Following the last ice age, Turtle Mountain Provincial Park became the first inhabited location in Manitoba. It is also the biggest remaining natural deciduous forest in southwestern Manitoba. Once coniferous forests grew and animals were attracted to the area, nomadic hunters soon followed. Stone tools have been found, confirming their presence. Based on the exhumed artifacts, archaeologists have concluded these people were hunter gatherers, not farmers. In 1875 George Mercer Dawson became the first geologist to travel through Turtle Mountain Provincial Park. Dawson noted the glacial deposits throughout the park.
Indigenous peoples
from the Red River Colony travelled to Turtle Mountain Provincial Park for annual hunting trips between 1810 and 1870. After the buffalo hunt ended many Métis built homesteads within the park. Two notable cultural sites are the Dunseith Trail and Oskar Lake archeological site. The Dunseith Trail was the first trail across Turtle Mountain, and the archeological site was used by Cree hunters over 400 years ago.
Use and activities
Formerly, the park was predominantly used for agricultural purposes due to the presence of hardwoods. The area is no longer dependant on Turtle Mountain for timber, so it is now mainly used for recreation and ranching. There is a trail system used for biking, hiking, and horseback riding. There are also various beaches, playgrounds, and picnic areas for recreational use. The eutrophication of many of the water bodies can make it difficult for recreation in the summer. The most common type of farming is grain farming.
Geography
Turtle Mountain Provincial Park is situated on the Turtle Mountain, one of a number of significant geographic features located along the Manitoba Escarpment, the Canadian portion of the Pembina Escarpment. It is located in the Southwest Manitoba Uplands Ecoregion, within the Canadian Prairies. The park is situated at an elevation of 245 metres. This region is covered by glacial till and fluvioglacial deposits, which remain from the pleistocene ice age. A study of dinoflagellates confirmed the paleocene age of the Turtle Mountain formation. Once deglaciation finished 14,000 years ago the irregular melting pattern left the area covered in hummocky terrain. The soils are mainly grey and black chernozems. There are grey luvisols at higher elevations. The bedrock in the park is composed ofsandstone, shale, lignite coal. There are over 200 lakes and wetlands in this region. Many of the shorelines are covered in thick vegetation due to the littoral zonecattails. This park is home to the largest oak trees in Manitoba, which are the lone survivors of a fire that occurred in the early 20th century. Many of the water bodies are less than 15 feet deep, which often results in a winter decline in fish populations due to lack of oxygen.