ARCTIC Some Practical Applications of Obsidian Hydration Dating in the Subarctic

ABSTRACT. Eight case studies of obsidian hydration dating in the Koyukuk River region of northwestern interior Alaska are discussed. Historiographic conclusions include recognition of late and early microblade industries, apparent verification of the hypothesis that northern fluted points date withi...

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Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.556.4713
http://pubs.aina.ucalgary.ca/arctic/Arctic37-2-91.pdf
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spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.556.4713 2023-05-15T14:19:48+02:00 ARCTIC Some Practical Applications of Obsidian Hydration Dating in the Subarctic The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.556.4713 http://pubs.aina.ucalgary.ca/arctic/Arctic37-2-91.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.556.4713 http://pubs.aina.ucalgary.ca/arctic/Arctic37-2-91.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://pubs.aina.ucalgary.ca/arctic/Arctic37-2-91.pdf text ftciteseerx 2016-01-08T11:48:03Z ABSTRACT. Eight case studies of obsidian hydration dating in the Koyukuk River region of northwestern interior Alaska are discussed. Historiographic conclusions include recognition of late and early microblade industries, apparent verification of the hypothesis that northern fluted points date within a Palm-Indian time frame, and validation of a Tuktu-like first millennium A.D. Northern Archaic phase. However, variance in the data and lack of firm hydration rates render the results less precise than is desired. Methodological conclusions have ramifications that should apply throughout the subarctic region and well beyond. These are: 1) Hydration measurements may be unreliable for dating individual specimens; 2) Lack of closely controlled hydration rates or dependence on 14-C dates with large errors for calibration can be crippling; 3) The average of a series of specimens can be used to date components which were formed during a brief period of occupation, though high variance of the data may be disconcerting; 4) Variance was low in one case for specimens all derived from the same piece of raw material, but for dating it may be necessary to find, through induced hydration or other means, the precise hydration rate ap-plicable to each different piece of raw material (from a single component); and 5) Many variables may be responsible for results.which render some sample sets unreliable or unusable, especially those from surface sites. Some of these variables require further technical investigation- loss of the hydration layer and recommencement of hydration after exposure to forest and tundra fires, for instance. Other factors are reasonably well under-stood by researchers, but it would be desirable to have computer simulations of site contexts in order to assess the magnitude, correlations, and cumulative results of their effects. Key words: archaeology, western Subarctic, Alaska, dating, obsidian, obsidian hydration Text Arctic Arctic Northern Archaic Subarctic Tundra Alaska Unknown Arctic Indian
institution Open Polar
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op_collection_id ftciteseerx
language English
description ABSTRACT. Eight case studies of obsidian hydration dating in the Koyukuk River region of northwestern interior Alaska are discussed. Historiographic conclusions include recognition of late and early microblade industries, apparent verification of the hypothesis that northern fluted points date within a Palm-Indian time frame, and validation of a Tuktu-like first millennium A.D. Northern Archaic phase. However, variance in the data and lack of firm hydration rates render the results less precise than is desired. Methodological conclusions have ramifications that should apply throughout the subarctic region and well beyond. These are: 1) Hydration measurements may be unreliable for dating individual specimens; 2) Lack of closely controlled hydration rates or dependence on 14-C dates with large errors for calibration can be crippling; 3) The average of a series of specimens can be used to date components which were formed during a brief period of occupation, though high variance of the data may be disconcerting; 4) Variance was low in one case for specimens all derived from the same piece of raw material, but for dating it may be necessary to find, through induced hydration or other means, the precise hydration rate ap-plicable to each different piece of raw material (from a single component); and 5) Many variables may be responsible for results.which render some sample sets unreliable or unusable, especially those from surface sites. Some of these variables require further technical investigation- loss of the hydration layer and recommencement of hydration after exposure to forest and tundra fires, for instance. Other factors are reasonably well under-stood by researchers, but it would be desirable to have computer simulations of site contexts in order to assess the magnitude, correlations, and cumulative results of their effects. Key words: archaeology, western Subarctic, Alaska, dating, obsidian, obsidian hydration
author2 The Pennsylvania State University CiteSeerX Archives
format Text
title ARCTIC Some Practical Applications of Obsidian Hydration Dating in the Subarctic
spellingShingle ARCTIC Some Practical Applications of Obsidian Hydration Dating in the Subarctic
title_short ARCTIC Some Practical Applications of Obsidian Hydration Dating in the Subarctic
title_full ARCTIC Some Practical Applications of Obsidian Hydration Dating in the Subarctic
title_fullStr ARCTIC Some Practical Applications of Obsidian Hydration Dating in the Subarctic
title_full_unstemmed ARCTIC Some Practical Applications of Obsidian Hydration Dating in the Subarctic
title_sort arctic some practical applications of obsidian hydration dating in the subarctic
url http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.556.4713
http://pubs.aina.ucalgary.ca/arctic/Arctic37-2-91.pdf
geographic Arctic
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genre Arctic
Arctic
Northern Archaic
Subarctic
Tundra
Alaska
genre_facet Arctic
Arctic
Northern Archaic
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http://pubs.aina.ucalgary.ca/arctic/Arctic37-2-91.pdf
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