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Encyclopedia > Grand Canyon
Arizona Portal

The Grand Canyon is a steep-sided gorge carved by the Colorado River in the U.S. state of Arizona. It is largely contained within the Grand Canyon National Park — one of the first national parks in the United States. President Theodore Roosevelt was a major proponent of preservation of the Grand Canyon area, and visited on numerous occasions to hunt and enjoy the scenery. Image File history File links Portal. ... Grand Canyon may refer to: The Grand Canyon of the Colorado River, United States (the best-known Grand Canyon) Grand Canyon National Park, surrounding the canyon in Arizona Grand Canyon Village, Arizona, a community within the national park Grand Canyon of the Tuolumne, USA Grand Canyon of Pennsylvania, USA Grand... A gorge is a narrow passage between steep mountains or hills. ... The Colorado River from the bottom of Marble Canyon, in the Upper Grand Canyon Colorado River in the Grand Canyon from Desert View The Colorado River from Laughlin Horseshoe Bend is a horseshoe-shaped meander of the Colorado River located near the town of Page, Arizona The Colorado River is... For other uses of terms redirecting here, see US (disambiguation), USA (disambiguation), and United States (disambiguation) Motto In God We Trust(since 1956) (From Many, One; Latin, traditional) Anthem The Star-Spangled Banner Capital Washington, D.C. Largest city New York City National language English (de facto)1 Demonym American... Official language(s) English Spoken language(s) English 74. ... Grand Canyon National Park is one of the United States oldest national parks and is located in Arizona. ... This article is about national parks. ... For other persons named Theodore Roosevelt, see Theodore Roosevelt (disambiguation). ...

View from the South Rim.
View from the South Rim.

The longstanding scientific consensus has been that the canyon was created by the Colorado River over a period of six million years, but research released in 2008 suggests a much longer 17 million year[1] time span. The canyon is 277 miles (446 km) long, ranges in width from 4 to 18 miles (6.4 to 29 km) and attains a depth of more than a mile (1.6 km). Nearly two billion years of the Earth's history have been exposed as the Colorado River and its tributaries cut their channels through layer after layer of rock while the Colorado Plateau was uplifted. The "canyon started from the west, then another formed from the east, and the two broke through and met as a single majestic rent in the earth some six million years ago. [...] The merger apparently occurred where the river today, coming from the north, bends to the west, in the area known as the Kaibab Arch."[1] The Colorado River from the bottom of Marble Canyon, in the Upper Grand Canyon Colorado River in the Grand Canyon from Desert View The Colorado River from Laughlin Horseshoe Bend is a horseshoe-shaped meander of the Colorado River located near the town of Page, Arizona The Colorado River is... This article is about Earth as a planet. ... In physical geography, a channel is the physical confine of a river, slough or ocean strait consisting of a bed and banks. ... The Colorado Plateau, also called the Colorado Plateaus Province, is a physiographic region of the Intermontane Plateaus, roughly centered on the Four Corners region of the southwestern United States. ... A tectonic uplift is a geological process most often caused by plate tectonics which increases elevation. ...


During prehistory, the area was inhabited by Native Americans who built settlements within the canyon and its many caves. The Pueblo people considered the Grand Canyon ("Ongtupqa" in Hopi language) a holy site and made pilgrimages to it.[citation needed] This article is about the people indigenous to the United States. ... The Zia symbol is on the New Mexico state flag. ... Hopi is an Uto-Aztecan language spoken by the Hopi people of northeastern Arizona, USA, although today some Hopi are monolingual English speakers. ...


The first European known to have viewed the Grand Canyon was García López de Cárdenas from Spain, who arrived in 1540.[2] For other uses, see Europe (disambiguation). ... The son of Alonso de Cárdenas y doña Elvira de Figueroa and Maria García Osorio, Garcia Lopez de Cardenas was the comendador de Caravaca. ...


The Grand Canyon was largely unexplored until after the U.S. Civil War. In 1869, Major John Wesley Powell, a one-armed Civil War veteran with a thirst for science and adventure, made the first recorded journey through the canyon on the Colorado River. He accomplished this trek with nine men in four small wooden boats, though only six men completed the journey. Powell referred to the sedimentary rock units exposed in the canyon as "leaves in a great story book". The American Civil War was fought in the United States from 1861 until 1865 between the northern states, popularly referred to as the U.S., the Union, the North, or the Yankees; and the seceding southern states, commonly referred to as the Confederate States of America, the CSA, the Confederacy... John Wesley Powell, second Director of the USGS. Served from 1881-1894. ... Two types of sedimentary rock: limey shale overlaid by limestone. ...

Contents

Geography

View from the North Rim of the Grand Canyon
View from the North Rim of the Grand Canyon

The Grand Canyon is a massive rift in the Colorado Plateau that exposes uplifted Proterozoic and Paleozoic strata and is also one of the six distinct physiographic sections of the Colorado Plateau province. The Grand Canyon is unmatched throughout the world for the vistas it offers to visitors on the rim. It is not the deepest canyon in the world — both the Cotahuasi Canyon (11598 feet or 3535 m), Colca Canyon (10499 feet or 3200 m), both in Arequipa, Peru and Hell's Canyon on the Oregon-Idaho border are deeper — but Grand Canyon is known for its overwhelming size and its intricate and colorful landscape. Geologically it is significant because of the thick sequence of ancient rocks that are beautifully preserved and exposed in the walls of the canyon. These rock layers record much of the early geologic history of the North American continent. The Colorado Plateau, also called the Colorado Plateaus Province, is a physiographic region of the Intermontane Plateaus, roughly centered on the Four Corners region of the southwestern United States. ... The Proterozoic (IPA: ) is a geological eon representing a period before the first abundant complex life on Earth. ... The Paleozoic Era (from the Greek palaio, old and zoion, animals, meaning ancient life) is the earliest of three geologic eras of the Phanerozoic eon. ... Cotahuasi Canyon is considered deepest of the Americas. ... Colca Canyon is a canyon of the Colca River in southern Peru. ... For the cactus genus, see Oreocereus. ... Hells Canyon in Oregon Hells Canyon is a canyon created by the Snake River. ...

From the South Rim, November 2007.
From the South Rim, November 2007.

