Half Dome Granodiorite

Half Dome Granodiorite is granodiorite found in a region on and near Half Dome, in Yosemite National Park, California, United States. The granodiorite forms part of the Tuolumne Intrusive Suite, one of the four major intrusive suites within the Sierra Nevada.

Mineralogy

The granodiorite has large crystals of biotite, hornblende, and both feldspars — orthoclase and plagioclase. The space between crystals tends to be filled with quartz. The hornblende tends to have large, over rectangular crystals. The biotite forms hexagonal "blocks," up to across. A knife blade can peel the edges.
Sphene is found in Half Dome Granodiorite. The grains are honey-colored, and large at across. Uranium is also present.
From petrographic observation, the average mineral proportion of non-layered rocks of Half Dome Granodiorite is 45% plagioclase feldspar, 25% quartz, 8% biotite, 15% K-feldspar, 5% hornblende, 1% titanite, and 1% magnetite.

Age

Half Dome Granodiorite traces to early Late Cretaceous. Its age is between 85 and 83.4 Ma, with average age of 84.1 Ma. It is younger than Sentinel granodiorite, and older than Cathedral Peak granite. Half Dome Granodiorite is the Valley's youngest plutonic rock.

Locations

Half Dome Granodiorite dominates Yosemite Valley area east of Royal Arches and Glacier Point. At Church Bowl and in the cliff west of Royal Arches, horizontal dikes of Half Dome Granodiorite cut the older granodiorite of Kuna Crest. Half Dome Granodiorite forms the sheer cliffs to the north of the trail between the Ahwahnee Hotel and Mirror Lake. The trail to Vernal and Nevada Falls also crosses through Half Dome Granodiorite.