Benjamin J. Hales was born in Peterborough, Ontario on November 24, 1868. Hales lived in Peterborough until attending the University of Toronto, where he graduated in 1894. In 1897, Hales travelled west to teach at Broadview, North West Territories. He moved to McGregor, Manitoba in 1899, where he was Principal of the school, and in 1902, he moved to Hartney, Manitoba. Between 1907 and 1911, Hales devoted his time to working for the provincial Normal School that offered courses for prospective teachers in Portage La Prairie, Manitou, and Brandon. In 1911, the normal courses were established in Brandon and Hales moved to Brandon, where he resided for the rest of his life. Hales acted as the Principal of the Brandon Normal School from 1912 until his retirement in 1938. B.J. Hales married Elizabeth Lewis of Peterborough, who died in 1942. The couple had one daughter Marion Hales Doig. B.J. Hales was a well-known naturalist and author of several texts dealing with prairie flora and fauna. Hales also built a museum of Manitoban flora and fauna in the Normal School. Hales was an alderman on Brandon City Council from 1920 to 1923, and served as the chairman of the city's Parks Board from 1937 until his death in 1945. Hales was twice the president of the Western Manitoba Teacher's Association, and once the head of the Manitoba Educational Association. B.J. Hales was also a member of the First United Church and served on its board. He died on December 23, 1945 at his home in Brandon.
Custodial History
This fonds was accessioned by the McKee Archives in 1998. Previous custodial history is unknown.
Scope and Content
Fonds includes three books written by B.J. Hales, titled, "Selected Western Flora: Manitoba, Saskatchewan, Alberta"(1925); "Prairie Birds"(1927); and "Forests and Trees"(1925), all published in Toronto by The MacMillan Company of Canada. The fonds also includes two books of field notes concerning specimens held in the Brandon Normal School Museum, as well as a list of birds in the Atkinson Collection also located at the Brandon Normal School Museum.
The Canadian Union of Public Employees came into existence in September 1963, during a convention in Winnipeg when The National Union of Public Employees and the National Union of Public Service Employees merged. In 1964, the Manitoba Division of CUPE (now CUPE Manitoba) held its founding convention in The Pas. At that time, there were 12 affiliated local unions and a total membership of 1,300. The Canadian Union of Public Employees is Canada's largest union. Public service employees formed CUPE to protect their rights, to negotiate wages and working conditions, and to achieve dignity in the workplace.
Custodial History
Fonds was in the possesssion of the Brandon CUPE Office until its donation to the S.J. McKee Archives in 1995.
Scope and Content
Fonds contains general administrative files of the CUPE including agreements, newspaper clippings, correspondence, and convention records. In addition, fonds includes records for many CUPE locals in southwestern and north-central Manitoba. These includes files for each local containing agreements, lists of officials, correspondence and financial records. An extensive body of records dating from 1956 exists for CUPE local #69. This local began its existence as the Brandon Civic Employees Federal Union formed in April 1919.
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.
C. J. Barnes was born in Brandon, Manitoba in February 1884. His parents were native Nova Scotians who arrived in Brandon in the early 1880s. In 1884, the family settled on a homestead near the present town of Lauder. This homestead was sold in 1899, and the family moved to farm in the district of Medora. C. J. Barnes took over the operation of this farm in the early 1900s. He farmed until 1924. Barnes was educated in schools in the Truro School District and the village of Lauder. He was active in the original Territorial Grain Growers' Association.
Custodial History
This fonds was accessioned by the McKee archives in 1997. Prior custodial history is unknown.
Scope and Content
Fonds contains a pamphlet written and published by C.J. Barnes titled Seventy Years in Southwestern Manitoba. The pamphlet contains an account of life in rural southwestern Manitoba from the 1880s through to the 1940s. The pamphlet is based on a variety of sources including diaries written by Mr. Barnes' father. Fonds also includes some hand-drawn maps not included in the published version of the pamphlet, as well as four letters c.1962, between C.J. Barnes and Rev. Robert Harvey in his capacity as a columnist for the Brandon Sun.
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.
Cover of Young School minute book is moderately damaged, but pages are in good condition with only minor water damage and a few ripped pages.
History / Biographical
Dorothy Cox (nee Frost) moved from Elm Creek to Justice in 1946 to work as a schoolteacher. In 1948, she married Laval Cox and together they had four children: Larry, Herd, Rosalie and Heather.
