Zion National Park
|
|
| Zion | |
| |
| Designation | National Park |
| Location | Utah, United States |
| Nearest City | Springdale, Utah |
| Coordinates | Template:Coor dm |
| Area | 146,592 acres 59,324 ha (593 km²) |
| Date of Establishment | November 19, 1919 |
| Visitation | 2,451,977 (2003) |
| Governing Body | National Park Service |
| IUCN category | II (National Park) |
Zion National Park is located near Springdale, Utah in the southwestern United States. It has an area of 229 mile² (593 km²) and ranges in elevation from a low point of 3,666 ft (1,128 m) on Coalpits Wash to a high point at 8,726 ft (2,660 m) at Horse Ranch Mountain. Established in 1909 as Mukuntuweap National Monument, it became Zion National Park in 1919. The Kolob section was added in 1937.
Zion is an ancient Hebrew word meaning "place of refuge" or "sanctuary," often used by the LDS settlers in Utah. Protected within the park is a dramatic landscape of sculptured canyons and soaring cliffs, mostly from the 170 million year old tan to orange-red sandstone of the Navajo Formation. Zion is located at the junction of the Colorado Plateau, Great Basin, and Mojave Desert provinces. This unique geography and the variety of life zones within the park make Zion significant as a place of unusual plant and animal diversity.
Among the notable geographical features of the park are:
- Virgin River Narrows
- Emerald Pools (photo)
- Angels Landing (photo)
- The Great White Throne (photo)
- The Three Patriarchs (photo)
- Kolob Arch, a remote cliff wall arch
| Contents |
Geography
Zion_National_Park_map1.jpg
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. This unique geography and the variety of life zones within the park add to Zion's significance as a place of unusual plant and animal diversity. The northern part of the park is known as the Kolob Canyons section and is accessible from Interstate 15.
The 8726 foot (2660 m) summit of Horse Ranch Mountain (photo) is the highest point in the park; the lowest point is the 3666 foot (1128 m) elevation of Coal Pits Wash, creating a relief of about 5100 feet (1500 m).
Streams in the area follow rectangular paths because they follow jointing planes in the rocks. The headwaters of the Virgin River are at about 9000 feet (2700 m) and it empties into Lake Mead 200 miles (320 km) southeast after flowing 8000 feet (2400 m) downward. This gives the Virgin a stream gradient that ranges from 50 to 80 feet per mile (9 to 15 m/km)—one of the steepest stream gradients in North America.
Spring weather is very unpredictable with stormy, wet days being common, but warm, sunny weather may also occur. Precipitation peaks in March and 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. Fall days are usually clear and mild; nights are often cool. Autumn tree-color displays begin in September in the high country; inside 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, but 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 cause roads to be icy. Zion roads are plowed, except the Kolob Terrace Road, which is closed in winter. Winter driving conditions persist from November through March.
Human history
Archaeologists have divided the long span of Zion's human history into four cultural periods, each characterized by distinctive technological and social adaptations.
Archaic period
Scouts_reconstructing_an_Anasazi_granary_near_Weeping_Rock.jpeg
The first evidence of human use in the region dates to about 8,000 years ago when small family groups camped wherever they could hunt or collect plants and seeds. About 2,000 years ago, some groups began growing maize and other crops, leading to an increasingly sedentary lifestyle. Later groups in this period built permanent villages (often called pueblos). Archaeologists call this the Archaic period and it lasted until about 500. Baskets, cordage nets, and yucca fiber sandals have been found and dated to this period. The Archaic toolkits also included flaked stone knives, drills, and stemmed dart points. The dart points were hafted to wooden shafts and propelled by throwing devices called atlatls.
By about 300, some of the archaic groups developed into an early branch of seminomadic Anasazi, the Basketmakers. Basketmaker sites often have grass- or stone-lined storage cists and shallow, partially underground dwellings, called pithouses. They were hunters and gathers who supplemented their diet with limited agriculture. Locally collected pine nuts were important for food and trade.
