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.
9.46 m textual records; 1919 photographs & graphics
History / Biographical
Brandon, Manitoba was incorporated as a city in 1881. In 1882, led by Charles Whitehead and a small Board of Directors that included J.W. Vantassel, Charles Pilling, George Halse, J.E. Smith, William Johnson, R.T. Evans, and Thomas Lockhart, it was decided to hold an agricultural exhibition. These men were all involved in the farm business in one way or another, and they wanted an opportunity to help residents realize the agricultural potential of the region. In October of that year, the fledgling community held its first agricultural exhibition . The fair was held in downtown Brandon at what was known as “Market Square.” Market Square was two acres of land located on Princess Avenue between Eighth and Ninth Streets. Due to poor weather, and the fact that not many people were ready to show animals and grain, there was a relatively small turnout. The following year was much improved. There were 730 entries into the exhibition. By 1884, the Board of Directors of the Brandon Agricultural Society, which was in charge of the exhibition, realized that they were in poor financial shape, to the point of being personally out of pocket. It was realized that October was not the best time for farmers to be leaving their farms to go to an exhibition. In 1888, it was decided to move the exhibition to the summer time, when it was much easier for people to attend.
The first Brandon Summer Fair was held in July 1889, and it was a resounding success. The Board of Directors had added many items of interest to appeal to the entire public, not just agricultural people. In 1892, the Western Agricultural and Arts Association (WAAA) was formally established to take over duties from the Brandon Agricultural Society. However, it was not until 1897 that the WAAA held its first meeting. There is no explanation as to why there is a five year gap between the formation and the first meeting of this organization. 1897 was the turning point of the Brandon Exhibition. The fair was now firmly established in Brandon, and the Board of Directors was instrumental in ensuring that it remained so. This was done by petitioning to both the municipal and provincial governments for grant money. As well, the Board booked midway and grandstand acts that would bring the city dwellers to the agricultural exhibition.
There were also early attempts at holding an agricultural exhibition in the winter. The first such attempt was in 1884. There was also a Spring Stallion show held in 1891. By 1904, however, a petition by J.D. McGregor had gone out to formally establish a winter exhibition. This effort also failed, but by 1906, it was decided by businessmen, politicians, and farm representatives in Brandon, including McGregor, to organize a winter fair. Rather than seeing this new fair as competition, the Board of Directors of the summer fair felt that it would complement their exhibition. The new fair would remain primarily agricultural. The first winter fair was held in 1906. While the two fairs were not amalgamated, they did share the same secretary-manager. The secretary-manager was responsible for the day to day management of the fair, as well as keeping track of meetings and decisions reached by the various fair boards and committees. In 1907, the Brandon Winter Fair and Livestock Association (BWFLA) was formed to act primarily as a land-holding joint stock company. The following year the Provincial Winter Fair and Fat Stock Association (PWFFSA), an entirely separate organization from the BWFLA, was formed to manage the activities of the winter fair. The PWFFSA name was soon changed to the Manitoba Winter Fair and Fat Stock Association (MWFFSA).
By 1906, Brandon could boast two full size exhibitions, one in the summer and one in the late winter, both of which were considered to be premiere events. In 1908, the Brandon summer fair was renamed the Inter-Provincial Exhibition, and in 1912 it held it’s first Traveller’s Day, an event which would soon become an important addition to the fair and is still in existence today. It is thought that the name “Traveller’s Day” came from the fact that it was held on a Saturday, a day when many people could travel to Brandon for the exhibition.
In 1913, Brandon was bestowed with the honour of hosting the Dominion Exhibition. This was a national exhibition sponsored by the federal government. It was held in a different city every year. There were several cities vying for the 1913 Dominion Exhibition, but it was Brandon that impressed the sponsors the most. With the government funds received for this honour, the Board of Directors supervised the building of a new grandstand, display buildings, and racetrack, as well as the general expansion and improvements to the fairgrounds.
In the spring of 1912, it was decided by the Board of Directors of the winter fair that the facilities they were currently housed in were inadequate for their needs. The mayor and city clerk of Brandon went to the provincial legislature in order to request that there be an amendment added to the Brandon city charter. This amendment would allow the city to guarantee bonds issued by the winter fair board to help pay for the construction of a new facility. This request was granted, and a $70 000 addition was built next to the original winter fair building. The new building was opened in 1913.
