scholarly journals Caddo Ceramic Assemblages from Sites in the Ayish and Palo Gaucho Bayou Basins, San Augustine County, Texas

Author(s):  
Timothy K. Perttula

In 1939 and 1940, G. E. Arnold recorded a number of archaeological sites in and around San Augustine, in East Texas, as part of a Works Progress Administration-funded (WPA) archaeological survey of East Texas. The eight sites of concern in this article are in either the Ayish Bayou or Palo Gaucho Bayou basins; the former is a southward-flowing tributary to the Angelina River, while the latter is a southeast-flowing tributary to the Sabine River. In several instances, depending upon the circumstances, Arnold was able to collect substantial numbers of ancestral Caddo ceramic and lithic artifacts from several of these sites. The character of these ceramic sherds—and their stylistic and technological similarities or differences to the ceramic assemblages from the 1716-1719, 1722-1773 Mission Dolores de los Ais in San Augustine as well as other known sites on Palo Gaucho and Housen bayous and Attoyac Bayou are the primary focus of the analysis reported on herein, but other temporally diagnostic ceramic and lithic artifacts are discussed as well.

Author(s):  
Timothy K. Perttula ◽  
Mark Walters

In the winter of 2003, the junior author completed archaeological survey investigations of a small area of the Sabine River valley in northeastern Smith County in the East Texas Pineywoods. The work consisted of limited surface collections and shovel tests, and four archaeological sites were found during the work. The sites are about 2.4-3.0 km south-southwest of the Early Caddo period Boxed Spring mound site (41UR30) on the north side of the Sabine River. Two of the archaeological sites (41SM307 and 41SM308) are situated on alluvial landforms in the Sabine River valley at elevations of ca. 280-290 ft. amsl. The other two (41SM309 and 41SM310) are on upland landforms at elevations of 310 ft. amsl and 350 ft. amsl, respectively.


Author(s):  
Timothy K. Perttula ◽  
Robert Richey

This article discusses a collection of ancestral Caddo ceramic and lithic artifacts found at the Robert Richey site in northern Van Zandt County in East Texas. The site is in a pasture on an upland landform facing year-round flowing Caney Creek about 130-180 m to the east, a northern-flowing tributary that merges with the Sabine River about 2.2 miles to the north. The site lies within the flood pool of the long-defunct Mineola Reservoir, but the Robert Richey site was not recorded at the time of the early 1970s archaeological survey of the reservoir. Sites 41VN53-56, prehistoric sites of either uncertain age (41VN53), Woodland period age (41VN54, 41VN55, and 41VN56), as well as ancestral Caddo (41VN55), likely Early or Middle Caddo period in age. were recorded on alluvial terraces on both sides of Caney Creek not far from the Robert Richey site. For years, Mr. Richey’s father had been advised by one of the old-timers who owned the adjoining ranch about a rise in his field “that particular mound in the pasture was an Indian mound.” Richey’s father identified the structure to him years ago. So, it was a known and identifiable rise in their land that had (tongue-in-cheek) been called an Indian mound for many years. Richey’s investigation into the rise was prompted by the fact that he had found a ceramic vessel sherd along the banks of a dam of a recently constructed pond. That sherd was discovered approximately 180 m south of the Robert Richey site, on a landform with tan sandy loam sediments; this place may be 41VN55 recorded by Malone. Malone indicated the site had plain sherds, scrapers, lithic debris, Gary points, as well as an ancestral Caddo sherd with a cross-hatched incised rim and rows of fingernail impressed punctations on the vessel body. From there, Mr. Richey took that rumor a step further last year and dug four test trenches about 3 feet deep and 10 feet long in the rise and waited for rain. Frankly, he did not expect to discover anything as he has not found much in the way of artifacts on the place. After digging the trenches he waited for rain. After a rain, the artifacts discussed in this article were found over an area about 15 m in diameter; they represent about 50 percent of what had been noted there. He did not note any charcoal in the trenches. The soil on the Robert Richey site appears to be a reddish-brown loam, and not the black lands characteristic of the soils in the Sabine River floodplain. There is an old and majestic Oak tree growing along the edge of the rise. Generally speaking, this is pasture land.


