Atlantic Seaboard Fall Line

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The Atlantic Seaboard Fall Line, or Fall Zone, is a 900-mile (1,400 km) escarpment where the Piedmont and Atlantic coastal plain meet in the eastern United States.[1] Much of the Atlantic Seaboard fall line passes through areas where no evidence of faulting is present.

The fall line marks the geologic 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. Examples of the Fall Zone include the Potomac River's Great Falls and the rapids in Richmond, Virginia, where the James River falls across a series of rapids down to the tidal estuary of the James River.

Before navigation improvements such as locks, the fall line was often the head of navigation on rivers due to rapids and waterfalls, such as the Great Falls of the Potomac River. Numerous cities were founded at the intersection of rivers and the fall line. U.S. Route 1 links many of the fall line cities. Some of the cities along the Piedmont—Coastal Plain fall line include, from north to south:

Atlantic Seaboard fall line, north-to-south
State Point (crossing) Elevation & coordinates Fall zone:
drop/width (slope)
Geomorphology
Piedmont—Coastal plain
New Jersey New Brunswick (Raritan River) 460 ft (140 m)40°29′18″N 74°26′52″W / 40.48833°N 74.44778°W / 40.48833; -74.44778
Trenton (Delaware River) 40°13′18″N 74°45′22″W / 40.22167°N 74.75611°W / 40.22167; -74.75611 8 ft
Pennsylvania Philadelphia (Schuylkill River by I-76)
Delaware Wilmington (Brandywine Creek)
Maryland Conowingo Dam (Susquehanna)
Ellicott City[5] (Patapsco) 39°16.044′N 76°47.573′W / 39.267400°N 76.792883°W / 39.267400; -76.792883[1] crystalline rock—unconsolidate marine sediments [2]
Great Falls (Potomac River) 38°59′51″N 77°15′9″W / 38.99750°N 77.25250°W / 38.99750; -77.25250 76 ft/<1 mi (>1.4%)
Virginia Fredericksburg (Rappahannock) 39°16.044′N 76°47.573′W / 39.267400°N 76.792883°W / 39.267400; -76.792883[3] [west of Interstate 95 bridge][6]
Emporia (Meherrin River)[7]

References

  1. ^ a b c Freitag, Bob (2009). Floodplain Management: A New Approach for a New Era. Island Press. p. 77. ISBN 978-1-59726-635-2. Retrieved 17 November 2010. {{cite book}}: Unknown parameter |coauthors= ignored (|author= suggested) (help)
  2. ^ a b c Shamsi, Nayyar (2006). Encyclopaedia of Political Geography. Anmol Publications. pp. 92–93. ISBN 978-81-261-2406-0. Retrieved 17 November 2010.
  3. ^ a b Deane, Winegar (2002). Highroad Guide to Chesapeake Bay. John F. Blair. p. 5. ISBN 978-0-89587-279-1. Retrieved 17 November 2010.
  4. ^ a b Roberts, David C. (2001). Roger Tory Peterson (ed.). A Field Guide to Geology: Eastern North America. Houghton Mifflin Harcourt. p. 242. ISBN 978-0-618-16438-7. Retrieved 17 November 2010. {{cite book}}: Unknown parameter |coauthor= ignored (|author= suggested) (help)
  5. ^ "History/Culture". PatapscoHeritageGreenway.org. Retrieved 2010-09-07. George Ellicott House: A block away is the 1789 George Ellicott House at 24 Frederick Road., which has been saved, moved out of the flood plain, and restored. The Ellicott family settled here along the fall line of the Patapsco River in 1772 and built an innovative, water-powered flour mill
  6. ^ "Fall Line". VirginiaPlaces.org. Retrieved 2010-08-13.
  7. ^ "River and "Fall Line" Cities". VirginiaPlaces.org. Retrieved 2010-08-13.