New Mexico
Wheeler Peak |
Metamorphic (metamorphosed volcanic) |
Bedrock: Unnamed gneiss |
Early Proterozoic (older than 1.75 b.y.) |
Well foliated fine- to medium-grained biotite gneiss, biotite-hornblende gneiss, hornblende gneiss and amphibolite, interlayered on scales from a few centimeters to several meters. Minerals in these gneisses are quartz, plagioclase, blue-green hornblende, brown biotite, epidote and magnetite. Locally thin lenses of ferruginous quartzite, magnetite ironstone and quartz-epidote-calcite marble are included in the gneiss. The rocks have been severely deformed and contain rootless isoclinal fold noses and other indicators of extremely ductile deformation. The gneiss is intruded by the Red River tonalite, also Early Proterozoic and dated at 1.75 b.y. Walter and Frazier Peaks to the north are made up of the layered gneiss; the younger tonalite lies between them and Wheeler Peak. The gneisses are also locally intruded by diabase dikes. The range was uplifted during the Cretaceous Laramide Orogeny. Surficial Geology: The approach via Williams Lake Trail crosses Pleistocene glacial till and a Holocene rock glacier, a lobate deposit of angular rock fragments. Soil Series: Penitente cobbly loam: Dark brown cobbly loam developed from bedrock residuum in widely scattered depressions between rock outcrops. |
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