Pierian Spring was intended to be a literary quarterly publishing poetry, short stories, creative prose and art work. Submissions were accepted from anyone anywhere on any theme and in any style. The name Pierian Spring was originally suggested by Mr. John Moyle, a former English teacher at Harrison High School, Brandon. The Pierian spring in Thrace was the home of the Muses, daughters of Zeus and Titaness Mnemosyne (Memory). The quarterly was published by Brandon University Press.
Scope and Content
Pierian Spring (Winter 1976) Volume One, Number One contains poetry, short stories, creative prose and art work by various contributors.
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.
Sub-series consists of four scrapbooks detailing life at Clark Hall and Brandon College. They include newspaper clippings, photographs, cards, various programs and ephemera.
Storage Location
RG 1 Brandon College fonds
Series 9: Clark Hall Women's Residence
Item is a scrapbook created by Ernestine Whiteside during her years as Lady Principal of Clark Hall, the women's residence at Brandon College. Scrapbook contains photographs, cards, programs, newspaper clippings and ephemera that document the lives and activities of Brandon College students.
Storage Location
RG 1 Brandon College fonds
Series 9: Clark Hall Women's Residence
Item is a scrapbook created by Ernestine Whiteside during her years as Lady Principal of Clark Hall, the women's residence at Brandon College. Scrapbook contains photographs, cards, programs, newspaper clippings and ephemera that document the lives and activities of Brandon College students.
Storage Location
RG 1 Brandon College fonds
Series 9: Clark Hall Women's Residence
Item is a scrapbook begun by Ernestine Whiteside during her years as Lady Principal of Clark Hall, the women's residence at Brandon College, and continued by successive Deans of Women Olive Wilkins (1919-1925), Jane (Jennie) Turnbull (1926-1927) and Annie (Evans) Wright (1927-1934). Scrapbook contains photographs, cards, programs, newspaper clippings and ephemera that document the lives and activities of Brandon College students.
Storage Location
RG 1 Brandon College fonds
Series 9: Clark Hall Women's Residence
Item is a scrapbook begun by Annie (Evans) Wright during her years as Dean of Women at Brandon College (1927-1934) and continued by her successors D. Werthenbach (1934-1935), Marjorie McKenzie (1935-1936) and Sarah Persis Darrach (1937-1953). Scrapbook contains photographs, cards, programs, newspaper clippings and ephemera that document the lives and activities of Brandon College students.
Storage Location
RG 1 Brandon College fonds
Series 9: Clark Hall Women's Residence
Item is a scrapbook created by Sarah Persis Darrach during her years as Dean of Women at Brandon College. Scrapbook contains photographs, cards, programs, newspaper clippings and ephemera that document the lives and activities of Brandon College students.
Storage Location
RG 1 Brandon College fonds
Series 9: Clark Hall Women's Residence
Item is a scrapbook created by Sarah Persis Darrach during her years as Dean of Women at Brandon College. Scrapbook contains photographs, cards, programs, newspaper clippings and ephemera that document the lives and activities of Brandon College students.
Storage Location
RG 1 Brandon College fonds
Series 9: Clark Hall Women's Residence
Item is a scrapbook created by Sarah Persis Darrach during her years as Dean of Women at Brandon College. Scrapbook contains photographs, cards, programs, newspaper clippings and ephemera that document the lives and activities of Brandon College students.
Storage Location
RG 1 Brandon College fonds
Series 9: Clark Hall Women's Residence
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
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 Atkinson site was named for the landowners Ken and Karen Atkinson who were very helpful to the archaeology and geoarchaeology crews that worked at the site. Their support made the project possible.
The Atkinson site story begins with the discovery of a charcoal lens eroding from the north bank of the Souris River in the summer of 2002. Study of Cultural Adaptations on the Prairie Ecozone (SCAPE) project geoarchaeologist Dr. Garry Running was exploring the stratigraphic layering in the bank when he noted the lens and reported it to Dr. Bev Nicholson. Upon closer examination, a tiny pressure flake was observed on the lens exposure and it was decided to collect a charcoal sample for radiocarbon dating.
The resulting date of 5250B.P cal. 4225 B.C. placed the site in the early Archaic period. A second date on bone collagen of 5580B.P. cal. 4500 B.C. confirmed the earlier date and gave an averaged date of circa 4400 B.C or 6,500 years ago.
The Atkinson site is one of the oldest excavated sites in Manitoba. Based on the date of the site and the kind of lithics (stone tools) present it is considered a Gowen occupation. The Atkinson site is evidence that bison hunters were active on the northern plains at a very early date. Similar sites have also been found on the High Plains in the U.S. and are referred to as the Mummy Cave Complex.
The Atkinson Site is of great importance as it is the first undisturbed site of this type to be excavated in Manitoba and extends the range of these sites south and east from the type-sites in central Saskatchewan. Based on the date and sample evidence further excavations were conducted by Dr. Nicholson's team. in 2003, 2004 and 2006.
Scope and Content
Sub series has been divided into three sub sub series including: (1) Atkinson 2003, (2) Atkinson 2004; (3) Atkinson 2006
Flintstone Hill is located on the north bank of the Souris River. It is a deeply stratified lacustrine, fluvial and aeolian soil profile that has been exposed by the river through stream-bank erosion. This section is thought to be the most complete middle to late Holocene exposure on the northeastern plains. While the value of the site is primarily for paleo-environmental research and reconstruction, cultural deposits have been identified at the site. Local collectors have picked up lithic materials as they eroded out of the bank for the past several decades and it was they who had named the site. Mr. Bruce Timms from Lauder first drew the Flintstone Hill site to the attention of Dr. Nicholson of Brandon University.
