Radiocarbon date reports have been scanned in multi-page PDF files.
History / Biographical
The North Lauder locale has a long archaeological and geological history that is important for understanding the forces that shaped the region. Archaeological research in the locale shows that the area has been occupied by humans for at least the past 6,500 years. Environmental forces provided an area of diverse resources that attracted early peoples.
Archaeologists from Brandon University have been conducting research in the North Lauder locale that has focused on the Atkinson site, a 6,500 year old hunter-gatherer site and Flintstone Hill.
The geomorphology of the glacial Lake Hind Basin over the past 11,000 years is known primarily through the study of a cut bank along the Souris River. Flintstone Hill contains the most complete stratigraphic record for the post-glacial period on the northern plains. The site has been extensively studied by geoarchaeologists, geologists and paleoenvironmentalists over many years and their findings have contributed to our understanding of the region.
Radiocarbon dates were obtained from the Atkinson site and Flintstone Hill.
Radiocarbon dating
The technique of radiocarbon dating was developed by Willard Libby and his colleagues at the University of Chicago in 1949.
Radiocarbon dating is used to estimate the age of organic remains from archaeological sites. Organic matter has a radioactive form of carbon (C14) that begins to decay upon death. C14 decays at a steady, known rate of a half life of 5,730 years. The technique is useful for material up to 50,000 years. Fluctuations of C14 in the atmosphere can affect results so dates are calibrated against dendrochronology. Radiocarbon dates are calibrated to calendar years.
Dates are reported in radiocarbon years or Before Present. Before Present refers to dates before 1950. The introduction of massive amounts of C14, due to atomic bomb and surface testing of atomic weapons, has widely increased the standard deviation on all dates after A.D. 1700 causing these dates to be unreliable.
Accelerated mass spectrometry can more accurately measure C14 with smaller samples and can date materials to 80,000 years.
Scope and Content
Sub sub series contains radiocarbon dates from: the Atkinson site and Flintstone Hill.
See RG 6 Brandon University fonds, 7.4.1 Dean of Music for biographical information.
Custodial History
The records were collected during the course of Jones' career as a member of the School of Music and as Dean of the School of Music. They remained in his possession until their donation to the McKee Archives on June 29, 2011.
Scope and Content
Collection consists of records created and collected during the course of Lawrence Jones' teaching career in the School of Music and during his tenure as Dean of the School of Music at Brandon University.
Records include: dean's log books; recital programs and related materials; personal documents; academic papers; planning documents; contracts; administration documents; workshop documents; teaching documents; proposals; reviews; evaluations; violin concerto by S.C. Eckhardt-Gramatte, piano score, edited by Lawrence Jones. Topics include: planning for the School of Music; Master's degree program; award winners; the music building expansion; adjudicating; the New Brandon University Trio; and the National Music Festival.
The Westman Recycling Council was started by a small group of avid recyclers with financial and volunteer help from the Kiwanis Club of Brandon, among others. Volunteers organized the first outdoor recycling depots in June and October 1989. The first event with recorded minutes was the first annual meeting, November 15, 1989.
The organization was incorporated in February 1990, and became a registered charity in 1995. The Mission Statement was: "to support and promote the reduction, re-use, and recycling of material resources for the benefit of Westman's environment and future generations."
The major partner in the work of the organization was the City of Brandon. In 2003, Westman Recycling, in partnership with the City, built a Material Recovery Facility (MRF) at the Brandon Landfill; Westman Recycling owned the building on the City-owned land. It was a $4 million structure - financed by federal and provincial grants (about one-quarter of the total) and a mortgage (about three-quarters). Details are in the Board and other Committee minutes and agreements.
In late 2005, Westman Recycling faced a severe cash crunch - as a result of poor markets for recyclables, changes in support funding from the Manitoba Product Stewardship Corporation (MPSC), and a drop in public recycling levels. In February 2006, the City decided to sign a contract with another organization to operate the MRF; after that there appeared to be no role for Westman Recycling.
