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North Lauder locale Radiocarbon Report 5

http://archives.brandonu.ca/en/permalink/descriptions12331
Part Of
RG 7 Beverley Nicholson fonds
Description Level
Sub sub series
GMD
multiple media
Date Range
1997-2000
Accession Number
1-2010
Part Of
RG 7 Beverley Nicholson fonds
Description Level
Sub sub series
Series Number
2.5.5
Accession Number
1-2010
GMD
multiple media
Date Range
1997-2000
Physical Description
pages 3-5
Material Details
Radiocarbon date reports have been scanned in multi-page PDF files.
History / Biographical
North Lauder Radiocarbon Date report by Beta Analytic Inc. for Flintstone Hill #111142 and #111143. Radiocarbon dating The technique of radiocarbon dating was developed by Willard Libby and his colleagues at the University of Chicago in 1949. Radiocarbon dating is used to estimate the age of organic remains from archaeological sites. Organic matter has a radioactive form of carbon (C14) that begins to decay upon death. C14 decays at a steady, known rate of a half life of 5,730 years. The technique is useful for material up to 50,000 years. Fluctuations of C14 in the atmosphere can affect results so dates are calibrated against dendrochronology. Radiocarbon dates are calibrated to calendar years. Dates are reported in radiocarbon years or Before Present. Before Present refers to dates before 1950. The introduction of massive amounts of C14, due to atomic bomb and surface testing of atomic weapons, has widely increased the standard deviation on all dates after A.D. 1700 causing these dates to be unreliable. Accelerated mass spectrometry can more accurately measure C14 with smaller samples and can date materials to 80,000 years.
Scope and Content
Sub sub series contains radiocarbon dates from: Atkinson site and Flintstone Hill.
Name Access
North Lauder locale Radiocarbon Report 5
Subject Access
Archaeology North Lauder locale North Lauder locale Radiocarbon Report 5
Documents

2.5.5_FSH_RC14_Beta_111142_111143.pdf

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Crepeele locale Radiocarbon Report I

http://archives.brandonu.ca/en/permalink/descriptions11968
Part Of
RG 7 Beverley Nicholson fonds
Description Level
Sub sub series
GMD
multiple media
Date Range
2003-2008
Accession Number
1-2010
Part Of
RG 7 Beverley Nicholson fonds
Description Level
Sub sub series
Series Number
1.5.1
Accession Number
1-2010
GMD
multiple media
Date Range
2003-2008
Physical Description
3 pages
Material Details
Radiocarbon date reports have been scanned in multi-page PDF files.
History / Biographical
Crepeele locale Radiocarbon Dates. C14 report by IsoTrace Laboratory for Crepeele site 2005 XU 8. From 2003 to 2008 field work took place at the Crepeele locale with 75 - 1m x1m units excavated. To help establish the cultural sequence at the locale Radiocarbon dates were obtained from the three sites in the Crepeele locale. Radiocarbon dating The technique of radiocarbon dating was developed by Willard Libby and his colleagues at the University of Chicago in 1949. Radiocarbon dating is used to estimate the age of organic remains from archaeological sites. Organic matter has a radioactive form of carbon (C14) that begins to decay upon death. C14 decays at a steady, known rate of a half life of 5,730 years. The technique is useful for material up to 50,000 years. Fluctuations of C14 in the atmosphere can affect results so dates are calibrated against dendrochronology. Radiocarbon dates are calibrated to calendar years. Dates are reported in radiocarbon years or Before Present. Before Present refers to dates before 1950. The introduction of massive amounts of C14, due to atomic bomb and surface testing of atomic weapons, has widely increased the standard deviation on all dates after A.D. 1700 causing these dates to be unreliable. Accelerated mass spectrometry can more accurately measure C14 with smaller samples and can date materials to 80,000 years.
Scope and Content
Sub sub series contains radiocarbon dates from: Crepeele, Sarah and Graham sites.
Name Access
Crepeele locale Radiocarbon Report I
Subject Access
Archaeology Crepeele locale Crepeele locale Radiocarbon Dates
Documents