Uplift associated with mountain building events later moved these sediments thousands of feet upward and created the Colorado Plateau. The higher elevation has also resulted in greater precipitation in the Colorado River drainage area, but not enough to change the Grand Canyon area from being semi-arid. The uplift of the Colorado Plateau is uneven, and the north-south trending Kaibab Plateau that Grand Canyon bisects is over a thousand feet higher at the North Rim (about 1,000 ft/300 m) than at the South Rim. The fact that the Colorado River flows in a curve around the higher North Rim part of the Kaibab Plateau and closer to the South Rim part of the plateau is also explained by this asymmetry. Ivo Lucchitta of the U.S. Geological Survey first suggested that, as the Colorado River developed before significant erosion of the region, it naturally found its way across or around the Kaibab Uplift by following a "racetrack" path to the south of the highest part of the plateau. Almost all runoff from the North Rim (which also gets more rain and snow) flows toward the Grand Canyon, while much of the runoff on the plateau behind the South Rim flows away from the canyon (following the general tilt). The result is deeper and longer tributary washes and canyons on the north side and shorter and steeper side canyons on the south side. For other uses, see Mountain (disambiguation). ... Elevation histogram of the surface of the Earth – approximately 71% of the Earths surface is covered with water. ... The Colorado Plateau, also called the Colorado Plateaus Province, is a physiographic region of the Intermontane Plateaus, roughly centered on the Four Corners region of the southwestern United States. ... The Kaibab Plateau is located in northern Arizona in the United States. ... This article is about precipitation. ... For other uses, see Snow (disambiguation). ...


Temperatures on the North Rim are generally lower than the South Rim because of the greater elevation (averaging 8,000 ft/2,438 m above sea level).[3] Heavy rains are common on both rims during the summer months. Access to the North Rim via the primary route leading to the canyon (Arizona State Route 67) is limited during the winter season due to road closures. Views from the North Rim tend to give a better impression of the expanse of the canyon than those from the South Rim. Temperature is the physical property of a system which underlies the common notions of hot and cold; the material with the higher temperature is said to be hotter. ... State Route 67 (SR-67) is a forty-two mile, north-south state highway in northern Arizona. ...


Geology

The principal consensus among geologists is that the Colorado River basin (of which the Grand Canyon is a part) has developed in the past 40 million years. A recent study by geologists at the University of New Mexico, led by Victor Polyak, places the origins of the canyon beginning some 17 million years ago. Previous estimates had placed the age of the canyon at 5 to 6 million years. The study, which was published in 2008 in the journal Science, was conducted with the help of the National Science Foundation and utilized uranium-lead dating to analyze calcite deposits found on the walls of nine caves throughout the canyon. [4] There is a substantial amount of controversy because this research suggests a such substantial departure from prior widely supported scientific belief.[5] As of 2008 this research is too new to consider the scientific consensus settled. The Grand Canyon from Navajo Point. ... The University of New Mexico (UNM) is a public university in Albuquerque, New Mexico. ... 2008 (MMVIII) is the current year, a leap year that started on Tuesday of the Anno Domini (or common era), in accordance to the Gregorian calendar. ... Science is the journal of the American Association for the Advancement of Science (AAAS). ... The logo of the National Science Foundation The National Science Foundation (NSF) is an independent United States government agency that supports fundamental research and education in all the non-medical fields of science and engineering. ... Radiometric dating is a technique used to date materials based on a knowledge of the decay rates of naturally occurring isotopes, and the current abundances. ... Doubly refracting Calcite from Iceberg claim, Dixon, New Mexico. ...


The result of all this erosion is one of the most complete geologic columns on the planet. For morphological image processing operations, see Erosion (morphology). ...

Looking down Bright Angel trail to the Grand Canyon. The green area is Indian Gardens and the trail continues to Phantom Ranch at the river where a suspension bridge allows access to the North Rim.
Looking down Bright Angel trail to the Grand Canyon. The green area is Indian Gardens and the trail continues to Phantom Ranch at the river where a suspension bridge allows access to the North Rim.

The major geologic exposures in Grand Canyon range in age from the 2 billion year old Vishnu Schist at the bottom of the Inner Gorge to the 230 million year old Kaibab Limestone on the Rim. Interestingly, there is a gap of about one billion years between the stratum that is about 500 million years old and the lower level, which is about 1.5 billion years old. That indicates a period of erosion between two periods of deposition. Image File history File linksMetadata Size of this preview: 800 × 600 pixel Image in higher resolution (1600 × 1200 pixel, file size: 357 KB, MIME type: image/jpeg) The Grand Canyon File links The following pages on the English Wikipedia link to this file (pages on other projects are not listed... Image File history File linksMetadata Size of this preview: 800 × 600 pixel Image in higher resolution (1600 × 1200 pixel, file size: 357 KB, MIME type: image/jpeg) The Grand Canyon File links The following pages on the English Wikipedia link to this file (pages on other projects are not listed... Phantom Ranch is the lodge at the bottom of the Grand Canyon. ...


Many of the formations were deposited in warm shallow seas, near-shore environments (such as beaches), and swamps as the seashore repeatedly advanced and retreated over the edge of a proto-North America. Major exceptions include the Permian Coconino Sandstone, which most (though not all)[6][7][8][9][10] geologists claim was laid down as sand dunes in a desert, and several parts of the Supai Group. Interstate road cut through limestone and shale strata in eastern Tennessee In geology and related fields, a stratum (plural: strata) is a layer of rock or soil with internally consistent characteristics that distinguishes it from contiguous layers. ... For other uses, see Beach (disambiguation). ... This article does not cite any references or sources. ... North American redirects here. ... Coconino Sandstone at the Chute of Muddy Creek, Utah Coconino Sandstone is a geologic formation that spreads across the Colorado Plateau province of the United States, including northern Arizona, northwest Colorado, Nevada, and Utah. ... This article is about the sand formations, for other meanings see Dune (disambiguation) Mesquite Flat Dunes in Death Valley National Park In physical geography, a dune is a hill of sand built by eolian (wind-related) processes. ... This article is about arid terrain. ...


