|
Newton Butte
Newton Butte, in the Grand Canyon, Arizona, United States is a prominence below the South Rim, northwest of Grandview Point, and north on a ridgeline from Shoshone Point which is one mile east of Yaki Point, East Rim Drive. Shoshone Point and Yaki are both on access roads from East Rim Drive, with Yaki being the more advantageous to different viewing directions. Newton Butte is , and located on a point/ridge, just south of Granite Gorge on the Colorado River. The point location of Newton Butte extends due north from an intermediate point on the South Rim, Shoshone Point, which at the end of the Newton Butte point ridgeline, also forms the west perimeter of the ''Lonetree Canyon'' drainage, into Granite Gorge. Just north of Newton Butte, 3/4 mi on the end of the point, is Pattie Butte, a lower elevation prominence, . Two hiking trails are closest to Newton Butte. Across Granite Gorge, views south can be made from the Clear Creek Trail, at lower elevations or as it climbs pa ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Grand Canyon National Park
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 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. History The Grand Canyon became well known to Americans in the 1880s after railroads were built and pioneers developed infrastructure and early tourism. In 1903, President Theodore Roosevelt visited the site and said, The Grand Canyon fills me with awe. It is beyond comparison—beyond description; absolutely unparalleled ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Williams, Arizona
Williams ( yuf-x-hav, Wii Gvʼul) is a city in Coconino County, Arizona, United States, located west of Flagstaff. Its population was 3,023 at the 2010 census. It lies on the routes of Historic Route 66 and Interstate 40. It is also the southern terminus of the Grand Canyon Railway, which takes visitors to Grand Canyon Village. There are numerous inns, motels, restaurants and gas stations catering to the large influx of tourists rather than local residents, especially during the summer and holiday seasons. Also known as the "Gateway to the Grand Canyon", Williams was the last city on Historic Route 66 to be bypassed by Interstate 40. The community, bypassed on October 13, 1984, continues to thrive on tourism. Boasting seven fishing lakes in the area, hiking trails up Bill Williams Mountain and into Sycamore Canyon, an alpine ski area and cross country ski trails, four-seasons weather and an abundance of wildlife, Williams offers unlimited recreational opportunities for the out ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Landforms Of Coconino County, Arizona
A landform is a natural or anthropogenic land feature on the solid surface of the Earth or other planetary body. Landforms together make up a given terrain, and their arrangement in the landscape is known as topography. Landforms include hills, mountains, canyons, and valleys, as well as shoreline features such as bays, peninsulas, and seas, including submerged features such as mid-ocean ridges, volcanoes, and the great ocean basins. Physical characteristics Landforms are categorized by characteristic physical attributes such as elevation, slope, orientation, stratification, rock exposure and soil type. Gross physical features or landforms include intuitive elements such as berms, mounds, hills, ridges, cliffs, valleys, rivers, peninsulas, volcanoes, and numerous other structural and size-scaled (e.g. ponds vs. lakes, hills vs. mountains) elements including various kinds of inland and oceanic waterbodies and sub-surface features. Mountains, hills, plateaux, and plains are the fo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Grand Canyon, South Rim
Grand may refer to: People with the name * Grand (surname) * Grand L. Bush (born 1955), American actor * Grand Mixer DXT, American turntablist * Grand Puba (born 1966), American rapper Places * Grand, Oklahoma * Grand, Vosges, village and commune in France with Gallo-Roman amphitheatre * Grand Concourse (other), several places * Grand County (other), several places * Grand Geyser, Upper Geyser Basin of Yellowstone * Grand Rounds National Scenic Byway, a parkway system in Minneapolis, Minnesota, United States * Le Grand, California, census-designated place * Grand Staircase, a place in the US. Arts, entertainment, and media * ''Grand'' (Erin McKeown album), 2003 * ''Grand'' (Matt and Kim album), 2009 * ''Grand'' (magazine), a lifestyle magazine related to related to grandparents * ''Grand'' (TV series), American sitcom, 1990 * Grand piano, musical instrument * Grand Production, Serbian record label company * The Grand Tour, a new British automobile show Othe ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
