70 b&w photographs (various sizes)
7 mm textual records
Physical Condition
Good
History / Biographical
Frances Elizabeth Percival (nee Fraser) attended Brandon College in 1928-1929. She was from Wawanesa, Manitoba and passed away on August 3, 2004 at the age of 93 years.
Custodial History
The records were donated to the McKee Archives by Joy Lalonde, a realtive of Fran Percival's, in 2005.
Scope and Content
Fonds consists of three dance cards from the Brandon Normal School, a photograph album of Brandon College students and activities (many of them identified) and an autographed copy of the 1929 Brandon College Annual Graduation Program.
Approximately 5000 photographic negatives, and some colour prints.
History / Biographical
Morris Predinchuk was a professional photographer, who during the period 1987-1999, was retained by Brandon University to photograph convocations and graduants. Each of the personal portraits was the product of a contract between Predinchuck and a graduant for a graduation photograph. Morris Predinchuk died in Moosomin, Saskatchewan on January 16, 2007 at the age of 75 years.
Custodial History
The images were picked up by the Archives from Predinchuk's business in the Towne Centre Mall on Septemeber 27, 2005.
Scope and Content
Sub-series consists of negatives and prints of approximately 2600 graduants and honourary degree recipients at Brandon University spring and fall convocations from 1987-1998 and the spring convocation of 1999. All the images were taken by Morris Predinchuk.
Notes
For descriptive purposes it was decided to group the negatives by convocation rather than describing each individual negative. Predinchuck's obituary appeared in the January 19, 2007 edition of the Brandon Sun.
Repro Restriction
Copyright privileges do apply. Copyright was assigned to the University through the donor form.
Storage Location
Brandon University Photograph Collection
Series 1: Convocation, scholarships and awards
1.2 Morris Predinchuck fonds
Boxes 1-3
Arrangement
Original order - chronological. All of the negatives are labelled and placed in labelled envelopes.
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,