The great depth of the Grand Canyon and especially the height of its strata (most of which formed below sea level) can be attributed to 5,000 to 10,000 feet (1500 to 3000 m) of uplift of the Colorado Plateau, starting about 65 million years ago (during the Laramide Orogeny). This uplift has steepened the stream gradient of the Colorado River and its tributaries, which in turn has increased their speed and thus their ability to cut through rock (see the elevation summary of the Colorado River for present conditions). For considerations of sea level change, in particular rise associated with possible global warming, see sea level rise. ... The Laramide orogeny was a period of mountain building in western North America, which started in the Late Cretaceous, 70 to 80 million years ago, and ended 35 to 55 million years ago. ... Stream gradient is the ratio of drop in a stream per unit distance, usually expressed as feet per mile or meters per kilometer. ... The Colorado River from the bottom of Marble Canyon, in the Upper Grand Canyon Colorado River in the Grand Canyon from Desert View The Colorado River from Laughlin Horseshoe Bend is a horseshoe-shaped meander of the Colorado River located near the town of Page, Arizona The Colorado River is...


Weather conditions during the ice ages also increased the amount of water in the Colorado River drainage system. The ancestral Colorado River responded by cutting its channel faster and deeper. Variations in CO2, temperature and dust from the Vostok ice core over the last 400 000 years For the animated movie, see Ice Age (movie). ...


The base level and course of the Colorado River (or its ancestral equivalent) changed 5.3 million years ago when the Gulf of California opened and lowered the river's base level (its lowest point). This increased the rate of erosion and cut nearly all of the Grand Canyon's current depth by 1.2 million years ago. The terraced walls of the canyon were created by differential erosion.[11] The Gulf of California (also known as the Sea of Cortez or Sea of Cortés; locally known in the Spanish language as Mar de Cortés or, much less frequently, Golfo de California) is a body of water that separates the Baja California Peninsula from the Mexican mainland. ... The base level of a river or stream is the lowest point to which it can flow, often referred to as the mouth of the river. ...


About one million years ago, volcanic activity (mostly near the western canyon area) deposited ash and lava over the area, which at times completely obstructed the river. These volcanic rocks are the youngest in the canyon. Cleveland Volcano in the Aleutian Islands of Alaska photographed from the International Space Station For other uses, see Volcano (disambiguation). ... Ash plume from Mt Cleveland, a stratovolcano Diamond Head, a well-known backdrop to Waikiki in Hawaii, is an ash cone that solidified into tuff Volcanic ash consists of very fine rock and mineral particles less than 2 mm in diameter that are ejected from a volcanic vent. ... Look up lava, Aa, pahoehoe in Wiktionary, the free dictionary. ...


Human history

A view of the Colorado River flowing through the Grand Canyon.
A view of the Colorado River flowing through the Grand Canyon.

The known history of the Grand Canyon area stretches back 10,500 years when the first evidence for human presence in the area started. ... The Colorado River from the bottom of Marble Canyon, in the Upper Grand Canyon Colorado River in the Grand Canyon from Desert View The Colorado River from Laughlin Horseshoe Bend is a horseshoe-shaped meander of the Colorado River located near the town of Page, Arizona The Colorado River is...

The Ancestral Puebloans (The Ancient Ones, or Anasazi)

The Grand Canyon, as seen from river-level.
The Grand Canyon, as seen from river-level.

Ancient Pueblo People, or Ancestral Puebloans is the preferred term for the group of peoples often known as Anasazi who are the ancestors of the modern Pueblo peoples. ... The Grand Canyon from Navajo Point. ... Bright Angel Trail is a hiking trail inside Grand Canyon National Park in the U.S. state of Arizona. ... Cliff Palace, Mesa Verde National Park White House Ruins, Canyon de Chelly National Monument Ancient Pueblo People or Ancestral Puebloans were a prehistoric Native American culture centered around the present-day Four Corners area of the Southwest United States, noted for their distinctive pottery and dwelling construction styles. ... Image File history File linksMetadata Download high-resolution version (2272x1704, 1249 KB) Summary A picture of the Marble Canyon section of the Grand Canyon, from river-level. ... Image File history File linksMetadata Download high-resolution version (2272x1704, 1249 KB) Summary A picture of the Marble Canyon section of the Grand Canyon, from river-level. ...

Other cultures

  • The Cohonina[12]
  • The Sinagua
  • The Pai (The People)
  • The Hualapai (The People of the Pine Trees)
  • The Havasupai (The People of the blue-green water)
  • The Paiutes (The Water People)
  • The Dineh (The People)

The Sinagua were a pre-Columbian cultural group occupying an area in central Arizona between the Little Colorado River and the Salt River (between Flagstaff and Phoenix, Arizona) including the Verde Valley and significant portions of the Mogollon Rim country between approximately 500 AD and 1425 AD. Some archaeologists have... The Hualapai are a tribe of Native Americans who live in the mountains of Arizona. ... Havasupai home, Arizona, 1887 Havasu Falls, located 2 miles further into the canyon from Supai The Havasupai (sometimes called Havasu Baaja) are a Native American tribe inhabiting the western Grand Canyon area in the U.S. state of Arizona. ... “Piute” redirects here. ... Map of the Navajo Nation The Navajo Nation (Diné in Navajo language) encompasses all things important to the Navajo. ...

European arrival and settlement

The Spanish explorers

In September 1540, under orders from the conquistador Francisco Vázquez de Coronado to search for the fabled Seven Cities of Cibola, Captain Garcia Lopez de Cardenas, along with Hopi guides and a small group of Spanish soldiers, traveled to the South Rim of the Grand Canyon between Desert View and Moran Point. Pablo de Melgrossa, Juan Galeras, and a third soldier descended some one third of the way into the Canyon until they were forced to return because of lack of water. In their report, they noted that some of the rocks in the Canyon were "bigger than the great tower of Seville."[13] It is speculated that their Hopi guides must have been reluctant to lead them to the river, since they must have known routes to the canyon floor. Afterwards, no Europeans visited the Canyon for over two hundred years. A Conquistador (Spanish: []) (English: Conqueror) was a Spanish soldier, explorer and adventurer who took part in the gradual invasion and conquering of much of the Americas and Asia Pacific, bringing them under Spanish colonial rule between the 15th and 19th centuries. ... This article or section does not cite its references or sources. ... For the real places of this name, see Cibola, Arizona and Cibola County, New Mexico. ... The son of Alonso de Cárdenas y doña Elvira de Figueroa and Maria García Osorio, Garcia Lopez de Cardenas was the comendador de Caravaca. ... Moki redirects here. ...


