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Bell Rock (Arizona)
Bell Rock is a butte just north of the Village of Oak Creek, Arizona, south of Sedona in Yavapai County. With an elevation at its summit of , it is just west of Courthouse Butte. Its panoramic views make it a popular landmark and tourist attraction. The most popular route is a moderate hike that reaches a small plateau on the northwest face of the butte. A challenging unmarked trail must be taken to reach the summit. Geology Bell Rock is a butte composed of horizontally bedded sedimentary rock of the Permian Supai Formation. See also * Schnebly Hill Formation References External links Bell Rock Pathway / Vista USFS The United States Forest Service (USFS) is an agency of the U.S. Department of Agriculture that administers the nation's 154 national forests and 20 national grasslands. The Forest Service manages of land. Major divisions of the agency in ... {{Commons category, Bell Rock (Sedona) Protected areas of Yavapai County, Arizona Landforms of Yavap ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Yavapai County, Arizona
Yavapai County is near the center of the U.S. state of Arizona. As of the 2020 United States census, 2020 census, its population was 236,209, making it the fourth-most populous county in Arizona. The county seat is Prescott, Arizona, Prescott. Yavapai County comprises the Prescott, AZ Metropolitan statistical area, Metropolitan Statistical Area as well as the northern portions of Peoria, Arizona, Peoria and Wickenburg, Arizona, Wickenburg, the balance of which are in the Phoenix Metropolitan Area. History Yavapai County was one of the four original Arizona counties created by the 1st Arizona Territorial Legislature. The county territory was defined as being east of longitude 113° 20' and north of the Gila River. Soon thereafter, the counties of Apache County, Arizona, Apache, Coconino County, Arizona, Coconino, Maricopa County, Arizona, Maricopa, and Navajo County, Arizona, Navajo were carved from the original Yavapai County. Yavapai County's present boundaries were establish ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Arizona
Arizona ( ; nv, Hoozdo Hahoodzo ; ood, Alĭ ṣonak ) is a state in the Southwestern United States. It is the 6th largest and the 14th most populous of the 50 states. Its capital and largest city is Phoenix. Arizona is part of the Four Corners region with Utah to the north, Colorado to the northeast, and New Mexico to the east; its other neighboring states are Nevada to the northwest, California to the west and the Mexican states of Sonora and Baja California to the south and southwest. Arizona is the 48th state and last of the contiguous states to be admitted to the Union, achieving statehood on February 14, 1912. Historically part of the territory of in New Spain, it became part of independent Mexico in 1821. After being defeated in the Mexican–American War, Mexico ceded much of this territory to the United States in 1848. The southernmost portion of the state was acquired in 1853 through the Gadsden Purchase. Southern Arizona is known for its desert cl ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
United States Geological Survey
The United States Geological Survey (USGS), formerly simply known as the Geological Survey, is a scientific agency of the United States government. The scientists of the USGS study the landscape of the United States, its natural resources, and the natural hazards that threaten it. The organization's work spans the disciplines of biology, geography, geology, and hydrology. The USGS is a fact-finding research organization with no regulatory responsibility. The agency was founded on March 3, 1879. The USGS is a bureau of the United States Department of the Interior; it is that department's sole scientific agency. The USGS employs approximately 8,670 people and is headquartered in Reston, Virginia. The USGS also has major offices near Lakewood, Colorado, at the Denver Federal Center, and Menlo Park, California. The current motto of the USGS, in use since August 1997, is "science for a changing world". The agency's previous slogan, adopted on the occasion of its hundredt ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Butte
