Richard Walter and Andy Cloud are visiting researchers from the Center for Big Bend Studies at Sul Ross State University in Alpine, Texas. This article is part of the March 2018 TARL Newsletter.
In the 1940s, pioneer archaeologist J. Charles Kelley hypothesized that sometime after A.D. 1450, villagers from the La Junta region began making their own pottery rather than acquiring it from outside sources in the Casas Grandes and Jornada Mogollon regions as they had done for the previous two hundred years. Their new, local-made pottery was distinguished from earlier wares by being largely undecorated sand-tempered brownwares with a lesser number of decorated and surface-treated vessels bearing simple designs (Fig. 1). Limited petrographic and Instrumental Neutron Activation Analyses (INAA) have largely supported Kelley’s hypothesis, but additional analyses are needed to refine our understanding of these local wares. The La Junta Ceramic Project, designed to address this shortcoming, focuses on these later brownwares from five village sites at La Junta. The Center for Big Bend Studies (CBBS) plans to submit around 300 sherds for both INAA and petrographic analyses from collections housed at the CBBS and the Museum of the Big Bend—both of Sul Ross State University in Alpine, Texas—and the Texas Archeological Research Laboratory (TARL) in Austin.
CBBS archeologists Taylor Greer and Richard Walter recently chose ca. 70 plain brownware, red-on- brown, surface-treated, and slipped earthenware sherds from various La Junta village sites housed at TARL. Most of these sherds were recovered from the Millington site (41PS14), a pueblo occupied by various groups over time and the site of Mission San Cristobál established ca. A.D. 1684. The project is being funded by the Texas Preservation Trust Fund with additional help from the National Science Foundation Subsidy Program for Archaeological Research at the Missouri University Research Reactor Center. Results from these studies are expected to provide new insights concerning acculturation, cultural interactions, and social systems of the La Junta villagers during a period of rapid cultural change amidst Spanish missionization and colonization.
This article is part of the March 2018 TARL Newsletter.
TARL’s map collection is quite extensive. Besides curating maps from present day projects, TARL’s map collection includes those from WPA work around the State of Texas during the 1930s and early 1940s, maps from the archeological work done during the primary Reservoir building era and later, and maps done during the extensive George C. Davis site (41CE19) excavations. Those project maps you may have seen or at least heard about. TARL also has copies of many historic maps as well (many of these maps are white on black copies). Some of the interesting and unique maps in our collection are:
A Geographical Map to Show the Viceroy of New Spain the Results of a Reconnaissance, 1717
A Replica Chart of the Galveston-Houston Area ca. 1836
New Map of the Western Part of the Province of Louisiana, based on the Observations and Reports of Bernard de la Harpe, 1720
A Map of the Red River in Louisiana from the Spanish Camp where the exploring part of the U.S. was met by the Spanish troops to where it enters the Mississippi. Reduced from protracted courses & corrected to the latitude by NS King 1806
Abstract of Title to the Manchester Subdivision: City of Houston and Township of Harrisburg, Harris Co., Tx., Sept 1921
Outline Maps of South America by Alex Krieger, 1961
This map collection is available for both professional and avocational researchers to use. Please let TARL staff know ahead of time, so that we can retrieve the maps you have requested to view.
WPA-Era Maps of the Rob Roy Site, 41TV41
One example of the use of the TARL map collection in current research comes from the work of Dan Prikryl, a well-known Texas archeologist. Dan has been doing research on the Rob Roy site (41TV41), using maps from the 1938-1939 WPA excavations at that site and has prepared this write-up for the Friends of TARL Newsletter:
The map file for the Rob Roy Site, 41TV41, contains the original stratigraphic profile drawings of various parts of the excavation blocks. These profiles are very helpful since the professional archeologists did not provide a thorough discussion of the soil stratigraphy for all the different parts of the site in their field notes summary. The map file also contains the original contour map drawn of the site and surrounding vicinity on a large Mylar sheet. This map is invaluable since the site and surrounding river valley are currently partially inundated by Lake Austin. It has sufficient detail for usage in scientific publications.
Nadya Prociuk is an Affiliated Researcher at TARL. This article is part of the March 2018 TARL Newsletter.
For the past several months, TARL’s own Lauren Bussiere and I have been working with the A. E. Anderson Collection, which has been housed at TARL for more than 65 years. A. E. Anderson was a civil engineer based in Brownsville, and over the course of his career he surveyed and collected from around 200 sites in the Rio Grande Delta, both in Texas and Tamaulipas. Anderson’s collection contains over 2, 000 prehistoric artifacts such as shell ornaments and tools, chipped stone tools, bone, groundstone, and ceramics. Thanks to his lifetime of work, Anderson’s collection is the most significant resource currently available for the study of the cultural prehistory of the Rio Grande Delta.
Several researchers have worked with the Anderson Collection over the years, though none have completely inventoried or analyzed the collection up to this point. T. N. Campbell studied the collection when it first arrived at the University of Texas in the 1940s, and Richard MacNeish also used the collection as a starting point for his definitions of the Brownsville and Barril Complexes. In the 1970s Elton Prewitt re-surveyed the Anderson sites located in Cameron County, and compiled an inventory of the artifacts from those sites. Multiple salvage and cultural resource management projects have been undertaken in the Rio Grande Valley that have added to our understanding of the archaeology of the area. Unfortunately, work with Anderson’s collection stalled until the late 1990s when William J. Wagner III completed a Master’s thesis on the ceramics in the collection. With his research Wagner confirmed Gordon Eckholm’s early assessment that a number of the ceramics in the Anderson Collection actually came from the Huastecan region of the Mexican Gulf Coast, suggesting significant long-distance trade ties with that area. Though other research has been done in the Rio Grande Delta area since that time, such as Tiffany Terneny’s Doctoral dissertation analyzing local burials, Wagner’s ceramic analysis was the last substantive work done with the Anderson Collection until now.
