In 1975, Brandon University in cooperation with the Manitoba Pool Elevators, founded the Rural Resources Centre. The Centre was designed to provide rural Manitoba with resource materials for use in the discussion and analysis of problems related to rural social development. It was given a mandate to collect publications and archival materials related to the history of the Manitoba Pool Elevators, cooperative societies, churches, exhibitions, school districts, and Women’s Institutes.
In September 1978, the University transformed the Rural Resources Centre into the Brandon University Archives. Originally housed in a trailer, from October 1981 to September 1998 the University Archives operated out of the Archives Centre located in the basement of the Jeff Umphrey Building at 20th Street and Victoria Avenue.
In 1990 the University Board of Governor’s renamed the University Archives the S. J. McKee Archives. The S. J. McKee Archives was so established on Saturday, November 19, 1990, to mark the anniversary of the opening of the Brandon Academy by S. J. McKee and his wife Laura McKee one hundred years earlier. In 1899, the Brandon Academy founded by Samuel and Laura McKee became Brandon College.
The S. J. McKee Archives moved to its current location on the mezzanine floor of the John E. Robbins Library in the summer of 1998.
The McKee Archives is the principal repository for records of archival value created by the University or which relate to the history and mandate of Brandon College and Brandon University. The Archives collects records of selected Brandon College and Brandon University faculty and alumni.
The McKee Archives also acquires manuscript collections, which support the research and teaching programs offered at Brandon University. These include archival records related to rural development, education, agriculture, heath studies, First Nations, and the city of Brandon.
UNIVERSITY ARCHIVISTS:
SALLY CUNNINGHAM (1975 - ?)
No biographical information yet.
EILEEN MCFADDEN (1981 - 1997)
See RG 6, series 8, sub-series 1 (University Librarian) for biographical information on Eileen McFadden.
TOM MITCHELL (1997 - present)
See RG 6, series 5 (Registrar's Office) for biographical information on Tom Mitchell.
Scope and Content
The sub-series has been divided into four sub sub series, including: (1) Archives - general files; (2) Archives - budget files; (3) Archives - correspondence files; and (4) Archives - exhibits and displays.
Notes
History/Bio information taken from articles in "The Quill" (September 24, 1981 and November 20, 1990) and the S.J. McKee Archives hompage at http://www.brandonu.ca/library/archives/ (September 2006).
Storage Location
RG 6 Brandon University fonds
Series 8: Library Services
In 1970, the Department of Extension was divided into the Department of Extension (Non-Credit) and the Department of Extension (Credit). In 1974, the two departments were amalgamated into the Department of Extension (Credit and Non-Credit). The department's name was changed again in 1977, when it became the Department of Continuing Education (Credit and Non-Credit).
In 1986, the Office of Continuing Education and Summer Session was renamed the Office of Extension with responsibility for non-credit offerings, distance eduation and off-campus credit courses. From 1999 to the 2001-2003 calendar, Kathleen Matheos, the last Director of Extension, is listed as the Director of the Education Technology Unit. After the 2001-2003 calendar, the Department of Extension became part of Campus Manitoba.
DIRECTORS OF EXTENSION:
R.B. INCH - Extension (1967-1969) and Extension (Non-Credit) (1970-1971)
George Robert Boyer Inch, more commonly known as R.B. Inch, was born in 1903 in Oak Point, New Brunswick. His father, James Nathaniel Inch, was a local shopkeeper and served as town postmaster. James Inch married Phoebe Elizabeth Inch (nee Boyer), a native of Hartland, New Brunswick. While working in Ontario between 1939 and 1939, R.B. Inch met and married Elizabeth Gowling of Ottawa. The couple had two children; a son named George and a daughter named Jeanne. Elizabeth Inch (nee Gowling) passed away in 1956.
R.B. Inch was educated first at Mount Allison Academy in Sackville, New Brunswick. He later went on to study at Mount Allison University, where he earned a Bachelor of Arts degree in 1924. After graduating, Inch traveled to western Canada looking for employment in his chosen field of journalism. From 1924-1926 Inch was unable to find a job in the newspapers so he subsisted by teaching classes at Mount Royal College in Calgary and attending lessons at the Calgary Normal School. In June 1926, the Calgary Herald, then known as the Calgary Albertan, hired Inch as a regular journalist. He stayed in that position in Calgary for two years. Inch later accepted a job with the Winnipeg Free Press, where he worked from 1928-1929.
