The main trilobite-bearing formation in Colorado is the Manitou Formation (Manitou Dolomite), which is Lower Ordovician in age. The Manitou Formation is composed of mainly limestone, dolomite, and red dolomite. It has been divided into the Deadhorse and Tie Gulch Members in its northwest province near Glenwood Springs, Garfield Co. in the Piceance basin and the Helena Canyon, Ptarmigan, and Fairplay Members in its southeast province near Salida, Gunnison Co. in the Piceance basin. The Manitou Formation is exposed along the Front Range of Colorado, and extends southward (as far as the San Luis Valley), and north and west (as far as the northern Sangre De Cristo range in the San Isabel National Forest of south central Colorado).
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