Contains the following files:
13.1 Georgina McPherson newspaper clippings 1897-1949 (arranged by Margaret McPherson in 1952)
13.2 Angus McPherson autograph album 1901
13.3 Ella McKay McPherson 1903
13.4 Jessie Sellers autograph album 1883
13.5 Postcard albums [early 1900's] - some are loose
13.6 Souvenir cards and photo album
13.7 Angus and Ethel McPherson photograph album 1909-1915
13.8 Photograph album [turn of the 20th century] - many of the photographs appear to be of Roseland, B.C.
Notes
Part of the Alfred Angus Murray McPherson collection.
The A.E. McKenzie Seed Co. Ltd. originated with the McKenzie family Flour, Grain and Seed business, started by F. B. McKenzie in the early 1880's. When F. B. McKenzie passed away in 1896, his son, Albert Edward McKenzie, assumed control of the company, and renamed it The Brandon Seed House. With its main office and plant in Brandon, Manitoba, the company specialized in the production and sale of field seeds and service exclusively to seed buyers in the prairie provinces and British Columbia. In later years, a complete line of products including garden seeds, lawn grass, and other allied lines was developed for sale across Canada.
In 1906, the company underwent a change of name when A. E. delete determined that the growth of the country demanded a larger seed institute than could be managed by one man. As a result, the company was incorporated under provincial statutes and the federal Joint Stock Companies Act as A. E. McKenzie Seed Co. Ltd., and new personnel were hired.
Under the Joint Stock Companies Act, A.E. McKenzie Seed Co. Ltd. was required to elect a Board of Directors of not less than three, and not more than nine individuals. Only shareholders of the company were eligible for election, and election was to take place yearly with each shareholder entitled to as many votes as shares owned in the company. The Act also dictated that the directors were, from time to time, to elect from among themselves, a president of the company. They were also able to appoint and remove all other officers of the company and to create company by-laws. The directors were not obliged to pay any dividend on shares if the company should became insolvent. Under the Act, the stock of the company was deemed a personal estate and was only transferable as such. In addition, the company could acquire, hold, and transfer real estate, and was required to submit annual statements.
A. E. McKenzie was elected President of the newly constituted company. For the memaninder of his natural life he remained in this position and supervised the operation of the company. S. A. Bradford, who was given responsibility for various company departments, filled the position of General Manager. H. L. Patmore became the Vice-President, overseeing the nursery business, while W. A. McCracken was put in charge of the warehouse stock, and shipping department. McCracken also supervised the mail order department.
The Company was intially comprised of three divisions: The Brandon Seed House, Brandon Nurseries, and Brandon Greenhouses. Each division was registered under Dominion Patents. Later, the company was divided into Retail Mail Order, Wholesale and Commission Packet Trade divisions. It also undertook some export business.
By registering the divisions of the company under under federal legislation affecting trademarks and industrial designs, McKenzie and the Board,were able to register both the company’s trademarks and to protect the company’s industrial techniques. Thet company could thus patent the methods and processes of its operations so that no other individual or business could duplicate them.
Located at 30 9th Street, the head office and plant of A.E. McKenzie Seed Co. Ltd. housed all the facilities and staff of the company, with the exception of the regional sales offices and warehouses. The business of the A. E. McKenzie Co. Ltd. was conducted from a frame warehouse until the current McKenzie building was constructed on the same site after a fire destroyed the original premises. Designed by architect Thomas Sinclair, and built by the Brandon Construction Company, the new building opened in 1911. In time, The A. E. McKenzie Co. Ltd. came to be known as Western Canada's Greatest Seed House.
During the 1930's, before a new building was erected in 1945, the A. E. McKenzie Co. occupied space at five different locations in Brandon, including the Massey Harris Building, the International Harvester Building and the Security Building. The last of these premises was destroyed by fire in 1972. As a result of its proximity to the Security Building, the main McKenzie Building also suffered heavy fire and water damage. A. E.
McKenzie Co. Ltd. also utilized a warehouse on the north side of Pacific Avenue alongside the Canadian Pacific Railway tracks between 5th and 6th streets. This building and its contents were destroyed by fire (1946). In May of 1949, the company purchased and erected a Quonset structure on the west side of 15th Street between Rosser and Pacific Avenues.