Fathers Francisco Atanasio Domínguez and Silvestre Vélez de Escalante were two Spanish Priests who, with a group of Spanish soldiers, explored southern Utah and traveled along the North Rim of the Canyon in Glen and Marble Canyons in search of a route from Santa Fe to California in 1776. They eventually found a crossing at present-day Lees Ferry. Francisco Atanasio Domínguez was a Franciscan missionary and explorer of the Southwest United States in 1776. ... The route of the Dominguez-Escalante Expedition of 1776 Painting of Dominguez-Escalante Expedition found in the Utah State Capitol building Silvestre Vélez de Escalante was a Franciscan missionary and explorer of the Southwest United States during the late 18th century. ... This article is about the U.S. state. ... Nickname: Location in Santa Fe County, New Mexico Coordinates: , Country State County Santa Fe Founded ca. ... This article is about the U.S. state. ... Lees Ferry is named after John D. Lee a Mormon settler who established a ferry crossing on the Colorado River near Page, Arizona. ...


Also in 1776, Fray Francisco Garces, a Franciscan missionary, spent a week near Havasupai, unsuccessfully attempting to convert a band of Indians. He described the Canyon as "profound".[13] Jacob Hamblin (a Mormon missionary) was sent by Brigham Young in the 1850s to locate easy river crossing sites in the Canyon. Building good relations with local Native Americans and white settlers, he discovered Lee's Ferry in 1858 and Pierce Ferry (later operated by, and named for, Harrison Pierce) - the only two sites suitable for ferry operation.[citation needed] He also acted as an advisor to John Wesley Powell before his second expedition to the Grand Canyon, acting as a diplomat between Powell and the local native tribes to ensure the safety of his party. Jacob Hamblin (April 6, 1819 – August 31, 1886) was a Western pioneer, Mormon missionary, and diplomat to various Native American Tribes of the Southwest and Great Basin. ... This article is about the history and use of the word Mormon. For information about the religious beliefs and culture of Mormons, see Mormonism. ... Brigham Young (June 1, 1801 – August 29, 1877) was a leader in the Latter Day Saint movement and was the president of The Church of Jesus Christ of Latter-day Saints from 1847 until his death. ... This article is about the people indigenous to the United States. ... Lees Ferry is named after John D. Lee a Mormon settler who established a ferry crossing on the Colorado River near Page, Arizona. ... John Wesley Powell, second Director of the USGS. Served from 1881-1894. ...


In 1857 Edward Fitzgerald Beale superintendent of an expedition to survey a wagon road along the 35th parallel from Fort Defiance to the Colorado river led a small party of men in search of water on the Coconino plateau on the south rim of the Grand Canyon. On September 19th near present day National Canyon they came upon what May Humphreys Stacey described in his journal as "...a wonderful canyon four thousand feet deep. Everyone (in the party) admitted that he never before saw anything to match or equal this astonishing natural curiosity." US Brigadier General Edward Fitzgerald Ned Beale (February 4, 1822 - April 22, 1893) is best known for his carrying out former Secretary of War Jefferson Davis Camel Corps experiment in the Coachella Valley of California. ...


Also in 1857, the U.S. War Department asked Lieutenant Joseph Ives to lead an expedition to assess the feasibility of an up-river navigation from the Gulf of California. Also in a stern wheeler steamboat "Explorer", after two months and 350 miles (560 km) of difficult navigation, his party reached Black Canyon some two months after George Johnson.[citation needed] The "Explorer" struck a rock and was abandoned. Ives led his party east into the Canyon — they were the first Europeans to travel the Diamond Creek drainage and traveled eastwards along the South Rim. Line drawing of the Department of Wars seal. ...


In 1858, John Strong Newberry became probably the first geologist to visit the Grand Canyon. John Strong Newberry (1822 - 1892) was a U.S. geologist. ...

  • The John Wesley Powell River Expeditions
  • The Brown-Stanton River Expedition
  • Other expeditions

John Wesley Powell, second Director of the USGS. Served from 1881-1894. ...

Settlers in and near the canyon

Seth Tanner (1828-1918) was a Mormon settler who established the Tanner Trail in the Grand Canyon National Park. ... Charles Spencer is a current American Football offensive guard for the Houston Texans. ... D. W. James Mooney (d. ... John D. Lee (September 12, 1812 - March 23, 1877) was a prominent, early Latter-day Saint (LDS or Mormon) and central figure in the Mountain Meadows Massacre. ... It has been suggested that this article or section be merged with John Doyle Lee. ... Charles Spencer is a current American Football offensive guard for the Houston Texans. ... Mary Jane Elizabeth Colter (April 4, 1869 Pittsburgh, Pennsylvania – 1958), American architect. ... Ralph H. Cameron Ralph Henry Cameron (October 21, 1863–February 12, 1953) was an American Republican politician, and a delegate and Senator from the state of Arizona. ...

Federal protection

The federal government administrators who manage park resources face many challenges. These include issues related to the recent reintroduction into the wild of the highly endangered California Condor, air tour overflight noise levels, water rights disputes with various tribal reservations that border the park, and forest fire management. The Grand Canyon National Park superintendent is Steve Martin. Martin was named superintendent on February 5, 2007 to replace retiring superintendent Joe Alston. Martin was previously the National Park Service Deputy Director and superintendent of several other national parks including Denali and Grand Teton.[14] Another recent administrative challenge involves a controversy over the sale in Park bookstores of a creationist book claiming the Grand Canyon was created by Noah's Flood 4500 years ago, which disagrees with the actual timeframe and evidence.[15] Binomial name (Shaw, 1797) Synonyms Genus-level: Antillovultur Arredondo, 1976 Pseudogryphus Species-level: Vultur californianus Shaw, 1797 Gymnogyps amplus L. H. Miller, 1911 The California Condor, Gymnogyps californianus, is a species of North American bird in the New World vulture family Cathartidae. ... Denali National Park Denali National Park and Preserve is located in Interior Alaska and contains Mount McKinley, the tallest mountain in North America. ... Grand Teton National Park is a United States National Park located in western Wyoming, south of Yellowstone National Park. ... Creationism is generally the belief that the universe was created by a deity, or alternatively by one or more powerful and intelligent beings. ... This article is about the biblical Noah. ...


