A Brief, Illustrated History of Landscape and Aboriginal Peoples in - - PDF document

Presenta

• n to the Lake of Bays Heritage Founda
• n 2009,

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A Brief, Illustrated History of Landscape and Aboriginal Peoples in the Muskoka River Region Presenta

• n to the Lake of Bays Heritage Founda
• n Annual Mee

ng by Mar n Cooper (Archaeological Services, Inc., Toronto) and Andrew Stewart (Strata Consul ng, Inc., Toronto) 15 August 2009

At the end of the last Ice Age, 11,000 years ago, as the con nental glacier melted it fl

• oded low-

lying areas south of it, including today’s Great Lakes and surrounding lowlands. On this map, the purple line represents the shoreline of glacial Lake Algonquin, which fl

• oded the Huron-

Georgian Bay-Lake Simcoe basin for about 1000 years. This ancient lake was at a level about 10 m higher than the present Huron-Georgian Bay level. The land was depressed by the weight of the ice – it has since rebounded – and so traces of this shoreline are now found as much as 100-150 m above the present water level in Georgian Bay. Further south, where today this shoreline passes through an open landscape of ploughed fi elds, archaeologists can search these fi elds for traces of people who lived on the shore of Lake Algonquin, known to archaeologists as Palaeo-Indians. Several Palaeo-Indian sites containing 11,000-year-old stone tools have been found on this shoreline, as shown here.

Sources: Freeman 1979, Stewart 2004; Storck 2004.

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This book is the best general account of the archaeology of the earliest se lement of southern Ontario by people immediately a er the Ice Age (11,000 – 10,000 yrs ago). The cover illustra

• n shows people hun

ng caribou at a me when the southern Ontario landscape was similar to subarc c tundra -- lightly forested with spruce trees with open areas. The margin of the con nental ice sheet was somewhere along, or just north of, the French River. Above the hunters in the illustra

• n is a

dis nc ve type of stone dart or spear point that Palaeo-Indians made during this period out of a rock called chert (like fl int), which was quarried from the Niagara Escarpment near Collingwood. These are the kinds of stone tools that archaeologists fi nd along the Lake Algonquin shoreline.

Source: Storck 2004. Illustra

• n (drawing by Ivan Kocsis) courtesy of UBC Press and the Royal Ontario Museum,

used on the cover of Journey to the Ice Age by Peter Storck (UBC Press and Royal Ontario Museum, 2004)

On this map, you can see that Lake of Bays represents a former inlet of glacial Lake Algonquin and that Peninsula and Fairy Lakes formed the mouth of this inlet.

Sources: Bajc 1994; Bajc and Henry 1991; Long 1989.

In the Muskoka region, the shoreline is less dis nct; ploughed fi elds, where archaeologists can usually clearly see if ar facts are present, are scarce. You can, however, see traces of the shoreline east of Highway 11. Because sediment in this area of the Canadian Shield is generally thin, these traces tend to be only weakly visible.

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Not all Palaeo-Indian sites are found south of Lake Simcoe. This spear point from the Late Palaeo-Indian period comes from a site located

• n the Algonquin shoreline in the

region of the Lake of Bays inlet.

Source: Allen 2002.

In addi

• n to glacial lake

shorelines, other natural features are of interest to archaeologists. The Lower Oxtongue River fl

• odplain on Lake of Bays formed
• ver the last 10,000 years by the

fl

• oding and meandering ac
• n
• f the river channel and the

accumula

• n of sand and mud in

its fl

• odplain.

This is the kind of se ng where archaeological sites typically get buried and preserved. Further upstream, to the right, is a record of older fl

• oding and deposi
• n by glacial outwash

sands at the end of the Ice Age. To the west and north of the lower Oxtongue River are shallow-water sands deposited in glacial Lake Algonquin.

Sources: Ontario Ministry of Natural Resources Natural Heritage Informa

• n Centre, Natural Areas Information,

http://nhic.mnr.gov.on.ca/MNR/nhic/areas.cfm; Bajc 1994; Bajc and Henry 1991; Geddes and McClenaghan 1984; Ontario Geological Survey 2003.

