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According to the Köppen Climate Classification system, Canyon de Chelly has a cold semi-arid climate, abbreviated "BSk" on climate maps. The hottest temperature recorded in Canyon de Chelly was 105 °F (40.6 °C) on July 2, 2002, July 14, 2003, and June 21, 2016, while the coldest temperature recorded was −32 °F (−35.6 °C) on January 2 ...
Canyon de Chelly Ruins located in Canyon de Chelly National Monument: Awatovi: Navajo County: Ruins Bailey Ruin: Pinedale, Arizona: Ruins of a multistoried pueblo of 200–250 rooms, AD 1275–1325 (late Pueblo III Era and/or early Pueblo IV Era). Betatakin: Ancestral Pueblo Kayenta: Navajo Reservation: Grand house Ruins located at the Navajo ...
At Canyon de Chelly, the trail to White House Ruin, [7] descends through the Shinarump Conglomerate, but also has a tributary slot canyon landform with large accumulations of the Shinarump erosional debris on the slot-canyon floor. The trail then descends through the cross–bedded cliffs (fossil sand dunes) of the De Chelly Sandstone.
Chinle (Navajo: Chíńlį́) is a census-designated place (CDP) in Apache County, Arizona, United States.The name in Navajo means ' flowing out ' and is a reference to the location where the water flows out of the Canyon de Chelly. [3]
What is Canyon de Chelly National Monument? The park lies within the Four Corners region inside the Navajo Nation and is among the most visited national monuments in the United States. It's known for its soaring sandstone cliffs and 800-foot (244-meter) high Spider Rock spire.
At the roundabout, US 191 travels north to Chinle, where it intersects BIA Route 7, which provides access to Canyon de Chelly National Monument. [4] Continuing north, the route intersects BIA Route 59 in Many Farms, BIA Route 12 in Round Rock, and BIA Route 35 in Rock Point, before arriving at a T-intersection with US 160 near Mexican Water.
Canyons of Canyon de Chelly National Monument were cut by streams with headwaters in the Chuskas. The Chuska Mountains are sparsely populated. Nearby settlements are small, including Crystal, New Mexico, Lukachukai, Arizona, and Toadlena, New Mexico. Trading posts at Crystal and at Two Grey Hills (about 10 km east of Toadlena), are associated ...
The watershed origins also come from the southwest near Ganado, closer to the southwest Defiance Plateau perimeter. At Sawmill, northeast of Ganado is Bonito Canyon a northwest tributary to south-flowing Black Creek. The water divide separating the Chinle Creek watershed, (southeast, with Canyon de Chelly), is 3-mi [3] north-northeast of Sawmill.