dbo:abstract |
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. 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 alluvial plain of the upper continental shelf, formed of unconsolidated Cretaceous and Cenozoic sediments. Examples of Fall Zone features include the Potomac River's Little Falls and the rapids in Richmond, Virginia, where the James River falls across a series of rapids down to its own tidal estuary. Before navigation improvements such as locks, the fall line was generally the head of navigation on rivers due to their rapids or waterfalls, and the necessary portage around them. Numerous cities initially formed along the fall line because of the easy river transportation to seaports, as well the availability of water power to operate mills and factories, thus bringing together river traffic and industrial labor. U.S. Route 1 and I-95 link many of the fall-line cities. In 1808, Treasury Secretary Albert Gallatin noted the significance of the fall line as an obstacle to improved national communication and commerce between the Atlantic seaboard and the western river systems: The most prominent, though not perhaps the most insuperable obstacle in the navigation of the Atlantic rivers, consists in their lower falls, which are ascribed to a presumed continuous granite ridge, rising about one hundred and thirty feet above tide water. That ridge from New York to James River inclusively arrests the ascent of the tide; the falls of every river within that space being precisely at the head of the tide; pursuing thence southwardly a direction nearly parallel to the mountains, it recedes from the sea, leaving in each southern river an extent of good navigation between the tide and the falls. Other falls of less magnitude are found at the gaps of the Blue Ridge, through which the rivers have forced their passage... (en) |
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wiki-commons:Special:FilePath/United_States_Fall_Line.jpg?width=300 |
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http://www.mde.maryland.gov/assets/document/Patapsco%20LNB%20Stressor%20ID%20Report_04-20-09.pdf http://www.hmdb.org/Marker.asp%3FMarker=193 |
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dbr:Camden,_South_Carolina dbr:Cape_Fear_River dbr:Potomac_River dbr:Princeton,_New_Jersey dbr:Rocky_Mount,_North_Carolina dbr:Savannah_River dbr:Schuylkill_River dbr:Brandywine_Creek_(Christina_River) dbr:Black_Warrior_River dbr:Blue_Ridge_Mountains dbr:Brandywine_Creek_(Christina_River_tributary) dbr:Delaware dbr:Delaware_River dbr:Alluvial_plain dbr:Hudson_River dbr:Little_Falls_(Potomac_River) dbr:Atlantic_coastal_plain dbr:Patapsco_River dbr:Patuxent_River dbr:Pee_Dee_River dbr:Pennsylvania dbr:Perryville,_Maryland dbr:Petersburg,_Virginia dbr:Richmond,_Virginia dbr:Roanoke_Rapids,_North_Carolina dbr:Roanoke_River dbr:United_States_Secretary_of_the_Treasury dbr:Virginia dbr:Eastern_United_States dbr:Columbia,_South_Carolina dbr:Columbus,_Georgia dbr:Congaree_River dbr:Conowingo_Dam dbr:Coosa_River dbr:Cretaceous dbr:Maryland dbr:Meherrin_River dbr:Escarpment dbr:Oconee_River dbr:Elkridge,_Maryland dbr:Ellicott_City,_Maryland dbr:Emporia,_Virginia dbr:Fredericksburg,_Virginia dbr:Georgia_(U.S._state) dbr:Theodore_Roosevelt_Island dbr:Appomattox_River dbr:Lumber_River dbr:Lumberton,_North_Carolina dbr:Macon,_Georgia dbr:Piedmont_(United_States) dbr:Portage dbr:Taconic_orogeny dbr:Augusta,_Georgia dbr:Baltimore dbr:Cenozoic dbr:Trenton,_New_Jersey dbr:Troy,_New_York dbr:Tuscaloosa,_Alabama dbr:U.S._Route_1 dbr:Washington,_D.C. dbr:Washington,_DC dbr:Wateree_River dbr:Weldon,_North_Carolina dbr:Wetumpka,_Alabama dbr:Wilmington,_Delaware dbr:Jones_Falls dbr:Albert_Gallatin dbr:East_Brunswick,_New_Jersey dbr:Edison,_New_Jersey dbr:Fayetteville,_North_Carolina dbr:Fall_line dbr:Havre_de_Grace,_Maryland dbr:Herring_Run dbc:East_Coast_of_the_United_States dbr:Interstate_95 dbr:James_River dbr:Tallapoosa_River dbr:Tallassee,_Alabama dbr:Tar_River dbr:The_Carolinas dbc:Escarpments_of_the_United_States dbr:Chattahoochee_River dbr:Cheraw,_South_Carolina dbr:Chesapeake_Bay dbr:Laurel,_Maryland dbr:Susquehanna_River dbr:Philadelphia dbr:Milledgeville,_Georgia dbr:Millstone_River dbr:Neuse_River dbr:New_Brunswick,_New_Jersey dbr:New_Jersey dbr:Newark,_Delaware dbr:Occoquan,_Virginia dbr:Occoquan_River dbr:Ocmulgee_River dbr:Raleigh,_North_Carolina dbr:Rappahannock_River dbr:Raritan_River dbr:Gwynns_Falls dbr:Sediment dbr:Interstate_76_(east) dbr:Faulting dbr:White_Clay_Creek_(Christina_River) dbr:Wikt:head_of_navigation |
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dbr:New_Jersey Carolinas or Georgia (en) |
dbp:location |
United States (en) |
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Map showing part of the Eastern Seaboard Fall Line where the pale colored coastal plain meets the brightly colored Piedmont. (en) |
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United States Fall Line.jpg (en) |
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Atlantic Seaboard fall line (en) |
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dbr:Escarpment |
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dbc:East_Coast_of_the_United_States dbc:Escarpments_of_the_United_States |
rdfs:comment |
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. Much of the Atlantic Seaboard fall line passes through areas where no evidence of faulting is present. In 1808, Treasury Secretary Albert Gallatin noted the significance of the fall line as an obstacle to improved national communication and commerce between the Atlantic seaboard and the western river systems: (en) |
rdfs:label |
Atlantic Seaboard Fall Line (en) |
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wikidata:Atlantic Seaboard Fall Line https://global.dbpedia.org/id/4TRDP |
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wikipedia-en:Atlantic_Seaboard_Fall_Line?oldid=1124102378&ns=0 |
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wiki-commons:Special:FilePath/United_States_Fall_Line.jpg |
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wikipedia-en:Atlantic_Seaboard_Fall_Line |
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