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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.
CANYON DE CHELLY NATIONAL MONUMENT, Ariz. (AP) — Commercial air tours will soon be prohibited over Canyon de Chelly National Monument in northeastern Arizona under a plan approved this week by the Federal Aviation Administration and the National Park Service.
Map of the San Juan Basin showing the Chinle Creek Chinle Creek is a tributary stream of the San Juan River in Apache County, Arizona and San Juan County, Utah . Its source is at 36°53′40″N 109°44′37″W / 36.89444°N 109.74361°W / 36.89444; -109.74361 , the confluence of Laguña Creek and the Chinle Wash arroyo
The monument was established in 1931 primarily to preserve the archaeological sites and record of ancient human history. Canyon de Chelly is unique among the National Park Service units because the park is located entirely on Navajo tribal land, and it has a residential community in the canyon.
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.
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 ...
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