Box contains minutes geenrated by local MPE associations, collected and microfilmed by the central office. Rolls in this box include the following:
Roll 13: Oakbank 1940-51; Oakburn 1940-51; Oak Lake 1928-51; Oakland 1928-51; Oakville 1928-51; Osbourne 1927-51; Rapid City 1926-51; Pierson 1928-51; Pilot Mound 1928-51; Pipestone 1929-51; Poplar Point 1947-51; Portage 1927-51; Purves 1928-51
Roll 14: Rapid City 1926-27; Rathwell 1928-51; Regent 1927-51; Reston 1927-51; Rhodes 1928-48; Riverton 1948-51; Sandy Lake 1943-51; Selkirk 1947-51; Roblin 1926-51; Rossburn 1929-51; Roundthwaite 1928-51; Russell 1940-51; Ste Agathe 1946-51; St Jean 1949-51; Sanford 1927-51; Scrick 1944-51
Roll 15: missing
Roll 16: Starbuck 1927-40; Stonewall 1939-51; Strathclair 1947-51; Swan Lake 1928-51; Teulon 1940-51; Thorn Hill 1926-51; Tilston 1928-51; Treherne 1928-51; Vista 1940-51; Warren 1947-51; Waskada 1925-51; Wawanesa 1927-51; Wood Bay 1937-51; Wood Bay 1926-37; Wood North 1928-51
Roll 17: Side 1 Alexander to Birdtail Oct 1951 – June 1957; Side 2 Birnie to Cartwright Oct 1951 – June 1957
Roll 18: Side 1 Chillon to Ebor Oct 1951 – June 1957; Side 2 Eden to Fork River Oct 1951 – June 1957
Roll 19: Side 1 Forrest to Hamiota Oct 1951 – June 1957; Side 2 Harding to Kronsgart Oct 1951 – June 1957
Roll 20: Side 1 Landseer to Maples Oct 1951 – June 1957; Side 2 Margaret to Napinka Oct 1951 – June 1957
Roll 21: Side 1 Neelin to Purvis Oct 1951 – June 1957; Side 2 Rapid City to Silverton Oct 1951 – June 1957
Roll 22: Side 1 Sinclair to Warren Oct 1951 – June 1957; Side 2 Waskada to Woodnorth Oct 1951 – June 1957
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 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.
See sub sub series RG 6 14.5.3 The Quill for History/Bio information.
The duplicates retained were chosen to provide an illustration of the changing content and format of the Quill from 1930-1975. They are primarliy for display purposes, as microfilm copies are available for researchers. The original copies of the Quill provide an archival record, but these may be used only under most unusal circumstances. Additional duplicates were culled.
Custodial History
See sub sub series RG 6 14.5.3 The Quill for Custodial history.
Scope and Content
The McKee Archives holds duplicate editions of The Quill for the following years:1930-1931, 1933 to 1942, 1946 to 1949, 1955 to 1959, 1962-1963 and 1975-1976.
The microfilm copies of the Quill cover the period from September 1930 to March 1972, and are located with the originals. The Archives holds both positive and negative versions of the microfilmed editions. The microfilming was made possible through a grant from Dr. Thomas McLeod (Brandon College 1940) in 1999.
Notes
The Quill duplicates and special editions are stored in the same box.
The Brandon Sun transferred the original copies of the Brandon Daily Sun, 1900-1917 to the McKee Archives for the purpose of having them preserved and microfilmed.
Money provided by the Manitoba Council on Post-secondary Education for the development of Manitobia, a website created by the Manitoba Libraries Consortium, included funds for the microfilming and digitization of the Brandon Daily Sun held at the S.J. McKee Archives.
In the summer of 2009, the hard copy edition of the Brandon Daily Sun were sent to the offices of OCLC Preservation Service Center, now Backstage Library Works, in Bethlehem, Pennsylvania. Backstage undertook to cut the bindings of the paper and prepare master and service microfilm copies of the entire run of the publication.
The microfilm copies were shipped from Backstage to the University of Manitoba and subsequently to the McKee Archives, arriving the week of January 18, 2010. The original hard copies of the Brandon Daily Sun will also be returned to the McKee Archives.
A digital version of the microfilm will appear of the Manitobia website.
Custodial History
Microfilm was created by Backstage Library Works in Pennsylvania from hard copies of the Brandon Daily Sun held by the McKee Archvies during the winter of 2009-2010. The master and service copies of the microfilm were delivered to the McKee Archives in January 2010.