1.5.1_Crepeele05_RC14.pdf

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Crepeele locale Radiocarbon Report II

http://archives.brandonu.ca/en/permalink/descriptions11969
Part Of
RG 7 Beverley Nicholson fonds
Description Level
Sub sub series
GMD
multiple media
Date Range
2003-2008
Accession Number
1-2010
Part Of
RG 7 Beverley Nicholson fonds
Description Level
Sub sub series
Series Number
1.5.2
Accession Number
1-2010
GMD
multiple media
Date Range
2003-2008
Physical Description
8 pages
Material Details
Radiocarbon date reports have been scanned in multi-page PDF files.
History / Biographical
Crepeele locale Radiocarbon Dates. C14 report by Beta Analytic Inc. for Crepeele site XU 48 and Graham site XU 54. From 2003 to 2008 field work took place at the Crepeele locale with 75 - 1m x1m units excavated. To help establish the cultural sequence at the locale Radiocarbon dates were obtained from the three sites in the Crepeele locale. Radiocarbon dating The technique of radiocarbon dating was developed by Willard Libby and his colleagues at the University of Chicago in 1949. Radiocarbon dating is used to estimate the age of organic remains from archaeological sites. Organic matter has a radioactive form of carbon (C14) that begins to decay upon death. C14 decays at a steady, known rate of a half life of 5,730 years. The technique is useful for material up to 50,000 years. Fluctuations of C14 in the atmosphere can affect results so dates are calibrated against dendrochronology. Radiocarbon dates are calibrated to calendar years. Dates are reported in radiocarbon years or Before Present. Before Present refers to dates before 1950. The introduction of massive amounts of C14, due to atomic bomb and surface testing of atomic weapons, has widely increased the standard deviation on all dates after A.D. 1700 causing these dates to be unreliable. Accelerated mass spectrometry can more accurately measure C14 with smaller samples and can date materials to 80,000 years.
Scope and Content
Sub sub series contains radiocarbon dates from: Crepeele, Sarah and Graham sites.
Name Access
Crepeele locale Radiocarbon Report II
Subject Access
Archaeology Crepeele locale Crepeele locale Radiocarbon Dates
Documents

1.5.2_Crepeele08_RC14.pdf

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Crepeele locale Radiocarbon Report III

http://archives.brandonu.ca/en/permalink/descriptions11970
Part Of
RG 7 Beverley Nicholson fonds
Description Level
Sub sub series
GMD
multiple media
Date Range
2003-2008
Accession Number
1-2010
Part Of
RG 7 Beverley Nicholson fonds
Description Level
Sub sub series
Series Number
1.5.3
Accession Number
1-2010
GMD
multiple media
Date Range
2003-2008
Physical Description
9 pages
Material Details
Radiocarbon date reports have been scanned in multi-page PDF files.
History / Biographical
Crepeele locale Radiocarbon Dates. C14 report by Beta Analytic Inc. for Crepeele site XUs 8, 30, 50. From 2003 to 2008 field work took place at the Crepeele locale with 75 - 1m x1m units excavated. To help establish the cultural sequence at the locale Radiocarbon dates were obtained from the three sites in the Crepeele locale. Radiocarbon dating The technique of radiocarbon dating was developed by Willard Libby and his colleagues at the University of Chicago in 1949. Radiocarbon dating is used to estimate the age of organic remains from archaeological sites. Organic matter has a radioactive form of carbon (C14) that begins to decay upon death. C14 decays at a steady, known rate of a half life of 5,730 years. The technique is useful for material up to 50,000 years. Fluctuations of C14 in the atmosphere can affect results so dates are calibrated against dendrochronology. Radiocarbon dates are calibrated to calendar years. Dates are reported in radiocarbon years or Before Present. Before Present refers to dates before 1950. The introduction of massive amounts of C14, due to atomic bomb and surface testing of atomic weapons, has widely increased the standard deviation on all dates after A.D. 1700 causing these dates to be unreliable. Accelerated mass spectrometry can more accurately measure C14 with smaller samples and can date materials to 80,000 years.
Scope and Content
Sub sub series contains radiocarbon dates from: Crepeele, Sarah and Graham sites.
Name Access
Crepeele locale Radiocarbon Report III
Subject Access
Archaeology Crepeele locale Crepeele locale Radiocarbon Dates
Documents

