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In geomorphology, a fall line (at times referred to as a fall zone) marks the area where an upland region (continental bedrock) and a coastal plain (coastal alluvia) meet. Geomorphology (from Greek: γη ge, "earth" μορφή morfé, "form" and λόγος Logos, "knowledge" Bedrock is the native consolidated rock underlying the surface of a terrestrial planet usually the Earth. A coastal plain is an area of flat low-lying land adjacent to a seacoast and separated from the interior by other features Alluvium (from the Latin, alluvius, from alluere, "to wash against" is Soil or Sediments deposited by a river or other running Technically, a fall line is an unconformity. An unconformity is a buried Erosion surface separating two rock masses or strata of different ages indicating that Sediment deposition was not A fall line is typically prominent when crossed by a river, for there will often be rapids or waterfalls. Many times a fall line will recede upstream as the river cuts out the uphill dense material, many times forming “c” shaped waterfalls. Because of these features river boats typically cannot travel any farther inland without portaging unless locks are built. Portage refers to the practice of carrying a Canoe or other Boat over land to avoid an obstacle on the water route (such as Rapids or a Waterfall On the other hand, the rapid change in elevation of the water, and the resulting energy release, makes the fall line a good location for a water mill. Because of the need for a port and a ready supply of water power, settlements often develop where rivers cross a fall line.

The fall line in the United States

Along the eastern coast of the United States, the east-facing escarpment where the Piedmont of the Appalachians descends steeply to the coastal plain forms a fall line over 1500 kilometers long. The United States of America —commonly referred to as the In Geomorphology, an escarpment is a transition zone between different physiogeographic provinces that involves a sharp steep Elevation differential characterized Piedmont is a plateau region located in the eastern United States between the Atlantic Coastal Plain and the main Appalachian Mountains, stretching The Appalachian Mountains ( often called the Appalachians, are a vast system of mountains in eastern North America. The Atlantic Coastal Plain is the flat stretch of land that borders the Atlantic Ocean (including the Gulf of Mexico) The kilometre ( American spelling: kilometer) symbol km is a unit of Length in the Metric system, equal to one thousand This long fall line (also referred to as the Fall Zone) played a major role in settlement patterns along rivers, back into prehistoric times. It is often referred to simply as "the fall line" or "the fall zone". In some places the fall line may be abrupt, while in others it is a zone that may be many miles wide. Geologically the fall line marks the boundary of hard metamorphosed terrain—the product of the Taconic orogeny—and the sandy, relatively flat outwash plain of the upper continental shelf, formed of unconsolidated Cretaceous and Tertiary sediments. The Taconic orogeny was a great mountain building period that perhaps had the greatest overall effect on the geologic structure of basement rocks within the New York Bight The Cretaceous (kriːˈteɪʃəs, usually abbreviated 'K' for its German translation "Kreide" is a geologic period and system, reaching from the end of The chuprichondira geological time interval covers roughly the time span between the demise of the non- avian Dinosaurs and beginning of the most recent Ice Age, approximately Sediment is any particulate matter that can be transported by fluid flow and which eventually is deposited as a layer of solid particles on the bed or bottom of a body of Examples of the Fall Zone include the rapids in Richmond, Virginia, where the James River falls across a series of rapids down to the tidal estuary of the James River. This article is about the city of Richmond the capital of the Commonwealth of Virginia. The James River in the US state of Virginia is a long River, including its Jackson River source

There are a few different theories as to how a Fall Line is formed or why they exist, and one in particular, brought forward by American Physiographer W. J. McGee states that a Fall Line is created through monoclinal faulting/flexing experienced in the region. While this theory is accepted by many geomorphologists much of the fall line along the east coast of the United States passes through areas where no evidence of faulting is present. In Geology a fault, or fault line, is a planar rock fracture which shows evidence of relative movement

In the 19th Century, the fall line often represented the head of navigation on rivers at points like Little Falls or the Great Falls, on the Potomac River. The Great Falls of the Potomac River are located at the Fall line of the Potomac River, 14 miles (22 However, since the advent of flumes for water supply and canals for shipping in the early 20th Century, the most prominent feature of fall line settlement was the establishment of the cities along it. A flume is an open artificial water channel in the form of a gravity chute, that leads Water from a Diversion dam or Weir completely aside As the cities were linked by the early highways, U.S. Route 1 and Interstate 95 came to pass through many of these cities, roughly tracing the fall line. US Route 1 (US 1 is a major north-south US Highway that serves the East Coast of the United States. Interstate 95 ( I-95) is the main Highway on the East Coast of the United States, paralleling the Atlantic Ocean from Maine to

Cities along the Piedmont – Coastal Plain fall line include, from north to south:

Cities along other fall lines include:

See also

References

Dictionary

fall line

-noun

  1. (geography) A line marking a boundary between an upland region and a plane; sometimes marked by a series of waterfalls on rivers that cross it.
  2. (snowboarding) The imaginary line downhill that something falling downhill would naturally follow.
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