In 1908, the first branch of the A. E. McKenzie Seed Co. Ltd. was established at Calgary. In the following sixteen years, additional branches were established in Edmonton and Saskatoon (1923), Moose Jaw, Toronto (1934) and Winnipeg (1935). Both the Edmonton and Saskatoon branches were seasonal, operating for a four-month period, March to June inclusive. Business in the Maritime Provinces of Prince Edward Island, Nova Scotia and New Brunswick further extended the company's operations by the mid 1940's. In 1946, the company purchased property in Gilbert Plains, Manitoba, 120 miles north of Brandon. This purchase enabled the company to handle larger quantities of Sweet Clover, a popular crop that was grown in the surrounding area. Additional offices were opened in Vancouver and Quebec City in rented premises by the early 1960's.
In the years 1944-1945, the McKenzie Foundation was created. Through the Foundation, arrangements were put in place to transfer shares of the company to the Manitoba Government for the benefit of higher education, specifically Brandon College. In return for this gift, which included 90% of all capital resources of the company together with all of the income earned each year, except for the amount retained annually to ensure sufficient operating capital, the A.E. McKenzie Co. Ltd. received exemption from paying Corporate Tax.
Prior to the establishment of the McKenzie Foundation, in 1945, the National Trust for the benefit of the College held the shares of McKenzie Seeds. On April 7, 1945 the Manitoba Legislature passed legislation whereby A. E. McKenzie retained effective management control of his company, but 1031 shares out of 1145 issued shares were gifted to the Provincial Government. In return, the government agreed that all financial benefits from the shares would go to Brandon College through the A. E. McKenzie Foundation. When Mr. McKenzie passed away in 1964, the primary responsibility of appointing the Board of Directors for McKenzie Seeds passed to the Provincial government.
The remaining 114 shares of the Company were turned over to the Crown on July 16, 1975 in accordance with an agreement between Brandon University, A. E. McKenzie Co. Ltd. and the Manitoba government. The same agreement also turned the McKenzie Foundation over to Brandon University. Therefore, since 1975 the crown has held all shares of the McKenzie Co. through the Province of Manitoba.
A.E. McKenzie died on September 25, 1964 at the age of 94 and was succeeded as President of the company by J. Lasby Lowes. When Mr. Lowes retired in 1968, A. R. Swanson was appointed by the government to fill the position and was responsible for all operations of the company under a Board of Directors comprised mainly of appointees of the government. It has proven impossible to establish a complete list of those individuals who held the positions of President/General Manager of McKenzie Seeds after 1964. A partial account is as follows: Anthony J. Maruca became President of A. E. McKenzie Co. Ltd. in 1972. In 1975, the Board of Directors appointed William Moore General Manager, creating a new position to relieve the President of the company from management of plant operations. At the same time, Pat Kelleher was named new interim President. Following the resignation of Kelleher, William Moore assumed the role of President as well. Moore left the company in the early 1980s. He was later convicted of criminal misconduct as President of the company. Keith Guelpa became President/General Manager in the mid 1980's; Raymond West was his successor.
Beginning in 1969, the A. E. McKenzie Seed Co. Ltd. began phasing out the Field Seed division of their company, including business related to forage crops and cereals. Seed cleaning equipment located in Brandon and and the company’s Calgary and Toronto cleaning plants was sold. The Company concentration its resources on the production and sale of vegetable and flower seeds, and lawn and turf grasses. It acted as a wholesaler and conducted business through chain stores, grocery, hardware and general stores.
Late in 1971, A. E. McKenzie Co. Ltd. purchased its largest competition in packaged seeds - Steele Briggs Seed Co. from Maple Leaf Mills Inc. for two million dollars. At the time of the acquisition the company changed its name to A. E. McKenzie Co. - Steele Briggs Seeds, in order to benefit from the favorable reputation held by Steele Briggs Seeds across Canada. In the early 1970s, the acquisition of Brett-Young Seeds Ltd., a Winnipeg company that dealt exclusively in the production and sale of field seed, brought the A. E. McKenzie Co. back into the field seed market.
In 1994 the Manitoba Government sold the A.E. McKenzie Seed Co. Ltd. to Regal Greetings and Gifts, Canada's largest non-retail mail-order catalogue company, which is owned by MDC Corporation of Toronto.
In 2001, McKenzie Seeds is Canada's leading supplier of packaged seeds and related gardening products. It is divided into a Retail Consumer Products division which features well known seed brands including McKenzie Seeds, Pike Seeds and Thompson & Morgan Seeds from England. As well, this division also carries a complete range of lawn seeds and perishables. It also continues to ship the seed racks invented by A.E. McKenzie to numerous retail stores. The second division, Direct Mail, consists of the McFayden and McConnell catalogues which reach over 500,000 Canadian homes each year.