Nearly a year ago Lauren approached me about an opportunity to contribute to an upcoming edited volume on trade and cultural interaction in North America, and suggested using the Anderson Collection to look at potential interactions between the Rio Grande Delta area and the Huastecan region. We decided to collaborate on the paper, which has proven to be an unexpectedly rich undertaking. Our goal in writing the paper has been to understand the nature of the interaction between the cultures of the Rio Grande Delta and the Huasteca, including what types of items they may have been trading. We have also sought to provide an example of how cultures which may be considered marginal, such as those of the Rio Grande Delta, can be active participants in wider economies of trade and exchange. An added benefit of our research is also to raise the profile of this archaeological region both within Texas and farther afield, since it is often ignored in favor of other areas. We have submitted the first draft of our chapter to the editors, and publication is expected sometime in 2019. In addition to our book chapter, we will be presenting our research at the Annual Meeting of the Society for American Archaeology in Washington D.C. this April, and are looking forward to spreading the word about this fascinating region and getting feedback on our research.
While conducting the research for these projects it became clear to us that though the Anderson Collection is an invaluable resource for the study of the archaeology of the Rio Grande Delta, no comprehensive inventory has been completed since Anderson was in possession of the collection. Such an inventory, with up-to-date classifications, artifact counts, locations, and site information, is a necessary step towards TARL’s goal of making this collection accessible to future researchers. To that end I have been working with the collection since January, and have been fascinated particularly with the abundant use of shell both as ornament and also for tools. It is clear that the people of the Rio Grande Delta were adept at utilizing the abundant marine resources at their disposal to craft a variety of utilitarian and decorative items, and that this shell industry was likely a key element in their interaction with outside groups. It is our hope that through this work the Anderson Collection will become a productive and useful resource for future study of the Rio Grande Delta area, and that others will begin to take a more active interest in pursuing research in this intriguing area.
In order to encourage student researchers and help them with their work, Beta Analytic has opened up the first ever AMS date raffle! Current students and recent grads can enter the free raffle for a chance to win one of five AMS dates (worth $595 each) for free.
We at TARL think this is a great opportunity for students to get some free data, so we encourage anyone with a relevant research project to enter. And if you’re looking for a research project, we can help you find one!
The raffle is open to all students in Europe, Africa, Asia Pacific, North America and South America. Students will need to show proof of enrollment as a graduate or undergrad student for any semester in 2018. You’ll be able to enter through November 30, 2018 and winners will be announced in December.
Christopher J. Jurgens is an Affiliated Researcher with the Texas Archeological Research Lab. An excerpt of this article appeared in the December 2017 TARL Newsletter.
In 2014, Dr. Steve Black requested that I dust off my ‘research hat’ when I retired after a career in state government. As with my own academic beginnings, Steve was a product of the undergraduate Archaeological Studies program at UT-Austin in the 1970s. Dr. Black worked at the Texas Archeological Research Laboratory (TARL) after completing his Ph.D. at Harvard University before becoming a professor in the Anthropology Department at Texas State University.
My doctoral research focused on the Lower Pecos cultural region of the Texas borderlands and was completed in 2005. TARL’s prolific and well-preserved collections from Arenosa Shelter (site 41VV99) formed the basis for my research (Jurgens 2005, 2008). Bone preservation in the region’s dry rockshelters is typically very good, especially for sites with cultural materials in Holocene-age contexts. Remember Ezekiel’s Biblical message about dry bones? As an analogy to this prophet’s ancient words, bone fragments ‘come alive’ to help us understand the prehistoric cultures in this region and, increasingly, in other regions of Texas.
Black’s “come visit” invitation came nearly a decade after completing my Ph.D. at UT-Austin. Dr. Black invited me to join his Ancient Southwest Texas (ASWT) project research team at Texas State University, adding my research specialties of zooarchaeology and bone technology to the team. Since then, I’ve also worked with the Center for Archaeological Studies (CAS) at Texas State University. At CAS, I am conducting similar research for a data recovery project at the Spring Lake site in San Marcos and smaller, historic period sites in San Antonio.
Zooarchaeologists study animal (aka, faunal) remains from archaeological sites using a specifically anthropological standpoint instead of a biological or paleontological perspective (Reitz and Wing 2008). Zooarchaeological faunal studies are also used to investigate site formation, biological processes, and cultural processes that are reflected in the particular collection (or sites) being studied. The anthropological perspective addresses the complex interaction between humans, their environment, and the consequences of that relationship. Animal bone fragments are analyzed to identify the animals and eco-niches represented and any human modification from subsistence or bone technology activities. Analyses begin with sorting of bone fragments into groups, based on size of animal, skeletal element, signs of burning, or other obvious evidence of butchering, skinning, or technological modification (Figure 1).
