The Dragon (Arizona)
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The Dragon (Arizona)
The Dragon is a 8,105-foot-elevation summit located in the Grand Canyon, in Coconino County of Arizona, US. It is situated north of the Hindu Amphitheater, and about ~4.5 miles north-northwest of Shiva Temple, and ~2.5 mi north of Dragon Head. Both of the Dragon landforms are on a connected ridgeline, (Dragon Head being the ridgeline terminus), defining two south trending canyon watersheds – Dragon Creek, (east), and (Upper)- Crystal Creek (Arizona), (west).Aerial photos of The Dragon and Dragon Head were taken as Draft Environmental Impact Statement (DEIS) studies for public flight-path routes within the entire Grand Canyon. Geology & biology The geology of The Dragon prominence is a ~250 to 300 ft layer of cliff-forming, whitish Kaibab Limestone. Its hardness supports an approximately horizontal tableland of Ponderosa Pine forest. Below the Kaibab is an even larger unit of the slope-forming Toroweap Formation. The slope is modestly vegetated, and has large area ...
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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 ...
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Shiva Temple (Grand Canyon)
Shiva Temple is a summit located in the Grand Canyon, in Coconino County, Arizona, Coconino County of Arizona, Southwestern United States, US. It is situated six miles north of Hopi Point overlook of the canyon's South Rim, about 2.5 miles southwest of North Rim's Tiyo Point, and two miles northwest of Isis Temple, where it towers above the Colorado River. Shiva Temple is named for Shiva, the Hindu deity, destroyer of the universe. This name was applied by Clarence Dutton who began the tradition of naming geographical features in the Grand Canyon after mythological deities.Randy Moore and Kara Felicia Witt, ''The Grand Canyon: An Encyclopedia of Geography, History, and Culture'', 2018, ABC-CLIO Publisher, page 150. Dutton believed Shiva Temple was the largest, grandest, and most majestic of the Grand Canyon buttes, with a broad, level, forested top. This mountain's name was officially adopted in 1906 by the U.S. Board on Geographic Names. In 1937, the American Museum of Nat ...
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Mountains Of Arizona
Arizona is a landlocked state situated in the southwestern region of the United States of America. It has a vast and diverse geography famous for its deep canyons, high- and low-elevation deserts, numerous natural rock formations, and volcanic mountain ranges. Arizona shares land borders with Utah to the north, the Mexican state of Sonora to the south, New Mexico to the east, and Nevada to the northwest, as well as water borders with California and the Mexican state of Baja California to the southwest along the Colorado River. Arizona is also one of the Four Corners states and is diagonally adjacent to Colorado. Arizona has a total area of , making it the sixth largest U.S. state.Summary of 2000 Census
Table 17
Of this area, just 0.3% consists of water, which makes Arizona the state with the second lowest ...
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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 ...
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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 ...
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Slope-former
A slope-former is a unit of bedrock which is less resistant to erosion than overlying or underlying units and consequently results in outcrops with low relative slope angles. It may be contrasted with cliff-former. Typical slope forming lithologies include shales, and limestone Limestone ( calcium carbonate ) is a type of carbonate sedimentary rock which is the main source of the material lime. It is composed mostly of the minerals calcite and aragonite, which are different crystal forms of . Limestone forms whe ...s in humid environments. Geomorphology Erosion landforms {{geomorph-stub ...
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Ponderosa Pine
''Pinus ponderosa'', commonly known as the ponderosa pine, bull pine, blackjack pine, western yellow-pine, or filipinus pine is a very large pine tree species of variable habitat native to mountainous regions of western North America. It is the most widely distributed pine species in North America.Safford, H.D. 2013. Natural Range of Variation (NRV) for yellow pine and mixed conifer forests in the bioregional assessment area, including the Sierra Nevada, southern Cascades, and Modoc and Inyo National Forests. Unpublished report. USDA Forest Service, Pacific Southwest Region, Vallejo, CA/ref> ''Pinus ponderosa'' grows in various erect forms from British Columbia southward and eastward through 16 western U.S. states and has been successfully introduced in temperate regions of Europe, and in New Zealand. It was first documented in modern science in 1826 in eastern Washington near present-day Spokane (of which it is the official city tree). On that occasion, David Douglas misidenti ...
