Caddoan Archeology Journal
The Hudnall-Pirtle (41RK4) site is situated on a large T-1 alluvial terrace of the Sabine River in northern Rusk County of Texas. This part of Texas, comm.only referred to as Northeast Texas, is part of the Southern Gulf Coastal Plain, a relatively level, sloping plain formed by pre-Pleistocene embayments of the Gulf of Mexico. From a biogeographical perspective, the site is located in the Oak-Hickory-Pine Forest. This area represents the western extension of the Southern coniferous forests, and is dominated by shortleaf, longleaf, slash, and loblolly pine trees (Jordan, Bean, and Holmes 1984:28). In the floodplains of rivers and major creeks of Northeast Texas, the dominant vegetation is hardwood trees, including oak, hickory, elm, and gum. Soils consist of light colored to dark colored sands and sandy loams, with denser clays in the floodplains of major rivers and creek. The soils have been heavily leached by relatively high rainfall that ranges between 40 and 50 inches per year (Bomar 1983). Soils are generally acid, causing poor preservation of faunal remains in archeological deposits.
Burseth, James E.
"Hudnall-Pirtle Site: An Early Caddoan Mound Complex in Northeast Texas,"
Index of Texas Archaeology: Open Access Gray Literature from the Lone Star State: Vol. 1991
, Article 15.
Available at: https://scholarworks.sfasu.edu/ita/vol1991/iss1/15
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