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The scientific importance of Wanuskewin Heritage Park lies in the number and diversity of archaeological sites present in a single area. Wolf Willow and Dog Child are multicomponent occupation sites located in the Opimihaw Valley and both contain McKean components. McKean Complex sites are relatively uncommon on the Northern Plains which makes the cluster at Wanuskewin Heritage Park important. McKean lithic materials are mainly locally produced with very few exotics. Materials from McKean assemblages have a heavy reliance on local lithic materials such as chert and quartzite. McKean levels at the Thundercloud, Cut Arm, and Red Tail sites, all located in Wanuskewin Heritage Park, are consistent with this pattern of lithic resource utilization. The presence of exotic lithic materials can allude to territory, trade networks spanning vast amounts of land, or even show preference for an exotic material over locally available tool stone. This thesis will allow Wolf Willow and Dog Child to be understood in the broader context of McKean sites on the Northern Plains. Secondarily, Eldon Johnson’s 1998 “Properties and Sources of Some Saskatchewan Lithic Materials of Archaeological Significance”, a popular and highly utilized thesis, is updated here with new information concerning raw materials found in Wanuskewin Heritage Park.

The archaeological record of the first Americans in Mexico is poorly known and somewhat confusing. However, the state of Sonora presents a remarkably pristine setting for studying the late Pleistocene occupation of North America. The early archaeological record in Sonora is stunning in terms of its relative abundance and only within the past ten years has this fact become evident. The Paleo-Indian sites are concentrated in north-central Sonora on and surrounding, the Llanos de Hermosillo. The settlement pattern appears to indicate that Clovis groups were generalized hunter and gatherers that exploited a wide range of environments, and their diet was based upon a wide variety of foodstuffs. The Clovis groups of Sonora developed a sophisticated settlement pattern and land use determined by the location of lithic sources for tool making, water sources, large prey animals and a mosaic of edible plants and small animals. Exploiting an extensive territory probably permitted them to remain in the same region for longer periods of time. The presence of only few late Paleo-Indian diagnostic points could represent the decrease of population density in Sonora, but most likely it is an indication that after Clovis a regionalization of the hunter and gather groups took place in Sonora. The Sonoran Clovis occupation is a testimony that multiple regional Clovis adaptations emerged each with specific responses of plants, animals and resources.

Esta pesquisa visa a compreensão das indústrias líticas relacionadas ao sambaquis Bacanga, Panaquatira e Paço do Lumiar, existentes, respectivamente, nos municípios de São Luís, São José de Ribamar e Paço do Lumiar, localizados na Ilha de São Luís, Maranhão. Os sítios cujo material foi analisado estão em uma região costeria, inseridos em ambiente de estuário e apresentaram cronologias variando entre 3.840 e 1420 anos antes do presente. Os conceitos básicos utilizados para compreender as indústrias foram os de cadeia operatória e sistema tecnológico. / This research aims at understanding the lithic industries related to shellmounds Bacanga, Panaquatira and Paço do Lumiar existing, respectively, in the municipalities of São Luís, São José de Ribamar and Paço do Lumiar, located on the island of São Luís, Maranhão. The sites where in a coastal region inserted in estuary environment and showed varying timelines between 3840 and 1420 years before present. The key concepts used to understand the industries were the operative chain and technological system.