Scope and Content
Fonds consists of Archival Master copies and Service copies of the Brandon Daily Sun (February 5, 1900- December 31, 1917).
Photograph was donated by C. Allan Elsey in September 2003. The photograph belonged to the donor's father Charles Spurgen Elsey.
Scope and Content
Item consists of portraits of the members of the Ministerial Association of Brandon College. Members included: J.W. Williamson; L. Whitelaw; C.S. Elsey; C. Gale; R. Standerwick; A.S. Parnell; W.P. Freeman; John Erb; A. Bowbrick (Vice President); E. Selley (President); H.S. Sneyd (Sec. Treasurer); A.W. Mayse; H.S. Mullowney; William Parsons; Rev. R. McKay; Dr. A.P. McDiarmid; R.J.M. Caul; W. Smalley; H. Winton; George Reynolds; George Merritt; G. Siemens; F.W. McKinnon; F. Crossley; H.F. Finch; H.H. Best; J.H. Frith; H.S. Bagnell; and James Start.
Bob and Kay Howland at Dunrobin, in Ottawa, hosted a reunion of the Brandon University Alumni Association. Present at the function were : Jim and Marina Lalung, Mr. and Mrs. Assison Boles, Ed Neal, Connie and Del Hewitt-White, Dorine and Hugh Best, Mary and Jack Wickers, Ian and Beverley Barnes, Nevin and Mary Ann Shaw, Mr. and Mrs. Roberts, Carol and Bob Milne, Dorothy and Clay Elston, Lenore Dinsdale, Bob and Elsie Farrell, Willa Davies, Jack Perkins (Association President), Bob and Kay Howland. This reunion included people from Orleans, Fitzroy Harbour, Stittsville, Manotick, Kingston, Ottawa, and Brandon, MB. Group photo taken at the reunion
Photograph shows Robert (Bob) Ford dressed as the Pied Piper playing a soprano saxophone surrounded by children in costume, some carrying Brandon University Alumni pennants. Photo was taken during the Brandon University Homecoming Parade held in downtown Brandon.
Block B consisted of 20 contiguous 1m2 units excavated to 30 cm below surface. (except unit 58 which was excavated to 35 cm bs to obtain extended soil profile). The block is situated in recent oak and poplar forest at the head of a ravine leading to Jock’s Creek, adjacent to an area cleared for market gardening. As was the case with Block A, the understory is heavily overgrown with hazelnut, chokecherry, saskatoon, and a poison ivy/sarsaparilla ground cover.
The soil levels below the sod in Block B consisted of a black, silty, and gritty loam layer from 5 cm to 23 cm below surface, a yellow and sandy clay from 23 cm to 30 cm below surface, and glacial till at 30 cm below surface. As in Block A, limestone cobbles were found throughout the occupation level around the bone. It is evident that bioturbation – primarily tree roots and rodent burrowing – have significantly altered patterns of original deposition of lithics, ceramics and small bone.
The faunal layer lay close to the surface, situated entirely in the black loam 5 cm – 23 cm below surface. The 23 cm depth also marked the end of the dark silty loam. At 10 cm below surface, a discernible patterning of the bone appeared. Concentrations of bone in narrow rows ran in an irregular pattern from the northwest to the southeast part of the block. This pattern was most apparent in the north end of the block which is the highest point in the block. In the same 1m2 unit, patches of weathered, very poorly preserved bone would be found lying close to patches of well preserved bone. It is believed that this variability in preservation results from uneven rates of burial due to taphic activities of pocket gophers or other agents of bioturbation. The same pattern of uneven preservation occurs over much of the locale but is most evident in Block B.
Diagnostic lithics included eleven projectile points that were predominantly Plains or Prairie Side-notch types, but included two unnotched triangular points. Cord-wrapped impressed rim sherds and body sherds were recovered. The ceramics are variants of the Woodland Blackduck horizon.
RC dates: XU49 – 675/80 BP XU 59 – 705/75BP.
Scope and Content
Sub-sub-sub series contains: Summary information of field methology, number and co-ordinates of excavations, personnel and their staff position; Field journals are daily records of recoveries, features and activities at the site; Site records include excavation level and unit summaries, feature sheets, profiles; sample records and maps; Artifact catalogues are lists and identifications of all artifacts recovered; Photographs are of excavation units, features, the landscape and personnel.
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