The northern boundary of the park follows the shore of Lake Winnipeg along Sturgeon Bay. The park has no road access and no facilities for visitors within its boundaries. It is low lying, with a mean elevation of about above sea level, sloping very gently to the lake. Wave action and changes in lake level have created a
ridge and swale pattern in the upland areas parallel to the lakeshore. Soils in the park are generally poorly drained
organic soils varying in depth over stony calcareous glacial till. The park has a network of small creeks and ponds draining generally towards the north east into the river and the bay. These are fed by precipitation, shallow aquifers of sand and gravel from glacial deposits and some
Silurian limestone bedrock aquifers. Drainage is slowed by the land profile creating a complex of marshlands, wet meadows,
fens, and
muskeg or
bogs. ==Ecology==