14 Facts About Cumberland Mountains

1.

Cumberland Mountains are a mountain range in the southeastern section of the Appalachian Mountains.

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2.

Variant names of the Cumberland Mountains include Cumberland Mountain, Cumberland Range, Ouasioto Mountains, Ouasiota Mountains, Laurel Mountain, and Pine Mountain.

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3.

Cumberland Mountains range includes Pine Mountain, Cross Mountain, Cumberland Mountain, Log Mountain, Little Black Mountain, and Black Mountain, as well as others.

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4.

Cumberland Mountains are a physiographic section of the larger Appalachian Plateau province, which in turn is part of the larger Appalachian physiographic division.

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5.

Cumberland Mountain, not to be confused with the Cumberland Mountains within which it resides, is a long ridge extending from northeastern Tennessee, southeastern Kentucky and southwestern Virginia.

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6.

The southeastern side of Cumberland Mountains Mountain is a cliff-lined wall that was a barrier to exploration and settlement in Kentucky during the westward expansion in the late eighteenth century.

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7.

The famous Cumberland Mountains Gap is one of several gaps along Cumberland Mountains Mountain that allowed access across the mountain.

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8.

Cumberland Mountains Mountain is a long ridge running from near Caryville, Tennessee, northeastward to near Norton, Virginia, a distance of approximately 97 miles .

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9.

Cumberland Mountains Mountain is roughly parallel to Pine Mountain which lies from eight to ten miles to the northwest.

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10.

Cumberland Mountains Mountain is part of the Cumberland Mountains Overthrust Sheet or block and is the northern limb of the Powell Valley Anticline, a ramp anticline.

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11.

The southwestern terminus of Cumberland Mountains Mountain is marked by the northwest-trending Jacksboro Fault, a lateral ramp fault .

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12.

The various gaps in Cumberland Mountains Mountain are caused by rock weaknesses at cross-cutting faults or joints.

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13.

For example, Cumberland Mountains Gap was caused by erosion along the cross-cutting Rocky Face Fault.

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14.

Cliff-lined southeastern slope of Cumberland Mountains Mountain was created by erosion along the breached side of the Powell Valley Anticline.

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