A general meeting on September 22, 2008 voted to dissolve the organization. At that meeting, the suggestion was made (agreed to by consensus) that the files of the organization be donated to Brandon University to be made available for researchers. A Board of Directors meeting on the same date voted to donate all remaining funds to a perpetual "Westman Recycling" fund with the Brandon Area Community Foundation.
A final wind-up meeting was held on March 26, 2009
Custodial History
The organization was overseen by volunteers / volunteer Board of Directors. The files were first held by volunteers / Board members in their homes. In May 1991, the organization hired David McConkey as Coordinator / General Manager, who was directed by the Board to manage the files on a daily basis from that date forward.
The files were kept in the organization's rented office space in the 1300 block of Pacific Avenue from May 1991 to September 1992, and then in the rented space in the Massey building at 6th Street and Pacific Avenue. The files were kept at the new facility at the landfill from April 2003 to February 2006. They were then stored in the basement of the Marquis Project, 912 Rosser Avenue, until August 2011 when they were donated to the S.J. McKee Archives, Brandon University.
Some files (e.g. minutes from 1995-96) were found to be missing entirely. Other files were disposed of by recycling and/or shredding as they were judged to be confidential (e.g. personnel), of an ordinary business nature only (e.g. invoices), or not useful for future research (e.g. extra copies, routine correspondence, building and equipment plans and other arrangements).
Scope and Content
Fonds consists of records that document the origin, activities, demise, and legacy of the Westman Recycling Council. Records include minutes, financial summaries, scrapbooks, newsletters, brochures, media clippings, photographs and miscellaneous documents related to the construction in collaboration with the City of Brandon of Brandon's principal recycling facility.
Notes
Administrative history courtesy David McConkey. See additional notes on the organization in the curatorial file. Description by Tom Mitchell.
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.
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.
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
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.
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.
Radiocarbon date reports have been scanned in multi-page PDF files.
History / Biographical
The Crepeele locale is located within the larger Lauder Sandhills area, located in southwestern Manitoba. The area is a complex region of high biodiversity made up of stabilized sand dunes and wetlands that encourage the development of mixed forest and grass prairie. This area provided a variety of subsistence resources for pre-European hunter-gatherers. At the present time the grass prairie is now farm land but the areas of vegetated sand dunes have not been cultivated and have revealed numerous pre-contact archaeological sites.
Archaeological surveying was conducted in 2003. The results of the 2003 Casselman survey showed over 300 test uints contained cultural material and indicated several areas for further examination including the Crepeele site DiMe-29, Sarah site DiMe-28 and Graham sites DiMe-30.
From 2003 to 2008 field work took place at the locale with 75 - 1m x1m units excavated. The Crepeele locale is a complex region of high biodiversity made up of stabilized sand dunes and wetlands that encourage the development of mixed forest and grass prairie. This area provided a variety of subsistence resources for pre-European hunter-gatherers. At the present time the grass prairie is now farm land but the areas of vegetated sand dunes have not been cultivated and have revealed numerous pre-contact archaeological sites.
To help establish the cultural sequence at the locale Radiocarbon dates were obtained from the three sites in the Crepeele locale.
Radiocarbon dating
The technique of radiocarbon dating was developed by Willard Libby and his colleagues at the University of Chicago in 1949.
Radiocarbon dating is used to estimate the age of organic remains from archaeological sites. Organic matter has a radioactive form of carbon (C14) that begins to decay upon death. C14 decays at a steady, known rate of a half life of 5,730 years. The technique is useful for material up to 50,000 years. Fluctuations of C14 in the atmosphere can affect results so dates are calibrated against dendrochronology. Radiocarbon dates are calibrated to calendar years.
Dates are reported in radiocarbon years or Before Present. Before Present refers to dates before 1950. The introduction of massive amounts of C14, due to atomic bomb and surface testing of atomic weapons, has widely increased the standard deviation on all dates after A.D. 1700 causing these dates to be unreliable.
Accelerated mass spectrometry can more accurately measure C14 with smaller samples and can date materials to 80,000 years.
Scope and Content
Sub sub series contains radiocarbon dates from: Crepeele, Sarah and Graham sites.
