The Carlisle site (41WD46) is located on the Sabine River near its confluence with Lake Fork Creek in the Upper Sabine River Basin. As defined by Perttula, the Upper Sabine River Basin includes the area from the headwaters of the Sabine River to the mouths of Cherokee Bayou and Hatley Creek at the western edge of the Sabine Uplift. Lake Fork Creek is one of several large south-southeastward flowing streams within the Upper Sabine River Basin. The town of Mineola is approximately 13 kilometers (km) west of the Carlisle site. The site is situated at the tip of an upland projection overlooking the Sabine River floodplain, but extends into the floodplain to within ca 30 meters of the river bank. The Lake Fork Creek channel is approximately one km east of the site. While the site was an improved pasture for many years prior to 1975 and to the present, it had been previously cultivated. In fact, this cultivation may have contributed to its initial identification in the early 1930s, as well as its subsequent partial burial. The upland sandy soils derive from the Queen City Formation, and these are highly susceptible to erosion and colluvial downwasting. Colluvial deposition seems to have been a prominent factor in the burial of cultural materials along valley margins and lower footslopes elsewhere in the Upper Sabine Basin, and the site's topographic position suggests that both alluvial and colluvial deposition is responsible for the burial of the floodplain cultural deposits at the Carlisle site.

Site 41VN63 is a multiple component Late Archaic (circa [ca.] 5000-2500 years B.P.) and Woodland period (ca. 2500-1150 years B.P.) site on an upland landform in the upper Sabine River basin. The site was recorded by James Malone (1972) during the archaeological survey of then-proposed Mineola Reservoir on the Sabine River; the reservoir has not been built. Malone described the site in 1971 as being located on an upland ridge on the southeast side of Caney Creek, and covered a 20 x 50 m area. He noted and/or collected from the site surface chert, quartzite, and petrified wood lithic debris (n=28) and cores (n=11) . Malone also mentioned finding flake tools as well as plain pottery sherds at the site, but no such artifacts were mentioned in Malone’s tabulations. This collection has yet to be examined at the Texas Archeological Research Laboratory at The University of Texas at Austin. Shortly thereafter, Bob D. Skiles learned of the site and, with the permission of the landowner, conducted surface collections there on several occasions over the next two years, and recorded the site as GS-1 in his site recording system. In the late 1980s, Skiles loaned Perttula the artifacts he had collected from the site, and they were studied and documented at that time. Now, this many years later, the results of those analyses are provided in this article.

The Steck site (41WD529) is a 15th to early 16th century A.D. Caddo settlement situated in the far western margins of the modern Pineywoods of East Texas, in the upper Sabine River basin in Wood County. The site is specifcally situated in the uplands more than 12m above the Dry Creek foodplain, in the upper part of the Lake Fork Creek drainage basin. Two natural springs emerge from the Queen City Eocene formation immediately below the site. There are two midden deposits at the Steck site, as well as evidence for structures arranged around an open plaza in a small community. The archaeological investigations reported on in this article took place in 1976 in a ca. 9 m diameter trash midden deposit along the edge of the upland landform; the trash midden was ca. 30 cm in thickness. Available notes and analysis records have been used to reconstruct what was accomplished at the site and the kind and range of recovered artifacts.

In this article we document 18 ceramic vessels from three ancestral Caddo sites with cemeteries in the Lake Fork Creek basin in Wood County, Texas. Each site has a Late Caddo period Titus phase (ca. A.D. 1430-1680) component.

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