Quote:
Originally Posted by xzmattzx
~ Are Lake Telford and Lake Saunders part of some ancient river valley? I originally thought Lake Telford was going to be some kind of clean lake, but it was pretty brown, stagnant, and swampy. Then I looked at it on satellite imagery.
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It is part of the Beaverhill Moraine, connected to Elk Island National Park and all the way south to the Hand Hills. It is a large drainage system when Glacial Lake Edmonton drained.
The big sights for this structure are the following:
Antler Hill (just east of Red Deer): the largest esker in the moraine and causes Red Deer Valley to make a big meander to the north.
Battle River (Big Knife Provincial Park, Highway 36 crossing), another large drainage channel.
Beaver Hills (most prominent around Ryley, I feel like, but also includes Elk Island National Park): the northern terminus of the Beaverhill moraine, where sediments accumulated in the Glacial Lake
Coal Lake (Gwynne): A large channel carved out by the glacial waters
Dry Island Buffalo Jump: A large drainage channel, connected to Dry Snake Valley
Dry Snake Valley (Rumsey Natural Area): a section of hummocky terrain that is better known as "knob and kettle"
Hand Hills: The southern terminus of the Beaverhill Moraine, where sediments accumulated at the apex of Glacial Lake Edmonton.