See fonds level description of RG 4 for history/bio of MPE
Scope and Content
This sub-series consists of summaries of elevator operations. The records include the following:
Box 1:
Summary of Operations 1925-1968 Alexander-Gretna
Summary of Operations 1925-1968 Hamiota-Morris
Summary of Operations 1925-1968 Napinka-Woodnorth
Box 2:
Association Financial and Debt Repayment Summary 1925-1963
Association Financial and Debt Repayment Summary 1925-1963
Box 3:
Summary of Operations 1964-1968
Summary of Operations 1964-1968
Summary of Operations 1964-1968
Box 4:
Summary of Operations A-K 1925-1996
Summary of Operations L-Z 1925-1996
Elevator Points Closed A-L 1926-1987
Elevator Points Closed M-Z 1926-1987
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.
Edwin Association Minutes 1928-1981; Sub-district #101 Minutes Oct 6 1969-July 18 1978; Agent's Letters Dec 24 1928-July 15 1947; Cirrculars Spet 19 1969-August 15 1978; Correspondence Nov 7 1960-Sept 8 1978; Memo of Association and By-laws 1928-1953; Member Certificates 1947-1953; Newsletters Jan 1976-August 1978; Attendance records 1946-1962; Financial 1929-1983; Miscellaneous (correspondance, Grain Handling Commission, Crop Development and Seed Clubs, publications) 1951-1978; Membership Lists 1955-1978
Notes
Description by Jill Sutherland (2010)
The records for Edwin Association are unique in that more that just minute books were sent to the McKee archives
Forrest Association Minutes 1927-1991; Circulars April 21 1965-Oct 19 1981; Correspondance May 22 1927-May 25 1981; Documents Feb 11 1927-July 31 1969; Financial 1928-1968; Membership 1948-1969; Miscellaneous 1952-1980
Notes
Description by Jill Sutherland (2010)
The records for Forrest Association are unique in that more that just minute books were sent to the McKee archives
Border Fertilizers Ltd was a parnership agreement between the Pool and M.G. Smerchanski to provide better fertilizer services to Pool members. MPE entered the agreement in 1963 but sold their shares in 1969 due to heavy losses.
See also fonds level description of RG 4 for history/bio of MPE
Scope and Content
This sub-series consists of legal documents, financial statements, proposals and reports.
Co-enerco was a co-operative energy company that resulted from the Co-operative Resources Project.
See also fonds level description of RG 4 for history/bio of MPE
Scope and Content
This sub-series consists of records pertaining to the formation of Co-enerco.
CSP Foods Ltd resulted from an amalgamtion of Co-op Vegetable Oils Ltd with MPE in 1975. The company operated crushing plants in Altona, Manitoba and in Saskatchewan, and was overseen by members of MPE and the Sask Wheat Pool.
See also fonds level description of RG 4 for history/bio of MPE
Scope and Content
This sub-series consists of minutes, correspondence, reports, and promotional materials.
Notes
Description by Jillian Sutherland (2010)
History taken from F.W. Hamilton's "Service at Cost"
Co-op Farm Implements was a subsidiary company designed to serve Pool members in Manitoba and Saskatchewan.
See also fonds level description of RG 4 for history/bio of MPE
Scope and Content
This sub-series consists of general documents and photographs.
Pool Insurance Limited was created in 1939 and re-incorporated at Pool Insurance Company in 1940. It was designed to internalize some of the insurance risk of MPE, which had previously been carried by an extenal company.
Co-operative Life Insurance Company was formed in 1945 to offer pool members affordable life insurance tailored to their lives as producers.
See also fonds level description of RG 4 for history/bio of MPE
Scope and Content
This sub-series consists of documents and minutes.
The Pool livestock advisory boards and livestock markets were organized under the MPE when MPE merger with the Manitoba Co-operative Livestock Producers Ltd in 1948. The livestock pools operated in much the same way the grain pools did. The MPE Livestock Division was overseen by the Canadian Livestock Co-operative (Western) Limited (known as the C.L.C.). Local shipping associations shipped livestock to a central selling agency in St. Boniface, although this changed with the development of the rural highway system in Manitoba and the founding of Pool Packers.
See also fonds level description of RG 4 for history/bio of MPE
Scope and Content
This sub-series consists of Livestock Division records, Virden Auction Market records, Brandon Livestock Advisory Committee records, Elkhorn Co-operative Livestock records, and Swan River Livestock Association Ltd.