In 1949, Dorothy and Laval purchased Gibb Gillespie's PSV business and began hauling grain, cattle and agricultural equipment. Dorothy went back to teaching in 1959, first at Justice and then Elton Collegiate. After retiring from teaching in 1978, Dorothy started a greenhouse, which operated for 21 years.
All six members of the Cox family were active in community events and organizations. Dorothy was involved in establishing the baby band in 1951; her sons Larry and Herb were members. Along with Laval, Dorothy was a leader of the Cubs in 1955-1956 and again in 1958-1959. Laval was the leader of the local hockey club in 1958, and of a bible study group in 1960. Larry, Herb and Rosalie were avid skaters in 1960-64. Heather and Rosalie were enrolled in senior grades of Sunday school in 1970.
Custodial History
Records were collected by Dorothy Cox, a resident of Justice, over a number of years. She donated them to the McKee Archives on April 4, 2012.
Scope and Content
Collection consists of records related to the history of the Justice district. It includes a history of the Justice Church (1910-1970); minute and expense books for the Justice Hockey Club (1949-1966); a minute and expense book for Young Protestant School (1884-1898); a copy of the Justice 100th Anniversary community history (2009); and four color photographs of Justice Church.
Notes
History/Bio information taken from the content of the collection. Description by James Heaman (2012).
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
Gerry Beaubier was born in Wainwright, Alberta to Beatty and Babe Beaubier. He completed his high school in Saskatoon, before receiving a BSc in Geography from Brandon University.
Before attending university Gerry served in the army as a special reserve, while working as a night clerk at the Bessbourough Hotel in Saskatoon. His post-graduate career consisted primarily of work for Canada Agriculture, under the PFRA Branch (Prairie Farm Rehabilitation Administration). Later he would work as an Executive Manager, helping develop forage and range management programs for several post secondary schools, including, Assiniboine Community College, as well as schools in Red Deer, Lethbridge, and Saskatoon.
Gerry Beaubier married Joyce Abercrombie, of Saskatoon. Together they had two sons: Neil and Dean. Neil, an Account Advisor for the Royal Bank, was born in Regina, and currently works in Swift Current. Dean was born in Swift Current, received his PhD in Education and currently lives in Forrest working at Elton Collegiate.
The Beaubiers, who were originally from Ireland, emigrated to the Canadian West, making Gerry part of the fourth generation of his family to call the region home. His great-grandfather, along with his grandfather and great uncle were amongst the first one hundred settlers in Brandon. Together they first built the Beaubier House, a boarding house for early settlers and travellers. After it burnt down they began construction on the Beaubier Hotel, which stood at the corner of 8th Street and Princess Avenue in Brandon until August 17th, 2008. His grandfather, David Wilson Beaubier, continued to build and operate hotels throughout the prairies, including the Empire Hotels (of Brandon and Saskatoon) and The Park (Moose Jaw).
David Wilson Beaubier served as a secretary of the Orange Lodge of Manitoba. As an Orange Lodge Colonel, he worked with other Orange Lodge members, to recruit throughout the prairies for the purpose of World War One. For his efforts , David was promoted to Leftenant Colonel, and later Captain of the 99th Manitoba Rangers. David's sons (Gerry’s father, at University of Manitoba, and uncle at McGill), were both working towards undergraduate degrees when war broke out in 1914, and each would leave school to join their father at Camp Hughes.
Custodial History
Gerry Beaubier collected these photos primarily in the years 2000-2011, largely
from family and friends who knew of his interest in the topic. They were donated to the S.J. Mckee Archives in 2011.
Scope and Content
Collection consists of digital photographs of those who trained for battle in World War I at Camp Hughes and in Brandon, Manitoba. It also includes a digital copy of the cover of the Nominal Roll of Officers, Non-Commissioned Officers and Men, who departed from Brandon in 1917.
The photos, taken primarily at Camp Hughes, are of a number of battalions, including the 34th, 100th, 108th, 181st and 214th. The photo, PT in England, is a postcard sent home from Beaty Beaubier. The Massey Harris building seen on the right side of, WW1 B parade0001, was used to house troops throughout the war. The man standing alone at the front of the parade in, 181 Parade, is David Wilson Beaubier.
