Zion Canyon
Encyclopedia
Zion Canyon is a deep and narrow gorge in southwestern Utah
Utah
Utah is a state in the Western United States. It was the 45th state to join the Union, on January 4, 1896. Approximately 80% of Utah's 2,763,885 people live along the Wasatch Front, centering on Salt Lake City. This leaves vast expanses of the state nearly uninhabited, making the population the...

, United States
United States
The United States of America is a federal constitutional republic comprising fifty states and a federal district...

, carved by the North Fork of the Virgin River
Virgin River
The Virgin River is a tributary of the Colorado River in the U.S. states of Utah, Nevada, and Arizona. The river is about long. It was designated Utah's first wild and scenic river in 2009, during the centennial celebration of Zion National Park.-Course:...

. Nearly the entire canyon is located within the eastern half of Zion National Park
Zion National Park
Zion National Park is located in the Southwestern United States, near Springdale, Utah. A prominent feature of the park is Zion Canyon, which is 15 miles long and up to half a mile deep, cut through the reddish and tan-colored Navajo Sandstone by the North Fork of the Virgin River...

.

Description

The beginning of the canyon is usually delineated as the Temple of Sinawava, a vertical-walled natural amphitheater nearly 3000 feet (914.4 m) deep. The canyon actually begins much further upstream, however, and runs southward about 16 miles (25.7 km) through the Narrows to reach the Temple, where the North Fork plunges over a tall waterfall. The gorge then runs southwest through the national park, approaching 2000 feet (609.6 m) deep in places. While the canyon rim is dominated by desert, the canyon floor supports a forest and riparian zone
Riparian zone
A riparian zone or riparian area is the interface between land and a river or stream. Riparian is also the proper nomenclature for one of the fifteen terrestrial biomes of the earth. Plant habitats and communities along the river margins and banks are called riparian vegetation, characterized by...

 watered by the North Fork Virgin River. The gorge then merges with Pine Creek Canyon as it winds out of the national park and past the community of Springdale
Springdale, Utah
Springdale is a town in Washington County, Utah, United States. The population was 457 at the 2000 census. It is located immediately outside the boundaries of Zion National Park, and is oriented around the resulting tourist industry. It was originally settled as a Mormon farming community in 1862...

. The canyon's end is where it meets the Virgin River, some 100 miles (160.9 km) northeast of Lake Mead
Lake Mead
Lake Mead is the largest reservoir in the United States. It is located on the Colorado River about southeast of Las Vegas, Nevada, in the states of Nevada and Arizona. Formed by water impounded by the Hoover Dam, it extends behind the dam, holding approximately of water.-History:The lake was...

, which the river ultimately flows into.
Zion Canyon Drive and Zion-Mount Carmel Highway are the two major roads throughout the canyon. Zion Canyon Drive ends at the Temple of Sinawava, where hiking trails follow the river upstream to the Emerald Pools. Hiking trails further upstream descend into the Narrows, where the canyon floor is on average 20 feet (6.1 m) wide. Hiking is permitted in the Narrows when water levels are low enough, however, flash flood
Flash flood
A flash flood is a rapid flooding of geomorphic low-lying areas—washes, rivers, dry lakes and basins. It may be caused by heavy rain associated with a storm, hurricane, or tropical storm or meltwater from ice or snow flowing over ice sheets or snowfields...

s are known to rise quickly following heavy rainstorms. Many areas in the drainage of Zion Canyon have little or no soil cover, contributing to extremely brief but heavy storm runoff. In contrast, the floor of most of the main Zion Canyon is close to 1000 feet (304.8 m) wide, and is rich with river-deposited sediments. Tributaries to the river within the canyon include Deep, Kolob, Goose, Pine, and Oak Creeks.

Geology and history

Geologically Zion Canyon is part of the Navajo sandstone
Navajo Sandstone
Navajo Sandstone is a geologic formation in the Glen Canyon Group that is spread across the U.S. states of northern Arizona, northwest Colorado, and Utah; as part of the Colorado Plateau province of the United States...

 Colorado Plateau
Colorado Plateau
The Colorado Plateau, also called the Colorado Plateau Province, is a physiographic region of the Intermontane Plateaus, roughly centered on the Four Corners region of the southwestern United States. The province covers an area of 337,000 km2 within western Colorado, northwestern New Mexico,...

, which contained many joints and cracks when first uplifted, one of which was cut by the North Fork of the Virgin River to become Zion Canyon. The river was the largest force in cutting the canyon, mostly by flash floods, as the average flow of the river is very light. This relatively quick downcutting has left many seasonal tributaries with hanging valleys. Some of the largest tributaries have cut down to nearly an equal elevation as the valley floor.

Strong winds continue to sculpt the canyon walls, creating natural arches. It is believed that there is another 1000 feet (304.8 m) of vertical bedrock that the Virgin River can still erode. Mass wasting
Mass wasting
Mass wasting, also known as slope movement or mass movement, is the geomorphic process by which soil, regolith, and rock move downslope under the force of gravity. Types of mass wasting include creep, slides, flows, topples, and falls, each with its own characteristic features, and taking place...

, often caused by ice wedging into cracks in the canyon walls, is another force that widens the valley. The Navajo Sandstone formation is easily eroded and is known to be very porous. Unstable geology is prevalent throughout the canyon, and occasional rockslides have formed impounded lakes in the canyon, the most recent of which was roughly 4,000 years ago. Owing to the extreme depth of the canyon, there are many springs
Spring (hydrosphere)
A spring—also known as a rising or resurgence—is a component of the hydrosphere. Specifically, it is any natural situation where water flows to the surface of the earth from underground...

 fed by the surrounding groundwater
Groundwater
Groundwater is water located beneath the ground surface in soil pore spaces and in the fractures of rock formations. A unit of rock or an unconsolidated deposit is called an aquifer when it can yield a usable quantity of water. The depth at which soil pore spaces or fractures and voids in rock...

, permitting water in the canyon to run year round.

The first settlers in Zion Canyon were Mormon
Mormon
The term Mormon most commonly denotes an adherent, practitioner, follower, or constituent of Mormonism, which is the largest branch of the Latter Day Saint movement in restorationist Christianity...

s that migrated from the lower Virgin River area in the late 1850s. The canyon was named by settler Isaac Behunin, who named the canyon after a "place of peace" mentioned in the Bible
Bible
The Bible refers to any one of the collections of the primary religious texts of Judaism and Christianity. There is no common version of the Bible, as the individual books , their contents and their order vary among denominations...

. Explorer John Wesley Powell
John Wesley Powell
John Wesley Powell was a U.S. soldier, geologist, explorer of the American West, and director of major scientific and cultural institutions...

 is credited with the name Mukuntuweap, supposedly the native name of the canyon. In 1909, the canyon was first declared a national monument, and in 1919 was declared a national park. The Zion-Mount Carmel Highway, cutting through Pine Creek Canyon and lower Zion Canyon, first opened in 1930.
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