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Chilhowee Mountain
Chilhowee Mountain is the name of two non-contiguous low ridges in the U.S. state of Tennessee. The northern section is at the outer edge of the Great Smoky Mountains, stretching between the Little Tennessee River and Chilhowee Dam to the west, and the Little Pigeon River watershed to the east. The southern section is within the outer edge of the Unicoi Mountains in Polk County. While not entirely within the Great Smoky Mountains National Park, the northernmost mountain's crest is traversed by the westernmost section of the Foothills Parkway. Background While the northern ridge is long, it rarely reaches a width of more than or . Little River cuts a large gap in the middle of the mountain (near Walland), dividing it into eastern and western sections. The highest point on the western section is at a knob known as Look Rock. The highest point on the eastern section, known as The Three Sisters, rises to , and is visible from nearby Maryville, Tennessee. The southern ridge is a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Blount County, Tennessee
Blount County is a county located in the East Tennessee Grand Division of the U.S. state of Tennessee. As of the 2020 census, its population was 135,280. The county seat is Maryville, which is also the county's largest city. Blount County is included in the Knoxville, Tennessee metropolitan statistical area. History What is today Blount County was for many thousands of years Indian territory, passed down to the Cherokee tribe that claimed the land upon the arrival of White settlers in the late 18th century. Shortly thereafter, on July 11, 1795, Blount County became the 10th county established in Tennessee, when the Territorial Legislature voted to split adjacent Knox and Jefferson Counties. The new county was named for the governor of the Southwest Territory, William Blount, and its county seat, Maryville, was named for his wife Mary Grainger Blount. This establishment, however, did little to settle the differences between White immigrants and Cherokee natives, which was, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cherokee National Forest
The Cherokee National Forest is a United States National Forest located in the U.S. states of Tennessee and North Carolina that was created on June 14, 1920. The forest is maintained and managed by the United States Forest Service. It encompasses an estimated area of . Location The Cherokee National Forest headquarters are located in Cleveland, Tennessee. The Cherokee National Forest mostly lies within eastern Tennessee, along the border with North Carolina, and comprises nearly the entire border area except for sections within the Great Smoky Mountains National Park and the Copper Basin. The Cherokee National Forest has two separate sections: a northern region to the northeast of the Great Smoky Mountains National Park and a southern section to the southwest of the Smokies. The Cherokee National Forest contains such notable sites as the Ocoee River (site of the 1996 Olympic whitewater events); 150 miles (240 km) of the Appalachian National Scenic Trail; Citico Creek Wil ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountains Of Great Smoky Mountains National Park
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher than a hill, typically rising at least 300 metres (1,000 feet) above the surrounding land. A few mountains are isolated summits, but most occur in mountain ranges. Mountains are formed through tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable terrain ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ridges Of Tennessee
A ridge or a mountain ridge is a geographical feature consisting of a chain of mountains or hills that form a continuous elevated crest for an extended distance. The sides of the ridge slope away from the narrow top on either side. The lines along the crest formed by the highest points, with the terrain dropping down on either side, are called the ridgelines. Ridges are usually termed hills or mountains as well, depending on size. Smaller ridges, especially those leaving a larger ridge, are often referred to as spurs. Types There are several main types of ridges: ;Dendritic drainage, Dendritic ridge: In typical dissected plateau terrain, the stream drainage valleys will leave intervening ridges. These are by far the most common ridges. These ridges usually represent slightly more erosion resistant rock, but not always – they often remain because there were more Joint (geology), joints where the valleys formed or other chance occurrences. This type of ridge is generally ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cades Cove
Cades Cove is an isolated valley located in the Tennessee section of the Great Smoky Mountains National Park. The valley was home to numerous settlers before the formation of the national park. Today Cades Cove, the single most popular destination for visitors to the park, attracts more than two million visitors a year because of its well preserved homesteads, scenic mountain views, and abundant display of wildlife. The Cades Cove Historic District is listed on the National Register of Historic Places. Geology Geologically, Cades Cove is a type of valley known as a "limestone window", created by erosion that removed the older Precambrian sandstone, exposing the younger Paleozoic limestone beneath. More weathering-resistant formations, such as the Cades sandstone which underlies Rich Mountain to the north and the Elkmont and Thunderhead sandstones which form the Smokies crest to the south surround the cove, leaving it relatively isolated within the Smokies. As with neighboring ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
English Mountain
English Mountain is a mountain located in the western foothills of the Great Smoky Mountains region of East Tennessee. Rising to a peak of 3,629 feet, it is known for offering scenic fall colors within a convenient drive from Knoxville. A few rugged mountain roads provide access to the summit. Alpine Drive provides the main access, providing service to several small communities along with several resort cabins in the area available for tourists. It continues across the gap to the Wilhite area, forming the only complete pass over the mountain to the Jones Cove and Camp Hollow areas at the southeastern foot of the mountain. The English Mountain Fire Lookout Tower is a historic landmark, according to the National Park Service, with a single access via Carson Springs Road. Forbidden Caverns is a cave attraction on the northwestern face of the mountain. Source of water The mountain is a significant source of drinking water for nearby communities. The English Mountain Spring release ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Muscogee People