As a zooarchaeologist, an important question that I must answer during research is how faunal remains enter archaeological contexts. Are the faunal remains there strictly as a result of natural processes? Are the faunal remains spatially associated with cultural materials? Context of faunal remains is the key to understand their role in any site. If the faunal remains are spatially associated with cultural materials, then the zooarchaeologist must ask additional questions. Have the faunal remains been modified by cultural behaviors processes (skinning, butchering, tool manufacture or use, bone breakage for marrow removal or bone grease production, etc.)? If so, then the cultural filter has played a role in how the faunal materials were placed in the site. The bone fragments shown in Figure 1 are from an extinct bison recovered during 2016 excavations at Eagle Cave (41VV167) by Texas State University (Castañeda, et al. 2016). They reveal a late Paleoindian cultural filter through remnant evidence of intensive butchering. The bison’s mandible had many cut marks resulting from muscles being cut to allow the tongue to be removed (Figure 2). Ethnographic analogy from historic period bison hunters in the North American Great Plains mirrors this prehistoric evidence—the tongue was a prized portion of meat. For thorough discussion of this topic and related literature, see Jurgens (2005, Chapter 3).
One reason zooarchaeological studies are important in archaeological projects is that they help us understand past environments. Some animals only thrive in certain ecological conditions, such as upland grasslands or streamside woodlands. Groups of animal bones from the same archaeological context allow archaeologists to infer about paleo-environmental conditions during the time period when those deposits were formed. For example, let’s consider the presence of both jackrabbits and swamp rabbits in the same strata in archaeological sites along the southern edge of the Edwards Plateau. These fragments point to prey being targeted in both dry and moist environmental niches by prehistoric hunters and gatherers.
Let’s go back to the saga of my post-retirement research. Following Steve Black’s invitation, I joined the ASWT project’s collaborative team. The ASWT project team is researching sites in Eagle Nest Canyon near Langtry in the western Lower Pecos cultural region. Incorporating the Eagle Nest Canyon data sets from the Eagle Cave, Skiles Shelter, and Kelley Cave collections allows them to be compared with that from Arenosa Shelter. Eagle Nest Canyon joins the Rio Grande about 15 miles west of Arenosa Shelter’s location on the Pecos River near its confluence with the Rio Grande. The Ancient Southwest Texas Project study allows me to link my Arenosa Shelter research to the ongoing Eagle Nest Canyon efforts. The linkage expands our understanding of life-ways in the western Lower Pecos cultural region and elsewhere in Texas.
Analytical comparisons between Arenosa Shelter and the Eagle Nest Canyon sites have been focusing on Late Archaic and Late Prehistoric bone technology and subsistence economies. Most Eagle Nest Canyon sites lack the deeply stratified deposits present in Arenosa Shelter. In my view, this distinction is moot. As shown by my earlier Arenosa Shelter study, sixty per cent of faunal materials and bone artifacts were found in upper deposits (strata 4 – 9) with a Terminal Late Archaic context dating between about 2,300 and 1,300 years ago. Late Archaic and Late Prehistoric faunal materials had good to excellent bone preservation, as did those in Paleoindian deposits. Arenosa Shelter’s Middle and Early Archaic deposits (strata 12 – 36) were heavily damaged by high energy Pecos River flooding. Most of the bone fragments that these deposits may have originally contained were removed, especially those from smaller animals. Remaining bone in these strata also quite often has been redeposited in secondary context.
Faunal analysis utilizes techniques I’ve applied over the past 20 years. Using standard zooarchaeological procedures, skeletal materials from reference specimens of fish, birds, and mammals were used to identify the archaeological faunal material, assigning it to the most appropriate taxonomic group. Some of the reference specimens were loaned from the UT-Austin Jackson School of Geoscience’s Vertebrate Paleontology Laboratory. Assignment of bone fragments to the most appropriate taxonomic group requires an understanding of bone structure and skeletal anatomy of all potential animal groups, from fish and reptiles to birds and mammals. Some of the bones are easy to identify, based on their structure and morphology. Distinctive features allow identification of bone fragments to specific animal form and portion of skeletal element. For example, the archaeological and reference specimen bones in Figure 3 are both identifiable as feet bones from species in the rabbit family.
Microscopic examination of bone fragments is used to verify taxonomic and skeletal element assignment, especially for smaller animals. It is also used to search for cultural modifications that may be present on fragments.
Microscopic examination uses a 10x-25x binocular microscope (Figure 4). Specialized lighting includes an overhead general light and a low sidelight low that increases contrast (Figure 5). The sidelight reveals changes to the bone surface. Butchering damage and technological modifications made during tool or ornament manufacture and use each leave distinctive traces on the surface of bone. The human modification may be the form of cut and chop marks, scrape marks, grinding, surface polish, and microscopic striations from use-wear. Carnivore damage and root-etching also modify the bone surface.
The fauna from Eagle Nest Canyon sites parallel those from Arenosa Shelter. They appear to contain very similar faunal remains, including those of small to large mammals, fish, birds, turtles, and other reptiles. Bone preservation is variable in both locales, dependent on site formation processes and post-deposition effects of moisture on bone within the strata. The moisture present is from groundwater exiting from bedrock seeps or is from rainwater funneled from the canyon rims above the sites.
Many bone fragments showed signs of butchering or cooking by the site’s inhabitants. Skinning and butchering leave distinctive cutmarks, as does dynamic bone breakage to remove marrow. The bone flake from the Spring Lake site in Central Texas is a good example of a result from cultural activities to harvest bone marrow during butchering (Figure 6). Similar bone flakes are found in the Lower Pecos cultural region and elsewhere in Texas.
