Three Creek Tributary to Nottoway River | |
---|---|
Location | |
Country | United States |
State | Virginia |
County | Greensville Southampton Sussex |
City | Emporia |
Physical characteristics | |
Source | Confluence of Tryall Creek and Cooks Branch |
⁃ location | about 2 miles north of Pleasant Shade, Virginia |
⁃ coordinates | 36°47′16″N077°38′13″W / 36.78778°N 77.63694°W [1] |
⁃ elevation | about 168 feet |
Mouth | confluence with the Nottoway River |
⁃ location | about 1/2 mile west of Sebrell, Virginia |
⁃ coordinates | 36°46′53″N077°09′50″W / 36.78139°N 77.16389°W [2] |
⁃ elevation | about 15 feet amsl |
Length | 75.4 km/46.9 miles [3] |
Basin features | |
Progression | roughly east |
River system | Nottoway River |
Tributaries | |
⁃ left | Cooks Branch Reedy Branch Cattail Creek Uriah Branch Browns Branch Chatman Branch Applewhite Swamp Smith Swamp Poplar Swamp Hornet Swamp |
⁃ right | Tryall Creek Maclins Creek Nicholson Creek Angelico Creek |
Waterbodies | Slagles Lake |
Bridges | Greensville County Routes 605, 613, 619, 610, 617, I-95, US 301, Greensville County Route 616, Sussex County Route 611, Southampton County Routes 615, 659, 308, 609 (Crichton Bridge) |
Three Creek is a nearly 47 mile (75.4 km) long tributary of the Nottoway River in southeastern Virginia in the United States.
The Nottoway River is in southern Virginia and northeastern North Carolina. It is part of the Chowan River system, which flows into Albemarle Sound in North Carolina.
Virginia, officially the Commonwealth of Virginia, is a state in the Southeastern and Mid-Atlantic regions of the United States located between the Atlantic Coast and the Appalachian Mountains. The geography and climate of the Commonwealth are shaped by the Blue Ridge Mountains and the Chesapeake Bay, which provide habitat for much of its flora and fauna. The capital of the Commonwealth is Richmond; Virginia Beach is the most populous city, and Fairfax County is the most populous political subdivision. The Commonwealth's estimated population as of 2018 is over 8.5 million.
The United States of America (USA), commonly known as the United States or America, is a country comprising 50 states, a federal district, five major self-governing territories, and various possessions. At 3.8 million square miles, the United States is the world's third or fourth largest country by total area and is slightly smaller than the entire continent of Europe, which is 3.9 million square miles. With a population of over 327 million people, the U.S. is the third most populous country. The capital is Washington, D.C., and the most populous city is New York City. Most of the country is located contiguously in North America between Canada and Mexico.
Three Creek is formed at the confluence of Tryall Creek and Cooks Branch in Greensville County, Virginia. From the confluence, the creek flows east then south into Slagles Lake. After Slagles Lake it flows further south for about a mile and then flows roughly southeast and then northeast through swampland towards the Nottoway River. Three Creek forms the county boundary between Greensville and Sussex Counties for part of its course.
Greensville County is a county located in the Commonwealth of Virginia. As of the 2010 census, the population was 12,243. Its county seat is Emporia.
Tryall Creek rises from about 290 feet amsl near Pleasant Grove Church and flows northeast to meet Cooks Branch. Cooks Branch rises near Smoky Ordinary at about 315 feet amsl and flows east then south to meet with Tryall Creek. Cooks Branch has one tributary called Kettlestick Branch that comes in on the left. [4]
Three Creek drains a mostly forested watershed and contains a lot of swampland towards the Nottoway River. Agriculture makes a large amount of the rest of the area. [5]
Three Creek has one impoundment, Slagles Lake along its course. A number of the tributaries have their own impoundments.
The confluence of Tryall Creek and Cooks Branch is in the Piedmont of Virginia in mafic and felsic metavolcanic rocks. Both tributaries arise in granite (Tryall Creek) or granite gneiss (Cooks Branch). Three Creek flows into the Coastal Plain in the Bacon Castle Formation and then for most of its length, especially the swampy areas it is in alluvium. [6]
The Piedmont is a plateau region located in the Eastern United States. It sits between the Atlantic coastal plain and the main Appalachian Mountains, stretching from New York in the north to central Alabama in the south. The Piedmont Province is a physiographic province of the larger Appalachian division which consists of the Gettysburg-Newark Lowlands, the Piedmont Upland and the Piedmont Lowlands sections.
Granite is a common type of felsic intrusive igneous rock that is granular and phaneritic in texture. Granites can be predominantly white, pink, or gray in color, depending on their mineralogy. The word "granite" comes from the Latin granum, a grain, in reference to the coarse-grained structure of such a holocrystalline rock. Strictly speaking, granite is an igneous rock with between 20% and 60% quartz by volume, and at least 35% of the total feldspar consisting of alkali feldspar, although commonly the term "granite" is used to refer to a wider range of coarse-grained igneous rocks containing quartz and feldspar.
The Cullasaja River is a short river located entirely in Macon County, North Carolina. It is a tributary of the Little Tennessee River, into which it flows near the county seat of Franklin. It originates to the southeast, near Highlands, the county's only other town. It flows from manmade Lake Sequoyah, which is fed by Mirror Lake and other creeks and streams originating on the western side of the Eastern Continental Divide, which runs through the east side of Highlands.
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The Little Nottoway River is a 14.31 mi (23.03 km) long tributary to the Nottoway River in the United States state of Virginia. Located in the southeastern part of the state, it is part of the larger Chowan-Albemarle drainage.
Rowanty Creek is a 14-mile long creek that is a tributary to the Nottoway River in southeastern Virginia. It is formed at the confluence of Hatcher Run and Gravelly Run.
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