Is a quartz monzonite porphyry in Eagle basin composed of abundant phenocrysts of feldspars, quartz, and biotite in a gray or greenish crystalline matrix. Is later than Lincoln porphyry. Was formerly included in Lincoln porphyry. Assigned to early Tertiary.
Source: GNU records (USGS DDS-6; Denver GNULEX).
Occurs principally as sills in area between East Fork of Eagle River and East Tennessee Creek, Eagle Co., CO in Eagle basin. Is assigned to Paleocene?.
Source: GNU records (USGS DDS-6; Denver GNULEX).
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