Walnut Canyon National Monument
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Walnut Canyon National Monument (
Hopi The Hopi are a Native American ethnic group who primarily live on the Hopi Reservation in northeastern Arizona, United States. As of the 2010 census, there are 19,338 Hopi in the country. The Hopi Tribe is a sovereign nation within the United ...
: Wupatupqa) is a
United States National Monument In the United States, a national monument is a protected area that can be created from any land owned or controlled by the federal government by proclamation of the President of the United States or an act of Congress. National monuments prot ...
located about southeast of downtown
Flagstaff, Arizona Flagstaff ( ) is a city in, and the county seat of, Coconino County in northern Arizona, in the southwestern United States. In 2019, the city's estimated population was 75,038. Flagstaff's combined metropolitan area has an estimated population ...
, near
Interstate 40 Interstate 40 (I-40) is a major east–west Interstate Highway running through the south-central portion of the United States. At a length of , it is the third-longest Interstate Highway in the country, after I-90 and I-80. From west to ea ...
. The
canyon A canyon (from ; archaic British English spelling: ''cañon''), or gorge, is a deep cleft between escarpments or cliffs resulting from weathering and the erosive activity of a river over geologic time scales. Rivers have a natural tendency to cu ...
rim elevation is ; the canyon's floor is 350 ft lower. A long loop trail descends into the canyon passing 25 cliff dwelling rooms constructed by the
Sinagua The Sinagua were a pre-Columbian culture that occupied a large area in central Arizona from the Little Colorado River, near Flagstaff, to the Verde River, near Sedona, including the Verde Valley, area around San Francisco Mountain, and signifi ...
, a pre-Columbian cultural group that lived in Walnut Canyon from about 1100 to 1250 AD. Other contemporary habitations of the Sinagua people are preserved in the nearby Tuzigoot and Montezuma Castle national monuments.


History

Sinagua is Spanish for "without water", an acknowledgement that the
Sinagua The Sinagua were a pre-Columbian culture that occupied a large area in central Arizona from the Little Colorado River, near Flagstaff, to the Verde River, near Sedona, including the Verde Valley, area around San Francisco Mountain, and signifi ...
people were able to live in such a dry region. By living in such a region the Sinagua became experts at conserving water and dealing with droughts. The Sinagua were also believed to have been active traders whose activities and influence stretched to the Gulf of Mexico and even as far as Central America. The Sinagua, who inhabited the dwellings in Walnut Canyon, left mysteriously around 1250 AD. It is thought that the Sinagua left because of fear of neighboring tribes or droughts, but it is not certain. The Sinagua left over 80 cliff dwellings behind. The Sinagua built their homes under limestone ledges, deep within the canyon, some time between 1125 and 1250 – taking advantage of the natural recesses in the limestone cliff walls which were eroded over millions of years by flowing water. The dwellings themselves were small, but large enough for the inhabitants to cook and sleep. Most of the cliff dwelling rooms are situated near the loop trail, typically slightly above the trail and immediately outside the loop itself. A typical room might have been the dwelling of a single family, and might measure approximately two meters high by six meters long by three meters deep. Because of the area's dry climate, the water present in the canyon was essential for its inhabitants over 700 years ago as it is for animal and plant life today. The plant life is very diverse in Walnut Canyon, with more than 387 different plant species, including the Prickly Pear cactus and the Arizona Black Walnut. The biodiversity of the area includes high concentrations of sensitive plant species that probably contributed to the decision made by prehistoric people to settle in the area. There are other ruins in the area, but none are publicly accessible. Many more dwellings can be seen up close in the canyon just east of the Monument, although it is illegal to enter the canyon. Walnut Canyon was proclaimed a national monument on November 30, 1915, by President Woodrow Wilson to preserve the ancient cliff dwellings. It was transferred from the
USDA Forest Service The United States Forest Service (USFS) is an agency of the U.S. Department of Agriculture that administers the nation's 154 national forests and 20 national grasslands. The Forest Service manages of land. Major divisions of the agency inc ...
to the
National Park Service The National Park Service (NPS) is an agency of the United States federal government within the U.S. Department of the Interior that manages all national parks, most national monuments, and other natural, historical, and recreational properti ...
on August 10, 1933. As with all historic areas administered by the National Park Service, the national monument was listed on the
National Register of Historic Places The National Register of Historic Places (NRHP) is the United States federal government's official list of districts, sites, buildings, structures and objects deemed worthy of preservation for their historical significance or "great artistic ...
on October 15, 1966. At Walnut Canyon, there are trails for tourists to get a close view of the dwellings.


