The Beaver Creek site: A prehistoric stone quarry on Syncrude Lease #22

The significance of the Beaver Creek Quarry site and the kinds of information we may expect to glean from it may now be enumerated. With reference to the recently published results of archaeological reconnaissance conducted on the Tar Sands Syncrude Lease #17, it was noted that over 67% of the total...

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Main Author: Syncrude Canada Ltd.
Format: Report
Language:English
Published: 1974
Subjects:
Online Access:https://era.library.ualberta.ca/items/952f3f10-8d7c-4d62-aaea-d5bfad0ef24d
https://doi.org/10.7939/R3G73796K
id ftunivalberta:oai:era.library.ualberta.ca:952f3f10-8d7c-4d62-aaea-d5bfad0ef24d
record_format openpolar
spelling ftunivalberta:oai:era.library.ualberta.ca:952f3f10-8d7c-4d62-aaea-d5bfad0ef24d 2023-05-15T15:40:51+02:00 The Beaver Creek site: A prehistoric stone quarry on Syncrude Lease #22 Syncrude Canada Ltd. 1974 https://era.library.ualberta.ca/items/952f3f10-8d7c-4d62-aaea-d5bfad0ef24d https://doi.org/10.7939/R3G73796K English eng https://era.library.ualberta.ca/items/952f3f10-8d7c-4d62-aaea-d5bfad0ef24d doi:10.7939/R3G73796K Conditions of Use Syncrude Canada Ltd., 1974. The Beaver Creek site: A prehistoric stone quarry on Syncrude Lease #22. Syncrude Canada Ltd., Edmonton, Alberta. Environmental Research Monograph 1974-2. 112 pp. Permission for non-commercial use, publication or presentation of excerpts or figures is granted, provided appropriate attribution (as above) is cited. Commercial reproduction, in whole or in part, is not permitted without prior written consent. The use of these materials by the end user is done without any affiliation with or endorsement by Syncrude Canada Ltd. Reliance upon the end user's use of these materials is at the sole risk of the end user. Archaeology Oil Sands Tar Sands Syncrude Environmental Research Monograph 1974-2 Alberta Report 1974 ftunivalberta https://doi.org/10.7939/R3G73796K 2022-08-22T20:12:26Z The significance of the Beaver Creek Quarry site and the kinds of information we may expect to glean from it may now be enumerated. With reference to the recently published results of archaeological reconnaissance conducted on the Tar Sands Syncrude Lease #17, it was noted that over 67% of the total stone assemblage recovered from 28 localities consists of quartzite derived from the Beaver Creek Quarry. It was also shown that the majority of the artifacts produced from Beaver Creek quartzite consists of flakes and detritus as opposed to finished tools. This in turn suggests that while the production of preforms at the quarry remains to be established, a significant amount of subsequent tool manufacture probably took place within a certain radius of quarry locale. The quartzite exposed along the banks of Beaver Creek may represent a unique deposit in the region. Little, indeed, is known of potential aboriginal stone sources in northern Alberta. In the central region of the province, water-rolled quartzite pebbles and cobbles found along streams and river beds is the ubiquitous stone type. North of the Tar Sands region lies the Canadian Shield which offers a variety of quartz minerals but in difficult to extract seams and veins. Some beds of chert are known to occur in the Paleozoic formations which border the pre-cambrian platform. To the west, near Peace River, Alberta dark volcanics are found in sites and en cache that were apparently traded in from aboriginal British Columbia. Should the Beaver Creek quartzite turn out to be a unique deposit in the Athabasca region, it offers an ideal opportunity to trace its dispersion and perhaps aboriginal trade networks as well. The value of being able to reconstruct a total technological process with an eye to defining an archaeological tradition has already been discussed. The potential of the Beaver Creek Quarry in this respect should be obvious. It is most opportune that this site exists and that it was located early in the archaeological research of the region. Once ... Report Beaver Creek University of Alberta: Era - Education and Research Archive
institution Open Polar
collection University of Alberta: Era - Education and Research Archive
op_collection_id ftunivalberta
language English
topic Archaeology
Oil Sands
Tar Sands
Syncrude
Environmental Research Monograph 1974-2
Alberta
spellingShingle Archaeology
Oil Sands
Tar Sands
Syncrude
Environmental Research Monograph 1974-2
Alberta
Syncrude Canada Ltd.