Some of the faunal remains and bone artifacts from the Eagle Nest Canyon sites have been burned, mirroring those in Arenosa Shelter. Two patterns of burning are evident—roasting and disposal. Direct heat cooking, such as grilling or roasting, leaves distinctive discoloration of bone fragments where bone was not covered by meat during cooking. The disposal pattern of burning is hypothesized to represent burning of food remains or incorporation of remnant bone into earth oven fill. Sometimes, discard pattern bone has been burned so intensely that most organic matter is removed from the bone. Bones incinerated by heat over 850o F caused this condition termed calcination. Similar patterns are being documented in analysis of the fauna from the Spring Lake site.
The Eagle Nest Canyon/Arenosa Shelter comparisons have allowed me a clearer understanding of the western Lower Pecos cultural region. The concurrent analysis of the Spring Lake faunal material is extending that knowledge to the eastern edge of the Edwards Plateau. My research has documented 1) eco-niches targeted by the prehistoric inhabitants, 2) specific subsistence behaviors (e.g. filleting of fish, specific cuts to overcome defensive pectoral fin spines in catfish, and specialized skinning of mammalian carnivores), and 3) manufacturing and use of tools or ornaments from boney subsistence remnants.
A wide variety of formal bone tool and ornament types have been recorded, as have the manufacturing processes for them. Evidence of manufacturing processes included scrape marks made to remove the periosteum layer from the bone surface; distinctive grooves cut to facilitate controlled snapping of the bone into segments; scraping and grinding to shape tool or bead preforms; and wear left by contact with plant materials, hides, or other substances during use.
Most formal tools were made from deer lower leg bones (Figures 7-9). Other skeletal elements of deer were also used to manufacture formal tools, such as the ulna or antler times (Figure 10). In addition, bones of smaller mammals formed the raw material for tool manufacture, as did the pectoral fin spines of catfish (Figure 11). Informal expediency tools are rare, but manufactured from large mammal long bones during butchering and retain use-wear from meat, sinew, or hide (Figures 12 and 13).
In my research, I have adopted a bone tool typology based on tool morphology, supplemented with use-wear analyses to document the actual function. Many bone tools from the Lower Pecos cultural region have been mistermed “awls” in the literature, implying function based on the tool form. The morphology of these tool’s cross-section is generally flat and ovoid. The main differences are in the tip (distal) section. Measurements of width and thickness at and near the tip are used to assign the tools into types. Use-wear analysis is then conducted to determine actual function. Use-wear studies revealed that those tools were used by prehistoric inhabitants to extract other resources from the environment or to manipulate them. Hides, desert succulent fibers, meat, wood—wear from all of these were revealed on tools or tool fragments through microscopic examination.
Beads were manufactured from bird or small-medium mammal long bones, with hawk and rabbits being the most common source animals (Figure 14). A Eureka! moment in my research came when I recognized that long bone ends from these animals retained evidence of being cut off during bead manufacture. Linking bead cross-section to morphology of the cut-off bone ends allowed identification of species that were the most common source animals (Figure 15).
During the on-going Spring Lake Site faunal analysis, I’ve noticed many parallels to the Lower Pecos study results, especially in the presence of bone technology remnants. The Spring Lake site shows that the same processes used to make the tools and ornaments in the Lower Pecos were in use in Central Texas by the Early Archaic.
One problem that I’ve come to face in the Spring Lake site study is that bone tool or ornament fragments, and evidence for their manufacture, have rarely been recognized or documented in Central Texas. Part of that scarcity is due to the differences in site types between the Lower Pecos and Central Texas. Fewer dry rockshelters are present in Central Texas. Bone preservation in the clay soils of Central Texas is another problem. Mechanical crushing is caused by movement in the region’s expansive clay soils. Overall bone fragment size of archaeological faunal remains in Central Texas is much smaller than in the Lower Pecos.
A separate problem is the lack of trained zooarchaeological specialists. This problem can be addressed by appropriate interdisciplinary education in university archaeological programs. I was fortunate during my undergraduate and graduate education to be trained by paleontologists and zooarchaeologists. These dedicated educators continue to mentor me even near the end of their careers or in retirement. Following their examples, I am mentoring the current generation of students. Training in zooarchaeological methods is no different than training in lithic or ceramic analytical methods. Unless students are taught the methods, how can they identify animals represented in archaeological sites, much less recognize the signals of bone technology amongst the subsistence debris?
Sites such as Arenosa Shelter, the Eagle Nest Canyon sites, and the Spring Lake site help us open doors onto the past. Once we throw those doors open, we can begin to understand how prevalent and widespread cultural processes, such as bone technology, were in prehistory across Texas.
Ezekiel’s right: we archaeologists must open our eyes and minds to the dry bones that help us understand the remnants of prehistoric cultures that surround us.
Castañeda, Amanda M., Christopher Jurgens, Charles W. Koenig, Stephen L. Black, J. Kevin Hanselka, and Haley Rush
2016 “Multidisciplinary Investigations of a Paleoindian Bison Butchery Event in Eagle Cave.” Paper presented at the 87th Texas Archeological Society Annual Meeting. Nacogdoches, Texas.
