Official state symbol Louisiana State Soil

Ruston Soil Series

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Ruston Soil Series

Official State Soil of Louisiana

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Artsiom Dusau Reviewed by Artsiom Dusau
Overview

State Soil of Louisiana

Louisiana's state soil is the Ruston series — a deep red loamy soil named for Ruston in Lincoln Parish that covers the rolling uplands of north Louisiana, where it grows some of the state's largest longleaf and loblolly pine forests and its signature sweet potato crop. This profile appears in the list of U.S. state soils.
Status
Official state soil

Louisiana State Soil

The Ruston soil series is Louisiana's official state soil. It sits on the gently rolling uplands and ridgetops of the West Gulf Coastal Plain in north and central Louisiana — old, stable land surfaces that have been above sea level and weathering for a very long time.

Ruston is an Ultisol, the most heavily leached of the major soil orders in humid climates. Ultisols form where warm temperatures and high rainfall have dissolved and washed away most of the soluble minerals over millions of years, leaving behind iron oxides, aluminum oxides, and stubborn clay minerals.

The result is a soil that looks poor — pale and sandy at the surface, with a bleached layer just below — but has a deep, clay-enriched subsoil that holds water and nutrients where roots can reach them. It is the dominant agricultural soil of north Louisiana and one of the most common upland soils in the Gulf South.

Why Louisiana Chose the Ruston Soil

The Ruston series was first described and established in Lincoln Parish, Louisiana, and named for Ruston — the parish seat and home of Louisiana Tech University. USDA soil scientists follow the standard practice of naming series after local geographic features, and Ruston was the center of the region where this soil was first systematically studied.

Louisiana soil scientists and the USDA Natural Resources Conservation Service identified the Ruston series as the most representative upland soil of north Louisiana, the region that defines the state's timber and sweet potato industries. The series is widespread, well documented, and directly tied to the land uses that shaped north Louisiana's economy.

The Ruston series was chosen as the state soil because it captures something distinct about Louisiana's landscape — not the famous delta and marshes of the south, which attract most attention, but the old, red-soiled uplands of the north that have supported farming and forestry for generations.

Ruston Soil Profile and Horizons

Measured Ruston profile with distinct horizons exposed beside a scale
A measured Ruston 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.

The Ruston profile is a study in what happens when warm rain falls on the same land for millions of years. At the surface, the soil is pale — fine sandy loam, not much color. Just below is a bleached layer where water has washed minerals downward. Then, abruptly, the soil shifts to reddish yellow and then to red as you enter the argillic horizon where iron oxide has concentrated.

That red clay layer can be several feet thick. Soil scientists call it a Bt horizon with kandic properties — a deeply weathered argillic zone where kaolinite clay dominates and iron is so concentrated it looks like brick. Below it, the soil stays red well past the depth most crop roots reach.

0" 8" 16" 32" 60" 80"
Ap
E
Bt1
Bt2
Bt3
Surface layer 0–8 in
fine sandy loam
sandy, low organic matter; pale compared to vivid subsoil
Eluvial layer 8–16 in
fine sandy loam
bleached by downward mineral washing; visible as lighter band
Upper argillic subsoil 16–32 in
sandy clay loam
iron oxide builds rapidly; reddening marks the weathered zone
Deep red clay 32–60 in
clay
hematite-stained kaolinite clay; stores water through dry spells
Lower subsoil 60+ in
clay loam
iron-stained parent sediment from ancient Coastal Plain deposits

Where Ruston Soil Grows in Louisiana

Piney Woods Map in Louisiana
Piney Woods Map in Louisiana. Ruston is associated with the broader landscape where the series is most often mapped.

Ruston soil covers the rolling upland terrain of north and central Louisiana, where the West Gulf Coastal Plain rises above the river floodplains and deltas of the south. This is a landscape of pine forests, red clay roads, and small farms on gently sloping ridges.

Lincoln Parish, where the series is named, is near the center of the Ruston soil belt. The series extends through the surrounding parishes — Claiborne, Union, Bienville, Jackson, Winn, Natchitoches, and others — covering much of the land that lies between the Red River to the west and the Ouachita River valley to the east.