South Rim buildings

There are several historical buildings located along the South Rim; most are in Grand Canyon Village. Grand Canyon Village is a census-designated place located right on the south rim of the Grand Canyon, in Coconino County, Arizona. ...

Buckey O'Neill Cabin was built during the 1890s by William Owen O'Neill. He built the cabin because of a copper deposit that was nearby. He had several occupations such as miner, judge, politician, author and tour guide. This cabin is the longest continually standing structure in the South Rim. It is currently used as a guest house; booking is required well in advance. Image File history File links Yavapai_Observation_Station. ... Image File history File links Yavapai_Observation_Station. ... Desert View Watchtower Desert View Watchtower is a 70 foot high stone building located on the South Rim of the Grand Canyon within Grand Canyon National Park in Arizona, United States. ...


Kolb Studio was built in 1904 by brothers Ellsworth and Emery Kolb. They were photographers who made a living by photographing visitors walking down the Bright Angel Trail. In 1911, the Kolb brothers filmed their journey down the Green and Colorado Rivers. Emery Kolb showed this movie regularly in his studio until 1976, when he died at the age of 95. Today the building serves as an art gallery and exhibit. Bright Angel Trail is a hiking trail inside Grand Canyon National Park in the U.S. state of Arizona. ... Green River may refer to: Canada Green River (Whistler,BC), Runs out of Green Lake and heads toward Pemberton. ... The Colorado River from the bottom of Marble Canyon, in the Upper Grand Canyon Colorado River in the Grand Canyon from Desert View The Colorado River from Laughlin Horseshoe Bend is a horseshoe-shaped meander of the Colorado River located near the town of Page, Arizona The Colorado River is...


The El Tovar Hotel was built in 1905 and is the most luxurious lodging on the South Rim. The hotel consists of 4 stories with a rustic chalet appearance. It was designed by Charles Whittlesley. A gift shop and restaurant are located inside the hotel. An early view of the El Tovar Hotel. ...


Hopi House was built by Mary Jane Colter in 1905. It is based on structures that were built in an ancient Hopi settlement called Old Oraibi, located on the Third Mesa in eastern Arizona. It served as a residence for the Hopi Indians who sold arts and crafts to visitors in the South Rim. Orayvi, also called Oraibi, is a Hopi pueblo in Navajo in the U.S. state of Arizona. ...


Verkamp's Curios was built by John Verkamp in 1905. He sold arts and crafts as well as souvenirs. It is currently run by his descendants and stands next to the Hopi House. John Verkamp is a Veteran and former state Senator who is now running for Senate in Arizona. ...


Grand Canyon Railway Depot was built in 1909 and contains 2 levels. It is one of only three log-cabin-style train stations currently standing in the United States, of the fourteen ever built in the U.S. The depot is the northern terminus of the Grand Canyon Railway which begins in Williams, Arizona. The Grand Canyon Railway (AAR reporting mark GCRX), is a passenger railroad and heritage railway which operates between Williams, Arizona and the South Rim of Grand Canyon National Park. ... Williams is a city located in Coconino County, Arizona. ...


Lookout Studio was built in 1914 and is another structure that was designed by Mary Colter. Photography artwork, books, souvenirs, and rock and fossil specimens are sold here. A great view of Bright Angel Trail can be seen here. Lookout Studio is a stone building located on the South Rim of the Grand Canyon, within Grand Canyon National Park in Arizona. ...


Desert View Watchtower was built in 1932 and is one of Mary Colter's best-known works. Situated at the far eastern end of the South Rim, 27 miles (43 km) from Grand Canyon Village, the tower sits on a 7,400 foot (2,256 m) promontory. It offers one of the few views of the bottom of the Canyon and the Colorado River. It is designed to mimic an Anasazi watchtower though it is larger than existing ones.[16] Desert View Watchtower Desert View Watchtower is a 70 foot high stone building located on the South Rim of the Grand Canyon within Grand Canyon National Park in Arizona, United States. ... Ancient Pueblo People, or Ancestral Puebloans is the preferred term for the group of peoples often known as Anasazi who are the ancestors of the modern Pueblo peoples. ...


Bright Angel Lodge was built of logs and stone in 1935. Mary Colter designed the lodge and it was built by Fred Harvey. Inside the lodge is a small museum honoring Fred Harvey, who played a major role in popularizing the Grand Canyon. In the history room is a fireplace that is made of stone from the South Rim that is layered in the same sequence as in the canyon. Mary Jane Elizabeth Colter (April 4, 1869 Pittsburgh, Pennsylvania – 1958), American architect. ... Frederick Henry Harvey (June 27, 1835–February 9, 1901) was an entrepreneur who developed the Harvey House lunch rooms, restaurants, souvenir shops, and hotels, which served rail passengers on the Atchison, Topeka and Santa Fe Railway, the Gulf Coast and Santa Fe Railway, the Kansas Pacific Railway, the St. ...


Ecosystem

Federal officials started a flood in the Grand Canyon in hopes of restoring its ecosystem on March 5, 2008. The canyon's ecosystem was permanently changed after the construction of the Glen Canyon Dam in 1963.[17] For other uses, see Ecological Systems Theory. ... This article is about the day. ... 2008 (MMVIII) is the current year, a leap year that started on Tuesday of the Anno Domini (or common era), in accordance to the Gregorian calendar. ... Glen Canyon Dam on 19 June 2005. ... For other uses, see 1963 (disambiguation). ...


Weather

Weather in the Grand Canyon varies according to elevation.