In 1929, Inch accepted a position with the National Research Council in Ottawa as Secretary to the President and information officer. Between 1929 and 1933 he also volunteered as editor of the magazine "Interdependence," the official publication of the League of Nations Society in Canada. In 1935, Inch resigned his post at the National Research Council to become the National Secretary of the League of Nations Society in Canada. There he served until the collapse of the League at the outbreak of World War II in 1939.
In 1942, Inch was commissioned by the Canadian Broadcasting Corporation (CBC) to prepare a series of programs entitled "Of Things to Come - Inquiry on the Post-War World." In 1943, Inch joined the Royal Canadian Army Service Corps, but never saw action in Europe. After the war, Inch was hired by his alma mater, Mount Allison University, to serve as Director of Alumni and Public Relations. He remained in Sackville from July 1945 through to 1967. In July 1967, Inch was hired by Brandon University as the Director of Extension and as a political science lecturer.
After retiring in 1972, Inch was active in the formation of the Canadian branch of Amnesty International. He would later become National Director Emeritus of the organization.
R.B. Inch died in Brandon, Manitoba on January 7, 1983.
H.S. PERDUE - Extension (Credit) (1970-1971)
Dr. Henry Stewart Perdue was born in 1904 near Souris, Manitoba. He graduated from Souris Collegiate in 1920. After working several odd jobs, Perdue entered Brandon College in 1924. He graduated with his B.A. in 1928. After graduation, Perdue was hired as a teacher in the Academic Department. He received his M.A. in 1930, and went on to receive his Ph.D. in Geology from the University of Chicago. In 1930, Perdue became the Director of the Matriculation Department, as well as an Instructor in Geology. In 1931, he took over the position of Resident Master. In 1937, he married Ella May Higgens, who was the Resident Nurse. From 1938 until 1948, Perdue acted as Registrar of Brandon College.
In 1947, Perdue accepted the position on College Dean. This position ran until 1952, when it was changed to the position of Dean of Arts and Science. Perdue also held this position until 1962, when the office separated into the Dean of Arts and the Dean of Science. Perdue continued in the position of Dean of Science until 1967. After Dr. Evans' death in July of 1959, Perdue became acting President. He held this position from August 1959 until August 1960, when Dr. Robbins was appointed President. Perdue held the position of Director of Extension (Credit) from 1970-1971. He retired from teaching Geology in 1973. Dr. Perdue died on December 22, 1979 at the age of 75.
EVAN H. PEPPER - Extension (Credit) (1972-1974)
Evan H. Pepper was born in Windsor, Ontario. He received his BSc in Biology and Chemistry from the University of Detroit and his MSc and PhD from Michigan State University in the same fields. Pepper also attended the Henry Ford Trade School, the United States Brewer's Academy (Brewing Technology) and the Ryerson Institute (Instrictional Technology). In 1945-1946 he served in the U.S. Merchant Marine, and from 1954-1956, in the U.S. Army.
From 1960-1962, Pepper was a technical coordinator for Ladish Malting Co. He began his academic career in 1962 as an Assistant Professor in the Department of Plant Pathology at North Dakota State University, leaving that position in 1967. From 1967-1988, he was an Associate Professor, and later a Professor (1971-1988) in the Department of Botany at Brandon University.
While at Brandon University, Pepper served on the Brandon University Senate, the Senate Executive Committee, the Extension Committee, the University Act Committee and the Senate By-Laws Revision Committee. He was also assigned as a liaison to Inter-Universities North (IUN) and helped to design the RN/RPN program (1970). Pepper's administrative duties included Director of Credit Extension, Director and designer of the FOCUS program and Chair of the Botany Department. In addition, he also taught, designed and developed several courses for the Biology and Botany Departments at Brandon University.
Evan Pepper retired in 1988. He died on March 27, 2013.
R. BRUCE MCFARLANE - Extension (Non-Credit) (1972-1973); Extension (Credit and Non-Credit) (1974-1976); Continuing Education (Credit and Non-Credit) (1977-1986); and Extension - acting (1990)
No biographical information yet.
