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Haileybury in Temiskaming Shores in Timiskaming District, Ontario — Central Canada (North America)
 

Lake Temiskaming and the Mugwamp
⎯⎯⎯
Lac Témiscamingue et le Mugwamp

 
 
Lake Temiskaming and the Mugwamp / Lac Témiscamingue et le Mugwamp Marker image. Click for full size.
Photographed by Cosmos Mariner, June 2, 2022
1. Lake Temiskaming and the Mugwamp / Lac Témiscamingue et le Mugwamp Marker
Inscription.  
[English] Lake Temiskaming, a freshwater lake is shared by both Ontario and Quebec as it forms part of the provincial border between the two provinces. Created during the last ice age, as the glacier carved its way through the rock, the lake is what remains of the original Lake Barlow-Ojibwa, which existed over 10,000 years ago. The waters of the lake are deep and who knows what could be swimming beneath its waters! The names given to the creature of Lake Temiskaming are “Mugwamp”, “Mudwump” or “Tess”. Some attribute the strange occurrences to that of a large sturgeon or a creature that is long and shaped like a dinosaur. Keep your eyes open!

[Français] Le lac Témiscamingue est un lac d'eau douce qui se partage entre les provinces de l'Ontario et du Québec en servant de frontière interprovinciale. Formé au cours de la dernière glaciation alors que les glaciers se frayaient un passage dans le roc, le lac est le vestige de l'ancien lac Barlow-Ojibwa d'il y a 10 000 ans. Les eaux du lac sont profondes, et qui sait ce qui nage au fond! Le nom donné à cette créature du lac Témiscamingue est « Mugwamp », « Mudwump » ou « Tess ». Certains interprètent ce phénomène par la présence d'un énorme esturgeon ou une créature de même dimension et apparence qu'un dinosaure. Nous vous conseillons de bien ouvrir l'œil!
 
Erected by Province
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of Ontario, South Temiskaming SUD Community Futures Development Corporation, Federal Economic Development Agency for Northern Ontario.
 
Topics. This historical marker is listed in this topic list: Natural Features.
 
Location. 47° 27.639′ N, 79° 38.399′ W. Marker is in Temiskaming Shores, Ontario, in Timiskaming District. It is in Haileybury. It is on Lakeshore Road South 0.3 kilometers north of Latchford Street, on the right when traveling north. The marker is overlooking Lake Temiskaming from Hughes Lookout. Touch for map. Marker is in this post office area: Temiskaming Shores ON P0J 1K0, Canada. Touch for directions.

Regionally, this marker is in Northeastern Ontario and specifically in Northern Ontario. It is also in Central Canada. Globally, it is in North America, the Great North Woods, the Western Hemisphere, the Western World, and the Anglosphere. Historically, it finds itself in what was once a British colony, the Viceroyalty of New France, the Haudenosaunee (Iroquois) Confederacy, and Rupert’s Land.

Other nearby markers. At least 8 other markers are within
Lake Temiskaming and the Mugwamp / Lac Témiscamingue et le Mugwamp Marker image. Click for full size.
Photographed by Cosmos Mariner, June 2, 2022
2. Lake Temiskaming and the Mugwamp / Lac Témiscamingue et le Mugwamp Marker
Looking east across Lake Temiskaming from Lakeshore Road South. The marker is on the left side of the picnic shelter.
walking distance of this marker: Millionaires Row / Le Rang des Millionaires (approx. 0.7 kilometers away); William H. Wright Building Art Deco Sculpture (approx. 0.9 kilometers away); School of Mines and RockWalk Park / L'École des Mines et le Parc RockWalk (approx. 0.9 kilometers away); The Inukshuk (approx. 0.9 kilometers away); Living Underground at Coober Pedy (approx. 0.9 kilometers away); Calcite Breccia (approx. one kilometer away); Haileybury Jail / Le prison de Haileybury (approx. 1.3 kilometers away); Court House / Le Palais de Justice (approx. 1.3 kilometers away). Touch for a list and map of all markers in Temiskaming Shores.
 
Also see . . .  Lake Ojibway (Wikipedia).
Excerpt:  Lake Ojibway was a prehistoric lake in what is now northern Ontario and Quebec in Canada. Ojibway was the last of the great proglacial lakes of the last ice age. The proglacial lake was named Ojibway in 1909 by Canadian geologist Arthur Philemon Coleman after an Indigenous people whose homeland coincides with his proposed location of the lake. Comparable in size to Lake Agassiz (to which it was likely linked), and north of the Great
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Lakes, it was at its greatest extent c. 8,500 years BP. The former lakebed forms the modern Clay Belt, an area of fertile land.

Lake Ojibway was relatively short-lived. The lake likely drained approximately 8,200 years BP. One hypothesis is that a weakening ice dam separating it from Hudson Bay broke, as the lake was roughly 820 ft above sea level but recent studies assert Lake Ojibway drained in two separate events and through a combination of ice dam breach and subglacial flooding.

(Submitted on July 3, 2026, by Cosmos Mariner of Cape Canaveral, Florida.) 
 
 
Credits. This page was last revised on July 4, 2026. It was originally submitted on July 1, 2026, by Cosmos Mariner of Cape Canaveral, Florida. This page has been viewed 7 times since then. Photos:   1, 2. submitted on July 3, 2026, by Cosmos Mariner of Cape Canaveral, Florida.
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Jul. 8, 2026