Brandon University received its charter on June 5, 1967, on the occasion of the visit of Her Royal Highness Princess Alexandra and the Honourable Angus Ogilvie. The institution has its roots in Brandon College, which was established in 1899, by the Baptist Convention of Manitoba and the Northwest Territories and was administered by that authority until 1938. During these years it was an affiliate, first of the University of Manitoba and, from 1911 to 1938, of McMaster University. In 1938, it became a non-denominational affiliate of the University of Manitoba, under a board of directors elected by the Brandon College Corporation, and it continued as such until it was made a provincial university in 1967.
1967-1968 was the first year of operation as Brandon University.
The University is a co-educational, non-denominational, government-supported institution within the Province of Manitoba. It is a member of the Association of Universities and Colleges of Canada (AUCC) and the Association of Commonwealth Universities (ACU).
As stated in The Brandon University Act (1998), the purposes and objects of the university are: (a) the advancement of learning and the creation, preservation and dissemination of knowledge; and (b) the intellectual, social, ethical and physical development and improvement of its students and employees and of society. To further its purposes and objects the university may: (a) establish and maintain such colleges, faculties, schools, institutes, departments, chairs and courses of instruction as the board considers appropriate; (b) give instruction and training in all branches of learning; (c) grant degrees, including honorary degrees, diplomas and certificates of proficiency; (d) provide facilities for original research in every branch of learning, and conduct or facilitate the conducting of such research; and (e) generally promote and carry on the work of a university.
The mission statement of the University is to shape the whole person and enable students to make a positive difference as citizens and leaders. In a welcoming and supportive setting, the University emphasizes research, scholarship, critical thinking, performance, artistic creation, communication and participation, as a means of imparting value and meaning to society and contributing to the public good. The University nurtures and develops excellence in its programs, attracts an outstanding faculty, defends academic freedom, preserves knowledge and sustains a scholarly community where cultural differences are valued. The University strives to complement its primary mission of teaching and research by sharing the expertise of its staff, its information resources and its facilities with the greater community.
PROGRAM EVOLUTION:
1967 Brandon College became Brandon University with authority to grant degrees
1998 The Brandon University Act was passed by the Manitoba Legislature, replacing the Brandon University Regulations
Arts:
1902 First Arts graduates
1975 B.A. (4 year Specialist) degree
1983 B.A. (4 year General) degree
1990 Major in Business Administration
1991 Minor in Women's Studies
1992 Minor in Aboriginal Art
1996 Major in Business Administration (4 year)
1997 4 year Bachelor of Business Admin
Science:
1975 B.Sc. (4 year Spec)
1983 B.Sc. (4 year General)
1986 Post-Diploma degree for Registered Nurses and Registered Psychiatric Nurses
1995 4 year degree in Psychiatric Nursing
Education:
1952 Ed courses offered for the first time
1967 B.Ed. (5 year)
1969 B.Teaching (3 year)
1972 Project for the Education of Native Teachers (PENT) initiated
1974 Brandon University Northern Teacher Education Program (BUNTEP) initiated
1978 B.Ed (4 year)
1981 B.Teaching (3 year) discontinued as at October 17, 1981
1988 Concurrent B.Music/B.Ed (AD) degree program
1990 M.Ed.
1994 Brandon University Hutterian Education Programme (BUHEP) initiated
Music:
1906 Dept of Music (Conservatory) established
1973 B.Mus. (4 year General)
1977 B.Mus. (5 year Music Education)
1980 Master of Music Degree offered for the first time in Manitoba
1988 Concurrent B.Music/B.Ed (AD) degree program
Health Studies:
1998 School of Health Studies created and assumes responsibility for Bachelor of Science in Nursing, Bachelor of Science in Mental Health and Bachelor of Science in Psychiatric Nursing
Interdisciplinary degree programs:
1972 B.G.S.
1998 Masters degree in Rural Development
1998 Bachelor of First Nations and Aboriginal Counselling degree program
On December 19, 1985, the Board of Governors approved a set of recommendations regarding the administrative structure of the university. The recommendations renamed, abolished and instituted a number of positions at Brandon University.
