[3], From Simple English Wikipedia, the free encyclopedia, "High Knob – Climbing, Hiking & Mountaineering", "Highroad Guide to the Virginia Mountains", https://simple.wikipedia.org/w/index.php?title=Cumberland_Mountains&oldid=5440878, Creative Commons Attribution/Share-Alike License. [1], Variant names of the Cumberland Mountains include Cumberland Mountain, Cumberland Range, Ouasioto Mountains, Ouasiota Mountains, Laurel Mountain, and Pine Mountain. The more-gentle northwestern slope is the dip slope and roughly parallel to the dip of the Early Pennsylvanian sandstones. The Cumberland Mountains are a mountain range in the southeastern part of the Appalachian Mountains.They run from northern Tennessee to West Virginia. The Pine Mountain ramp forms the northwestern limb of this syncline and Cumberland Mountain (the northwestern limb of the Powell Valley Anticline) forms the southeastern limb. Pine Mountain is a long, narrow ridge starting in northern Tennessee and extending northeastward into southeastern Kentucky and southwestern Virginia. These are all synclinal mountains and reside along the axis of the northeast-trending Middlesboro Syncline. [1] Their highest peak, with an elevation of 4,223 feet (1,287 m) above mean sea level, is High Knob, which is located near Norton, Virginia. - rather than say "I'm going mountain biking in the Blue Ridge on Saturday." The southwestern terminus of Pine Mountain is marked by the northwest-trending Jacksboro Fault, a lateral ramp fault (part of the Pine Mountain Thrust Fault). Built on a plateau of the Cumberland Mountains, the area is primarily rolling hills interspersed by hollows and deep ravines with several small creeks meandering through the colony. The Cumberland Mountains were named for England's Duke of Cumberland. Map showing the Cumberland Mountains in orange, ✪ Cumberland Gap And Mountains of Eastern Kentucky, ✪ Cumberland Gap 1986 National Park Service narrated by Lorne Greene 11min, ✪ My World - Powell Valley and Cumberland Mountains. Softer rocks have been eroded away, leaving the resistant sandstones to form a ridge. This is also the northern limb of the Middlesboro Syncline. The various gaps in Cumberland Mountain are caused by rock weaknesses at cross-cutting faults or joints. Pine Mountain is at the headward ramp of the Pine Mountain Thrust Fault. Their highest peak, with an elevation of 4,223 feet (1,287 m) above mean sea level, is High Knob, which is located near Norton, Virginia. in … [1] They are named for Prince William, Duke of Cumberland.[2]. They are located in southern West Virginia, western Virginia, eastern edges of Kentucky, and eastern middle Tennessee, including the Crab Orchard Mountains. Its peak forms the boundary between Kentucky and Virginia in some areas. Congratulations on this excellent venture… what a great idea! Their highest peak, with an elevation of 4,223 feet (1,287 m) above sea level, is High Knob near Norton, Virginia. They run from northern Tennessee to West Virginia. Lua error in Module:Coordinates at line 668: callParserFunction: function "#coordinates" was not found. [1] They are named for Prince William, Duke of Cumberland.[2]. The Cumberland Mountains range includes Pine Mountain, Cumberland Mountain, Log Mountain, Little Black Mountain and Black (Big Black) Mountain, as well as others. But this long and narrow mountain in Virginia's southwest corner has a history that goes back much further in time than any English duke. Cumberland Mountain is a long ridge running from near Caryville, Tennessee northeastward to near Norton, Virginia, a distance of approximately 97 miles (156 km). This northwestward dip is the northern limb of the Powell Valley Anticline. The Cumberland Mountains are a mountain range in the southeastern section of the Appalachian Mountains. The ridge is interrupted by several gaps, most famous of which is Cumberland Gap, but also includes Big Creek Gap between Ivydell and LaFollette, Tennessee, Pennington Gap near Pennington Gap, Virginia, and Big Stone Gap near Big Stone Gap, Virginia. Cumberland Mountain is a long ridge running from near Caryville, Tennessee, northeastward to near Norton, Virginia, a distance of approximately 97 miles (156 km). The cliff-lined southeastern slope (escarpment slope) of Cumberland Mountain was created by erosion along the breached side of the Powell Valley Anticline. The Cumberland Plateau in Tennessee. The conservation organizations include The Nature Conservancy, the Doris Duke Charitable Foundation, and the Natural Resources Defense Council with focus on the Cumberland Plateau. The southeastern slope of the ridge is cliff lined, whereas the northwestern slope is more gentle. The northwestern terminus is located near Norton, Virginia where the hard sandstones dip below the surface as the axis of the Powell Valley anticline plunges to the northeast. Several mountains that lie between Pine Mountain and Cumberland Mountain include Black Mountain and Little Black Mountain as well as a number of smaller mountains (Short, Walnut, Rich, Log, Reynolds, etc.). CUMBERLAND MOUNTAINS, the westernmost of the three great divisions of the Appalachian uplift in the United States, composed of many small ranges of mountains (of which Cumberland mountain in eastern Kentucky is one).

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