INITIAL NOTES ON THE X-RAY FLUORESCENCE CHARACTERIZATION OF THE RHYODACITE SOURCES OF THE TAOS PLATEAU,NEW MEXICO

A preliminary statement of the energy dispersive X-ray fluorescence characterization of six spatially discrete rhyodacite sources of the Taos Plateau, New Mexico is presented. Geochemical characterization serves to determine the sources of an initial sample of 30 rhyodacite artifacts from three archaeological sites some 20–40 km distant from the sources. The initial results indicate that barium, strontium and zirconium are particularly effective in identifying and discriminating among the various northern Rio Grande-Taos Plateau rhyodacite sources.     

Archaeological Publications

Abstract

A number of lithic studies over the past several years have indicated that average flake weight (size) appears to be a direct reflection of the ease of lithic procurement, with the greater the distance to the lithic source, the smaller the respective general flake size. Similar high-quality lithic materials from Pot Creek Pueblo and the Cerrita pithouse site of the Taos area of the northern Rio Grande Valley in New Mexico provide an excellent basis for the study of the effects of source distance on the metrical attributes of lithic material due to the wide array of local and nonlocal lithic resources available at varying distances from the two settlements and utilized within them. The analysis indicates that flake thickness and volume (flake length × width × thickness) provide statistically significant linear trends and patterns in relation to respective source material distance. The general flake dimensional-decremental trend with increasing source distance probably reflects smaller lithic parent material sizes with increasing material source distance as well as a lithic technology oriented toward greater material conservation and less technological variability as the distance to the respective lithic material source increases.     

Local recipes or distant commodities? Lead isotope and chemical compositional analysis of glaze paints from the Salinas pueblos,New Mexico

For nearly four hundred years, Pueblo potters in the Rio Grande Valley of New Mexico produced technologically innovative glaze-decorated bowls and exchanged them widely among different villages. While potential sources of lead ores used to make glaze paints are found throughout the Rio Grande Valley region, researchers have only recently begun to identify which ore sources potters exploited and to understand the social and economic factors underlying patterns of ore resource use. In this paper we use stable lead isotope and electron microprobe analysis of glaze paints on Rio Grande Glaze Ware made at two Salinas pueblos to identify ore sources and glaze recipes used by their potters. Despite some isotopic overlap of ore sources, the lead isotope data point to regular exploitation of ores from the Socorro area of the southern Rio Grande. Salinas potters apparently used other sources as well, and likely mixed ores from different sources. We also identify four local glaze recipes that appear to incorporate multiple ore sources, suggesting that Salinas potters obtained raw ores rather than finished glaze paints.     

Stable Lead Isotope Analysis of Rio Grande Glaze Paints and Ores Using ICP-MS: A Comparison of Acid Dissolution and Laser Ablation Techniques

High resolution inductively-coupled plasma mass spectrometry (ICP-MS) analyses of stable lead isotopes in Rio Grande glaze paints and New Mexico lead ores (galena) are compared using both acid dissolution and laser ablation techniques. These comparisons demonstrate that acid dissolution is preferable when more accurate measurements are required. In particular, acid dissolution with aqueous induction provided a better match between the archaeological glaze paints and their potential ore sources. However, these comparative studies also show that laser ablation may be an acceptable alternative for examining archaeological materials when the emphasis is on rapid, relatively non-destructive analyses of large data sets.     

Tewa Place Names for Early Habitation Sites in the Northern Rio Grande Valley,New Mexico

Place names have the potential to aid in the investigation of regional settlement histories because they reflect the importance of specific locations in the social or cultural memories of indigenous groups. Unique place names for ancient habitation sites such as villages or hamlets, i.e., those names for which there are no cognates in other languages, suggest that those ancient villages or hamlets still retain the names given to them by their original inhabitants. Here, we present Tewa place names for habitation sites identified archaeologically in the northern Rio Grande Valley of New Mexico. The results of our study strongly suggest that the Tewa language was spoken in the northern Rio Grande Valley, specifically, within the southern Tewa Basin, as early as the Late Developmental period (a.d. 900–1200), thus challenging the currently well-accepted model postulating a Mesa Verde origin for the Tewa language and culture.     

Book Reviews

Abstract

Obsidian studies play an integral part in archaeology around the world, particularly in the Americas, but few archaeologists have employed obsidian studies to understand Native American life at historical archaeological sites. Yet, obsidian sourcing and hydration analysis can provide critical insights into site chronology and use, lithic recycling, and procurement and trade at contact and colonial sites. Obsidian geochemical sourcing and hydration analyses of a 19th-century rancho site in northern California have revealed new information on Native Americans who labored there in the second quarter of the 19th century. The obsidian data indicate a significant amount of lithic manufacture and use, a change in obsidian procurement in the 1800s, and an unprecedented number of obsidian sources represented on-site. The implications for general obsidian studies, as well as for regional archaeological issues, concern the problems with popular sourcing methods in northern California and the need to revisit current understandings of the first micron of hydration rim development.     