Formative period
As centuries passed, their culture became less nomadic and more dependent on farming until they became almost totally dependent upon horticulture by around 500, thus becoming what archaeologists call the Virgin Anasazi. Petroglyphs (rock art) from this period indicate that their culture was more complex and connected to its surroundings than it had been. Virgin Anasazi sites typically occur on river terraces along the Virgin River and its major tributaries, overlooking the fertile river bottoms where corn, squash, and other crops could be grown. This is called the Formative period and it lasted until about 1300.
The Parowan Fremont lived in the north part of what now is the park. There is little evidence to suggest any long-term relationship between the two groups, even though they lived similar lives. They do, however, appear to have interacted along cultural contact zones, such as the Kolob Plateau, during the last years of the Formative period. Parowan Fremont sites are found along stream courses and near springs. They cultivated a variety of corn, Fremont Dent, tolerant of drought and cold and that could be successfully grown at higher elevations.
Both cultures grew maize and squash, which were stored for the winter months, and both lived in small groups. A sedentary lifestyle for both cultures encouraged the production of plain and painted ceramic vessels. The Fremont and the Anasazi both left the area around 1200 to 1300 for unknown reasons. Extended droughts in the 11th and 12th centuries interspersed with catastrophic flooding might have made horticulture impossible in this arid region. Competition from mobile Numic-speaking peoples (such as the Paiute and Ute), who moved into the region by at least 1100, might also be a cause.
Neo-Archaic period
Southern_Paiute_kaun_huts.jpeg
The Parrusits and several other Southern Paiute subtribes lived in the Virgin River Valley south of Zion Canyon for hundreds of years following the departure of the Anasazi and Fremont Indians. Tradition and some archaeological evidence holds that they are a Numbic-speaking cousin of the Virgin Anasazi. Parrusists seasonally migrated up and down the valley in search of wild seeds and nuts in what is called the Neo-Archaic period. Some farming and hunting supplemented their diet.
Evidence suggests that the Parrusits had great reverence for the large monoliths and turbulent waters in Zion Canyon. They also believed that they were responsible for the streams and springs they depended upon by communicating with the rocks, animals, water, and plants that make their home there. Modern bands of Southern Paiute still visit sites within the park to perform rituals and collect plants.
Historic period
Early exploration
The Historic period begins in the late 18th century, with the exploitation and settlement of southern Utah by Euro-Americans. Padres Dominguez and Escalante passed near what is now the Kolob Canyons Visitor Center on October 13, 1776, becoming the first white men known to visit the area. In 1826, trapper and trader Jedediah Smith led 16 men to explore the area in a quest to find a route to California. These and other explorations by traders from New Mexico blazed the Old Spanish Trail, which followed the Virgin River for a portion of its length.
Captain John C. Fremont wrote about his 1844 journeys in the region. During the next century, American fur trappers and government surveyors added new overland travel routes across the region.
Mormon pioneers and the Powell expedition
In the early 1850s, Mormon farmers and cotton growers from the Salt Lake area became the first white people to settle the Virgin River region. In 1851, the Cedar City, Utah area was settled by Mormons who used the Kolob Canyons area for timber, and for grazing cattle, sheep, and horses. They also prospected for mineral deposits and diverted Kolob water to irrigate crops in the valley below. Mormon settlers named the area Kolob, which in Mormon scripture is the star nearest the residence of God.
By 1858, they had expanded 75 miles (120 km) up the Virgin River and into the immediate Zion Canyon area, which was still virtually unknown and unexplored by whites. That year, a Southern Paiute guide led a young Mormon missionary and translator named Nephi Johnson into Zion Canyon. Johnson wrote a favorable report about the agricultural potential of the canyon floor and, by 1861, Mormon pioneer Joseph Black became the first white man to build a cabin and farm in the canyon. His stories about the Canyon were at first seen as exaggerated, prompting his neighbors to call the Canyon "Joseph's Glory." Interest in the area remained low until several farming families founded Springdale, Utah in 1862, just outside the mouth of Zion Canyon.
