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 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 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 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 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.
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.
ARCH 2: North Lauder Locale
The North Lauder locale has a long archaeological and geological history that is important for understanding the forces that shaped the region. Archaeological research in the locale shows that the area has been occupied by humans for at least the past 6,500 years. Environmental forces provided an area of diverse resources that attracted early peoples.
Environment of the Lauder Sandhills
The North Lauder locale is part of the greater Lauder Sandhills area. The glaciers that covered this region began to recede approximately 11,000 years ago leaving a large lake known as glacial Lake Hind. The Souris River, the Lauder Sandhills and the Oak Lake Aquifer are remnants of the environmental and geological forces that shaped the region.
The Lauder Sandhills region is characterized by a landscape of sand sheets and stabilized sand dunes interspersed with a variety of wetlands. This complex topographic and hydrological situation favoured the development of an island mosaic of mixed forest, wetland and meadow, surrounded by mixed grass prairie. The result was a large, isolated ecotone which provided a rich variety of subsistence resources for hunter-gatherers.
Research in the Lauder Sandhills
Archaeologists from Brandon University have been conducting research in the Lauder Sandhills since 1991. Research in the North Lauder locale has focused on the Atkinson site, a 6,500 year old hunter-gatherer site and Flintstone Hill.
The Atkinson site
The Atkinson site is one of the oldest excavated sites in Manitoba and has been Radiocarbon dated to 6,500 years before present. The Atkinson site is located on the bank of the Souris River and was discovered when a hearth (fire pit) was seen eroding out of the bank. Based on the date of the site and the kind of lithics (stone tools) present it is considered a Gowen occupation. The Atkinson site is evidence that bison hunters were active on the northern plains at a very early date. Similar sites have also been found on the High Plains in the U.S. and are referred to as the Mummy Cave Complex.
The Atkinson Site is of great importance as it is the first undisturbed site of this type to be excavated in Manitoba and extends the range of these sites south and east from the type-sites in central Saskatchewan.
Flintstone Hill
The geomorphology of the glacial Lake Hind Basin over the past 11,000 years is known primarily through the study of a cut bank along the Souris River. Flint Stone Hill contains the most complete stratigraphic record for the post-glacial period on the northern plains. The site has been extensively studied by geoarchaeologists, geologists and paleoenvironmentalists over many years and their findings have contributed to our understanding of the region.
The North Lauder locale Borden designations of Atkinson site DiMe-27 and Flintstone Hill site DiMe-26.
Borden System
Archaeological sites in Canada are identified by the Borden system, which is a uniform site designation system. The country is divided into grids based on latitude and longitude in blocks of 10 x 20 minutes. The first 4 letters indicate the block and the following numbers indicate the actual site. For example the area of the Lauder Sandhills in southwestern Manitoba is identified by the letters DM and the North Lauder locale within that area is DiMe. The Atkinson site is DiMe-27 and the Flintstone Hill site DiMe-26. As new sites are discovered they will be numbered sequentially.
Scope and Content
The Series has been divided into two sub-series, including (1) Atkinson site DiMe-27 and Flintstone Hill site DiMe-26.
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 series was created by the committee involved with the financial aspects of the winter and summer fairs, as well as the committee formed in the mid1960s to look into the feasibility of creating a complex that could house both fairs
Custodial History
The records were housed at the Inter-Provincial Exhibition, the PEM, and the MEA until c1986 when they were transferred to the S.J. McKee Archives at Brandon University.
Scope and Content
The series includes financial records, proposals for an arena complex, financial statements, economic evaluations, annual reports, and a ledger with names and wages in it.
Notes
Part of RG2SF4. Inventory of documents in the series is available in the printed finding aid.
Storage Location
RG 2 Provincial Exhibition of Manitoba Association fonds
RG2SF4 Miscellaneous
See fonds level description of custodial history of A. E. McKenzie Seed Co. Ltd.
Scope and Content
This sub-series includes financial statements of various kinds for McKenzie Seeds and combined financial statements for McKenzie Seeds and its subsidiaries, particularly McFayden Seeds. Chartered Accountants used for this purpose include: Marwick, Mitchell & Co., Webb, Read, Hegan, Callingham & Co./Webb, Read & Co., George A. Touche & Co., Oscar Hudson & Co., Morden, Sprague & Co./Laird, Sprague & Co., Edwards, Morgan, Halliday & Co., Welch, Hinton and Welch, McDonald, Currie & Co./Cooper Brothers & Co., Meyers Dickens Norris Penny & Co./Meyers, Norris, Penny & Co. and the Comptroller-General for the Province of Manitoba.
