ARCH 2: North Lauder Locale
The North Lauder locale has a long archaeological and geological history that is important for understanding the forces that shaped the region. Archaeological research in the locale shows that the area has been occupied by humans for at least the past 6,500 years. Environmental forces provided an area of diverse resources that attracted early peoples.
Environment of the Lauder Sandhills
The North Lauder locale is part of the greater Lauder Sandhills area. The glaciers that covered this region began to recede approximately 11,000 years ago leaving a large lake known as glacial Lake Hind. The Souris River, the Lauder Sandhills and the Oak Lake Aquifer are remnants of the environmental and geological forces that shaped the region.
The Lauder Sandhills region is characterized by a landscape of sand sheets and stabilized sand dunes interspersed with a variety of wetlands. This complex topographic and hydrological situation favoured the development of an island mosaic of mixed forest, wetland and meadow, surrounded by mixed grass prairie. The result was a large, isolated ecotone which provided a rich variety of subsistence resources for hunter-gatherers.
Research in the Lauder Sandhills
Archaeologists from Brandon University have been conducting research in the Lauder Sandhills since 1991. Research in the North Lauder locale has focused on the Atkinson site, a 6,500 year old hunter-gatherer site and Flintstone Hill.
The Atkinson site
The Atkinson site is one of the oldest excavated sites in Manitoba and has been Radiocarbon dated to 6,500 years before present. The Atkinson site is located on the bank of the Souris River and was discovered when a hearth (fire pit) was seen eroding out of the bank. 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.
Flintstone Hill
The geomorphology of the glacial Lake Hind Basin over the past 11,000 years is known primarily through the study of a cut bank along the Souris River. Flint Stone Hill contains the most complete stratigraphic record for the post-glacial period on the northern plains. The site has been extensively studied by geoarchaeologists, geologists and paleoenvironmentalists over many years and their findings have contributed to our understanding of the region.
The North Lauder locale Borden designations of Atkinson site DiMe-27 and Flintstone Hill site DiMe-26.
Borden System
Archaeological sites in Canada are identified by the Borden system, which is a uniform site designation system. The country is divided into grids based on latitude and longitude in blocks of 10 x 20 minutes. The first 4 letters indicate the block and the following numbers indicate the actual site. For example the area of the Lauder Sandhills in southwestern Manitoba is identified by the letters DM and the North Lauder locale within that area is DiMe. The Atkinson site is DiMe-27 and the Flintstone Hill site DiMe-26. As new sites are discovered they will be numbered sequentially.
Scope and Content
The Series has been divided into two sub-series, including (1) Atkinson site DiMe-27 and Flintstone Hill site DiMe-26.
The Lovstrom locale first came to the attention of Dr. Nicholson through conversations with landowners Mr. and Mrs. Herb Lovstrom in 1985. Lovstrom is a multi-component archaeological locale located 25km south of Brandon overlooking the Souris River channel. The landowner’s surface collection and the presence of bone and artifacts in a cultivated field indicated the presence of one or more sites.
Limited testing was conducted in 1985 and 1986, followed by major excavations in 1987, 1988 and 1991. Eight sites of block excavations with a total of 132 1m2 excavation units were completed. The locale area extends approximately 500m north from the edge of the Souris Valley escarpment and over 200m east from the Jock’s Creek escarpment.
Physical and biological environment As has been noted above, the locale is bounded on the south by the Souris channel and on the west by the incised channel of Jock’s Creek and a till plain extends to the north and the east. This plain is characterized by buff colored glacial till with numerous rocks embedded in the surface. Surrounding these rocky knolls are dark-soil hollows where the various cultural occupations are found. The depth of the topsoil layer suggests a long term grassland cover with the present oak forest likely developing in historic times due to the elimination of bison grazing and the controlling of prairie fires in late historic times. A small cleared patch of farmland is found within the boundaries of the locale area. This area has provided a substantial surface collection of artifacts.
Present vegetation in the area is a mosaic of aspen/oak forest groves and mesic grass prairie that includes introduced species such as brome grass. In poorly drained areas, willow and red osier dogwood are present. The Lovstrom locale is found in a forested area dominated by oak with an under story of saskatoon, chokecherry, pin cherry, and hazelnut brush. Poison ivy is abundant as well as sarsaparilla.