Throughout the First World War, both the winter fair and Provincial Exhibition buildings were used for the war effort. There was one distinct difference however. The summer fair Board was able to negotiate a deal with the army that enabled it to reclaim the fair buildings during fair week. The winter fair, however, had to give up the idea of holding fairs in 1915 and 1916. It was not until 1917, that the winter fair was able to resume.
During this time, due to the financial problems that had beset the winter fair, the two exhibitions considered amalgamation. The Board of Directors of the winter fair felt that because they were the smaller of the two fairs, their interests would be swallowed up by the summer fair. The winter fair withdrew from the negotiations to amalgamate. With this rather sudden turn of events, the Board of Directors of the summer fair petitioned the government to be allowed to incorporate. This was granted, and in 1920, the WAAA was incorporated as the Provincial Exhibition of Manitoba. From 1920, the summer fair was officially known as the Provincial Exhibition of Manitoba. This was the first time that the summer fair was incorporated, and received the “status and financial assistance” that came with incorporation.
More problems beset the winter fair in the 1920s. In 1920, a fire burned down the winter fair pavilion, located at the south end of the winter fair buildings, and caused the Board to cancel the 1921 winter fair. It was not until 1922, that a new building was completed. By 1929, both fairs were well regarded throughout Canada. In 1929, a decade long Depression hit the west. While many fairs closed during this time, Brandon struggled to keep its open. The Directors of both fairs felt that the agricultural shows “encouraged excellence at a time when faith and enthusiasm were at a low ebb.” The summer fair proved to be quite successful during the Depression, likely as a result of the few moments one was able to forget one’s troubles while there. The winter fair was not quite as successful, although both fairs received government grants and work relief projects. There was little new entertainment in these exhibitions.
There were changes about to manifest themselves at the summer fair, however. While the winter fair had representatives from various associations on its Board of Directors, the summer fair Board of Directors was a small close-knit group of men. Citizens saw entry into this elite group as elusive and difficult. To ward off the possibility of the Board becoming a “self-sustaining clique,” that only chose Directors from within, it was decided by several citizens to try and elect some new blood into the fair Board. In 1933, there was a general election for the Board. Instead of the usual men shuffling positions, there were forty-four nominations for the twenty positions. When the voting was all over, seven new men sat on the Board. Despite some inner rumblings, especially on the summer fair Board over the next few years, both exhibitions survived the Depression.
During the Second World War the fairs once again were forced to operate under adversity. Once again, the buildings were requisitioned for the army, although they were released during fair week. The summer fair was forced to make several concessions, and the winter fair was relocated to the summer fair grounds for the duration.
The winter fair did not survive the Second World War intact. Due to financial reasons, in December of 1945, the Board of Directors turned the winter fair buildings over to the City of Brandon. By 1946, the BWFLA, which was the joint-stock land holding company, had ceased operations because the city now controlled the winter fair land and buildings.
The next fifteen years would be a time of rebuilding for both of Brandon’s exhibitions. Children especially were more active participants in the agricultural exhibitions. The summer fair continued to diversify and look for new ways of entertaining the public at large. The winter fair remained primarily agricultural. By the end of the 1950s the winter fair, which was used to struggling, was now both successful and stable; and the summer fair, a perennial success, was starting to fade.
By 1969, both the winter and summer fair Boards had realized that amalgamation was the best possible decision, both practically and financially, for the future of the two fairs. On 29 October, 1969, the two exhibitions amalgamated to become the Manitoba Exhibition Association. The reconstituted Provincial Exhibition of Manitoba was now responsible for both the winter and summer fairs. A new building was erected on the summer fair grounds to house both of the exhibitions. On 2 April 1973, the Keystone Centre was officially opened at the winter fair, although it had been in use since October of the preceding year.
In 1970, Manitoba’s Centennial, it was decided that an organization in Manitoba would receive the title of “Royal,” as a way to celebrate the centennial. Although many organizations applied for the honour, it was the Brandon winter fair that received the accolades. The winter fair was bestowed with the title “Royal”, and became known as the Royal Manitoba Winter Fair.
In 1975, a third exhibition was added, this time a purely agricultural fall show known as the Agricultural Exhibition, or AgEx. This fair was partly organized on behalf of the cattle growers, who found that the summer and winter fairs did not give them adequate time and space to properly show their cattle. The return to a fall show, which had not existed since 1888, would be the return to a purely agricultural exhibition. This show was to be primarily a show and sale event. On 3 November 1975, the first AgEx was opened to resounding success.
The Provincial Exhibition of Manitoba, the Royal Manitoba Winter Fair and AgEx are all still in existence in Brandon. They are regarded as three of the most important events to take place annually in the city.
