Dr. John Everett Robbins was born 9 October 1903 in Hampton, Ontario the son of John and Gertrude (Brown) Robbins. He married Catherine St. Denis on 11 June 1934 in Ogdens, New York. John Robbins was raised in Darlingford, Manitoba. He attended the University of Manitoba graduating with a B.A. Hon 1928 and M.A.in 1929. Dr. Robbins completed a Ph.D at the University of Ottawa in 1935. From 1936-1951 he was Director of the Education Division, Dominion Bureau of Statistics.
Dr. Robbins helped to found the Canadian Association for Adult Education, the Social Science Research Council of Canada, the Humanities Research Council of Canada, the United Nations Association in Canada, and the Canadian Citizenship Council. In 1942 he became a member of the Board of Directors of Carlton University. Dr. Robbins was active in UNESCO work: he was a member of Canadian Government delegations to foreign conferences, and, in 1951-52, he spent a year as Director of an educational project for Palestinian Refugees in the Middle East.
In 1960, while editor-in-chief of the newly compiled “Encyclopedia Canadiana,” Dr. Robbins was asked to become President of Brandon College. From 1960 to 1967, he oversaw construction of the Arts and Library Building and Lecture Theatre, a Men's Residence, a Dining Hall, a Heating Plant, a Ladies’ Residence, a Music Building, a Physical Education Building and an Education Building. After the university charter was granted in 1967, Dr. Robbins was installed as the first President of Brandon University.
After his retirement from Brandon University Dr. Robbins was appointed Canadian Ambassador to the Vatican 1970-73. In the years after his departure from Brandon, he held many positions including President of World Federalists of Canada 1977-79 and President of the Canadian Writers Foundation
1976-78. Dr. Robbins served as Executive Chairman and Treasurer of Amnesty International in Canada 1973-75.
He was the recipient of an honorary LLD from the University of Manitoba (1967), Carleton University ( 1969) and Brandon University (1974). In 1994, the title President Emeritus of Brandon University was conferred on John Robbins by the Board of Governors of the University. Dr. Robbins died in 1995, at the age of 91.
Scope and Content
Dr. Robbins' administrative records are located in the Brandon University fonds.
Notes
Dr. John E. Robbins archival papers are held at the Library and Archives Canada.
These records were created by the Director of Library Services from the year 1957 until 1963. It is mainly business correspondence and memorandums. The files include correspondence between the Director of Library Services and various people regarding the library. There are also memorandums to the faculty.
Storage Location
RG 1 Brandon College fonds
Series 14: Brandon College Library
Related Material
RG 6 (Brandon University fonds), sub-series 8.1 (Director of Library Services).
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.
See series level description of the administrative history of the Office of the President/General Manager
Custodial History
See fonds level description of custodial history of A. E. McKenzie Seed Co. Ltd.
Scope and Content
This sub-series includes publications covering a variety of topics related to the seed industry and/or McKenzie Seeds. Publications include:
1. Building Bigger Business/by Charles Austen Bates. Winnipeg, 1925, 4 pp.
2. Business Correspondence/ by C.A. Burt. Chicago, 1905, 221 pp.
3. The Production of Timothy Seed in Alberta/ by H. A. Craig. Edmonton, [no date], 8 pp.
4. Sweet Peas for All Purposes/by A. J. Macself. London, [no date], vi, 84 pp.
5. Growing Quality Beans in Manitoba/by the Manitoba Department of Agriculture, 1976, 12 pp.
6. 1979 Field Crop Recommendations for Manitoba/by the Manitoba Department of Agriculture. Winnipeg, 1979, 69 pp.
7. The Canada Year Book 1915/by the Minister of Trade and Commerce. Ottawa, 1916, xvi, 707 pp.
8. 1974 Vegetable Production Recommendations/by New York State College of Agriculture and Life Sciences, 36 pp.
9. Lawn Care: A Bulletin Service for Turf Enthusiasts/by O. M. Scott & Sons Co. Marysville, Ohio, August 1928 - 1943(?), plus index
10. 1965 Guide to Chemical Weed Control/by the Ontario Department of Agriculture. Toronto, 1965, 67 pp.