Custodial History
Following the sale of the A.E. McKenzie Seed Co. Ltd. to Regal Greetings and Gifts, the records of McKenzie Seeds and its subsidiaries were retained in the McKenzie Plant on 9th Street. In April of 1997, the records were transferred to the McKee Archives at Brandon University. Because the company was a crown corporation, the records of McKenzie Seeds belonged to the Province of Manitoba and might have been placed in the Provincial Archives. However, Provincial Archivist Gordon Dodds permitted the retention of the records in Brandon at the S. J. McKee Archives. The minutes of the Board of Directors, previously transferred to the Provincial Archives, remain in Winnipeg. Until 1960 these minutes, by-laws of the Company, and the letters patent of incorporation (April 7, 1906) were in the possession of the Company's lawyers, Johnson, Garson, Forrester, Davidson, & Steen.
Scope and Content
The fonds consists of textual records, photographs and artifacts from A.E. McKenzie Seed Co. Ltd. The textual records include minutes, documents, financial records, administrative records, by-laws, legal records, catalogues, sales literature, seed packets, newspaper clippings, appraisals, publications, scrapbooks and miscellaneous sections.
In addition, some of the records within the fonds relate to the operations of McKenzie subsidiaries -- Brett-Young Seeds, Steele-Briggs Seeds, Pike & Co. and McFayden Seeds -- and various properties owned by McKenzie Seeds.
Fonds contains approximately 500 photographs. These depict the operations and employees of McKenzie Seeds and the seed industry in general. Artifacts contained in the fonds include blueprints, newspaper clippings, copper printing plates, seed bags and plaques.
Fonds also includes an artificially created series of records dealing with Brandon College Inc., the A.E. McKenzie Foundation, the Brandon Allied Arts Council and the Brandon Board of Trade. These records stand outside the provenance of the McKenzie Seed Co.
Of particular interest within the textual records are the transcripts of various features of the company's history as dictated, researched and recalled by its second President/General Manager, J. Lasby Lowes. The fonds also contains a collection of company catalogue which is almost complete. Outside of the seed industry, the records dealing with both Brandon College Inc. and the McKenzie Foundation are significant records relating to the history of Brandon College/University and the City of Brandon.
Because the A.E. McKenzie Seed Co. Ltd. was a crown corporation, the records in the fonds are subject to the Freedom of Information and Protection of Privacy Act (FIPPA).
Storage Location
RG 3 A.E. McKenzie Company fonds
Related Material
Additional records regarding A.E. McKenzie Seed Co. Ltd. are housed at the Provincial Archives of Manitoba. In order to gain access to these records it is necessary to contact the Archives of Manitoba.
Arrangement
RG 3 A.E. McKenzie Seed Co. Ltd. Fonds
McS 1 Board of Directors
1.1 Documents
1.2 Minutes/Meetings
1.3 Management Consultant Reports
1.4 Miscellaneous
1.5 Financial Records
McS 2 Office of the President/General Manager
2.1 A.E. McKenzie
2.2 J. Lasby Lowes
2.3 Comptroller
2.4 Properties
2.5 Marketing
2.6 Reference Library
2.7 Miscellaneous Publications/Correspondence
McS 3 Acquisitions
3.1 Brett-Young Seeds/Sabetha
3.2 Steele-Briggs Seed Co.
3.3 Pike & Co.
3.4 McFayden Seeds
McS 4 Seed Marketing Co.
McS 5 Photographs
5.1 McKenzie Seed Co. Ltd. Executives
5.2 Construction at McKenzie Seed Co. Brandon (two files)
5.3 Exterior Photographs of the A. E. McKenzie Co. Building
5.4 McKenzie Seed Co. Plant Operations and Workers (2 files)
5.5 McKenzie Seed Co. Equipment and Plant - Head Office 1983
5.6 McKenzie Seed Co. Field Operations and Workers
5.7 McKenzie Seed Co. Strike 1944
5.8 Fires at McKenzie Seed Co. 1910, 1945, 1972
5.9 McKenzie Seed Co. Centennial Exhibition 1996
5.10 Miscellaneous McKenzie Seed Co. Photographs
5.11 People Connected to McKenzie Seed Co.
5.12 Princess Anne's Visit to McKenzie Seed Co. 1982
5.13 Onion Set Production Book
5.14 Irene Cullen Photographs - McKenzie Seeds Employee Photos
5.15 Josiph Airey Photographs - McKenzie Product Photos
5.16 Alan R. Mundie Seed Production Photographs
5.17 Steele Robertson/Steele Briggs Seeds Photographs
5.18 Seed Packet Display Units Photographs
5.19 Product Photographs
5.20 Parade Photographs
5.21 Oversized Photographs
5.21.1 Drawer #1: Executive Photographs
5.21.2 Drawer #2: Office and Equipment/Plant Photographs
5.21.3 Drawer #3: Miscellaneous Oversized Photographs
5.21.4 Drawer #4: Artifacts
McS 6 Miscellaneous
6.1 Centennial Exhibition
6.2 Miscellaneous Publications
6.3 Scrapbooks
MG 1 A.E. McKenzie Fonds
1.1 Brandon College Inc.
1.2 McKenzie Foundation
1.3 Brandon Allied Arts Council
1.4 Brandon Board of Trade
1.5 Miscellaneous
Radiocarbon date reports have been scanned in multi-page PDF files.