Unlike the famous soils of south Louisiana — the rich alluvial silts of the Mississippi delta or the organic soils of the coastal marshes — Ruston soil sits on old, stable uplands that have been forming and weathering since before the Mississippi River built its current delta.

Ruston Soil Series · 12 counties
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Farming and Forests on Ruston Soil

North Louisiana Pines in Louisiana
North Louisiana Pines in Louisiana. Ruston is tied to the working landscape and plant communities described for this state soil.

Longleaf pine and loblolly pine are the dominant plants on Ruston soil today, covering millions of acres of north Louisiana uplands in managed timber production. The deep, well-drained profile suits pine well — roots reach deep into the red clay subsoil, and the sandy surface layer dries quickly enough to prevent root rot. North Louisiana's timber industry is one of the most productive in the South, and Ruston soil underlies most of it.

Sweet potatoes are the crop most associated with Ruston soil in Louisiana. The state is among the leading sweet potato producers in the United States, and north Louisiana — particularly Beauregard, Evangeline, and neighboring parishes where similar soils occur — grows most of that crop. Sweet potatoes need deep, loose, well-drained soil to develop without cracking or rotting. Ruston's sandy surface and deep profile provide exactly those conditions.

Cotton was the defining crop of north Louisiana for most of the nineteenth and early twentieth centuries, and Ruston soil supported most of it. As cotton declined, farmers shifted to timber, soybeans, corn, and hay. The red clay subsoil holds enough water to carry row crops through short dry spells, which is important in a climate where summer rainfall is inconsistent.

Ruston Soil Facts

Quick Answers

What is Louisiana's state soil?
Louisiana's state soil is the Ruston series, a deep red loamy soil found on the rolling uplands of north and central Louisiana. It is named for Ruston, the seat of Lincoln Parish, where the series was first formally described by USDA soil scientists.
Why is Ruston soil red?
The red color comes from hematite — an iron oxide mineral that forms when other minerals dissolve away under warm, wet conditions. North Louisiana gets heavy rainfall and stays warm year-round. Over millions of years, that climate leached out calcium, magnesium, and most other soluble minerals, leaving iron concentrated in the subsoil as hematite. The same process makes soils red across the entire Gulf South.
What is an Ultisol?
An Ultisol is a heavily leached soil that forms in warm, humid climates. The name comes from the Latin ultimus, meaning last, because these soils are at an advanced stage of weathering — most of the easily dissolved minerals are gone. Ultisols are common across the southeastern United States, where warm temperatures and high rainfall drive intense long-term leaching. Ruston is an Ultisol; Kentucky's Crider is an Alfisol; Iowa's Tama is a Mollisol — each reflects a different climate and weathering history.
What grows in Ruston soil?
Longleaf pine, loblolly pine, and slash pine are the dominant plants on Ruston soil, covering millions of acres of managed timber land in north Louisiana. Sweet potatoes are the most distinctive crop — Louisiana is among the leading sweet potato producers in the United States, and the Ruston series provides the deep, loose, well-drained profile the crop needs. Cotton historically dominated, and corn and soybeans are grown on Ruston soil today.
Where is Ruston soil found in Louisiana?
Ruston soil is found on the rolling uplands of north and central Louisiana, primarily in Lincoln, Claiborne, Union, Bienville, Jackson, Winn, Natchitoches, and surrounding parishes. It sits on old Coastal Plain uplands that rise above the river floodplains and marshes of south Louisiana.
How is Ruston soil different from south Louisiana soils?
Ruston is an old, leached, red upland soil formed over millions of years on stable high ground in north Louisiana. South Louisiana soils are geologically young — they were deposited by the Mississippi River and the Gulf of Mexico within the last few thousand years. They are dark, organic-rich alluvial silts and marsh peats, not red clay. Ruston and the Mississippi delta soils are among the most geologically different soils in the same state.
Why is the surface of Ruston soil paler than the subsoil?
The surface layers of Ruston soil are sandy and relatively pale because water has been washing minerals downward for a very long time. Just below the surface is an eluvial layer — a bleached zone where iron and clay have been leached out and moved deeper. Below that, those same iron compounds accumulated, turning the subsoil bright reddish yellow and then deep red. The dramatic color change from pale surface to vivid subsoil is one of the most recognizable features of Gulf South Ultisols.

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