Custodial History
Records in the fonds were in the possession of the President's Office until 1980, at which point they were transferred to the McKee Archives upon its creation. Subsequently, additional records have been transferred from the President's Office, the Senate Office and some faculties. Most records transferred after 1980 have separate accession numbers.
Scope and Content
Fonds consists of sixteen series, including: (1) Office of the Chancellor; (2) Board of Governors; (3) Office of the President; (4) Office of the Vice-President; (5) Office of the Registrar; (6) Brandon University Senate; (7) Faculties and Schools; (8) Library Services; (9) Department of Extension; (10) Office of Development; (11) Brandon University Foundation; (12) Student Services; (13) Miscellaneous Publications; (14) Brandon University Students' Union (BUSU); (15) Brandon University Faculty Association (BUFA); and (16) Brandon University/College Artifacts.
Notes
Information for the History/Bio field was taken from Brandon University calendars 1967-2006, the Brandon University website (December 2005) and an article in "The Quill" (January 9, 1986). Description by Christy Henry, unless otherwise noted.
The Board of Governors of Brandon University is a body established by the Brandon University Act (1998), a statute of the Province of Manitoba. The Act vests in the Board the authority for governing Brandon University. The members of the Board of Governors, as trustees, hold the University in trust for the people of the Province of Manitoba. Responsibilities for maintaining this trust include: selection of a president, monitoring his/her performance, providing guidance to the University via its policies, and often delegating authority to the administration.
The Board of Governors is a collective representing the entire community (both internal and external of the University). As a collective, the Board of Governors is responsible for ensuring the financial stability of the institution and for seeing that the overall plans of the institution are consistent with the institution’s philosophy, goals, and financial resources.
Scope and Content
Fonds consists of records generated and collected by the Brandon University Board of Governors in the course of perfoming its functions. The fonds is divided into six sub-series, incuding: (1) Documents; (2) Board Executive; (3) General Board agendas, minutes and packages; (4) Correspondence and subject files; (5) Board of Governors' committees; and (6) Board projects.
Notes
The information in the History/Bio field was taken from the Brandon University webpage (http://www.brandonu.ca/Administration/Governors/) on December 2, 2005.
Access Restriction
All files in the series are restricted. Researchers are required to contact the Executive Secretary to the Board of Governors to obtain written permission to access the records. Contact:
204-727-9714
board@brandonu.ca
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.
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
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.
The Lovstrom locale first came to the attention of Dr. Nicholson through conversations with landowners Mr. and Mrs. Herb Lovstrom in 1985. Lovstrom is a multi-component archaeological locale located 25km south of Brandon overlooking the Souris River channel. The landowner’s surface collection and the presence of bone and artifacts in a cultivated field indicated the presence of one or more sites.
Limited testing was conducted in 1985 and 1986, followed by major excavations in 1987, 1988 and 1991. Eight sites of block excavations with a total of 132 1m2 excavation units were completed. The locale area extends approximately 500m north from the edge of the Souris Valley escarpment and over 200m east from the Jock’s Creek escarpment.
Physical and biological environment As has been noted above, the locale is bounded on the south by the Souris channel and on the west by the incised channel of Jock’s Creek and a till plain extends to the north and the east. This plain is characterized by buff colored glacial till with numerous rocks embedded in the surface. Surrounding these rocky knolls are dark-soil hollows where the various cultural occupations are found. The depth of the topsoil layer suggests a long term grassland cover with the present oak forest likely developing in historic times due to the elimination of bison grazing and the controlling of prairie fires in late historic times. A small cleared patch of farmland is found within the boundaries of the locale area. This area has provided a substantial surface collection of artifacts.
Present vegetation in the area is a mosaic of aspen/oak forest groves and mesic grass prairie that includes introduced species such as brome grass. In poorly drained areas, willow and red osier dogwood are present. The Lovstrom locale is found in a forested area dominated by oak with an under story of saskatoon, chokecherry, pin cherry, and hazelnut brush. Poison ivy is abundant as well as sarsaparilla.
