Jane Gibson was crew chief for the Lovstrom locale in 1987. Her field journals contain information about all Block/sites excavated. Pages 9-27 relate to Block E.
Scope and Content
Record of excavation methods, items recovered, features, local environment and weather noted by teaching assistant.
Record of excavation unit 115 feature 3 at Lovstrom Block E.
Scope and Content
Site records of excavation units may include: level summaries, floor plans, feature sheets, wall profiles, unit summaries and any other additional information relating to the unit.
Georgina Bernice Matiation (Hill) was born in Virden, Manitoba on February 19, 1936, daughter of Gordon and Florence Hill. She received her education at Brandon College (1954-1956). Originally a student in Arts, she graduated from the Teacher Training program in 1956. During her time at Brandon College, Matiation participated in the College Glee Club as well as college track and field meets. She also acted as Junior Ladies Athletic Representative in 1955. In addition, Matiation was was the President of her Normal School class.
Matiation began her teaching career in Hargrave and Melita, before taking a position at Prince Charles School in Portage la Prairie in 1960. She remained at that institution until her retirement in 1991. In addition to her teaching career, Matiation was a past president of the Portage Evening Ladies Curling Club, a past president of the La Prairie Lioness and a leader of CGIT. She was a lifelong member of the Lenore Presbyterian Church.
Georgina Hill married Zane Matiation in 1970. They had no children. Georgina Matiation died on October 28, 1995 in Portage la Prairie at the age of 59 years.
Custodial History
This collection was donated to the McKee Archives by Bessie Marie Hill of Winnipeg on May 1, 1998.
Scope and Content
The collection consists of items collected by Mrs. Matiation (Hill) during her years as a student at Brandon College. The collection contains a scrapbook of photos of students and activities at the College taken from 1954-1956. Fonds includes copies of speeches made by her at various school events, such as her validictorian speech at the Normal School Graduation in 1956. There is also an autograph book with messages to her from friends and classmates. Finally, the collection includes two photographs of students in the 1924-25 Brandon Normal School, and one photograph of the Westminister Presbyterian Church in Brandon.
MG 2 Brandon College Students
2.23 Georgina Matiation (Hill)
The collection is located with MG 2 2.2 Gerald Brown. It was placed there as a result of space issues.
Record of site excavation unit 3 at Graham site 2005.
Scope and Content
Site records of excavation units may include: level summaries, floor plans, feature sheets, wall profiles, unit summaries and any other additional information relating to the unit.
For custodial history see the collection level description of the Lawrence Stuckey collection.
Scope and Content
Brandon Hills Church
Notes
View from northwest showing part of cemetery. Best neg.
[Mr. Stuckey had taped a print to the outside of the envelope. We have separated the negative and the print, numbering them OA3(1) and OA3(1a) respectively.]
For custodial history see the collection level description of the Lawrence Stuckey collection.
Scope and Content
Brandon Hills Church
Notes
View from northwest showing part of cemetery. Best neg.
[Mr. Stuckey had taped a print to the outside of the envelope. We have separated the negative and the print, numbering them OA3(1) and OA3(1a) respectively.]
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
For custodial history see the collection level description of the Lawrence Stuckey collection.
Scope and Content
Brandon Hills Church Choir
Notes
Left to right. Back row: Mrs. Alden Blight, Wes. Stewart, Bessie Waugh (nee Roddick, later Chapman), Mary Baker, Alden Blight. Front row: Rachael Baker, Aletha Blight, Mr. Waugh.
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