Everything Old Is New Again: Recent Approaches to Research on the Archaic Period in the Western United States

There are regional differences in how archaeologists conduct their research on the Archaic period. The rich array of techniques and approaches used to examine this period in the West include human behavioral ecology and other evolutionary perspectives, technological style and aspects of practice theory, neuropsychological theory, and more. Recent research in the Great Basin, Southwest, Great Plains, Columbia-Fraser Plateau, and coastal California is surveyed to highlight commonalities and differences in the questions asked of the archaeological data and in the techniques that are used.     

The Emergence of Kwahe’e Black-on-white pottery in the Tewa Basin,New Mexico

Despite the importance of ceramic typologies for defining archaeological cultures and making chronological inferences, the ceramic types comprising these typologies are not always well dated. Here, we present an analysis of radiocarbon dates generated from Accelerator Mass Spectrometry of corn remains found in association with Kwahe’e Black-on-white (Kwahe’e B/w) ceramics from the Tewa Basin of the Northern Rio Grande region of New Mexico in the American Southwest. This autochthonous ceramic type is the first in a cohesive lineage of decorated white wares known as the Rio Grande ceramic series. A Bayesian analysis of these dates yielded a 95% probability range of a.d. 975–1023 for the beginning temporal boundary marking the emergence of Kwahe’e B/w. This estimate for the chronological emergence of Kwahe’e B/w is at least 27 years earlier than previously demonstrated and appears to coincide with the initial population increase in the Tewa Basin during the Late Developmental period (a.d. 900–1200), and with the emergence of the Tewa language that is still spoken in the region.     

Determining the Provenance of native copper artifacts from Northeastern North America: evidence from instrumental neutron activation analysis

The emergence of archaeological interest in native copper in the mid-1800s developed in concert with explanations that privileged the Lake Superior area over other potential sources of copper. Most scholars have thus assumed that when copper artifacts first appeared in Northeastern North America, they arrived as finished implements or were locally made from Lake Superior raw materials. Procurement models that point to Lake Superior as the sole source of native copper have been widely accepted in the absence of systematic large-scale testing. This article evaluates the dominant model for native copper procurement and presents trace element data derived from instrumental neutron activation analysis (INAA) to determine whether hunter-gatherers in the Northeast utilized one dominant source of copper or in fact exploited a number of geological deposits. I specifically report on the chemical characterization of copper from 13 discrete geological deposits and 18 archaeological sites dating to the Late Archaic (ca. 5000–3000 B.P.) and Early Woodland (ca. 3000–2000 B.P.) periods to suggest that the dominant model for native copper procurement is oversimplified.     

Archaeological geology of two flow-banded spherulitic rhyolites in New England,USA: their history,exploitation and criteria for recognition

Artifacts of spherulitic rhyolite derived from two locations in northern New Hampshire are significant to minor components of numerous Paleoindian, Archaic and Woodland archaeological sites in Maine, New Hampshire, Massachusetts, Vermont and easternmost Quebec. The two known sources of are a dike near the city of Berlin, New Hampshire, and blocks-in-till near the village of Jefferson, New Hampshire. The source near Berlin has been a known source for “Indian relics” since the middle of the nineteenth century. The second source near Jefferson New Hampshire was first recognized in 1997. Both sources are situated along prominent east–west routes between the east flowing Androscoggin River on the east and the south flowing Connecticut River on the west. Mount Jasper is located above the Dead River. The Dead River flows east and enters the Androscoggin River approximately 3 km from Mount Jasper. Passage between the Connecticut and Androscoggin Rivers would have taken the travelers directly beneath Mount Jasper. To the west, from the upper reaches of the Dead River, the portage to Head Pond is approximately 0.9 to 1.5 km. From Head Pond access to the Connecticut is by way of the North Branch Upper Ammonoosuc River. The Jefferson source is located on terraces on the northwest side of the modern Israel River. The Israel River flows west and north for approximately 25 km into the Connecticut River. To the east the Israel River rises to a divide which separates it from the east flowing Moose River, which empties into the Androscoggin. Attribution to source is based upon comparison with known outcrops which include the combined characteristics of gross lithology, weathering characteristics, and bulk mineralogy. Comparison of dike samples with artifacts also indicate that the thickness and continuity of the flow bands together with spherule characteristics, which include, size, shape, volume, microscopic structures and weathering character, further suggest a limited source.     