11. 1968 Ontario Vegetable Production Recommendations/ by the Ontario Department of Agriculture and Food. Toronto, 1968, 47 pp.
12. 1978 Vegetable Production Recommendations/by the Ontario Ministry of Agriculture and Food. 72 pp.
13. The Canadian Newspaper Directory, seventh edition. Montreal, 1911, xx, 138 pp.
14. The Shareholders' and Directors' Manual/by J. D. Warde. Seventh edition. Toronto, 1907, 617 pp.
THE BUSINESS MAN'S LIBRARY:
15. The Business Man's Library, volume II - Business Correspondence/ by Glenn S. Noble, et al. Chicago, 1907, 221 pp.
16. The Business Man's Library, volume III - Cost of Production/ by Alexander H. Revell, et al. Chicago, 1907, viii, 196 pp.
17. The Business Man's Library, volume V - Book on Buying/ by H.T. Kett, et al. Chicago, 1907, 216 pp.
18. The Business Man's Library, volume VI - Organizing a Factory/ by Clinton E. Woods. Chicago, 1907, 190 pp.
19. The Business Man's Library, volume VII - Book on Advertising/ by Truman A. DeWeese. Chicago, 1907, v, 165 pp.
20. The Business Man's Library, volume X - Accounting and Office Methods/ by W. Vernon Booth, et al. Chicago, 1907, v, 136pp, plus 45 p. index.
Storage Location
RG 3 A.E. McKenzie Company fonds
McS 2 Office of the President/General Manager
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.
Sub-series of one sub sub series: (1) Brandon Aboriginal Literary Festival.
Notes
Records for special events held in the S.J. McKee Archives can be found in the Archives' sub-series: RG 6, 8.2 This sub-series is specifically for special events held under the auspices of the University Librarian.
Storage Location
RG 6 Brandon University fonds
Series 8: Library Services
The sub-series contains the minutes from Library Committee meetings. There are also minutes from the meetings of various sub-committees such as the Open Shelf Sub-Committee and the Sub-Committee on Apportionment of Library Funds. Includes minute books and files.
Storage Location
RG 1 Brandon College fonds
Series 14: Brandon College Library
Sub-series consists of accession records listing the accession number, author, title, publisher, cost and “source” for each book accessioned into the Brandon College Library. It includes a total of 10 accession catalogues covering the period December 1899 - June 1965: 2 accession catalogues (12x18x5) and 8 accession catalogues (9x12x .75 cm)
Storage Location
RG 1 Brandon College fonds
Series 15: Brandon College Library
Esther Moore was born in Norfolk, Nebraska and moved to Canada at age 3. There is a vague reference to her being related to the composer Dvorak in The Quill of 1913. She registered as a music student at Brandon College in 1909. In 1910, Miss Moore received a medal for sight-reading and accompanying in Edmonton. She took her examinations of the Toronto Conservatory of Music in 1910, and her Senior examinations in 1911. She completed her theory work in 1913, as well as finishing the academic requirements. In 1913, Esther Moore became the first graduate of the Music department at Brandon College. After graduation, Miss Moore taught music in Unity, as well as being the choirleader and organist. She returned to her home in Olds, Alberta for a rest from teaching. However, she was not idle for long. She took up teaching again, and she was the organist and choirleader at church. She also began a Glee Club. Between these responsibilities Miss Moore finished a course in the Household Science Department at the Olds Agricultural College. She returned to Brandon College to take postgraduate work, becoming the first Brandon College student to receive her L.T.C.M. in 1916. In 1922 Miss Moore began to teach piano at Brandon College. She received her Bachelor of Music in 1925, and her Master of Music in 1926.
Custodial History
Records were accessioned by the McKee Archives in 1998. Prior custodial history is unknown.
Scope and Content
Esther Moore’s records consist of newspaper clippings, recital programmes, concert programmes, and commencement programmes. As well, there are dance cards, invitations, tickets, and the programme for the annual Graduation Banquet for several years. There are Track and Field programmes and a ribbon. There are also Alumni Luncheon programmes for a few years. There is an issue of The Western Baptist from 1926, and the programmes for the installation of Dr. Robbins as President and the opening of the Arts and Library building and the J.R.C. Evans Lecture Theatre in 1960. There is also a letter from William L. Wright, director of the music department at Brandon College.
