Sabine River, 1962, prior to creation of Toledo Bend
Reservoir, Sabine County, Texas (on left bank). TARL archives.
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The southwestern part of the Caddo Homeland was home to
the Hasinai Caddo groups. This is the only area that is not part of the
Red and Mississippi drainage system. The Sabine, Neches, and Angelina
rivers are part of the Sabine watershed. The Sabine empties into the Gulf
of Mexico almost 300 miles west of the mouth of the Mississippi. The rivers
are prone to flooding and have relatively wide floodplains with meander
features such as oxbow lakes and terraces of differing ages. Prior to
historic land-use practices, the bottomlands were covered in dense hardwood
forests and swampy areas.
The southwestern Caddo Homeland lies within the southern
pine forests (piney woods) of deep east Texas. Upland areas here typically
have shallow soils poorly suited for farming. The deeper, more fertile
soils along the river floodplains attracted Caddo farmers. Hardwood forests
along the rivers also provided habitat for many of the plants and animals
upon which the Caddo depended.
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Prior to 20th-Century, large hardwood trees, such
as this white oak with a 16 foot circumference, dominated the floodplain
forests of the southern Caddo Homeland. TARL archives, Bayou Loco project,
Nacogdoches County, Texas
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