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 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
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,
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
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.
24 cm textual records
ca. 95 photographs
memorabilia
History / Biographical
Margaret (Peggy) Doran was born on May 27, 1919 in Brandon, Manitoba to parents Sol and Margaret (Honan) Roberts. Doran grew up in Brandon and was very active in theatre during her high school and college years. Her first theatrical success came at age 20, when she directed Brandon Little Theatre's production of "Send Her Victorious," which received top honours in the Manitoba Drama Festival.
Following her graduation from Brandon College in 1941, she trained as a nurse at Montreal's Royal Victoria Hospital during the Second World War and worked at Vancouver General Hospital for almost a year.
On August 25, 1945, Peg married Dennis Roberts, whom she had met in high school. Dennis, a music graduate from the University of Manitoba in Winnipeg, became interested in psychology after serving overseas with the Royal Canadian Air Force, so the couple moved to Toronto so that he could pursue a psychology degree at the University of Toronto. After Dennis graduated in 1950, the family moved to Sudbury, where Dennis and Peg became actively involved with the education and cultural life of the city. Peg was especially involved with the Sudbury Little Theatre Guild (SLTG), which was founded in 1948.
Between 1950 and 1956, Peg directed or acted in five plays. Her directorial works included: Blithe Spirit, The Importance of Being Earnest, The Glass Menagerie and Antigone. Peg was recognized for her directing of Antigone when she won the Edgar Stone Trophy for Directing in the Dominion Drama Festival in 1955. For the 1956-1957 season, Peg assumed the role of President of the SLTG. During this time, she successfully petitioned the Dominion Drama Festival to create a new region and thus in 1957, the Quebec-Ontario Theatre Association (QUONTA) was founded and Peg acted as its first regional chairperson. Peg's further accomplishments included co-founding and serving on the board of directors of the Sudbury Theatre Centre, as well as acting as drama consultant for the Sudbury Secondary School Board.
Peg was diagnosed with breast cancer in 1997 and, shortly after, in 1998, she moved back to Toronto. She died there on April 2, 2003. Peg and Dennis had three children: Judith Marion (b. June 23, 1946), Steven John (b. September 8, 1950), and Patricia May (b. April 5, 1955).
Custodial History
After Peg's death in April 2003, materials in the collection were gathered and donated to the S.J. Mckee Archives by her children Judith, Steven and Patricia Roberts on July 19, 2003.
Scope and Content
Collection consists of textual records, photographs and other material that belonged to Margaret Doran Roberts. The textual materials include various personal letters, yearbooks, newspaper articles, journals, graduation diplomas, playbills and other miscellaneous records. The collection also includes approximately 95 photographs, mostly personal photographs of weddings and family, but also professionally taken group photos of the play casts. Other materials in the collection include various artefacts kept by Peg throughout her life.
Notes
Description and inventory by Ayn Lewandoski (2003).
Storage Location
MG 2 Brandon College students
2.22 Margaret Doran Roberts
Related Material
Additional archival material pertaining to Peg and Dennis Roberts is located in the archives at Laurentian University in Sudbury, Ontario.
Arrangement
Inventory of the collection:
Pack of matches from Mona's Dress Shop
Cigar that belonged to Sol Doran
Water colour picture, in frame, of St. Paul's Cathedral by Ev Lindsay Hunt from Brandon (1930s)
Earl Haig Graduation bracelet and Grade IX notebook belonging to Peg Doran
Nursing diploma and various other memorabilia from Royal Victoria Hospital, Montreal
Unidentified pictures of war squadron, World War II
RCAF Christmas card from Sergeant William S. Day
Possible home economic project of Peg Doran filled with cake recipes
Photograph: Gordon Savage and Edith Laycock, plus Royal Winnipeg Rifles locket given by Gordon Savage to Peg Doran (with pictures of Gordon and Peg inside)
Francis Bernard Roberts' (Dennis' father) materials: correspondence with Mayo Clinic, photographs and negatives of Indian Chief etc.
