D. W. Mooney

Last updated
D.W. "James" Mooney
Died1882
Occupation Prospector
Mooney Falls near Supai, AZ, where D.W. Mooney fell, now bears his name Mooney Falls, Arizona, 2006.jpg
Mooney Falls near Supai, AZ, where D.W. Mooney fell, now bears his name

D. W. "James" Mooney (died 1882) was a miner and an early explorer of the Grand Canyon. He fell to his death at Mooney Falls, a waterfall on the Havasupai Reservation in the Grand Canyon.


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<span class="mw-page-title-main">Grand Canyon National Park</span> National park in Arizona, United States

Grand Canyon National Park, located in northwestern Arizona, is the 15th site in the United States to have been named as a national park. The park's central feature is the Grand Canyon, a gorge of the Colorado River, which is often considered one of the Wonders of the World. The park, which covers 1,217,262 acres of unincorporated area in Coconino and Mohave counties, received more than six million recreational visitors in 2017, which is the second highest count of all American national parks after Great Smoky Mountains National Park. The Grand Canyon was designated a World Heritage Site by UNESCO in 1979. The park celebrated its 100th anniversary on February 26, 2019.

<span class="mw-page-title-main">Grand Canyon</span> Steep-sided canyon carved by the Colorado River in Arizona, United States

The Grand Canyon is a steep-sided canyon carved by the Colorado River in Arizona, United States. The Grand Canyon is 277 miles (446 km) long, up to 18 miles (29 km) wide and attains a depth of over a mile.

<span class="mw-page-title-main">Canyon</span> Deep ravine between cliffs

A canyon, 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 cut through underlying surfaces, eventually wearing away rock layers as sediments are removed downstream. A river bed will gradually reach a baseline elevation, which is the same elevation as the body of water into which the river drains. The processes of weathering and erosion will form canyons when the river's headwaters and estuary are at significantly different elevations, particularly through regions where softer rock layers are intermingled with harder layers more resistant to weathering.

<span class="mw-page-title-main">Grand Canyon Village, Arizona</span> Town in Arizona, United States

Grand Canyon Village is a census-designated place (CDP) located on the South Rim of the Grand Canyon, in Coconino County, Arizona, United States. Its population was 2,004 at the 2010 Census. Located in Grand Canyon National Park, it is wholly focused on accommodating tourists visiting the canyon. Its origins trace back to the railroad completed from Williams, to the canyon's South Rim by the Santa Fe Railroad in 1901. Many of the structures in use today date from that period. The village contains numerous landmark buildings, and its historic core is a National Historic Landmark District, designated for its outstanding implementation of town design.

<span class="mw-page-title-main">Geology of the Grand Canyon area</span> Aspect of geology

The geology of the Grand Canyon area includes one of the most complete and studied sequences of rock on Earth. The nearly 40 major sedimentary rock layers exposed in the Grand Canyon and in the Grand Canyon National Park area range in age from about 200 million to nearly 2 billion years old. Most were deposited in warm, shallow seas and near ancient, long-gone sea shores in western North America. Both marine and terrestrial sediments are represented, including lithified sand dunes from an extinct desert. There are at least 14 known unconformities in the geologic record found in the Grand Canyon.

<span class="mw-page-title-main">Colorado Plateau</span> Plateau in the Four Corners region of the Southwest United States

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<span class="mw-page-title-main">Havasupai</span> Indigenous ethnic group of Arizona, US

The Havasupai people are an American Indian tribe who have lived in the Grand Canyon for at least the past 800 years. Havasu means "blue-green water" and pai "people".

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The known human history of the Grand Canyon area stretches back 10,500 years, when the first evidence of human presence in the area is found. Native Americans have inhabited the Grand Canyon and the area now covered by Grand Canyon National Park for at least the last 4,000 of those years. Ancestral Pueblo peoples, first as the Basketmaker culture and later as the more familiar Pueblo people, developed from the Desert Culture as they became less nomadic and more dependent on agriculture. A similar culture, the Cochimi also lived in the canyon area. Drought in the late 13th century likely caused both groups to move on. Other people followed, including the Paiute, Cerbat, and the Navajo, only to be later forced onto reservations by the United States Government.

<span class="mw-page-title-main">Grand Canyon Railway</span> Historic railway to Grand Canyon National Park in Arizona

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Havasu Falls is a waterfall of Havasu Creek, located in the Grand Canyon, Arizona, United States. It is within Havasupai tribal lands.

<span class="mw-page-title-main">Grand Canyon University</span> Private, for-profit, Christian university in Phoenix, Arizona, U.S.

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<span class="mw-page-title-main">Havasupai Indian Reservation</span> Reservation

The Havasupai Indian Reservation is a Native American reservation for the Havasupai people, surrounded entirely by the Grand Canyon National Park, in Coconino County in Arizona, United States. It is considered one of America's most remote Indian reservations. The reservation is governed by a seven-member tribal council, led by a chairman who is elected from among the members of the council. The capital of the reservation is Supai, situated at the bottom of Cataract Canyon, one of the tributary canyons of the Grand Canyon. Havasupai is a combination of the words Havasu and pai, thus meaning "people of the blue-green waters".

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<span class="mw-page-title-main">Grand Canyon Scenic Airlines</span> Airline of the United States

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<span class="mw-page-title-main">Redwall Limestone</span> Mississippian age cliff-forming unit in the Grand Canyon, Arizona

The Redwall Limestone is a resistant cliff-forming unit of Mississippian age that forms prominent, red-stained cliffs in the Grand Canyon, ranging in height from 500 feet (150 m) to 800 feet (240 m).