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Eastern Continental Divide
Hydrological divide in eastern North America From Wikipedia, the free encyclopedia
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The Eastern Continental Divide, Eastern Divide or Appalachian Divide is a hydrological divide in eastern North America that separates the easterly Atlantic Seaboard watershed from the westerly Gulf of Mexico watershed. It is one of six continental hydrological divides of North America which define several drainage basins, each of which drains to a particular body of water.
The divide nearly spans the United States from south of Lake Ontario through the Florida peninsula, and consists of raised terrain including the Appalachian Mountains to the north, the southern Piedmont Plateau and lowland ridges in the Atlantic Coastal Plain to the south.
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Course
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Northern portion
_crossing_the_Eastern_Continental_Divide_on_top_of_Allegheny_Mountain_in_Pendleton_County,_West_Virginia.jpg)
The divide's northern portion winds through the middle of the Appalachian Mountains, either through the interior of the Allegheny Plateau or along the Allegheny Mountains. In this portion, the western drainage of the divide flows into the watersheds of the Allegheny River, Monongahela River, and New River, all tributaries of the Ohio River. The eastern drainage flows into the watersheds of the Susquehanna River, Potomac River, and James River, all of which flow into Chesapeake Bay before entering the Atlantic Ocean.
At its northern terminus, the Eastern Continental Divide originates at Triple Divide Peak[a] in Ulysses Township, Pennsylvania, about 10 mi (16 km) south of the New York-Pennsylvania border, where it diverges from the St. Lawrence Divide. This point divides the eastern United States into three watersheds: those of the Genesee River flowing into Lake Ontario and then the St. Lawrence River to the north; Pine Creek into the Susquehanna River as part of the Atlantic seaboard watershed to the east; and the Allegheny River into the Ohio, the Mississippi, and the Gulf of Mexico to the west.
From north to south, the divide passes through the broader Allegheny Plateau region, following the boundary between the Allegheny River and Susquehanna River watersheds through most of Pennsylvania. At Blue Knob near Altoona, the Divide begins to follow Allegheny Mountain and then Little Savage Mountain. A few miles before the state border, the Divide begins to separate the Youghiogheny River and Potomac River watersheds.[2]
In Maryland, the Divide runs significantly west of the Allegheny Front, following Backbone Mountain, and passing near the source of the North Branch Potomac River at the Fairfax Stone. The Divide then passes through a plateau of the Allegheny Mountains of West Virginia, passing between the north end of the Canaan Valley in the Cheat River watershed, and the Mount Storm Lake basin in the Potomac River watershed. The Divide then rejoins the Allegheny Front.
A significant portion of the Divide forms part of the border between West Virginia and Virginia along Allegheny Mountain and then Peters Mountain, separating the Greenbrier River and James River watersheds. It then makes a dramatic arc to the east around the Sinking Creek valley, and then follows the hill crest east of Blacksburg, Virginia.[3][4]
Central portion
The divide's central portion generally follows the easternmost ridge of the Blue Ridge Mountains and thus of the Appalachian Mountains as a whole, which takes the form of a high escarpment. In this portion, the western drainage of the divide flows into the watersheds of the New River and Tennessee River, both tributaries of the Ohio River. The eastern drainage flows into the watersheds of the Roanoke River, Pee Dee River, and Santee River.[5]
The divide initially separates the headwaters of the New River from that of the Roanoke River.[3][4] Just before the Divide passes into North Carolina, it begins to separate the New River and Yadkin River watersheds. It then separates upper tributaries of the Tennessee River from those of the Santee River.[5][6] Its high point is on Grandfather Mountain at 5,946 feet (1,812 m); although Mount Mitchell is the highest point in the Appalachian Mountains, it is not on the Divide, but 4 miles west of it.
Southern portion
Past the southern end of the Appalachian Mountains, the divide's southern portion winds through the lowlands of Georgia and Florida. In this portion, the western drainage of the divide flows into the watersheds of the Apalachicola River, Suwannee River, Withlacoochee River, and Peace River, all of which drain directly to the Gulf of Mexico. The eastern drainage flows into the watersheds of the Savannah River, Altamaha River, Satilla River, St. Marys River, and St. Johns River.
In Georgia, the Divide generally separates the Apalachicola River, watershed in the west from the Savannah River and Altamaha River watersheds to the east, passing through the Atlanta metropolitan area and extending past the southern end of the Appalachian Mountains southeasterly across the Georgia plateau. In southern Georgia, it separates the Suwannee River and Satilla River watersheds.[7]
In Florida, the Divide generally follows the western edge of the St. Marys River and then St. Johns River, meandering into the low country of Northern Florida until it reaches Central Florida. The west side of the divide continues to be the Suwannee River and then the Withlacoochee River watersheds.
The southern terminus of the Eastern Continental Divide is at the triple divide between the St. Johns, Peace, and Kissimmee River watersheds, which is in Haines City, Florida on the Lake Wales Ridge.[8][9][10][11] Because the Kissimmee River flows into Lake Okeechobee, whose distributaries reach both the Gulf of Mexico and the Atlantic Ocean via low swampland covered by a network of diverging canals and natural waterways, its watershed's land is not clearly divisible between the two watersheds.[citation needed]
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Weather
Because the divide is at or in proximity to the highest terrain, air is forced upwards regardless of wind direction. This process of orographic enhancement leads to higher precipitation than surrounding areas. In winter, the divide is often much snowier than surrounding areas, due to orographic enhancement and cooler temperatures with elevation.
History
Prior to about 1760, north of Spanish Florida, the Appalachian Divide represented the boundary between British and French colonial possessions in North America. [12] The Royal Proclamation of 1763 separated settled lands of the Thirteen Colonies from lands north and west of it designated the Indian Reserve; the proclamation border ran along the Appalachian Divide but extended beyond its Pennsylvania-New York terminus north into New England.
The exact route of the ECD shifts over time due to erosion, tectonic activity, construction projects, and other factors.
Locations
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See also
Notes
- @41°50′48″N 77°50′14″W, elevation: 2,507 feet (764 m)[1]
References
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