B. WESTFALL - Extension (1987-1989)
Beth Westfall was born in Birmingham, England. Her undergraduate degree in European Studies was obtained from the University of Sussex; she recieved her Master's Degree in German from the University of British Columbia and her Ed.D. in adult education from Nova University.
Westfall came to Brandon University in January 1987, as the Director of Extension. Prior to that time she a director on a regional campus on the College of New Caledonia in British Columbia. She also had extensive experience in teaching basic adult education and English as a second language, and in facilitating women's support groups and communication skills workshops.
In September 1989, Westfall became Brandon University's Dean of Student Services. See RG 6, series 12 (Student Services) for additional biographical information.
K. MATHEOS (1990 - 1997/1998)
Kathleen Matheos was appointed Director of the Office of Extension for a five year term effective September 1, 1990. Prior to coming to Brandon University, she was the Agricultural Distance Education Coordinator/Community Programs Division at Assiniboine Community College. In 1999, Matheos' title was changed to Director of the Education Technology Unit and ca. 2003 the Office of Extension was absorbed into Campus Manitoba. Matheos left Brandon University some time thereafter, and currently (January 2006) works for the Department of Extension at the University of Saskatchewan.
Scope and Content
The series is divided into four sub series, including: (1) General files; (2) FOCUS; (3) Brandon University Art Exhibition Committee; and (4) Publications.
Notes
History/Bio information was taken from Brandon University calendars and an article in "The Quill" (January 9, 1986). Biographical information on R.B. Inch was taken from the finding aid for the R.B. Inch collection written by Matthew Palmer (2003). Biographical information on H.S. Perdue was taken from the "Brandon College finding aid" prepared by Karyn Riedel for McKee Archives in 1998. Biographical information for Evan H. Pepper was taken from his resume (given to the Archives in 2006). History/Bio information for Kathleen Matheos was taken from Campus News - July/August 1990.
Storage Location
RG 6 Brandon University fonds
Related Material
Additional material on R.B. Inch is located in MG 3 1.8 R.B. Inch collection.
The high biodiversity and evidence of pre-Europeon contact prompted the decision to test the Crepeele locale. The survey was named in recognition of the Casselman family, the original landowners.
Archaeological testing began in the Crepeele locale in May 2003 on property now owned by the Crepeele family. The locale covers over 6 sections or approximately 3,800 acres of land in an area of stabilized sand dunes and wetlands covered with mixed forest and prairie grass. Given the terrain, the size of the crew and time constrains, an area of approximately 60 acres was chosen for the survey. The survey used the established archaeological methodology of walking the selected area and using a shovel test surveyed grid. The use of GIS technology to locate the exact test spot and record the information into a GIS database was a significant advance and was one of the advantages of the integration of multi-disciplinary techniques encouraged by the SCAPE project. Over one half of the test pits resulted in the recovery of cultural materials. The results of the Casselman survey indicated several areas for further examination including areas that became the Crepeele, Sarah and Graham sites.
Scope and Content
Sub sub series has been divided into five sub sub sub series including: (1) Summary information; (2) Field journals; (3) Site records; (4) Artifact catalogues; and (5) Photographs.
In 1988 four units were excavated in Block G. The vegetation is similar to other areas in the locale with an open oak forest with a light understory of saskatoon, hazelnut, poison ivy and sarsaparilla.
Excavations recovered artifacts between 0 cm – 15 cm b.s. The cultural deposits are very shallow and it is quite possible that what appears to be a single occupation may in fact represent multiple occupation compressed deposits as a result of deflation or the lack of sedimentation in this raised area. This latter view is supported by the ceramics which appear to be a mixture of Blackduck and Vickers Focus wares.
The frequency and distribution of cultural material from block G contrasts with that of other sites in the locale. While the diagnostic materials are similar, the nature of the background debris and the associated lithic assemblage suggests that this area was utilized for a different set of activities.
Unlike Blocks E and H, there is very little in the way of ceramics, fire-cracked rock or bison bone, yet a significant amount of lithic debitage and six Plains/Prairie Side-notched projectile points were recovered. No unifaces or scrapers were recovered. This may be an area where activities such as manufacture and hafting of projectile points; hunting activities, butchering and refuse disposal took place.
No RC dates were taken.
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.
The vegetation in block H is similar to other areas in the locale with an open oak forest with a light understory of saskatoon, hazelnut, poison ivy and sarsaparilla.
