Jack Stothard was born on February 16, 1932 in Brandon, MB. He attended public schools in the city (Central School, Park School, and Earl Oxford) and graduated from Brandon Collegiate Institute (BCI). Stothard married Velma Pollock in 1957 and together they had two daughters: Debra and Kimberly. Stothard was employed in the plumbing and heating business until 1960, when he joined Manitoba Hydro. In the course of his employment with Manitoba Hydro, he became Station Superintendent of the Brandon Generating Station. Stothard retired in 1995. Stothard was a member of the Canadian Numismatic Association, the Canadian Association of Token Collectors and the Toronto Postcard Club. Jack Stothard died on November 3, 2021 in Brandon, MB.
Custodial History
Accession 1-2003 was in the possession of Stothard until donated to the McKee Archives in 2003. Accession 12-2006 was acquired by Lawrence Stuckey at some point after the photograph was taken. Stuckey later sold a copy of the photograph. This copy was later acquired by Jack Stothard in the course of his collecting of Brandon postcards. Stothard donated the image to the McKee Archives in 2004. Accession 8-2007 was prepared by Jack Stothard in the course of 2007. He provided a copy to the Archives upon its completion. Accession 8-2008 was in the possession of Fred McGuinness until he gave jit to Jack Stothard in February 2008. Stothard donated the records to the McKee Archives on February 12, 2008. Accession 18-2008 was donated to the McKee Archives by Stothard on August 18, 2008. Accession 11-2009 was donated to the McKee Archives by Stothard on February 20, 2009. Accession 4-2012 was donated to the McKee Archives by Stothard on August 24, 2011. Accession 4-2013 was donated to the McKee Archives by Stothard in March 2013. Accession 8-2016 was donated to the McKee Archives by Stothard on January 21, 2015.
Scope and Content
Accession 1-2003 contains brief research reports prepared by Stothard on various topics concerning historical Brandon. These include: a listing of hotels, inns and motels that have operated in Brandon since the 1880s; reports dealing with the Café Aagard, Central United Church, the 1913 Dominion Exhibition, Brandon, the Empire Hotel, Brandon’s Central Steam Heating System, the Post Office and the Clement Block. It also contains one booklet: Facts About Brandon: An Industrial Survey of the City of Brandon. Winnipeg: Department of Industry and Commerce [n.d.]
Accession 12-2006 consists of one photograph of the Great Northern Engine 208, built by Rogers Locomotive Company 1887. Cylinders 18 x 24, Drivers 63". G.N. line Church's Ferry, N.D. to Brandon, Manitoba. Opened 1906, Closed 1936.
Accession 8-2007 consists of a brief typed report entitled "The Day the Lights Went Out in Brandon - Strike of 1919" by Jack Stothard. Document provides an account of the sources and delivery of hydro electric power to Brandon beginning in the early 1900s and the brief power outage at the beginning of the Brandon General Strike May 25, 1919.
Accession 8-2008 consists of "The Brandon Sun Challenge Cup" ledger, which contains two b/w photographs, newspaper clippings and information on the history and first race (1908) of the cup; 3 additional b/w photographs of different races; and the Brandon Old Timers Association record book (c. 1900).
Accession 18-2008 consists of a copy of Stothard's Brandon Postcards index. The index is divided into various sub-headings and consists of colored reproductions of postcards in Stothard's collection. The index contains pages that were discarded by Stothard as he updated his inventory, therefore the index is only up to date as of August 18, 2008.
Accession 11-2009 consists of a typed research report entitled "Brandon Police Department Stations and Locations" by Jack Stothard. The report outlines the location of the Brandon Police Department from 1882 - 2008, and also includes a section on "What the Future Holds."
Accession 4-2012 consists of pages for Stothard's Brandon Postcards index (18-2008) and a photocopy of a Brandon Municipal Railway ticket.
Accession 4-2013 consits of eight binders of handwritten notes/facts about Brandon compiled by Jack Stothard. The notes are a collection of names, places, things, events and items related mostly to the first 100 years of Brandon (1882-1982), although the notes continue into the 2000's. Some notes centre on the late 1930's to early 1950's during the period of Stothard's youth. The information in the binders was taken from a variety of publications, while some notes are Stothard's own comments. A list of sources, as well as a cross reference index for all eight binders, can be found in Book No. 1.