Le sud-est français est un espace particulier pour le Paléolithique supérieur récent : il forme l’interface entre les domaines nord-occidental d’une part et méditerranéen et oriental d’autre part, entre la séquence Solutréen-Ba¬degoulien-Magdalénien-Azilien et l’Épigravettien.Alors que cette région forme encore un angle mort de la Pré¬histoire pour cette période, cette thèse s’intéresse aux industries lithiques épigravettiennes de l’arc liguro-provençal dans une perspective techno-économique qui permet un réexamen en profondeur de l’évolution des traditions techniques entre la fin du Gravettien (circa 23 000 cal. BCE) et le début du premier Mésolithique (circa 9 500 cal. BCE). Deux grands axes structurent ce travail : (1) La question chronologique. Il s’agit de réintégrer les industries étudiées dans un modèle chronocul¬turel en cours de redéfinition. Pour ce faire, l’étude des séries et l’obtention de dates par radiocarbone sont discutées avec une synthèse des connaissances concernant l’Épigravettien.(2) Les systèmes de mobilité et les stratégies d’approvisionnement. Le contexte régional est particulière¬ment favorable pour des raisons intrinsèques (domaine géologique compartimenté et espace géogra¬phique contraint) et extrinsèques (recherches effectuées depuis les années 1980 autour des ressources siliceuses régionales). Les résultats obtenus dans une perspective techno-économique sont mobilisés pour appréhender la structuration des territoires et son évolution dans le temps.Partie prenante d’une dynamique de renouvellement des connaissances sur l’Épigravettien dans sa globalité, cette thèse propose, en conclusion, un état des comparaisons possibles avec la séquence occidentale. / Southeastern France is a particular area as regards the late upper Palaeolithic as it lies between the northwestern prehistoric domain on one side, and the Mediterranean and eastern one on the other side; between the Solutrean-Badegoulian-Magdalenian-Azilian sequence and the Epigravettian one. This PhD work focuses on the techno-economic study of lithic industries originating from the Liguro-Provencal corridor, an area weakly-known for its upper Paleolithic industries. The aim is to re-assess in detail the evolution of technical traditions from the end of the Gravettian (circa 23 000 cal. BCE) to the beginning of the Mesolithic (circa 9 500 cal. BCE).This work addresses two primary objectives : (1) The Chronological framework. The industries studied are replaced in a newly defined chronocultural model. To do so, the results of the techno-economic studies and radiocarbon dates are combined and discussed in parallel with a synthesis of existing knowledge concerning the Epigravettian.(2) Mobility patterns and raw material provisioning strategies. The regional background is a particu¬larly favorable research context due to intrinsic factors (a compartmentalized geological domain and a constraining geographical area) and extrinsic ones (intensive research conducted since the 1980’s on lithic raw material availabilities). The results obtained are then mobilized to infer on ter¬ritorial organization and its evolution through time.

The Midsouth has long been known to be a locus of Paleoindian (13,200-10,000 yrs B.P.) populations. Paleoindian populations have generally been characterized as highly mobile hunter-gatherers with egalitarian social structure. Utilizing the theoretical lens of diversification and intensification of resource use, the Late Pleistocene adaptations of the region’s populations are examined from both a large scale or coarse grain perspective as well as more fine grain data from the site level. Previous models of Paleoindian adaptations are defined and tested in this study to determine the applicability of these models with new data. Coarse grain data are derived from lithic raw material use in diagnostic artifacts from six Paleoindian archaeological sites concentrated in the lower Tennessee River Valley that are referred to as the Tennessee-Duck River Paleoindian complex. Numerous Paleoindian projectile points have been recovered from these sites that allow for raw material use across the lower Tennessee River to be evaluated. Site specific data are derived from analysis of lithic artifacts and spatial distributions at the Carson-Conn-Short site (40BN190), also situated in the lower Tennessee River Valley. The Carson-Conn-Short site is a large multi-component Paleoindian site located near the confluence of the Duck and Tennessee Rivers. The regional or coarse grain data indicate a pattern of increasing regionalization and intensification of local resource use. The site level data suggest that the Paleoindian occupants of the Carson-Conn-Short site were more sedentary than previously thought. Traditional thought suggests that large, riverine Paleoindian sites are the product of either aggregation of different groups or re-occupation of the same landform over time. Rather than reflecting aggregation or re-occupation by Late Pleistocene populations, these people continuously occupied the site with minimal movement. The site was continuously occupied through the entirety Late Pleistocene into the Early Holocene. The Carson-Conn-Short site was situated at a particular locale that allowed for access to the greatest diversity of resources and also provided a mechanism that allowed for social information to be transferred via riverine mechanisms. This study suggests that Paleoindian populations in the Midsouth exhibited a greater degree of social complexity and sedentism than previously thought that provided the foundation for the development of agriculture and associated social institutions.