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 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.
1965-1980, predominant 25 May 1965 - 30 September 1976
Physical Description
12 cm textual records
6 b/w photographs (loose)
1 artefact
Physical Condition
Some of the items in the scrapbook have come loose from their pages, some documents are stained from a liquid, likely coffee
History / Biographical
In 1965, Chris Verhoef, member of the Overture Concert Association, Allied Arts Centre, and Brandon Citizens' Commitee for the Performing Arts, called for a meeting of Western manitoba citizens interested in the prospect of a Philharmonic Choir for the region. The meeting took place on 26 May 1965; the steering committee that gathered, led by Margaret Goodman, undertook the formation of the Choir. The Choir would have an Executive consistign of at least four members, and a committee consisting of a minimum seven members. Each executive member would be elected on an annual basis. The Choir's executive, in collaboration with the conductor, would determine the choir's repertoire for the year. The establishment of the Western Manitoba PHilharmonic Choir (WMPC) sought to encourage amateurs to sing for enjoyment, provide the opportunity for a choir to perform choral compositions in collaboration with a symphony orchestra and promote and sponsor the musical arts in the Western Manitoba region. Membership to the choir would be open to all citizens of the region, and members would be accepted based on the discretion of the conductor. The first meeting of prospective members took place on 27 September 1965 in St. Matthews Cathedral parish Hall where more than 90 people gathered and registered to become a member of the WMPC.
Chris Verhoef led the Western Manitoba Philharmonic Choir into its first season as President of the choir's Executive Committee. For the organization's first season, the WMPC hired two members of the Brandon College School of Music: Lucien Needham for the position of conductor and Louise Chapman for the position of accompanist. Brandon College, as well as other donors sponsored the choir for its first season. The Choir held its debut performance in collaboration with the Winnipeg Sympnay Orchestra (WSO) on 12 March 1966, and the Choir's performance of Vivaldi's Gloria and Handel's Dettingen te Deum attracted an audience of more than 1400 people. The performance was well received by the public. The debut performance's asuccess earned the CHoir a rcommendation for a grant from the Manitoba Centennial Corporation that would sponsor a special concert during the centennial year. Furthermore, the Canada Council supported the Winnipeg Symphony Orchestra, by the means of special funds, to make the Symphony's appearance witht he Philharmonic Choir possible.
For the WMPC's second season, membership rose to 111 amateur singers. Verhoef remained as President of the Executive, while the Brandon Citizens' Committee for the Performing Arts provided sponsorship. Following the Choir's performance of Schubert's Mass in Eb Major on 17 November 1966, the membership increased to 132 singers. On 20 January 1967, the WMPC's first taped broadcast was released over CBC and CKX. The broadcast's success resulted in an offer from CBC to record another broadcast for a similar release. The Kiwanis Club of Rivers invited the Choir to perform in Rivers on 25 january 1967. On 7 April 1967, the Choir performed Haydn's oratorio, The Creation, in the Brandon College Gymnasium.
The choir elected Murray Ames as President to lead it through its thrid and fourth seasons. In its third season, the WMPC, conducted by Leonard Mayoh, performed Handel's Messiah on 22 November 1967 in the Brandon University Gymnasium. The Choir's spring concert, name the "Chris Verhoef Memorial Concert," in honour of Chris Verhoef who had passed away December 1967, featured works by Bach, Brahms and Perry. Held on 9 March 1968, in the Brandon University Gymansium, the concert featured Brandon university student James Stewart as soloist and was received with great praise. In addition to the memorial concert, the WMPC also established a $500 scholarship for a Brandon University music student to honour Verhoef's substantial contribution to the community.
The first concert of the Western Manitoba Philharmonic Choir's fourth season was held on 10 December 1968, in the J.R.C. Evans Lecture Theatre at Brandon University and featured selections from Handel's Messiah. A piano trio comprised of Francis Chaplin (violin), Malcom Tait (cello) and Gordon Macpherson (piano), as well as a brass trio, also performed at the chori's winter concert. In its fourth season, the WMPC performed two concerts in the second half of its season. On 15 FEbrurary 1969, in cooperation with CKX Radio and Television, the choir performed works by Mozart, Hindemith, and Mahler in collaboration with the Winnipeg Sympony Orchestra conducted by George Cleve. Later in the season, the choir performed Brahms' Requiem Mass, once again in collaboration with the Winnipeg Symphony Orchestra.