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Cliff-former
A cliff-former is a geological unit of bedrock that is more resistant to erosion than overlying or underlying strata and consequently produces outcrops with high slope angles. It is more or less equivalent to ''ridge-former'', and may be contrasted with slope-former. In humid environments, sandstones are typically cliff-formers. In arid environments, limestones are often cliff-formers also. Recent lavas may be cliff-formers as well. In the Ridge-and-Valley Appalachians of the eastern United States the major ridge-formers are the Tuscarora Tuscarora may refer to the following: First nations and Native American people and culture * Tuscarora people **''Federal Power Commission v. Tuscarora Indian Nation'' (1960) * Tuscarora language, an Iroquoian language of the Tuscarora people * ..., Pocono, and Pottsville Formations. References {{geomorph-stub Erosion landforms Geomorphology ...
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Crystal Creek (Arizona)
Crystal Creek (also known as Saltwater Creek) is a creek in the City of Townsville, Queensland, Australia. It runs for 17.5 km, beginning just below Paluma, flowing through the township of Mutarnee and emptying into the Coral Sea. It forms part of the Paluma Range National Park and is known for its division into two tourist destinations, namely Little Crystal Creek and Big Crystal Creek. Little Crystal Creek is situated approximately two thirds of the way along Mt Spec Road, heading towards the village of Paluma. This location consists of a number of small swimming holes and waterfalls, as well as the Little Crystal Creek Bridge, an historical arch bridge of which construction began in 1932. Facilities here include a wheelchair accessible picnic area, barbecues and toilets. Big Crystal Creek is located a few kilometres downstream from Little Crystal Creek, at the end of Spiegelhauer Road. Facilities at Big Crystal Creek also include a wheelchair accessible picnic a ...
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Dragon Head (Arizona)
Dragon Head (Arizona) is a elevation summit located in the Grand Canyon, in Coconino County, Arizona, Coconino County of Arizona, Southwestern United States, US. It is situated in the north of the Hindu Amphitheater, ~2.0 miles west of Shiva Temple (Grand Canyon), Shiva Temple, and ~2.5 mi southeast of Grama Point (northeast of Point Sublime). Unlike the extensive Ponderosa Pine forest of Shiva Temple, tableland/plateau prominence, Dragon Head’s flat-topped (minor plateau), is only populated with a marginal non-Ponderosa forest. Shiva Temple (Grand Canyon), Shiva Temple is approximately 275 acres (0.43 mi2), where Dragon Head is an ~5 acre prominence platform. Geology & Forests The lightly forested horizontal platform of Dragon Head, is created because of the debris from the eroded platform of the cliff-former, Kaibab Limestone. (Cliff formers also produce platforms.) Below the Kaibab are slope-former, slopes of the Toroweap Formation, on the shorter cliff of C ...
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Southwestern United States
The Southwestern United States, also known as the American Southwest or simply the Southwest, is a geographic and cultural region of the United States that generally includes Arizona, New Mexico, and adjacent portions of California, Colorado, Nevada, Oklahoma, Texas, and Utah. The largest cities by metropolitan area are Phoenix, Las Vegas, El Paso, Albuquerque, and Tucson. Prior to 1848, in the historical region of Santa Fe de Nuevo México as well as parts of Alta California and Coahuila y Tejas, settlement was almost non-existent outside of Nuevo México's Pueblos and Spanish or Mexican municipalities. Much of the area had been a part of New Spain and Mexico until the United States acquired the area through the Treaty of Guadalupe Hidalgo in 1848 and the smaller Gadsden Purchase in 1854. While the region's boundaries are not officially defined, there have been attempts to do so. One such definition is from the Mojave Desert in California in the west (117° west longitude) t ...
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Grand Canyon
The Grand Canyon (, yuf-x-yav, Wi:kaʼi:la, , Southern Paiute language: Paxa’uipi, ) is a steep-sided canyon carved by the Colorado River in Arizona, United States. The Grand Canyon is long, up to wide and attains a depth of over a mile (). The canyon and adjacent rim are contained within Grand Canyon National Park, the Kaibab National Forest, Grand Canyon–Parashant National Monument, the Hualapai Indian Reservation, the Havasupai Indian Reservation and the Navajo Nation. President Theodore Roosevelt was a major proponent of the preservation of the Grand Canyon area and visited it on numerous occasions to hunt and enjoy the scenery. Nearly two billion years of Earth's geological 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.
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