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Beaver Hills-Cooking Lake Moraine, a remnant
of the last ice sheet, is characterized
by knob and kettle topography.
When the glaciers retreated from the area,
they left debris clustered around chunks
of ice that formed the knobs, while the
melting ice made shallow ponds or kettles.
These are eutrophic ponds, meaning they
have a very poor oxygen supply, but they
contain rich accumulations of nutrients,
making them an excellent habitat for plants
and wildfowl. The park has more than 250
lakes, ponds and wetlands over 20% of
its surface area. Astotin Lake, near the
parkŪs north end is 3.9 kilometres long,
almost 3.1 kilometres wide and .5 - 10
metres deep, the parkŪs largest body of
water.

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The forested hills
and rolling meadows are surrounded by
grain fields and pasture, the aspen thickets
providing forage and protection for the
wildlife. Unique vegetation communities
of white spruce, white birch, sand hill
vegetation and saline wetlands are also
found. Trembling aspen appears on the
higher slopes and paper birch on the lower
wetlands. In the northern end of the park
are the boreal-type forest, orchids, Indian
pipe, yellow pond lily and white water
lily. In the central region are the black
spruce bogs with muskeg vegetation such
as round-leafed sundew. Browsing moose,
elk, and deer munch berry bushes such
as dogwood and saskatoon. Some prairie
vegetation that may appear within the
park are hawthorn, buckbean, buckbrush,
prairie sage and Black-eyed Susan.
For thousands of years
the aboriginal peoples occasionally used
the area now known as Beaver Hills. Glaciation
has destroyed any evidence of occupancy
before 10 500 years ago. The mix of vegetation
would have been very important to native
people, who probably relied on the location
for winter food and shelter. In the summer,
the surrounding plains would have provided
bison. It has always been an excellent
habitat for elk, moose, deer, bear and
game birds, berries, wild vegetables and
fish. The camp could depend on the site
for fresh water and firewood. The European
trappers, who came to develop the fur
trade, rapidly depleted these resources
making the land inhospitable to settlers
who arrived in the early 1900s but
rarely stayed to homestead.
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