Named for Pitts Meadow in the southwest part of Black Ridge quad, T51N, R9W, Montrose Co, CO, Southern Rocky Mountain region. This locality called the type area. Is well exposed on top of Pitts Meadow and in steep canyon walls that flank mesa above Gunnison River, and along length of Black Canyon between Pitts Meadow and Smiths Fork, and in lower part of gorge of Crystal Creek. Consists chiefly of strongly to weakly foliated, medium-grained, gneissic trondhjemitic granodiorite or quartz diorite. Mineral proportions vary considerably. Is batholithic in size, though exposed in only a few sq mi area. Has a whole rock Rb-Sr age of 1.73 +/-0.19 b.y. Assigned to the Precambrian.
Source: GNU records (USGS DDS-6; Denver GNULEX).
Mapped west of Gunnison River, Red Rock Canyon quad, sec 2, T50N, R9W, Montrose Co, CO in the Southern Rocky Mountain region. [May represent eastern limit of formation.]
Source: GNU records (USGS DDS-6; Denver GNULEX).
Probably a batholithic body but exposed only in northwest part of Black Canyon of Gunnison River, Montrose Co, CO in Southern Rocky Mountain region. Listed with granitic rocks of circa 1,700 m.y. (Precambrian X) age group.
Source: GNU records (USGS DDS-6; Denver GNULEX).
Is one of nine formally named lithodemic units assigned to the Early Proterozoic Routt Plutonic Suite (new name). Occurs as a pluton in Gunnison area in Southern Rocky Mountain region, CO. It may be present in the subsurface, but its extent beyond the Black Canyon is not known. Is a trondhjemitic granodiorite and quartz diorite.
Source: GNU records (USGS DDS-6; Denver GNULEX).
For more information, please contact Nancy Stamm, Geologic Names Committee Secretary.
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