Named for development around Mount Lincoln [which lies north of Alma, Park Co, CO in the South Park basin, according to Wilmarth (1938, US geologic names lexicon, USGS Bull. 896)]. Mapped with other porphyries on geologic map. Consists of quartz, orthoclase and plagioclase feldspars, and biotite. Its most striking peculiarity is the frequent occurrence of large crystals of glassy-looking orthoclase feldspar about 1 in long. Quartz occurs in double pyramids, has a rounded outline, and frequently a rose tint. Mica generally decomposed and of greenish color. Age not clearly stated. [Is probably a Tertiary porphyry].
Source: GNU records (USGS DDS-6; Denver GNULEX).
Is a quartz monzonite porphyry in Eagle basin. Contains large phenocrysts of light-gray or pink orthoclase. Is younger than Elk Mountain porphyry and older than Eagle River porphyry. Assigned to early Tertiary.
Source: GNU records (USGS DDS-6; Denver GNULEX).
Has a K-Ar date on biotite of 64 m.y. Is one of youngest of porphyries, or of very early Paleocene age.
Source: GNU records (USGS DDS-6; Denver GNULEX).
A coarse-grained porphyritic monzogranite mapped as Paleocene by Tweto (1960) mapped as the Oligocene (35.6 +/-1.2 m.y. K-Ar date) Turquoise Lake stock in Eagle basin.
Source: GNU records (USGS DDS-6; Denver GNULEX).
For more information, please contact Nancy Stamm, Geologic Names Committee Secretary.
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