The major faunal resources in Precontact times would have been bison, with elk and mule deer playing a minor role. Antelope may have been present also. Small animals included snowshoe hare, cottontails, porcupines and beaver. Canids, including wolf, coyote, fox and domesticated dog were present, as well as mustelids such as badger, mink, and weasel. Fragments from a fisher were also recovered in the excavations.
Summation.
The Lovstrom locale has eight sites. The sites were designated and excavated as Blocks A, B, C, D, E, F, G and H. Many of the sites are multi-occupations.
The Vickers materials are primarily confined to Blocks D, E, F, G and H. Vickers Focus materials overlie Blackduck/Duck Bay materials. Blackduck and Duck Bay materials are found in the lower levels of all excavation blocks and in most test units. The Vickers occupations at the Lovstrom locale, based upon ceramic wares and an overlapping of C14 dates, appear to have been contemporary with the Lowton type site to the east, near Belmont. A small protohistoric occupation was identified overlying part of Block D. Faunal remains are abundant with bison clearly dominating the assemblages. Lesser amounts of canid are present as well as small mammals including beaver, hare and mustelids. Small amounts of avian species are also present.
Publications
Nicholson, B.A.
2011 The Role of Pocket Gophers (Thomomys talpoides) in Restructuring Stratigraphic Relationships at the Lovstrom Site. Canadian Journal of Archaeology 35:323-331.
Nicholson, Bev, Scott Hamilton, Matthew Boyd and Sylvia Nicholson
2008 A Late Plains Woodland Adaptive Strategy in the Northern Parklands: the Vickers Focus Forager-Horticulturists. Invited Paper for Papers in Northeastern Plains Prehistory, eds. Michael G. Michlovic and Dennis L. Toom, North Dakota Journal of Archaeology Vol. 8:19-34.
Nicholson, Bev and Scott Hamilton
2001 Cultural Continuity and Changing Subsistence Strategies During the Late Precontact Period in Southwestern Manitoba. Canadian Journal of Archaeology 25:53-73.
Nicholson, Bev
1996 Plains Woodland Influx and the Blackduck Exodus in South-Western Manitoba During the Late Precontact Period. Manitoba Archaeological Journal 6(1):69-85.
Nicholson, Bev and Mary Malainey
1991 Report on the 1991 Field School Excavations at the Lovstrom Site (DjLx-1), Southwestern Manitoba. Manitoba Archaeological Journal 1(2): 51-93.
Nicholson, Bev and Jane Gibson
1990-91 Lovstrom Site Field Report, 1987 Excavations. Saskatchewan Archaeology 11&12:46-68.
Nicholson, Bev and Ian Kuiijt
1990 Field Report and Interpretations of the 1988 Archaeological Excavations at the Lovstrom Site (DjLx-1) in Southwestern Manitoba. North Dakota Journal of Archaeology 4:166-205.
Nicholson, Bev
1990 Ceramic Affiliations and the Case for Incipient Horticulture in Southwestern Manitoba. Canadian Journal of Archaeology 14:33-60.
Nicholson, Bev
1986 The Lovstrom Site: Culture Contact in Prehistory. Manitoba Archaeological Quarterly 10(1):35-71.
Scope and Content
The Series has been divided into nine sub-series, including (1) Survey (2) Block A; (3) Block B (4) Block C; (5) Block D; (6) Block E; (7) Block F; (8) Block G; (9) Block H
Introduction
Information on archaeological materials in this locale first came to the attention of Dr. Nicholson through Doug Jackson, a local artifact collector from Souris. Doug had observed archaeological materials that included bone, ceramics and lithic material that had been exposed by municipal road building activity, northwest of Lauder Manitoba
Environment
The Makotchi-Ded Dontipi locale is located among stabilized sand dunes in the Lauder Sandhills in Southwestern Manitoba, northwest of the village of Lauder. The area is a mosaic of medium grass prairie and copses of aspen poplar and aspen-oak, together with intermittent sedge grass marshes and small ponds. These wetlands are bordered with balsam poplar, water birch, willows and red osier dogwood.
The well-drained upland forest also contains saskatoon, chokecherry, wild current, hazelnut bushes and occasional wild plums. Lowland areas have nannyberries and high-bush cranberry. Wild strawberries grow in lightly shaded areas along trail margins and in open patches in aspen forest.