Geology

Walnut Canyon lies on the
Colorado Plateau The Colorado Plateau, also known as the Colorado Plateau Province, is a physiographic and desert region of the Intermontane Plateaus, roughly centered on the Four Corners region of the southwestern United States. This province covers an area o ...
and cuts through the
Permian The Permian ( ) is a geologic period and stratigraphic system which spans 47 million years from the end of the Carboniferous Period million years ago (Mya), to the beginning of the Triassic Period 251.9 Mya. It is the last period of the Paleo ...
Kaibab Limestone The Kaibab Limestone is a resistant cliff-forming, Permian geologic formation that crops out across the U.S. states of northern Arizona, southern Utah, east central Nevada and southeast California. It is also known as the Kaibab Formation in ...
, which exposes the Toroweap Formation and
Coconino Sandstone Coconino Sandstone is a geologic formation named after its exposure in Coconino County, Arizona. This formation spreads across the Colorado Plateau province of the United States, including northern Arizona, northwest Colorado, Nevada, and Utah. ...
.Ulrich, G.E., Billingsley, G.H., Hereford, Richard, Wolfe, E.W., Nealey, L.D. and Sutton, R.L., 1984, Map showing geology, structure, and uranium deposits of the Flagstaff 1 degrees x 2 degrees quadrangle, Arizona: U.S. Geological Survey, Miscellaneous Investigations Series Map I-1446, scale 1:250000. The Kaibab formation also forms the rim of the
Grand Canyon The Grand Canyon (, yuf-x-yav, Wi:kaʼi:la, , Southern Paiute language: Paxa’uipi, ) is a steep-sided canyon carved by the Colorado River in Arizona, United States. The Grand Canyon is long, up to wide and attains a depth of over a m ...
.
Crossbedding In geology, cross-bedding, also known as cross-stratification, is layering within a stratum and at an angle to the main bedding plane. The sedimentary structures which result are roughly horizontal units composed of inclined layers. The origina ...
is present in the Coconino Sandstone. The Walnut Canyon site contains Walnut Creek, which carved a 600 foot deep canyon that flows east. The creek joins into the Little Colorado River en route to the Grand Canyon. The creek has also created a varied and abundant array of vegetation. The shaded, north-facing walls are covered in fir and ponderosa pine trees. The sunny, south facing slopes have agaves and several species of cactus including opuntia, echinocereus and cholla. The floor of the canyon is home to several species of walnut trees, for which the canyon is named. The rocks in the canyon walls are formed of three distinct layers – the upper third of Walnut Canyon's walls contain
Kaibab Limestone The Kaibab Limestone is a resistant cliff-forming, Permian geologic formation that crops out across the U.S. states of northern Arizona, southern Utah, east central Nevada and southeast California. It is also known as the Kaibab Formation in ...
that varies in layers and hardness, where the cliff dwellings are found, which overlies steep, scrub covered slopes of the
Toroweap Formation The Middle Permian Toroweap Formation is a thin, darker geologic unit, between the brighter colored units of the Kaibab Limestone above, and Coconino Sandstone below. It is a prominent unit in Grand Canyon, Arizona, USA, found through sections ...
, while the lowest third is the sheer-walled, cross-bedded
Coconino Sandstone Coconino Sandstone is a geologic formation named after its exposure in Coconino County, Arizona. This formation spreads across the Colorado Plateau province of the United States, including northern Arizona, northwest Colorado, Nevada, and Utah. ...
. Many layers of the limestone eroded, creating alcoves that the Sinagua Indians used as cave-dwellings. Today a variety of archeological and natural resources are preserved on approximately 3600 acres.


Climate

Not all of Arizona is warm dry desert. At Walnut Canyon (6690'/2039m above sea level), has snow in winter, hot sun in summer with afternoon thunderstorms, and in the spring, strong gusty winds on the rim and/or in the canyon. Even though the climate was and still is somewhat harsh, the Sinagua Indians that lived there were able to harvest maize, beans and squash.


Operating hours and seasons

Park entrance road, trails, and Visitor Center are open all year, except December 25. From May until October the monument is open from 8:00 a.m. to 5:00 p.m. MST and is open from 9:00 a.m. to 5:00 p.m. MST the remainder of the year. Entry to park trails closes 1 hour before the monument closes. The Walnut Canyon site is near Flagstaff. It is 7 miles east of I-40 and 3 miles south of exit 204. The park has a museum and a small visitor center atop a cliff. Many of the ancient dwellings were built around a U-shaped meander in the canyon, where the creek circles around three sides of a high rocky plateau, almost creating an 'island', and this region now forms the central attraction of the national monument. There are other ruins in the surround area which are not open to the public. Other dwellings of the Sinagua people can be found in the nearby Tuzigoot and Montezuma Castle monuments. The
Old Headquarters The Cliffs Ranger Station is an early United States Forest Service ranger station in what is now Walnut Canyon National Monument Walnut Canyon National Monument (Hopi: Wupatupqa) is a United States National Monument located about southeast o ...
is listed on the
National Register of Historic Places The National Register of Historic Places (NRHP) is the United States federal government's official list of districts, sites, buildings, structures and objects deemed worthy of preservation for their historical significance or "great artistic ...
.


References


External links


Walnut Canyon National Monument
Official NPS website.
American Southwest, a National Park Service ''Discover Our Shared Heritage'' Travel Itinerary
* * {{Authority control National Park Service National Monuments in Arizona Cliff dwellings Canyons and gorges of Arizona Landforms of Coconino County, Arizona Museums in Coconino County, Arizona Ancient Puebloan archaeological sites in Arizona Native American museums in Arizona Parks in Arizona Archaeological sites on the National Register of Historic Places in Arizona National Register of Historic Places in Coconino County, Arizona 1915 establishments in Arizona Protected areas established in 1915 Protected areas of Coconino County, Arizona Former populated places in Coconino County, Arizona Historic districts on the National Register of Historic Places in Arizona Sinagua