This sub-series also includes a number of purchase offers made to A.E. McKenzie Seed Co. Ltd as well as proposed plans to sell the company. Offers were received from United Grain Growers, Maple Leaf Mills, McKenzie Seeds Staff, Manitoba, Saskatchewan and Alberta Wheat Pools, and the Ferry Morse Seed Co.
Twelve ledgers, including branch order, mail order and cash registers, general ledgers, current ledgers, payroll sheets and branch daily cash reports, are also part of the sub-series. Other miscellaneous financial records and statements include information on McKenzie Seeds' proposal to the Manitoba Government for re-financing in the early to mid 1980's.
Notes
Additional dates for the records in the financial sub-series are as follows:
1. Prepared Financial Statements: 1907-1918, 1920-1923, 1926-1938, and 1942-1979.
2. Purchase Offers: U.G.G. (1959, 1966), Wheat Pools (1961), McKenzie Staff (1963),
Maple Leaf Mills (c. 1965), Ferry Morse Seed Co. (c. 1969-1970).
The extent of the ledgers in sub-series McS 1 1.5 (Financial Records) separate from the other
financial records in the sub-series is 95.9 cm. The financial records without the ledgers measure 60 cm.
Storage Location
RG 3 A.E. McKenzie Company fonds
McS 1 Board of Directors
Related Material
Financial statements and records for the individual companies acquired by
McKenzie Seeds are located in Series III.
Information regarding the sale of McKenzie Seeds is located in Series II (Office of the President/GM), sub-series I (A.E. McKenzie), in the file entitled A.E. correspondence with W.A. Johnson. Some of these records are connected to the purchase offers received by McKenzie Seeds.
Series A is comprised of the records of the local co-operative elevator association as established in the period 1925 - 1968 under the Co-operative Associations Act. Until 1968 the local associations were the main administrative unit of Manitoba Pool Elevators. Subsequent to 1968 Pool Elevators became a direct membership top down organization. The central office was at the top, and the province was divided into seven administrative districts, which were in turn each divided into six sub-districts. Each sub-district would usually contain approximately five "locals". Please note that local associations were not obliged to become part of the new structure of Manitoba Pool Elevators, and as late as 1975 there were still 29 locals that did not belong to a sub-district. The records of each local within the Series may, but do not necessarily, contain the following: organizational papers, minutes of executive board, minutes of shareholders annual meeting, financial statements, correspondence, membership lists, miscellaneous. Series has been divided into 233 sub-series.
Notes
This series contains records for both local associations and for sub-districts. Item number does not correspond to sub-district number, so an item number and sub-district number may be the same and correspond to two seperate records.
DEANS OF STUDENT SERVICES:
R. BRUCE MCFARLANE (1968 - 1976)
No biographical information yet.
CAM CONNORS (1978 - 1982)
Campbell Connors was born in England and raised in South Africa. He came to Canada in 1963, and attended the United College in Winnipeg (now the University of Winnipeg). Connors had planned to return to Zimbabwai, but after the Declaration of Independence in 1966, he was unable to. Subsequently, he became a United Church minister in Russell, Manitoba for four years. In 1971, he was invited to head a special Mature Students project at Brandon University, and in 1976, he became that institution's Dean of Student Services.
TOM MITCHELL (1985 - 1989)
See RG 6 Brandon University fonds, Series 5 Office of the Registrar, 5.1Registrar's files for biographical information on Tom Mitchell.
BETH WESTFALL (1989 - 1992)
Additional biographical information for Beth Westfall is located at RG 6, series 9 (Office of Extension).
On September 1, 1989, Westfall became the first female dean at Brandon University when she accepted the position of Dean of Student Services. Westfall left Brandon University in 1992 to accept a position as President of Keewatin Community College, in The Pas, Manitoba. At present (January 2007), Beth Westfall Davies is the Senior Education Administrator of Northwest Community College in British Columbia.
DARCY BOWER (1994 - 2005)
See RG 6 Brandon University fonds, Series 5 Office of the Registrar, 5.1Registrar's files for biographical information on Darcy Bower.