History of Excavations
The Makotchi-Ded Dontipi locale is a virtual "island" of forest and marshlands in a vast expanse of mixed grass prairie. This archaeologically and environmentally rich area was given the Dakota name Makotchi-Ded Dontipi, meaning "the place where we live".
Summation
Prior to European settlement, the area was a rich environment for hunter-gatherer people. Archaeological investigations from 1992 to 2002 have revealed numerous sites within the locale. Some of these sites have been extensively excavated while others have been identified or tested.
Seven sites that have been identified in this locale range in age from the historic through protohistoric periods and extend into the middle precontact period. The major sites are the initial Middle Missouri Duthie site, the late precontact Jackson, Bradshaw sites and the protohistoric Twin Fawns, Schuddemat and Hollow B sites. The multi-component Vera site includes historic Métis, late precontact Vickers Focus, and middle precontact Besant, Pelican Lake, McKean Complex and Oxbow occupations. Over 230 units were excavated as well as numerous test pits and several extensive surveys.
Scope and Content
Scope and Content
The Series has been divided into seven sub-series, including (1) Duthie site (2) Jackson site (3) Twin Fawns site (4) Vera site (5) Schuddemat site (6) Bradshaw site (7) Hollow B site.
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 Brandon College Dean was the head of the College in the absence of the President. It was created in 1925 after the sudden passing of Dr. Sweet. Dr. Harris MacNeill, who had been Dean in Arts up until that time assumed the position of College Dean. The duties of the College Dean were as follows:
1. In the absence of the President of the College he shall exercise the functions of the President in relation to all “inside” College matters; it being understood that frequently it may be necessary for him to exercise his personal judgment apart from anything that may be specified in this memorandum.
2. With respect to matters of special importance arising unexpectedly he shall consult with the Chairman of the Board, or by telegram with the President, or both.
3. All questions arising that have a direct connection with the “business” aspects of College affairs shall naturally be referred to the Chairman of the Board, or the President, or both.
4. In the absence of the President he shall preside at all Faculty meetings, Committee meetings of which the President is Chairman, and shall attend meetings of Committees of which the President is an ex-officio member.
5. In the President’s absence he shall preside at the regular Chapel Exercises and at special College gatherings in the Chapel at which the President would naturally be expected to preside.
6. He shall also keep in touch with the work of the several departments of the College and shall consult frequently with the Heads of such departments.
7. While the Lady Principal and the Resident Master are responsible for the detailed administration and discipline of the College life and activities of Clark Hall and Brandon College respectively, the College Dean shall have the absent President’s responsibility for the general discipline of the College in respect of the students’ relation to Courses of Study, Corridor, Campus, etc.
8. That the President when absent may be kept in touch with the work of the Institution it is desirable that the College Dean keep him informed of the more important happenings and problems with College life.
9. Throughout the Session the College Dean shall be Registering Head of the Arts Department.
The position of College Dean continued until 1952. In 1952 the position became known as the Dean of Arts and Science. In 1963, another change occurred, with the two departments going separate ways. From that time on there was both a Dean of Arts and a Dean of Science.
BRANDON COLLEGE DEANS:
HARRIS LACHLAN MACNEILL (1925, 1926-1928)
Dr. MacNeill was born in Paisley, ON on November 29 or 30, 1871, the son of Rev. Donald and Amanda (Hemenway) MacNeill. He received his B.A. from McMaster University in 1894. He was also educated at the Ontario College of Pedagogy and the University of Toronto. From 1895 until 1898 he was a teacher at Woodstock College. In 1899 he married Anne Hatch. From 1899 until 1903 he was a professor of Latin at Washburn College in Topeka, Kansas. In 1903 he accepted an offer to teach Latin and German at Brandon College. In 1909 he was a Professor of the New Testament, Language and Literature, as well as Resident Master. Dr. MacNeill was the Academy Principal for two years. He then received his Ph.D. from the University of Chicago in 1911. MacNeill acted as the Dean of Arts from 1912 until 1930. Dr. MacNeill was the central figure in the scandal involving Brandon College in the early 1920’s. The Fundamentalist Baptists accused Brandon College, and Dr. MacNeill especially, of teaching Modernist views. He was absolved of any charges at the 1924 Baptist Convention in Chicago.