The Howlands Butte
The Howlands Butte, elevation , is a minor butte in the southeast drainage of the very large Clear Creek drainage. Clear Creek is a medium length flowing creek, just upstream of the major Bright Angel Creek outfall into the Colorado River, Granite Gorge. The Howlands Butte was officially named in 1932 for brothers Seneca and Oramel G. Howland, members of the Powell Geographic Expedition of 1869. Just two days from the expedition's intended destination, the pair and William H. Dunn left the expedition, fearing they could not survive the dangers of the river much longer. They hiked out of the canyon and were never seen again. Separation Rapids on the river is where they departed from Powell. Gallery File:The Howlands Butte, Redwall Limestone, Grand Canyon (view from the South Rim).jpg, Howlands Butte, south aspect File:The Howlands Butte viewed from Clear Creek Trail.jpg, The Howlands Butte viewed from northwest on Clear Creek Trail File:Clear Creek Grand Canyon.jpg, Angels Gat ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Surprise Canyon Formation
The Surprise Canyon Formation is a geologic formation that consists of clastic and calcareous sedimentary rocks that fill paleovalleys and paleokarst of Late Mississippian (Serpukhovian) age in Grand Canyon. These strata outcrop as isolated, lens-shaped exposures of rocks that fill erosional valleys and locally topography and caves developed in the top of the Redwall Limestone. The Surprise Canyon Formation and associated unconformities represent a significant period of geologic time between the deposition of the Redwall Limestone and the overlying Supai Group.Hodnett, J.P.M. and Elliott, D.K., 2018. '' Carboniferous chondrichthyan assemblages from the Surprise Canyon and Watahomigi formations (latest Mississippian–Early Pennsylvanian) of the western Grand Canyon, Northern Arizona.'' ''Journal of Paleontology'', 92(S77), pp. 1–33.Billingsley, G.H., and Beus, S.S., 1985, ''The Surprise Canyon Formation—an upper Mississippian and Lower Pennsylvanian (?) rock unit in the Grand ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Redwall Limestone
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 to . Lithology Redwall Limestone consists predominantly of light-olive-gray to light-gray, fine- to coarse-grained, thin- to thick-bedded, often cherty, limestone. Its lower part consists of brownish-gray, interbedded finely crystalline dolomite and fine- to coarse-grained limestone with layers of white chert lenses and yellowish-gray and brownish-gray, cliff-forming, thick-bedded, fine-grained dolomite. It is divided into Horseshoe Mesa Member, Mooney Falls Member, Thunder Springs Member, and Whitmore Wash Member.Chronic, H (1983) ''Roadside Geology of Arizona.'' The Mountaineers Books, Seattle, Washington. (softcover, ) Its origins date to the Mississippian age. Contacts The upper and lower contacts of the Redwall Limestone are both unconformities. Locally, the Redwall Limestone directly overlies the unconformity ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kaibab Plateau
The Kaibab Plateau is a plateau almost entirely in Coconino County, Arizona (but extending slightly north into Kane County, Utah) in the Southwestern United States. The high plain is also known as the Buckskin Mountain, Buckskin Plateau, and Kaibab Mountain. Description The plateau, part of the larger Colorado Plateau, is bordered on the south by the Grand Canyon and reaches an elevation of . The plateau is divided between Kaibab National Forest and the "North Rim" portion of Grand Canyon National Park. Tributary canyons of the Colorado River form the plateau's eastern and western boundaries, and tiers of uplifted cliffs define the northern edges of the landform. Winter snowfall is often heavy (sometimes exceeding ), and this creates opportunities for backcountry Nordic skiing and snow camping. This broad feature is heavily forested with aspen, spruce- fir, ponderosa pine, and pinyon-juniper woodland, and stands in sharp contrast to the arid lowlands encircling it. The ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