JANET S. WRIGHT (2005 - July 31, 2008)
See RG 6 Brandon University fonds, Series 7 Faculties and Schools, 7.2.1 Dean of Science for biographical information on Janet Wright.
DAVID ROWLAND (August 1, 2008 - July 31, 2013)
David Rowland is a native of Toronto, ON. He obtained his B.Sc. in Physical Education from Coastal Carolina University in Conway, South Carolina in 1997. He completed his Master of Education degree in Special Education at the University of Charleston in 1999.
From 2000-2005, Rowland was the Assistant Dean of Students at the College of Charleston before taking the position of Dean of Students at Mount Allison University in 2006. His term as Dean of Student Services at Brandon University began in 2008.
Scope and Content
Sub-series consists of correspondence and minutes.
Notes
History/Bio information on Cam Connor was taken from Connexion December 1971 and an article in "The Quill" (September 27, 1979). Biographical information for Beth Westfall was taken from articles in "The Quill" (August 30, 1989) and from the government of British Columbia's Board Member biography page on Beth Westfall Davies located at: http://www.fin.gov.bc.ca/oop/brdo/memView.asp?Member=142002 (January 2007). History/Bio information for David Rowland taken from the September 1, 2008 issue of the Quill.
Storage Location
RG 6 Brandon University fonds
Series 12: Student Services
The Lovstrom locale first came to the attention of Dr. Nicholson through conversations with landowners Mr. and Mrs. Herb Lovstrom in 1985. Lovstrom is a multi-component archaeological locale located 25km south of Brandon overlooking the Souris River channel. The landowner’s surface collection and the presence of bone and artifacts in a cultivated field indicated the presence of one or more sites.
Limited testing was conducted in 1985 and 1986, followed by major excavations in 1987, 1988 and 1991. Eight sites of block excavations with a total of 132 1m2 excavation units were completed. The locale area extends approximately 500m north from the edge of the Souris Valley escarpment and over 200m east from the Jock’s Creek escarpment.
Physical and biological environment As has been noted above, the locale is bounded on the south by the Souris channel and on the west by the incised channel of Jock’s Creek and a till plain extends to the north and the east. This plain is characterized by buff colored glacial till with numerous rocks embedded in the surface. Surrounding these rocky knolls are dark-soil hollows where the various cultural occupations are found. The depth of the topsoil layer suggests a long term grassland cover with the present oak forest likely developing in historic times due to the elimination of bison grazing and the controlling of prairie fires in late historic times. A small cleared patch of farmland is found within the boundaries of the locale area. This area has provided a substantial surface collection of artifacts.
Present vegetation in the area is a mosaic of aspen/oak forest groves and mesic grass prairie that includes introduced species such as brome grass. In poorly drained areas, willow and red osier dogwood are present. The Lovstrom locale is found in a forested area dominated by oak with an under story of saskatoon, chokecherry, pin cherry, and hazelnut brush. Poison ivy is abundant as well as sarsaparilla.
The major faunal resources in Precontact times would have been bison, with elk and mule deer playing a minor role. Antelope may have been present also. Small animals included snowshoe hare, cottontails, porcupines and beaver. Canids, including wolf, coyote, fox and domesticated dog were present, as well as mustelids such as badger, mink, and weasel. Fragments from a fisher were also recovered in the excavations.
Summation.
The Lovstrom locale has eight sites. The sites were designated and excavated as Blocks A, B, C, D, E, F, G and H. Many of the sites are multi-occupations.
The Vickers materials are primarily confined to Blocks D, E, F, G and H. Vickers Focus materials overlie Blackduck/Duck Bay materials. Blackduck and Duck Bay materials are found in the lower levels of all excavation blocks and in most test units. The Vickers occupations at the Lovstrom locale, based upon ceramic wares and an overlapping of C14 dates, appear to have been contemporary with the Lowton type site to the east, near Belmont. A small protohistoric occupation was identified overlying part of Block D. Faunal remains are abundant with bison clearly dominating the assemblages. Lesser amounts of canid are present as well as small mammals including beaver, hare and mustelids. Small amounts of avian species are also present.
Publications
Nicholson, B.A.
2011 The Role of Pocket Gophers (Thomomys talpoides) in Restructuring Stratigraphic Relationships at the Lovstrom Site. Canadian Journal of Archaeology 35:323-331.