Dr. MacNeill was Acting President of Brandon College after Dr. Sweet died for the period from January 1925 until Dr. Bovington was hired in August 1925. After Dr. Bovington resigned in May of 1926, Dr. MacNeill again accepted the position of Acting President from May 1926 until April 3, 1928, when he retired as College Dean. Dr. MacNeill taught Latin and Greek for two more years then retired from Brandon College in 1930. He accepted a position at Fairview Church in Vancouver, B.C. where he remained until 1932. In 1932 he was offered a teaching position at McMaster University. He married his second wife, Vera Leech, in 1939. He remained at McMaster teaching New Testament Interpretation until 1943 when he retired. Dr. MacNeill was the first person to receive an honorary degree from Brandon University in 1967. He continued to do religious research until his eyesight failed at age 97. On January 15, 1974, Dr. MacNeill died at the Chedoke Hospital at the age of 102.
JOHN ROBERT CHARLES EVANS (1928)
Information on J.R.C. Evans can be found under the heading Office of the President.
W. BURTON HURD (1929-1935)
No biographical information yet.
C.F. RICHARDS (1935-1937)
Information on C.F. Richards can be found under the heading Office of the Registrar.
REV. EVAN M. WHIDDEN (1937-1938)
See MG 1 Brandon College Teaching and Administration, 1.8 Evan McDonald Whidden fonds for biographical information and additional records related to Rev. Evan M. Whidden.
A. HAYWARD FOSTER (1938-1939)
No biographical information yet.
F.J. WESTCOTT (1939-1945)
Frederick James Westcott was born in Douglas, Manitoba. He began taking classes in the Academy at Brandon College in 1918. He entered the Arts course in 1921 and specialized in Political Economy. He received the Special Political Economy Medal in his final year. He was very active on committees and associations, as well as sports. Westcott served as the Senior Stick during the school term 1924-1925. He graduated with his B.A. from Brandon College in 1925.
Westcott received the position of Student Assistant in the Academy the following year. He left soon after to pursue post-graduate work. He received his M.A. in economics from Harvard and spent two years at the University of Toronto on a teaching scholarship in economics, completing the course work leading to the Ph.D. degree. In 1929, he returned to Brandon College and took up the position of Associate Professor of Political Economy. It was also in 1929, that Westcott married Rose Vasey, a 1926 Brandon College graduate. The following year, Westcott was the Resident Master of Brandon College, as well as being an Instructor in Political Economy and Sociology. The Resident Master position only lasted the one school year. He accepted the post of Acting Dean of Arts and Science in 1939. From 1942 until 1945 he was away on military leave with the National War Finance Committee. He resigned from the position of College Dean in 1945. From 1945 on Westcott and his family resided in Toronto. He died suddenly in 1961.
HENRY STEWART PERDUE (1947-1952)
Dr. Perdue was born in 1904 near Souris. He graduated from the Souris Collegiate in 1920. After working several odd jobs, Dr. Perdue entered Brandon College in 1924. He graduated with his B.A. in 1928. After graduation, Dr. Perdue was hired as a teacher in the Academic Department. He received his M.A. in 1930, and went on to receive his Ph.D. in Geology from the University of Chicago. In 1930, Dr. Perdue became the Director of the Matriculation Department as well as an Instructor in Geology. In 1931, he took over the position of Resident Master. In 1937, he married Ella May Higgens, who was the Resident Nurse. From 1938 until 1948, Dr. Perdue acted as Registrar of Brandon College.
In 1947, Dr. Perdue accepted the position of College Dean. This position ran until 1952, when it was changed to the position of Dean of Arts and Science. Dr. Perdue also held this position until 1962, when the office separated into the Dean of Arts and the Dean of Science. Dr. Perdue continued in the position of Dean of Science until 1967. After Dr. Evans death in July of 1959, Dr. Perdue became Acting President. He held this position from August 1959 until August 1960, when Dr. Robbins was appointed President. Dr. Perdue retired from teaching Geology in 1973. He died on December 22, 1979 at the age of 75.
DEAN OF ARTS AND SCIENCE:
H.S. PERDUE (1952-1963)
Information on H.S. Perdue can be found under the heading College Dean.
