2.4 m textual records; c. 5 photographs; 1 minute book (measuring 1"x 9"x 14")
History / Biographical
The Brandon Trades and Labour Council was established in 1906, as an affiliate of the Trades and Labour Congress of Canada. The original Council contained thirteen locals, including those of railway workers, sheet metal workers, plumbers and steam fitters, bricklayers, carpenters and joiners, cigar makers, printers, and barbers. By 1912, the Council contained twenty four locals. The Council's principal function was to advance the corporate interests of labour within the framework of a largely unregulated capitalism. After 1955, the Council was affiliated with the Canadian Labour Congress, which was created through a merger of the Trades and Labour Congress of Canada and the Canadian Congress of Labour.
Custodial History
Fonds remained in possession of Brandon and District Labour Council prior to donation to the S.J. McKee Archives.
Scope and Content
Fonds consists of financial and administrative records of the Brandon and District Labour Council. Records also include collective agreements, correspondence, publications of the Labour Council and affiliated unions, some union local minutes, newspaper clippings, petitions, and various miscellaneous files. Fonds also includes a minute book for the Council (1971-1985) and two union charters.
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.
This record group was artifically created in January 2007 by Tom Mitchell and Christy Henry of the McKee Archives.
Scope and Content
The record group consists of various fonds and collections concerned with the political, cultural, social, and educational life of western Manitoba. See the Subject Access field for a list of titles.
30 photographs -- 25 at 3.5" x 8" (color and b/w); 5 at 8"x10" (b/w); 3 magnates; 1 plaque (8 x 3 cm)
History / Biographical
The chancellor is the titular head of the university and confers all degrees. Where possible the Chancellor also attends official functions on behalf of the University and may take on special projects keeping with the goals of the University. According to "The Brandon University Act 1998," there is to be a chancellor of the university elected by the senate for a term of three years; the chancellor continues to hold office after his or her term expires until re-elected or until a successor is elected; the chancellor is eligible for re-election; and if a vacancy occurs in the office of chancellor before the end of the term, the successor elected to replace the incumbent chancellor is to hold office for the remainder of the incumbent's term.
BRANDON UNIVERSITY CHANCELLORS:
MAITLAND B. STEINKOPF (1967-1970)
Maitland B. Steinkopf (September 10, 1912 - 1970) was born in Winnipeg, Manitoba. He was educated at the University of Manitoba, and was called to the Manitoba Bar in December 1936. He served in the Canadian armed forces in World War Two, as a Private in the Queen's Own Cameron Highlanders and a Lieutenant Colonel with the R.C.O.C. He later founded the Canada West Shoe Manufacturing Company, and was a president of several companies including Bonded Investments Ltd., L.H. Packard Co. Ltd., Dayton Shoe Mfg. Col. Ltd., and the Tel Aviv Hilton Hotel. Steinkopf was a member of the Canada Israel Development Corporation, and served as chairman of State of Israel bonds in Manitoba. He was also an honorary counsel with the government of Czechoslovakia until 1948. Prior to his election, he assisted the Roblin government in land-development for cultural projects.
Steinkopf was elected to the Manitoba legislature in the 1962 provincial election as a member of Dufferin Roblin's Progressive Conservative government and was appointed to cabinet on June 12, 1963, as Provincial Secretary and Minister of Public Utilities. He later resigned his position and his seat in the legislature as a result of being implicated in a controversial land assembly payment. He was re-elected and re-appointed to the Cabinet in 1964. Steinkopf did not run for re-election in 1966. He later served as chair of the Manitoba Centennial Centre Corporation, which established a Maitland Steinkopf Youth Fund in 1972 for students in the arts.
Steinkopf married Helen Katz of Chicago and they had six children. He died suddenly in 1970 of a heart attack.
THE HONOURABLE STANLEY HOWARD KNOWLES (November 1970 - November 1990)
Stanley Knowles (June 18, 1908 - June 9, 1997) graduated from Brandon College in 1930, received his B.Div. from the University of Winnipeg in 1933, and was ordained by the United Church of Canada. Until 1940, he was a minister in Winnipeg churches. He organized public forums and created radio programs on social themes. He spoke for the Co-operative Commonwealth Federation (CCP), becoming its chairman, then provincial secretary, for Manitoba.
In 1942, Knowles was elected to the House of Commons as MP for Winnipeg North Centre. He was an MP from 1942 until 1958, was re-elected in 1962 and served until 1984. Throughout his political career, he struggled for a decent life and income for older people. He was instrumental in amending the industrial relations bill so that legal strikes did not interfere with employee pension rights, eliminating the "means test" from the Old Age Security Act and indexing the Canadian Pension Plan and Civil Security Pensions. He played a major role in creating the New Democratic Party in 1961, presiding over the founding convention. He was the Deputy Leader of that party from 1962-84.
