Luseland, elevation 701 m ( 2300 ft), is situated directly beneath the apex of Palliser's Triangle, on the southern fringe of the aspen parklands, between the arms of two ancient glacial valleys that originate in the Neutral Hills ( glacial moraines), just across the Alberta border to the west. Hearts Hill, the most prominent feature in the Luseland district, is the most eastern outlier of the moraine fields, separating the Buffalo Coulee system that drains into the South Saskatchewan River valley, from the Grass Lake system that drains eastward into Tramping Lake.
Luseland, elevation 701 m (2300 ft), is situated directly beneath the apex of Palliser's Triangle, on the southern edge of the aspen parklands, between the arms of two ancient glacial valleys that originate in the Neutral Hills (glacial moraines), just across the Alberta border to the west. Hearts Hill, the most prominent feature in the Luseland district, is the most eastern outlier of the moraine fields, separating the Buffalo Coulee system that drains into the South Saskatchewan River valley, from the Grass Lake system that drains eastward into Tramping Lake.