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Rowanty Creek facts for kids

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Rowanty Creek
Location of the mouth of Rowanty Creek
Location of the mouth of Rowanty Creek
Other name(s) Tributary to Nottoway River
Country United States
State Virginia
County Sussex
Prince George
Dinwiddie
Physical characteristics
Main source confluence of Hatcher Run and Gravelly Run
about 4 miles east of Dinwiddie, Virginia
about 98 feet
37°05′40″N 077°28′25″W / 37.09444°N 77.47361°W / 37.09444; -77.47361
River mouth confluence of Rowanty Creek and Nottoway River
about 2 miles northeast of Stony Creek, Virginia
50 feet amsl
36°58′17″N 077°20′46″W / 36.97139°N 77.34611°W / 36.97139; -77.34611
Length 22 km/14 miles
Basin features
Progression southeast
River system Nottoway River
Tributaries
  • Left:
    Hatcher Run
    Picture Branch
    Rocky Branch
    Arthur Swamp
    Warren Swamp
  • Right:
    Gravelly Run
    Little Cattail Creek
    Health Meadows Branch
    Fox Branch
    Harvells Branch
    Bolling Swamp
    Galley Swamp
Bridges Dinwiddie County 669
Dinwiddie County 703
US 301
I-95
Sussex County 602

Rowanty Creek is a stream in southeastern Virginia. It is about 14 miles (22 kilometers) long. This creek flows into the Nottoway River.

Rowanty Creek starts where two smaller streams, Hatcher Run and Gravelly Run, meet. This meeting point is about 4 miles east of Dinwiddie, Virginia.

The Journey of Rowanty Creek

Rowanty Creek flows mostly to the southeast. It begins in a swampy area where many small streams twist and turn. As it flows, the creek sometimes gets narrower.

Near where it joins the Nottoway River, several swamps are connected to Rowanty Creek. These swamps are important parts of the local environment.

How the Land Shaped the Creek

Rowanty Creek flows through an area called the Coastal Plain. This area is made of soft sediments like sand, silt, and clay. These materials were carried by water and deposited over a long time.

However, the two streams that form Rowanty Creek, Hatcher Run and Gravelly Run, start in a different type of land. They begin in an area with hard rock called Petersburg Granite. This granite is part of the Piedmont region, which is higher and rockier than the Coastal Plain.

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