The major faunal resources in Precontact times would have been bison, with elk and mule deer playing a minor role. Antelope may have been present also. Small animals included snowshoe hare, cottontails, porcupines and beaver. Canids, including wolf, coyote, fox and domesticated dog were present, as well as mustelids such as badger, mink, and weasel. Fragments from a fisher were also recovered in the excavations.
Summation.
The Lovstrom locale has eight sites. The sites were designated and excavated as Blocks A, B, C, D, E, F, G and H. Many of the sites are multi-occupations.
The Vickers materials are primarily confined to Blocks D, E, F, G and H. Vickers Focus materials overlie Blackduck/Duck Bay materials. Blackduck and Duck Bay materials are found in the lower levels of all excavation blocks and in most test units. The Vickers occupations at the Lovstrom locale, based upon ceramic wares and an overlapping of C14 dates, appear to have been contemporary with the Lowton type site to the east, near Belmont. A small protohistoric occupation was identified overlying part of Block D. Faunal remains are abundant with bison clearly dominating the assemblages. Lesser amounts of canid are present as well as small mammals including beaver, hare and mustelids. Small amounts of avian species are also present.
Publications
Nicholson, B.A.
2011 The Role of Pocket Gophers (Thomomys talpoides) in Restructuring Stratigraphic Relationships at the Lovstrom Site. Canadian Journal of Archaeology 35:323-331.
Nicholson, Bev, Scott Hamilton, Matthew Boyd and Sylvia Nicholson
2008 A Late Plains Woodland Adaptive Strategy in the Northern Parklands: the Vickers Focus Forager-Horticulturists. Invited Paper for Papers in Northeastern Plains Prehistory, eds. Michael G. Michlovic and Dennis L. Toom, North Dakota Journal of Archaeology Vol. 8:19-34.
Nicholson, Bev and Scott Hamilton
2001 Cultural Continuity and Changing Subsistence Strategies During the Late Precontact Period in Southwestern Manitoba. Canadian Journal of Archaeology 25:53-73.
Nicholson, Bev
1996 Plains Woodland Influx and the Blackduck Exodus in South-Western Manitoba During the Late Precontact Period. Manitoba Archaeological Journal 6(1):69-85.
Nicholson, Bev and Mary Malainey
1991 Report on the 1991 Field School Excavations at the Lovstrom Site (DjLx-1), Southwestern Manitoba. Manitoba Archaeological Journal 1(2): 51-93.
Nicholson, Bev and Jane Gibson
1990-91 Lovstrom Site Field Report, 1987 Excavations. Saskatchewan Archaeology 11&12:46-68.
Nicholson, Bev and Ian Kuiijt
1990 Field Report and Interpretations of the 1988 Archaeological Excavations at the Lovstrom Site (DjLx-1) in Southwestern Manitoba. North Dakota Journal of Archaeology 4:166-205.
Nicholson, Bev
1990 Ceramic Affiliations and the Case for Incipient Horticulture in Southwestern Manitoba. Canadian Journal of Archaeology 14:33-60.
Nicholson, Bev
1986 The Lovstrom Site: Culture Contact in Prehistory. Manitoba Archaeological Quarterly 10(1):35-71.
Scope and Content
The Series has been divided into nine sub-series, including (1) Survey (2) Block A; (3) Block B (4) Block C; (5) Block D; (6) Block E; (7) Block F; (8) Block G; (9) Block H
The Brandon University Teaching and Administration series is an artificially created collection. It contains the private papers of former Brandon University faculty and staff.