The excavations of the eight 1m2 units in 1988 resulted in the recovery of over 650 ceramic fragments including 20 rim sherds from at least four vessels, a grooved maul, fire-cracked rock, lithic debitage and a reworked Avonlea projectile point. A large amount of bison bone, including a number of axial elements and a fragmented skull were also recovered.
Based on the 1988 recoveries at the site further excavations took place in 1991. Nine excavation units were opened next to the previous excavations. Another 250 ceramic sherds were recovered in 1991. Nine vessels have been identified based on rim sherds. Vickers Focus and Woodland vessels have been identified and two vessels similar to Scattered Village Complex were recovered.
The lithic material assemblage is intermediate between Blocks G and E with KRF being the most frequent material category followed by local cherts.
Two features, a hearth and a curvilinear arrangement of rock were recovered. The high numbers of ceramic fragments suggests a habitation area, rather than hunting or butchering behavior. However, the separation of occupations at the site is difficult to establish and there may be different uses of the site by successive occupations.
Radiocarbon dates from this block indicate two occupations separated in time by some 300 years. XU 181 – 405/110 BP and XU 184 – 780/110 BP.
Scope and Content
Sub-series has been divided into sub sub series including: Lovstrom Block H 1988 and Lovstrom Block H 1991.
Robert (Bob) Troy Blair was born on March 11, 1930 in Brandon, MB. His first six years were spent in Alexander, MB, where his father and uncle operated a grocery store. In 1936, his family moved to Souris, MB, where his father ran a grocery store. Blair received his primary and high school education, with the exception of Grade 12, in Souris.
Blair remembers his school years in Souris as mainly happy years. He was involved with both piano and organ music lessons. he was never interested in physical sports with the exception of golf. World War II broke out in September of 1939. Souris became the site of #17 SFTS and home base for the British Commonwealth Air Training Plan. Many of the service men came from England, Australia and New Zealand. Blair's mother always entertained at least two for dinner every Sunday. Rationing of sugar, tea and coffee, butter and meat became a way of life. Blair had the job every Saturday of pasting the ration coupons into booklets. It was also when he was in Grade 6, that Blair realized he was more attracted to boys than to girls. Perhaps it was because so many attractive airmen surrounded him!
In November of 1947, the Blair family relocated to Alexander where Bob Blair finished his Grade 11. This was not a good year due to bullying. In September of 1948, Blair moved to Winnipeg to attend United College for his Grade 12. Upon completion of Grade 12, Blair remained in Winnipeg until June 1950. he worked at a number of businesses - Gestetner, Eaton's Mail Order shoe department, Maple Leaf Milling, and the drug store in the Medical Arts Building. In September 1950, he entered Brandon College. Blair was very active in extra-curricular affairs while at Brandon College; particularly drama. Following his B.A. he enrolled in the Education Faculty, having decided to become a teacher.
Blair's teaching career spanned 34 years. All but one year was spent in the Brandon School Division. On his first day of teaching in the Division he met the man with whom he would spend the next 46 years. He was primarily a teacher of English and Music. A highlight of his career was exchange teaching in Sacramento, California in 1961. Orientation for exchange took place in August in Washington, D.C., where Blair had the opportunity to meet President J.F. Kennedy. He vividly recals the morning that JFK was assassinated on November 22, 1963. In September 1965, Blair assumed the principalship of Park School and in September of 1969, the same position at George Fitton School where re remained until his retirement in 1989. He was a member of the Brandon Picnipals' Association, the National Association of Elementary School Principals, and servedas President of the Brandon Teachers' Association. Among his major accomplishments during his time as principal were the introduction of a centralized school library in both Park and George Fitton Schools and the integration of special needs students into regular classroom situations wherever possible. He was made a Life Member of the Manitoba Teachers' Society (Brandon) in June 1990. Following his retirement Blair worked as a Library Automation Consultant (1989-1993).
Blair also had numerous community involvements during his time in Brandon. he was active in the Brandon Little Theatre (Best Actor Award, Manitoba Drama Festival for One Act Plays in 1963), the Brandon Festival of the Arts, the Eckhardt-Gramatte National Music Competition, and Arm Industries to name a few.
