BRANDON COLLEGE BUILDING
The construction of the Brandon College Building, also known as the Original Building, was primarily financed by Mr. and Mrs. William Davies, a Toronto based Baptist meat packer, and his sister Mrs. Emily Davies, also of Toronto, who pledged $5,000 a year for five years to the new Baptist College. Four city blocks between 18th and 20th streets were purchased for the College campus and the tender of Messrs. T.M. Harrington of Winnipeg was accepted in the spring of 1900; Mr. Hugh McCowan of Winnipeg appointed as architect. Mrs. Davies laid the cornerstone for the Brandon College Building on July 13, 1900.
The Brandon College Building was conceived as a substantial five story brick structure with a stone basement. The Tyndall Manitoba quarries, located thrity miles northeast of Winnipeg, supplied the stone and presented the College with the stone steps at the main entrance. The basement contained the dining room, kitchen, laundry, furnace room, a science laboratory, and maids' rooms. The first floor housed the reception room, office, library, four classrooms and the teachers' cloak rooms. The second floor had five classrooms, a reading room, five rooms for resident students and a resident teacher. Teachers' rooms and seventeen rooms for students comprised the third floor; and additional thirteen rooms for residents took up the fourth floor. The residence was to house 70 men. The total cost of the building and furnishings was $44,000. The Brandon College Building was ready for occupancy by October 1, 1901.
CLARK HALL
The cornerstone of Clark Hall was laid by Mrs. A.P. McDiarmid, wife of the Principal of Brandon College, on May 24, 1906. The residence was officially opened on Thanksgiving Day, October 18, of the same year. The construction of the building grew our of a demand for a ladies' college. A canvass made in Eastern Canada had resulted in subscriptions totaling $10,000. When Dr. McDiarmid reported the results of the canvass to the Chairman of the Board, Dr. C.W. Clark of Winnipeg, Clark proposed that he and his wife be allowed to provided the balance of the funds, some $30,000. While presenting the building at the opening ceremony, Clark stated that the reason for his donation was his belief in the power of cultured womanhood - he believed "that refined and Christian mothers were the strength of a nation and that he wished to see in Brandon a chool of learning for women in which every Christian virtue and grace might be illustrated."
Clark Hall was built immediately north of the Brandon College Building and was connected to it by classrooms and the iron door with its door bell, which was rung by gentlemen before being admitted. It is a five story brick building, with fittings of imported Georgia pine. In the basement was the gymnasium, studios and maids' rooms. On the main floor was a spacious reception room furnished by the Honorable A.C. Rutherford, the Premier of Alberta and the Lady Principal's suite, furnished by Mrs. N. Wolverston, wife of the treaurer of the College Board. Music studios and the offices of the resident matron were also on the main floor. The second and third floors were dormitories. The fourth floor was meant to be art studios, but due to registration demands, it was divided into students' rooms. The residence was designed to house fifty students and seven teachers. Piano practice areas were also designated on the west side of the building and on the groundlevel half way between the basement and the first floor.
BRANDON COLLEGE BUILDING AND CLARK HALL RESTORATION PROJECT
By the early 1990s, it was clear that major reconstruction work on the Brandon College Building and Clark Hall was necessary if the buildings were to remain in use. The alternative was to demolish both buildings and construct a new central administrative structure for the campus. Because of the historic character of the two original campus buildings, the decision was taken to mount a complete restoration of the structures that involved a complete removal of everything except for the surrounding brick fascade and the construction of new buildings within the old external walls. This project was financed by the Provincial government of Manitoba, who granted the University approximatley 10 million dollars. The Chief Architect for the restoration was George Cibinal. Work began in 1996 and was completed by the fall of 1997. In addition to the restoration of the Brandon College Building and Clark Hall, a new entrance was built on the west side of the buildings, as well as an addition to Clark Hall, which included a skywalk connecting it to the A.E. McKenzie Building.
