Intrusive Suite of Yosemite Valley

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The Intrusive Suite of Yosemite Valley is indicated in yellow Map of Yosemite National Park.svg
The Intrusive Suite of Yosemite Valley is indicated in yellow

The Intrusive Suite of Yosemite Valley (see Yosemite Valley) 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 Sonora Pass
  6. Tuolumne Intrusive Suite
  7. Johnson Granite Porphyry

It is an intrusive suite composed mainly of granitic rocks, which near the metasedimentary pendant have locally mingled with granitic to gabbroic compositions. [1]

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<span class="mw-page-title-main">Yosemite National Park</span> National park in California, United States

Yosemite National Park is a national park in California. It is bordered on the southeast by Sierra National Forest and on the northwest by Stanislaus National Forest. The park is managed by the National Park Service and covers 759,620 acres in four counties – centered in Tuolumne and Mariposa, extending north and east to Mono and south to Madera. Designated a World Heritage Site in 1984, Yosemite is internationally recognized for its cliffs, waterfalls, clear streams, giant sequoia groves, lakes, mountains, meadows, glaciers, and biological diversity. Almost 95 percent of the park is designated wilderness. Yosemite is one of the largest and least fragmented habitat blocks in the Sierra Nevada.

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

The exposed geology of the Yosemite area includes primarily granitic rocks with some older metamorphic rock. The first rocks were laid down in Precambrian times, when the area around Yosemite National Park was on the edge of a very young North American continent. The sediment that formed the area first settled in the waters of a shallow sea, and compressive forces from a subduction zone in the mid-Paleozoic fused the seabed rocks and sediments, appending them to the continent. Heat generated from the subduction created island arcs of volcanoes that were also thrust into the area of the park. In time, the igneous and sedimentary rocks of the area were later heavily metamorphosed.

<span class="mw-page-title-main">Cathedral Peak (California)</span>

Cathedral Peak is part of the Cathedral Range, a mountain range in the south-central portion of Yosemite National Park in eastern Mariposa and Tuolumne Counties. The range is an offshoot of the Sierra Nevada. The peak which lends its name to the range derives its name from its cathedral-shaped peak, which was formed by glacial activity: the peak remained uneroded above the glaciers in the Pleistocene.

<span class="mw-page-title-main">Sierra Nevada Batholith</span> Batholith in the Sierra Nevada mountain range, United States

The Sierra Nevada Batholith is a large batholith which forms the core of the Sierra Nevada mountain range in California, exposed at the surface as granite.

<span class="mw-page-title-main">Little Yosemite Valley</span> Valley in Mariposa County, California

Little Yosemite Valley is a smaller glacial valley upstream in the Merced River drainage from the Yosemite Valley in Yosemite National Park. The Merced River meanders through the 3.5 mi (5.6 km) long flat valley, draining out over Nevada Fall and Vernal Fall before emptying into the main Yosemite Valley. It can be reached by a day hike from the main valley, and is the most popular area in the Yosemite Wilderness. The Valley provides access to nearby destinations such as the back side of Half Dome, Clouds Rest and the High Sierra Camp at Merced Lake.

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

Yosemite National Park is located in the central Sierra Nevada of California. Three wilderness areas are adjacent to Yosemite: the Ansel Adams Wilderness to the southeast, the Hoover Wilderness to the northeast, and the Emigrant Wilderness to the north.

<span class="mw-page-title-main">Cathedral Peak Granodiorite</span> Suite of intrusive rock in the Sierra Nevada

The Cathedral Peak Granodiorite (CPG) was named after its type locality, Cathedral Peak in Yosemite National Park, California. The granodiorite forms part of the Tuolumne Intrusive Suite, one of the four major intrusive suites within the Sierra Nevada. It has been assigned radiometric ages between 88 and 87 million years and therefore reached its cooling stage in the Coniacian.

<span class="mw-page-title-main">Vishnu Basement Rocks</span> Lithostratigraphic unit in the Grand Canyon, Arizona

The Vishnu Basement Rocks is the name recommended for all Early Proterozoic crystalline rocks exposed in the Grand Canyon region. They form the crystalline basement rocks that underlie the Bass Limestone of the Unkar Group of the Grand Canyon Supergroup and the Tapeats Sandstone of the Tonto Group. These basement rocks have also been called either the Vishnu Complex or Vishnu Metamorphic Complex. These Early Proterozoic crystalline rocks consist of metamorphic rocks that are collectively known as the Granite Gorge Metamorphic Suite; sections of the Vishnu Basement Rocks contain Early Paleoproterozoic granite, granitic pegmatite, aplite, and granodiorite that have intruded these metamorphic rocks, and also, intrusive Early Paleoproterozoic ultramafic rocks.

<span class="mw-page-title-main">Half Dome Granodiorite</span> Half Dome Granodiorite is granodiorite (see also granite) found in Yosemite National Park

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.

<span class="mw-page-title-main">El Capitan Granite</span> El Capitan Granite is a type of granite (also see granodiorite), Yosemite National Park

El Capitan Granite is a type of granite, in a large area near El Capitan, in Yosemite National Park, California, United States. The granite forms part of the Tuolumne Intrusive Suite, one of the four major intrusive suites within the Sierra Nevada.

<span class="mw-page-title-main">Exfoliating granite</span> Granite skin peeling like an onion (desquamation) because of weathering

Exfoliating granite is a granite undergoing exfoliation, or onion skin weathering (desquamation). The external delaminated layers of granite are gradually produced by the cyclic variations of temperature at the surface of the rock in a process also called spalling. Frost and ice expansion in the joints during the winter accelerate the alteration process while the most unstable loosen external layers are removed by gravity assisted by runoff water.

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.

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">Intrusive suite</span>

An intrusive suite is a group of plutons related in time and space. All rocks in an intrusive suite result from the same magma-producing event.

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

The Tuolumne Intrusive Suite 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 Sonora Pass
  6. Intrusive Suite of Yosemite Valley
  7. Johnson Granite Porphyry
<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">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.

<span class="mw-page-title-main">Intrusive Suite of Merced Peak</span> Intrusive Suite of Merced Peak is an intrusive suite, of Yosemite National Park

The Intrusive Suite of Merced Peak 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 Sonora Pass
  5. Intrusive Suite of Yosemite Valley
  6. Tuolumne Intrusive Suite

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

References

  1. Memeti, Vali; Paterson, Scott R.; Economos, Rita; Erdmann, Saskia; Miller, Robert B. (2012). "Geology of the Benson Lake Pendant, Western Yosemite National Park, Central Sierra Nevada". geosociety.org. Retrieved 3 January 2019.