Following the death of his partner in 2001, Blair moved to Saskatoon to live with a younger gay couple. He has been active in volunteerism: as an Ambassador for the Saskatoon Airport Authority, assistant with the Saskatoon Health Region's Immunization Clinics, information clerk for the Festival of Trees, data entry clerk for the Saskatoon Music Festival, on the Board of the Saskatoon Jazz Society, and Hospitality Coordinator for the Saskatoon Jazz Festival.
As of October 2013, Bob Blair continues to live in Saskatoon, SK.
Custodial History
Records were in Blair's possession until he donated them to the Mckee Archives on Homecoming weekend October 2013.
Scope and Content
Fonds consists of two scrapbooks containing 145 photographs and ephemera (play and graduation programs, tickets, pins, newspaper clippings) documenting Bob Blair's days at Brandon College. Social events and extra-curricular activities are heavily featured in the two scrapbooks. Also included are graduation portraits for the Classes of 1951, 1952 and 1953. Of the 145 photographs all are black and white except for two photos of the Class of '53 reconvocation (May 1993), and one from the Class of '53 reunion (2003).
Block C was situated in sparse oak forest with an understory of saskatoon, hazelnut and a thick ground cover of poison ivy and sarsaparilla. The block measured 3m and 3m and contained nine excavation units. All units were excavated to 35cm below surface. The soil horizons were much like the other blocks, except for a rusty brown stain in the first level, giving the upper black loam a mottled appearance. The brown patches were clay mixed with loam and were harder than the surrounding matrix. No definitive interpretation of these phenomena was attempted but this effect may be the result of natural brush or forest fires. Under the 5cm so d/humus (Ah) layer, the loam horizon extended approximately 5cm – 25 cm below surface, and averaged 20 cm thick. Bone was concentrated within this horizon between 10 cm – 20 cm below surface.
Block C was notable for its concentrations of articulated bison bone. Most noteworthy was an articulated unit composed of lumbar vertebrae, pelvis, and sacrum. Several thoracic vertebra/proximal rib end concentrations were also recovered. There were more vertebrae and rib sections recovered in the units in proportion to other bones. A few sherds, some debitage and a single Prairie Side-Notched point fragment were among the recoveries. Based on the quantity of bone, the density of the bone layer, and the articulated butchering units the area has been interpreted as a bone midden.
Faunal material was analysed by Jessica MacKenzie for her Honours Thesis: "A reconstruction of butchering processes in Block C from the Lovstrom site DjLx-1 in Southwestern Manitoba."
Radiocarbon date: 850/115BP XU 79.
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.
Block D was wooded with oak and an understory of saskatoon and hazelnut with a thick ground cover of poison ivy and sarsaparilla. Root and rodent disturbance was extensive.
Based on the recoveries from Test Unit 22 during the survey, further excavations were carried out. Two units 87 and 93 were excavated in 1987. A further four units were excavated in 1988. There appears to be a pre contact occupation and a protohistoric feature within the block.
Diagnostic lithics included a chert Plains Side-notch projectile point, and a large Woodland side-notched point. The lithic materials from Block D are primarily local cherts followed in abundance by Knife River Flint and Tongue River Silicified Sediment – both of which are exotics imported from the southwest. Faunal remains were primarily bison.
Thin-walled obliterated fabric impressed pottery with grit temper was recovered in all units. Diagnostic ceramics included two rims, one with a fabric impressed exterior and the lip notched with dowel impressions, and a second thick walled rim was fabric impressed to the lip. The ceramic wares appear to be essentially a Woodland complex with overtones of Plains influence.
RC date: 230/90 BP.
Scope and Content
Sub-series has been divided into sub sub series including: Lovstrom Block D 1987 and Lovstrom Block D 1988.
This site is situated in a naturally sheltered area with a low rise to the east and south partly encircling a flat area open to the west. Present natural vegetation is an open oak forest with a light understory of saskatoon, hazelnut, poison ivy and sarsaparilla. It is situated on the till plain at the upper end of a ravine leading to Jock’s Creek.
Two test units six meters apart were excavated in 1987 and produced cultural materials which warranted a block excavation, so seven contiguous 1m2 units were then opened. These units proved to be very productive of cultural remains. Subsequent excavations in 1988 increased the number of excavated units to 21. In 1991 a further eight units were excavated for a total of 29 excavations and two test units. Excavations went deeper in this block than in Blocks C or B. Remains from the block included bison bone, bone tools, fire-cracked rock, ceramics, lithics including tools and debitage and a hearth. Another occupation was recovered in 1991 containing a hearth and living floor.