Custodial History
These files were housed with the Manitoba Exhibition Association until c1986 when they were transferred to the S.J. McKee Archives at Brandon University.
Scope and Content
The fonds consists of textual records and photographs comprised of the records from the three annual exhibitions that are held in Brandon, Manitoba: the Provincial Exhibition of Manitoba, the Royal Manitoba Winter Fair, and the Agricultural Exhibition (Ag-Ex). The textual records include prize lists, programs, minutes, financial, administrative files, original results, scrapbooks, tickets, news releases, contracts, by laws, documents as well as a miscellaneous section. There are approximately 1846 photographs that include scenes from these three exhibitions. These records provide a unique perspective on the development of agriculture and rural life in southwestern Manitoba. Fairs such as these have been and remain prime media of farm improvement, technological and scientific advancement in rural Canada, and the promoters of country living. These fairs also reflected the long tradition inherited from Britain and Europe of country fairs as centers of entertainment, social interchange and diversion. These records are a principal source of information about the most broadly based vocational, entertainment and social events held on an annual basis in southwestern Manitoba over the last century. The records are vital to academic research on agriculture or fairs, individual biography, or community history.
Notes
The RG 2 Provincial Exhibition of Manitoba Association finding aid was created by Karyn (Riedel) Taylor with the exception of Series 9 and the accompanying database, which were created by Donica Belisle. This finding aid was created in August 1999.
Researchers are responsible for observing Canadian copyright restrictions.
Finding Aid
Available
Storage Location
RG 2 Provincial Exhibition of Manitoba Association fonds
Storage Range
RG 2 Provincial Exhibition of Manitoba Association fonds
Related Material
Additional records regarding the Provincial Exhibition of Manitoba, the Royal Manitoba Winter Fair, and AgEx are housed at the Provincial Exhibition of Manitoba Association offices. To gain access to these records, it is necessary to contact the general manager of the Provincial Exhibition of Manitoba Association.
Arrangement
The fonds is divided into sous-fonds by exhibition. There is a Provincial Exhibition sous-fonds, a Royal Manitoba Winter Fair sous-fonds, an Ag-Ex sous-fonds, and a Miscellaneous sous-fonds that holds information that could not be easily broken down into one exhibition. The arrangement is as follows:
RG 2 Provincial Exhibition Association of Manitoba fonds
RG2SF1 Provincial Exhibition of Manitoba
1.1 Documents
1.2 Minutes
1.3 Financial Records
1.4 Administrative Files
1.5 Prize Lists and Programs
1.6 News Releases
1.7 Original Results
1.8 Tickets
1.9 Photographs
1.10 Scrapbooks
1.11 Miscellaneous
RG2SF2 Royal Manitoba Winter Fair
2.1 Documents
2.2 Minutes
2.3 Financial Records
2.4 Administrative Files
2.5 Prize Lists and Programs
2.6 News Releases
2.7 Original Results
2.8 Tickets
2.9 Photographs
2.10 Scrapbooks
2.11 Miscellaneous
RG2SF3 AgEx
3.4 Administrative Files
3.5 Prize Lists and Programs
3.6 News Releases
3.7 Original Results
3.9 Photographs
RG2SF4 Miscellaneous
4.1 Documents
4.2 Minutes
4.3 Financial Records
4.4 Administrative Files
4.9 Photographs
4.10 Scrapbooks
4.11 Miscellaneous
Some of the pages and photographs in the scrapbooks have become loose
History / Biographical
Southwest B "Region" Women's Institute is a regional board within Manitoba Women's Institute.
According to their website, Manitoba Women’s Institute (MWI) operates under an umbrella structure of a provincial board and regional boards as directed in the Constitution and Bylaws. The provincial board serves to co-ordinate the activities of the organization on a provincial scale and link with other provincial, national, and international organizations. Regional boards are responsible for activities within their regions and for assisting with communication between the provincial board and the membership. Local institutes serve members in local communities or local geographic areas.
The Southwest B "Region" Women's Institute covers the area south of the Trans Canada Highway and from Killarney west to the Saskatchewan border. Historically it has encompassed locals from the follwing areas: Bardal, Boissevain, Broomhill, Dand, Deloraine, Dublin, Ebor, Elgin, Elva, Hartney, Kemnay, Lauder, Lyleton, Medora, Melita, Napinka, Pierson, Regent, Souris, Springvale, Tilston, Wakada and Whitewater.
