What are the mountains that Waynesville, North Carolina is located between that are a physiographic province of the larger Appalachian Mountains range?
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Waynesville, North Carolina Waynesville is a town in and the county seat of Haywood County, North Carolina, United States. It is the largest town in Haywood County and the largest in Western North Carolina west of Asheville. Waynesville is located about 30 mi southwest of Asheville between the Great Smoky and Blue Ridge mountains.
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Blue Ridge Mountains The Blue Ridge Mountains are a physiographic province of the larger Appalachian Mountains range. This province consists of northern and southern physiographic regions, which divide near the Roanoke River gap. The mountain range is located in the eastern United States, starting at its southernmost portion in Georgia, then ending northward in Pennsylvania. To the west of the Blue Ridge, between it and the bulk of the Appalachians, lies the Great Appalachian Valley, bordered on the west by the Ridge and Valley province of the Appalachian range.
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Watauga River The Watauga River is a large stream of western North Carolina and East Tennessee. It is 78.5 mi long with its headwaters on the slopes of Grandfather Mountain and Peak Mountain in Watauga County, North Carolina.
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Wawayanda Mountain Wawayanda Mountain is a ridge in the New York-New Jersey Highlands region of the Appalachian Mountains. The summit lies within Sussex County, New Jersey.
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Powell Mountain Powell Mountain (or "Powells Mountain") is a mountain ridge of the Ridge-and-valley Appalachians of the Appalachian Mountains. It is a long and narrow ridge, running northeast to southwest, from about Norton, Virginia to near Tazewell, Tennessee. It separates the Clinch River basin and the Powell River basin of Powell Valley. It was named for an 18th-century explorer.
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Caraway Mountains The Caraway Mountains are a mountain range located in western Randolph County and Chatham County, North Carolina and a section of eastern Davidson County, North Carolina. The mountains are located between the cities of Asheboro and Lexington and are bisected by US Highway 64. The mountains are known for their rugged and steep terrain and rise to over 1,000 feet. Typically the Caraways are said to be a part of the Uwharrie Mountains and make up the northern extent of this range. They extend from roughly south of High Point, NC and transition into the Uwharries, stretching roughly 30 miles. The range is only about 10 miles wide. The range takes its name from Caraway Creek, which was named after a Native American tribe that lived in the area before European settlement. The area was once a highly used Indian trading area and many early settlers noted that the Indian trading paths tended to "disappear" into the mountains. Prominent peaks in the area are Caraway Mountain, Back Creek Mountain, Daves Mountain, Ridges Mountain, and Mount Shepherd, the latter at 1,150 feet being the highest point in Randolph County. Its foothills are in Chatham County
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East Waynesville Baptist Church East Waynesville Baptist Church is a Baptist church in Waynesville, a small town in the Great Smoky Mountains of Western North Carolina, United States of America. It is an independent and autonomous member of the Southern Baptist Convention and the Baptist State Convention of North Carolina (BSCNC). As of May 2005 it had 100 members. The church was involved in a 2005 controversy after the pastor allegedly expelled members because of their political views.
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Bear Pond Mountains The Bear Pond Mountains are a sub-range in the Appalachian Mountains, that straddle Pennsylvania and Maryland in the United States. These mountains are a part of the Ridge and Valley Appalachians and reach their highest point at Cross Mountain (Pennsylvania) 2062 ft . A unique geologic feature known as the "Punchbowl" occurs in this range. This feature was created by the weathered shales of the Ordovician age in the center of a south-plunging anticline, having been eroded to expose a large amphitheater like feature (punchbowl). Cross and Hearthstone Mountain are made of hard resistant quartzite of the Tuscarora Formation of the Silurian age, which form the walls of the bowl.
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Waynesboro, Pennsylvania Waynesboro is a borough in Franklin County, Pennsylvania, on the southern border of the state. Waynesboro is in the Cumberland Valley between Hagerstown, Maryland, and Chambersburg, Pennsylvania. It is part of Chambersburg, PA Micropolitan Statistical Area, which is part of the Baltimore–Washington metropolitan area. It is 2 miles north of the Mason–Dixon line and close to Camp David and the Raven Rock Mountain Complex.
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North Mountain (Pennsylvania) North Mountain is a 2584 ft ridge primarily located in Davidson Township of Sullivan County in the U.S. state of Pennsylvania. Its summit is that county's highest point, the 10th highest among the state's 67 counties. Portions also extend into neighboring Lycoming, Luzerne, and Wyoming counties. The mountain has a topographic isolation of 57.99 mi . U.S. Route 220 passes near the mountain. The mountain once had a prolific population of animals, including grouse, deer (including white deer), and bears.
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Ashby Gap Ashby Gap, more commonly known as Ashby's Gap is a wind gap in the Blue Ridge Mountains on the border of Clarke County, Loudoun County and Fauquier County in Virginia. The gap is traversed by U.S. Route 50. The Appalachian trail also passes across the gap.
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Allegheny Mountain (Pennsylvania) Allegheny Mountain is a stratigraphic ridge that extends northeast to southwest from south of Blue Knob (Pennsylvania) to a saddle point at the Savage Mountain anticline. It merges with Negro Mountain just north of the Cambria County line where the Berlin-Salisbury basin expires .