1.5.3_Crepeele08_RC14.pdf

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Crepeele locale Radiocarbon Report IV

http://archives.brandonu.ca/en/permalink/descriptions11971
Part Of
RG 7 Beverley Nicholson fonds
Description Level
Sub sub series
GMD
multiple media
Date Range
2003-2008
Accession Number
1-2010
Part Of
RG 7 Beverley Nicholson fonds
Description Level
Sub sub series
Series Number
1.5.4
Accession Number
1-2010
GMD
multiple media
Date Range
2003-2008
Physical Description
2 pages
Material Details
Radiocarbon date reports have been scanned in multi-page PDF files.
History / Biographical
Crepeele locale Radiocarbon Dates. C14 report by IsoTrace Analytic Laboratory for Sarah site XU17. From 2003 to 2008 field work took place at the Crepeele locale. The Crepeele, Graham and Sarah sites were excavated with 75 - 1m x1m units excavated To help establish the cultural sequence at the locale Radiocarbon dates were obtained from the three sites in the Crepeele locale. Radiocarbon dating The technique of radiocarbon dating was developed by Willard Libby and his colleagues at the University of Chicago in 1949. Radiocarbon dating is used to estimate the age of organic remains from archaeological sites. Organic matter has a radioactive form of carbon (C14) that begins to decay upon death. C14 decays at a steady, known rate of a half life of 5,730 years. The technique is useful for material up to 50,000 years. Fluctuations of C14 in the atmosphere can affect results so dates are calibrated against dendrochronology. Radiocarbon dates are calibrated to calendar years. Dates are reported in radiocarbon years or Before Present. Before Present refers to dates before 1950. The introduction of massive amounts of C14, due to atomic bomb and surface testing of atomic weapons, has widely increased the standard deviation on all dates after A.D. 1700 causing these dates to be unreliable. Accelerated mass spectrometry can more accurately measure C14 with smaller samples and can date materials to 80,000 years.
Scope and Content
Sub sub series contains radiocarbon dates from: Crepeele, Sarah and Graham sites.
Name Access
Crepeele locale Radiocarbon Report IV
Subject Access
Archaeology Crepeele locale Crepeele locale Radiocarbon Dates
Documents

1.5.4_Sarah07_RC14.pdf

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Crepeele locale Radiocarbon Report V

http://archives.brandonu.ca/en/permalink/descriptions11972
Part Of
RG 7 Beverley Nicholson fonds
Description Level
Sub sub series
GMD
multiple media
Date Range
2003-2008
Accession Number
1-2010
Part Of
RG 7 Beverley Nicholson fonds
Description Level
Sub sub series
Series Number
1.5.5
Accession Number
1-2010
GMD
multiple media
Date Range
2003-2008
Physical Description
2 pages
Material Details
Radiocarbon date reports have been scanned in multi-page PDF files.
History / Biographical
Crepeele locale Radiocarbon Dates. C14 report by IsoTrace Analytic Laboratory for Graham site XUs 5 and 8. From 2003 to 2008 field work took place at the Crepeele locale. The Crepeele, Graham and Sarah sites were excavated with 75 - 1m x1m units excavated To help establish the cultural sequence at the locale Radiocarbon dates were obtained from the three sites in the Crepeele locale. Radiocarbon dating The technique of radiocarbon dating was developed by Willard Libby and his colleagues at the University of Chicago in 1949. Radiocarbon dating is used to estimate the age of organic remains from archaeological sites. Organic matter has a radioactive form of carbon (C14) that begins to decay upon death. C14 decays at a steady, known rate of a half life of 5,730 years. The technique is useful for material up to 50,000 years. Fluctuations of C14 in the atmosphere can affect results so dates are calibrated against dendrochronology. Radiocarbon dates are calibrated to calendar years. Dates are reported in radiocarbon years or Before Present. Before Present refers to dates before 1950. The introduction of massive amounts of C14, due to atomic bomb and surface testing of atomic weapons, has widely increased the standard deviation on all dates after A.D. 1700 causing these dates to be unreliable. Accelerated mass spectrometry can more accurately measure C14 with smaller samples and can date materials to 80,000 years.
Scope and Content
Sub sub series contains radiocarbon dates from: Crepeele, Sarah and Graham sites.
Name Access
Crepeele locale Radiocarbon Report V
Subject Access
Archaeology Crepeele locale Crepeele locale Radiocarbon Dates
Documents

