The Executive Committee is a standing committee of the Brandon University Board of Governors that meets regularly two weeks prior to the regular Board meeting. Its membership consists of: Chair of the Board of Governors; Vice-Chair of the Board of Governors; President of the University; Secretary of the Board of Governors; Treasurer of the Board of Governors; Student Representative from the Board of Governors; and Senate Representative from the Board of Governors. The Vice-President (Academic and Research) and the Vice-President (Administration and Finace) act as resource persons. Elections for the Executive Committee take place at the Board of Governors' August meeting each year.
Specific responsibilities of the Executive Committee include: setting the agenda for each regular and special meeting of the Board of Governors; reviewing relevant matters coming before the Board of Governors; acting as a consultative body to the President of the University; dealing with matters delegated by the Board of Governors; referring items to appropriate standing committees of the Board of Governors; acting with the full authority of the Board in situations requiring immediate action prior to the next regular meeting of the Board. The Executive Committee also reviews and recommends policies governing university finance and long-range planning. The Executive of the Board reports to the Board of Governors.
Scope and Content
Sub-series consists of records created by the Executive of the Brandon University Board of Governors. It has been divided into three sub sub series: (1) Board Executive Minutes; (2) Board Executive Correspondence; and (3) Board Executive Agendas.
Notes
History/Bio information taken from Board of Governors By-law No. 11 - Committees of the Board of Governors, Section III - Executive Committee (revised November 23, 2006).
Storage Location
RG 6 Brandon University fonds
Series 2: Board of Governors
2.2 Board Executive
The Brandon College and Brandon University Art Exhibition Committee was active from 1960 to 1972. The Committee was established to promote the visual arts in Brandon through education and to sponsor exhibitions featuring the work of local artists.
Custodial History
The records were assembled by Robert Inch of the Brandon University Extension Office and Professor D.V. Reilly, who taught art through the Faculty of Education at Brandon University. They were donated to the McKee Archives in 1997.
Scope and Content
The sub-series contains records of past exhibitions, minutes and correspondence of the Brandon University Art Exhibition Committee. Sub-series also contains personal files on some artists consisting of correspondence and information pertaining to exhibitions of their work. There are also extensive files on past exhibits including advertising, correspondence, newspaper clippings, publications and files concerning local affiliated art clubs, such as the Student Camera Club at Brandon University.
1.5 cm textual records; 25 photographs various sizes; 3 strips of negatives
Physical Condition
Very good
History / Biographical
William Robert Morrison was born January 26, 1942, in Hamilton, Ontario. He graduated from McMaster University with a B.A. (Hons. English and History) in 1963, and an M.A. (History) in 1964. He completed his Ph.D. in Canadian History at the University of Western Ontario in 1973.
From 1964-1965, Morrison was a secondary school teacher in London, Ontario and from 1968-1969, he was a historical researcher at the National Historic Sites Service in Ottawa. Morrison began his career at Brandon University in 1969. During his time there he taught in the History Department and was also a member of the Knowles-Douglas Commission (1986-1987), a member of the Brandon University Senate (six years), Chairman of the Scholarship Committee (three years), a member of the Senate Executive Committee (two years), Chairman of the Athletic Directorate (three years), a member of the Board Budget Committee (two years), the originator of the English Proficiency Test for Graduating Students, a member of various Arts Faculty Committees, a member of the BUFA Executive (three years) and Chairman of the Department of History (three years). In addition, Morrison also played in the Brandon University Wind Ensemble, was a member of the Executive of the Western Manitoba Science Fair (four years) and a member of the Executive Committee of the Manitoba Record Society (two years). Morrison resigned from Brandon University in August 1989 to accept a position at Lakehead University.
At Lakehead University, Morrison was a professor of history at the Centre of Northern Studies. He left Thunder Bay in 1999 and moved to Prince, George, British Columbia to teach at the University of Northern British Columbia. Throughout his career he has also taught courses at the University of Victoria and Duke University. In addition, Morrison was the founding Dean of Research and Graduate Studies at UNBC. Morrison's research interests include Northern Canadian history, First Nations and Canadian-American relations. He is the author and co-author of twelve books and many book chapters and journal articles, most of them on the history of Northern Canada. In particular, beginning at Brandon University, Morrison has develped and maintained a close academic partnership with Kenneth S. Coates, and together they have published a number of works. Morrison has also served as the co-editor of the "Northern History Newsletter" and as a member of the advisory board of the "Northern Review."
William R. Morrison is married, with four children, and as of January 2006, living in Prince George, British Columbia.