The accession includes: Book No. 1 - Notes of Brandon (A to B); Book No. 2 - Notes of Brandon (C to F); Book No. 3 - Notes of Brandon (G to O); Book No. 4 - Notes of Brandon (P to Z); Book No. 5 - Notes of Brandon: Churches, Hostpitals, Hotels; Book No. 6 - Notes of Brandon: Police Department, Fire Department; Book No. 7 - Notes of Brandon: Brandon City Council, City of Brandon etc.; Book No. 8 - Notes of Brandon: Brandon College/University, Brandon Schools, ACC, Brandon School Board. Accession also includes pages from Stothard's Brandon Postcards index (18-2008).
Accession 6-2016 consists of local history books, pamphlets, bakery tokens, local magazines, one binder containing handwritten notes/facts about Brandon compiled from the Brandon Sun's "Looking Back" column, and an accordian file box containing newspaper clippings about Brandon.
The accession includes the following local history books: Betty Watson's "One Day in Brandon Manitoba 9/9/99" (Brandon, Manitoba: Bart Art Books, 1999); P.N. Breton's "Popular Illustrated Guide to Canadian Coins, Medals, &. &.," (Winnipeg: Canadian Numismatic Publishing Institute, 1963 [reprint]); "Facts About Brandon: An Industrial Survey of the City of Brandon," (Province of Manitoba: Department of Industry and Commerce, [1946]); The Polish Gymnastic Association Sokol's "75th Anniversary: From the Past to the Future!" ([Brandon, Manitoba: Polish Gymnastic Association Sokol, 1988]); and Brandon Kinsmen Club's "'Together...Once Again': A History of the Kinsmen Club of Brandon, Manitoba, 1925-1975 (Brandon, Manitoba: The Historical Committee of the Kinsmen Club of Brandon, 1975).
Pamplets and magazines include: Brandon Generating Station (1957) and (1969), The Brandon Quota Club presents...A Century in Revue (1982), Canadian Rail No. 168/July-August 1965 [featuring Brandon Municipal Railway], Prairie City Issue No. 3/1994, and Prairion May/June 1997.
The binder is titled Book No. 9 - "Year by year: miscellaneous items from 1969 to 2000"; an asterik (*) indicates notes have been made on each subject or item in the other Books. Each section is housed in
The files in the accordian file box have been rehoused and include the following topics: banks, Brandon 125 beer, Behlen Industries, breweries, Brandon Shoppers' Mall, calendars, Canadian Motors Ltd., Canexus/Nexen, Canada Games - Summer and Winter, Canadian Tire, CKX Radio & TV/CKLQ, Corral Centre, flour mills, hospitals, Keystone, Maple Leaf, Fred McGuinness, miscellaneous, A.E. McKenzie, people, railways, Simplot, Westman Recycling (new facility), weather-storms-floods, and extra copies of postcards.
Notes
Description by Christy Henry. Accession 4-2013: Book No. 1 contains a photocopied photograph of Aagaard's Cafe, photographs of the Dominion Bank and Barney's Drive Inn and a photo reproduction of the Bass Building. Book No. 2 contains a photograph of the Provincial Goal. Book No. 3 contains photographs of T. Eaton Company (4 construction photos) and a photo reproduction of tents on the Exhibition grounds (c. 1940). Book No. 4 contains photoraphs of the Oak Theatre and Western Motors. There are also photopied photographs of The Fun Shop.
Rosser Co-operative Elevator Association Limited Minutes of Council meetings: Jan, March, Sept, 1988 - Jan, Aug, Feb, April, June, Oct, 1990 - Feb, 1991. Miscellaneous, Invitation to the Grand Opening of the Rosser Elevator. Note: Minutes of the council meetings for Bergen and Bergen-Gordon (Amalgamated) for Feb. 1973 to Nov. 1987 are included in Rosser file MPE A 200. Corporate Name: Rural Municipality of Rosser
Files consist of salary briefs, notices, correspondence, reports, briefs and minutes for the Brandon College Faculty Association. File 1b also contains minutes, correspondence and reports (particularly from the Library) for the General Faculty of Brandon College and Brandon University for the years 1959-1967.