Manitoba Pool Elevators was a part of and associated with many other producer co-operatives in Manitoba.
See also fonds level description of RG 4 for history/bio of MPE
Scope and Content
.This sub-series consists of records from the following co-operative organizations: Canadian Poultry Pool Ltd, Canadian Poutry Sales, Manitoba Co-operative Poultry Marketing Association, Manitoba Dairy and Poultry Co-operative Ltd, The Co-operative Promotion Board, Manitoba Fish Products, Pool Co-operative Seed Association, XCAN Grain Pool
Records for the above organizations may include but do not necessarily include the following: financial records, minutes, correpondence, reports, addresses, and memoranda.
Notes
Description by Jillian Sutherland (2010)
Original order in this sub-series was rearranged by Eileen McFadden. The order established by her has been left intact.
The Wasagaming Foundation was founded in 1964 to plan an educational centre at Clear Lake, part of which would become Camp Wannakumbac in 1965. The Foundation was the joint effort of MPE, Federated Co-opertives Limited, Manitoba Farm Bureau, and United Grain Growers.
See also fonds level description of RG 4 for history/bio of MPE
Scope and Content
.This sub-series consists of two files of the Wasagaming Foundation.
A copy of a Local Associations (later the Local Pool Committees) would be sent to the Central Office, where it was stored until a microfilm copy could be made. Records were only transferred to microfilm until 1957.
Custodial History
Local Association records recieved by the Central Office dating from 1925 to 1957 are on microfilm. Records subsequent to 1957 are hardcopies.
Scope and Content
Sub-series MPE B.3 consists of Local Association records from the formation of the association until 1993 or said association's closure. See Box level entries for B.3 for detailed contents of records.
Notes
Description by Jillian Sutherland (2009). Records contained in Series B.3 on microfilm or in hardcopy may also be contained in Series A.
The Sarah site was chosen for excavation based on the results of the Casselman survey. The survey recovered significant amounts of faunal remains, some ceramics and lithics from the test pits. Excavations took place in 2003 at Crepeele West (Units 1-5) and Crepeele East (Units 6-9). The site was subsequently renamed the Sarah site DiMe-28. In 2004 another 9 units were excavated (Units 10-18).
Based on the recoveries it was determined that the Sarah site is a stratified site with woodland ceramics in the upper occupation and late woodland points in both of the upper occupations. These upper occupations produced abundant bison bone including foetal bone. The lower occupations produced less bone and no foetal bone, although absence of foetal bone in the lower occupations does not necessarily indicate a warm season occupation. This could be due to sample error or perthotaxic factors such as scavenging of the fragile bone by dogs or other carnivores.
The dates from the Sarah site include 550+/-40 B.P.; 1430+/-80 B.P; 2810+/-80 B.P.; 3120+/-130 B.P. The lower occupations did not yield any diagnostic materials although debitage was abundant. These occupations were most productive at the edge of the large sand dune at the southern edge of the excavations. It is assumed that the major portion of these occupations have been overridden by the dune in the past 3000 years. Heavy earthmoving equipment would be required to remove this overburden which limits the possibility of future excavation.
Environment
The Sarah site is a large area located at the eastern end of the Crepeele locale. Ground cover is a mosaic of aspen poplar groves and patches of mesic grass prairie. Excavation profiles indicate that this has been the situation since early precontact times, although as local climatic conditions change (primarily rainfall), the relative size of these areas and where they may have occurred also changed. The soil is aeolian sand sheet derived from delta outwash deposits along the western edge of glacial Lake Hind. The present topography is a variable dune landscape reworked by aeolian activity that creates a mosaic of microhabitats. These include forested patches in the lee of sand dunes with grassland on the southern and western exposures and small damp lowlands that support balsam poplar, willows, red osier dogwood, high-bush cranberry and water birch. There is no permanent water source in the area although a small seasonal stream meanders through a damp lowland to the east of the Sarah site.
Scope and Content
Sub-series has been divided into sub sub series including: Sarah 2003 and Sarah 2004,
Block D was wooded with oak and an understory of saskatoon and hazelnut with a thick ground cover of poison ivy and sarsaparilla. Root and rodent disturbance was extensive.
Based on the recoveries from Test Unit 22 during the survey, further excavations were carried out. Two units 87 and 93 were excavated in 1987. A further four units were excavated in 1988. There appears to be a pre contact occupation and a protohistoric feature within the block.