O'Neill Butte
O'Neill Butte is a -elevation summit located in the Grand Canyon, in Coconino County of northern Arizona, United States. It is situated east-northeast of Grand Canyon Village, northeast of Mather Point, and one mile immediately northwest of Yaki Point. Cedar Ridge connects O'Neill Butte with Yaki Point on the South Rim. Topographic relief is significant as O'Neill Butte rises above the Colorado River in . Access to this prominence is via the South Kaibab Trail which traverses the east slope of the peak. According to the Köppen climate classification system, O'Neill Butte is located in a cold semi-arid climate zone. Geology The summit block of O'Neill Butte is composed of Permian Esplanade Sandstone, which is the uppermost member of the Pennsylvanian-Permian Supai Group. The rest of the Supai Group overlays Mississippian Redwall Limestone. The cliff-forming Redwall overlays the Cambrian Tonto Group, and below that Paleoproterozoic Vishnu Basement Rocks at river level in Gra ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Newberry Butte
Newberry Butte is a summit located in the Grand Canyon, in Coconino County, Arizona, Coconino County of northern Arizona, Southwestern United States, US. It is situated 4.5 miles north of the South Rim's Grandview Point, three miles southwest of Vishnu Temple (Grand Canyon), Vishnu Temple, and 2.5 miles south of Wotans Throne. Topographic relief is significant as it rises over above the Colorado River and Granite Gorge in one mile. According to the Köppen climate classification system, Newberry Butte is located in a Cold semi-arid climate zone. Etymology Newberry Butte is named for John Strong Newberry (1822–1892), the geologist for an 1858 expedition headed by Lieutenant Joseph Christmas Ives which explored the Colorado River up to the lower Grand Canyon. After returning, Newberry convinced fellow geologist John Wesley Powell that a boat run through the Grand Canyon to complete the survey would be worth the risk. Powell would later lead the Powell Geographic Exped ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lyell Butte
Lyell Butte is a elevation summit located in the Grand Canyon, in Coconino County of northern Arizona, United States. It is situated east of Grand Canyon Village, immediately east of and below Shoshone Point, and 1.5 mile southeast of Newton Butte, which is the nearest higher neighbor. Topographic relief is significant as Lyell Butte rises above the Colorado River in 1.5 mile (2.4 km). Access is via the Tonto Trail which traverses the base of the peak. According to the Köppen climate classification system, Lyell Butte is located in a cold semi-arid climate zone, with precipitation runoff draining northeast to the Colorado River via Grapevine and Boulder Creeks. History Lyell Butte was named in 1906 after Sir Charles Lyell (1797–1875), eminent Scottish geologist best known as the author of ''Principles of Geology''. This feature's name was officially adopted in 1906 by the U.S. Board on Geographic Names. The first ascent of Lyell Butte was made January 24, 1970, by Alan Doty ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Flagstaff, Arizona
Flagstaff ( ) is a city in, and the county seat of, Coconino County, Arizona, Coconino County in northern Arizona, in the southwestern United States. In 2019, the city's estimated population was 75,038. Flagstaff's combined metropolitan area has an estimated population of 139,097. Flagstaff lies near the southwestern edge of the Colorado Plateau and within the San Francisco volcanic field, along the western side of the largest contiguous Pinus ponderosa, ponderosa pine forest in the continental United States. The city sits at about and is next to Mount Elden, just south of the San Francisco Peaks, the highest mountain range in the state of Arizona. Humphreys Peak, the highest point in Arizona at , is about north of Flagstaff in Kachina Peaks WildernessThe geology of the Flagstaff areaincludes abundant volcanic rocks associated with the San Francisco Volcanic Field that range in age from late Miocene to late Holocene. It also includes exposed rock from the Mesozoic and Paleozoic ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
.jpg "Click for more on -> Landforms Of Coconino County, Arizona")
.svg "Click for more on -> Flagstaff, Arizona")