Dr. R. Parker filled the position of President of the Executive for the duration of the Choir's fifth, sixth and seventh seasons. The fifth season saw the WMPC performing four concerts. Conducted by Leonard Mayoh, it opened its season on 11 october 1969 with a performance at the Grand Finale of the Grand Opening of the Western manitoba Centennial Auditorium, performing theoverture to Mozart's The Magic Flute and Beethoven's Symphony No. 9. Their Christmas concert, also conduceted by Mayoh, took place on 10 December 1969. The Choir's third concert of its fifth season was held on 31 january 1970, in cooperation with CKX RAdio and Television, and featured works by Mendelssohn, Ravel, and Schubert, in collaboration with the WSO under the direction of conductor George Cleve. The season concluded with another concert in collaboration with the WSO on 7 March 1970, conducted by Leonard Mayoh. This concert featured works by Vaughn Williams, Handel and Poulenc.
Seasons six and seven consisted of two concerts each. The Choir held its fifth annual Christmas Concert on 5 December 1970. Led by Leonard Mayoh, it performed its spring concert on 10 April 1971 in collaboration with members from the Winnipeg Symphony, featuring selections by Bach and Mozart in the Western manitoba Centennial Auditorium. Into its seventh season, the Choir performed Bach's Christmas Oratorio on 4 December 1971 in the Central United Church. For its final concert of the year, the WMPC revisited a piece that had been the main focus of its second season: Haydn's oratorio, The Creation. The Choir performed this Haydn masterwork on 8 April 1972 under the direction of Piero Gamba.
Helen Riesberry led the choir through its eigth and ninth seasons as President of the Executive. In its eigth season, the WMPC held its annual Christmas concert on 12 December 1972 in collaboration with the Winnipeg Symphony Orchestra in the style of a sing-along led by Mitch Miller. The choir's spring concert featured another masterwork, Beethoven's Missa Solemnis, conducted by Piero Gamba. The WMPC and members of the WSO performed the Requiem Mass on 28 April 1973 at the Western Manitoba Centennial Auditorium. Despite the lack of attendance at rehearsals since the Christmas concert, the WMPC presented an overall effective performance of the challenging Requiem Mass.
In its ninth season, Derek Morphy took over the position of conductor from Leonard Mayoh. Morphy had his debut performance as conductor with the WMPC at the annual Christmas concert on 17 December 1973. In March 1974, in collaboration with members from the WSO, Morphy led the Choir in its performance of Mendelssohn's oratorio, Elijah, in the Western Manitoba Centennial Auditorium. later in the season, the choir performed a concert entitled "Reflections," a choral programme for Lent and Easter, accompanied by organist Arthur Bower.
Nearing the end of its ninth season, the Philharmonic Choir encountered severe financial challenges. The Choir released a notice in the newspaper that the anticipated $3000 grant from the Manitoba Arts Council had been cut to $1000, leaving the Choir $3100 in debt. The notice explained that the Choir needed funds in order to enable operation and continue hiring the WSO for concerts. The WMPC executive and committee held a Leonard Mayoh Night in an attempt to gain funds and donations. Although the Manitoba Arts Council raised thegrant to $2000 and the City of Brandon contributed $500, the Choir's financial situation remained in a dire state as its ninth season came to a close.