2008 “The Fish Fauna from Arenosa Shelter (41VV99), Lower Pecos Cultural Region, Texas.” In: Joaquín Arroyo-Cabrales and Eileen Johnson, Guest Editors, Contributions to Latin American Zooarchaeology in Honour of Oscar J. Polaco, Fryxell Award Recipient for Interdisciplinary Research. Quaternary International 185:26-33.
Reitz, Elizabeth J. and Elizabeth S. Wing
2008 Zooarchaeology (Second Edition). Cambridge Manuals in Archaeology. Cambridge University Press, Cambridge, U.K.
David Glen Robinson is an Affiliated Researcher with the Texas Archeological Research Lab. This article is part of the December 2017 issue of the TARL Newsletter.
An unusual painted potsherd was unearthed in the 1938-1939 WPA excavations of the Hatchel Mound in Bowie County, Northeast Texas (Perttula 2014). The sherd was part of a large lot of ceramics and only recently came to the notice of analysts. Painted ceramics of any type are rare in the Caddo region, and so detailed studies of the sherd were conducted to learn, if possible, about its origins, technology and functions. The zone in the mound from which the sherd came is estimated to date to the early 16th century A.D.
The small specimen measures 24 X 23 mm, making typological assessment very difficult. A wide literature search was conducted to find similar or matching stylistic types. The closest approach to a similar type was Nodena Red and White, widely but not abundantly distributed from parts of northeast Texas through Louisiana and parts of Mississippi. That type is tempered with shell, while the Hatchel Mound sherd has quartz temper, so some uncertainty remains with the typological assessment. Avenue Polychrome was also mentioned, but that type has even more tenuous connections to the Hatchel sherd.
The sherd has a layered look in megascopic view, its interior layer a gray tempered paste gradually transitioning to a red-brown paste color on the exterior surface. The difference in colors and the gradual transition from dark to light on the same kind of paste suggest skilled control of firing atmospheres to produce the differences. A white or pinkish white paint layer sits conformably on the reddish exterior paste. The paint is made of either finely ground shell or a slurry of refined clay with admixed crushed shell. Microphotographs of the paint layer in thin section reveal an arcuate bit of shell and circular, silt-sized masses within the paint layer. All these bodies have calcitic traits that indicate shell material (non-fossilized).
Altogether, this ceramic piece retains some mystery even after microscopic analysis. It certainly reveals, however, the fact that it was an exceptionally well-made pottery piece in the Caddo tradition, and when whole it was a prized and attractive ceramic vessel.
Dr. Timothy K. Perttula was the principal investigator of the Hatchel Mound studies that produced the unusual bichrome sherd from lot #1296. His facilitation of the project is greatly appreciated. Dr. George Sabo conducted some of the typological survey that homed in on Nodena Red and White. The microscopic work was conducted at Texas Archeological Research Laboratory, The University of Texas at Austin. The staff is thanked very much for their assistance.
Perttula, T. K.
2014 Archaeological Studies of the Hatchel Site (41BW3) on the Red River in Bowie County, Texas. Special Publication No. 23. Friends of
Northeast Texas Archaeology, Austin and Pittsburg.
Timothy K. Perttula is an Affiliated Researcher with the Texas Archeological Research Lab. This article is part of the December 2017 issue of the TARL Newsletter.
Woodland period artifact assemblages in inland Southeast Texas dating from as early as ca. 2100 B.P. have ceramic vessels, particularly sandy paste wares of the Goose Creek Plain series; Lower Mississippi Valley Tchefuncte and Marksville wares also occur in low frequencies in inland Southeast Texas Woodland period sites. These sites are part of the Mossy Grove culture (Story 1990:257) (Figure 1). By ca. A.D. 1000, Late Prehistoric ceramic wares were made with grog temper, and these grog-tempered ceramics have stylistic and cultural affiliations with ancestral Caddo groups in the Neches/Angelina and Sabine River basins as well as with coastal Texas groups. The grog-tempered ceramics are likely from vessels obtained from ancestral Caddo groups living in East Texas.
Sandy paste sherds from Goose Creek Plain, var. unspecified vessels are the principal Mossy Grove ceramics (between 80-95 percent) in the 20+ assemblages of ceramic vessel sherds and more than 15,000 sherds I examined for this study from sites in Montgomery (Lake Conroe), Polk (Lake Livingston), San Jacinto, and Walker counties. A small percentage of Goose Creek Plain, var. unspecified sherds have naturally occurring hematite nodules in the paste, and may come from vessels manufactured along the upper Texas Coast (Linda W. Ellis, June 2017 personal communication). The Goose Creek Plain, var. unspecified sherds in general are from compact and smoothed vessels made by coiling, probably jars or deep bowls. The smoothing served to better weld the coils together before firing. The paste is not contorted, thus suggesting that vessels were decently prepared for vessel shaping. The remainder of the ceramics in these collections are from tempered ancestral Caddo ceramics, especially plain or decorated sherds from grog-tempered and grog-tempered-sandy paste vessels (2.7-19.5 percent of the assemblages).
The largest ceramic vessel sherd assemblages are from the Burris 1 (41PK88) (n=6042), Jones Hill (41PK8) (n=2226), Strawberry Hill (41SJ160) (n=1834), 41MQ6 (n=1212), Houston (41SJ19) (n=1077), and Burris 2 (41PK89) (n=468) sites, and these assemblages have been employed for comparisons with each other in terms of paste and temper characteristics as well as decorative methods and elements. The sherd collections I examined are curated at Stephen F. Austin State University and the Texas Archeological Research Laboratory.
