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The swing of things : contributions to archaeological research in Alberta, 2018.

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The swing of things: Contributions to archaeological research in Alberta, 2018 is part of the Archaeological Survey of Alberta. This issue contains a series of archaeology articles that inform... More ≫

Description

The swing of things: Contributions to archaeological research in Alberta, 2018 is part of the Archaeological Survey of Alberta. This issue contains a series of archaeology articles that inform research, management practices, and methods in Alberta.

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Testing debitage typologies with statistical analysis : experimental inferences upon archaeological material from FaPx-1, a sub-alpine hunting camp in the Alberta Rockies

Description

Stone production debris (debitage) is the most common artifact type found at archaeological sites in North America. A significant time investment is required to catalogue debitage from large... More ≫

Description

Stone production debris (debitage) is the most common artifact type found at archaeological sites in North America. A significant time investment is required to catalogue debitage from large assemblages. Conventional thought holds that, because lithic tool manufacture is reductive, the attributes of flake size and cortex amount will decrease throughout production while dorsal flake scars increase. Dorsal scar count is an attribute commonly used to infer trends in an assemblage; however, the statistical significance of dorsal scars as a measure of the stage of lithic tool production has not been addressed adequately. Cortex amount is also used to deduce lithic reduction stages; however, the author argues that this may not represent behavioral patterns as meaningfully as platform morphology.

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New Vertical Series rock art at the Glenwood Erratic, DiPi-42, Alberta

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The Vertical Series type of Indigenous rock art is found at only a handful of sites across the northern Great Plains. Discovery of a new site is therefore significant. In 2012 the Glenwood Erratic... More ≫

Description

The Vertical Series type of Indigenous rock art is found at only a handful of sites across the northern Great Plains. Discovery of a new site is therefore significant. In 2012 the Glenwood Erratic in southwestern Alberta was reported as a heavily vandalized rock art site. Inspection, however, revealed no rock art where originally specified. Instead, previously unknown rock art was found on many surfaces of the erratic, all of which is faint and challenging to describe. The age of the artwork is estimated at between 500 to 1,000 years before present. The identity of the cultural group responsible is unknown.

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The swing of things : contributions to archaeological research in Alberta, 2018. Dedication : Milton (Milt) J. Wright

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The swing of things: Contributions to archaeological research in Alberta, 2018 is part of the Archaeological Survey of Alberta. This issue is a dedication to Wilt Wright, an Alberta archaeologist... More ≫

Description

The swing of things: Contributions to archaeological research in Alberta, 2018 is part of the Archaeological Survey of Alberta. This issue is a dedication to Wilt Wright, an Alberta archaeologist who recently passed away.

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Identifying Knife River Flint in Alberta : a silicified lignite toolstone from North Dakota

Description

This article is the fourth in a series intended to assist the identification of raw materials used for precontact stone tools in Alberta. Each article focuses on one raw material; the current... More ≫

Description

This article is the fourth in a series intended to assist the identification of raw materials used for precontact stone tools in Alberta. Each article focuses on one raw material; the current article discusses a silicified lignite called Knife River Flint (KRF) that originates in North Dakota and appears in archaeological sites across Alberta. Local materials, including chalcedony, silicified peat/petrified wood, and translucent chert, can be mistaken for KRF: macroscopic and microscope qualities of these materials are described with an accompanying photograph library to assist identification. Several methods were tested to assess their feasibility for distinguishing KRF from local materials. KRF so closely resembles other materials in terms of macroscopics, microscopics, and geochemistry that conclusively demonstrating provenance remains problematic.

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