Diagnostic lithics included a chert Plains Side-notch projectile point, and a large Woodland side-notched point. The lithic materials from Block D are primarily local cherts followed in abundance by Knife River Flint and Tongue River Silicified Sediment – both of which are exotics imported from the southwest. Faunal remains were primarily bison.
Thin-walled obliterated fabric impressed pottery with grit temper was recovered in all units. Diagnostic ceramics included two rims, one with a fabric impressed exterior and the lip notched with dowel impressions, and a second thick walled rim was fabric impressed to the lip. The ceramic wares appear to be essentially a Woodland complex with overtones of Plains influence.
RC date: 230/90 BP.
Scope and Content
Sub-series has been divided into sub sub series including: Lovstrom Block D 1987 and Lovstrom Block D 1988.
This site is situated in a naturally sheltered area with a low rise to the east and south partly encircling a flat area open to the west. Present natural vegetation is an open oak forest with a light understory of saskatoon, hazelnut, poison ivy and sarsaparilla. It is situated on the till plain at the upper end of a ravine leading to Jock’s Creek.
Two test units six meters apart were excavated in 1987 and produced cultural materials which warranted a block excavation, so seven contiguous 1m2 units were then opened. These units proved to be very productive of cultural remains. Subsequent excavations in 1988 increased the number of excavated units to 21. In 1991 a further eight units were excavated for a total of 29 excavations and two test units. Excavations went deeper in this block than in Blocks C or B. Remains from the block included bison bone, bone tools, fire-cracked rock, ceramics, lithics including tools and debitage and a hearth. Another occupation was recovered in 1991 containing a hearth and living floor.
Radiocarbon samples have produced two distinct sets of radiocarbon dates from 1987 and 1988 excavations. There appears to be two or possibly three cultural horizons definable within this block.
An upper cultural horizon, located between 14-21 cm below surface, contains large bison bone and fire-cracked rock dating to 465/100B.P from XU 128.
A lower horizon in the 20-25 cm level contained FCR, bison bone and lithic scatter that was dated to 675/70 B.P. from XU 122 and 715/110 from XU 114.
Scope and Content
Sub-series has been divided into sub sub series including: Lovstrom Block E 1987, Lovstrom Block E 1988 and Lovstrom Block E 1991.
The Graham site is a located adjacent to the Crepeele site towards the western end of the Crepeele locale. The Graham site was initially designated as a separate site early in the testing of the Crepeele locale due to what appeared to be a distinction between Early and Late Woodland ceramics. Subsequent testing has shown that this distinction was premature and that the cultural mosaic represented in the western section of the Crepeele locale may not readily separate in this manner. However, due to the records management that was already in place, the original separate designations have been retained.
Environment
Ground cover is a mosaic of aspen poplar groves and patches of mesic grass prairie. Excavation profiles indicate that this has been the situation since early precontact times, although as local climatic conditions change (primarily rainfall), the relative size of these areas and where they may have occurred also changed. The soil is aeolian sand sheet derived from delta outwash deposits along the western edge of glacial Lake Hind. The present topography is a variable dune landscape reworked by aeolian activity that creates a mosaic of microhabitats. These include forested patches in the lee of sand dunes grassland on the southern and western exposures and small damp lowlands that support balsam poplar, willows, red osier dogwood, high-bush cranberry and water birch. There is no permanent water source in the area although a small seasonal stream meanders through a damp lowland along the eastern margin of the Crepeele locale.
Excavations at the Graham site took place from 2004 to 2008. Analyses of the recoveries shows that, with two exceptions, all of the occupations that have been tested produced bison foetal bone. The presence of foetal bison is a strong indicator of wintering occupations...The absence of foetal in some area does not necessarily indicate warm season occupations since these excavation series are small and the absence could be due to sample error or perthotaxic factors, such as scavenging of the fragile bone by dogs or other carnivores.
From this evidence the Graham site has been interpreted as being primarily a wintering area. This is consistent with the lack of surface water (snow would serve as a substitute in winter) and the abundance of wood for fuel – a critical requirement for winter occupation. Cultural occupations date from Mortlach circa 250 B.P to woodland circa 580 B.P.
Scope and Content
Sub-series has been divided into sub sub series including: Graham 2004, Graham 2005, Graham 2006 and Graham 2008