DEAN OF ARTS
R.F.B. KING (1963 - Brandon University)
Information on R.F.B. King can be found under RG 6 Brandon University fonds, sub-sub series 7.1.1 Dean of Arts.
DEAN OF SCIENCE:
H.S. PERDUE (1963-1967)
Information of H.S. Perdue can be found under the heading College Dean.
Scope and Content
The series consists of records from MacNeill's term as College Dean (1921-1928). It also includes correspondence during the time that MacNeill was Acting President. It contains letters to and from MacNeill regarding examinations, students, business, and finances. Some earlier letters also include correspondence regarding the controversy MacNeill was in during the Baptist Fundamentalist/Modernist Debate in the early 1920’s.
Records from Evans' term as Acting Dean have been included in his Presidents' files. There are no records from the terms of the other College Deans, except R.F.B. King; his records have been encorporated into RG 6 (Brandon University fonds), 7.1.1 (Dean of Arts).
Storage Location
RG 1 Brandon College fonds
Series 6: Office of the College Dean
Related Material
RG 6, sub sub series 7.1.1 (Dean of Arts) for additional Dean's records and RG 6, series 9 (Department of Extension) for additional records related to H.S. Perdue.
In 1914 World War I broke out in Europe. As soon as Britain became involved in the war, Canada, as part of the British Empire, was involved. As soon as Canada became involved in the war, Brandon College became involved. In keeping with the patriotism of the time, Brandon College organized a Canadian Officers Training Corps in 1915. It was soon a common sight to see students drilling several times a week in every type of weather. Often the women of the college would offer food and drink after the more grueling experiences. In 1916, a Brandon College platoon was organized under J.R.C. Evans. When he was declared medically unfit to go overseas, the command went to Lieutenant William Carey McKee. Carey was the son of S.J. McKee. He had graduated from Brandon College in 1914, and secured his M.A. in 1915. The Brandon College platoon joined up with the Western Universities Battalion, the 196th. The men went overseas in 1916, most remained there until after the war. Sadly, their admired leader, Carey McKee, was killed on August 26th, 1918 at Arras, just months before the end of the war.
Over thirty other Brandon College men failed to return home from the war. Remaining students immediately began planning for a memorial gymnasium to honour their fallen friends. They eventually raised over $20 000 towards the gym, but the money was given as a gift to the administration during the late 1920’s and early 1930’s when the College was in dire need of money. Although the Students’ Memorial Gymnasium Fund went on for several years, due to lack of money and rising building costs, the memorial gymnasium was never built.
The C.O.T.C. remained on the campus, but it was not as integral a part of daily routine until the late 1930s. Once again, hostilities broke out in Europe. This time, however, Canada did not automatically become involved in the war when Britain did. In an attempt to show the world its independence, Canada waited five days before officaially declaring war. By 1940, the C.O.T.C. was in full swing again. As well, part of Brandon College was given to the Royal Canadian Air Force for use as classrooms and accomodations.
After the cessation of World War II, the C.O.T.C. remained on campus. The S.J. McKee Archives has records of the organization up until 1960. The 1951 Brandon College Calendar decribes the University of Manitoba contingent of the C.O.T.C., so at some point the two organizations were amalgamated. The 1954 Brandon College Calendar decribes the R.C.A.F. (Reserve) University of Manitoba Squadron that students can apply for. Finally, the 1957 Brandon College Calendar contains a description on the Regular Officers Training Plan, which students could apply for. All of these programs were still in effect when the College was granted its University Charter in 1967.
Scope and Content
The first member of Brandon College to join up was a professor, Philippe Louys. He happened to be visiting his father in France when hostilities broke out. He joined the French Army, and was almost immediately taken prisoner. For several years he tried to escape, finally being successful on his fourth try. Louys immediately began retraining in the French Army, but as soon as he was ready to fight again, the war ended. Philippe Louys’ story is not uncommon in the history of Brandon College. The professors and students felt it was their duty to join the ranks and fight along with the rest of the British Empire. Most of them left the halls of the College, and many never returned.
