<?xml version="1.0" encoding="UTF-8"?><xml><records><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>13</ref-type><contributors><secondary-authors><author><style face="normal" font="default" size="100%">Colin Varley</style></author></secondary-authors><tertiary-authors><author><style face="normal" font="default" size="100%">Lynn Meskell</style></author><author><style face="normal" font="default" size="100%">Robert W. Preucel</style></author></tertiary-authors></contributors><titles><title><style face="normal" font="default" size="100%">A Companion to Social Archaeology</style></title><secondary-title><style face="normal" font="default" size="100%">Canadian Journal of Archaeology/Journal canadien d&#039;archéologie</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2009</style></year></dates><volume><style face="normal" font="default" size="100%">33</style></volume><pages><style face="normal" font="default" size="100%">166-169</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><issue><style face="normal" font="default" size="100%">1</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">J. Rod Vickers</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Seasonal Round Problems on the Alberta Plains</style></title><secondary-title><style face="normal" font="default" size="100%">Canadian Journal of Archaeology/Journal canadien d&#039;archéologie</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">1991</style></year></dates><volume><style face="normal" font="default" size="100%">15</style></volume><pages><style face="normal" font="default" size="100%">055-072</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p&gt;This paper examines the articulation of archaeological data with models of Native settlement pattern on the Alberta Plains. The models are derived from ethnographic accounts for the Historic equestrian Blackfoot, and from bison ecology for prehistoric pedestrian hunters. Both models assume that the Plains Indians were organized into residential bands which may have formed tribal aggregates in some seasons. The archaeological data indicate that two patterns of spring settlement existed; one of bands communally hunting bison, another of extended family groups stalking bison. There is no evidence for summer tribal aggregations; rather, it appears that small family camps were situated along the edges of river valleys. Large fall season communal kills and camps are under-represented in comparison to the Wyoming record; this may be a sampling problem. Two patterns exist for winter: large, isolated, multi-band camps in major river valleys, and smaller band camps distributed more continuously along smaller streams. The large winter camps form the best evidence for residential aggregates larger than the band in prehistoric times. These data suggest that the settlement pattern was more complex than accounted for by existing models.&lt;/p&gt;</style></abstract><custom1><style face="normal" font="default" size="100%">&lt;p&gt;Dans ce travail, nous étudions l&amp;#39;articulation des données archéolgiques avec les modèles d&amp;#39;établissement des Indiens vivant dans les plaines de l&amp;#39;Alberta. Les informations ethnographiques ont permis de reconstituer le modèle d&amp;#39;établissement des Pieds-Noirs, chasseurs équestres de la période historique, et c&amp;#39;est à partir de l&amp;#39;écologie des bisons que nous avons reconstituer celui des chasseurs pédestres de la période préhistorique. Nous supposons que dans les deux cas, les Indiens des Plaines composaient des bandes qui pouvaient se réunir en groupes tribaux à certaines saisons. Selon les évidences archéologiques, il y aurait alors eu deux types de campements printaniers. L&amp;#39;un aurait correspondu à la présence de bandes pourchassant le bison de manière concertative et l&amp;#39;autre, à l&amp;#39;activité de groupes familiaux étendus, chassant le bison à l&amp;#39;aff_t. Il n&amp;#39;y a aucune attestation de groupes tribaux durant l&amp;#39;été alors que des petits camps familiaux, dressés sur le bord des vallées, semblent avoir prévalu. Nous n&amp;#39;arrivons pas non plus à identifier autant de grandes chasses communautaires d&amp;#39;automne ou de camps qui y correspondraient, qu&amp;#39;au Wyoming. Cette sous-représentation pourrait cependant n&amp;#39;être qu&amp;#39;un biais d&amp;#39;échantillonnage. Il y a deux modèles de campements d&amp;#39;hiver. L&amp;#39;un correspond à de grands rassemblements discontinus de plusieurs bandes dans les vallées principales, l&amp;#39;autre à l&amp;#39;établissement plus continu de camp plus petits, le long de cours d&amp;#39;eau secondaires. Les grands camps d&amp;#39;hiver fournissent la meilleure preuve de la présence préhistorique d&amp;#39;unités de rassemblement supérieures à la bande. On peut alors croire que le modèle d&amp;#39;établissement préhistorique était plus complexe que les modèles actuels ne permettaient de le supposer.