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The Ridge-and-Valley Appalachians, also called the Ridge and Valley Province or the Valley and Ridge Appalachians, are a physiographic province of the larger Appalachian division and are also a belt within the Appalachian Mountains extending from southeastern New York through northwestern New Jersey, westward into Pennsylvania and southward into Maryland, West Virginia, Virginia, Tennessee, Georgia and Alabama. They form a broad arc between the Blue Ridge Mountains and the Appalachian Plateau physiographic province (the Allegheny and Cumberland Plateaus).
These mountains are characterized by long, even ridges, with long, continuous valleys in between. From a great enough altitude, they almost look like corduroy, except that the widths of the valleys are somewhat variable and ridges sometimes meet in a vee.
The ridge and valley system presents an important obstacle to east-west land travel even with today's technology and was a nearly insurmountable barrier to railroads crossing the range and especially to underfunded migrants traveling west to settle the Ohio Country, Northwest Territory and Oregon Country, before the days of motorized transportation. In the era when animal power dominated transportation there was no safe way to cross east-west in the middle of the range, only nearer its extremes save for the presence of a few rough passages opened mid-range during the colonial era such as Braddock's Road and Forbes Road, later improved into America's first National Roads (respectively Cumberland Road, Lincoln Highway or designated U.S. 40 and U.S. 30 in later years).
The eastern head of the Ridge and Valley region is marked by the Great Appalachian Valley, which lies just west of the Blue Ridge. The western side of the Ridge and Valley region is marked by steep escarpments such as the Allegheny Front, the Cumberland Mountains, and Walden Ridge.
These curious formations are the remnants of an ancient fold-and-thrust belt, west of the mountain core that formed in the Alleghenian orogeny (Stanley, 421-2). Here, strata have been folded westward, and forced over massive thrust faults; there is little metamorphism, and no igneous intrusion.(Stanley, 421-2) The ridges represent the edges of the erosion-resistant strata, and the valleys portray the absence of the more erodible strata. Smaller streams have developed their valleys following the lines of the more easily eroded strata. But a few major rivers, such as the Delaware River, the Susquehanna River, and the Potomac River are evidently older than the present mountains, having cut water gaps that are perpendicular to hard strata ridges. The evidence points to a wearing down of the entire region (the original mountains) to a low level with little relief, so that major rivers were flowing in unconsolidated sediments that were unaffected by the underlying rock structure. Then the region was uplifted slowly enough that the rivers were able to maintain their course, cutting through the ridges as they developed.
These mountains are at their highest development in central Pennsylvania, a phenomenon termed the Pennsylvania climax.
|Shawangunk Ridge||New York|
|Kittatinny Mountains||New Jersey|
|Bald Eagle Mountain||Pennsylvania|
|Wills Mountain||Pennsylvania and Maryland|
|Sideling Hill||West Virginia, Maryland, and Pennsylvania|
|Cacapon Mountain||West Virginia|
|Knobly Mountain||West Virginia|
|Mill Creek Mountain||West Virginia|
|New Creek Mountain||West Virginia|
|North Fork Mountain||West Virginia|
|Patterson Creek Mountain||West Virginia|
|Sleepy Creek Mountain||West Virginia|
|South Branch Mountain||West Virginia|
|Spruce Knob||West Virginia|
|Allegheny Mountain||Virginia and West Virginia|
|Great North Mountain||Virginia and West Virginia|
|North Mountain||Virginia and West Virginia|
|Pine Mountain||Kentucky, Virginia, and Tennessee|
|Clinch Mountain||Tennessee and Virginia|
|Powell Mountain||Tennessee and Virginia|
|Lookout Mountain||Tennessee, Alabama, and Georgia|
|This article relies largely or entirely upon a single source. (December 2007)|