The sandy paste wares in these sites are rarely decorated: from a trace to no more than 2.6 percent of the assemblage, while as
much as 10.6 percent of the ancestral Caddo tempered vessel sherds in the assemblage at the Burris 1 site are decorated. The
most common decorated sandy paste wares are from Goose Creek Incised (Figure 2c), Goose Creek Red-Filmed, Goose Creek
Punctated, lip notched Goose Creek Plain, var. Burris, Goose Creek Incised-Punctated, and Goose Creek Brushed (likely dating to
after ca. A.D. 1200). Aten (1983:Figure 14.5) suggests that all of the decorated sandy paste vessel sherds in these Mossy Grove
sites postdate ca. A.D. 900-1000, and they correlate in time with the introduction and use of ancestral Caddo ceramic wares.
Aten (1983:295) also notes that Caddo ceramics in the Conroe-Livingston area have a “prominent frequency.”
Based on the identification of a number of defined ceramic types, the ancestral Caddo tempered wares from Mossy Grove sites in the Conroe-Livingston area can be sorted into types from three different chronological periods: pre-A.D. 1200, Late Caddo period (ca. A.D. 1400-1680), and Historic Caddo period (ca. A.D. 1680-1730). The suite of Early Caddo period types, including Davis Incised, Dunkin Incised, Holly Fine Engraved (Figure 3a), Kiam Incised, and Weches Fingernail-Impressed, var. Weches is most abundant at the Burris 1 site, but there are examples of Holly Fine Engraved and Kiam Incised from 41MQ6 and Strawberry Hill. The range of defined types are associated with Early Caddo period communities on the Neches River, likely the large Caddo mound center and village at the George C. Davis site (41CE19).
Ancestral Caddo period utility ware and fine ware vessel sherds from Late Caddo Ancestral Caddo period utility ware and fine ware vessel sherds from Late Caddo period (ca. A.D. 1400-1680) vessels are more abundant in these Mossy Grove culture sites; two sherds at two Mossy Grove sites (41MQ6 and Burris 1) with asphaltum designs or surface coating are from Rockport wares, and likely date to the same post-A.D. 1400 interval. Given the common occurrence of sherds from tempered Caddo brushed vessels, the post-A.D. 1400 use of these Mossy Grove sites was considerable, given that the manufacture and use of brushed vessels is a feature of post-A.D. 1400 Caddo ceramic traditions in much of East Texas. In general, the identified ancestral Caddo ceramic types, including Bullard Brushed (see Figures 2a-b), Maydelle Incised, Pease Brushed-Incised, and Poynor Engraved (see Figure 3e-e’), point to interrelationships between Mossy Grove peoples and Frankston phase Caddo communities in the upper and middle Neches River basin in East Texas marked by the trade or exchange of ceramic vessels from Caddo groups. The presence of Ripley Engraved sherds (see Figure 3f-g) from the Burris 1 site also suggests contacts between Mossy Grove peoples and Caddo groups affiliated with the Titus phase; these Caddo groups lived in the Big Cypress and mid-Sabine River basins.
The Historic Caddo ceramic types in the Mossy Grove sites are confined to the Burris 1 and Houston sites. The utility wares include Foster Trailed-Incised, var. Moore and Spradley Brushed-Incised types, and their occurrence suggest wide-ranging contacts between Mossy Grove groups and ancestral Hasinai Caddo and Kadohadacho communities in the Neches-Angelina (e.g., Spradley Brushed-Incised) and the Red River (e.g., Foster Trailed-Incised) basins, respectively. The same can be said for the fine wares, as Patton Engraved (which is present at the Burris 1 site) occurs in Hasinai Caddo communities on the Neches-Angelina, and Keno Trailed vessels (see Figure 3h) are most common in the Red River basin among Kadohadacho communities.
The adoption and use of sandy paste Goose Creek Plain pottery by Woodland period hunter-gatherer foragers in eastern and southeastern Texas was apparently a better way to cook foods than the hot rock cooking/stone boiling in hide-lined pits or basketry of earlier times because stews/broths could instead be cooked and simmered in ceramic vessels. Traditional and new food stuffs could be prepared in ways that were more effective, leaving the food in the pot rather than to be subject to loss over open flames. The introduction of this new cooking technology after ca. 2500 years ago in Southeast and East Texas was not apparently associated with the use of any agricultural domesticate or the simmering of starchy foods. Only after ca. A.D. 800, in East Texas, were domesticated plant foods beginning to be prepared with a cooking technology where foods were cooked in ceramic vessels that were set directly over or in fire.
Aten, L. E. 1983 Indians of the Upper Texas Coast. Academic Press, New York.
Story, D. A. 1990 Cultural History of the Native Americans. In The Archeology and Bioarcheology of the Gulf Coastal Plain, by D. A. Story, J. A. Guy, B. A. Burnett, M. D. Freeman, J. C. Rose, D. G. Steele, B. W. Olive, and K. J. Reinhard, pp. 163-366. 2 Vols. Research Series No. 38. Arkansas Archeological Survey Research Series, Fayetteville.
Dan Prikryl is an Affiliated Researcher with the Texas Archeological Research Lab. This article is part of the December 2017 issue of the TARL Newsletter.
