Valley and Ridge Physiographic Province
Enlarge text Shrink text-
Save successfulThe item can be found in your Personal ZoneשגיאהLog in to your account to save
Information for Authority record
Other Identifiers
- Work cat: Swain, Lindsay A. Summary of the hydrogeology of the Valley and Ridge, Blue Ridge, and Piedmont physiographic provinces in the eastern United States, 2004:page 1 (Valley and Ridge Physiographic Province)
- National Park Service, April 3, 2018:Physiographic Provinces Valley and Ridge (The Valley and Ridge province is a set of northeast-southwest trending valleys and ridges that stretch from central Alabama to New York; these ridges and valleys are the result of folded Paleozoic sedimentary beds)
- New Georgia Encyclopedia, April 3, 2018:Valley and Ridge Geologic Province (The Valley and Ridge is the westernmost physiographic province of the Appalachian Mountains, bounded to the east by the Blue Ridge, the south by the Piedmont, and the northwest by the Appalachian Plateau; characterized by long north-northeasterly trending ridges separated by fertile valleys and extends continuously from New York to the edge of the Coastal Plain (fall line) in Alabama; much of northwest Georgia lies within the Valley and Ridge province)
- Britannica online, June 8, 2018:Ridge and Valley (physiographic province, part of the Appalachian Highlands in the eastern United States; bordered on the east by the Blue Ridge and Piedmont provinces and on the west by the Appalachian Plateau)
Wikipedia description:
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 Highlands division. The physiographic province is divided into three sections: the Hudson Valley, the Central, and the Tennessee. The river valleys were areas of indigenous settlements for thousands of years. In the historic period, the Cherokee people had towns along many of the rivers in western South Carolina and North Carolina, as well as on the western side of the Appalachian Mountains in present-day Tennessee. Similarly, the Catawba people occupied areas along the upper Catawba River in Western North Carolina, to the east of Cherokee County. The ridge and valley system presents an important obstacle to east–west land travel even with today's technology. It was a nearly insurmountable barrier to European-American migrants who walked or rode horses traveling west to settle the Ohio Country, and later the Northwest Territory and Oregon Country. In the era when animal power dominated transportation, there was no safe way to cross east–west in the middle of the range; crossing was only possible nearer its extremes except for a few rough passages opened mid-range during the colonial era, including Cumberland Gap, Braddock's Road, and Forbes Road. These were later improved as America's first National Roads, including Wilderness Road, Cumberland Road, Lincoln Highway, designated as U.S. Route 40 and U.S. Route 30 in later years. Early settlers of Ohio Country tended to enter it via the Ohio River; river systems were the most important transportation corridors. It was difficult in the late 19th and 20th centuries to construct railroads and modern highways through this area.
Read more on Wikipedia >