stripes
Within an area of 1000x300 m about 10 silico-carbonatite dykes up to 10 m thick, trending north-northwest-south-southeast, cut the Precambrian Pikes Peak granite. The largest dyke has a hanging wall of red, hematite-rich potassic fenite. The carbonatite consists essentially of calcite, baryte and hematite. Cutting the highly brecciated fenite and adjacent granite are veins rich in amethyst and smoky quartz. Heinrich and Salotti (1975, Fig. 1) indicate the presence of carbonatite nearby at Gribble Mountain.
HEINRICH, E.W. and SHAPPIRIO, J.R. 1966. Alkalic rocks and carbonatites of the Arkansas River Canyon, Fremont County, Colorado. 3. The Amethyst carbonatites. American Mineralogist, 51: 1088-106.
HEINRICH, E.W. and SALOTTI, C.A. 1975. A colloform carbonatite, McCoy Gulch, Fremont County, Colorado. Mountain Geologist, 12: 103-11