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  2. Geology of Nevada - Wikipedia

    en.wikipedia.org/wiki/Geology_of_Nevada

    Metamorphic and igneous rocks formed 1.7 billion years ago underlie Clark County and the populous areas around Las Vegas. The region was part of the supercontinent Rodinia one billion years ago, situated at the equator. The continent rifted apart between 700 and 600 million years ago. No continental rocks exist in western Nevada from more than ...

  3. Northern Snake Range metamorphic core complex - Wikipedia

    en.wikipedia.org/wiki/Northern_Snake_Range...

    The Northern Snake Range metamorphic core complex is a gently domed structure that forms the northern part of the Snake Range in Nevada. The metamorphic core complex consists of an upper plate of brittlely-faulted Cambrian to Permian mainly carbonate sedimentary rocks, unconformably overlain by Cenozoic volcanic and clastic rocks and separated ...

  4. Snake Range - Wikipedia

    en.wikipedia.org/wiki/Snake_Range

    Snake Range. /  38.98583°N 114.31389°W  / 38.98583; -114.31389. The Snake Range is a mountain range in White Pine County, Nevada, United States. [1] The south-central portion of the range is included within Great Basin National Park, with most of the remainder included within the Humboldt-Toiyabe National Forest.

  5. Geology of the Yosemite area - Wikipedia

    en.wikipedia.org/wiki/Geology_of_the_Yosemite_area

    These rocks were later metamorphosed and today can be seen in the gold-bearing metamorphic belt of California's Mother Lode country. In the area of the park these rocks are exposed along the Merced River and State Route 140. This was directly part of the creation of the Sierra Nevada Batholith, and the resulting rocks were mostly granitic in ...

  6. Sierra Nevada - Wikipedia

    en.wikipedia.org/wiki/Sierra_Nevada

    The earliest rocks in the Sierra Nevada are metamorphic roof pendants of Paleozoic age, the oldest being metasedimentary rocks from the Cambrian in the Mount Morrison region. These dark-colored hornfels , slates , marbles , and schists are found in the western foothills (notably around Coarsegold , west of the Tehachapi Pass ) and east of the ...

  7. Geology of the Death Valley area - Wikipedia

    en.wikipedia.org/wiki/Geology_of_the_Death...

    Early sedimentation Proterozoic complex. Little is known about the history of the oldest exposed rocks in the area due to extensive metamorphism.This somber, gray, almost featureless crystalline complex is composed of originally sedimentary and igneous rocks with large quantities of quartz and feldspar mixed in. The original rocks were transformed to contorted schist and gneiss, making their ...

  8. Rocky Mountains - Wikipedia

    en.wikipedia.org/wiki/Rocky_Mountains

    metamorphic. The Rocky Mountains, also known as the Rockies, are a major mountain range and the largest mountain system in North America. The Rocky Mountains stretch 3,000 miles (4,800 kilometers) [3] in straight-line distance from the northernmost part of western Canada, to New Mexico in the southwestern United States.

  9. Metamorphic rock - Wikipedia

    en.wikipedia.org/wiki/Metamorphic_rock

    Metamorphic rock. Quartzite, a type of metamorphic rock. Metamorphic rock, deformed during the Variscan orogeny, at Vall de Cardós, Lérida, Spain. Metamorphic rocks arise from the transformation of existing rock to new types of rock in a process called metamorphism. The original rock ( protolith) is subjected to temperatures greater than 150 ...