In 1970, Knowles became Chancellor of Brandon University and in 1990, was designated Chancellor emeritus. He became an honorary member of Canada's Privy Council in 1979, and was awarded the Order of Canada in 1984.
THE HONOURABLE JUDGE RONALD D. BELL (1990 - October 1996)
Ronald Dean Bell was born in Deloraine, Manitoba and graduated from Brandon College in 1951. He received his law degree from the University of Manitoba in 1955. Bell worked for several years as a solicotor for the Department of National Revenue, Taxation Division and as a partner in the Calgary law firm Fenerty & Co. He was appointed Queen's Counsel in 1976, and in 1978, he formed Bell Felesky Flynn, a law practice focusing on taxation. In 1991, Bell was appointed Judge of the Tax Court of Canada.
Throughout his distinguised career, Bell has continued to support Brandon University. In addition to his duties as Chancellor, he has also served on various BU boards and worked tirelessly to promote the institution. He also made siginificant financial contributions to improve physical structures, programs and student scholarships, including the establishment of the R.D. Bell Schoalrship and the R.D. Bell String Scholarships. The R.D. Bell Hall in the Queen Elizabeth II music building was named in his honour, as was the Bell Tower atop the orginal Brandon College building, which is now part of Clark Hall. Justice Bell recieved an Honorary Degree from Brandon University at the spring 2006 convocation and is presently Chancellor emeritus.
DR. KEVIN KAVANAGH (November 1996 - October 2002)
Born and raised in Brandon, Kevin Kavanagh graduated from Brandon Collegiate Institute in 1950, and completed his commerce degree at the University of Manitoba in 1953. That same year he joined the Group Insurance Division of the Great-West Life Assurance Company. From 1978-1992, he served as president and CEO of that organization. During his career, Kavanagh has also served on various provincial and national boards, including the Royal Winnipeg Ballet, National Leasing Group, Winnipeg Airports authority, the Conference Board of Canada, the Crown Corporations Council and the Canadian Life and Health Insurance Association Inc. Kavanagh was also a member of the Roblin Commission. In 1996, he was named the fourth Chancellor of Brandon University, and in addition to his duties as Chancellor, he has been involved with the university as a member of the Brandon University Foundation and as a member of the Corporate Challenge Campaign. In September 2006, the courtyard between Clark Hall and the George T. Richardson building was renamed The Kavanagh Courtyard in honour of Kavanagh and his wife in recognition of their vision and leadership with Brandon University and their dedication to the advancement of post-secondary education.
In 1963, Kavanagh married his wife Els, and together they had two children: Jennifer and Sean. At present, (July 2007), Kevin Kavanagh is Chancellor Emeritus of Brandon University.
THE RIGHT HONOURABLE EDWARD R. SCHREYER (November 1, 2002 - present)
Edward Schreyer was born on December 21, 1935 in Beausejour, Manitoba. He studied at United College, St. John's College and the University of Manitoba, receiving a Bachelor of Pedagogy in 1959, a Bachelor of Education in 1962, a Master of Arts in International Relations and a second Master of Arts in Economics in 1963. From 1962 to 1965, Schreyer taught International Relations at St. Paul's College. On June 30, 1960, Schreyer married Lily Schulz. The couple had two daughters, Lisa and Karmel, and two sons, Jason and Tobin.
Schreyer was elected to the Legislative Assembly of Manitoba in 1958, as a member of the Manitoba Co-operative Communwealth Federation, representing the rural consituency of Brokenhead. In 1965 he resigned to run successfully for the House of Commons. In 1969, Schreyer returned to provincial politics as leader of the New Democratic Party of Manitoba. He led his party to victory in the 1969 provincial election, and served as Premier of Manitoba from 1969 until 1977.
Schreyer was appointed Governor General in 1979 by Pierre Trudeau. That same year, he was made a Companion of the Order of Canada along with his wife Lily Schreyer. As Governor General, Schreyer championed women's issues, the environment, and official bilingualism. He established the Governor General's Award in Commemoration of the "Persons Case," instituted the Governor General's Conservation Awards (1981), and presided over the first Governor General's Canadian Study Conference. Schreyer retired as Governor General in 1984.
