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This side canyon of Grand Coulee in Washington was carved by the Missoula floods.
This side canyon of Grand Coulee in Washington was carved by the Missoula floods.
A view through a coulee in Alberta, with steep but lower sides, and water in the bottom.
A view through a coulee in Alberta, with steep but lower sides, and water in the bottom.
Drumheller Channels in the Columbia Basin of Washington
Drumheller Channels in the Columbia Basin of Washington
A view upward into a coulee in the Oldman River valley in Lethbridge, Alberta
A view upward into a coulee in the Oldman River valley in Lethbridge, Alberta
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Ice Age floods cut coulees into the basalt of the Channeled Scablands (ecoregion 10a)
Ice Age floods cut coulees into the basalt of the Channeled Scablands (ecoregion 10a)
Quincy Lake, one of the Pleistocene Lake Basins, is a remnant of the temporary Pleistocene lakes that were created by flood waters from glacial Lake M
Quincy Lake, one of the Pleistocene Lake Basins, is a remnant of the temporary Pleistocene lakes that were created by flood waters from glacial Lake Missoula.
Arrowleaf Balsamroot (Balsamorhiza sagittata), Antelope Bitterbrush (Purshia tridentata) and scattered Ponderosa Pine grow in the Yakima Folds (ecoreg
Arrowleaf Balsamroot (Balsamorhiza sagittata), Antelope Bitterbrush (Purshia tridentata) and scattered Ponderosa Pine grow in the Yakima Folds (ecoregion 10g)