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
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,
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
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.
Georgina Bernice Matiation (Hill) was born in Virden, Manitoba on February 19, 1936, daughter of Gordon and Florence Hill. She received her education at Brandon College (1954-1956). Originally a student in Arts, she graduated from the Teacher Training program in 1956. During her time at Brandon College, Matiation participated in the College Glee Club as well as college track and field meets. She also acted as Junior Ladies Athletic Representative in 1955. In addition, Matiation was was the President of her Normal School class.
Matiation began her teaching career in Hargrave and Melita, before taking a position at Prince Charles School in Portage la Prairie in 1960. She remained at that institution until her retirement in 1991. In addition to her teaching career, Matiation was a past president of the Portage Evening Ladies Curling Club, a past president of the La Prairie Lioness and a leader of CGIT. She was a lifelong member of the Lenore Presbyterian Church.
Georgina Hill married Zane Matiation in 1970. They had no children. Georgina Matiation died on October 28, 1995 in Portage la Prairie at the age of 59 years.
Custodial History
This collection was donated to the McKee Archives by Bessie Marie Hill of Winnipeg on May 1, 1998.
Scope and Content
The collection consists of items collected by Mrs. Matiation (Hill) during her years as a student at Brandon College. The collection contains a scrapbook of photos of students and activities at the College taken from 1954-1956. Fonds includes copies of speeches made by her at various school events, such as her validictorian speech at the Normal School Graduation in 1956. There is also an autograph book with messages to her from friends and classmates. Finally, the collection includes two photographs of students in the 1924-25 Brandon Normal School, and one photograph of the Westminister Presbyterian Church in Brandon.
MG 2 Brandon College Students
2.23 Georgina Matiation (Hill)
The collection is located with MG 2 2.2 Gerald Brown. It was placed there as a result of space issues.
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.
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.
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.
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.
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.
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.
approximatley 65 cm textual records;
approximatley 30 photographs
History / Biographical
Bessie Marie Hill was born in 1933. She graduated from Winnipeg Normal School in 1953. Throughout her forty year teaching career, she taught at Hagyard (1953-56), Melita (1956-62), Shilo (1962-65), Kenora (1965-68), DND Germany (1968-76), Kenora (1976-80), Assiniboine South School Division - Laidlaw (1980-84), and Assiniboine South School District - Royal (1984-92).
Florence Mabel (Nelson) Hill was born on June 19, 1907 in Esterhazy, Saskatchewan. She attended the Brandon Normal School in 1924-1925, then taught at Rose Lea School (1925-1929), Errol, at Lenore (1929-1931) and Ravine School (1955-1956). In 1931, she married Gordon Orval Hill (1898-1969). Together they had three children: Allan Hill, Bessie Marie Hill and Georgina Bernice (Hill) Matiation. Florence Mabel Hill died in Lenore, Manitoba on December 23, 1992 in her 86th year.
Sarah Viola Hill was born on June 28, 1900, and was Florence Mabel (Nelson) Hill's sister-in-law. Viola attended the Brandon Normal School in 1916-1917, and took graduate studies at the University of Manitoba. During her thirty-nine year teaching career she taught at Hagyard, Oak Lake (1917-1918), Cottonwood (1918-1919), Rose Park (1919), Grand Coulee (1919-1920), Virden (1920-1922), Lumsden, Saskatchewan (1922-1925), Lenore (1925-1934), Gunton (1934-1936), Birtle Indian Residential School (1936-1941), Ravine, Lenore (1947-1950), The Pas (1950-1956) and Woodnorth (1956-1966). During the war years, Viola worked as part of the Civil Service in Ottawa in the Department of Finance (1941) and later in Vancouver, B.C. Sarah Viola Hill died on January 19, 1988 at Virden District Hospital.
For biographical information on Georgina (Hill) Matiation, see the Georgina (Hill) Matiation collection (29-1998).
Custodial History
Records in all accessions were in the possession of Bessie Marie Hill until she gave them to Gerald Brown who delivered them to the McKee Archives.
Scope and Content
Accession 33-1999: 1 photograph; 6 cm textual records (c. 1900-1952; predominant 1925-1930)
The accession includes one b/w photograph (30x 36 cm) of the Brandon Normal School 1926.
