The Canadian Union of Public Employees came into existence in September 1963, during a convention in Winnipeg when The National Union of Public Employees and the National Union of Public Service Employees merged. In 1964, the Manitoba Division of CUPE (now CUPE Manitoba) held its founding convention in The Pas. At that time, there were 12 affiliated local unions and a total membership of 1,300. The Canadian Union of Public Employees is Canada's largest union. Public service employees formed CUPE to protect their rights, to negotiate wages and working conditions, and to achieve dignity in the workplace.
Custodial History
Fonds was in the possesssion of the Brandon CUPE Office until its donation to the S.J. McKee Archives in 1995.
Scope and Content
Fonds contains general administrative files of the CUPE including agreements, newspaper clippings, correspondence, and convention records. In addition, fonds includes records for many CUPE locals in southwestern and north-central Manitoba. These includes files for each local containing agreements, lists of officials, correspondence and financial records. An extensive body of records dating from 1956 exists for CUPE local #69. This local began its existence as the Brandon Civic Employees Federal Union formed in April 1919.
Inter-Universities North (IUN) began under a mandate established by the Committee of Presidents of Universities in Manitoba to coordinate delivery of degree credit courses from all three Manitoba uniersities to students living in communities north of the 53rd parallel.
Emily Sawicki became the first person to complete an entire degree program exclusively in the north through IUN in 1979.
Originally the Office of Extension was responsible for the logistics of compiling lists of candidates, arranging interviews and identifying instructors. Student Services provided study skills kits and the Library provided a library skills kit. Library services for IUN students have been available from Brandon University since the early 1970s.
The five First Year by Distance Education (FYDE) communities were Flin Flon, The Pas, Thompson, Dauphin and Russell.
Notes
History/Bio information taken from Campus News - April/May 1992
Storage Location
RG 6 Brandon University fonds
Series 5: Office of the Registrar
The Southwest Branch of the Manitoba Genealogical Society was established in 1978. The Branch was formed following a meeting with members of the Manitoba Genealogical Association formed in 1977. The organization was created to assist individuals interested in doing genealogical research through the provision of genealogical data and archival resources. Since its creation the Southwest Branch has also issued a newletter and published a series of cenusus summaries based on the 1901 Canadian census.
Custodial History
These records were donated to the McKee archives in 1990 by J.D. Wall on behalf of the Southwest Branch of the Manitoba Genealogical Society.
Scope and Content
Fonds includes transcripts of the records transcribed from cemetery headstones located in cemeteries throughout southwestern Manitoba. Each transcript includes details about the cemetery records and all details including names, dates, and inscriptions from each headstone. The collection includes a "Cemetery Transcript List" detailing those cemeteries for which transcripts exist. Transcripts include those for the following cemeteries: Alexander, Birdtail Sioux Indian Reserve, Blenheim Church, Glencoe, Boissevain, Brandon, Brandon Hills Church Cemetery, Brookdale, Carberry District, Coultervale, Elgin, Elkhorn, Humesville, Lauder, Kerfoot (Gregg Cemetery), Icelandic Gravesite (Tilston), History of Kingsley Cemetery near Somerset, Madford Cemetery, Old Medora Cemetery, Melgund, Millford Cemetery, Noble Cemetery, Methven , Millord Cemetery, Roseville Anglican Church Cemetery, St. Savior's Anglican Church, St. George's Anglican Church, Rounthwaite, Souris (Glenwood Cemetery), Skalholt, Wellwood, Woodville (Lund, Kola, Bennett, Two Creeks), Patterson (near Nesbitt), Sparling (near Justice), Tilston (near Sinclair), Royal Canadian Air Force Memorial (20 miles north of Rivers).
The Brandon Art Club was founded in November 1907, and operated in an art studio on the top floor of the Brandon College Women's Residence. The club appears to have been the creation of Miss. H. Hancock, who became the Director of the Department of Art at Brandon College c. 1907. The club moved to larger facilities made available at the First Methodist Church; the organization remained there until sometime during the Great War when the club relocated to St. Paul's Presbyterian Church and then in 1921, to the Prince Edward Hotel. The club's first public art exhibitions were held at the Prince Edward Hotel. Art classes were held for the first time in 1928. In 1968, the Brandon Art Club merged with the Allied Arts Center, which had been formed in 1959. The Allied Arts Center was located at 1036 Louise Avenue. In April 1984, the Allied Arts Center was moved to new facilities at the Arts Center of Western Manitoba located at 638 Princess Avenue. In 1989, it was renamed the Art Gallery of Southwestern Manitoba, and began to function as a "professional, regional art gallery." The Art Gallery of Southwestern Manitoba relocated to 2-710 Rosser Ave. c. 2001.
Custodial History
These records were created at different times between 1907 and 1993, and remained in the possession of the administration of the above mentioned organizations until May 2001, when they where donated to the McKee Archives.