The Choir elected Edith Hayden to lead it through its tenth and eleventh seasons as President of the Executive. The opening of the tenth season challenged the WMPC. In addition to its financial woes, the Choir's Executive struggled to overcome the lack of attendance at rehearsals and the shortage of male voices. The WMPC had experienced membership issues in earlier seasons as well. In its third season, despite a membership of 130 individuals, the choir had struggled to create a balanced sound due to a lack of male membership and therefore a lack of lower voices. In its sixth season, the Choir opened their concert year with an appeal for members. In an effort to improve the choir's financial affairs, the Choir Executive and conductor decided against hiring the Winnipeg Symphony Orchestra for the time being. In an attempt to improve the situation, Derek Morphy wrote a letter to the members of the Choir outlining his concern that he may not be meeting their expectations as a conductor but hoped to generate positive and hopeful prospects for the future of music-making together.
The Choir's annual Christmas concert featured a collaboration with the Brandon School Division Music Department and Brandon School Orchestra and Band Association, as well as dancers choreographed by Barbra Enhes. The WMPC performed Haydn's Mass in D minor at its spring concert on 27 April 1975, accompanied by Arthur Bower. By the end of the season, the Western Manitoba Philharmonic Choir's financial situation had begun to improve.
The WMPC hired conductor peter Allen to lead the Chori through its final season of operation. The Choir held its annual Christmas concert in the Central United Church on 7 December 1975, and featured Vivaldi's Glora, accompanied by pianist Barry Anderson. The choir perfomed Deller's Psalm 148, Teleman's Cantata for the Fourth Sunday after the Feast of the Three Kings, and Dvorak's Stabat Mater at its spring concert held at the Central United Church on 25 April 1976.
Despite its best efforts, the Western Manitoba Philharmonic Choir's first rehearsal of its twelfth season saw just 26 members in attendance. As a result of lack of membership, the Choir Executive decided to disband the WMPC for its 1976/1977 season, with plans to reassess the situation in September of 1977 for the prospect of a 1977/1978 season. Matters were further complicated by financial considerations; by June 1977 the choir's financial situation had worsened as a result of the administrative fees that the WMPC covered for the duration of its unexpected inactive 1976/1977 season. Unlike past years, there were not any ticket sales to cover such expenses.
Following its year off, membership interest in the Western Manitoba Philharmonic Choir did not increase and the decision was made not to return for another season. In 1980, the WMPC revoked its registration as an organization and officially ceased to exist.
Custodial History
Records in the 8-2001 accession were donated to the McKee Archives in 2001, by three representatives of the Philharmonic Choir: Dr. Bill Paton, Botany Department, Brandon University; Mrs. Edith Hayden, WMPC President; and Mary Davidson WMPC Archives Committee. Records in accession 13-2016 were given to Terry Stamper in the School of Music by Marilyn Hayden and then transferred to the McKee Archives on September 21, 2015.
Scope and Content
Fonds consists of records that document the origin, activities, and ultimate disbandment of the Western Manitoba Philharmonic Choir. These records were created and accumulated during the eleven year existence of the WMPC.
Records include: the organization's constitution and history from 1965-1968; financial records, which include grants received from the Manitoba Arts Council, Canada Council, and City of Brandon, as well as materials documenting the organization's financeial struggles from 1974-1976; minutes from executive and committee meetings from 18 June 1973 to 24 June 1974; correspondence in the form of letters between the president of the executive and the choir members, and between the conductor of the choir and its members; membership lists from each season of the WMPC; and concert programmes from every major Christmas and Spring concert that the organization performed. Fonds also contains mewspaper notices, advertisements and reviews of various performances, as well as posters advertising perfomrances of the WMPC in the 1967/68, 1970/71, 1971/72 and 1973/74 seasons; the posters advertise the choir, collaborators, patrons and featured works.
Also included in the fonds is a scrapbook detailing the choir's history. Each page of the scrapbook is decorated with hand painted images of plants native to the southwestern Manitoba region. The scrapbook includes concert programs and photographs of the choir from all years of the organization's operation. The scrapbook also contains an assorment of informal photographs from various WMPC events. There are also six black and white group photos of the WMPC from various seasons.
Finally, the fonds contains one artifact, a leather bag/zippered file folder with "WMPC" printed on it.
Notes
History/Bio information was provided by representatives of the Western Manitoba Philharmonic Choir. Copies of the history can be found in the fonds. Description by Jessi Gilchrist (October 2016).