A storm over the Grand Canyon
A storm over the Grand Canyon

The forested rims are high enough to receive winter snowfall, but along the Colorado River in the Inner Gorge, temperatures are similar to those found in Tucson and other low elevation desert locations in Arizona. Conditions in the Grand Canyon region are generally dry, but substantial precipitation occurs twice annually, during seasonal pattern shifts in winter (when Pacific storms usually deliver widespread, moderate rain and high-elevation snow to the region from the west) and in late summer (a phenomenon known as the "monsoon", which delivers waves of moisture from the southeast, causing dramatic, localized thunderstorms fueled by the heat of the day).[18] Average annual precipitation on the South Rim is less than 16 inches (35 cm), with 60 inches (132 cm) of snow, the higher North Rim usually receives 27 inches (59 cm) of moisture, with a typical snowfall of 144 inches (317 cm), and Phantom Ranch, far below the Canyon's rims along the Colorado River at 2,500 feet (762 m) gets just 8 inches (17.6 cm) of rain, and snow is a rarity. For other uses, see Monsoon (disambiguation). ...

Grand Canyon covered with snow

Temperatures vary wildly throughout the year, with summer highs within the Inner Gorge commonly exceeding 100 °F (37.8 °C) and winter minimum temperatures sometimes falling below zero degrees Fahrenheit (-17.8 °C) along the canyon's rims.[18] Visitors are often surprised by these potentially extreme conditions, and this, along with the high altitude of the canyon's rims, can lead to unpleasant side effects such as dehydration, sunburn, and hypothermia. Be prepared for a variety of potential weather conditions when visiting, and keep in mind the Grand Canyon is a rugged natural feature located in a remote area subject to a wide range of environmental hazards. For other uses, see Fahrenheit (disambiguation). ... Dehydration (hypohydration) is the removal of water (hydro in ancient Greek) from an object. ... Hypothermia is a condition in which an organisms temperature drops below that Required fOr normal metabolism and Bodily functionS. In warm-blooded animals, core [[body Temperature]] is maintained nEar a constant leVel through biologic [[homEostasis]]. But wheN the body iS exposed to cold Its internal mechanismS may be unable...


Weather conditions can greatly affect hiking and canyon exploration, and visitors should obtain accurate forecasts because of hazards posed by exposure to extreme temperatures, winter storms and late summer monsoons. While the park service posts weather information at gates and visitor centers, this is a rough approximation only, and should not be relied upon for trip planning. For accurate weather in the Canyon, hikers should consult the National Weather Service's NOAA weather radio or the official NWS website.[19] The National Oceanic and Atmospheric Administration (NOAA) is a scientific agency of the United States Department of Commerce focused on the conditions of the oceans and the atmosphere. ... For other uses, see NWS (disambiguation). ...

Two hikers looking down on the Grand Canyon
Two hikers looking down on the Grand Canyon

Public Domain image from National Park Service Website File history Legend: (cur) = this is the current file, (del) = delete this old version, (rev) = revert to this old version. ... Public Domain image from National Park Service Website File history Legend: (cur) = this is the current file, (del) = delete this old version, (rev) = revert to this old version. ...

Air pollution

The Grand Canyon has suffered some problems with air pollution, attributed to the nearby Navajo Generating Station, a coal-burning power plant. In 1991 an agreement was reached with the Navajo Generating Station in Page, Arizona to add air pollution control devices to their smokestacks.[20] Air pollution is the modification of the natural characteristics of the atmosphere by a chemical, particulate matter, or biological agent. ... Navajo Generating Station is a coal-fired powerplant with a power of 2280 megawatts at Page, Arizona, USA. Navajo Generating Station has three 236 meter high chimneys, which are the tallest structures in Arizona. ... Page is a city located in Coconino County, Arizona near Glen Canyon Dam and Lake Powell. ...


Grand Canyon tourism

Grand Canyon National Park is one of the world’s premier natural attractions, attracting about five million visitors per year. Overall, 83% were from the United States: California (12.2%), Arizona (8.9%), Texas (4.8%), Florida (3.4%) and New York (3.2%) represented the top domestic visitors. Seventeen percent of visitors were from outside the United States; the most prominently represented nations were the United Kingdom (3.8%), Canada (3.5%), Japan (2.1%), Germany (1.9%) and The Netherlands (1.2%).[21]


Activities

Further information: Grand Canyon travel guide from Wikitravel
A view of Grand Canyon Skywalk from Outside Ledge
A view of Grand Canyon Skywalk from Outside Ledge

Aside from casual sightseeing from the South Rim (averaging 7000 feet (2100 meters) above sea level), whitewater rafting, hiking and running are especially popular. The floor of the valley is accessible by foot, muleback, or by boat or raft from upriver. Hiking down to the river and back up to the rim in one day is discouraged by park officials because of the distance, steep and rocky trails, change in elevation, and danger of heat exhaustion from the much higher temperatures at the bottom. Rescues are required annually of unsuccessful rim-to-river-to-rim travelers. Nevertheless, hundreds of fit and experienced hikers complete the trip every year. Wikitravel is a project to create an open content, complete, up-to-date, and reliable world-wide travel guide. ... Image File history File linksMetadata No higher resolution available. ... Image File history File linksMetadata No higher resolution available. ... Skywalk from Outside Ledge The Grand Canyon Skywalk is a tourist attraction along the Colorado River on the edge of the Grand Canyon (Grand Canyon West) in the U.S. state of Arizona. ... Rafting is a recreational activity utilizing a raft to navigate a river or other body of water. ... Hyperthermia is an acute condition resulting from excessive exposure to heat, it is also known as heat stroke or sunstroke. ...

Helicopter used for tourist flights over the Grand Canyon (photo taken during 1985)
Helicopter used for tourist flights over the Grand Canyon (photo taken during 1985)

Camping on the North and South Rims is generally restricted to established campgrounds and reservations are highly recommended, especially at the busier South Rim. All overnight camping below the rim requires a backcountry permit from the Backcountry Country Office (BCO). Each year Grand Canyon National Park receives approximately 30,000 requests for backcountry permits. The park issues 13,000 permits, and close to 40,000 people camp overnight.[22] The earliest a permit application is accepted is the first of the month, four months prior to the proposed start month. Applying as soon as allowed will improve your chances of obtaining an overnight backcountry use permit for the dates of your choice. Image File history File links Size of this preview: 602 × 600 pixelsFull resolution (747 × 744 pixel, file size: 64 KB, MIME type: image/jpeg) I, the creator of this work, hereby release it into the public domain. ... Image File history File links Size of this preview: 602 × 600 pixelsFull resolution (747 × 744 pixel, file size: 64 KB, MIME type: image/jpeg) I, the creator of this work, hereby release it into the public domain. ...


