuous but less exposed.
Venture onto a shifting sea of red sand. Changed by winds, these mountains and hills of sand can move as much as 50 feet per year. With areas for off-highway vehicle enthusiasts and those with non-motorized pursuits, the dunes offer adventures for all. The geology of the sand dunes is an intriguing subject. The sand comes from Navajo sandstone from the geologic period call Middle Jurassic. The same iron oxides and minerals that give us spectacular red rock country are responsible for this landscape of coral pink sand.Sand dunes are created by three factors: Sand, high winds,and a unique influence upon the wind. The notch between the Moquith and Moccasin mountains causes this unique influence. The wind is funneled through the notch, thereby increasing wind velocity to a point where it can carry sand grains from the eroding Navajo sandstone.This phenomenon is known as the Venturi Affect. Once the wind passes through the notch and into the open valley, the wind velocity decreases, causing the sand to be deposited.These dunes are estimated at 10,000 to 15,000 years old.Coral Pink Sand Dunes support a diverse population of insects, including the Coral Pink tiger beetle that is found only here. Melting snow often creates small ponds on the dunes that support amphibians such as salamanders and toads.The park is also a popular destination for ATV riders. About 90% of the dunes are open for riding, but all of the dunes are open for hiking and just playing in the sand.Opened to the public as a state park in 1963.Visit Coral Pink Sand Dunes State Park
South Campground is located ½ mile from the South Entrance. There are 127 campsites (including three wheelchair accessible) available first-come, first-served. There are no hook-ups; a dump station is available for campers. Generators are allowed from 8:00 a.m. to 10:00 a.m. and from 6:00 p.m. to 8:00 p.m. Campsites are $16.00 per night. Owners of an Interagency Senior or Access or a Golden Age or Access Pass receive a 50% discount on camping fees. Shaded/tree sites can only accommodate vehicles with maximum height of 13' (3.96m).Visit South Campground
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