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The level of Lake Algonquin fell dras cally at the end of the Palaeo-Indian period, to well below present Georgian Bay levels. Water levels in the Great Lakes only reached their modern levels (which are s ll fl uctua ng within a narrower range) between about 4000 and 5000 years ago. At this me, during the period that archaeologists refer to as the Late Archaic (about 4500 – 2900 years ago), people established camps on or near shorelines and traveled along river and lake routes that are essen ally familiar to us today (disregarding the changes to hydrology brought about by canals and dams built in the 19th and 20th centuries).

Sources: Allen 2002; Ellis et al. 1990; Karrow and Warner 1990; Long 1989; The Archaeology of Ontario: h p:// www.ontarioarchaeology.on.ca/summary/contents.htm.

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The materials and ar facts in the last slide were imported from all over the Great Lakes region during the Middle Woodland period (possibly even from Labrador) via routes of travel following major rivers and lakes. Sources: Allen 2002; Spence et al. 1990. The mouth of the Severn River, at the southwest edge of the Muskoka Lakes region, is known as an important loca

• n in central Ontario during various periods, including especially the Middle

Woodland period (AD 0 – 500), a me when ceremonial mounds were built across Ohio and in many river valleys of the Great Lakes region, including the Trent River valley. This image is an example of a collec

• n of ar

facts and raw materials from a site that was probably a Middle Woodland ceremonial mound removed by co age development of this built-up area during the mid-20th century. Sources: Allen 2002; The Archaeology of Ontario: h

p://www.ontarioarchaeology.on.ca/

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This Petroglyph site located on Sparrow Lake was men

• ned but

not visited by Dewdney during his extensive documenta

• n of

pictograph sites in Ontario. It was relocated by ASI during the Heritage Master Plan for Muskoka in 1993. To date, it is the only example of aboriginal rock art in the Muskoka District.

Sources: ASI 1994, Dewdney and Kidd 1967

This map shows some of the Iroquoian- and Algonquian-speaking peoples and na

• ns in central Ontario that were recorded by the

Jesuits who were living among the Huron in the Orillia-to-Midland area during the fi rst half of the 17th century.

Source: Heidenreich 1987.

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Picking up the story from the historical record in the 19th century, it is not known whether the Anishinaabeg, the aboriginal peoples living in the eastern Georgian Bay-Muskoka region during the late 18th and early 19th century (who eventually se led at places like Rama, Parry Island and Beausoleil and Chris an Islands), were directly descended from some of the groups shown in the last slide (e.g., the Sagahanirini in western Muskoka), or whether these early 19th century peoples were part of a southeastward movement of people known today, collec vely, as the Anishinaabeg who, following the dispersal of the Huron in 1649, moved down from the north shore of Lake Huron and Lake Superior during the late 17th century. Western Muskoka came to be occupied by families affi liated with the Muskoka band, who were permanently based at Coldwater, then moved to Beausoleil Island (1842), then to Chris an Island (1856). Southern and eastern Muskoka was used by families – with names like Yellowhead and Bigwin -- from Rama (now Mnjikaning). Families based at places like Rama and Beausoleil Island in the winter would travel to the Muskoka region in spring to establish gardens as well as to hunt and trap (deer, bear, muskrat, beaver) and trade in the area around their se

• lements. James Bigwin (Bigwind) and Chief

William Yellowhead (Mesquakie), who dis nguished themselves in the War of 1812 (at the Ba le of York, 27 April, 1813), were from Rama. Bigwin had his se lement on Bigwin Island In Lake of Bays and at Cedar Narrows (today’s Dorset) leading into Trading Lake. Yellowhead had a se lement at Kehkapekon (Bracebridge portage). Menominee, well known to mid-late- nineteenth-century Muskoka se lers, hunted between Lake of Bays and Mary Lake, eventually establishing a farm at Menominee Lake before moving to Parry Island in the 1870s.