During the mid 1990’s to the early 2000’s archaeological testing took place on Flintstone Hill. In 1998, an archaeological field crew dug a series of overlapping trenches down the slope of the profile and produced a schematic drawing. A peat layer at the bottom of this profile, dated from the top at 9,400 RCY and at the bottom to 10,400 RCY, has provided details of marsh plant and insect communities at this time.
Subsequent archaeological investigations at the site recovered several cultural deposits including: a hearth dating to 3250+/-70 R.C.Y. (BETA 109529); a butchered atlas bone 4090+/-70 R.C.Y. (BETA 109990); and bone fragments accompanied by Swan River Chert and Knife River Flint lithic flakes 5350+/-50 (BETA 109530). While no diagnostic tools were recovered, these dates suggest that this occupation, which is contemporary with the Atkinson site, may be a Gowen occupation.
Extensive paleo-environmental research has been conducted at the site. Dr. Running, a geomorphologist from the University of Wisconsin – Eau Claire, participated in the Study of Cultural Adaptations in the Prairie Ecozone (SCAPE) Project and he and his students tested the site for several years. He was joined in this effort by Dr. Havholm, Dr. Boyd, Dr. Wiseman, Dr. Beaudoin, and other SCAPE researchers in the interpretation of the paleo-environment of the Glacial Lake Hind basin. The following article is recommended reading.
Running, Garry L., Karen G. Havholm, Matt Boyd and Dion J. Wiseman
2002 Holocene Stratigraphy and Geomorphology of Flintstone Hill, Lauder Sandhills, Glacial Lake Hind Basin, Southwestern Manitoba. Geographie Physique et Quaternaire
56(2-3):291-303.
Scope and Content
Sub series has been divided into two sub sub series including: (1) Flintstone Hill 1997 (2) Flintstone Hill 1998-2000
Hubert Clayton Weidenhamer was born near Dand, Manitoba in 1926. He was raised in Dand and attended school in the Dand Consolidated School District. Weidenhamer enlisted in the Canadian Army in 1943. He became a member of the Priness Patricia's Canadian Light Infantry. Following training in Canada and England Weidenhamer was sent to Italy. He was badly wounded in battle in mid-September and died of his injuries in November 1944 at age 21. He was buried in the Ancona Military Cemetery, Ancona Italy.
Custodial History
These records were in the possession of Bea Chapin (née Weidenhamer) following their creation in the 1940s until they were donated to the S. J. McKee Archives in January 2011.
Scope and Content
Collection consists of correspondence from Hubert Clayton Weidenhamer to his sister Bea. The letters begin in the spring of 1943. Weidenhamer had enlisted in the Canadian Army in January 1943. His letters detail his induction into miltary life in Fort Garry, Winnipeg and his training experience in Canada, principally at Camp Ipperwash, Lambton County, Ontario. He relates his experience of travels on leave to Detriot. Weidenhamer left Canada from Halifax in late 1943 and arrived in Great Britain in December for additional military training. In England, maintaining his morale, waiting for deployment, and coming to terms with British currency were challenges. Transferred to the Princess Patricia's Canadian Light Infantry, Weidenhamer was deployed to Italy in March 1944. The letters dating from March 1944 to September relate in oblique fashion his's experience of military life on the Italian frontier as the Canadian Army fought its way north - "hard fighting" - and the impact of the war on Italian cities and the countryside. He was "proud" of his conduct in action. Weidenhamer's last letter is dated September 11, 1944.
Collection also includes correspondence on Weidenhamer's behalf from his military Chaplin; two press clippings dealing with his military career, and several facimiles of telegrams and correspondence from the Canadian government officials related to Weidenhamer's death and burial in Italy.
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.
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.
The Executive Committee is a standing committee of the Brandon University Board of Governors that meets regularly two weeks prior to the regular Board meeting. Its membership consists of: Chair of the Board of Governors; Vice-Chair of the Board of Governors; President of the University; Secretary of the Board of Governors; Treasurer of the Board of Governors; Student Representative from the Board of Governors; and Senate Representative from the Board of Governors. The Vice-President (Academic and Research) and the Vice-President (Administration and Finace) act as resource persons. Elections for the Executive Committee take place at the Board of Governors' August meeting each year.
Specific responsibilities of the Executive Committee include: setting the agenda for each regular and special meeting of the Board of Governors; reviewing relevant matters coming before the Board of Governors; acting as a consultative body to the President of the University; dealing with matters delegated by the Board of Governors; referring items to appropriate standing committees of the Board of Governors; acting with the full authority of the Board in situations requiring immediate action prior to the next regular meeting of the Board. The Executive Committee also reviews and recommends policies governing university finance and long-range planning. The Executive of the Board reports to the Board of Governors.
Scope and Content
Sub-series consists of records created by the Executive of the Brandon University Board of Governors. It has been divided into three sub sub series: (1) Board Executive Minutes; (2) Board Executive Correspondence; and (3) Board Executive Agendas.
Notes
History/Bio information taken from Board of Governors By-law No. 11 - Committees of the Board of Governors, Section III - Executive Committee (revised November 23, 2006).
Storage Location
RG 6 Brandon University fonds
Series 2: Board of Governors
2.2 Board Executive
For administrative history see RG 6 (Brandon University fonds), series 2 (Board of Governors).
Scope and Content
Sub-series consists of correspondence and various other documents, including: financial information, legal documents, agendas, reference materials, minutes, blueprints, drawings, reports, briefs, recommendations, proposals and newsclippings.
Storage Location
RG 6 Brandon University fonds
Series 2: Board of Governors
2.4 Correspondence and subject files