Inter-Universities North (IUN) began under a mandate established by the Committee of Presidents of Universities in Manitoba to coordinate delivery of degree credit courses from all three Manitoba uniersities to students living in communities north of the 53rd parallel.
Emily Sawicki became the first person to complete an entire degree program exclusively in the north through IUN in 1979.
Originally the Office of Extension was responsible for the logistics of compiling lists of candidates, arranging interviews and identifying instructors. Student Services provided study skills kits and the Library provided a library skills kit. Library services for IUN students have been available from Brandon University since the early 1970s.
The five First Year by Distance Education (FYDE) communities were Flin Flon, The Pas, Thompson, Dauphin and Russell.
Notes
History/Bio information taken from Campus News - April/May 1992
Storage Location
RG 6 Brandon University fonds
Series 5: Office of the Registrar
ARCH 2: North Lauder Locale
The North Lauder locale has a long archaeological and geological history that is important for understanding the forces that shaped the region. Archaeological research in the locale shows that the area has been occupied by humans for at least the past 6,500 years. Environmental forces provided an area of diverse resources that attracted early peoples.
Environment of the Lauder Sandhills
The North Lauder locale is part of the greater Lauder Sandhills area. The glaciers that covered this region began to recede approximately 11,000 years ago leaving a large lake known as glacial Lake Hind. The Souris River, the Lauder Sandhills and the Oak Lake Aquifer are remnants of the environmental and geological forces that shaped the region.
The Lauder Sandhills region is characterized by a landscape of sand sheets and stabilized sand dunes interspersed with a variety of wetlands. This complex topographic and hydrological situation favoured the development of an island mosaic of mixed forest, wetland and meadow, surrounded by mixed grass prairie. The result was a large, isolated ecotone which provided a rich variety of subsistence resources for hunter-gatherers.
Research in the Lauder Sandhills
Archaeologists from Brandon University have been conducting research in the Lauder Sandhills since 1991. Research in the North Lauder locale has focused on the Atkinson site, a 6,500 year old hunter-gatherer site and Flintstone Hill.
The Atkinson site
The Atkinson site is one of the oldest excavated sites in Manitoba and has been Radiocarbon dated to 6,500 years before present. The Atkinson site is located on the bank of the Souris River and was discovered when a hearth (fire pit) was seen eroding out of the bank. Based on the date of the site and the kind of lithics (stone tools) present it is considered a Gowen occupation. The Atkinson site is evidence that bison hunters were active on the northern plains at a very early date. Similar sites have also been found on the High Plains in the U.S. and are referred to as the Mummy Cave Complex.
The Atkinson Site is of great importance as it is the first undisturbed site of this type to be excavated in Manitoba and extends the range of these sites south and east from the type-sites in central Saskatchewan.
Flintstone Hill
The geomorphology of the glacial Lake Hind Basin over the past 11,000 years is known primarily through the study of a cut bank along the Souris River. Flint Stone Hill contains the most complete stratigraphic record for the post-glacial period on the northern plains. The site has been extensively studied by geoarchaeologists, geologists and paleoenvironmentalists over many years and their findings have contributed to our understanding of the region.
The North Lauder locale Borden designations of Atkinson site DiMe-27 and Flintstone Hill site DiMe-26.
Borden System
Archaeological sites in Canada are identified by the Borden system, which is a uniform site designation system. The country is divided into grids based on latitude and longitude in blocks of 10 x 20 minutes. The first 4 letters indicate the block and the following numbers indicate the actual site. For example the area of the Lauder Sandhills in southwestern Manitoba is identified by the letters DM and the North Lauder locale within that area is DiMe. The Atkinson site is DiMe-27 and the Flintstone Hill site DiMe-26. As new sites are discovered they will be numbered sequentially.