Scope and Content
Fonds contains administrative records, minutes, personal files, correspondence, newsletters, photographs, summaries of collections and exhibits, scrapbooks, programs, submitted papers, and other miscellaneous records. All are a record of the growth and evolution of the Art Club, its administration, and of the art community in Brandon.
The A.E. McKenzie Company fonds (RG 3 MG 1, 1.3) located in the McKee Archives contains some records, primarily correspondence and minutes, relating to the Brandon Allied Arts Council.
ARCH 2: North Lauder Locale
The North Lauder locale has a long archaeological and geological history that is important for understanding the forces that shaped the region. Archaeological research in the locale shows that the area has been occupied by humans for at least the past 6,500 years. Environmental forces provided an area of diverse resources that attracted early peoples.
Environment of the Lauder Sandhills
The North Lauder locale is part of the greater Lauder Sandhills area. The glaciers that covered this region began to recede approximately 11,000 years ago leaving a large lake known as glacial Lake Hind. The Souris River, the Lauder Sandhills and the Oak Lake Aquifer are remnants of the environmental and geological forces that shaped the region.
The Lauder Sandhills region is characterized by a landscape of sand sheets and stabilized sand dunes interspersed with a variety of wetlands. This complex topographic and hydrological situation favoured the development of an island mosaic of mixed forest, wetland and meadow, surrounded by mixed grass prairie. The result was a large, isolated ecotone which provided a rich variety of subsistence resources for hunter-gatherers.
Research in the Lauder Sandhills
Archaeologists from Brandon University have been conducting research in the Lauder Sandhills since 1991. Research in the North Lauder locale has focused on the Atkinson site, a 6,500 year old hunter-gatherer site and Flintstone Hill.
The Atkinson site
The Atkinson site is one of the oldest excavated sites in Manitoba and has been Radiocarbon dated to 6,500 years before present. The Atkinson site is located on the bank of the Souris River and was discovered when a hearth (fire pit) was seen eroding out of the bank. Based on the date of the site and the kind of lithics (stone tools) present it is considered a Gowen occupation. The Atkinson site is evidence that bison hunters were active on the northern plains at a very early date. Similar sites have also been found on the High Plains in the U.S. and are referred to as the Mummy Cave Complex.
The Atkinson Site is of great importance as it is the first undisturbed site of this type to be excavated in Manitoba and extends the range of these sites south and east from the type-sites in central Saskatchewan.
Flintstone Hill
The geomorphology of the glacial Lake Hind Basin over the past 11,000 years is known primarily through the study of a cut bank along the Souris River. Flint Stone Hill contains the most complete stratigraphic record for the post-glacial period on the northern plains. The site has been extensively studied by geoarchaeologists, geologists and paleoenvironmentalists over many years and their findings have contributed to our understanding of the region.
The North Lauder locale Borden designations of Atkinson site DiMe-27 and Flintstone Hill site DiMe-26.
Borden System
Archaeological sites in Canada are identified by the Borden system, which is a uniform site designation system. The country is divided into grids based on latitude and longitude in blocks of 10 x 20 minutes. The first 4 letters indicate the block and the following numbers indicate the actual site. For example the area of the Lauder Sandhills in southwestern Manitoba is identified by the letters DM and the North Lauder locale within that area is DiMe. The Atkinson site is DiMe-27 and the Flintstone Hill site DiMe-26. As new sites are discovered they will be numbered sequentially.
Scope and Content
The Series has been divided into two sub-series, including (1) Atkinson site DiMe-27 and Flintstone Hill site DiMe-26.
Radiocarbon date reports have been scanned in multi-page PDF files.
History / Biographical
The North Lauder locale has a long archaeological and geological history that is important for understanding the forces that shaped the region. Archaeological research in the locale shows that the area has been occupied by humans for at least the past 6,500 years. Environmental forces provided an area of diverse resources that attracted early peoples.
Archaeologists from Brandon University have been conducting research in the North Lauder locale that has focused on the Atkinson site, a 6,500 year old hunter-gatherer site and Flintstone Hill.
The geomorphology of the glacial Lake Hind Basin over the past 11,000 years is known primarily through the study of a cut bank along the Souris River. Flintstone Hill contains the most complete stratigraphic record for the post-glacial period on the northern plains. The site has been extensively studied by geoarchaeologists, geologists and paleoenvironmentalists over many years and their findings have contributed to our understanding of the region.
Radiocarbon dates were obtained from the Atkinson site and Flintstone Hill.
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: the Atkinson site and Flintstone Hill.
File consists of copies of Impacte materials, including a report and evaluation of the first 18 months, correspondence, minutes for the ad hoc committee of the Indian-Metis Teacher Preparation and a report from a meeting with Dr. Halamandaris.
Storage Location
RG 6 Brandon University fonds
Series XV: BUFA
Box 6
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.