Scope and Content
Sub-series consists of photographs of the Brandon College Building and Clark Hall.
Notes
History/Bio information was taken from Brandon College: A History, 1899-1967 by C.G. Stone and F. Joan Garnett (Brandon, Manitoba: Brandon University, 1969), chapters 2 and 3. Tom Mitchell provided history/bio information on the restoration project.
The Citizens' Science Building was built in 1922 and financed by Brandon citizens. It was renamed the Knowles-Douglas Student Union Centre c. 1984 in honour of Brandon College graduates Stanley Knowles and Tommy Douglas, both of the Class of 1930. The Knowles-Douglas Addition was completed in 1987.
Scope and Content
Sub-series consists of photographs of the Citizens' Science Building and the Knowles-Douglas buildings, which include the Knowles-Douglas Student Union Centre and the Knowles-Douglas Addition.
The Gymnasium is located on the southside of Louise Avenue at the corner of 20th Street. It was completed in 1965 and houses the Athletic programme, which includes both intercollegiate sports and intermural sports and recreation. In the 1960s, it was also the venue for student dances and performers, including Gordon Lightfoot, the Mitchell Trio, the Guess Who and others. Convocation was also held in the Gym for a number of years. In 2007, a financial campaign was launched to raise money for extensive rennovations to the Gym.
Scope and Content
Sub-series consists of photographs of the Gymnasium.
The Original Music Building was completed in 1963. The School of Music moved to the Queen Elizabeth II Music Building in 1985. From c.1986 until 1997, the Original Music Building housed Student Services. Since 1997, the building has been used by the School of Health Studies; a new segment was added to the Original Music Building in 2003 to create the Health Studies Complex.
Scope and Content
Sub-series consists of photographs of the Original Music Building and the Queen Elizabeth II Music Building.
Notes
Queen Elizabeth II Music Building has been abbreviated to QEII Music Building.
Arrangement
All photographs of the Health Studies Complex, which includes the Original Music Building, are part of BUPC sub-series 2.10.
The John R. Brodie Science Centre was completed in 1971, with the official opening on May 7, 1972. It is located in the southeast corner of the campus and houses the Faculty of Science. The Brodie Building was named for John R. Brodie, a Brandon man who donated $250,000 to Brandon College in 1963 with the stipulation that the money be used for a Science Centre.
Scope and Content
Sub-series consists of photographs of the John R. Brodie Science Centre.
Notes
Additional biographical information on John R. Brodie is available in his bio file in the Reading Room.
The Jeff Umphrey Memorial Centre was completed in 1970 and is located on the north side of Victoria Avenue and 20th Street. Campus Books was located in the basement of the Umphrey Centre from 1970 to 1978. Once Campus Books moved to the lower McMaster Concourse, the University Archives occupied the basement from 1981 to 1997. A branch of the Bank of Montreal was located on the west side of the building until c. 2006 when the Department of Fine Arts moved into the Umphrey Centre and the Glen P. Sutherland Gallery was constructed on the main floor.
Scope and Content
Sub-series consists of photographs of the Jeff Umphrey Memorial Centre and the various University organizations that have operated out of the Centre.
Physical Plant provides security, workplace health and safety, building maintenance, utilities, cleaning, groundskeeping, and key storage services, as well as capital project management for the Brandon University campus. It includes the new Physical Plant building and new steam plant on 20th Street and the Site Services building on the corner of 20th Street and Louise Avenue. Prior to the opening of the new Physical Plant building in 2010, services were operated out of World War II era H-Huts in the centre of campus. The original steam plant (1962-1990s) was sold following the construction of the new steam plant.
Scope and Content
Sub-series consists of photographs of Physical Plant buildings including: the original Steam Plant; the (new) Steam Plant; the Site Services Building; the Physical Plant H-Hut; and the new Physical Plant building.
