Half Dome Granodiorite

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Half Dome Granodiorite
Stratigraphic range: early Late Cretaceous 85–83.4  Ma
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Half dome granodiorite.jpg
Type Geological formation
Lithology
Primary Granodiorite
Location
Region Yosemite National Park
CountryUnited States
Type section
Named for Half Dome
Map of Cathedral Peak Granodiorite.svg
A geologic map of Yosemite National Park

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.

Contents

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

Related Research Articles

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<span class="mw-page-title-main">Lamprophyre</span> Ultrapotassic igneous rocks

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<span class="mw-page-title-main">Geography of the Yosemite area</span>

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Kuna Crest Granodiorite, is found, in Yosemite National Park, United States. The granodiorite forms part of the Tuolumne Intrusive Suite, one of the four major intrusive suites within the Sierra Nevada. Of the Tuolumne Intrusive Suite, it is the oldest and darkest rock.

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Sentinel granodiorite is a type of granodiorite found in Yosemite National Park. It is a poorly understood western "outlier" of the ~93-85-Ma Tuolumne Intrusive Suite of the Sierra Nevada batholith. It is only slightly older than the undated Yosemite Creek Granodiorite and the Kuna Crest Granodiorite.

<span class="mw-page-title-main">Tuolumne Intrusive Suite</span> One of several intrusive suites in Yosemite National Park

The Tuolumne Intrusive Suite is the youngest and most extensive of the intrusive suites of Yosemite National Park, and also comprises about 1/3 of the park's area. The Suite includes Half Dome Granodiorite, Cathedral Peak Granite, and Kuna Crest Granodiorite.

<span class="mw-page-title-main">Intrusive Suite of Buena Vista Crest</span> One of several intrusive suites in Yosemite National Park

The Intrusive Suite of Buena Vista Crest is an intrusive suite which extends 30 kilometres (19 mi) southward, from Yosemite Valley to Yosemite National Park's southeastern boundary, into plutons of the Sierra Nevada Batholith, which are slightly older. These intrusive suites also include

  1. Fine Gold Intrusive Suite
  2. Intrusive Suite of Jack Main Canyon
  3. Intrusive Suite of Merced Peak
  4. Intrusive Suite of Sonora Pass
  5. Intrusive Suite of Yosemite Valley
  6. Tuolumne Intrusive Suite
<span class="mw-page-title-main">Intrusive Suite of Sonora Pass</span> Intrusive Suite of Sonora Pass is one of several intrusive suites in Yosemite National Park

The Intrusive Suite of Sonora Pass is one of several intrusive suites in Yosemite National Park. These also include

  1. Fine Gold Intrusive Suite
  2. Intrusive Suite of Buena Vista Crest
  3. Intrusive Suite of Jack Main Canyon
  4. Intrusive Suite of Merced Peak
  5. Intrusive Suite of Yosemite Valley
  6. Tuolumne Intrusive Suite
<span class="mw-page-title-main">Mammoth Peak</span> Mountain in Yosemite National Park

Mammoth Peak is a mountain in the area of Tuolumne Meadows, Yosemite National Park, California. The summit is a class 1-2 cross-country hike that features river crossings and boulder scrambling. The peak lies at the northern end of the Kuna Crest and is close to California State Route 120. From the road, its summit appears rounded and quite rocky. Though Mammoth Peak is not as popular as other nearby peaks, its relatively easily accessed summit affords tremendous views of Mount Gibbs, Mount Dana, and Mount Lewis.

<span class="mw-page-title-main">Kuna Crest</span> Mountain range near Tuolumne Meadows, in Yosemite National Park, California

Kuna Crest is a mountain range near Tuolumne Meadows, in Yosemite National Park, California.

Johnson Granite Porphyry is found in Tuolumne Meadows, Yosemite National Park.

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. 1 2 PD-icon.svg 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.