The records consist mainly of correspondence having to do with the Canadian Officers Training Corps. There are also letters refering to Brandon College students who served in the World Wars. As well, there are lists of Unit Orders and Syllabii for the instructors of the C.O.T.C. There are also files regarding the War Maintenance Fund from 1918 and 1919. These records are a good source of material for studying how Brandon College viewed the outbreak of hostilities in Europe, and how the College responded to the crisis. Also, they show how attitudes changed about war and the college’s role in it from the period of 1915 to 1960. The Presidents’ files also have information on the role the military played at Brandon College. Finally, the series contains attestation and application for military training forms (1941-1943).
Storage Location
RG 1 Brandon College fonds
Series 11: Brandon College Military Training Programs
In accordance with "The Brandon University Act (1998)" the Brandon University Senate consists of the following members: (a) the chancellor of the university; (b) the president of the university; (c) the vice-presidents of the university; (d) the deputy minister of the department whose minister is responsible for The Council on Post-Secondary Education Act, or his or her designate; (e) the deans of each faculty and school in the university; (f) the director of the Educational Technology Unit or, if there is none, the person exercising comparable functions (g) the chair of the Bachelor of General Studies degree program or, if there is none, the person exercising comparable functions; (h) the University Librarian or, if there is none, the person exercising comparable functions; (i) the Dean of Students or, if there is none, the person exercising comparable functions; (j) one member of the board appointed by the board; (k) one representative from each faculty or school who has been on the staff of the university for at least two years, elected by and from the staff of that faculty or school; (l) six professors or associate professors of the university, elected by the professors, associate professors, assistant professors and lecturers; (m) two assistant professors or lecturers of the university who have been on the staff of the university for at least two years, elected by the professors, associate professors, assistant professors, and lecturers; (n) one member of the rank of professional associate of the university elected by the members of that rank; (o) eight students elected or appointed as follows: (i) one appointed by the executive of the Brandon University Students’ Union who is a member of that executive. (ii) one elected from each faculty or school of the university, (iii) the remainder elected from the student body of the university at large.
Elected and appointed members of the senate, other than student members, are to hold
office for two years, beginning on July 1 of the year in which they are elected or appointed. Student members of the senate are to hold office for one year, beginning on the first day of July of the year in which they are elected. Ex officio members are to hold office until they cease to hold the position that qualify them for membership. An elected or appointed member of the senate is eligible for re-election or re-appointment, but the senate may set a maximum number of consecutive terms of office that any member may hold.
The president of the university shall be the chair of the senate. If the president of the university is absent or unable to act as chair, the vice-president (academic and research) or, in his or her absence, an academic dean appointed by the president, shall be the chair at meetings of the senate. The registrar of the university or, if there is none, the person exercising comparable functions shall be the secretary of the senate.
The senate shall meet at least four times a year and may meet more often if its rules so provide. The secretary of the senate shall call special meetings at the request of the chair or at the written request of at least four members of the senate.
The senate is responsible for the academic policy of the university. The senate may (a) establish rules and procedures for the conduct of its proceedings, including fixing a quorum; (b) elect the chancellor of the university; (c) appoint any standing and other committees that it considers necessary; (d) consider and determine all courses of student, including requirements for admission, examination and graduation; (e) recommend to the board the establishment of additional faculties, school, departments, chairs and courses of instruction; (f) determine the degrees, honorary degrees, diplomas and certificates of proficiency to be granted by the university, and the persons to whom they are to be granted; (g) award scholarships, medals and prizes; (h) make rules and regulations respecting the academic conduct and activities of students; (i) consider and make recommendations to the board about any other matters that the senate considers appropriate for achieving the objects and purposes of the university.
Scope and Content
Series has been divided into six sub-series, including: (1) Senate minutes; (2) Committees of Senate; (3) General Faculty Council; (4) Ad Hoc Committees of Senate; (5) Convocation services, Baccalaureate services, Banquets; and (6) Brandon College/University calendars.
Notes
Information in the History/Bio field was taken from "The Brandon University Act (1998)" at http://www.brandonu.ca/administration/governors/documents/BU_Act.pdf (December 2005).
The Brandon University Foundation was incorporated by an act of the Legislature in 1981, with the express purpose of promoting education in the Brandon area. The Foundation is limited to 21 Directors. There Foundation also has a Liaison Committee, formed as a communications link between the Board of Governors and the Foundation, composed of three members from each group.
