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
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,
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
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
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.
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.
Robert (Bob) Troy Blair was born on March 11, 1930 in Brandon, MB. His first six years were spent in Alexander, MB, where his father and uncle operated a grocery store. In 1936, his family moved to Souris, MB, where his father ran a grocery store. Blair received his primary and high school education, with the exception of Grade 12, in Souris.
Blair remembers his school years in Souris as mainly happy years. He was involved with both piano and organ music lessons. he was never interested in physical sports with the exception of golf. World War II broke out in September of 1939. Souris became the site of #17 SFTS and home base for the British Commonwealth Air Training Plan. Many of the service men came from England, Australia and New Zealand. Blair's mother always entertained at least two for dinner every Sunday. Rationing of sugar, tea and coffee, butter and meat became a way of life. Blair had the job every Saturday of pasting the ration coupons into booklets. It was also when he was in Grade 6, that Blair realized he was more attracted to boys than to girls. Perhaps it was because so many attractive airmen surrounded him!
In November of 1947, the Blair family relocated to Alexander where Bob Blair finished his Grade 11. This was not a good year due to bullying. In September of 1948, Blair moved to Winnipeg to attend United College for his Grade 12. Upon completion of Grade 12, Blair remained in Winnipeg until June 1950. he worked at a number of businesses - Gestetner, Eaton's Mail Order shoe department, Maple Leaf Milling, and the drug store in the Medical Arts Building. In September 1950, he entered Brandon College. Blair was very active in extra-curricular affairs while at Brandon College; particularly drama. Following his B.A. he enrolled in the Education Faculty, having decided to become a teacher.
Blair's teaching career spanned 34 years. All but one year was spent in the Brandon School Division. On his first day of teaching in the Division he met the man with whom he would spend the next 46 years. He was primarily a teacher of English and Music. A highlight of his career was exchange teaching in Sacramento, California in 1961. Orientation for exchange took place in August in Washington, D.C., where Blair had the opportunity to meet President J.F. Kennedy. He vividly recals the morning that JFK was assassinated on November 22, 1963. In September 1965, Blair assumed the principalship of Park School and in September of 1969, the same position at George Fitton School where re remained until his retirement in 1989. He was a member of the Brandon Picnipals' Association, the National Association of Elementary School Principals, and servedas President of the Brandon Teachers' Association. Among his major accomplishments during his time as principal were the introduction of a centralized school library in both Park and George Fitton Schools and the integration of special needs students into regular classroom situations wherever possible. He was made a Life Member of the Manitoba Teachers' Society (Brandon) in June 1990. Following his retirement Blair worked as a Library Automation Consultant (1989-1993).
Blair also had numerous community involvements during his time in Brandon. he was active in the Brandon Little Theatre (Best Actor Award, Manitoba Drama Festival for One Act Plays in 1963), the Brandon Festival of the Arts, the Eckhardt-Gramatte National Music Competition, and Arm Industries to name a few.
Following the death of his partner in 2001, Blair moved to Saskatoon to live with a younger gay couple. He has been active in volunteerism: as an Ambassador for the Saskatoon Airport Authority, assistant with the Saskatoon Health Region's Immunization Clinics, information clerk for the Festival of Trees, data entry clerk for the Saskatoon Music Festival, on the Board of the Saskatoon Jazz Society, and Hospitality Coordinator for the Saskatoon Jazz Festival.
Robert Troy Blair died on July 2, 2024 in Saskatoon, SK. He is buried in Brandon, MB.
Custodial History
Records were in Blair's possession until he donated them to the Mckee Archives on Homecoming weekend October 2013.
Scope and Content
Fonds consists of two scrapbooks containing 145 photographs and ephemera (play and graduation programs, tickets, pins, newspaper clippings) documenting Bob Blair's days at Brandon College. Social events and extra-curricular activities are heavily featured in the two scrapbooks. Also included are graduation portraits for the Classes of 1951, 1952 and 1953. Of the 145 photographs all are black and white except for two photos of the Class of '53 reconvocation (May 1993), and one from the Class of '53 reunion (2003).
The Manitoba Wheat Pool and Manitoba Pool Elevators kept and preserved a chronological record of the meetings of the MPE Board of Directors and annual delegate meetings. The minutes were typed and bound, then placed in the MPE reference library so that employees and members could access them.
Scope and Content
This sub-series consists of minutes of organizational meetings and later meetings held by the Central Office of the Manitoba Wheat Co-operative Producers, Ltd (later known as the Manitoba Wheat Pool) from 1923 until it went under in 1934, and of meetings held by the central office of Manitoba Pool Elevators from 1925 until 1997.