This thesis presents the results from archaeological test excavations at site 5GN1.2. The focus of this research is to evaluate Stiger's Late Prehistoric settlement-subsistence hypothesis. According to this hypothesis, post-3000 B.P. occupations of the Upper Gunnison Basin were limited to logistically organized big-game hunting forays originating from residential camps located outside of the basin. Since Stiger's model is based on Binford's forager-collector continuum model, archaeological test implications of his hypothesis include hunter-gatherer settlement mobility, site types, feature types, artifact assemblage characteristics, and the organization of lithic technology. Test excavations at 5GN1.2 revealed intact archaeological deposits reflecting aboriginal occupation during the Late Prehistoric between about 3000 and 1300 B.P. Late Prehistoric features include four hearths associated with abundant debitage, small-game faunal remains, burnt seeds, and lithic tools. Identified lithic tools include ground stone, projectile point fragments, cores, and bifaces. Individual flake attribute analysis of the debitage assemblage provides evidence lithic reduction activities were dominated by bifacial reduction of local and non-local raw materials. Archaeological evidence rules out site 5GN1.2 as a Late Prehistoric logistical big-game hunting site. Site 5GN1.2 contains all the hallmarks of a residential base camp, including constructed hearths, rock art, evidence of plant resource processing, small-game procurement, comparatively high tool diversity, high proportion of locally available tool-stone, late-stage tool manufacture, and tool maintenance debitage. Site 5GN1.2 likely served as a short-term residential base camp occupied by whole family groups during the Late Prehistoric. The Late Prehistoric occupations of site 5GN1.2 represent a more diverse settlement-subsistence adaptation than envisioned by Stiger's culture history. Some hunter-gatherers may have occupied the UGB on long-range logistical big-game hunting forays, but at 5GN1.2 this is simply not the case. This lithic technology research project represents the first published comprehensive debitage analysis of an archaeological component at 5GN1.2 and 5GN1. These results and data can serve as a database for later archaeological research within the UGB.

The Consort Pebble Chert Quarry site (EkOr-8) is a Pre-Contact quarry site located south of the Village of Consort, Alberta. Despite knowledge of the site's existence by local area farmers, it was only in 1999 that it was first recorded as an archaeological site. It is described as a large area dominated by the presence of marked depressions that vary in size from less than a metre in depth and diameter to well over three metres in depth and diameter as well as an abundance of chert pebbles on the ground surface. Originally believed to be an example of meteorite impacts, the site was explored by geologists from the University of Calgary. Further visits by provincial archaeologists resulted in numerous theories as to the cause of the depression features and the purpose of the site. No archaeological investigation was undertaken prior to the summer of 2006.<p>No diagnostic artifacts were recovered from within the site area; however, a possible temporal indicator to site usage may be indicated based on the discovery of a Duncan projectile point in a site immediately to the south of the Consort Pebble Chert Quarry. An abundance of lithic artifacts were uncovered as results of the shovel test program undertaken by the author during the summer of 2006. The majority of these lithic artifacts were derived from the abundant lithic material within the site area known as pebble chert. No other non-lithic artifacts were found during the course of this excavation. <p>Shovel tests were used to provide an indication of the subsurface stratigraphy at the site. No evidence of cultural strata was found and the subsurface deposits present reflect a history of glacial landscapes. A number of glacial phenomena are the likely causes of the depression features. The presence of pebble chert on the ground surface; however, did make this area an attractive location for collecting unmodified lithic material in order to fashion stone tools. The existence of numerous artifacts made from pebble chert at the site indicates that past cultural groups had visited and collected from the area. An overview of archaeological sites on the Canadian Plains demonstrates that pebble chert is a valuable lithic material that was used in a wide variety of archaeological sites throughout the Pre-Contact era.

The Consort Pebble Chert Quarry site (EkOr-8) is a Pre-Contact quarry site located south of the Village of Consort, Alberta. Despite knowledge of the site's existence by local area farmers, it was only in 1999 that it was first recorded as an archaeological site. It is described as a large area dominated by the presence of marked depressions that vary in size from less than a metre in depth and diameter to well over three metres in depth and diameter as well as an abundance of chert pebbles on the ground surface. Originally believed to be an example of meteorite impacts, the site was explored by geologists from the University of Calgary. Further visits by provincial archaeologists resulted in numerous theories as to the cause of the depression features and the purpose of the site. No archaeological investigation was undertaken prior to the summer of 2006.<p>No diagnostic artifacts were recovered from within the site area; however, a possible temporal indicator to site usage may be indicated based on the discovery of a Duncan projectile point in a site immediately to the south of the Consort Pebble Chert Quarry. An abundance of lithic artifacts were uncovered as results of the shovel test program undertaken by the author during the summer of 2006. The majority of these lithic artifacts were derived from the abundant lithic material within the site area known as pebble chert. No other non-lithic artifacts were found during the course of this excavation. <p>Shovel tests were used to provide an indication of the subsurface stratigraphy at the site. No evidence of cultural strata was found and the subsurface deposits present reflect a history of glacial landscapes. A number of glacial phenomena are the likely causes of the depression features. The presence of pebble chert on the ground surface; however, did make this area an attractive location for collecting unmodified lithic material in order to fashion stone tools. The existence of numerous artifacts made from pebble chert at the site indicates that past cultural groups had visited and collected from the area. An overview of archaeological sites on the Canadian Plains demonstrates that pebble chert is a valuable lithic material that was used in a wide variety of archaeological sites throughout the Pre-Contact era.