Vermilion Cliffs National Monument

Summary

Vermilion Cliffs National Monument is located in northern Coconino County, Arizona, United States, immediately south of the Utah state line. This national monument, 293,689 acres (118,852 ha)[1] in area, protects the Paria Plateau, Vermilion Cliffs, Coyote Buttes, and Paria Canyon. Elevations in the monument range from 3,100 feet to 6,500 feet above sea level (944 to 1,981 meters).

Vermilion Cliffs National Monument
A photo of the wave on a sunny summer day
A map of the United States showing the location of Vermillion Cliffs National Monument
A map of the United States showing the location of Vermillion Cliffs National Monument
Location in the United States
A map of the United States showing the location of Vermillion Cliffs National Monument
A map of the United States showing the location of Vermillion Cliffs National Monument
Location in Arizona
LocationCoconino County, Arizona, United States
Nearest cityPage, Arizona
Coordinates36°48′23″N 111°44′28″W / 36.80639°N 111.74111°W / 36.80639; -111.74111
Area293,689 acres (118,852 ha)[1]
EstablishedNovember 9, 2000
Governing bodyU.S. Bureau of Land Management
Websitehttps://www.blm.gov/national-conservation-lands/arizona/vermilion-cliffs/
Vermilion Cliffs In Arizona
View Of the upper reaches of the Vermilion Cliffs.
Vermilion Cliffs National Monument Sign
A Vermilion Cliffs National Monument Sign in Marble Canyon, AZ.

Creation and designation edit

Established on November 9, 2000 by a presidential proclamation by President Bill Clinton,[2][3] Vermilion Cliffs National Monument was carved from existing lands already under the management of the U.S. Government in extreme northern Coconino County, Arizona, immediately south of the border with the state of Utah. The monument is administered by the U.S. Bureau of Land Management, an agency within the U.S. Department of the Interior. The Vermilion Cliffs themselves run along the southern and eastern edges of the monument. Much of the monument's land consists of the Paria Plateau, a flat area extending northward from the tops of the cliffs.

Vermilion Cliffs edit

 
Sunrise through a cleft in the Vermilion Cliffs

The Vermilion Cliffs are steep eroded escarpments consisting primarily of sandstone, siltstone, limestone, and shale which rise as much as 3,000 feet (910 m) above their bases. These sedimentary rocks have been deeply eroded for millions of years, exposing hundreds of layers of richly colored rock strata. Mesas, buttes, and large tablelands are interspersed with steep canyons, where some small streams provide enough moisture to support a sampling of wildlife.

 
Cobra Arch north of Buckskin Gulch, Vermilion Cliffs National Monument

Flora and fauna edit

More than twenty species of raptors, including bald eagles and golden eagles, peregrine falcons, and several hawk species, have been observed. The endangered California condor was re-introduced into this region in 1996[4] due to its remote location and lack of human habitation. Desert bighorn sheep, pronghorns, and mountain lions make up most of the large mammals found here, with about 30 more species of smaller mammals. Several examples of rare fish species, such as the flannelmouth sucker and the speckled dace live in the streams of the monument. The Welsh's milkweed Asclepias welshii, a threatened plant species that grows on sand dunes and helps stabilize them, is known to exist only in the monument and one other area in neighboring Utah.

Human settlements edit

 
White Pocket area formation

Human settlement in the region dates back 12,000 years, and hundreds of Native American pueblos are spread across the monument. The remains of the natives' villages, with houses, granaries, burial areas, and associated ruins, can be found here. The monument also contains one of the largest number of rock art sites in any nationally protected area. Many of these petroglyphs are believed to be among the oldest in the United States.

The first explorers into the region were Spanish missionaries and explorers from the 1776 Domínguez–Escalante expedition. Later, Mormon explorers searched the region during the 1860s, some of them settling on land that is now within the monument. They built one of the first ferry crossings on the Colorado River in 1871. That same year, John Wesley Powell ventured through this region during his scientific explorations of the Colorado River plateau.

Below the Vermilion cliffs runs the historic "Honeymoon Trail", a wagon route for Mormons who journeyed to have their marriages sealed in the temple at St. George, Utah, and then to return. The route, through remote country, was otherwise seldom used. Historical markers denote this history.

Today, the region surrounding the monument is relatively unspoiled with virtually no permanent inhabitants remaining and limited road access.

See also edit

References edit

  1. ^ a b "National Monument detail table as of April 2012" (PDF). Bureau of Land Management. Retrieved 2012-12-27.
  2. ^ "Proclamation 7374 – Vermilion Cliffs National Monument" (PDF). United States Statutes at Large, volume 114, page 3422. U.S. Government Printing Office.
  3. ^ "Press release" (PDF). Grand Canyon Trust.org. November 9, 2000. Retrieved 2009-06-20.[dead link]
  4. ^ "California Condor Reintroduction & Recovery". National Park Service. Retrieved 7 December 2023.

External links edit

  • Official website
  • Proclamation establishing Vermilion Cliffs National Monument
  • USGS Navajo Bridge (AZ) Topo Map
  • National Geographic: Vermilion Cliffs National Monument