Tourists wishing for a more vertical perspective can board helicopters and small airplanes in Las Vegas and Phoenix for canyon flyovers. Scenic flights are no longer allowed to fly within 1500' of the rim within the national park. The last aerial video footage from below the rim was filmed in 1984. However, some helicopter flights land on the Havasupai and Hualapai Indian Reservations within Grand Canyon (outside of the park boundaries). Recently, the Hualapai Tribe opened the glass-bottomed Grand Canyon Skywalk on their property, Grand Canyon West. The Skywalk has seen mixed reviews since the site is only accessible by driving down a 14-mile (23 km) dirt road, costs a minimum of $85 in total for reservation fees, a tour package and admission to the Skywalk itself and the fact that cameras are not permitted on the Skywalk at any time. The Skywalk is located 242 miles from the South Rim National Park. Many people mistake the west side of the park by Hermit's Rest as the location of the Skywalk. This however is incorrect information. However, the views of the canyon at the South Rim are better than you can get at the Skywalk, so that is one benefit to this common mistake. For other uses, see Helicopter (disambiguation). ... For further information, see Las Vegas metropolitan area and Las Vegas Strip. ... Nickname: Location in Maricopa County and the state of Arizona Coordinates: , Country State County Maricopa Incorporated February 25, 1881 Government  - Type Council-Manager  - Mayor Phil Gordon (D) Area  - City  515. ... Skywalk from Outside Ledge The Grand Canyon Skywalk is a tourist attraction along the Colorado River on the edge of the Grand Canyon (Grand Canyon West) in the U.S. state of Arizona. ...


Viewing the canyon

Lipan Point is a promontory located on the South Rim. This point is located to the east of the Grand Canyon Village along the Desert View Drive. There is a parking lot for visitors who care to drive along with the Canyon's bus service that routinely stops at the point. The trailhead to the Tanner Trail is located just before the parking lot. The view from Lipan Point shows a wide array of rock strata and the Unkar Creek area in the inner canyon. Grand Canyon Village is a census-designated place located right on the south rim of the Grand Canyon, in Coconino County, Arizona. ... This article or section does not cite its references or sources. ...


Perhaps the most heart-stopping view of the canyon is had from the Toroweap Overlook (Tuweep) situated 3000 vertical feet above the Colorado River, about 50 miles downriver from the South Rim and 70 upriver from the Grand Canyon Skywalk. This region — “One of the most remote in the United States” — according to the National Park Service, is reached only by one of three lengthy dirt tracks, that start from St. George, Utah, Colorado City or near Pipe Spring National Monument (both in Arizona). These roads traverse wild, uninhabited land for 97, 62 and 64 miles respectively. A visit to this area can be challenging, but rewarding. The Park Service manages the area for its primitive values and, therefore, improvements and services are minimal. Skywalk from Outside Ledge The Grand Canyon Skywalk is a tourist attraction along the Colorado River on the edge of the Grand Canyon (Grand Canyon West) in the U.S. state of Arizona. ... Nickname: Settled 1861 Incorporated 1862 Government  - Mayor Dan McArthur  - City Manager Gary Esplin Area  - City  64. ...


Grand Canyon fatalities

Grand Canyon rescue Helicopter, 1978
Grand Canyon rescue Helicopter, 1978

About 600 deaths have occurred in the Grand Canyon since the 1870s. Some of these deaths occurred as the result of overly zealous photographic endeavors, some were the result of airplane collisions within the canyon, and some visitors drowned in the Colorado River. Many hikers overestimate their fitness level, become dehydrated and confused, and must be rescued. The Park Service now posts a picture of an attractive and fit young man at several trailheads with the caption "Every year we rescue hundreds of people from the Canyon. Most of them look like him", in an attempt to discourage hikers from feats which are beyond their abilities. Image File history File links GrandCanyonRescueHelicopter1978. ... Image File history File links GrandCanyonRescueHelicopter1978. ...


According to Over the Edge: Death in the Grand Canyon, 50 fatalities have resulted from falls; 65 deaths were attributable to environmental causes, including heat stroke, cardiac arrest, dehydration, and hypothermia; 7 were caught in flash floods; 79 were drowned in the Colorado River; 242 perished in airplane and helicopter crashes (128 of them in the 1956 disaster mentioned below); 25 died in freak errors and accidents, including lightning strikes and rock falls; 47 committed suicide; and 23 were the victims of homicides.


1956 air disaster

Main article: 1956 Grand Canyon mid-air collision

In 1956 the Grand Canyon was the site of the deadliest commercial aviation disaster in the United States at the time. United Airlines Flight 718, Mainliner Vancouver, registration N6324C, was a Douglas DC-7 en route from Los Angeless International Airport to Chicago, Newark and Philadelphia on June 30, 1956. ...


On the morning of June 30, 1956, a TWA Lockheed Super Constellation and a United Airlines Douglas DC-7 departed Los Angeles International Airport within three minutes of one another on eastbound transcontinental flights. Approximately 90 minutes later, the two propeller-driven airliners collided above the canyon while both were flying in unmonitored airspace. is the 181st day of the year (182nd in leap years) in the Gregorian calendar. ... The Twa, also known as Batwa, are a pygmy people who were the oldest recorded inhabitants of the Great Lakes region of central Africa. ... TWA was one of the most well-known Constellation operators. ... United Airlines is a major airline of the United States. ... The Douglas DC-7 is an aircraft built by the Douglas Aircraft Company from 1953 to 1958. ...


The wreckage of both planes fell into the eastern portion of the canyon, on Temple and Chuar buttes, near the confluence of the Colorado and Little Colorado rivers. The disaster killed all 128 passengers and crew members aboard both planes.


This accident led to the institution of high-altitude flightways and positive control by en route ground controllers. For the Canadian musical group, see Air Traffic Control (band). ...


See also

The following is a list of major rapids and other notable features on the Colorado River, in order of their position downstream of Lees Ferry. ... Grand Canyon National Park is one of the United States oldest national parks and is located in Arizona. ... The following is a list of hiking trails that are, in whole or part, within the established boundaries of Grand Canyon National Park, located in Coconino and Mohave counties in the U.S. state of Arizona. ... The English language is a West Germanic language that originates in England. ... Colca Canyon is a canyon of the Colca River in southern Peru. ... Jacob Lake is a small unincorporated community on the Kaibab Plateau in Coconino County, Arizona, United States, at the junction of U.S. Route 89A and State Route 67. ...

