In 2003 Units 1 to 9 were excavated at the Sarah site by supervisor James Graham and crew of Sarah Graham, Mike Evans, Todd Kristensen, Shayne Kolesar, Lisa Sonnenburg and Emily Ansell.
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. Sarah Graham's field journal contains notes on the Casselman survey and Crepeele 2003 as well as the Sarah site 2003.
Scope and Content
Record of excavation methods, items recovered, features, local environment and weather noted by teaching assistant.
In 2003 Units 1 to 9 were excavated at the Sarah site by supervisor James Graham and crew of Sarah Graham, Mike Evans, Todd Kristensen, Shayne Kolesar, Lisa Sonnenburg and Emily Ansell.
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. Sarah Graham's field journal contains notes on the Casselman survey and Crepeele 2003 as well as the Sarah site 2003.
Scope and Content
Record of excavation methods, items recovered, features, local environment and weather noted by teaching assistant.
The Sarah site was initially 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 the Sarah site DiMe-28.
In 2004 further excavation took place as part of a Brandon University Archaeology Field School. Units 10 to 18 were excavated with Denise Ens as the instructor and James Graham teaching assistant.
Scope and Content
Record of excavation methods, items recovered, features, local environment and weather noted by teaching assistant.
The Sarah site was initially 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 the Sarah site DiMe-28.
In 2004 further excavation took place as part of a Brandon University Archaeology Field School. Units 10 to 18 were excavated with Denise Ens as the instructor and James Graham teaching assistant.
Scope and Content
Record of excavation methods, items recovered, features, local environment and weather noted by a crew member.
IThe Sarah site was initially 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 the Sarah site DiMe-28.
In 2004 further excavation took place as part of a Brandon University Archaeology Field School. Units 10 to 18 were excavated with Denise Ens as the instructor and James Graham teaching assistant.
Scope and Content
Record of excavation methods, items recovered, features, local environment and weather noted by the instructor.
Field journal by Brandon University Archaeology field school assistant James Graham of excavation methods, items recovered, features, local environment and weather.
In 2005 the Brandon University Field School was held at the Crepeele site in the Crepeele locale.
Denise Ens instructed the school and James Graham was teaching assistant. Field journals were kept by both instructors.
Scope and Content
Record of excavation methods, items recovered, features, local environment and weather noted by teaching assistant.
Field journal by Brandon University Archaeology field school instructor Denise Ens of excavation methods, items recovered, features, local environment and weather.
Brandon University Archaeology field school assistant Jessica McKenzie worked at the Graham and Atkinson sites in 2006. Pages 1 to 44 relate to the Graham site.
Scope and Content
Field journal by Brandon University Archaeology field school assistant Jessica McKenzie. Journal contains information about excavation methods, items recovered, features, local environment and weather. Pages 1-44 relate to the Graham 2006 site.
Field journal by Brandon University Archaeology field school student Erin Platt. Journal contains information about excavation methods, items recovered, features, local environment and weather.
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,