Other pioneers followed, including Issac Behunin, who farmed tobacco, sugar cane, and fruit trees. He lived in a cabin that he built in 1863 near what is now the site of Zion Lodge. The naming of Zion Canyon, a reference to a peaceful place mentioned in the Bible, is attributed to Behunin. Catastrophic flooding by the river (especially in the Great Flood of 1861-1862), little arable land, and poor soils made agriculture in the upper Virgin River a risky venture.
Crawford_ranch_in_Zion_Canyon.jpeg
More settlers moved into the canyon and improved its ability to serve their needs. Cattle and other domesticated animals, however, pushed out wild game and depleted native grasses. This made conditions worse for the Parrusits still living in the area (whose numbers had been greatly reduced by disease and slavery under the Spanish in the 18th century). In time, their numbers decreased to almost zero as the remaining inhabitants migrated to less-crowded lands south and cultural assimilation. The canyon was farmed until it was protected in 1909.
The John Wesley Powell expedition entered the area in 1869 after their first trip through the Grand Canyon. Powell and geologist Grove Karl Gilbert explored Zion Canyon in 1872 and named it Mukuntuweap under the impression that was the Paiute name for the canyon. Powell Survey photographers, Jack Hillers and James Fennemore, first visited the Zion Canyon and Kolob Plateau region in the spring of 1872. Hillers returned in April of 1873 to add more photographs to the "Virgin River Series" of photographs and stereographs. Hillers described wading the canyon for 4 days and nearly freezing to death from the cold and exposure to take his photographs. Fellow geologist Clarence Dutton later mapped the region and artist William H. Holmes documented the scenery.
Protection and tourism
Zion_great_white_throne.jpg
Paintings of the canyon by Frederick S. Dellenbaugh were exhibited at the St. Louis World's Fair in 1904, followed by a glowing article in Scribner's Nagazine the next year. That, along with previously created photographs, paintings, and reports, led to U.S. President William Howard Taft's proclamation creating Mukuntuweap National Monument on July 31, 1909. In 1917, the acting director of the newly created National Park Service visited the canyon and proposed changing its name back to Zion from the locally unpopular Mukuntuweap. That occurred the following year. The United States Congress then added more land and established Zion National Park on November 19, 1919. Park expansion in 1937 and 1956 included the Kolob Canyons area.
Travel to the area before it was made into a national park was rare due to its remote location, lack of accommodations, and the absence of real roads in that part of Utah. For a long time, the only road to Zion Canyon was a dirt track that followed the Virgin River to Springdale from the neighboring valley. At the turn of the 20th century, local rancher John Winder improved an old Native American trail that reached Long Valley through the Zion area (park officials later improved the trail and renamed it the East Rim Trail). Then the Utah State Road Commission, established the same year that the national monument was created, set out to develop a state highway system that would include southern Utah. The first all-weather paved route from Cedar City to Springdale opened in 1913. State officials also negotiated with the Union Pacific Railroad to develop rail and automobile links and tourism facilities in southern Utah.
Tour_buses_at_Zion_Lodge_in_1929.jpeg
By the summer of 1917, touring cars could finally reach Wylie Camp, a tent camping resort that provided the first visitor lodging in Zion Canyon. The Utah Parks Company, a subsidiary of the Union Pacific Railroad, acquired the Wylie Camp in Zion, and offered ten-day rail/bus tours to Zion, Bryce, Kaibab, and the North Rim of the Grand Canyon. Construction of the Zion Lodge complex began in the mid-1920s at the site of the Wylie Way tent camp and was completed in 1927. Architect Gilbert Stanley Underwood designed Zion Lodge in the "Rustic Style" and the Utah Parks Company funded the construction. In 1968, the main lodge building was destroyed by fire but was later rebuilt. The detached Western Cabins (photo) survived and were added to the National Register of Historic Places.