__NOTOC__ In geomorphology, a butte () is an isolated hill with steep, often vertical sides and a small, relatively flat top; buttes are smaller landforms than mesas, plateaus, and tablelands. The word ''butte'' comes from a French word meaning knoll (but of any size); its use is prevalent in the Western United States, including the southwest where ''mesa'' (Spanish for "table") is used for the larger landform. Due to their distinctive shapes, buttes are frequently landmarks in plains and mountainous areas. To differentiate the two landforms, geographers use the rule of thumb that a mesa has a top that is wider than its height, while a butte has a top that is narrower than its height. Formation Buttes form by weathering and erosion when hard caprock overlies a layer of less resistant rock that is eventually worn away. The harder rock on top of the butte resists erosion. The caprock provides protection for the less resistant rock below from wind abrasion which leaves it stan ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Village Of Oak Creek, Arizona
Village of Oak Creek is an unincorporated community located within Big Park a census-designated place (CDP) in Yavapai County, Arizona, United States. The population was 6,147 at the 2010 census, up from 5,245 in 2000. Big Park is the name of the CDP while the community is more commonly known as the Village of Oak Creek (VOC), and is a bedroom community for Sedona, located seven miles away. Tourism and service to retirees and second-home owners are the basis for the local economy. Big Park, the pioneers' name for the large open area that became the Village of Oak Creek in the early 1960s, is set among scenic red-rock buttes and canyons. The Bell Rock scenic area adjoins the north end of VOC, and the town is surrounded by the Coconino National Forest. A Forest Service Visitor Center is located at the south end of VOC. Big Park's FIPS code is 07570. Residents of VOC have a Sedona ZIP code, 86351. Geography According to the United States Census Bureau, the CDP has a total area ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sedona, Arizona
Sedona is a city that straddles the county line between Coconino and Yavapai counties in the northern Verde Valley region of the U.S. state of Arizona. As of the 2010 census, its population was 10,031. It is within the Coconino National Forest. Sedona's main attraction is its array of red sandstone formations. The formations appear to glow in brilliant orange and red when illuminated by the rising or setting sun. The red rocks form a popular backdrop for many activities, ranging from spiritual pursuits to the hundreds of hiking and mountain biking trails. Sedona is also the home to the nationally recognized McDonald's with turquoise arches, instead of the traditional Golden Arches. Sedona was named after Sedona Arabella Miller Schnebly (1877–1950), the wife of Theodore Carlton Schnebly, the city's first postmaster. She was celebrated for her hospitality and industriousness. Her mother, Amanda Miller, claimed to have made the name up because "it sounded pretty". Histor ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Courthouse Butte
Courthouse Butte is a butte just north of the Village of Oak Creek, Arizona, south of Sedona in Yavapai County. Summit elevation is . It is just east of Bell Rock. Geologically, Courthouse Butte is composed of horizontally bedded sedimentary rock of the Permian Supai Formation.Weir, G.W., Ulrich, G.E. and Nealey, L.D., 1989, Geologic map of the Sedona 30' X 60' quadrangle, Yavapai and Coconino Counties, Arizona: U.S. Geological Survey, Miscellaneous Investigations Series Map I-1896, scale 1:100000. See also * Cathedral Rock * Schnebly Hill Formation References External links {{commonscat, Courthouse Butte "Bell Rock Pathway" Coconino National Forest The Coconino National Forest is a 1.856-million acre (751,000 ha) United States National Forest located in northern Arizona in the vicinity of Flagstaff. Originally established in 1898 as the "San Francisco Mountains National Forest Reserve", th ..., includes Courthouse Butte and Bell Rock. Buttes of Arizona Landforms of Ya ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sedimentary Rock
Sedimentary rocks are types of rock that are formed by the accumulation or deposition of mineral or organic particles at Earth's surface, followed by cementation. Sedimentation is the collective name for processes that cause these particles to settle in place. The particles that form a sedimentary rock are called sediment, and may be composed of geological detritus (minerals) or biological detritus (organic matter). The geological detritus originated from weathering and erosion of existing rocks, or from the solidification of molten lava blobs erupted by volcanoes. The geological detritus is transported to the place of deposition by water, wind, ice or mass movement, which are called agents of denudation. Biological detritus was formed by bodies and parts (mainly shells) of dead aquatic organisms, as well as their fecal mass, suspended in water and slowly piling up on the floor of water bodies (marine snow). Sedimentation may also occur as dissolved minerals precipitate from ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Permian