Scope and Content
Series consists of the following files: preliminary investigation; Annual Giving Committee; BUFund (establishment) Committee; general; Student Assistant Fund; Student Christmas Fund; Blair Fraser Memorial Fund; Friends of Brandon College Inc. (USA); and Brandon University Association (1967-72).
Notes
History/Bio information taken from Campus News - September/October 1986.
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.
Radiocarbon date reports have been scanned in multi-page PDF files.
History / Biographical
The Crepeele locale is located within the larger Lauder Sandhills area, located in southwestern Manitoba. The area is a complex region of high biodiversity made up of stabilized sand dunes and wetlands that encourage the development of mixed forest and grass prairie. This area provided a variety of subsistence resources for pre-European hunter-gatherers. At the present time the grass prairie is now farm land but the areas of vegetated sand dunes have not been cultivated and have revealed numerous pre-contact archaeological sites.
Archaeological surveying was conducted in 2003. The results of the 2003 Casselman survey showed over 300 test uints contained cultural material and indicated several areas for further examination including the Crepeele site DiMe-29, Sarah site DiMe-28 and Graham sites DiMe-30.
From 2003 to 2008 field work took place at the locale with 75 - 1m x1m units excavated. The Crepeele locale is a complex region of high biodiversity made up of stabilized sand dunes and wetlands that encourage the development of mixed forest and grass prairie. This area provided a variety of subsistence resources for pre-European hunter-gatherers. At the present time the grass prairie is now farm land but the areas of vegetated sand dunes have not been cultivated and have revealed numerous pre-contact archaeological sites.
To help establish the cultural sequence at the locale Radiocarbon dates were obtained from the three sites in the Crepeele locale.
Radiocarbon dating
The technique of radiocarbon dating was developed by Willard Libby and his colleagues at the University of Chicago in 1949.
Radiocarbon dating is used to estimate the age of organic remains from archaeological sites. Organic matter has a radioactive form of carbon (C14) that begins to decay upon death. C14 decays at a steady, known rate of a half life of 5,730 years. The technique is useful for material up to 50,000 years. Fluctuations of C14 in the atmosphere can affect results so dates are calibrated against dendrochronology. Radiocarbon dates are calibrated to calendar years.
Dates are reported in radiocarbon years or Before Present. Before Present refers to dates before 1950. The introduction of massive amounts of C14, due to atomic bomb and surface testing of atomic weapons, has widely increased the standard deviation on all dates after A.D. 1700 causing these dates to be unreliable.
Accelerated mass spectrometry can more accurately measure C14 with smaller samples and can date materials to 80,000 years.
Scope and Content
Sub sub series contains radiocarbon dates from: Crepeele, Sarah and Graham sites.
Dr. Robert Harvey graduated from Brandon College in 1913 (McMaster Arts). He received a diploma in theology from Brandon College in 1915. Initially a minister in the Presbyterian Church, Dr. Harvey spent the greater part of his life as a minister in the service of the United Church of Canada.
Custodial History
This fonds was accessioned by the McKee Archives in 1998. Prior custodial history is unknown.
Scope and Content
This fonds consists of manuscripts written by Dr. Robert Harvey, various newspaper clippings, primarily from the Brandon Sun, featuring articles written by Harvey. Fonds also contains war-time publications from the Soviet Union, United States of America, and Canada. Topics include: the armistice, biographical accounts of war-time figures, the history of the church in Canada, human rights, communism and fascism.
The Duthie site is the first site identified in the Makotchi-Ded Dontipi locale. It was reported to Dr. Bev Nicholson by Doug Jackson, a local collector who had observed archaeological materials that had been exposed during the construction of Maple Hill Road northwest of Lauder. The site is named after the landowner, Randy Duthie.
The initial inspection of the exposed materials indicated that the eastern half of the site had been severely impacted by raising a road grade using an elevating grader. However, an undetermined amount of the site remained to the west, flanked by a low sand dune. Testing and preliminary excavations were conducted in 1992-93. In 1994 a field school added to the excavated sample. The undisturbed portion of the site, west of Maple Hill Road was situated at the base of a low sand dune and had an aspen and willow forest cover. The water table was approximately one meter below surface at the time of excavation. A rising water table has since prevented further excavations.
