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Location: 7 km S from Blairmore, Alberta, Canada
12331 20th AvenueBlairmoreAlberta, CanadaT0K 0E0
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The Montane Subregion occurs on lower slopes and valley bottoms, and its upper boundary is the lower limit of the Subalpine Natural Subregion. The Project is also located in the Rocky Mountain Foreland Thrust and Fold Belt, within a succession of generally west-dipping thrust faults and associated folds with predominantly west-dipping axial surfaces. The Project lies between two major thrust faults, in an area of somewhat lesser disturbance. The coal deposits of the Project area are typical of those for Inner Foothills and Rocky Mountain areas which have been subjected to a relatively high tectonic formation. Fault offsets are common but fault- bounded plates generally retain normal stratigraphic thicknesses. Grassy Mountain coal in the Mist Mountain Formation outcrop occurs in a general north-south direction for a strike length of approximately seven (7) km. The Mist Mountain Formation consists of 66 to 194 vertical metres of strata and is overlain by prominent, weather-resistant Blairmore conglomerate. The strata have been strongly folded and faulted, resulting in sediments and coal zones repeated in parallel bands. Coal deposits of this type are characterized by tight folds, some with steeply inclined or overturned limbs. Fault offsets are common but fault-bounded platesgenerally retain normal stratigraphic thicknesses.
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