Custodial History
Records were in the possession of the Southwest B Region Women's Institute until thier donation to the McKee Archives in 2014.
Scope and Content
Fonds consists of records created by the Southwest B Region Women's Institute during the course of their activities and operations.
Records include: eight minute books (1926-1997); a small scribbler listing Convention and some Board meeting attendance (2001-2013); and two Treasurer's/cash record books (1940-1944 and 1951-1992). The photographs are portraits of the Women's Institute Leadership Class (1961 and 1962), attendees on stage at the F.W.E.C Convention, Wolfville NS (July 1964) and the Manitoba delegation to Wolfville NS (July 1964).
Notes
History/Bio information was taken from the records and from the Manitoba Women's Instutite webpage (http://www.mbwi.ca/about-mwi/local-institutes/. Accessed January 2017). Description by Christy Henry.
Finding Aid
A detailed list of meeting dates for the minute books was provided by the donor. It is located in the donation file.
Storage Location
2016 accessions
photographs in RG 5 photograph drawer by accession number
Edith Mary Laycock was born on June 25, 1913. She attended Brandon Collegiate from 1929 until her graduation in 1931. Ms. Laycock attended Brandon College from 1931-1934, graduating with a Bachelor of Arts degree. In 1935, she attended the Wheat City Business College and graduated from the Stenographic Course. Ms. Laycock was employed by the Canadian Pacific Railway as a stenographer for many years and belonged to the Canadian Pacific Expressmen's Mutual Benefit Society from 1939.
Edith Laycock was very interested in drama. While attending Brandon Collegiate and Brandon College she participated in school and college plays. She was involved in drama and theatre throughout her aadult life. Edith Laycock directed many of Brandon College's major productions beginning in 1950. She was also the director of many of the plays put on by the Brandon Little Theatre from 1950. Ms. Laycock also performed in the Little Theatre productions when she was not directing.
Ms. Laycock was also involved in many other elements of Brandon life. She served alternatively as the vice-president, secretary, treasurer, and production manager of the Little Theatre throughout the 1940's and 1950's. She was the Social Manager for the Brandon Festival Committee in 1948, the Publicity Chairperson for the Brandon Music Festival Association in the 1950's, and the Secretary of the Brandon Overture Concert Association. Laycock also wrote play reviews for the Brandon Sun in the 1950's. She was the director of the Manitoba Delta Chapter of Beta Sigma Phi. In the 1960's Laycock was a member of the Brandon Council of Women and Chairperson of its Arts and Letters Committee. She was also the Vice-President of the Brandon Art Club in 1960. Edith Laycock also held a 12-week class in creative dramatics for children at the Allied Arts Centre in the early 1960's.
Edith Laycock died in Brandon on December 17, 1987.
Custodial History
This fonds was accessioned by the McKee Archives in 1998. Prior custodial history is unknown.
Scope and Content
This fonds consists of memorabilia kept by Edith Laycock. A large part of the collection consists of programs from plays that Laycock performed in or directed during the 1950's and 1960's. There are also numerous newspaper clippings about Laycock's plays including reviews, pictures, and advertisements. This collection also includes a folder of programs from the Brandon Little Theatre productions in the 1950's, as well as clippings about the Little Theatre. There are also numerous articles about miscellaneous drama and art events throughout Brandon, Manitoba, and Canada. The fonds also includes Laycock's daybook from 1962, and travel notes from Laycock's 1952 trip to Great Britain and Europe. The latter contains a passenger list for the Empress of Scotland, August 5, 1952. The collection further includes Canadian Pacific Railway passes dating from 1947-1963 and a copy of the Canadian Pacific Pension Plan. Fonds also contains material from the various organizations that Laycock was involved with including the Brandon Council of Women and Beta Sigma Phi. Fonds includes 12 photos that appear to be family photos from Laycock's childhood. Finally, the fonds contains various copies of plays that Laycock performed in or directed.
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.
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 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.
This site is situated in a naturally sheltered area with a low rise to the east and south partly encircling a flat area open to the west. Present natural vegetation is an open oak forest with a light understory of saskatoon, hazelnut, poison ivy and sarsaparilla. It is situated on the till plain at the upper end of a ravine leading to Jock’s Creek.