Nicholson, Bev, Scott Hamilton, Matthew Boyd and Sylvia Nicholson
2008 A Late Plains Woodland Adaptive Strategy in the Northern Parklands: the Vickers Focus Forager-Horticulturists. Invited Paper for Papers in Northeastern Plains Prehistory, eds. Michael G. Michlovic and Dennis L. Toom, North Dakota Journal of Archaeology Vol. 8:19-34.
Nicholson, Bev and Scott Hamilton
2001 Cultural Continuity and Changing Subsistence Strategies During the Late Precontact Period in Southwestern Manitoba. Canadian Journal of Archaeology 25:53-73.
Nicholson, Bev
1996 Plains Woodland Influx and the Blackduck Exodus in South-Western Manitoba During the Late Precontact Period. Manitoba Archaeological Journal 6(1):69-85.
Nicholson, Bev and Mary Malainey
1991 Report on the 1991 Field School Excavations at the Lovstrom Site (DjLx-1), Southwestern Manitoba. Manitoba Archaeological Journal 1(2): 51-93.
Nicholson, Bev and Jane Gibson
1990-91 Lovstrom Site Field Report, 1987 Excavations. Saskatchewan Archaeology 11&12:46-68.
Nicholson, Bev and Ian Kuiijt
1990 Field Report and Interpretations of the 1988 Archaeological Excavations at the Lovstrom Site (DjLx-1) in Southwestern Manitoba. North Dakota Journal of Archaeology 4:166-205.
Nicholson, Bev
1990 Ceramic Affiliations and the Case for Incipient Horticulture in Southwestern Manitoba. Canadian Journal of Archaeology 14:33-60.
Nicholson, Bev
1986 The Lovstrom Site: Culture Contact in Prehistory. Manitoba Archaeological Quarterly 10(1):35-71.
Scope and Content
The Series has been divided into nine sub-series, including (1) Survey (2) Block A; (3) Block B (4) Block C; (5) Block D; (6) Block E; (7) Block F; (8) Block G; (9) Block H
Consists of the BCSA constitution, electoral procedure documents, nomination forms, the Brandon College Crests and Awards Board constitution, the Brandon College Finance Board constitution, the Brandon College Athletic Board/Athletic Council constitution, the Brandon College Board of Publications constitution, the Brandon College Literary Board constitution, the Sigma Mu constitution, and BCSA statistical summary of Committee meetings.
Sub-series consists of accession records listing the accession number, author, title, publisher, cost and “source” for each book accessioned into the Brandon College Library. It includes a total of 10 accession catalogues covering the period December 1899 - June 1965: 2 accession catalogues (12x18x5) and 8 accession catalogues (9x12x .75 cm)
Storage Location
RG 1 Brandon College fonds
Series 15: Brandon College Library
This series was created by a committee attached to the Board of Directors of the winter fair.
Custodial History
See sous-fonds RG2SF2 for custodial history.
Scope and Content
The series contains financial statements from 1925 and 1926, as well as financial records from the 1930s to 1969. There is also a transfer ledger from the years 1939 to 1953. There is a box with the statement of prizes won from 1972 to 1977.
Notes
Inventory of the documents in the series is available in the printed finding aid.
Storage Location
RG 2 Provincial Exhibition of Manitoba Association fonds
RG2SF2 Manitoba Winter Fair
The structure of the Manitoba Pool Elevators from its beginning in 1925 until its restructuring in 1968 placed importance in the principle of democracy. The company was run from the local associations, the central office acting as a hub that facilitated communication between all the locals and between the locals and the selling agencies. The central office was not powerless, but important decisions or by-laws could not be made with out the consent of the majority of the locals.
After the restructuring of MPE in 1968 the central office took on more responsibilities. It became the top of the administrative structure and instead of members belonging to their local elevator, they were now direct members of MPE. This administrative structure continued until the 1998 merger with the Alberta Wheat Pool to form Agricore.
Scope and Content
Series B consists of an artificially assembled collection of Central Office records. It has been divided into the following sub-series: (1) Central Office minute books; (2) Documents; (3) Local Association Minutes; (4) Local association finacial statements; (5) District and Sub-district records; (6) Circulars; (7) Annual reports; (8) Speeches & Addresses; (9) Correspondence; (10) Broadcasts; (11) General Reports; (12) Indexes; (13) Summary of Association Operations; (14) Acquisitions; (15) Inter-provincial Committees; (16) Historical Topics.
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.