1.5.5_Graham07_RC14.pdf

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Lovstrom Block B - summary

http://archives.brandonu.ca/en/permalink/descriptions12479
Part Of
RG 7 Beverley Nicholson fonds
Description Level
Sub-series
GMD
multiple media
Date Range
1987
Accession Number
1-2010
Part Of
RG 7 Beverley Nicholson fonds
Description Level
Sub-series
Series Number
3.3
Accession Number
1-2010
GMD
multiple media
Date Range
1987
History / Biographical
Block B consisted of 20 contiguous 1m2 units excavated to 30 cm below surface. (except unit 58 which was excavated to 35 cm bs to obtain extended soil profile). The block is situated in recent oak and poplar forest at the head of a ravine leading to Jock’s Creek, adjacent to an area cleared for market gardening. As was the case with Block A, the understory is heavily overgrown with hazelnut, chokecherry, saskatoon, and a poison ivy/sarsaparilla ground cover. The soil levels below the sod in Block B consisted of a black, silty, and gritty loam layer from 5 cm to 23 cm below surface, a yellow and sandy clay from 23 cm to 30 cm below surface, and glacial till at 30 cm below surface. As in Block A, limestone cobbles were found throughout the occupation level around the bone. It is evident that bioturbation – primarily tree roots and rodent burrowing – have significantly altered patterns of original deposition of lithics, ceramics and small bone. The faunal layer lay close to the surface, situated entirely in the black loam 5 cm – 23 cm below surface. The 23 cm depth also marked the end of the dark silty loam. At 10 cm below surface, a discernible patterning of the bone appeared. Concentrations of bone in narrow rows ran in an irregular pattern from the northwest to the southeast part of the block. This pattern was most apparent in the north end of the block which is the highest point in the block. In the same 1m2 unit, patches of weathered, very poorly preserved bone would be found lying close to patches of well preserved bone. It is believed that this variability in preservation results from uneven rates of burial due to taphic activities of pocket gophers or other agents of bioturbation. The same pattern of uneven preservation occurs over much of the locale but is most evident in Block B. Diagnostic lithics included eleven projectile points that were predominantly Plains or Prairie Side-notch types, but included two unnotched triangular points. Cord-wrapped impressed rim sherds and body sherds were recovered. The ceramics are variants of the Woodland Blackduck horizon. RC dates: XU49 – 675/80 BP XU 59 – 705/75BP.
Scope and Content
Sub-sub-sub series contains: Summary information of field methology, number and co-ordinates of excavations, personnel and their staff position; Field journals are daily records of recoveries, features and activities at the site; Site records include excavation level and unit summaries, feature sheets, profiles; sample records and maps; Artifact catalogues are lists and identifications of all artifacts recovered; Photographs are of excavation units, features, the landscape and personnel.
Name Access
Lovstrom Block B - summary
Subject Access
Archaeology Lovstrom locale Lovstrom Block B
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North Lauder locale Radiocarbon Report I

http://archives.brandonu.ca/en/permalink/descriptions12327
Part Of
RG 7 Beverley Nicholson fonds
Description Level
Sub sub series
GMD
multiple media
Date Range
1997-2000
Accession Number
1-2010
Part Of
RG 7 Beverley Nicholson fonds
Description Level
Sub sub series
Series Number
2.5.1
Accession Number
1-2010
GMD
multiple media
Date Range
1997-2000
Physical Description
2 pages
Material Details
Radiocarbon date reports have been scanned in multi-page PDF files.
History / Biographical
North Lauder Radiocarbon Date report by IsoTrace Laboratory for Atkinson II site #TO-11882. Radiocarbon dating The technique of radiocarbon dating was developed by Willard Libby and his colleagues at the University of Chicago in 1949. Radiocarbon dating is used to estimate the age of organic remains from archaeological sites. Organic matter has a radioactive form of carbon (C14) that begins to decay upon death. C14 decays at a steady, known rate of a half life of 5,730 years. The technique is useful for material up to 50,000 years. Fluctuations of C14 in the atmosphere can affect results so dates are calibrated against dendrochronology. Radiocarbon dates are calibrated to calendar years. Dates are reported in radiocarbon years or Before Present. Before Present refers to dates before 1950. The introduction of massive amounts of C14, due to atomic bomb and surface testing of atomic weapons, has widely increased the standard deviation on all dates after A.D. 1700 causing these dates to be unreliable. Accelerated mass spectrometry can more accurately measure C14 with smaller samples and can date materials to 80,000 years.
Scope and Content
Sub sub series contains radiocarbon dates from: Atkinson site and Flintstone Hill.
Name Access
North Lauder locale Radiocarbon Report I
Subject Access
Archaeology North Lauder locale North Lauder locale Radiocarbon Report I
Documents