A pilot study of “black chert” sourcing and implications for assessing hunter-gatherer mobility strategies in Northern England

Mesolithic hunter-gatherer logistic strategies and raw material procurement locales have been topics of considerable interest in northern England, accelerated by the early discoveries at Star Carr. Here we present the results of a pilot study investigating the potential for geochemically sourcing “black chert”, a material with similar qualities to flint but of inland limestone origin, using ICP-AES, ICP-MS and LA-ICP-MS. Several geological sources of black chert are known, and it is commonly present at upland Mesolithic sites along the Pennine chain. Four geological sources were sampled and analysed, along with a small sample of black chert artefacts from two upland Pennine archaeological sites. The results demonstrate that the four sampled sources can be easily differentiated from one another chemically. This research reveals the potential to apply this approach at a larger scale; the archaeological sample together with the source results indicate that additional sources will need to be identified and sampled before such data can be applied to address current questions of the Mesolithic of northern England.     

Seismic Refraction at Ancestral Puebloan Sites on the Pajarito Plateau,New Mexico

Abstract

Geophysical techniques can be used for non-invasive surveys at archaeological sites. One under-utilized technique, seismic refraction, has many potential applications. It is an inexpensive, efficient way to characterize subsurface deposits, especially at sites with shallow accumulations over bedrock. Archaeologists and geophysicists participating in the Summer of Applied Geophysics Experience from Los Alamos National Laboratory and Bandelier National Monument on the Pajarito Plateau in northern New Mexico characterized Ancestral Puebloan sites (A.D. 1200–1450) using this technique. We provide an overview of how seismic refraction works and demonstrate the applicability of seismic refraction for identifying buried archaeological features such as communal structures and walls.     

The Organization of Late Paleoindian Lithic Procurement Strategies in Western Wisconsin

Abstract

The applicability of employing an organization of technology framework to the analysis of prehistoric lithic procurement strategies is demonstrated here. Analysis reveals that a spatial separation is present in the distribution of lithic raw materials used by Late Paleoindian populations in western Wisconsin. This raises the possibility that lithic raw material functioned as a stylistic indicator of group membership. To evaluate this suggestion microstylistic traits present on a large sample of diagnostic Late Paleoindian projectile points were examined. Significant differences in stylistic traits were observed between sample areas. Furthermore, these differences correspond to spatial differences in raw material use. The correlation between lithic raw material use and microstylistic traits is consistent with the idea that lithic raw material serves as a stylistic marker of group membership, and indicates the presence of some form of social boundary within western Wisconsin during the Late Paleo indian Period.     

The Geoarchaeological Context of Grand Island

Abstract

Interpretations of the geoarchaeological context of Grand Island, Michigan have been a critical part of prehistoric archaeological investigations. Geoarchaeological investigations have generally focused on determining the age of various geomorphic surfaces, interpreting site settings, and paleoenvironmental reconstructions. Although no Paleoindian materials have yet been found, the island was available for human occupation following final deglaciation sometime after 13,000 cal b.p. High lake levels during the Nipissing Phase (ca. 5700–4450 cal B.P.) built a series of coastal landforms that where heavily used by Archaic Period people. Post-Nipissing fluctuations in lake levels presented a highly variable coastal setting for Terminal Archaic and Woodland Period people     

Possible sources of archaeological maize found in Chaco Canyon and Aztec Ruin,New Mexico

Maize played a major role in Chaco's interaction with outlying communities in the southern Colorado Plateau. This paper seeks to determine where archaeological corn cobs brought to Chaco Canyon were grown. Strontium-isotope and trace-metal ratios of 180 soil-water and 18 surface-water sites in the Southern Colorado Plateau have revealed possible source areas for some of 37 archaeological corn cobs from Chaco Canyon and 10 archaeological corn cobs from Aztec Ruin, New Mexico. The most probable source areas for cobs that predate the middle-12th-century drought include several Upper Rio Chaco sites (not including Chaco Canyon). There are many potential source areas for cobs that date to the late A.D. 1100s and early 1200s, all of which lie in the eastern part of the study area. Some Athapascan-age cobs have potential source areas in the Totah, Lobo Mesa, and Dinetah regions. One Gallo Cliff Dwelling cob has a strontium-isotope ratio that exceeds all measured soil-water values. Field sites for this cob may exist in association with Paleozoic and Precambrian rocks found 80–90 km from Chaco Canyon. Potential source areas for most Aztec Ruin cobs (many of which were found in rooms dating to the first half of the 13th-century) appear to be associated with a loess deposit that blankets the Mesa Verde and McElmo Dome regions.     