Two test units six meters apart were excavated in 1987 and produced cultural materials which warranted a block excavation, so seven contiguous 1m2 units were then opened. These units proved to be very productive of cultural remains. Subsequent excavations in 1988 increased the number of excavated units to 21. In 1991 a further eight units were excavated for a total of 29 excavations and two test units. Excavations went deeper in this block than in Blocks C or B. Remains from the block included bison bone, bone tools, fire-cracked rock, ceramics, lithics including tools and debitage and a hearth. Another occupation was recovered in 1991 containing a hearth and living floor.
Radiocarbon samples have produced two distinct sets of radiocarbon dates from 1987 and 1988 excavations. There appears to be two or possibly three cultural horizons definable within this block.
An upper cultural horizon, located between 14-21 cm below surface, contains large bison bone and fire-cracked rock dating to 465/100B.P from XU 128.
A lower horizon in the 20-25 cm level contained FCR, bison bone and lithic scatter that was dated to 675/70 B.P. from XU 122 and 715/110 from XU 114.
Scope and Content
Sub-series has been divided into sub sub series including: Lovstrom Block E 1987, Lovstrom Block E 1988 and Lovstrom Block E 1991.
In 1988 four 1m2 units were excavated in this Block F. The forest cover is identical to that of Block E, with an open oak forest with a light understory of saskatoon, hazelnut, poison ivy and sarsaparilla.
Underneath the litter mat (Ah) is a shallow, 15-20 cm “A” horizon of dark grey/brown silty loam with a high representation of pebble size clasts. The glacial clays, encountered at 20 cm below surface, consist of a matrix of light tan sandy clays containing rounded pebble to cobble size rocks.
The recoveries from this block consisted of a few ceramics, including Vickers Focus rim sherds, four lithic tools and a number of small bison bone fragments. There was no discernible cultural stratigraphy in the four 1m2 units and the limited deposits of bone, ceramics and lithics were dispersed randomly throughout the 25 cm of cultural matrix. The lithic materials frequencies were similar to those in Block E with local cherts and KRF being the most abundant categories. A small amount of fire-cracked rock and a few large identifiable bison bones were recovered – all distributed randomly with little evidence for any pattern of clustering.
No RC dates.
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.
In 1988 four units were excavated in Block G. The vegetation is similar to other areas in the locale with an open oak forest with a light understory of saskatoon, hazelnut, poison ivy and sarsaparilla.
Excavations recovered artifacts between 0 cm – 15 cm b.s. The cultural deposits are very shallow and it is quite possible that what appears to be a single occupation may in fact represent multiple occupation compressed deposits as a result of deflation or the lack of sedimentation in this raised area. This latter view is supported by the ceramics which appear to be a mixture of Blackduck and Vickers Focus wares.
The frequency and distribution of cultural material from block G contrasts with that of other sites in the locale. While the diagnostic materials are similar, the nature of the background debris and the associated lithic assemblage suggests that this area was utilized for a different set of activities.
Unlike Blocks E and H, there is very little in the way of ceramics, fire-cracked rock or bison bone, yet a significant amount of lithic debitage and six Plains/Prairie Side-notched projectile points were recovered. No unifaces or scrapers were recovered. This may be an area where activities such as manufacture and hafting of projectile points; hunting activities, butchering and refuse disposal took place.
No RC 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.
The vegetation in block H is similar to other areas in the locale with an open oak forest with a light understory of saskatoon, hazelnut, poison ivy and sarsaparilla.
The excavations of the eight 1m2 units in 1988 resulted in the recovery of over 650 ceramic fragments including 20 rim sherds from at least four vessels, a grooved maul, fire-cracked rock, lithic debitage and a reworked Avonlea projectile point. A large amount of bison bone, including a number of axial elements and a fragmented skull were also recovered.
Based on the 1988 recoveries at the site further excavations took place in 1991. Nine excavation units were opened next to the previous excavations. Another 250 ceramic sherds were recovered in 1991. Nine vessels have been identified based on rim sherds. Vickers Focus and Woodland vessels have been identified and two vessels similar to Scattered Village Complex were recovered.
The lithic material assemblage is intermediate between Blocks G and E with KRF being the most frequent material category followed by local cherts.
Two features, a hearth and a curvilinear arrangement of rock were recovered. The high numbers of ceramic fragments suggests a habitation area, rather than hunting or butchering behavior. However, the separation of occupations at the site is difficult to establish and there may be different uses of the site by successive occupations.
Radiocarbon dates from this block indicate two occupations separated in time by some 300 years. XU 181 – 405/110 BP and XU 184 – 780/110 BP.
Scope and Content
Sub-series has been divided into sub sub series including: Lovstrom Block H 1988 and Lovstrom Block H 1991.
