Half Dome Granodiorite

Half Dome Granodiorite is granodiorite (see also granite) 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 (aka Tuolumne Batholith), one of the four major intrusive suites within the Sierra Nevada.

Half Dome Granodiorite
Stratigraphic range: early Late Cretaceous
TypeGeological formation
Lithology
PrimaryGranodiorite
Location
RegionYosemite National Park
CountryUnited States
Type section
Named forHalf Dome

A geologic map of Yosemite National Park

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 0.5 in (1.27 cm) rectangular crystals. The biotite forms hexagonal "blocks," up to 0.25 in (6.35 mm) across. A knife blade can peel the edges.

Sphene is found in Half Dome Granodiorite. The grains are honey-colored, and large at 0.25 in (6.35 mm) across.[1] Uranium is also present.[2]

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.[3]

Age

Half Dome Granodiorite traces to early Late Cretaceous. Its age is between 85 and 83.4 (+/-1 to 2%) Ma, with average age of 84.1 Ma. It is younger than Sentinel granodiorite (88.4 Ma), and older than Cathedral Peak granite (83.7 Ma).[4] Half Dome Granodiorite is the Valley's youngest plutonic rock.[5]

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.[5]

See also

References
  1. Glazner, Allen F; Stock, Greg M (2010). Geology Underfoot in Yosemite. Mountain Press. p. 50. ISBN 978-0-87842-568-6.
  2. Dunham, Sarah E; Lillie, Robert J (2009). "Interpreting Geology in Yosemite National Park: A Monument to Strong Granite, Powerful Glaciers, and the Perseverance of Life" (PDF). Retrieved 2017-04-29.
  3. Solgadi, F; Sawyer, E. W (2008). "Formation of Igneous Layering in Granodiorite by Gravity Flow: a Field, Microstructure and Geochemical Study of the Tuolumne Intrusive Suite at Sawmill Canyon, California". Journal of Petrology. 49 (11): 2009. Bibcode:2008JPet...49.2009S. doi:10.1093/petrology/egn056.
  4. Evernden, J.F.; Curtis, G.H.; Lipson, J. (1957). "Geologic Unit: Half Dome". Retrieved 7 May 2016.
  5. Public Domain This article incorporates public domain material from Huber, N. King (1987). The Geologic Story of Yosemite National Park. United States Geological Survey. Bulletin 1595. Retrieved 9 May 2016.


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