2.5.1_Atkinson_RC14_TO-11882.pdf

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North Lauder locale Radiocarbon Report 2

http://archives.brandonu.ca/en/permalink/descriptions12328
Part Of
RG 7 Beverley Nicholson fonds
Description Level
Sub sub series
GMD
multiple media
Date Range
1997-2000
Accession Number
1-2010
Part Of
RG 7 Beverley Nicholson fonds
Description Level
Sub sub series
Series Number
2.5.2
Accession Number
1-2010
GMD
multiple media
Date Range
1997-2000
Physical Description
2 pages
Material Details
Radiocarbon date reports have been scanned in multi-page PDF files.
History / Biographical
North Lauder Radiocarbon Date report by IsoTrace Laboratory for Atkinson site #TO-10640. Radiocarbon dating The technique of radiocarbon dating was developed by Willard Libby and his colleagues at the University of Chicago in 1949. Radiocarbon dating is used to estimate the age of organic remains from archaeological sites. Organic matter has a radioactive form of carbon (C14) that begins to decay upon death. C14 decays at a steady, known rate of a half life of 5,730 years. The technique is useful for material up to 50,000 years. Fluctuations of C14 in the atmosphere can affect results so dates are calibrated against dendrochronology. Radiocarbon dates are calibrated to calendar years. Dates are reported in radiocarbon years or Before Present. Before Present refers to dates before 1950. The introduction of massive amounts of C14, due to atomic bomb and surface testing of atomic weapons, has widely increased the standard deviation on all dates after A.D. 1700 causing these dates to be unreliable. Accelerated mass spectrometry can more accurately measure C14 with smaller samples and can date materials to 80,000 years.
Scope and Content
Sub sub series contains radiocarbon dates from: Atkinson site and Flintstone Hill.
Name Access
North Lauder locale Radiocarbon Report 2
Subject Access
Archaeology North Lauder locale North Lauder locale Radiocarbon Report 2
Documents

2.5.2_Atkinson_RC14_TO-10640.pdf

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North Lauder locale Radiocarbon Report 3

http://archives.brandonu.ca/en/permalink/descriptions12329
Part Of
RG 7 Beverley Nicholson fonds
Description Level
Sub sub series
GMD
multiple media
Date Range
1997-2000
Accession Number
1-2010
Part Of
RG 7 Beverley Nicholson fonds
Description Level
Sub sub series
Series Number
2.5.3
Accession Number
1-2010
GMD
multiple media
Date Range
1997-2000
Physical Description
1 page
Material Details
Radiocarbon date reports have been scanned in multi-page PDF files.
History / Biographical
North Lauder Radiocarbon Date report by IsoTrace Laboratory for Atkinson site #TO-13365. Radiocarbon dating The technique of radiocarbon dating was developed by Willard Libby and his colleagues at the University of Chicago in 1949. Radiocarbon dating is used to estimate the age of organic remains from archaeological sites. Organic matter has a radioactive form of carbon (C14) that begins to decay upon death. C14 decays at a steady, known rate of a half life of 5,730 years. The technique is useful for material up to 50,000 years. Fluctuations of C14 in the atmosphere can affect results so dates are calibrated against dendrochronology. Radiocarbon dates are calibrated to calendar years. Dates are reported in radiocarbon years or Before Present. Before Present refers to dates before 1950. The introduction of massive amounts of C14, due to atomic bomb and surface testing of atomic weapons, has widely increased the standard deviation on all dates after A.D. 1700 causing these dates to be unreliable. Accelerated mass spectrometry can more accurately measure C14 with smaller samples and can date materials to 80,000 years.
Scope and Content
Sub sub series contains radiocarbon dates from: Atkinson site and Flintstone Hill.
Name Access
North Lauder locale Radiocarbon Report 3
Subject Access
Archaeology North Lauder locale North Lauder locale Radiocarbon Report 3
Documents