The Muscogee, also known as the Mvskoke, Muscogee Creek, and the Muscogee Creek Confederacy ( in the Muscogee language), are a group of related indigenous peoples of the Southeastern Woodlands, indigenous (Native American) peoples of the Southeastern WoodlandsTranscribed documents Sequoyah Research Center and the American Native Press Archives in the United States, United States of America. Their original homelands are in what now comprises southern Tennessee, much of Alabama, western Georgia (U.S. state), Georgia and parts of northern Florida. Most of the Muscogee people were forcibly Indian Removal, removed to Indian Territory (now Oklahoma) by the federal government in the 1830s during the Trail of Tears. A small group of the Muscogee Creek Confederacy remained in Alabama, and t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Muskogean Languages
Muskogean (also Muskhogean, Muskogee) is a Native American language family spoken in different areas of the Southeastern United States. Though the debate concerning their interrelationships is ongoing, the Muskogean languages are generally divided into two branches, Eastern Muskogean and Western Muskogean. Typologically, Muskogean languages are agglutinative. One documented language, Apalachee, is extinct and the remaining languages are critically endangered. Genetic relationships Family division The Muskogean family consists of six languages that are still spoken: Alabama, Chickasaw, Choctaw, Creek-Seminole, Koasati, and Mikasuki, as well as the now-extinct Apalachee, Houma, and Hitchiti (the last is generally considered a dialect of Mikasuki). "Seminole" is listed as one of the Muskogean languages in Hardy's list, but it is generally considered a dialect of Creek rather than a separate language, as she comments. The major subdivisions of the family have long been controve ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Chilhowee (Cherokee Town)
Chilhowee ( chr, ᏧᎷᎾᎢ, translit=Tsulunawe) was a prehistoric and historic Native American site in present-day Blount and Monroe counties in Tennessee, in what were the Southeastern Woodlands. Although now submerged by the Chilhowee Lake impoundment of the Little Tennessee River, the Chilhowee site was home to a substantial 18th-century Overhill Cherokee town. It may have been the site of the older Creek village "Chalahume" visited by Spanish explorer Juan Pardo in 1567. The Cherokee later pushed the Muscogee Creek out of this area. Although Chilhowee was destroyed by Euro-American frontiersmen who fought the Cherokee in the late 18th century, the village's name is still used for various entities throughout East Tennessee. Along with Chilhowee Dam and its reservoir, places and entities named after Chilhowee include a mountain, a geologic formation, several churches and schools, and a park and neighborhood in Knoxville. Geography The Little Tennessee River enter ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Waterfall
A waterfall is a point in a river or stream where water flows over a vertical drop or a series of steep drops. Waterfalls also occur where meltwater drops over the edge of a tabular iceberg or ice shelf. Waterfalls can be formed in several ways, but the most common method of formation is that a river courses over a top layer of resistant bedrock before falling on to softer rock, which Erosion, erodes faster, leading to an increasingly high fall. Waterfalls have been studied for their impact on species living in and around them. Humans have had a distinct relationship with waterfalls for years, travelling to see them, exploring and naming them. They can present formidable barriers to navigation along rivers. Waterfalls are religious sites in many cultures. Since the 18th century they have received increased attention as tourist destinations, sources of hydropower, andparticularly since the mid-20th centuryas subjects of research. Definition and terminology A waterfall is gen ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Saddle (landform)
The saddle between two hills or mountains is the region surrounding the saddle point, the lowest point on the line tracing the drainage divide (the col) connecting the peaks. When, and if, the saddle is navigable, even if only on foot, the saddle of a (optimal) pass between the two massifs, is the area generally found around the lowest route on which one could pass between the two summits, which includes that point which is a mathematically when graphed a relative high along one axis, and a relative low in the perpendicular axis, simultaneously; that point being by definition the col of the saddle. Topography A saddle is the lowest area between two highlands (prominences or peaks) which has two wings which span the divide (the line between the two prominences) by crossing the divide at an angle, and, so is concurrently the local highpoint of the land surface which falls off in the lower direction. That is, the drainage divide is a ridge along the high point of the saddle, as ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Oswald Dome
Oswald Dome (elevation ), also known as Bean Mountain, is a mountain located in the Cherokee National Forest in Polk County, Tennessee. It is part of the Blue Ridge Mountains, which is part of the larger Appalachian Mountains. Description Oswald Dome is located on the western fringe of the Blue Ridge province of the Appalachian Mountains, and is sometimes considered part of the Unicoi Mountains, a subrange of the Blue Ridge Mountains. It is approximately west of Reliance, northeast of Benton, and south-southeast of Delano. The Hiwassee River flows along the north base, and a saddle separates the mountain from Chilhowee Mountain to the south, although both mountains are technically part of the same ridge. The Ridge-and Valley province is directly below the mountain to the west. The mountain is accessible by Oswald Dome Road, a forest service road which connects to U.S. 64, and two trails. The Lowry Cove Trail begins on top of the mountain and heads north. Several radio/televi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