Notes
Information for the biographical and custodial histories was provided by Gerry Beaubier on September 25, 2013. Description by Dustin Lane (October 2013).
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
Joseph Henry Hughes was born in London, Ontario on April 14, 1857, son of Joseph C. Hughes and Jane McAndless. His family farmed in Middlesex County until they retired to Brandon, MB. Huges received his education in Middlesex County then went on to attend the Toronto Normal School in 1874. He tuaght for only a short time in 1875 before going into business as a general merchant in Iderton, Ontario.
Hughes moved to Brandon, MB in 1882 and from 1882 to 1906 was engaged in the lumber business with yards in Rat Portage and Brandon and later with mils on Rainy River. His buisness partner was T.H. Patrick from 1882-1896. T.T. Atkinson was a partner in the business from 1882 until early 1888, running the company's lumber camp in the Rainy River Valley. Atkinson was replaced by a Mr. Kennedy in 1888. After disposing of the mills in 1901, Hughes & Company operated as a lumber dealer until 1908 when the lumber business was sold to Rat Portage Lumber Co., whose operations in Brandon were located on 10th Street between Rosser and Princess Avenues.
Thereafter, Hughes & Company focused on real estate, owning most of the property between 10th and 11th Streets, Rosser and Princess Avenues. The company built rental property and residences in Brandon, including the Strathcona Block on 10th Street and Hughes (Lorne) Terrace on Lorne Avenue. During this period Hughes & Company was also involved in insurance and farming, buying farmland in south eastern Saskatchewan and Manitoba for lease and sale.
Hughes was a city alderman for four years, dedicating himself mostly towards improvements to the city pertaining to electrical generation, water supply and the development of the streetcar franchise. In 1911, he resigned from City Council to stand as a successful candidate for mayor. He held this position for only one year, 1913-1914. During this period Hughes, along with other prominent citizens, set up the Patriotic Fund to help look after the dependents of those going off to fight in World War I. Hughes served as chairman of the project until his death in late 1917.
In addition to his role as a prominent city businessman, Hughes was also deeply involved in the First Methodist Church, and a member of the Independent Order of OddFellows (I.O.O.F.) and the Masonic Lodge.
Joseph Henry Hughes was survived by his wife Anna Maria Hughes, whom he married in 1993, and their daughters: Alma and May (Mrs. Wilfred C. Hughes and Mrs. Charles Leemnnis) and Ruth, and their sons Percy and Harley.
Upon J.H. Hughes' death in 1917, management of the company was taken over by Willard C. Hughes, who died in 1964. Following his death the company was administered on behalf of Alma Hughes by Barry Hughes, a Winnipeg lawyer and distant relative. The company remained active in real estate and property managment, as well as farming and oil, until the early 1990s when following the death of Alma Hughes and her daughter Anna, the company was liquidated.
Custodial History
The records in the Joseph H. Hughes fonds were held in two locations prior to their donation to the McKee Archives. Family related records, including paintings by Anna Hughes, music scores, photographs and various parchments, were stored at the family residence, Lorne Terrace (133-137 Lorne Avenue Brandon, MB). The balance of the records, being the records of Hughes & Co. as the firm came to be known, were stored on the fourth floor of the Alexander Block, also known as the Hughes Block, on the west side of 10th Street just south of Princess Avenue. In the early 1990s a decision was taken by Barry Hughes, who had succeeded Willard Hughes as the President of the company, to sell Hughes & Co. Hughes directed Joe Perry, the Brandon manager of Hughes & Co. to donate the records of the Hughes family and Hughes & Co. to Brandon Univeristy. Perry supervised the transfer of the records from Lorne Terrace and the Alexander Block to Brandon University. Initially the records were located in the Physical Plant H-Hut, they were then transfered to the Brandon University Steam Plant. The family records were transfered to the Archives in 1997, while the company records remained in the Steam Plant until January 2007 when some of the records were transfered to the Archives. The remaineder of the records were moved to a storage facility on 20th Street.
Scope and Content
The Joseph H. Hughes collection is divided into three series, including: (1) Photographs; (2) Edwardian music sheets; and (3) Hughes & Co. business records.
Notes
CAIN No. 202617. The Brandon Sun, August 6th, 1917 contains a report on the death of J.H. Hughes.
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.
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 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