The Sarah site was chosen for excavation based on the results of the Casselman survey. The survey recovered significant amounts of faunal remains, some ceramics and lithics from the test pits. Excavations took place in 2003 at Crepeele West (Units 1-5) and Crepeele East (Units 6-9). The site was subsequently renamed the Sarah site DiMe-28. In 2004 another 9 units were excavated (Units 10-18).
Based on the recoveries it was determined that the Sarah site is a stratified site with woodland ceramics in the upper occupation and late woodland points in both of the upper occupations. These upper occupations produced abundant bison bone including foetal bone. The lower occupations produced less bone and no foetal bone, although absence of foetal bone in the lower occupations does not necessarily indicate a warm season occupation. This could be due to sample error or perthotaxic factors such as scavenging of the fragile bone by dogs or other carnivores.
The dates from the Sarah site include 550+/-40 B.P.; 1430+/-80 B.P; 2810+/-80 B.P.; 3120+/-130 B.P. The lower occupations did not yield any diagnostic materials although debitage was abundant. These occupations were most productive at the edge of the large sand dune at the southern edge of the excavations. It is assumed that the major portion of these occupations have been overridden by the dune in the past 3000 years. Heavy earthmoving equipment would be required to remove this overburden which limits the possibility of future excavation.
Environment
The Sarah site is a large area located at the eastern end of the Crepeele locale. Ground cover is a mosaic of aspen poplar groves and patches of mesic grass prairie. Excavation profiles indicate that this has been the situation since early precontact times, although as local climatic conditions change (primarily rainfall), the relative size of these areas and where they may have occurred also changed. The soil is aeolian sand sheet derived from delta outwash deposits along the western edge of glacial Lake Hind. The present topography is a variable dune landscape reworked by aeolian activity that creates a mosaic of microhabitats. These include forested patches in the lee of sand dunes with grassland on the southern and western exposures and small damp lowlands that support balsam poplar, willows, red osier dogwood, high-bush cranberry and water birch. There is no permanent water source in the area although a small seasonal stream meanders through a damp lowland to the east of the Sarah site.
Scope and Content
Sub-series has been divided into sub sub series including: Sarah 2003 and Sarah 2004,
The Graham site is a located adjacent to the Crepeele site towards the western end of the Crepeele locale. The Graham site was initially designated as a separate site early in the testing of the Crepeele locale due to what appeared to be a distinction between Early and Late Woodland ceramics. Subsequent testing has shown that this distinction was premature and that the cultural mosaic represented in the western section of the Crepeele locale may not readily separate in this manner. However, due to the records management that was already in place, the original separate designations have been retained.
Environment
Ground cover is a mosaic of aspen poplar groves and patches of mesic grass prairie. Excavation profiles indicate that this has been the situation since early precontact times, although as local climatic conditions change (primarily rainfall), the relative size of these areas and where they may have occurred also changed. The soil is aeolian sand sheet derived from delta outwash deposits along the western edge of glacial Lake Hind. The present topography is a variable dune landscape reworked by aeolian activity that creates a mosaic of microhabitats. These include forested patches in the lee of sand dunes grassland on the southern and western exposures and small damp lowlands that support balsam poplar, willows, red osier dogwood, high-bush cranberry and water birch. There is no permanent water source in the area although a small seasonal stream meanders through a damp lowland along the eastern margin of the Crepeele locale.
Excavations at the Graham site took place from 2004 to 2008. Analyses of the recoveries shows that, with two exceptions, all of the occupations that have been tested produced bison foetal bone. The presence of foetal bison is a strong indicator of wintering occupations...The absence of foetal in some area does not necessarily indicate warm season occupations since these excavation series are small and the absence could be due to sample error or perthotaxic factors, such as scavenging of the fragile bone by dogs or other carnivores.
From this evidence the Graham site has been interpreted as being primarily a wintering area. This is consistent with the lack of surface water (snow would serve as a substitute in winter) and the abundance of wood for fuel – a critical requirement for winter occupation. Cultural occupations date from Mortlach circa 250 B.P to woodland circa 580 B.P.
Scope and Content
Sub-series has been divided into sub sub series including: Graham 2004, Graham 2005, Graham 2006 and Graham 2008
This record group was artifically created in January 2007 by Tom Mitchell and Christy Henry of the McKee Archives.
Scope and Content
The record group consists of various fonds and collections concerned with the political, cultural, social, and educational life of western Manitoba. See the Subject Access field for a list of titles.
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
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.