A Very Remote Storage Box Indeed: The Importance of Doing Archaeology with Old Museum Collections

Although our practice has come to be defined by a focus on excavation as the trademark of archaeological research, research on archaeological collections lies at the scientific heart of the discipline. We demonstrate through two very different case studies how a return to primary sources (in this case, boxes of artifacts) can upend our understanding of the objects themselves and create new narratives of social and technological change. At the same time, access to museum collections is becoming increasingly difficult as institutions struggle with the growing pressure to enhance public outreach and modernize data management, while simultaneously contending with persistent budget cuts. As archaeologists who work closely with museum curators and museum collections, we offer suggestions for how researchers can work with museums to ensure that future generations of researchers and the general public can learn from the ancient materials preserved within their collections.     

Patterning in procurement of obsidian in Chaco Canyon and in Chaco-era communities in New Mexico as revealed by X-ray fluorescence

X-ray fluorescence analysis of obsidian artifacts from sites located in Chaco Canyon and from three Chaco-era communities in New Mexico permits determination of their geological origin. These source data are used to describe patterning in obsidian procurement in sites located in Chaco Canyon dating from A.D. 500–1150, and in a three non-Canyon communities occupied during the period of Chaco Canyon's regional prominence (ca. A.D. 875–1150). These data demonstrate that the most proximate sources generally dominate the sourced obsidian assemblages from sites of all periods, but also suggest differences in procurement patterning both over time and across space. Within Chaco Canyon, there is a notable shift from Mount Taylor obsidian to use of Jemez Mountains sources over time. These data also suggest that earlier analyses of obsidian from sites in Chaco Canyon misidentified some obsidian artifact sources; these new data indicate the central areas of disagreement and provide a revision of procurement patterning. In the Chaco-era communities located outside Chaco Canyon, procurement patterning diverges. The Blue J community shows an increase in use of the nearby Mount Taylor source over time. Two communities located toward the southern extent of the Chaco great house distribution reveal a markedly distinct procurement pattern, obtaining nearly all of their obsidian from southern sources largely unrepresented at Chaco Canyon. Combined, these data provide new insights into raw material procurement and artifact production at sites in Chaco Canyon, and in communities occupied during the Chaco Phenomenon, the period of the Canyon's greatest regional influence.     

Stratigraphy and geochronology of La Playa archaeological site,Sonora, Mexico

La Playa archaeological site in northern Sonora, Mexico contains a long record of human activity that includes the Paleoindian period (terminal Pleistocene) and much of the Holocene. The size and complexity of La Playa has discouraged a systematic characterization of its stratigraphy and geochronology, a deficiency we redress in the study. We distinguished seven stratigraphic units ranging in age from >44,570 to 400 cal yr B.P. using ¹⁴C dates from charcoal and terrestrial gastropods found mostly in archaeological features. All of the buried (in situ) cultural remains are contained in Units B (4690–1580 cal yr B.P.) and C (1010–400 cal yr B.P.) and represent overbank deposition from the nearby Rio Boquillas. Occupation at the site peaks in Units B₄ and B₅, corresponding to the Cienega phase (2800–1800 cal yr B.P.) of the Early Agricultural period. This period coincides with the growth of early agricultural villages in the region and is marked at La Playa by thousands of archaeological features including roasting pits, human burials, and extensive canal irrigation systems. The presence of semi-aquatic and aquatic snails demonstrates that water was present year round in the canal systems constructed during this period. Stable and radiometric isotopic evidence suggests that early agriculturalists diverted ground water over several kilometers from the nearby Rio Boquillas. The extensive Cienega phase occupation ended after about 1700 cal yr B.P. with deep erosion of the site, an event also visible in alluvial records in southern Arizona that marked the end of the Early Agricultural period and significant changes in settlement organization in the region.     

War and Place: Landscapes of Conflict and Destruction in Prehistory

Abstract

The concept of place has rarely been applied to the archaeological study of warfare. Given that cultural landscapes embody meaning, however, the idea that places can be the focus of competition makes it evident that they can also shape associated conflict. As archaeologists move toward a more nuanced study of conflict in the past, such considerations will take on increasing importance, although as of yet most such studies are heavily reliant on textual sources and overtly symbolic material culture. This paper presents a case study from Burnt Corn Pueblo, in the Galisteo Basin, New Mexico, USA, and argues that evidence for conflict there at the beginning of the 13th century CE can be usefully interpreted through Ancestral Pueblo concepts of place.