See fonds level description of RG 4 for history/bio of MPE
Scope and Content
This artificially created sub-series contains a variety of legal and official documents related to the operation of the Manitoba Wheat Pool and MPE. Records include the following:
1. Agreements, General By-laws, and Contracts 1924-1972
2. General By-laws
3. Incorporations and Dissolutions
4. Operating Agreements, Agreements for Sale 1940-67
5. MPE Complete Legislation
6. Miscellaneous Documents
7. Elevator Policy, Agreements, Incorporation Certificates / Indebtedness
8. Quantitative Appraisal of Wheat Pool Building (left in original binding)
9. 9th Victory Loan Souvenir: A Portfolio of Reproductions of the Documents of Surrender
10a. Federal Agreement 1972 p.1-126
10b. Federal Agreement 1972
11a. Terminal Expansion 1961 – 1963
11b. Terminal Expansion 1961 – 1963
12. By-Laws and Constitutions
13. MPE & Connaught Laboratories Agreements 1964-66
14. MPE & Connaught Laboratories Agreements 1964-66
15. “Pool Pac” Trade Mark 1964, 1971, 1979
16. Patent #501894 Dust Control Apparatus 1954
17. MPE Agreement w/ Daniel Augustus Kane (General Superintendent appointment) 1928, 1933
18. Manitoba Co-operative Wheat Producers Ltd. Agreement w/ Richard M. Mahoney (Manager) 1924, 1925, 1928
19. MPE Acts
20. MPE Acts
21. Party & Supplementary Agreements 1931-1936
22a. Historical Documents of the Manitoba Wheat Pool 1924 - 1927
22b. Historical Documents of the Manitoba Wheat Pool 1927 - 1930
23a. Miscellaneous Documents 1925 -1996
23b. Miscellaneous Documents 1979 -1998
24. Association Documents 1940 - 1966
25. Deed of Trust and Mortage August 2 1928
26. Wheat and Coarse Grains Overpayments 1929-1930
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.
Circulars were used by Manitoba Pool Elevators to facilate communication between the central office and the local associations. Circulars were most often about Manitoba Pool Elevators and topic related to the running of the company, but they could also be about the co-operative movement, world events, or other aspects of rural life in Manitoba. See fonds level description of RG 4 for complete history/bio of MPE
Scope and Content
Sub-series MPE B.6 consists of circulars and newsletters. See Box level entries under B.6 for detailed contents of records.
As a co-operative company, the Manitoba Wheat Pool and later the Manitoba Pool Elevators was member controlled. In order to run the company successfully members needed to be educated and kept updated about the companies financial and organizational situation. Annual reports were one of the many ways the Pool tried to do this. See fonds level description of RG 4 for complete history/bio of MPE.
Scope and Content
Sub-series MPE B.7 consists of annual reports. There are two complete sets of annual reports, one for archival storage and one for use by researchers. Neither set contains a report for 1931. Reports from 1926 until 1928 are Manitoba Co-operative Wheat Producers, Ltd. Reports, 1929 - 1930 are Manitoba Wheat Pool Reports. All reports subsequent to 1931 are Manitoba Pool Elevators.
Archival set: (1) Bound Copies, MPE Annual Reports Vol. 1 1926 - 1949; MPE Annual Reports Vol. 2 1950 - 1959; MPE Annual Reports 1960 - 1969; (2) Individual MPE Annual Reports 1970 - 1998
Reserch set: Individual MPE Annual Reports 1926 - 1930, 1932 - 1998
See fonds level description of RG 4 for history/bio of MPE.
Scope and Content
Sub-series MPE B.4 consists of local association financial statements.The statements are bound in uniform hardcover volumes. The statements is organized chronologically, and alphabetically by local association name within each individual year.
The records for each individual local's fiscal year consists of: 1) letter of certification from the auditors; 2) summary of income and expenses of said local association.
Speeches and addresses given by executives of the Manitoba Wheat Pool and MPE as well as argricultural experts and supporters of the co-operative movement helped to spread and solidify support for the Pools. They also served to educate rural members on a variety of topics. See fonds level description of RG 4 for complete history/bio of MPE.
Scope and Content
Sub-series MPE B.8 consists of speeches made by various important members and executives of Manitoba Pool Elevators. Records include the following:
1a. Addresses 1930 -1946
1b. Addresses 1946 -1954
2. Addresses 1954 -1960
3. Addresses 1969 -1975
4a. Addresses 1972 -1979
4b. Addresses 1972 -1979
5a. F.W. Hamilton Speeches 1967 -1973
5b. F.W. Hamilton Speeches 1962 -1966
5c. F.W. Hamilton Speeches 1960 -1962
5d. F.W. Hamilton Speeches 1949 -1960
6a. W.J. Parker Speeches 1945
6b. W.J. Parker Speeches 1940 -1944
7a. W.J. Parker Speeches 1948 -1950
7b. W.J. Parker Speeches 1946 -1948
8a. W.J. Parker Speeches 1954 -1958
8b. W.J. Parker Speeches 1951 -1954
9a. W.J. Parker Speeches 1968 -1970
9b. W.J. Parker Speeches 1960 -1967
10. F.W. Ransom Addresses 1942 - 1948
11. Miscellaneous Addresses 1948 - 1955; no dates
12. Miscellaneous Addresses 1960; no dates
13. E.S. Russenholt Addresses
14. V. Martens " The Implications of Including Protein in Segregrating Canadian Wheat"
See fonds level description of RG 4 for history/bio of MPE
Scope and Content
This artificially created sub-series MPE B.9 consists of memos, letters to secretaries of locals, questionnaires, general correspondence, and responses. See Box level entries for B.9 for detailed contents of records.
Manitoba Pool Elevators was quick to realize the usefulness of the radio medium as a educational and promotional tool. It was also often used to defend the Pool and the co-operative movement in general on programs such as Farm Radio Forum. See fonds level description of RG 4 for complete history/bio of MPE.
Scope and Content
Sub-series MPE B.10 consists of textual radio broadcast transcriptions. The records include transcriptions from 1930 until 1971. Radio broadcasts are on a wide variety of topics, including argicultural science, the grain market and general economy of Canada and the world, government acts and legislation that affected the producer, co-operatives and the co-operative movement, rural life, young people, WWII, Manitoba, and the Manitoba Pool Elevators.