&lt;/p&gt;</style></custom1></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>13</ref-type><contributors><secondary-authors><author><style face="normal" font="default" size="100%">Laurie Milne</style></author></secondary-authors><tertiary-authors><author><style face="normal" font="default" size="100%">Natalia Vogeikoff-Brogan</style></author><author><style face="normal" font="default" size="100%">Jack L. Davis</style></author><author><style face="normal" font="default" size="100%">Vasiliki Florou</style></author></tertiary-authors></contributors><titles><title><style face="normal" font="default" size="100%">Carl W. Blegen: Personal and Archaeological Narratives</style></title><secondary-title><style face="normal" font="default" size="100%">Canadian Journal of Archaeology/Journal canadien d&#039;archéologie</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2016</style></year></dates><volume><style face="normal" font="default" size="100%">40</style></volume><pages><style face="normal" font="default" size="100%">348–351</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><issue><style face="normal" font="default" size="100%">2</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>5</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">John S. Vogel</style></author><author><style face="normal" font="default" size="100%">Thomas A. Brown</style></author><author><style face="normal" font="default" size="100%">John R. Southon</style></author><author><style face="normal" font="default" size="100%">D. Erle Nelson</style></author></authors><secondary-authors><author><style face="normal" font="default" size="100%">Jacques Cinq-Mars</style></author><author><style face="normal" font="default" size="100%">Jean-Luc Pilon</style></author></secondary-authors></contributors><titles><title><style face="normal" font="default" size="100%">Accelerator Radiocarbon Dates from the NOGAP Archaeology Project</style></title><secondary-title><style face="normal" font="default" size="100%">CAA Occasional Paper No. 1</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">1991</style></year></dates><volume><style face="normal" font="default" size="100%">1</style></volume><pages><style face="normal" font="default" size="100%">143-147</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">The technique of accelerator mass spectrometry was used to provide radiocarbon ages for
31 bone, antler and wood samples. The samples were sufficiently large (0.25 - 2g) and
well-preserved that routine preparative procedures could be used. We encountered no
unusual problems, and so we are confident that the results obtained are reliable.</style></abstract></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Peter H. von Bitter</style></author><author><style face="normal" font="default" size="100%">Betty Eley</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Balsam Lake Chert from the Upper Member of the Middle Ordovician Bobcaygeon Formation of Southern Ontario</style></title><secondary-title><style face="normal" font="default" size="100%">Canadian Journal of Archaeology/Journal canadien d&#039;archéologie</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">1984</style></year></dates><volume><style face="normal" font="default" size="100%">8</style></volume><pages><style face="normal" font="default" size="100%">135-148</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p&gt;Balsam Lake chert, a diagnostic lithic material characterized by its dark bluish-gray colour and peloidal texture, is of interest because of its use by native peoples of southern Ontario for the manufacture of tools and weapons. Archaeologists have found this material at various sites but its geological source has until now remained unknown. We have located two in situ sources of the chert in the upper member of the Bobcaygeon Formation on Balsam Lake. This chert is apparently, discontinuously bedded and restricted to one horizon, an important factor in tracing it elsewhere in the area and in locating Indian quarry and workshop sites.&lt;/p&gt;</style></abstract><custom1><style face="normal" font="default" size="100%">Notre étude du chert du Lac Balsam, matière diagnostique litée carctérisée par sa couleur gris bleuté et sa texture peloidale, est important à cause des Autochtones du sud de l&#039;Ontario qui s&#039;en servaient pour fabriquer des outils et des armes. Les archéologues ont découvert cette matière dans divers sites, mais, jusqu&#039;à présent, ils ne connaissaient pas sa source géologique. Nous avons maintenant découvert deux sources in situ de chert dans le membre supérieur de la Formation Bobcaygeon sur le Lac Balsam. Il paraît que ce chert forme des couches intermittentes et se limite à un horizon -- une découverte importante qui facilitera les recherches futures dans la région et la découverte de carrières amérindiennes et de sites de travail.</style></custom1><issue><style face="normal" font="default" size="100%">2</style></issue></record></records></xml>