Radiocarbon samples have produced two distinct sets of radiocarbon dates from 1987 and 1988 excavations. There appears to be two or possibly three cultural horizons definable within this block.
An upper cultural horizon, located between 14-21 cm below surface, contains large bison bone and fire-cracked rock dating to 465/100B.P from XU 128.
A lower horizon in the 20-25 cm level contained FCR, bison bone and lithic scatter that was dated to 675/70 B.P. from XU 122 and 715/110 from XU 114.
Scope and Content
Sub-series has been divided into sub sub series including: Lovstrom Block E 1987, Lovstrom Block E 1988 and Lovstrom Block E 1991.
In 1988 four 1m2 units were excavated in this Block F. The forest cover is identical to that of Block E, with an open oak forest with a light understory of saskatoon, hazelnut, poison ivy and sarsaparilla.
Underneath the litter mat (Ah) is a shallow, 15-20 cm “A” horizon of dark grey/brown silty loam with a high representation of pebble size clasts. The glacial clays, encountered at 20 cm below surface, consist of a matrix of light tan sandy clays containing rounded pebble to cobble size rocks.
The recoveries from this block consisted of a few ceramics, including Vickers Focus rim sherds, four lithic tools and a number of small bison bone fragments. There was no discernible cultural stratigraphy in the four 1m2 units and the limited deposits of bone, ceramics and lithics were dispersed randomly throughout the 25 cm of cultural matrix. The lithic materials frequencies were similar to those in Block E with local cherts and KRF being the most abundant categories. A small amount of fire-cracked rock and a few large identifiable bison bones were recovered – all distributed randomly with little evidence for any pattern of clustering.
No RC dates.
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.
The Sarah site was chosen for excavation based on the results of the Casselman survey. The survey recovered significant amounts of faunal remains, some ceramics and lithics from the test pits. Excavations took place in 2003 at Crepeele West (Units 1-5) and Crepeele East (Units 6-9). The site was subsequently renamed the Sarah site DiMe-28. In 2004 another 9 units were excavated (Units 10-18).
Based on the recoveries it was determined that the Sarah site is a stratified site with woodland ceramics in the upper occupation and late woodland points in both of the upper occupations. These upper occupations produced abundant bison bone including foetal bone. The lower occupations produced less bone and no foetal bone, although absence of foetal bone in the lower occupations does not necessarily indicate a warm season occupation. This could be due to sample error or perthotaxic factors such as scavenging of the fragile bone by dogs or other carnivores.
The dates from the Sarah site include 550+/-40 B.P.; 1430+/-80 B.P; 2810+/-80 B.P.; 3120+/-130 B.P. The lower occupations did not yield any diagnostic materials although debitage was abundant. These occupations were most productive at the edge of the large sand dune at the southern edge of the excavations. It is assumed that the major portion of these occupations have been overridden by the dune in the past 3000 years. Heavy earthmoving equipment would be required to remove this overburden which limits the possibility of future excavation.
Environment
The Sarah site is a large area located at the eastern end of the Crepeele locale. Ground cover is a mosaic of aspen poplar groves and patches of mesic grass prairie. Excavation profiles indicate that this has been the situation since early precontact times, although as local climatic conditions change (primarily rainfall), the relative size of these areas and where they may have occurred also changed. The soil is aeolian sand sheet derived from delta outwash deposits along the western edge of glacial Lake Hind. The present topography is a variable dune landscape reworked by aeolian activity that creates a mosaic of microhabitats. These include forested patches in the lee of sand dunes with grassland on the southern and western exposures and small damp lowlands that support balsam poplar, willows, red osier dogwood, high-bush cranberry and water birch. There is no permanent water source in the area although a small seasonal stream meanders through a damp lowland to the east of the Sarah site.
Scope and Content
Sub-series has been divided into sub sub series including: Sarah 2003 and Sarah 2004,
Sub-series consists of four scrapbooks detailing life at Clark Hall and Brandon College. They include newspaper clippings, photographs, cards, various programs and ephemera.