In the December 2016 issue of the TARL newsletter, I provided general background information on Works Progress Administration (WPA)-era excavations at the Rob Roy Site, 41TV41, which is located on Lake Austin in western Travis County, Texas. My work on these materials has continued with my most recent analysis focusing on the 21 deeply buried burned rock features that are present within a previously unrecognized Late Archaic I Period component as defined by Johnson (1995:73, 89-98).
One of the most interesting aspects of the analysis of these features concerns an obvious cluster of seven individual burned rock features that together form a large irregular circle. The University of Texas archaeologists who led the field project recognized this cluster, but they provided no interpretation (Woolsey and Oberg 1939:53). This cluster consists of Feature #26, a 1.7-meter (m) diameter, well-defined, basin-shaped circular hearth/earth oven, and six surrounding satellite burned rock features. A circular, 60 to 120 cm wide area that is mostly void of burned rocks exists between the outer edges of Feature #26 and the inner edges of the six satellite features (Figure #1). None of the six satellites are basin-shaped. Instead, they consist of one flat, dense continuous burned rock pavement (Feature 29), four flat, amorphous burned rock groupings (Features #24, 25, 28 and 30), and one somewhat circular burned rock heap (Feature #27). Several of the satellites cover quite large areas including Feature #28 which measures 3.00 x 1.11 m and Feature #29 which covers an area measuring at least 2.76 x 1.62 m.
Overall, the irregular circle formed by the seven features extends 5.97 m on an east-west line. The total length on a north-south line is unknown because two of the satellites (Features #27 and 29) continue into an unexcavated area. The exposed part on a north-south line covers a length of 3.05 m.
With the exceptions of Feature #25 and 30, charcoal and ash were reported as present in all features that comprise the
cluster. Bison bones were present among the burned rocks in Features #26, 29 and 30 with the most noteworthy faunal
specimen being a bison skull found in the top center of Feature #26. The only diagnostic artifact near feature grouping is a
Marshall point that was found between Features #28 and 30 at an elevation about 15 cm above these features.
The irregular circle is like some other feature patterns reported at sites in Central and West Texas that have either been as interpreted as aboriginal structures (Lintz et al. 1995; Johnson 1997) or as incipient burned rock middens (Luke 1983; Hixson 2014). All together, these feature patterns include examples that have been dated to the Early Archaic, Middle Archaic, Late Prehistoric Austin Phase, and Historic Indian periods.
Aside from one hollow area in one of the satellite features, there are no other apparent rock-free spaces within any of the other satellite features that would have been left by wooden posts to support the walls of a structure. Given the overall nature, sizes and shapes of satellite features, especially Features #27-29, the cluster of features more closely resembles an incipient burned rock midden. Hixson (2014) has provided a thorough discussion of the incipient burned rock midden model in which he proposes that these circular features consist of a central earth oven surrounded by satellite clusters of burned rocks that represent earth oven clean-out material resulting from repeated use of the central feature. Hixson (ibid) states that the generally 60 to 120 cm wide circular, vacant space that exists between the central feature and the satellite rock clusters could either be the workspace for the aboriginal people using the central cooking feature or could represent the eroded remains of a former circular berm of stockpiled dirt used in association with earth oven cooking.
Since the Rob Roy Site is situated on an alluvial terrace, it is probable that the incipient burned rock midden was buried during a flood event before continued use would have led to the development of a denser, mounded burned rock midden.
Hixson, C. A. 2014 A New Hypothesis to Explain the Large Burned Rock Features with Satellite Clusters. In A Cultural Resource Reconnaissance Survey of Select Portions of the Lake Buchanan Shoreline Exposed by Recent Droughts, Burnet and Llano Counties, Texas by C. A. Hixson, D. J. Prikryl, and A. F. Malof. Lower Colorado River Authority, Austin.
Johnson, L. 1995 Past Cultures and Climates at Jonas Terrace, 41ME29, Medina County, Texas. Office of The State Archeologist Report 40. Texas Department of Transportation and Texas Historical Commission, Austin.
1997 The Lions Creek Site (41BT105): Aboriginal Houses and Other Remains at a Prehistoric Rancheria in the Texas Hill Country (Burnet County). Archeology Studies Program, Report 1, Environmental Affairs Division, Texas Department of Transportation; Report 41, Office of the State Archeologist. Texas Historical Commission, Austin.
Lintz, C., A. Treece, and F. Oglesby1995 The Early Archaic Structure at the Turkey Bend Ranch Site (41CC112), Concho County, Texas. In Advances in Texas Archeology, Contributions from Cultural Resource Management, edited by J. E. Bruseth and T. K. Perttula. Cultural Resource Management Report 5. Texas Historical Commission, Austin.
Luke, C. J. 1983 The Musk Hog Canyon Project, Crockett County, Texas. Publications in Archaeology, Report No. 24. State Department of Highways and Public Transportation, Austin.
Woolsey, A. M. and K. Oberg 1939 Field Notes, Site 1, Miller Lake, Burnt Hollow, Roy Ranch. WPA Archeological Project Sponsored by the Anthropology Department, The University of Texas, Austin.
Kevin Hanselka is a regional archeologist with TxDOT. This article is part of the September 2017 TARL newsletter.
Firecracker Pueblo is a well-known archeological site and State
Archeological Landmark located within the proposed right of way for the Northeast Parkway, a new-location highway northeast of El Paso planned to ease heavy traffic along Interstate 10. Excavations here in the 1980s found that early in the 15th century, desert farmers established a small village or hamlet on the Firecracker site, probably with their corn and bean fields planted somewhere nearby. Early on these farmers built at least 17 “pit houses” (roughly circular or oval houses built over shallow pits) on the site, but later constructed an above-ground adobe-walled structure with about 16 rooms on top of the former pit houses.
