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fall line

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fall line

–noun
1. an imaginary line, marked by waterfalls and rapids, where rivers descend abruptly from an upland to a lowland.
2. (initial capital letters) Eastern U.S. the imaginary line between the Piedmont and the Atlantic coastal plain.
3. Skiing. the path of natural descent from one point on a slope to another.

Origin:
1880–85, Americanism
Dictionary.com Unabridged
Based on the Random House Dictionary, © Random House, Inc. 2009.
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fall line  
n.  
  1. A line connecting the waterfalls of nearly parallel rivers that marks a drop in land level.

  2. The natural line of descent, as for skiing, between two points on a slope.

The American Heritage® Dictionary of the English Language, Fourth Edition
Copyright © 2009 by Houghton Mifflin Company.
Published by Houghton Mifflin Company. All rights reserved.
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Science Dictionary
fall line   (fôl)  Pronunciation Key 
A line connecting the waterfalls of nearly parallel rivers that marks a drop in land level.
The American Heritage® Science Dictionary
Copyright © 2002. Published by Houghton Mifflin. All rights reserved.
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Encyclopedia

fall line

line of numerous waterfalls, as at the edge of a plateau, where streams pass from resistant rocks to a plain of weak ones below. Such a line also marks the head of navigation, or the inland limit that ships can reach from a river's mouth; because navigation is interrupted both upstream and downstream, important cities often occur along the fall line. In the eastern United States, a fall line exists between the Appalachian piedmont and the Atlantic coastal plain; waterfalls or rapids occur on all the principal rivers (e.g., the Delaware, Schuylkill, Patapsco, Potomac, James, and Savannah rivers), and the cities of Trenton, Philadelphia, Baltimore, Washington, Richmond, and Augusta are among those built along this line. Other examples are the extensive fall lines that separate the narrow coastal plains of Africa, Western Australia, Brazil, and India from their interior continental shields.

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Encyclopedia Britannica, 2008. Encyclopedia Britannica Online.
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