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Canyon de Chelly National Monument (/ d ə ˈ ʃ eɪ / də-SHAY) was established on April 1, 1931, as a unit of the National Park Service.Located in northeastern Arizona, it is within the boundaries of the Navajo Nation and lies in the Four Corners region.
By 6 January, Carson was re-equipped and ready to move against Canyon de Chelly despite heavy snow. Carson had with him 389 troopers from the 1st New Mexico Cavalry . He divided his command, sending Captain Albert H. Pfeiffer into the east end of the canyon with 100 men, while Carson led the remaining 289 to the west end of the canyon.
The Thunderbird Lodge. The Thunderbird Lodge is a historic motel in Chinle, Arizona.The only lodging facility within Canyon de Chelly National Monument, a national monument established in 1931, it has grown out of an old trading post built in 1896, the Thunderbird Lodge Trading Post.
The north terminus region of the Defiance Plateau contains three canyons, with watercourses flowing due-west, as headwaters of Chinle Creek. The canyons are the Canyon de Chelly National Monument; two other canyons are southwest, part of the five canyon system, Little White House and Three Turkey Canyons.
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 ...
Its sources is in Canyon de Chelly National Monument where Canyon de Chelly and Canyon del Muerto have their confluence at an elevation of 5,616 feet at It then trends northwest to its confluence with Laguña Creek where it forms Chinle Creek, 7 miles northeast of Dennehotso, Arizona at an elevation of 4,774 feet (1,455 meters).
Massive, fallen Shinarump Conglomerate block (erosion-resistant) at start of trail (viewed up-trail) down to White House Ruin, Canyon De Chelly National Monument (Note: pictured beside smooth-sided cliffs of the underlying De Chelly Sandstone) The Shinarump Conglomerate is a geologic formation found in the Four Corners region of the United States.
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