Scope and Content
The Series has been divided into two sub-series, including (1) Atkinson site DiMe-27 and Flintstone Hill site DiMe-26.
Radiocarbon date reports have been scanned in multi-page PDF files.
History / Biographical
The North Lauder locale has a long archaeological and geological history that is important for understanding the forces that shaped the region. Archaeological research in the locale shows that the area has been occupied by humans for at least the past 6,500 years. Environmental forces provided an area of diverse resources that attracted early peoples.
Archaeologists from Brandon University have been conducting research in the North Lauder locale that has focused on the Atkinson site, a 6,500 year old hunter-gatherer site and Flintstone Hill.
The geomorphology of the glacial Lake Hind Basin over the past 11,000 years is known primarily through the study of a cut bank along the Souris River. Flintstone Hill contains the most complete stratigraphic record for the post-glacial period on the northern plains. The site has been extensively studied by geoarchaeologists, geologists and paleoenvironmentalists over many years and their findings have contributed to our understanding of the region.
Radiocarbon dates were obtained from the Atkinson site and Flintstone Hill.
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: the Atkinson site and Flintstone Hill.
Radiocarbon date reports have been scanned in multi-page PDF files.
History / Biographical
North Lauder Radiocarbon Date report by IsoTrace Laboratory for Atkinson II site #TO-11882.
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: Atkinson site and Flintstone Hill.
Radiocarbon date reports have been scanned in multi-page PDF files.
History / Biographical
North Lauder Radiocarbon Date report by IsoTrace Laboratory for Atkinson site #TO-10640.
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: Atkinson site and Flintstone Hill.
Radiocarbon date reports have been scanned in multi-page PDF files.
History / Biographical
North Lauder Radiocarbon Date report by IsoTrace Laboratory for Atkinson site #TO-13365.
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: Atkinson site and Flintstone Hill.
Radiocarbon date reports have been scanned in multi-page PDF files.
History / Biographical
North Lauder Radiocarbon Date report by Beta Analytic Inc. for Flintstone Hill #109529 and #109530.
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: Atkinson site and Flintstone Hill.
Radiocarbon date reports have been scanned in multi-page PDF files.
History / Biographical
North Lauder Radiocarbon Date report by Beta Analytic Inc. for Flintstone Hill #111142 and #111143.
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: Atkinson site and Flintstone Hill.
Radiocarbon date reports have been scanned in multi-page PDF files.
History / Biographical
North Lauder Radiocarbon Date report by Beta Analytic Inc. for Flintstone Hill #109900.
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: Atkinson site and Flintstone Hill.
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.
Field journals have been scanned in multi-page PDF files. Artifact catalogues are PDF files in spreadsheet format. Photographs are in jpeg format.
History / Biographical
Block D is a 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.
Directed by Dr. Nicholson and with Jane Gibson as crew chief, two units were opened in Block D in 1987. A hearth was identified with a ring of stones containing charcoal and burnt bone. Recoveries included two rim sherds with tool-impressed decorations along the outer edge and two prairie side-notched points. Associated bone was primarily appendicular, indicating secondary butchering.
A radiocarbon date of 230+/-90 B.P. recovered in 1987 from 17 cm below surface is consistent with a Protohistoric occupation.
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.
Field journals have been scanned in multi-page PDF files. Artifact catalogues are PDF files in spreadsheet format. Photographs are in jpeg format.
History / Biographical
Block D is a 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.
Directed by Dr. Nicholson with Ian Kuijit as crew chief, five units were opened in Block D in 1988. Four units were excavated: 88, 91, 92 and 94. A feature in units 91 and 92 contained extensive deposits of large bison bone and fire-cracked rock. Several of the lower limb elements were articulated. Bone deposits were associated with numerous large fire-cracked rocks and were clustered in an area of one meter. Also recovered were a side-notched projectile point and two historic gun flints.
Judging from the association of the gun flints, projectile points, and bison bone, as well as the radiocarbon date of 230+/-90 B.P. recovered in 1987, it appears that this feature is from the Protohistoric period and related to refuse disposal.
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.
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.