Walnut Canyon National Monument

Walnut Canyon National Monument (Hopi: Wupatupqa) is a United States National Monument located about 10 mi (16 km) southeast of downtown Flagstaff, Arizona, near Interstate 40. The canyon rim elevation is 6,690 ft (2,040 m); the canyon's floor is 350 ft lower. A 0.9 mi (1.4 km) long loop trail descends 185 ft (56 m) into the canyon passing 25 cliff dwelling rooms constructed by the Sinagua, 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.

Walnut Canyon National Monument
IUCN category III (natural monument or feature)
LocationCoconino County, Arizona, United States
Nearest cityFlagstaff, Arizona
Coordinates35°10′18″N 111°30′35″W
Area3,529 acres (14.28 km2)[1]
CreatedNovember 30, 1915 (1915-November-30)
Visitors167,736 (in 2018)[2]
Governing bodyNational Park Service
WebsiteWalnut Canyon National Monument
Walnut Canyon National Monument
Nearest cityFlagstaff, Arizona
Area2,249.5 acres (910.3 ha)
NRHP reference No.66000174[3]
Added to NRHPOctober 15, 1966

History
Cliff dwellings in Walnut Canyon
Click for larger version of map

Sinagua is Spanish for "without water", an acknowledgement that the Sinagua 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 AD - taking advantage of the natural recesses in the limestone cliff walls which were eroded over millions of years by flowing water.[4] 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.[5]

Panorama of the southern cliff dwellings which are inaccessible to visitors

There are other ruins in the 20-by-10-mile (32 by 16 km) area, but none are publicly accessible. Many more dwellings to 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 to the National Park Service on August 10, 1933.[6] As with all historic areas administered by the National Park Service, the national monument was listed on the National Register of Historic Places on October 15, 1966. At Walnut Canyon, there are trails for tourists to get a close view of the dwellings.[3]

Geology
Geological strata: Kaibab Limestone, Toroweap Formation, and Coconino Sandstone

Walnut Canyon lies on the Colorado Plateau and cuts through the Permian Kaibab Limestone, which exposes the Toroweap Formation and Coconino Sandstone.[7] The Kaibab formation also forms the rim of the Grand Canyon. Crossbedding 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, echnocereus 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 that varies in layers and hardness, where the cliff dwellings are found, which overlies steep, scrub covered slopes of the Toroweap Formation, while the lowest third is the sheer-walled, cross-bedded Coconino Sandstone. 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.

Climate data for Walnut Canyon N.M. (1981–2010 normals)
Month Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec Year
Average high °F (°C) 45.1
(7.3)		 47.9
(8.8)		 54.6
(12.6)		 61.4
(16.3)		 71.7
(22.1)		 81.5
(27.5)		 85.0
(29.4)		 81.5
(27.5)		 77.2
(25.1)		 66.4
(19.1)		 54.7
(12.6)		 45.3
(7.4)		 64.4
(18.0)
Average low °F (°C) 17.2
(−8.2)		 22.4
(−5.3)		 26.6
(−3.0)		 32.7
(0.4)		 41.3
(5.2)		 49.0
(9.4)		 56.7
(13.7)		 54.3
(12.4)		 46.6
(8.1)		 33.9
(1.1)		 26.5
(−3.1)		 18.3
(−7.6)		 35.5
(1.9)
Average precipitation inches (mm) 1.79
(45)		 1.67
(42)		 1.58
(40)		 1.03
(26)		 0.52
(13)		 0.37
(9.4)		 2.43
(62)		 3.32
(84)		 2.04
(52)		 1.18
(30)		 1.36
(35)		 1.53
(39)		 18.82
(477.4)
Average snowfall inches (cm) 14.5
(37)		 13.5
(34)		 9.9
(25)		 5.9
(15)		 0.3
(0.76)		 0
(0)		 0
(0)		 0
(0)		 0
(0)		 0.9
(2.3)		 4.3
(11)		 9.5
(24)		 58.7
(149)
Average precipitation days (≥ 0.01 inch) 6.2 5.9 6.1 4.6 3.8 2.8 11.1 12.8 7.5 5.2 4.3 5.7 75.8
Average snowy days (≥ 0.1 inch) 3.6 4.1 3.1 1.7 0.2 0 0 0 0 0.4 1.6 3.6 18.3
Source: NOAA[8]

Operating hours and seasons
The Visitor Center

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 is listed on the National Register of Historic Places.[9]

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References
  1. "Listing of acreage as of December 31, 2011". Land Resource Division, National Park Service. Retrieved 2012-05-14.
  2. "NPS Annual Recreation Visits Report". National Park Service. Retrieved 2019-06-15.
  3. "National Register Information System". National Register of Historic Places. National Park Service. July 9, 2010.
  4. "Walnut Canyon National Monument". Arizona Gallery by Jacquie Lumb. Retrieved 8 April 2012.
  5. "Plants: Trees and Shrubs", United States National Park Service, 2006
  6. "History & Culture". Walnut Canyon. National Park Service.
  7. 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.
  8. "NowData - NOAA Online Weather Data". National Oceanic and Atmospheric Administration. Retrieved 2013-07-19.
  9. Holland, F. Ross (April 1972). "National Register of Historic Places Inventory - Nomination Form: Old Headquarters (B-13)". National Park Service. Retrieved 24 July 2012.
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