Over 2,400 lakes and 1,200 kilometres of streams and rivers are located within the park. Some notable examples include Canoe Lake and the Petawawa, Nipissing, Amable du Fond, Madawaska, and Tim rivers. These were formed by the retreat of the glaciers during the last ice age.
The park is considered part of the “border” between Northern Ontario and Southern Ontario. The park is in an area of transition between northern coniferous forest and southern deciduous forest. This unique mixture of forest types, and the wide variety of environments in the park, allows the park to support an uncommon diversity of plant and animal species. It is also an important site for wildlife research.
Algonquin Park was named a National Historic Site of Canada in 1992 in recognition of several heritage values including: its role in the development of park management; pioneering visitor interpretation programs later adopted by national and provincial parks across the country; its role in inspiring artists, which in turn gave Canadians a greater sense of their country; and historic structures such as lodges, hotels, cottages, camps, entrance gates, a railway station, and administration and museum buildings.
Over 2,400 lakes and 1,200 kilometres of streams and rivers are located within the park. Some notable examples include Canoe Lake and the Petawawa, Nipissing, Amable du Fond, Madawaska, and Tim rivers. These were formed by the retreat of the glaciers during the last ice age.
The park is considered part of the “border” between Northern Ontario and Southern Ontario. The park is in an area of transition between northern coniferous forest and southern deciduous forest. This unique mixture of forest types, and the wide variety of environments in the park, allows the park to support an uncommon diversity of plant and animal species. It is also an important site for wildlife research.
