Search results
Results From The WOW.Com Content Network
The oldest rocks in Nevada are in the East Humboldt Range in the northeast, with lead isotope data suggesting an age of 2.5 billion years, at the boundary of the Archean and Proterozoic. Metamorphic and igneous rocks formed 1.7 billion years ago underlie Clark County and the populous areas around Las Vegas.
The Ashe Metamorphic Suite is located in the Eastern Blue Ridge providence that extends from North Carolina up to South-Western Virginia. It is a collection of metamorphic rocks of both sedimentary and volcanic origin. Zircon dating indicates an age of 470 to 335 Ma for the unit. [2] The protolith of the Ashe Metamorphic Suite was deposited ...
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 ...
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. The range reaches a maximum elevation of 13,065 feet (3,982 m) at the summit of Wheeler Peak ...
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 to 200 °C (300 to 400 °F) and, often, elevated pressure of 100 megapascals (1,000 bar ) or more, causing profound physical or chemical changes.
In the southern part of the Western Belt the rocks have undergone folding as the main type of deformation. [1] The Western Belt is generally separated from the Central Belt by the Melones fault zone which also distinguishes between the metamorphic rocks of the Western and Central Belts of the Sierra Nevada. [1]
Grenville orogeny. The Grenville orogeny was a long-lived Mesoproterozoic mountain-building event associated with the assembly of the supercontinent Rodinia. Its record is a prominent orogenic belt which spans a significant portion of the North American continent, from Labrador to Mexico, as well as to Scotland.
Type of rock. batholith and igneous. The Sierra Nevada (/ siˌɛrə nɪˈvædə, - ˈvɑːd -/ see-ERR-ə nih-VA (H)D-ə) [6][a] is a mountain range in the Western United States, between the Central Valley of California and the Great Basin. The vast majority of the range lies in the state of California, although the Carson Range spur lies ...