Notes

  1. ^ a b New York Times article Grand Canyon Still Grand but Older published March 7, 2008 based on research by Victor Polyak, Carol Hill, and Yemane Asmerom, Science, Vol 319, 7 March 2008, pages 1377-1380.
  2. ^ History of the Colorado Plateau
  3. ^ Nature & Science. National Park Service (January 2007). Retrieved on 2007-03-29.
  4. ^ Wilford, John (2008-02-06). Study Says Grand Canyon Older Than Thought. New York Times. Retrieved on 2008-02-06.
  5. ^ Science Friday interview How Old is the Grand Canyon? (broadcast Friday, March 7th, 2008)
  6. ^ Geology Today, vol. 8(3), May–June 1992, pp, 78–79 (Wet tracks).
  7. ^ Monastersky, R., 1992. "Wading newts may explain enigmatic tracks." Science News, vol. 141 (1), p. 5.
  8. ^ Brand, L.R. and Tang, T., 1991. "Fossil vertebrate footprints in the Coconino Sandstone (Permian) of northern Arizona: Evidence for underwater origin." Geology, vol. 19, pp. 1201–1204.
  9. ^ Visher, G.S., 1990. Exploration Stratigraphy, 2nd edition, Penn Well Publishing Co., Tulsa, Oklahoma, pp. 211–213.
  10. ^ Kuenen, P.H. and Perdok, W.G., 1962. "Experimental abrasion - frosting and defrosting of quartz grains." Journal of Geology, vol. 70, pp. 648–658.
  11. ^ Definition and examples of differential erosion
  12. ^ Kaibab National Forest. USDA Forest Service. Retrieved on 2007-01-04.
  13. ^ a b Page Stegner (1994). Grand Canyon, The Great Abyss. HarperCollins, 25. ISBN 0-06-258564-9. 
  14. ^ Steve Martin named Superintendent of Grand Canyon National Park (PDF). National Park Service. Retrieved on 2007-02-20.
  15. ^ Faith-Based Parks?.
  16. ^ Grand Canyon Desert View Watchtower
  17. ^ Manmade flood roars through Grand Canyon. CNN. Retrieved on 2008-03-05.
  18. ^ a b Grand Canyon National Park Weather.
  19. ^ Flagstaff Weather Forecast Office. National Weather Service. Retrieved on 2007-01-04.
  20. ^ Trade Environment Database Projects: Grand Canyon Air Pollution
  21. ^ Executive Summary of Grand Canyon Tourism (PDF). Northern Arizona University. Retrieved on 2007-01-04.
  22. ^ Grand Canyon Backcountry Permit Page

Year 2007 (MMVII) is the current year, a common year starting on Monday of the Gregorian calendar and the AD/CE era in the 21st century. ... is the 88th day of the year (89th in leap years) in the Gregorian calendar. ... 2008 (MMVIII) is the current year, a leap year that started on Tuesday of the Anno Domini (or common era), in accordance to the Gregorian calendar. ... is the 37th day of the year in the Gregorian calendar. ... The New York Times is an internationally known daily newspaper published in New York City and distributed in the United States and many other nations worldwide. ... 2008 (MMVIII) is the current year, a leap year that started on Tuesday of the Anno Domini (or common era), in accordance to the Gregorian calendar. ... is the 37th day of the year in the Gregorian calendar. ... Year 2007 (MMVII) is the current year, a common year starting on Monday of the Gregorian calendar and the AD/CE era in the 21st century. ... is the 4th day of the year in the Gregorian calendar. ... Year 2007 (MMVII) is the current year, a common year starting on Monday of the Gregorian calendar and the AD/CE era in the 21st century. ... is the 51st day of the year in the Gregorian calendar. ... 2008 (MMVIII) is the current year, a leap year that started on Tuesday of the Anno Domini (or common era), in accordance to the Gregorian calendar. ... This article is about the day. ... Year 2007 (MMVII) is the current year, a common year starting on Monday of the Gregorian calendar and the AD/CE era in the 21st century. ... is the 4th day of the year in the Gregorian calendar. ... Year 2007 (MMVII) is the current year, a common year starting on Monday of the Gregorian calendar and the AD/CE era in the 21st century. ... is the 4th day of the year in the Gregorian calendar. ...

References

  • George Wuerthner (1998). Grand Canyon: A Visitor's Companion. Stackpole Books. 
  • Joseph Wood Krutch (1957). Grand Canyon: Today and All Its Yesterdays. 
  • Stephen J. Pyne (1998). How the Canyon Became Grand. Penguin. 
  • L. Greer Price (1999). An introduction to Grand Canyon Geology. Grand Canyon Association. ISBN 0-938216-68-6. 
  • Michael F. Anderson (2001). Along the Rim. Grand Canyon Association. ISBN 0-938216-75-9. 
  • Christa Sadler (2006). Life in Stone. Grand Canyon Association. ISBN 0-938216-81-3. 
  • Thomas M. Myers and Michael P. Ghiglieri (2001). Over the Edge: Death in Grand Canyon. Puma Press. ISBN 0-9700973-1-X. 
  • Macarthur Job (2001). Air Disaster Volume 4: The Propeller Era. Aerospace Publications. ISBN 1-875671-48-X. 
  • Edward Dolnick (2001). Down the Great Unknown : John Wesley Powell's 1869 Journey of Discovery and Tragedy Through the Grand Canyon. HarperCollins. 

Joseph Wood Krutch (November 25, 1893 - May 22, 1970) was an American writer, critic, and naturalist. ... Stephen J. Pyne is a professor in the School of Life Sciences at Arizona State University, specializing in the history of ecology, the history of exploration, and the history of fire. ... Edward Dolnick is an American writer, formerly the chief science writer at the Boston Globe. ...

External links

Wikimedia Commons has media related to:
Grand Canyon

Coordinates: 36.1° N 112.1° W* Map of Earth showing lines of latitude (horizontally) and longitude (vertically), Eckert VI projection; large version (pdf, 1. ...


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