The Permian ( ) is a geologic period and stratigraphic system which spans 47 million years from the end of the Carboniferous Period million years ago (Mya), to the beginning of the Triassic Period 251.9 Mya. It is the last period of the Paleozoic Era; the following Triassic Period belongs to the Mesozoic Era. The concept of the Permian was introduced in 1841 by geologist Sir Roderick Murchison, who named it after the region of Perm in Russia. The Permian witnessed the diversification of the two groups of amniotes, the synapsids and the sauropsids ( reptiles). The world at the time was dominated by the supercontinent Pangaea, which had formed due to the collision of Euramerica and Gondwana during the Carboniferous. Pangaea was surrounded by the superocean Panthalassa. The Carboniferous rainforest collapse left behind vast regions of desert within the continental interior. Amniotes, which could better cope with these drier conditions, rose to dominance in place of their am ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Supai Formation
The Supai Group is a slope-forming section of red bed deposits found in the Colorado Plateau. The group was laid down during the Pennsylvanian to Lower Permian. Cliff-forming interbeds of sandstone are noticeable throughout the group. The Supai Group is especially exposed throughout the Grand Canyon in northwest Arizona, as well as local regions of southwest Utah, such as the Virgin River valley region. It occurs in Arizona at Chino Point, Sycamore Canyon, and famously at Sedona as parts of Oak Creek Canyon. In the Sedona region, it is overlain by the Hermit Formation, and the colorful Schnebly Hill Formation. The Supai Group is coeval with the Hermosa Group of east and south Utah; the Hermosa Group extended southeastwards from Utah to Durango, extreme southwest Colorado, and adjacent to the Hermosa type section. The Supai Group was originally designated as the Supai Formation by N.H. Darton in 1910 for exposures at Supai, Arizona. It was first raised to group stratigraphic ra ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bell Rock Sedona Arizona
A bell is a directly struck idiophone percussion instrument. Most bells have the shape of a hollow cup that when struck vibrates in a single strong strike tone, with its sides forming an efficient resonator. The strike may be made by an internal "clapper" or "uvula", an external hammer, or—in small bells—by a small loose sphere enclosed within the body of the bell (jingle bell). Bells are usually cast from bell metal (a type of bronze) for its resonant properties, but can also be made from other hard materials. This depends on the function. Some small bells such as ornamental bells or cowbells can be made from cast or pressed metal, glass or ceramic, but large bells such as a church, clock and tower bells are normally cast from bell metal. Bells intended to be heard over a wide area can range from a single bell hung in a turret or bell-gable, to a musical ensemble such as an English ring of bells, a carillon or a Russian zvon which are tuned to a common scale and installe ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Schnebly Hill Formation
The Schnebly Hill Formation is a section of red bed deposits found at the Colorado Plateau, near Sedona, Arizona. It is a dark red sandstone, from to thick. It lies between Coconino Sandstone and the older Hermit Formation. It is near the Supai Group. The source of the name "Schnebly" is Sedona Schnebly, after whom the city of Sedona, Arizona was named. Geology The formation traces to the Permian Age. The formation is the most prominent layer of the red rocks of the Sedona area due the presence of hematite – iron-oxide, frankly, rust – giving the sandstone a red color. The Schnebly Hill Sandstone formation comprises three sections: * the Bell Rock member, * the Fort Apache member, and * the Sycamore Pass member. See also Sedona-area rocks * Bell Rock * Cathedral Rock * Courthouse Butte * Red Rock State Park * Slide Rock State Park Local geology * Colorado Plateau * Mogollon Rim * Supai Group Local interest * Cottonwood, Arizona * Honanki * Jerome ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