2.5.3_Atkinson_RC14_TO-13365.pdf

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North Lauder locale Radiocarbon Report 4

http://archives.brandonu.ca/en/permalink/descriptions12330
Part Of
RG 7 Beverley Nicholson fonds
Description Level
Sub sub series
GMD
multiple media
Date Range
1997-2000
Accession Number
1-2010
Part Of
RG 7 Beverley Nicholson fonds
Description Level
Sub sub series
Series Number
2.5.4
Accession Number
1-2010
GMD
multiple media
Date Range
1997-2000
Physical Description
pages 5-7
Material Details
Radiocarbon date reports have been scanned in multi-page PDF files.
History / Biographical
North Lauder Radiocarbon Date report by Beta Analytic Inc. for Flintstone Hill #109529 and #109530. Radiocarbon dating The technique of radiocarbon dating was developed by Willard Libby and his colleagues at the University of Chicago in 1949. Radiocarbon dating is used to estimate the age of organic remains from archaeological sites. Organic matter has a radioactive form of carbon (C14) that begins to decay upon death. C14 decays at a steady, known rate of a half life of 5,730 years. The technique is useful for material up to 50,000 years. Fluctuations of C14 in the atmosphere can affect results so dates are calibrated against dendrochronology. Radiocarbon dates are calibrated to calendar years. Dates are reported in radiocarbon years or Before Present. Before Present refers to dates before 1950. The introduction of massive amounts of C14, due to atomic bomb and surface testing of atomic weapons, has widely increased the standard deviation on all dates after A.D. 1700 causing these dates to be unreliable. Accelerated mass spectrometry can more accurately measure C14 with smaller samples and can date materials to 80,000 years.
Scope and Content
Sub sub series contains radiocarbon dates from: Atkinson site and Flintstone Hill.
Name Access
North Lauder locale Radiocarbon Report 4
Subject Access
Archaeology North Lauder locale North Lauder locale Radiocarbon Report 4
Documents

2.5.4_FSH_RC14_Beta-109529_109530.pdf

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North Lauder locale Radiocarbon Report 6

http://archives.brandonu.ca/en/permalink/descriptions12332
Part Of
RG 7 Beverley Nicholson fonds
Description Level
Sub sub series
GMD
multiple media
Date Range
1997-2000
Accession Number
1-2010
Part Of
RG 7 Beverley Nicholson fonds
Description Level
Sub sub series
Series Number
2.5.6
Accession Number
1-2010
GMD
multiple media
Date Range
1997-2000
Physical Description
1 page
Material Details
Radiocarbon date reports have been scanned in multi-page PDF files.
History / Biographical
North Lauder Radiocarbon Date report by Beta Analytic Inc. for Flintstone Hill #109900. Radiocarbon dating The technique of radiocarbon dating was developed by Willard Libby and his colleagues at the University of Chicago in 1949. Radiocarbon dating is used to estimate the age of organic remains from archaeological sites. Organic matter has a radioactive form of carbon (C14) that begins to decay upon death. C14 decays at a steady, known rate of a half life of 5,730 years. The technique is useful for material up to 50,000 years. Fluctuations of C14 in the atmosphere can affect results so dates are calibrated against dendrochronology. Radiocarbon dates are calibrated to calendar years. Dates are reported in radiocarbon years or Before Present. Before Present refers to dates before 1950. The introduction of massive amounts of C14, due to atomic bomb and surface testing of atomic weapons, has widely increased the standard deviation on all dates after A.D. 1700 causing these dates to be unreliable. Accelerated mass spectrometry can more accurately measure C14 with smaller samples and can date materials to 80,000 years.
Scope and Content
Sub sub series contains radiocarbon dates from: Atkinson site and Flintstone Hill.
Name Access
North Lauder locale Radiocarbon Report 6
Subject Access
Archaeology North Lauder locale North Lauder locale Radiocarbon Report 6
Documents

2.5.6_FSH_RC14_109900.pdf

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12 records – page 1 of 1.