H-Huts refer to structures built to house military personnel at the Commonwealth Air Training Program just north of Brandon during World War II. The name H-Hut derives from the layout of the structures, which were built in an "H" formation. The original H-Huts were moved onto the Brandon College campus in 1956 to house the library and arts classrooms.. Additional H-Huts have been located in various places and used for various departments and services on campus including Student Services, Continuing Education, and the carpenter's workshop. Only the Physical Plant H-Huts, located to the west of the Knowles-Douglas Student Union Centre, remain on campus in 2007.
Scope and Content
Sub-series consists of photographs of various H-Huts on campus.
DARRACH HALL
Darrach Hall is the men's residence and was completed in 1961. It is named after Robert and Sarah Darrach.
FLORA COWAN HALL
Flora Cowan Hall is the women's residence and was completed in 1962. It is named after Flora Cowan.
MCMASTER HALL
McMaster Hall is the co-ed residence and was completed in 1971. It is named in honour of Brandon College's association with McMaster University
DINING ROOMS
The Main Dining Room was completed in 1961 and is connected to all three residences either by a link (Flora Cowan Hall), the McMaster main concourse (McMaster Hall) or a hallway (Darrach Hall). Within the Main Dining room is the Louis Riel Room. The Louis Riel Room was previously the Small Dining Room, and later the Private Dining Room. It was renamed the Louis Riel Room in 2008 in honour of the Métis leader’s contribution to Manitoba history and heritage, as well as in honour of ongoing contributions to the University made by the Manitoba Métis Federation and the Louis Riel Institute. The room is often used to host dignitary dinners, awards and recognition ceremonies, seminar and conference sessions and other special events.
Scope and Content
Sub-series consists of photographs of Brandon College/University's three residences: Darrach Hall, Flora Cowan Hall and McMaster Hall, as well as images of the dining rooms.
Notes
History/Bio information for the Louis Riel Room was taken from the Brandon University website, available at: http://www.brandonu.ca/news (February 2008).
The Duthie site is the first site identified in the Makotchi-Ded Dontipi locale. It was reported to Dr. Bev Nicholson by Doug Jackson, a local collector who had observed archaeological materials that had been exposed during the construction of Maple Hill Road northwest of Lauder. The site is named after the landowner, Randy Duthie.
The initial inspection of the exposed materials indicated that the eastern half of the site had been severely impacted by raising a road grade using an elevating grader. However, an undetermined amount of the site remained to the west, flanked by a low sand dune. Testing and preliminary excavations were conducted in 1992-93. In 1994 a field school added to the excavated sample. The undisturbed portion of the site, west of Maple Hill Road was situated at the base of a low sand dune and had an aspen and willow forest cover. The water table was approximately one meter below surface at the time of excavation. A rising water table has since prevented further excavations.
Two dates on bone collagen were obtained during excavations. These were 880+/-80 B.P. (Beta 62705) and 970+/-40 B.P. cal. 1030 A.D. (TO 13366). These dates are consistent with an Initial Middle Missouri cultural assignment. The site occupation is identified by the distinctive ceramics found there. Ceramics at the Duthie Site are tool impressed with incising and lip modeling with fabric impressions on most vessels. Jill Taylor analysed the ceramics from the site for a Specialist thesis, Brandon University (1994) and a Masters of Arts degree from the University of Saskatchewan. (Taylor 1995).
Analysis of residue from Duthie site pottery by Matthew Boyd recovered corn (Zea mays) phytoliths and bean (Phaseolus sp.) starch grains indicating consumption of these domesticates at the Duthie site. (Boyd 2006)
The occupation of this site indicates a migration of people from the south who were well acquainted with horticultural farming. These people had previously migrated to South Dakota following river valleys into the central plains from the eastern woodlands during late Hopewell times. It appears that they later migrated well to the north into southern Manitoba but there is no evidence that they remained there for more than a single year.
