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Three Creek
Location of the mouth of Three Creek
Location of the mouth of Three Creek
Other name(s) Tributary to Nottoway River
Country United States
State Virginia
County Greensville
Southampton
Sussex
City Emporia
Physical characteristics
Main source Confluence of Tryall Creek and Cooks Branch
about 2 miles north of Pleasant Shade, Virginia
about 168 feet
36°47′16″N 077°38′13″W / 36.78778°N 77.63694°W / 36.78778; -77.63694
River mouth confluence with the Nottoway River
about 1/2 mile west of Sebrell, Virginia
about 15 feet amsl
36°46′53″N 077°09′50″W / 36.78139°N 77.16389°W / 36.78139; -77.16389
Length 75.4 km/46.9 miles
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 river in southeastern Virginia, United States. It flows for almost 47 miles (75.4 km) and is a tributary (a smaller stream that flows into a larger one) of the Nottoway River.

Where Does Three Creek Flow?

Three Creek starts where two smaller streams, Tryall Creek and Cooks Branch, meet in Greensville County, Virginia. From there, it flows east and then south into a place called Slagles Lake.

After leaving Slagles Lake, the creek continues south for about a mile. Then, it turns and flows generally southeast and northeast through swampy areas. It keeps going until it reaches the Nottoway River. For some of its journey, Three Creek forms the border between Greensville and Sussex Counties.

What is the Three Creek Watershed Like?

The watershed is all the land area that drains water into a river or creek. Three Creek's watershed is mostly covered by forests. It also has a lot of swampy land, especially closer to the Nottoway River. Farming is another big part of the land use in this area.

How Has Three Creek Been Changed?

Three Creek has one impoundment (a place where water is held back, usually by a dam) along its path, which is Slagles Lake. Some of the smaller streams that flow into Three Creek also have their own impoundments.

What is the Geology of Three Creek?

The area where Tryall Creek and Cooks Branch meet is in the Piedmont region of Virginia. This area has rocks that were formed from ancient volcanoes.

  • Tryall Creek starts in an area with granite rock.
  • Cooks Branch begins where there is granite gneiss (a type of rock similar to granite but with layers).

As Three Creek flows, it moves into the Coastal Plain region. Here, it passes through an area with a type of rock called the Bacon Castle Formation. For most of its length, especially in the swampy parts, the creek flows over alluvium. Alluvium is a mix of sand, silt, and clay that rivers deposit over time.

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