Shares belonging to F.B. Roberts
Unidentified photos of children from Brandon (2)
"Willa Cather and the West," essay by Dennis Roberts
Various letters and memborabilia in letter case including:
- personal letters
- Brandon College Annual Arts Banquet programme 1941
- Brandon College Annual Commencement programme 1941
- Brandon College Alumni Dinner program 1941
- Season ticket Manitoba Drama League Provincial Finals Festival 1939
- Manitoba Medical College 4th Annual Ball dance card 1902
- Postcard to Peggy - University of Manitoba Arts Building 1939
- Various report cards from Brandon Collegiate
- Brandon Little Theatre 1936 production "Hay Fever" programme
- Shares from the Brandon Golf and Country Club 1968
- Margaret Doran's United Church of Canada Member's certificate 1933
Blue scribbler from Expression class, filled with various poems, stories, plays etc. belonging to Peg Doran
Miscellaneous newspaper clippings ranging from 1940-1979 (when dated)
Brandon Sun 75th Anniversary edition Saturday January 19, 1957
Sol Doran's daily journal - 1963 (the year of his death)
Picture of Bessie Scott, housekeeper to Sol and Margaret Doran
Wedding photographs, Peg Doran and Dennis Roberts - one in glass frame
"Through the Gateway to Yesteryear" written by Eric Wells and Gordon Tucker and Friends, with inside inscription from Una Johnston
Sheet music (11) of F.B. Roberts, father-in-law of Peg Doran
Sheet music (8) of May Roberts, mother-in-law of Peg Doran
Sheet music (4) of Peg (Doran) Roberts
Unidentified school project, possibly a rough copy of a play, maybe Peg Doran's handwriting
Photo of cast of play "Out to Sea" 1940
Tube containing various graduation diplomas of Dennis Francis Roberts
Peg Doran's graduation diploma, Brandon College 1941; letter and certificate recognizing the change from Brandon College to Brandon University; recognition certificate of attendance to 50th Reunion (1991) as well as photographs from the event attended by Peg and one of her Brandon friends, Jean Downing
Identification bracelet, probably belonging to May Roberts from hospital in London when Dennis Roberts was born
Small glass from Smith Drug Store
Two teaspoons, with initials G.E.B.- George Edward Bennest - uncle of Doh (Doran) Bennest Hammond, lawyer in Winnipeg (Doh's mother, Nell Doran, married Fred Bennest)
Sterling silver child's cup (Peggy) and baby spoon, both belonging to Peg Doran
Various photographs
Dennis Roberts RCAF memorabilia including a hat, epaulettes, brass buttons etc.
Dennis Roberts' Men's Handicap Singles tennis trophy 1932
L.W.G.A. trophy 1933-34, believed to be awarded to Margaret [Mrs. Sol] Doran, an avid golfer
Several pages of photographs of family holidays
- 1958 - to Cornwall, Ontario to look for Doran relatives before St. Lawrence Seaway flooded low-lying graveyards
- 1959 - when family rented a cottage in Clear Lake
Two framed photos of Peg Roberts: as a baby and as a toddler
Wedding announcement of Peg Doran and Dennis Roberts
Dauphin Musical Society photograph 1924
Playbills: Othello (1943); Wonderful Town; and The King & I
Winnipeg Blue Bombers Annual Blue & Gold Football Game program 1959
Play scripts: "Symphony in Illusion;" "Buddy Speaks a Piece;" "At the Photographer's;" and "At the Matinee"
YMCA Winnipeg song sheet
The New Era: 1937 & 1938
The Sickle: 1939, 1940 & 1941
The Quill: Vol. XXIX No. 4 (Oct. 26/38); Vol. XXIX No. 5 (Nov. 4/38); Vol. XXIX No. 6 (Nov. 9/38); Vol. XXXI Nox. 8 (Dec. 12/40)
There are some holes and torn fabric. The flag also has some small stains.