Storage Location
RG 1 Brandon College fonds
Series 9: Clark Hall Women's Residence
The Graham site is a located adjacent to the Crepeele site towards the western end of the Crepeele locale. The Graham site was initially designated as a separate site early in the testing of the Crepeele locale due to what appeared to be a distinction between Early and Late Woodland ceramics. Subsequent testing has shown that this distinction was premature and that the cultural mosaic represented in the western section of the Crepeele locale may not readily separate in this manner. However, due to the records management that was already in place, the original separate designations have been retained.
Environment
Ground cover is a mosaic of aspen poplar groves and patches of mesic grass prairie. Excavation profiles indicate that this has been the situation since early precontact times, although as local climatic conditions change (primarily rainfall), the relative size of these areas and where they may have occurred also changed. The soil is aeolian sand sheet derived from delta outwash deposits along the western edge of glacial Lake Hind. The present topography is a variable dune landscape reworked by aeolian activity that creates a mosaic of microhabitats. These include forested patches in the lee of sand dunes grassland on the southern and western exposures and small damp lowlands that support balsam poplar, willows, red osier dogwood, high-bush cranberry and water birch. There is no permanent water source in the area although a small seasonal stream meanders through a damp lowland along the eastern margin of the Crepeele locale.
Excavations at the Graham site took place from 2004 to 2008. Analyses of the recoveries shows that, with two exceptions, all of the occupations that have been tested produced bison foetal bone. The presence of foetal bison is a strong indicator of wintering occupations...The absence of foetal in some area does not necessarily indicate warm season occupations since these excavation series are small and the absence could be due to sample error or perthotaxic factors, such as scavenging of the fragile bone by dogs or other carnivores.
From this evidence the Graham site has been interpreted as being primarily a wintering area. This is consistent with the lack of surface water (snow would serve as a substitute in winter) and the abundance of wood for fuel – a critical requirement for winter occupation. Cultural occupations date from Mortlach circa 250 B.P to woodland circa 580 B.P.
Scope and Content
Sub-series has been divided into sub sub series including: Graham 2004, Graham 2005, Graham 2006 and Graham 2008
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.
The Atkinson site was named for the landowners Ken and Karen Atkinson who were very helpful to the archaeology and geoarchaeology crews that worked at the site. Their support made the project possible.
The Atkinson site story begins with the discovery of a charcoal lens eroding from the north bank of the Souris River in the summer of 2002. Study of Cultural Adaptations on the Prairie Ecozone (SCAPE) project geoarchaeologist Dr. Garry Running was exploring the stratigraphic layering in the bank when he noted the lens and reported it to Dr. Bev Nicholson. Upon closer examination, a tiny pressure flake was observed on the lens exposure and it was decided to collect a charcoal sample for radiocarbon dating.
The resulting date of 5250B.P cal. 4225 B.C. placed the site in the early Archaic period. A second date on bone collagen of 5580B.P. cal. 4500 B.C. confirmed the earlier date and gave an averaged date of circa 4400 B.C or 6,500 years ago.
The Atkinson site is one of the oldest excavated sites in Manitoba. 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. Based on the date and sample evidence further excavations were conducted by Dr. Nicholson's team. in 2003, 2004 and 2006.
Scope and Content
Sub series has been divided into three sub sub series including: (1) Atkinson 2003, (2) Atkinson 2004; (3) Atkinson 2006
Flintstone Hill is located on the north bank of the Souris River. It is a deeply stratified lacustrine, fluvial and aeolian soil profile that has been exposed by the river through stream-bank erosion. This section is thought to be the most complete middle to late Holocene exposure on the northeastern plains. While the value of the site is primarily for paleo-environmental research and reconstruction, cultural deposits have been identified at the site. Local collectors have picked up lithic materials as they eroded out of the bank for the past several decades and it was they who had named the site. Mr. Bruce Timms from Lauder first drew the Flintstone Hill site to the attention of Dr. Nicholson of Brandon University.
During the mid 1990’s to the early 2000’s archaeological testing took place on Flintstone Hill. In 1998, an archaeological field crew dug a series of overlapping trenches down the slope of the profile and produced a schematic drawing. A peat layer at the bottom of this profile, dated from the top at 9,400 RCY and at the bottom to 10,400 RCY, has provided details of marsh plant and insect communities at this time.