In 2016 archeologists working on behalf of TxDOT surveyed the right of way in preparation for the Northeast Parkway project. Although the adobe walls and pit house foundations are not visible on the surface, the survey crew found a dense concentration of chipped stone artifacts and fragments of decorated ceramic pots near the location of the previous excavations. In addition to Firecracker, the crew also explored three other similar sites along the project corridor with dense surface scatters of prehistoric artifacts. These artifact concentrations suggest that unknown pit houses or adobe-walled rooms may yet await discovery under the surrounding sand dunes. Therefore additional investigations must happen on Firecracker and these nearby sites before construction on Northeast Parkway can start.
Testing and excavations on the four sites are planned for the upcoming year or two. These new TxDOT investigations will complement previous findings from Firecracker Pueblo (much of which remains unpublished) and enhance our knowledge about the lives of El Paso phase (ca. AD 1300 – 1450) Jornada Mogollon farmers. As this ongoing project develops, TxDOT continues to work closely with the Tigua Tribe of Ysleta del Sur Pueblo in El Paso as we weigh potential impacts to these and other cultural resources along the Northeast Parkway.
Timothy K. Perttula is a visiting researcher at TARL. This article was part of the September 2017 TARL newsletter.
In the summer of 2017, 21 ancestral Caddo ceramic vessels held since 1933 by the Gila Pueblo Museum and then by the Arizona State Museum were returned to the Texas Archeological Research Laboratory at The University of Texas at Austin (TARL). These vessels had not been properly or fully studied and documented when the University of Texas exchanged these vessels, so the purpose in documenting these vessels now is primarily to determine the stylistic (i.e., decorative methods, motifs, and decorative elements) and technological (i.e., vessel form, temper, and vessel size) character of the vessels that are in the collection, and assessing their cultural relationships and stylistic associations, along with their likely age. In 1933, little was known about the cultural and temporal associations of ancestral Caddo ceramic vessels from East Texas, but that has changed considerably since that time (e.g., Perttula 2013).
Ceramic Vessel Exchange
Harold Gladwin of the Gila Pueblo Museum (GPM) in Globe, Arizona, first proposed to The University of Texas (UT) an exchange of ceramic materials in November 1931 with Dr. J. E. Pearce of UT. Pearce was not prepared to exchange any ceramic vessels or sherd collections then because the ceramic materials in his possession had not been studied because they had only recently been recovered from excavations at East Texas Caddo sites.
However, by November 1933, Pearce felt an exchange of Southwestern vessels with ancestral Caddo vessels between the GPM and UT was worth doing, and 20 Caddo vessels from eight East Texas sites were selected by E. B. Sayles of the GPM. After Pearce obtained permission from UT President H. Y. Benedict and the Board of Regents, the vessels were shipped to the GPM. The eight ancestral Caddo sites that had vessels selected for the exchange included the Richard Patton Farm (41AN26, 2 vessels); Goode Hunt Farm (41CS23, 2 vessels); Mrs. H. L. Culpepper Farm (41HP1, 1 vessel); H. R. Taylor (41HS3, 7 vessels); T. M. Sanders Farm (41LR2, 2 vessels); Hooper Glover Farm (41MX4, 1 vessel); Russell Bros. Farm (41TT7, 1 vessel); and the J. M. Riley Farm (41UR2, 4 vessels). The vessels remained in Arizona museums until the summer of 2017.
The exchanged vessels from the T. M. Sanders site are from burial features in a Middle Caddo period (ca. A.D. 1200-1400) Sanders phase mound on the Red River. They include a Maxey Noded Redware bottle (Figure 1) and an East Incised bowl.
The fine ware and utility ware vessels from the Culpepper Farm, H. R. Taylor, Hooper Glover, Russell Brothers, and J. M. Riley sites are from Late Caddo period Titus phase sites (dating broadly from ca. A.D. 1430-1680) in the Big Cypress and Sulphur River basins in East Texas. The fine ware vessels include Ripley Engraved (Figure 2) and Taylor Engraved carinated bowls, a Wilder Engraved, var. Wilder
bottle, a Bailey Engraved olla, a red-slipped bowl, and Ripley Engraved compound bowls, while the utility wares are Bullard Brushed, Harleton Appliqued (Figure 3), and Karnack Brushed-Incised jars.
Finally, the ceramic vessels from the Richard Patton and Goode Hunt sites are from late 17th to early 18th century Historic Caddo burial features in the upper Neches River and Big Cypress Creek drainage basins, respectively. These burial features were in cemeteries created and used by Hasinai and Nasoni Caddo peoples. The historic Caddo ceramics from the Richard Patton site include two different varieties of Patton Engraved (Figure 4), while both vessels from the Goode Hunt site are Simms Engraved carinated bowls (Figure 5).
Thanks to Lauren Bussiere and Marybeth Tomka at TARL for facilitating access to the study of these vessels, and for providing photographs of the vessels taken by the Arizona State Museum. Kevin Stingley kindly assisted with the vessel documentation. All photos courtesy Arizona State Museum.
Perttula, T. K.
2013 Caddo Ceramics in East Texas. Bulletin of the Texas Archeological Society 84:181-212.