Winifred North (nee Seaborn) was born December 13, 1920 in Burwash, Sussex, England. At the age of five, she moved to Manitoba, growing up in the Osprey and Mentmore districts, attending Osprey and Gordon schools. Winnie married Alfred James North (1917-1994) on October 16, 1948. Together they had three children: Bruce, Heather and Maureen. Alf served in the armed forces during the Second World War. Following the war he farmed in the Norman district until 1966, at which point the family moved to Brookdale. Alf then served as custodian for the Brookdale school before retiring in 1983. In Brookdale, Winnie worked at the post office, becoming postmistress. Winnie was a member of the Brookdale United Church, the Neepawa Legion Ladies Auxiliary and the Brookdale Belles and Beaux square dancing group. Winifred North died on January 13, 2018 in Neepawa, MB. She is buried at Neepawa Cemetery.
Custodial History
As part of the Westman Oral History Collection, this collection was accessioned by the McKee Archives in 1998. The original tapes from the Westman Oral History project were deposited in the Brandon Public Library. Copies of these originals were made by Margaret Pollex of the Brandon University Language Lab at the request of Eileen McFadden, University Archivist in the early 1990s. These copies compose the collection held in the McKee Archives.
Scope and Content
Item is an audiocassette tape containing an interview with Winnie North about the 100th Anniversary of the Brookdale Post Office. Interviewer is Dorothy P. Martin.
Notes
History/bio information taken from the records and the Brookdale local history "Quest in Roots." Transcript by Megan Holowick (2014). Description by Christy Henry.
Language Note
English
Audio Tracks
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[This station, located 13 km north of Brandon on the east side of PTH 10, was] built in the early 1930s to replace Knox as the CNR’s mainline station for Brandon. All passenger trains stopped and buses operated between the CNR’s Brandon station and Brandon North to meet all trains. It was enlarged as shown here in late 1930s, and at peak operation in the 1940s & 1950s saw six daily passenger trains 1 - 2 & 3 - 4 “Continental Limited” and 11 - 12 locals. VIA trains 3 and 4 "Supercontinental" ceased operation Nov. 15, 1981 leaving no passenger service on the former Grand Trunk Pacific mainline of CNR [at that time]. This station was demolished in the fall of 1982.
Custodial History
For custodial history see the collection level description of the Lawrence Stuckey collection.
Papers of a conference sponsored by the University of Manitoba Faculty of Agriculture and Home Economics and the Iowa State University Center for Agricultural and Economic Development
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.
View is southwest from the north side of Princess Avenue. Photograph shows the north driveway entrance on campus. The original Music Building, the A.E. McKenzie Building, Clark Hall and part of the Brandon College Building are visible.
This bridge was condemned in the late 1930s but cyclists continued to use it until it was torn down (approximately 1940)
Until the early 1920s the Canadian Pacific Railway maintained a well and pumping station near the southeast corner of this bridge, which pumped water through a pipeline to a locomotive watering tank at Kemnay.
Custodial History
For custodial history see the collection level description of the Lawrence Stuckey collection.
Scope and Content
Assiniboine River Bridge North of Kemnay
Notes
[Mr. Stuckey put a negative and print in the same envelope. We have separated them, numbering the negative OB5(1) and the print OB5(1a).]
This bridge was condemned in the late 1930s but cyclists continued to use it until it was torn down (approximately 1940)
Until the early 1920s the Canadian Pacific Railway maintained a well and pumping station near the southeast corner of this bridge, which pumped water through a pipeline to a locomotive watering tank at Kemnay.
Custodial History
For custodial history see the collection level description of the Lawrence Stuckey collection.
Scope and Content
Assiniboine River Bridge North of Kemnay
Notes
[Mr. Stuckey put a negative and print in the same envelope. We have separated them, numbering the negative OB5(1) and the print OB5(1a).]