Scope and Content
Item was created by the Brandon College class of 1922 as part of their commencement activities. The flag, which is made of a cotton based material, features the class colours of yellow and black, as well as the class motto "Virtus in Arduis" ("Courage in difficulties"). The flag has a pocket for hanging.
Notes
Loose translations for the class mottos were provided by Dr. Rosanne Gasse (Latin) and Dr. Steve Robinson (Greek), as well as from googling the mottos in October 2006. Description by Trinity Nylen/Jessica Old (February 2024) and Christy Henry.
Some fraying and possible mouse holes. Staining on canvas.
Scope and Content
Item was created by the Brandon College class of 1923 as part of their commencement activities. The flag, which is made of wool and canvas, features the class colours of green and gold, as well as the class motto "Vincit qui patitur" ("The one who is patient wins"). The flag has a pocket for hanging.
Notes
Loose translations for the class mottos were provided by Dr. Rosanne Gasse (Latin) and Dr. Steve Robinson (Greek), as well as from googling the mottos in October 2006. Description by Trinity Nylen/Jessica Old (February 2024) and Christy Henry.
Item was created by the Brandon College class of 1924 as part of their commencement activities. The flag, which is made of wool, features the class colours of green and white, as well as the class motto "Vincit qui patitur" ("The one who is patient wins"). The flag has no method for hanging.
Notes
Loose translations for the class mottos were provided by Dr. Rosanne Gasse (Latin) and Dr. Steve Robinson (Greek), as well as from googling the mottos in October 2006. Description by Trinity Nylen/Jessica Old (February 2024) and Christy Henry.
Item was created by the Brandon College class of 1925 as part of their commencement activities. The flag, which is made of wool and canvas, features the class colours of burgundy and grey, as well as the class motto "Ministrare est Vincere" ("To serve is to conquer"). The flag has a pocket for hanging.
Notes
Loose translations for the class mottos were provided by Dr. Rosanne Gasse (Latin) and Dr. Steve Robinson (Greek), as well as from googling the mottos in October 2006. Description by Trinity Nylen/Jessica Old (February 2024) and Christy Henry.
Item was created by the Brandon College class of 1926 as part of their commencement activities. The flag, which is made of wool, features the class colours of green and orange, as well as the class motto "Non nobis solum" ("Not only for us" or "Not only for ourselves"). The flag has a pocket for hanging.
Notes
Loose translations for the class mottos were provided by Dr. Rosanne Gasse (Latin) and Dr. Steve Robinson (Greek), as well as from googling the mottos in October 2006. Description by Trinity Nylen/Jessica Old (February 2024) and Christy Henry.
Discolouration/bleaching in the centre, mild tearing in the corner, missing fabric on some letters.
Scope and Content
Item was created by the Brandon College class of 1927 as part of their commencement activities. The flag, which is made of wool, features the class colours of black and orange, as well as the class motto "In omnia paratus" ("Prepared for everything"). The flag has a pocket for hanging.
Notes
Loose translations for the class mottos were provided by Dr. Rosanne Gasse (Latin) and Dr. Steve Robinson (Greek), as well as from googling the mottos in October 2006. Description by Trinity Nylen/Jessica Old (February 2024) and Christy Henry.
Material is deteriorating around the edges, staining on canvas pocket, some letters are lifting, some with staining.
Scope and Content
Item was created by the Brandon College class of 1928 as part of their commencement activities. The flag, which is made of canvas, velvet and an undetermined woven material, features the class colours of purple and gold, as well as the class motto "Patet Omnibus Veritas" ("The truth is open to everyone"). The flag has ties for hanging.
Notes
Loose translations for the class mottos were provided by Dr. Rosanne Gasse (Latin) and Dr. Steve Robinson (Greek), as well as from googling the mottos in October 2006. Description by Trinity Nylen/Jessica Old (February 2024) and Christy Henry.