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
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
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
Based on the results of the testing in 2002 and the radiocarbon date of 6,500 years before present, further excavation was warranted at the Atkinson site. In 2003 Field Chief Holly Alston and crew Shayne Kolesar and Andrea Richards opened a 42m test excavation (units 1 - 4) that included the hearth area.
The site area was covered with a huge sand dune that was slowly sliding into the river as the supporting bank eroded away. As the dune was removed a late woodland camp was found at the dune interface and a large chunk of charcoal dated this occupation to 440+/-60 B.P. cal.1440A.D. This indicated that the dune was a relatively late incursion over the site. This occupation is likely connected to subsequent testing to the east in 2005 that came to be known as Atkinson II.
Methodology:
The crew began shovel shaving the upper strata with the intention of establishing an arbitrary datum when artifacts were encountered or when a level 25cm above the hearth was reached. At 25cm above the hearth an arbitrary surface datum was established and excavation in 5cm levels began. The overbank deposited matrix was a dense, compacted silt clay and it was necessary to soak the excavated materials in buckets and then water screen the material with a high pressure pump over ¼ inch hardware cloth.
Lithic flakes were found at 10cm below datum, above the hearth level. In the next level, large bone, a broken projectile point and additional flakes were found. Increasing amounts of bone and lithic flakes were found as the excavation continued through levels 3 to 5. The top of the hearth was identified at 28cm below datum, below a 2cm layer of well-sorted sand. This sand layer was confined to a small area directly overlying the hearth. It was considered to be a deliberate quenching of the hearth.
After the conclusion of excavating level 6 the hearth was profiled and photographed. The charcoal and ash layer of the hearth was shown to be directly below the sand layer. Levels 6 and 7 revealed a bison bone bed that was consistent with primary and secondary butchering including elements from the vertebral column and appendicular skeleton. Two additional Gowen (Mummy Cave Series) projectile points were also recovered adjacent to the hearth. Level 8 continued to produce larger amounts of bone and many lithic flakes. Level 9 produced a few bone fragments and a small number of lithic flakes. At the conclusion of the excavations, the crew shoveled sand down from the dune to protect the site over winter and through any subsequent spring flooding.
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
In 2004 Tomasin Playford and her crew of Andrea Richards, Sarah Graham and Shane Kolesar cleared sand cover from over the 2003 excavations and extended sand clearing back from the north edge of the 2003 units to permit implementation of four additional units. During this sand clearing a hearth was identified together with small numbers of lithics and pottery body sherds. This occupation had been noted during sand clearing in 2003 and a charcoal sample was collected and radiocarbon dated to 1440 A.D. This hearth was assigned to Atkinson II, a later occupation.
Four units (5, 6, 7, & 8) were surveyed in adjacent to the 2003 units. Excavation proceeded by means of shovel shaving until the datum pegs from the previous year were located. The new units were then given datum pegs and string boundaries and the high pressure pump was set up for water screening of silt/clay matrix.
Continued to shovel shave levels 1 - 4 and recovered small burned and unburned bone fragments. Level 5 produced a projectile point, an end scraper and a large heat-treated Swan River Chert (SRC) flake. Other SRC flakes were also recovered. Levels 6 and 7 yielded large numbers of flake debitage. The matrix in levels 5-7 contained a scatter of small, bright red ochre particles. The river began to rise on the ninth of June and the site was sandbagged on June 11th, temporarily bringing an end to excavation for Atkinson 1. Tomasin and her crew were relocated to the Crepeele site, west of Lauder.
On July 20th, Tomasin and her crew returned to the Atkinson site and commenced cleaning up the earlier excavation following the flooding. Following the clean up, excavations were resumed on the units that had been opened. An additional Gowen point was recovered from level 8 as well as some poorly preserved bison bone. A lot flakes and small amounts of bone were recovered on west side of block and larger bone and flakes in bone bed along the east side in levels 8 - 10. Two bifaces were recovered in level 11 and a third in level 13. The excavations were terminated at level 18 when water started coming up through the unit floors.
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.