Author(s):  
Timothy Perttula

The Pearson site (41RA5) in the Blackland Prairie of East Texas is one of a number of aboriginal archaeological sites recorded during a 1957 archaeological survey of the flood pool of then proposed Lake Tawakoni on the Sabine River; the site is now inundated. The Pearson site was located on several low sandy rises across ca. 25 acres in the Hooker Creek-Sabine River floodplain, and these rises had both aboriginal and European artifacts on the surface. Johnson and Jelks, and Duffield and Jelks have argued that the Pearson site was the Tawakoni-Yscani village visited by a Spanish missionary in 1760 and part of a recently defined Norteno focus, a complex of sites apparently associated with the Wichita tribes. Schambach, by contrast, considers the Pearson site to be an 18th century Tunican entrepot.


Author(s):  
Timothy Perttula

The Beckham (41SB35) and Print Bell (41SB36) sites were recorded by Gus E. Arnold of The University of Texas in December 1939 during his WPA-sponsored archaeological survey of East Texas. Both sites have substantial ancestral Caddo deposits. The Beckham site is in the Housen Bayou basin of the larger Sabine River drainage system, while the Print Bell site is on a tributary of the Angelina River (Figure 1). Excavations were conducted at the Print Bell site in the early 1950s by Jelks (1965:88- 93) prior to the construction of Lake Sam Rayburn, but there have been no further investigations at the Beckham site after Arnold’s 1939 survey.


Author(s):  
Timothy K. Perttula ◽  
Mark Walters

One of the more distinctive of the decorative methods represented in the ancestral Caddo ceramic assemblages from Lake Sam Rayburn sites is sherds and vessels with incised–punctated decorative elements. This diversity in the range and character of sherds and vessels with incised–punctated decorative elements is also the case in ancestral Caddo sites on the Sabine River and tributaries in the Toledo Bend Reservoir area of East Texas and Northwest Louisiana. Jelks included the incised–punctated vessels and sherds from the Lake Sam Rayburn sites in a newly defined type: Pineland Punctated–Incised. Pineland Punctated– Incised is a grog and/or bone–tempered utility ware, and occurs primarily as beaker–shaped jars as well as ollas and deep bowls. The vessels have concentric, triangular, rectangular, and curvilinear incised zones on the rim filled with tool punctation. Ollas and bowls have design elements on the vessel bodies. At Lake Sam Rayburn sites, Pineland Punctated–Incised sherds and vessels occur in both Middle Caddo (ca. A.D. 1200–1400/1450) and Late Caddo (ca. A.D. 1400/1450–1680) contexts. Based on the analyses discussed below, incised–punctated utility wares are most abundant in later Middle Caddo period components estimated to date from ca. A.D. 1300–1400/1450, and least common in post–A.D. 1400/1450 Late Caddo period components.


Author(s):  
Timothy K. Perttula

Gus Arnold identified and recorded many ancestral Caddo sites during his 1939-1940 Works Progress Administration (WPA)-sponsored archeological survey of East Texas. Currently, I have been engaged in studying the artifact collections from 51 WPA sites in Angelina, Cherokee, Gregg, Jasper, Nacogdoches, Sabine, and San Augustine counties, especially the ceramic sherd assemblages, held by the Texas Archeological Research Laboratory at The University of Texas. The sites are located in the Sabine River, Neches River, Angelina River, and Attoyac Bayou stream basins.


Author(s):  
Timothy K. Perttula

The 13 ancestral Caddo sites and collections discussed in this article were recorded by G. E. Arnold of The University of Texas at Austin between January and April 1940 as part of a WPA-funded archaeological survey of East Texas. The sites are located along the lower reaches of Patroon, Palo Gaucho, and Housen bayous in Sabine County, Texas. These bayous are eastward-flowing tributaries to the Sabine River in the Toledo Bend Reservoir area, but only 41SB30 is located below the current Toledo Bend Reservoir flood pool. This is an area where the temporal, spatial, and social character of the Caddo archaeological record is not well known, despite the archaeological investigations of Caddo sites at Toledo Bend Reservoir in the 1960s-early 1970s, and in more recent years.