Custodial History
Some the the material in this fonds was in the possession of the Brandon University Library prior to its possession by Dr. Morrison for use in the production of My Dear Maggie. The materials created by Dr. Morrison were in his possession until their donation to the McKee Archives in July 2002.
Scope and Content
The Morrison fonds is a result of the research conducted by Morrison in the Shellmouth region of Manitoba between 1986 and 1991 for the production of "My Dear Maggie." The fonds consists primariloy of pictures, homesteading documentation, and personal correspondence. Pictures include memberts of the Wallace family, their homestead and the Shellmouth area. Textual records consist of correspondence between Andrew Wallace and individuals at Brandon College ca. 1941, regarding the donation of the Wallace letters to the Brandon College Library. Photocopies of homesteading information from 1881 to 1905, as well as corresondence between Morrison and residents of the Shellmouth area regarding information about the Wallace family, are also included. Finally, there is extensive correspondence to and from Morrison in connection with the publication of "My Dear Maggie: Letters from a Western Manitoba Pioneer," a production of edited letters from the William Wallace fonds.
Notes
Information in the Location of Originals field, the History/Bio field, the Scope & Content field and the Arrangement field was taken from the William R. Morrison fonds finding aid written by Katie Pollock (2005).
There are photocopies of homsteading documentation, as well as letters to Maggie Wallace from William Wallace once he arrived in Canada. The orignals of the letters to M. Wallace can be found in the William Wallace fonds, while the originals of the homsteading documentation can likely be found in either the William Wallace fonds or through Archives Canada.
Storage Location
MG 3 Brandon University Teaching and Administration
1.5 William R. Morrison
Related Material
Additional records related to William R. Morrison are located in RG 6, series 7, sub sub series 7.1.1 (Dean of Arts). Other records relating to the Wallace family of the Shellmouth region can be found in the William Wallace fonds located in the McKee Archives (47-1997).
Arrangement
The fonds is divided into two files. The first file contains information that Morrison accumulated in his research for "My Dear Maggie," including pictures, as well as correspondence between Morrison and members of the Shellmouth community. The second file also contains correspondence between Morrison and members of the Shellmouth community, but consists primarily of communication between Morrison and a number of publishing companies.
File consists of reference materials regarding university libraries in Ontario gathered for the purpose of planning the use and/or expansion of the John E. Robbins Library at Brandon University. It includes two photographs of Carelton University Library.
Storage Location
RG 6 Brandon University fonds
Series 4: Office of the Vice-President
4.2 Office of the Vice-President (Administration &Finance)
Box 1
File consists of a request for approval in principle for financial assistance for special capital project to the Universities Grants Commission, correspondence and a copy of the grading design.
Storage Location
RG 6 Brandon University fonds
Series 2: Board of Governors
2.6 Board Projects
Box 1
File consists of a request for approval in principle and a request for final approval for financial assistance for special capital project to the Universities Grants Commission, correspondence, notes and a blueprint.
Storage Location
RG 6 Brandon University fonds
Series 2: Board of Governors
2.6 Board Projects
Box 1
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.
60 photographs (b/w) and 18 negatives; 3 cm textual records
History / Biographical
Rubina Isabella Miles (née McGregor) was born October 9th, 1909, in Maple Creek, Saskatchewan, the only child of Kate (née Rowe) and William McGregor. Her father, William Thom McGregor was a native of Scotland who, before coming to Canada, travelled to Australia and New Zealand, and served in the Boer War. Ruby Miles and her parents migrated to Australia in 1921. In 1925, the family moved to Papua New Guinea where Mr. McGregor was employed as Head Stockman on the Giligili Estate, part of the Commonwealth Copra Company. The family returned to Canada in 1929. In 1940, Ruby married Leonard "Len" Miles, a native of Moose Jaw, Saskatchewan. Following the Second World War, they settled in Brandon, Manitoba. Ruby spent her adult life as a homemaker. She died in April 2003.
Custodial History
The records came into Ruby Miles' possession through her husband (correspondence while he was overseas) and through the death of various family members. Following the death of Ruby Miles, the collection was donated to the S.J. McKee Archives by Errol Black, the executor of her estate.
Scope and Content
Collection includes c. 15 letters from Kate McGregor, to her parents Mr. and Mrs. A.A. Rowe of Brandon, Manitoba. The letters were written in the years 1925-1929, when Mrs. McGregor and her family were living in Papua New Guinea. Collection also includes photographs and photographic negatives containing images of the Giligili Estate in New Guinea. Collection contains correspondence with Len Miles during his service overseas in the Second World War, as well as Len Miles' service record, death certificate and various memorabilia from his time in military service. Finally, the collection includes various news clippings, documents and correspondence received or retained by Ruby Miles.
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 #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.
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.
