Official state symbol South Carolina State Soil

Orangeburg Soil Series

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Orangeburg Soil Series

Official State Soil of South Carolina

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Artsiom Dusau Reviewed by Artsiom Dusau
Overview

State Soil of South Carolina

South Carolina's state soil is the Orangeburg series — a deep, yellowish-red soil named after Orangeburg County, covering millions of acres on the sandy uplands of the Coastal Plain where tobacco, cotton, and soybeans have been grown for over two centuries. This profile appears in the list of U.S. state soils.
Status
Official state soil

South Carolina State Soil

Orangeburg soil has a split personality: the surface is pale and gritty — sandy loam that crumbles in your hand — while the subsoil is vivid yellowish-red to red clay, stained by iron that has been migrating downward for thousands of years. That contrast is visible in every road cut across the South Carolina interior.

The soil is well drained and deep, which makes it naturally productive for row crops and pine timber. In its undisturbed state, it supported longleaf pine, loblolly pine, and turkey oak — the fire-maintained woodland that once covered most of the inner South Carolina Coastal Plain.

Why South Carolina Chose the Orangeburg Soil

Soil scientists at the USDA Natural Resources Conservation Service selected the Orangeburg series to represent South Carolina because it is the most extensive and agriculturally significant soil on the state's inner Coastal Plain — the landscape that has shaped South Carolina farming since the 1700s.

The series is named after Orangeburg County in the center of South Carolina, where the soil was first formally described. Orangeburg County has been a hub of Coastal Plain agriculture since German and Swiss settlers established farms there in the 1730s.

The Orangeburg series is recognized by the USDA as South Carolina's state soil. It was selected because it captures the sandy, well-drained upland landscape that separates the river swamps and defines the character of the South Carolina interior.

Orangeburg Soil Profile and Horizons

Measured Orangeburg profile with distinct horizons exposed beside a scale
A measured Orangeburg profile exposes the horizon sequence soil scientists use to identify the series. Official USDA descriptions classify soils by recurring depth, texture, drainage, and parent material patterns.

Dig into Orangeburg soil and the surface is pale and gritty — sandy loam that crumbles in your hand. A foot below the surface, the sand gives way to a brighter, yellowish-brown transition zone. Keep digging and the soil turns unmistakably red: a sticky, iron-rich clay that marks the argillic horizon. The color deepens toward pure red at two to three feet, then fades back to pale yellowish brown as the ancient marine sediments return.

0" 7" 14" 18" 30" 44" 65"
Ap
E
BE
Bt1
Bt2
BC
Plow layer 0–7 in
sandy loam
light and gritty; organic matter keeps color dark
Eluvial layer 7–14 in
loamy sand
iron and clay leached downward; pale and loose
Transition layer 14–18 in
sandy loam
iron begins to accumulate; precursor to argillic below
Upper argillic 18–30 in
sandy clay loam
clay films on peds; diagnostic argillic horizon begins
Lower argillic 30–44 in
clay loam
reddest layer; iron oxides from marine sediment weathering
Parent material zone 44–65 in
sandy clay loam
iron decreases; original Coastal Plain sediment reasserts

Where Orangeburg Soil Grows in South Carolina

Landscape associated with Orangeburg in South Carolina
A landscape scene from South Carolina. Orangeburg is associated with the broader terrain where the series is most often mapped.

Orangeburg soil covers the gently rolling uplands of the inner Coastal Plain — the broad, level-to-undulating terrain that runs across the middle third of South Carolina between the Fall Line and the tidewater counties near the coast. Elevations range from 100 to 400 feet, with annual rainfall of 44 to 52 inches.

The series is concentrated in Orangeburg, Calhoun, Bamberg, and Barnwell counties at its center and extends north and south through Lexington, Richland, Sumter, Lee, and Williamsburg counties.

Orangeburg Soil Series · 10 counties
Other counties

Farming and Forests on Orangeburg Soil

Field or habitat scene associated with Orangeburg in South Carolina
A field or habitat scene from South Carolina. Orangeburg is tied to the working landscape and plant communities described for this state soil.

Tobacco has been the signature crop on Orangeburg soil for nearly 300 years. The well-drained, sandy surface that discourages many crops is exactly what flue-cured tobacco needs: fast drainage, warm soil temperatures, and low moisture retention that concentrates sugars in the leaf. South Carolina's tobacco belt runs directly through Orangeburg soil country.

Cotton, corn, soybeans, and peanuts are the other major row crops. Soybeans now exceed tobacco in total Orangeburg acreage as farm economics shifted through the late twentieth century. Sweet potatoes grow well on the sandier surface layers, particularly in the southern counties.

Loblolly pine plantations cover large areas of Orangeburg soil that were retired from crop production. Managed pine is a major industry across the inner Coastal Plain. Before European settlement, longleaf pine, turkey oak, and bluejack oak formed the open, fire-maintained woodland over most of this landscape.

Orangeburg Soil Facts

Quick Answers

What is South Carolina's state soil?
South Carolina's state soil is the Orangeburg series, a deep, yellowish-red to red soil found on the sandy uplands of the inner Coastal Plain. It is recognized by the USDA Natural Resources Conservation Service as South Carolina's representative state soil and supports tobacco, cotton, soybeans, and loblolly pine across the middle of the state.
Why is it called Orangeburg soil?
The series is named after Orangeburg County in central South Carolina, where USDA soil scientists first formally described and mapped the soil. Orangeburg County has been a center of Coastal Plain farming since the 1730s and sits in the heart of the soil's distribution.
What color is Orangeburg soil?
The surface is a pale sandy brown — light-colored and gritty. Below a pale eluvial layer, the argillic subsoil is yellowish red to red, stained by iron oxide minerals that formed as ancient marine sediments weathered over millions of years. The vivid contrast between pale surface and red subsoil is visible in road cuts across the inner Coastal Plain.
Where is Orangeburg soil found in South Carolina?
Orangeburg soil covers the gently rolling uplands of the inner Coastal Plain — the broad terrain running across the middle of South Carolina between the Fall Line and the tidewater coast. It is most concentrated in Orangeburg, Calhoun, Bamberg, Barnwell, and Lexington counties at elevations of 100 to 400 feet.
What crops grow in Orangeburg soil?
Tobacco, cotton, corn, soybeans, and peanuts are the main crops. Flue-cured tobacco has grown on Orangeburg soil for nearly 300 years, favored by the fast-draining sandy surface. Soybeans now cover more acres than tobacco. Sweet potatoes grow on the sandier sites. Loblolly pine plantations cover retired farmland.
Who chose Orangeburg as South Carolina's state soil?
Soil scientists at the USDA Natural Resources Conservation Service selected the Orangeburg series to represent South Carolina. It was chosen because it is the most extensive and agriculturally significant soil on the inner Coastal Plain — the landscape at the center of South Carolina's farming history.
How deep is the red clay layer in Orangeburg soil?
The argillic horizon — the red clay subsoil — runs from about 18 to 44 inches below the surface. Below that, a transition zone grades back into the pale parent material around 44 to 65 inches. The full soil profile is typically more than five feet deep before reaching unweathered marine sediment.

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