A number of aspects of the prehistory of northern Ontario are considered in these reports. Of central concern are the spatial variations of the Terminal Woodland ceramics and the evidence for the transition from the Laurel assemblage into Blackduck assemblage

Excavation at the Stampede Camp and the Saamis site, located in Medicine Hat, Alberta, resulted in the isolation of five site areas from which an abundance of artifacts were recovered, providing data for detailed typological analysis, cultural reconstruction and comparative studies. Together the two sites were occupied during the Middle Prehistoric, Late Prehistoric and Protohistoric periods.

This study is an analysis and functional interpretation of the cultural remains from a Middle Period bison hunters’ campsite situated in the parklands of central Saskatchewan. The Harder site, excavated by the author during 1969, 1970, 1971 and 1972, and radiocarbon dated at 3,400 years, belongs to the Oxbow archaeological complex.

This report describes the results of excavations at the Banting and Hussey sites, two Paleo-Indian campsites located near Alliston in Simcoe County, southern Ontario, and the results of survey work along the strandline of glacial Lake Algonquin in the Alliston area.

Excavations at the Lagoon site (OjRl-3) on the southern coast of Banks Island, Northwest Territories have provided a database with which to formulate hypotheses concerning the Paleoeskimo culture history of the western periphery of the Canadian Arctic at ca. 500 B.C.

Excavations at the Washout site (NjVi-2), Herschel Island, Yukon Territory were conducted for two field seasons in order to obtain data on early Thule subsistence, and to determine the affinity of the site to later Mackenzie Inuit occupations.

Excavations in 1971 and 1972 reveal two major occupation levels at the Estuary Bison Pound site, located near the head of a large coulee on the south bank of the South Saskatchewan River, just below its confluence with the Red Deer River. They present strong evidence to suggest that the Old Women’s phase developed from the Avonlea phase.