Textual records include a Herbarium and Plant Description workbook including pressed samples (1900); Florence Nelson’s Dominion Drawing Book 1925-1926; Florence Nelson’s Handwork, 1925-1926; Florence Nelson’s Professional Second Class Teacher’s Certificate, 1928; Florence Nelson’s Reading Course Certificate in The Teaching of History, Educational Measurement; A schoolmaster of the Great City, Manitoba Department of Education Examination 1922 in Drawing; Manitoba Department of Education Inspectors Tests June 1952 Literature Level One; The Canadian Teacher Vol. 34, No. 3, October 1929.
Accession 12-2001: 15 photographs; 55 cm textual records (1916-1950, predominant 1916-1935)
The accession includes a b/w photograph (5x7) of Florence Nelson (Hill); a b/w photo (2 ¾ x 4 ½") of the Birtle Residential School class “when Viola Hill was teaching there"; a b/w (10x14) class portrait of the Brandon Normal School 1916-1917 “Second Class” and 13 b/w photographs of various sizes.
Textual records include a Science Notebook created by Florence Nelson (Hill) c. 1924; 3 documents associated with the work-life and career of Florence Nelson (Hill); 21 Inspector’s “Teacher’s Report” on the teaching performance of Miss Viola Hill [n.d.]; various documents and publications including: Manitoba Department of Education Professional Certification documents; “A Union Jack Figure Drill;” Department of Education (Manitoba) Grade XII examinations in Algebra, Geometry, French, Rhetoric and Prose Literature, History of English Literature, Composition, Additional English – A, Tennyson, Additional English – B, Browning, History; Physical Science: A Handbook of First Aid (Toronto: Bauer & Bauer); Santa Claus Christmas Book [no publisher, nd]; School Broadcast Materials, Manitoba Department of Education in co-operation with the Canadian Broadcasting Corporation; Bernhart P.O. Horst (ed.), The New Teachers’ and Pupils’ Cyclopedia – A Reference Library of History, Geography, Biography, Literature, Economics, Civics, Arts, Sciences, Discoveries and Inventions (Holst Publishing Company); The Source Book: An International Encyclopedia Authority written from the New World Viewpoint. 10 volumes including study guide and index; Walter Keast, Canadian Business Arithmetic, Part I. (Pitman; E.C. Hills & R.T.); Holbrook (ed.), French Short Stories with vocabulary and notes (Copp Clark); Clarence Perkins, Introduction to World History. Educational Book Company.
Accession 5-2003: 15 b/w photographs and four certificates (1955-1956)
The accession includes 15 b/w photographs of members of the Brandon College Teacher Training Class of 1955-56. Textual records include the Graduation Certificate for Georgina Bernice Hill, and other certificates.
Accession 16-2008: 3mm texual records and eight certificates/diplomas (1917-2007). Accession consists of certificates, grades, contracts and correspondence relating to the education and teaching career of Sarah Viola Hill and a newspaper clipping and biographical sketch concerning Bessie Marie Hill.
Notes
History/Bio information provided by Bessie Marie Hill. The Normal School photograph from accession 33-1999 has been located with the Normal School collection in the map drawers of the Reading Room.
Storage Location
2003 accessions
Storage Range
2003 accessions
Related Material
Georgina (Hill) Matiation is Bessie Marie Hill's sister. Her records are located at 29-1998.
The Brandon Hills Busy Bees was formed in 1916 by eighteen women. The aim of the group was to assist with the war effort during World War One. At the end of the war it was decided to carry on the club and do community and welfare work. The Busy Bees met twice a month and, during World War Two, one meeting a month was devoted to Red Cross work.
In 1969, the younger members of the Brandon Hills Busy Bees decided to form their own organization called the Brandon Hills Community Fireflies.
The remaining members of the Busy Bees continued in their work until they disbanded as a society on September 14, 1988. At their last meeting it was decided to donate their records to the McKee Archives (minutes September 14, 1988).
Custodial History
In the minutes for the September 14, 1988 meeting of the Brandon Hills Busy Bees, Mrs. Mollie Baker made a motion to donate the record books of the organization to the Archive at Brandon University, and for Mrs. Nell Baker and Mrs. Lillian Coate to take them there. The motion was seconced by Mrs. Jean Kreller. Prior to their donation to the McKee Archives in 1988 the records were in the possession of members of the Brandon Hills Busy Bees.