Scope and Content
The series has been divided into the following sub-series:
MG 3 1.1 Errol Black
MG 3 1.2 John Mallea
MG 3 1.3 John Tyman
MG 3 1.4 Lorelei Cederstrom
MG 3 1.5 William Morrison
MG 3 1.6 Ken Hanly
MG 3 1.7 John Welsted
MG 3 1.8 Henri Francq
MG 3 1.9 D.R. MacKay
MG 3 1.10 R.B. Inch
MG 3 1.11 Dale Lakevold
MG 3 1.12 George MacDowell
MG 3 1.13 Donald Wheeler
MG 3 1.14 W.Leland Clark
MG 3 1.15 Bev Nicholson
MG 3 1.16 John Everitt
MG 3 1.17 Michael Blanar
MG 3 1.18 Christy Henry
MG 3 1.19 May Yoh
MG 3 1.20 Francis Chaplin
MG 3 1.21 John Weldon Grant
MG 3 1.22 Harvey Young
MG 3 1.23 Lorne Watson
MG 3 1.24 Lawrence Jones
Storage Location
MG 3 Brandon University Teaching and Administration
Fair. The photos have some crackling on the surface. Some of them also have what appears to be pencil marks on them.
History / Biographical
The Brandon Square Dancing Club was started by E.J. "Curly" Tyler as part of his degree program at the University of Utah. Part of his obligation for his degree was to organize a recreation group, so he organized the Square Dancers. The club operated for two years under Tyler's direction, with the individuals he taught receiving certificates for proficiency. After he ceased to be its leader, the Brandon Square Dancing Club continued for a number of years. Much of the dancing took place at the Ag Extension Centre.
Custodial History
Photographs turned up somewhere in the old Original Building at the time of the renovations (mid 1990s) and were brought to the McKee Archives.
Scope and Content
Fonds consists of 44 black and white photographs of the Brandon Square Dancing Club. The majority of the photographs depict actual dancing. There is also one file with photocopies of the photographs. These photocopies identify individuals in the photographs.
Individuals in the photographs include: Edith Laycock; Bill Clement; Bea Lissaman; Reg Lissaman; Jean Hawley; Mrs. Murray Simmons; Murray Simmons; Dood Cristal; JoAnn Myers; Bob Myers; Jim Creighton; Muriel Cumming; Frank Cowan; Dean Finch; Birk Birkinshaw; Bill Baynton; Gil Wankling; Hugh Knowlton; Hilda Evanson; Archie Evanson; Gwen MacKay; Don (D.R.) MacKay; Burt Hurst; Ena Skafel; Einar Skafel; Marian Jones; Ray Jones; Joan Tyler; Curly Tyler; Bea Matheson; Murray Matheson; Bill Coleman; Gladys Wankling; Percy Finch; Lois Gibson; Ken Pratt; Jack Findlay; Phyl Harwood; Ozzie Pullow; Jean Pullow; Ann McDiarmid; Barb Brodie; Mal Brodie; Bud McDiarmid; Doris Boyd; Ethel Norrison; Dr. Arhurst; Mrs. Arhurst; Bob McPherson; Mary Gooden; Ron Godfrey; Elizabeth Godfrey; Gordon Cummings; George Gooden; Marg Purdy; Kay Findlay; Jack Coleman; Betty Coleman; Marion Unicume; Nels Unicume; Bob Hawley; Nan Coleman; Jack Purdy; Kay Birkinshaw; Lyal McGill; Norm Emerson; Shirley Emerson; Zana Hurst; Ethel Morrison; Leo Kennedy; Hazel Jones; Dr. R.C. Jones; Jim Blencowe; Betty Knowlton; Wesley Nelson; Marian Nelson; Pauline Tennant; Dave Dick; and Bob McMullan.
Notes
George Gooden provided the names on the photographs. Description by Christy Henry.
Repro Restriction
Copyright restrictions apply
Conservation
Photographs have been removed from original matting.
Storage Location
2007 accessions
Storage Range
2007 accessions
Arrangement
Photograph number 40 is missing using the original numbering system. The numbers on the photographs have been adjusted accordingly (ex. old #43 is now #42). The numbers on the photocopies have also been adjusted to reflect the new numbering system.
The largest crest has a couple of holes in the background.
Custodial History
Items were accessioned in 2007 by the McKee Archives. Prior custodial history is unknown.
Scope and Content
Consists of three blue and gold Brandon College crests made from felt. Two are circular in shape, measuring 4.25" and 3.75" across. The third is oval in shape, measuring 4 x 3.5". All three are composed of the letters "B" and "C" in gold and intertwined on a blue background. The two circular crests also have a gold border.