Subsequent archaeological investigations at the site recovered several cultural deposits including: a hearth dating to 3250+/-70 R.C.Y. (BETA 109529); a butchered atlas bone 4090+/-70 R.C.Y. (BETA 109990); and bone fragments accompanied by Swan River Chert and Knife River Flint lithic flakes 5350+/-50 (BETA 109530). While no diagnostic tools were recovered, these dates suggest that this occupation, which is contemporary with the Atkinson site, may be a Gowen occupation.
Extensive paleo-environmental research has been conducted at the site. Dr. Running, a geomorphologist from the University of Wisconsin – Eau Claire, participated in the Study of Cultural Adaptations in the Prairie Ecozone (SCAPE) Project and he and his students tested the site for several years. He was joined in this effort by Dr. Havholm, Dr. Boyd, Dr. Wiseman, Dr. Beaudoin, and other SCAPE researchers in the interpretation of the paleo-environment of the Glacial Lake Hind basin. The following article is recommended reading.
Running, Garry L., Karen G. Havholm, Matt Boyd and Dion J. Wiseman
2002 Holocene Stratigraphy and Geomorphology of Flintstone Hill, Lauder Sandhills, Glacial Lake Hind Basin, Southwestern Manitoba. Geographie Physique et Quaternaire
56(2-3):291-303.
Scope and Content
Sub series has been divided into two sub sub series including: (1) Flintstone Hill 1997 (2) Flintstone Hill 1998-2000
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 Lovstrom surface collection came from small fields cleared within, and adjacent to, the major portions of the site which were excavated. The Lovstroms initial collection has since been added to by field personnel from Brandon University. The initial collections consisted of lithics and ceramics. A collection of faunal remains from the cultivated area was made by a Brandon University zooarchaeology class in 1986 which yielded specimens of elk, canid, mussels, and sucker, in addition to an expected abundance of bison. Since these materials were in a surface context, it may be that some of the faunal remains were historic.
The high biodiversity and evidence of pre-Europeon contact prompted the decision to test the Lovstrom locale. Nine 1m2 units were excavated in 1985 and, in 1986, an additional 15 1m2 units were excavated for a total of 24 test units. This testing indicated the presence of a large precontact locale with lithics, woodland ceramics and large amounts of reasonably well-preserved faunal materials.
The lithics indicated a late Prehistoric occupation (Nicholson 1986:35). However, the ceramics were more useful in that they identified the presence of Late Woodland cultures (Blackduck and Duckbay) and a single Middle Missouri vessel. It is believed that the Middle Missouri vessel was imported since the paste and construction/decorative technology differ distinctively from that of all other vessels recovered from the site. It was on the basis of an examination of these surface finds that the decision to test the Lovstrom site was made. These test excavations were conducted during the summers of 1985 and 1986.
Field investigations through shovel tests, excavation units, and examination of rodent mounds, indicated that the cultural deposits at the Lovstrom locale extend approximately 500m north from the edge of the Souris channel and eastward for over two hundred meters from the escarpment along Jock’s Creek. The presence of dense forest vegetation covering much of the locale, and the subsurface nature of the archaeological deposits obscured surface indications.
Radiocarbon dates: Test Unit 4: 1215/320 BP and Test Unit 8 1280/190 BP
Scope and Content
Sub-series has been divided into sub sub series including: Lovstrom survey 1985 and Lovstrom survey 1986
Block A was the most southern site in the locale. The excavation block consisted of 12 contiguous 1m2 units dug in a 3m x 4m rectangle. The block was the least productive of cultural materials, and bone preservation was the poorest. Under the sod, the black loam layer appeared at 5 cm below surface, and the glacial clay at 25 cm below surface. Excavators described the soil matrix as gritty and silty, and it became concrete hard when dried.
The occupation or bone layer extended from 10 to 25 cm below surface and consisted of a contiguous scatter of FCR and unidentifiable large ungulate bone which was heavily processed and intensively scavenged by carnivores. Most cultural materials were recovered within this layer. Fire cracked rock (FCR) and small burnt bone fragments were present but no intact hearths or processing features were evident.
Non-cultural materials included limestone and other natural pebbles derived from the parent till. (These small limestone pebbles were apparent in the occupation layers in other blocks as well). Root and rodent disturbance was extensive throughout Block A. Most units were excavated to gravelly clay till. Nine of the twelve units were dug to level 4b, which ended at 40 cm b.s.
No further excavations were done at this site. No C14 dates were taken.
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.