Scope and Content
Fonds consists of minute books with membership lists, accounts, newsclippings, correspondence, and reports, recipies (Treasurer's BK 1917-1919), treasurer's books, donation records, 2 photographs (1916 and ca. 1970s), a history of the Busy Bees 1916-1976 and calendars for the Womens' Auxiliary to the Grain Growers (Oakville, MB) for 1916-1918.
The mintue book for 1976-1981 also contains the minute book of The Red Cross Emergency Unit, Brandon Hills for December 1943-1947.
Notes
Description by Christy Henry.
Storage Location
2006 accessions
Storage Range
2006 accessions
Related Material
Albert Angus Murray McPherson collection (21-2006)
Bertha Miriam Clark was born on Prince Edward Island but attended public and high school in Brandon, MB. She was a member of the Class of 1929 and served as Lady Stick in her final year at Brandon College.
Clark married J. Scott Leith, Brandon College Class of 1928. Scott and Bertha Leith's son James Clark Leith is in the Canadian Who's Who.
Custodial History
Album was sent to Pat Britton, Brandon University Director of Alumni Relations, by Bertha Leith in April 1991. Britton then transferred it to the McKee Archives.
Scope and Content
Fonds consists of a small accordian style photograph album (7 x 10.5 x 3.5 cm) created by Bertha Clark during her years at Brandon College. The photographs, which measure 4" x 2.75", depict numerous people and events.
Notes
History/Bio information taken from the 1928-1929 Sickle.
Cover of Young School minute book is moderately damaged, but pages are in good condition with only minor water damage and a few ripped pages.
History / Biographical
Dorothy Cox (nee Frost) moved from Elm Creek to Justice in 1946 to work as a schoolteacher. In 1948, she married Laval Cox and together they had four children: Larry, Herd, Rosalie and Heather.
In 1949, Dorothy and Laval purchased Gibb Gillespie's PSV business and began hauling grain, cattle and agricultural equipment. Dorothy went back to teaching in 1959, first at Justice and then Elton Collegiate. After retiring from teaching in 1978, Dorothy started a greenhouse, which operated for 21 years.
All six members of the Cox family were active in community events and organizations. Dorothy was involved in establishing the baby band in 1951; her sons Larry and Herb were members. Along with Laval, Dorothy was a leader of the Cubs in 1955-1956 and again in 1958-1959. Laval was the leader of the local hockey club in 1958, and of a bible study group in 1960. Larry, Herb and Rosalie were avid skaters in 1960-64. Heather and Rosalie were enrolled in senior grades of Sunday school in 1970.
Custodial History
Records were collected by Dorothy Cox, a resident of Justice, over a number of years. She donated them to the McKee Archives on April 4, 2012.
Scope and Content
Collection consists of records related to the history of the Justice district. It includes a history of the Justice Church (1910-1970); minute and expense books for the Justice Hockey Club (1949-1966); a minute and expense book for Young Protestant School (1884-1898); a copy of the Justice 100th Anniversary community history (2009); and four color photographs of Justice Church.
Notes
History/Bio information taken from the content of the collection. Description by James Heaman (2012).
John C. Cousins was the son of Thomas Cousins (b. August 17, 1882 in Truro, Nova Scotia - d. March 5, 1914) and Mary Margaret Craig (b. April 14, 1824 - d. April 25, 1903). He married Eunice Eliza Nixon from London Township, County of Middlesex, Ontario. Together they had three children: Eunice M., Eric O. and Kathleen. J.C. Cousins was Reeve of the Rural Municipality of Daly from 1905 to 1910 and Assessor for the Town of Rivers from 1931-1938.
Custodial History
Record was accessioned in 2007 by the McKee Archives. Prior custodial history unknown.
Scope and Content
This document is a rambling memoir of John C. Cousins' recollections of life in the Rural Municipality of Daly from the settlement era in the early 1880s, through to the 1940s. He touches on various themes, including: his family history; the activities of the R.M. of Daly and his role as Reeve; the history of school districts in the municipality (lists names of first teachers and early students); the history of churches in the municipality; tragedies in the municipality; lists members of the Council of the municipality for the years 1885-1946; and the devastating impact of the Spanish Influenza on Aboriginal people in the municipality.
In addition, the memoir includes documentary records, such as minutes and copies of letters. There are also many photographs of both events and individuals (virtually all of the photographs are labelled and names are provided). The memoir goes beyond a simple recounting of facts. Cousins is discursive and thoughtful, often making references to developments happening in other parts of North America and Canada. There is also a link to the Maritimes, from which his family originated.