Author(s):  
Harry J. Shafer

This article presents a detailed analysis of chipped stone artifacts from the Redwine Site (41SM193), a Middle Caddo mound and village site located on the headwaters of Auburn Creek, a tributary of the Sabine River. The collection includes chipped stone recovered from the surface, test excavations, and arrow points associated with two adult burials. The site was investigated by avocational archeologist Sam Whiteside in the 1960s and more recently by Mark Walters and Patti Haskins under the direction of John Keller of Southern Archaeological Consultants. The investigations and material culture have been briefly described. This study is designed to take a closer look at the lithics with an emphasis on technological, material, contextual, and typological analyses of the lithic artifacts, and to compare the findings to the lithics at the nearby and possibly contemporaneous Leaning Rock site (41SM325). Archaeologists generally have not focused on Caddo lithic technology, and this class of material culture remains only cursorily studied. Rather, ceramics have received the vast amount of attention with little emphasis on other types of material culture. One reason for a lack of attention to lithics may be that East Texas generally lacks the resources from which well-crafted artifacts could have been made. Small chert cobbles or pebbles, and pebbles of orthoquartzite and silicified wood constitute the major sources for chipped stone. Lacking are outcrops of excellent chert (such as the Edwards Plateau) or novaculite (eastern Oklahoma and southwestern Arkansas). Artifacts of from these two sources are introduced into East Texas in finished form. Edwards chert and novaculite debitage found in East Texas sites is likely from recycling broken finished artifacts. When lithics are reported, they are generally relegated to brief descriptive treatments with an emphasis on artifact classification and raw material distribution. Detailed technological treatments are rare (for exceptions. It is preferable in archaeological studies to integrate all classes of material culture in analysis and interpretation to see what sets of material co-occur both functionally, technologically, stylistically, and symbolically. Rarely is this extended effort even attempted in archaeological studies in Texas, but until all surviving aspects of material culture are integrated and interpreted as a cultural whole and within the known context of Caddo culture and life way, only fragments of past cultures will be stressed with the risk of gross misinterpretation. While it is acknowledged that this study treats only a fragment of the material culture from the Redwine site, I will attempt to integrate the findings in such a way as to relate it to extant information from the site available to me from other sources. Another objective of this study is to examine the lithics from the Redwine site and compare them with the sample from the nearby Leaning Rock site. Both collections are assumed to be approximately the same age and may be from the same extended Middle Caddo community. I will specifically emphasize the technological styles of the formal tools and the implications of the debitage with regards to technology and raw material.


Author(s):  
Timothy K. Perttula

The Dead Cow site is an early to mid-19th century archaeological site located within the northern part (Sabine River basin) of the proposed Republic of Texas 1836 Cherokee Indians land grant in East Texas, generally east of the downtown area of the modem city of Tyler. Cherokee Indians had moved into East Texas by the early 1820s, and "most of the Cherokees cleared land and carved out farms in the uninhabited region directly north of Nacogdoches, on the upper branches of the Neches, Angelina, and Sabine rivers. By 1822 their population had grown to nearly three hundred." To date, historic archaeological sites identified as being occupied by the Cherokee during their ca. 1820-1839 settlement of East Texas remain illusive, and to my knowledge no such sites have been documented to date in the region. This article considers, from an examination of the historic artifact assemblage found here, the possibility that the Dead Cow site is a Cherokee habitation site.


Author(s):  
Timothy K. Perttula

The Boatstone site (GC-50 in Buddy Jones' site numbering system) is one of many Caddo sites that Buddy Jones investigated along the Sabine River and its tributaries in the Longview, Texas, area. In most cases, his investigations at the sites consisted of the surface collection of ceramic and lithic artifacts, and only in rare cases did Jones complete analyses or publications on his investigations. This article discusses the ancestral Caddo ceramic assemblage from the Boatstone site, which is situated near the confluence of Iron Bridge Creek and the Sabine River in southeastern Gregg County in the East Texas Pineywoods. This collection is curated at the Gregg County Historical Museum.


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