Later in 1984, Schreyer was sworn into the Privy Council and was subsequently appointed Canadian High Commissioner to Australia, Papua New Guinea, and the Solomon Islands, and as ambassador to Vanuatu. He held those positions until 1988. Returning to Manitoba, Schreyer worked as a national representative of Habitat for Humanity. In 2006, he was acclaimed as the NDP candidate in Selkirk-Interlake for the 2006 federal election.
Edward Schreyer became Chancellor of Brandon University in November 2002, and his term was extended in 2005 until October 31, 2008.
HENRY CHAMP (November 1, 2008 - October 31, 2011)
Henry Champ was born in Brandon, Manitoba in 1939. He attended Brandon College in 1957 and 1958.
Scope and Content
At present (July 2007), the series consists of the Stanley Knowles collection (accession 61-1997).
Notes
Administrative information in the History/Bio field was taken from "The Brandon University Act (1998)" at: http://web2.gov.mb.ca/laws/statutes/1998/c04898e.php (December 2005) and from: http://alumni.brandonu.ca/alumniNews/images/BU_Alumni_News05.pdf. Biographical information for Maitland Steinkopf was taken from http://en.wikipedia.org/wiki/Maitland_Steinkopf (December 2005). Biographical information for Stanley Knowles was taken from: http://www.mcmaster.ca/ua/alumni/gallery/G129664.htm (December 2005) and from: http://en.wikipedia.org/wiki/Stanley_Knowles (December 2005). Biographical information for Bell was taken from Brandon University calendars and the spring/summer 2006 issue of Alumni News. Biograpical information for Kavanaugh was taken from Brandon University calendars. Biographical information for Edward Schreyer was taken from: http://en.wikipedia.org/wiki/Edward_Schreyer (December 2005).
See RG 6, sub-series 4.1 Vice-President (Academic and Research) and 4.2 Vice-President (Administration and Finance) for history/bio information.
Scope and Content
Series consists of records generated and collected by the Office of the Vice-President in the course of performing its functions. The fonds has been divided into two sub-series, including: (1) Vice-President (Academic and Research); and (2) Vice-President (Administration and Finance).
Notes
A portion (2.3 m) of the records in this series are unprocessed.
John C. Cousins was the son of Thomas Cousins (b. August 17, 1882 in Truro, Nova Scotia - d. March 5, 1914) and Mary Margaret Craig (b. April 14, 1824 - d. April 25, 1903). He married Eunice Eliza Nixon from London Township, County of Middlesex, Ontario. Together they had three children: Eunice M., Eric O. and Kathleen. J.C. Cousins was Reeve of the Rural Municipality of Daly from 1905 to 1910 and Assessor for the Town of Rivers from 1931-1938.
Custodial History
Record was accessioned in 2007 by the McKee Archives. Prior custodial history unknown.
Scope and Content
This document is a rambling memoir of John C. Cousins' recollections of life in the Rural Municipality of Daly from the settlement era in the early 1880s, through to the 1940s. He touches on various themes, including: his family history; the activities of the R.M. of Daly and his role as Reeve; the history of school districts in the municipality (lists names of first teachers and early students); the history of churches in the municipality; tragedies in the municipality; lists members of the Council of the municipality for the years 1885-1946; and the devastating impact of the Spanish Influenza on Aboriginal people in the municipality.
In addition, the memoir includes documentary records, such as minutes and copies of letters. There are also many photographs of both events and individuals (virtually all of the photographs are labelled and names are provided). The memoir goes beyond a simple recounting of facts. Cousins is discursive and thoughtful, often making references to developments happening in other parts of North America and Canada. There is also a link to the Maritimes, from which his family originated.
Fonds consists of correspondence, newsclippings, reminiscences, historical information about Grand Valley, name and address lists for students and teachers, invitations to Grand Valley School District reunions (1935 and 1968), the program for the dedication ceremonies and reunion picnic (1968), and the guest book for the 1968 reunion and cairn dedication. The latter includes 3 photographs.
The Crown Protestant School District was founded in 1883, in the municipality of Whitewater, Manitoba. It became the Crown School District following school reform in Manitoba in 1890. The School District provided schooling for children in the Elgin, Fairfax, Heaslip and Minto communities. In 1930, the district was replaced with the creation of separate school districts for Elgin, Fairfax, and Lily.
Custodial History
This fonds was accessioned by the McKee Archives in 1997. Prior custodial history is unknown.
Scope and Content
Fonds contains minute books (1883-1930), financial records (1884-1917), attendance registers (1892 -1906), tax records for the District (1918-1930), and documents concerning the disestablishment of the Crown School Division.
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.
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.
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.
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.
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.
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.
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.
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.
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.
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.
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.