Sources: ASI 1994; Malcomson 2008

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Chief John Bigwin

Source: Avery 1974:4

As shown in this map of his route, John Bigwin (son of James) would travel during spring, for 45 years, from Rama down the Severn River through Washago to Morrison Lake, through Lag Lake, to Muskoka Bay, up the South Branch

• f the Muskoka River to Lake of Bays, ending at Cedar

Narrows and Trading Lake where he had his se lement and

• garden. Source: ASI 1994

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Around Lake of Bays are place names and sites origina ng in aboriginal se lement and land-use. The narrows at Trading Lake is where Bigwin grew potatoes and corn and fi shed. Another source of informa

• n about the

area are the maps and diaries of the early surveyors such as David Thompson, who crossed from Georgian Bay to the O awa River in the fall of 1837, accurately mapping the lakes and rivers of the Muskoka and Madawaska system en route. Earlier, Alexander Sherriff encountered Mohawks from Lake of Two Mountains (Oka) who were trading in the Muskoka-Algonquin region. Mohawks eventually came to se le here (Wahta) in the 1880s from Oka, having been familiar with the area from earlier guiding and trading ac vity.

Source: Franks 1985

As late as 1923, he collected birch bark in this area for making canoes. Paint Lake, a place of se lement for a Mnjikaning family, was also a source of red ochre (iron oxide) that, when mixed with fat, was used for body paint and petroglyphs (rock art). Bigwin Island was used as both se lement and burial ground. It contains the cemetery for Chief Bigwin’s ancestors and is the place he expressed his wish to be buried, but in the end, wasn’t. There is fi lm footage of Bigwin visi ng Bigwin Island cemetery in the 1930s. Menominee Lake is where Menominee established his farm by 1871 and crops were being grown on Norway Point in the early nineteenth century.

Source: ASI 1994

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These images are photographs taken during the Hayes canoe trip to Algonquin Park in 1897, four years a er the Parks crea

• n.

This map shows how hun ng territories of families (named) extended into the Muskoka region from Parry Island in the late 19th century (informa

• n recorded

in the 1930s by anthropologist Diamond Jenness). Territorial boundaries were generally avoided and features along these boundaries, e.g., Moon River, Skeleton (originally Paukuh [Spirit] Lake) were some mes associated with bad

• manidou. Source: Jenness 1935

Guides were hired at Rama because of their in mate knowledge with the shield area to the north including Muskoka, Algonquin Park and Haliburton. The large photographic collec

• n

including many more images of the Rama guides is housed in the Algonquin Provincial Park

• archive. Source: Tozer and Strickland 1986

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This map shows the loca

• n of First Na
• n reserves in the

District of Muskoka and the surrounding area.

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Sources Cited: Allen, W.A. 2002 Wa-nant-git-che-ang: Canoe Route to Lake Huron through Southern Algonquia. Ontario Archaeology 73:38-68. h p://www.ontarioarchaeology.on.ca/publica

• ns/pdf/oa_73_

part_05.pdf ASI [Archaeological Services Inc.] 1994 Report of the Master Plan of Archaeological Resources of the District of Muskoka and the Wahta Mohawks. 3 vols. On fi le at the District Municipality of Muskoka offi ce. Avery, S.G. 1974 Refl ec

• ns: Muskoka and Lake of Bays of Yesteryear. Herald-Gaze

e, Bracebridge. Bajc, A.F. 1994 Quaternary Geology of the Huntsville-Penetanguishene Area, Central Ontario. Ontario Geological Survey, Open File Report 5882 [includes Bajc and Henry 1991] Bajc, A.F. and A.P. Henry 1991 Quaternary Geology of the Huntsville-Bracebridge Area, Southern Ontario [map sheet]. Ontario Geological Survey, Open File Map 161, scale 1:50,000. During the early 1990s, Archaeological Services

• Inc. prepared a heritage master plan for the

District of Muskoka and the Wahta Mohawks to guide development and recommend strategies for avoiding or mi ga ng damage to heritage resources by development. Sources of informa

• n

for this 3-volume report came from the record archaeological sites registered with the Ministry of Culture, exis ng collec

• ns of archaeological

materials in private hands, historical records, and other sources. The study documents 11,000 years of se lement and land use in this region through knowledge of archaeological sites, resident knowledge, and historical records.