East_portal_of_Zion-Mt._Carmel_tunnel_in_early_1930s.jpg
Work on what is now Utah State Route 9, known as the Zion-Mt. Carmel highway, started in 1927 to provide reliable access to the eastern and southern parts of the park. The road opened in 1930 and park visitation and travel in the area greatly increased. Perhaps the most famous feature of the highway is the 1.1 mile (1.8 km) Pine Creek tunnel, which has six large windows cut into massive sandstone. Switchbacks take motorists from the tunnel to the floor of Zion Canyon.
A visitor center was built at the site of the old Crawford family ranch near the south entrance in the 1950s. The Park Service converted it into a human-history museum in the year 2000 (photo) and moved visitor center functions to a new solar powered facility between the Watchman campground and the south entrance.
Zion Canyon Scenic Drive was built to provide direct access in the canyon itself. It remained open to unregulated traffic for many years until traffic congestion forced the Park Service to limit private automobile access during peak visitation seasons to those with reservations at Zion Lodge. All other visitors must ride one of the frequent shuttle buses or walk to see the canyon. The 5 mile (8 km) Kolob Canyons Road was built in the mid-1960s to provide a scenic loop drive for that part of the park.
Geology
- Main article: Geology of the Zion and Kolob canyons area
The_Three_Patriarchs_in_Zion_Canyon.jpg
The nine known exposed formations visible in Zion National Park are part of a super-sequence of rock units called the Grand Staircase; they 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
- The dry near-shore environment of the Carmel Formation
Uplift affected the entire region, known as the Colorado Plateaus, by slowly raising these formations more than 10,000 feet (3000 m) higher than where they were deposited. This steepened the stream gradient of the ancestral Virgin and other rivers on the plateau.
Kolob_Canyons_midway_through_Kolob_Canyons_Road.jpg
The fast-moving streams took advantage of uplift-created joints in the rocks to remove all Cenozoic-aged formations and cut gorges 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 and carries much of the 3 million 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. Angels Landing between Twin Brothers Peak and Mountain of the Sun is a notable example of a hanging valley in the canyon.
|
 |
Rock Layer | Appearance | Where To See | Deposition | Rock Type | Photo |
| Dakota Formation | Cliffs | Top of Horse Ranch Mountain | Streams | Conglomerate and sandstone | Missing image Dakota_Sandstone.jpg Dakota Sandstone |
|
| Carmel Formation | Cliffs | Mt. Carmel Junction | Shallow sea and coastal desert | Limestone, sandstone and gypsum | Missing image Carmel_Formation.jpg Carmel Formation |
|
| Temple Cap Formation | Cliffs | Top of West Temple | Desert | Sandstone | Missing image Temple_Cap_Formation_atop_Navajo_Sandstone.jpg 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 and Checkerboard Mesa (photo)<p> | Desert sand dunes covered 150,000 mile² (390,000 km²)<p>Shifting winds during deposition created cross-bedding | Sandstone | Missing image Navajo_Sandstone_seen_from_Hidden_Canyon_Trail.jpg Navajo Sandstone showing its two tones |
|
| Kayenta Formation | Rocky slopes | Throughout canyon | Streams | Siltstone and sandstone | Missing image Keyenta_Formation_in_Kolob_Canyons.jpeg Keyenta Formation |
|
| Moenave Formation | Slopes and ledges | Lower red cliffs seen from Zion Human History Museum | Streams and ponds | Siltstone and sandstone | Missing image Moenave_Formation.jpeg Moenave Formation |
|
| Chinle Formation | Purpleish slopes | Above Rockville | Streams | Shale, loose clay and conglomerate | Missing image Chinle_Formation_near_Springdale,_Utah.jpeg Chinle Formation |
|
| Moenkopi Formation | Chocolate cliffs with white bands | Rocky slopes from Virgin to Rockville | Shallow sea | Shale, siltstone, sandstone, mudstone, and limestone | Missing image Moenkopi_Formation.jpeg Moenkopi Formation |
|
| Kaibab Formation | Cliffs | Hurricane Cliffs along I-15 near Kolob Canyons | Shallow sea | Limestone | Missing image Hurricane_Cliffs1.jpeg Hurricane Cliffs/Kaibab Fm. |