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New York–New Jersey Highlands The New York – New Jersey Highlands is a geological formation composed primarily of Precambrian igneous and metamorphic rock running from the Delaware River near Musconetcong Mountain, northeast through the Skylands Region of New Jersey along the Bearfort Ridge and the Ramapo Mountains, Sterling Forest, Harriman and Bear Mountain State Parks in New York, to the Hudson River at Storm King Mountain. The northern region is also known as the Hudson Highlands and the southern as the New Jersey Highlands. A broader definition would extend the region west to Reading, Pennsylvania, and east to the Housatonic River in Connecticut, encompassing the Reading Prong.
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Appalachia Appalachia ( ) is a cultural region in the Eastern United States that stretches from the Southern Tier of New York to northern Alabama, Mississippi and Georgia. While the Appalachian Mountains stretch from Belle Isle (Newfoundland and Labrador) in Canada to Cheaha Mountain in Alabama, the cultural region of Appalachia typically refers only to the central and southern portions of the range. As of the 2010 United States Census, the region was home to approximately 25 million people.
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North Fork Mountain North Fork Mountain is a quartzite-capped mountain ridge in the Ridge and Valley physiographic province of the Allegheny Mountains (or "High Alleghenies" or "Potomac Highlands") of eastern West Virginia, USA. Kile Knob, at 4,588 feet (1,398 m), is the mountain's highest point, and Panther Knob and Pike Knob are nearly as high.
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Southern Appalachian low-elevation pine forest The Southern Appalachian low-elevation pine forest is a forest system that occurs in Indiana, Kentucky, Tennessee, Alabama, Virginia, North Carolina, South Carolina, and Georgia. It is found in the lower elevations of the southern Appalachian Mountains and adjacent Piedmont and Cumberland Plateau, extending into part of the Interior Low Plateaus.
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Acadian orogeny The Acadian orogeny is a long-lasting mountain building event which began in the Middle Devonian, reaching a climax in the early Late Devonian. It was active for approximately 50 million years, beginning roughly around 375 million years ago, with deformational, plutonic, and metamorphic events extending into the Early Mississippian. The Acadian orogeny is the third of the four orogenies that created the Appalachian orogen and subsequent basin. The preceding orogenies consisted of the Potomac and Taconic orogeny, which followed a rift/drift stage in the Late Neoproterozoic. The Acadian orogeny involved the collision of a series of Avalonian continental fragments with the Laurasian continent. Geographically, the Acadian orogen extended from the Canadian Maritime provinces migrating in a southwesterly direction toward Alabama. However, the Northern Appalachian region, from New England northeastward into Gaspé region of Canada, was the most greatly affected region by the collision.
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Mount Pisgah (mountain in North Carolina) Mount Pisgah is a mountain in the Appalachian Mountain Range and part of the Blue Ridge Mountains of North Carolina, United States. The mountain's height is 5,721 feet (1,744 m) above sea level, and it sits approximately 15 miles (24 kilometers) southwest of Asheville, near the crossing of the boundaries of Buncombe, Haywood, Henderson and Transylvania counties. It is located on the border of Buncombe and Haywood counties, close to the point where Henderson and Transylvania meet them, but not actually within the latter two counties. The mountain is easily accessible via a hiking trail from the Blue Ridge Parkway, near the Pisgah Inn.
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Social and economic stratification in Appalachia The Appalachian region of the Eastern United States is home to over 25 million people and covers parts of mostly mountainous areas of 13 states, including Mississippi, Alabama, Pennsylvania, New York, Georgia, South Carolina, North Carolina, Tennessee, Virginia, Kentucky, Ohio, Maryland, and the entire state of West Virginia. The near-isolation of the area's rugged topography is home to communities with a distinct culture, who in many cases are put at a disadvantage because of the transportation and infrastructure problems that have developed.
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Pottsville Formation The Pennsylvanian Pottsville Formation is a mapped bedrock unit in Pennsylvania, western Maryland, West Virginia, and Ohio. The formation is also recognized in Alabama. It is a major ridge-former in the Ridge-and-Valley Appalachians of the eastern United States. The Pottsville Formation is conspicuous at many sites along the Allegheny Front, the eastern escarpment of the Allegheny or Appalachian Plateau.
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Howard Knob Howard Knob (variant: Howard's Knob) is a mountain in the North Carolina High Country, located in the town of Boone. According to the US Geological Survey, the mountain's proper name is Howard Knob, but it is known to locals and tourists as Howard's Knob. Howard Knob and the surrounding area are part of the Appalachian Mountain Range. The mountain has an elevation of 4396 ft above sea level, and rises nearly 1000 ft above the town of Boone and the campus of Appalachian State University.
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Piedmont Mountains The Piedmont Mountains are outlying mountains, sometimes called “low mountains”, that typically occur in the western Piedmont near the Blue Ridge. Most of the features within the Piedmont physiographic region of North America lie either on the eastern border where the plateau plunges onto the Coastal Plain at the Fall Line, in the broad valleys of the river systems, or on the western border where Piedmont Mountains likely occur. Occasionally, due to diverse rock formations, folds and outcroppings, these mountains can rise at various locations across the Piedmont like the Uwharrie Mountain Range in North Carolina or the Pine Mountain Range in Georgia. Most of these mountains, or hills, are what is left of ancient eroded mountains. Some, like Stone Mountain in Georgia, are solitary rock domes called Monadnocks which become further exposed with erosion. The Piedmont is part of the greater Appalachian Mountain Range and is also referred to as the Appalachian Plateau. The French definition of piedmont in itself translates as foothill; however, a Piedmont Mountain may be that of greater significance or prominent elevation.