The Beaver Creek site: A prehistoric stone quarry on Syncrude Lease #22
topic_facet Archaeology
Oil Sands
Tar Sands
Syncrude
Environmental Research Monograph 1974-2
Alberta
description The significance of the Beaver Creek Quarry site and the kinds of information we may expect to glean from it may now be enumerated. With reference to the recently published results of archaeological reconnaissance conducted on the Tar Sands Syncrude Lease #17, it was noted that over 67% of the total stone assemblage recovered from 28 localities consists of quartzite derived from the Beaver Creek Quarry. It was also shown that the majority of the artifacts produced from Beaver Creek quartzite consists of flakes and detritus as opposed to finished tools. This in turn suggests that while the production of preforms at the quarry remains to be established, a significant amount of subsequent tool manufacture probably took place within a certain radius of quarry locale. The quartzite exposed along the banks of Beaver Creek may represent a unique deposit in the region. Little, indeed, is known of potential aboriginal stone sources in northern Alberta. In the central region of the province, water-rolled quartzite pebbles and cobbles found along streams and river beds is the ubiquitous stone type. North of the Tar Sands region lies the Canadian Shield which offers a variety of quartz minerals but in difficult to extract seams and veins. Some beds of chert are known to occur in the Paleozoic formations which border the pre-cambrian platform. To the west, near Peace River, Alberta dark volcanics are found in sites and en cache that were apparently traded in from aboriginal British Columbia. Should the Beaver Creek quartzite turn out to be a unique deposit in the Athabasca region, it offers an ideal opportunity to trace its dispersion and perhaps aboriginal trade networks as well. The value of being able to reconstruct a total technological process with an eye to defining an archaeological tradition has already been discussed. The potential of the Beaver Creek Quarry in this respect should be obvious. It is most opportune that this site exists and that it was located early in the archaeological research of the region. Once ...
format Report
author Syncrude Canada Ltd.
author_facet Syncrude Canada Ltd.
author_sort Syncrude Canada Ltd.
title The Beaver Creek site: A prehistoric stone quarry on Syncrude Lease #22
title_short The Beaver Creek site: A prehistoric stone quarry on Syncrude Lease #22
title_full The Beaver Creek site: A prehistoric stone quarry on Syncrude Lease #22
title_fullStr The Beaver Creek site: A prehistoric stone quarry on Syncrude Lease #22
title_full_unstemmed The Beaver Creek site: A prehistoric stone quarry on Syncrude Lease #22
title_sort beaver creek site: a prehistoric stone quarry on syncrude lease #22
publishDate 1974
url https://era.library.ualberta.ca/items/952f3f10-8d7c-4d62-aaea-d5bfad0ef24d
https://doi.org/10.7939/R3G73796K
genre Beaver Creek
genre_facet Beaver Creek
op_relation https://era.library.ualberta.ca/items/952f3f10-8d7c-4d62-aaea-d5bfad0ef24d
doi:10.7939/R3G73796K
op_rights Conditions of Use Syncrude Canada Ltd., 1974. The Beaver Creek site: A prehistoric stone quarry on Syncrude Lease #22. Syncrude Canada Ltd., Edmonton, Alberta. Environmental Research Monograph 1974-2. 112 pp. Permission for non-commercial use, publication or presentation of excerpts or figures is granted, provided appropriate attribution (as above) is cited. Commercial reproduction, in whole or in part, is not permitted without prior written consent. The use of these materials by the end user is done without any affiliation with or endorsement by Syncrude Canada Ltd. Reliance upon the end user's use of these materials is at the sole risk of the end user.
op_doi https://doi.org/10.7939/R3G73796K
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