Two dates on bone collagen were obtained during excavations. These were 880+/-80 B.P. (Beta 62705) and 970+/-40 B.P. cal. 1030 A.D. (TO 13366). These dates are consistent with an Initial Middle Missouri cultural assignment. The site occupation is identified by the distinctive ceramics found there. Ceramics at the Duthie Site are tool impressed with incising and lip modeling with fabric impressions on most vessels. Jill Taylor analysed the ceramics from the site for a Specialist thesis, Brandon University (1994) and a Masters of Arts degree from the University of Saskatchewan. (Taylor 1995).
Analysis of residue from Duthie site pottery by Matthew Boyd recovered corn (Zea mays) phytoliths and bean (Phaseolus sp.) starch grains indicating consumption of these domesticates at the Duthie site. (Boyd 2006)
The occupation of this site indicates a migration of people from the south who were well acquainted with horticultural farming. These people had previously migrated to South Dakota following river valleys into the central plains from the eastern woodlands during late Hopewell times. It appears that they later migrated well to the north into southern Manitoba but there is no evidence that they remained there for more than a single year.
Boyd, M., C. Surette and B.A. Nicholson. 2006 Archaeobotanical Evidence of Prehistoric Maize (Zea mays) Consumption at the Northern Edge of the Great Plains. Journal of Archaeological Science 33: 1129-1140.
Taylor, J. 1994 An analysis of the ceramics recovered during 1992 and 1993 at the Precontact Duthie Site (DiMe-16). Specialist thesis, Brandon University.
Scope and Content
The Series has been divided into seven sub-series, including (1) Duthie site (2) Jackson site (3) Twin Fawns site (4) Vera site (5) Schuddemat site (6) Bradshaw site (7) Hollow B site.
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 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
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.
Block C was situated in sparse oak forest with an understory of saskatoon, hazelnut and a thick ground cover of poison ivy and sarsaparilla. The block measured 3m and 3m and contained nine excavation units. All units were excavated to 35cm below surface. The soil horizons were much like the other blocks, except for a rusty brown stain in the first level, giving the upper black loam a mottled appearance. The brown patches were clay mixed with loam and were harder than the surrounding matrix. No definitive interpretation of these phenomena was attempted but this effect may be the result of natural brush or forest fires. Under the 5cm so d/humus (Ah) layer, the loam horizon extended approximately 5cm – 25 cm below surface, and averaged 20 cm thick. Bone was concentrated within this horizon between 10 cm – 20 cm below surface.
Block C was notable for its concentrations of articulated bison bone. Most noteworthy was an articulated unit composed of lumbar vertebrae, pelvis, and sacrum. Several thoracic vertebra/proximal rib end concentrations were also recovered. There were more vertebrae and rib sections recovered in the units in proportion to other bones. A few sherds, some debitage and a single Prairie Side-Notched point fragment were among the recoveries. Based on the quantity of bone, the density of the bone layer, and the articulated butchering units the area has been interpreted as a bone midden.
Faunal material was analysed by Jessica MacKenzie for her Honours Thesis: "A reconstruction of butchering processes in Block C from the Lovstrom site DjLx-1 in Southwestern Manitoba."
Radiocarbon date: 850/115BP XU 79.
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 D was wooded with oak and an understory of saskatoon and hazelnut with a thick ground cover of poison ivy and sarsaparilla. Root and rodent disturbance was extensive.
Based on the recoveries from Test Unit 22 during the survey, further excavations were carried out. Two units 87 and 93 were excavated in 1987. A further four units were excavated in 1988. There appears to be a pre contact occupation and a protohistoric feature within the block.
Diagnostic lithics included a chert Plains Side-notch projectile point, and a large Woodland side-notched point. The lithic materials from Block D are primarily local cherts followed in abundance by Knife River Flint and Tongue River Silicified Sediment – both of which are exotics imported from the southwest. Faunal remains were primarily bison.
Thin-walled obliterated fabric impressed pottery with grit temper was recovered in all units. Diagnostic ceramics included two rims, one with a fabric impressed exterior and the lip notched with dowel impressions, and a second thick walled rim was fabric impressed to the lip. The ceramic wares appear to be essentially a Woodland complex with overtones of Plains influence.
RC date: 230/90 BP.
Scope and Content
Sub-series has been divided into sub sub series including: Lovstrom Block D 1987 and Lovstrom Block D 1988.