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Dewdney, S. and K.E. Kidd 1967 Indian Rock Pain ngs of the Great Lakes. University of Toronto Press, Toronto. Ellis, C.J., I.T. Kenyon and M.W. Spence 1990 The Archaic. In The Archaeology of Southern Ontario to AD 1650, edited by C.J. Ellis and N. Ferris, pp 65-124. Occasional Publica

• n 5.

Ontario Archaeological Society London Chapter. London. Franks, C.E.S. 1985 David Thompson’s Explora

• ns of the Muskoka and Madawaska Rivers.

In Nastawgan: the Canadian North by Canoe and Snowshoe, edited by B.W. Hodgins and M. Hobbs, pp 24-37. Betelgeuse Books, Toronto. Freeman, E.B. Geological Highway Map, Southern Ontario. Ontario Geological Survey map 2441. Geddes, R.S. and M.B. McClenaghan 1984 Quaternary Geology of the Kawagama Lake Area, Nipissing and Muskoka Districts and Haliburton County. Ontario Geological Survey Map P. 2705, Geological Series – Preliminary Map, scale 1:50,000. Heidenreich, C. 1987 Se lements and Missionaries, 1615-1650. In From the Beginnings to 1800, edited by R.C. Harris and G.J. Ma hews, Plate 34. Historical Atlas of Canada, volume 1, R.C. Harris and G.J. Ma hews general editors. University of Toronto Press, Toronto. Jenness, D. 1935 The Ojibwa Indians of Parry Sound, their Social and Religious Life. Bulle n 78, Anthropological Series 17. Canada Dept of Mines, Na

• nal Museum of Canada, O

awa. Karrow, P.F. and B.G. Warner 1990 The Geological and Biological Environment for Human Occupa

• n in Southern Ontario. In The Archaeology of Southern Ontario to AD 1650, edited by

C.J. Ellis and N. Ferris, pp 5-35. Occasional Publica

• n 5. Ontario Archaeological Society London
• Chapter. London.

Long, Gary 1989 This River: the Muskoka. Boston Mills Press, Erin, Ontario. Malcomson, Robert 2008 Capital in Flames: the American A ack on York, 1813. Robin Brass Studio, Montreal. Ontario Geological Survey 2003 Surfi cial Geology of Southern Ontario. OGS Miscellaneous Release Data 128. 2 vols (set of 2 CDs containing digital spa al data for GIS). Spence, M.W., R.H. Pihl and C.R. Murphy 1990 Cultural Complexes of the Early and Middle Woodland Periods. In The Archaeology of Southern Ontario to AD 1650, edited by C.J. Ellis and

• N. Ferris, pp 125-169. Occasional Publica
• n 5. Ontario Archaeological Society London Chapter.

London. Stewart, A. 2004 Intensity of Land Use Around the Holland Marsh: Assessing Temporal Change from Regional Site Distribu

• ns. In The Late Palaeo-Indian Great Lakes: Geological and

Archaeological Inves ga

• ns of Late Pleistocene and Early Holocene Environments, edited by

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L.J. Jackson. and A. Hinshelwood, pp 85-116. Mercury Series Archaeology Paper 165. Canadian Museum of Civiliza

• n, Ga

neau. Storck, P.L. 2004 Journey to the Ice Age: Discovering an Ancient World. UBC Press, Vancouver. Tozer, Ron and Dan Strickland 1986 (4th revision) A Pictorial History of Algonquin Provincial Park. The Friends of Algonquin Park and the Ontario Ministry of Natural Resources, Whitney, Ontario.