Boyd, M., C. Surette and B.A. Nicholson. 2006 Archaeobotanical Evidence of Prehistoric Maize (Zea mays) Consumption at the Northern Edge of the Great Plains. Journal of Archaeological Science 33: 1129-1140.
Taylor, J. 1994 An analysis of the ceramics recovered during 1992 and 1993 at the Precontact Duthie Site (DiMe-16). Specialist thesis, Brandon University.
Scope and Content
The Series has been divided into seven sub-series, including (1) Duthie site (2) Jackson site (3) Twin Fawns site (4) Vera site (5) Schuddemat site (6) Bradshaw site (7) Hollow B site.
Aerial photographs of the campus were generally commissioned by the College/University to record important milestones, such as centennials, changes in status, and building projects. The general campus photographs were placed in this sub-series because the composition of the images made it difficult to place them with individual buildings.
Scope and Content
Sub-series consists of photographs of the Brandon College and Brandon University campus.
The J.R.C. Evans Lecture Theatre and the A.E. McKenzie Building were both completed in 1960. The Evans Theatre is named for John Robert Charles Evans, who served as president of Brandon College from 1928 to 1959. The A.E. McKenzie Building was originally the Library and Arts building, and was named for A.E. McKenzie, a local businessman and supporter of the College. The George T. Richardson Centre, which includes the Evans Theatre and the John E. Robbins Library, was completed in 1993.
Scope and Content
Sub-series consists of photographs of the A.E. McKenzie Building, the George T. Richardson Centre, the J.R.C. Evans Lecture Theatre, the John E. Robbins Library and the link between the Evans Theatre and the McKenzie Building.
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.
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,
Block B consisted of 20 contiguous 1m2 units excavated to 30 cm below surface. (except unit 58 which was excavated to 35 cm bs to obtain extended soil profile). The block is situated in recent oak and poplar forest at the head of a ravine leading to Jock’s Creek, adjacent to an area cleared for market gardening. As was the case with Block A, the understory is heavily overgrown with hazelnut, chokecherry, saskatoon, and a poison ivy/sarsaparilla ground cover.
The soil levels below the sod in Block B consisted of a black, silty, and gritty loam layer from 5 cm to 23 cm below surface, a yellow and sandy clay from 23 cm to 30 cm below surface, and glacial till at 30 cm below surface. As in Block A, limestone cobbles were found throughout the occupation level around the bone. It is evident that bioturbation – primarily tree roots and rodent burrowing – have significantly altered patterns of original deposition of lithics, ceramics and small bone.
The faunal layer lay close to the surface, situated entirely in the black loam 5 cm – 23 cm below surface. The 23 cm depth also marked the end of the dark silty loam. At 10 cm below surface, a discernible patterning of the bone appeared. Concentrations of bone in narrow rows ran in an irregular pattern from the northwest to the southeast part of the block. This pattern was most apparent in the north end of the block which is the highest point in the block. In the same 1m2 unit, patches of weathered, very poorly preserved bone would be found lying close to patches of well preserved bone. It is believed that this variability in preservation results from uneven rates of burial due to taphic activities of pocket gophers or other agents of bioturbation. The same pattern of uneven preservation occurs over much of the locale but is most evident in Block B.
Diagnostic lithics included eleven projectile points that were predominantly Plains or Prairie Side-notch types, but included two unnotched triangular points. Cord-wrapped impressed rim sherds and body sherds were recovered. The ceramics are variants of the Woodland Blackduck horizon.
RC dates: XU49 – 675/80 BP XU 59 – 705/75BP.
Scope and Content
Sub-sub-sub series contains: Summary information of field methology, number and co-ordinates of excavations, personnel and their staff position; Field journals are daily records of recoveries, features and activities at the site; Site records include excavation level and unit summaries, feature sheets, profiles; sample records and maps; Artifact catalogues are lists and identifications of all artifacts recovered; Photographs are of excavation units, features, the landscape and personnel.
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.
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