History / Biographical
Crepeele locale Radiocarbon Dates. C14 report by IsoTrace Laboratory for Crepeele site 2005 XU 8.
From 2003 to 2008 field work took place at the Crepeele locale with 75 - 1m x1m units excavated.
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.
Radiocarbon date reports have been scanned in multi-page PDF files.
History / Biographical
Crepeele locale Radiocarbon Dates. C14 report by Beta Analytic Inc. for Crepeele site XU 48 and Graham site XU 54.
From 2003 to 2008 field work took place at the Crepeele locale with 75 - 1m x1m units excavated.
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.
Radiocarbon date reports have been scanned in multi-page PDF files.
History / Biographical
Crepeele locale Radiocarbon Dates. C14 report by Beta Analytic Inc. for Crepeele site XUs 8, 30, 50.
From 2003 to 2008 field work took place at the Crepeele locale with 75 - 1m x1m units excavated.
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.
Radiocarbon date reports have been scanned in multi-page PDF files.
History / Biographical
Crepeele locale Radiocarbon Dates. C14 report by IsoTrace Analytic Laboratory for Sarah site XU17.
From 2003 to 2008 field work took place at the Crepeele locale. The Crepeele, Graham and Sarah sites were excavated with 75 - 1m x1m units excavated
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.
Radiocarbon date reports have been scanned in multi-page PDF files.
History / Biographical
Crepeele locale Radiocarbon Dates. C14 report by IsoTrace Analytic Laboratory for Graham site XUs 5 and 8.
From 2003 to 2008 field work took place at the Crepeele locale. The Crepeele, Graham and Sarah sites were excavated with 75 - 1m x1m units excavated
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 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
Radiocarbon date reports have been scanned in multi-page PDF files.
History / Biographical
North Lauder Radiocarbon Date report by IsoTrace Laboratory for Atkinson II site #TO-11882.
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: Atkinson site and Flintstone Hill.
Radiocarbon date reports have been scanned in multi-page PDF files.
History / Biographical
North Lauder Radiocarbon Date report by IsoTrace Laboratory for Atkinson site #TO-10640.
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: Atkinson site and Flintstone Hill.
Radiocarbon date reports have been scanned in multi-page PDF files.
History / Biographical
North Lauder Radiocarbon Date report by IsoTrace Laboratory for Atkinson site #TO-13365.
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: Atkinson site and Flintstone Hill.
Radiocarbon date reports have been scanned in multi-page PDF files.
History / Biographical
North Lauder Radiocarbon Date report by Beta Analytic Inc. for Flintstone Hill #109529 and #109530.
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: Atkinson site and Flintstone Hill.
Radiocarbon date reports have been scanned in multi-page PDF files.
History / Biographical
North Lauder Radiocarbon Date report by Beta Analytic Inc. for Flintstone Hill #111142 and #111143.
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: Atkinson site and Flintstone Hill.
Radiocarbon date reports have been scanned in multi-page PDF files.
History / Biographical
North Lauder Radiocarbon Date report by Beta Analytic Inc. for Flintstone Hill #109900.
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: Atkinson site and Flintstone Hill.
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.
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.
Field journals have been scanned in multi-page PDF files. Artifact catalogues are PDF files in spreadsheet format. Photographs are in jpeg format.
History / Biographical
Large scale excavations of five block sites took place in 1987 under the direction of Bev Nicholson with Jane Gibson as crew chief. Block A consisted of 12 excavation units.
Scope and Content
Sub-sub-sub series contains: Summary information of field methology, number and co-ordinates of excavations, personnel and their staff position.
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.
Field journals have been scanned in multi-page PDF files. Artifact catalogues are PDF files in spreadsheet format. Photographs are in jpeg format.
History / Biographical
Large scale excavations of five block sites took place in 1987 under the direction of Bev Nicholson with Jane Gibson as crew chief. Block C consisted of nine excavation units. Miggs Green was Block C assistant.
Scope and Content
Sub-sub-sub series contains: Summary information of field methology, number and co-ordinates of excavations, personnel and their staff position.
