Talc City Hills
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Talc City Hills
The Talc City Hills is a mountain range in the northern Mojave Desert, in Inyo County, California. They are just north of California State Route 190 west of Panamint Springs and east of Owens Lake, southeast of the Inyo Mountains, and north of the Coso Range The Coso Range of eastern California is located immediately south of Owens Lake, east of the Sierra Nevada, and west of the Argus Range. The southern part of the range lies in the restricted Naval Air Weapons Station China Lake and the northern pa .... See also * Hidden Valley Dolomite Formation * Lost Burro Formation References Mountain ranges of Inyo County, California Mountain ranges of the Mojave Desert Hills of California {{InyoCountyCA-geo-stub ...
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Inyo County, California
Inyo County () is a county in the eastern central part of the U.S. state of California, located between the Sierra Nevada and the state of Nevada. In the 2020 census, the population was 19,016. The county seat is Independence. Inyo County is on the east side of the Sierra Nevada and southeast of Yosemite National Park in Central California. It contains the Owens River Valley; it is flanked to the west by the Sierra Nevada and to the east by the White Mountains and the Inyo Mountains. With an area of 10,192 square miles (26,397 km2), Inyo County is the second-largest county by area in California, after San Bernardino County. Almost one-half of that area is within Death Valley National Park. However, with a population density of 1.8 people per square mile, it also has the second-lowest population density in California, after Alpine County. History Present-day Inyo county has been the historic homeland for thousands of years of the Mono, Timbisha, Kawaiisu, and Nort ...
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USGS
The United States Geological Survey (USGS), formerly simply known as the Geological Survey, is a scientific agency of the United States government. The scientists of the USGS study the landscape of the United States, its natural resources, and the natural hazards that threaten it. The organization's work spans the disciplines of biology, geography, geology, and hydrology. The USGS is a fact-finding research organization with no regulatory responsibility. The agency was founded on March 3, 1879. The USGS is a bureau of the United States Department of the Interior; it is that department's sole scientific agency. The USGS employs approximately 8,670 people and is headquartered in Reston, Virginia. The USGS also has major offices near Lakewood, Colorado, at the Denver Federal Center, and Menlo Park, California. The current motto of the USGS, in use since August 1997, is "science for a changing world". The agency's previous slogan, adopted on the occasion of its hundredth anniv ...
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Mojave Desert
The Mojave Desert ( ; mov, Hayikwiir Mat'aar; es, Desierto de Mojave) is a desert in the rain shadow of the Sierra Nevada mountains in the Southwestern United States. It is named for the indigenous Mojave people. It is located primarily in southeastern California and southwestern Nevada, with small portions extending into Arizona and Utah. The Mojave Desert, together with the Sonoran, Chihuahuan, and Great Basin deserts, forms a larger North American Desert. Of these, the Mojave is the smallest and driest. The Mojave Desert displays typical basin and range topography, generally having a pattern of a series of parallel mountain ranges and valleys. It is also the site of Death Valley, which is the lowest elevation in North America. The Mojave Desert is often colloquially called the "high desert", as most of it lies between . It supports a diversity of flora and fauna. The desert supports a number of human activities, including recreation, ranching, and military training. ...
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California
California is a U.S. state, state in the Western United States, located along the West Coast of the United States, Pacific Coast. With nearly 39.2million residents across a total area of approximately , it is the List of states and territories of the United States by population, most populous U.S. state and the List of U.S. states and territories by area, 3rd largest by area. It is also the most populated Administrative division, subnational entity in North America and the 34th most populous in the world. The Greater Los Angeles area and the San Francisco Bay Area are the nation's second and fifth most populous Statistical area (United States), urban regions respectively, with the former having more than 18.7million residents and the latter having over 9.6million. Sacramento, California, Sacramento is the state's capital, while Los Angeles is the List of largest California cities by population, most populous city in the state and the List of United States cities by population, ...
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California State Route 190
State Route 190 (SR 190) is a state highway in the U.S. state of California that is split into two parts by the Sierra Nevada. The western portion begins at Tipton at a junction with State Route 99 and heads east towards Porterville before ending at Quaking Aspen in the Sequoia National Forest. The eastern portion begins at US 395 at Olancha, heads east through Death Valley National Park, and ends at State Route 127 at Death Valley Junction. The 43.0-mileCalifornia Department of TransportationTraversible Highways Report 2002 ic accessed January 2008 (69.2 km) portion over the Sierra Nevada remains unconstructed, and the California Department of Transportation (Caltrans) has no plans to build it through the wilderness areas. SR 190 is a National Scenic Byway known as the Death Valley Scenic Byway. Route description State Route 190 begins at State Route 99 just south of downtown Tipton in Tulare County and heads straight east along the flat San Joaquin Valley on Avenue 14 ...
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Panamint Springs, California
Panamint Springs is private resort in Inyo County, California. It consists of a motel, cabins, RV and tent campsites, restaurant, and gas station, all operated by Cassell Enterprises, LLC. It lies at an elevation of 1926 feet (587 m). Location Panamint Springs Resort is located along State Route 190 (SR190) between Old Toll Road and Panamint Valley Road. The closest store and gas station to Star Wars Canyon, the site features a motel, campground, restaurant, and the last gas station for many miles in either direction on SR190. Although not official by the Board of Geographic Names, Caltrans calls the SR190/Panamint Valley Road intersection 2.5 driving miles east of Panamint Springs Panamint Junction. Towne Pass, a landmark when traveling to Death Valley, is 13.9 driving miles east on SR190. Beyond the pass, SR190 descends about to the dry bed of Lake Manly. The Darwin Falls Wilderness, a U.S. Wilderness Area, is located just west of the resort. The nearby area also features t ...
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Owens Lake
Owens Lake is a mostly dry lake in the Owens Valley on the eastern side of the Sierra Nevada in Inyo County, California. It is about south of Lone Pine, California. Unlike most dry lakes in the Basin and Range Province that have been dry for thousands of years, Owens held significant water until 1913, when much of the Owens River was diverted into the Los Angeles Aqueduct, causing Owens Lake to desiccate by 1926. A 2004 court order required the LADWP to reestablish a small flow from the river into the lake. Nevertheless, as of 2013, it is the largest single source of dust pollution in the United States. History Owens Lake was given its present name by the explorer John C. Frémont, in honor of one of his guides, Richard Owens. Owens himself never set foot in the valley. The lake's original name, given by the ''Nüümü'' (Owens Valley Paiute), is ''Patsiata''. Before the diversion of the Owens River, Owens Lake was up to long and wide, covering an area of up to . In the ...
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Inyo Mountains
The Inyo Mountains are a short mountain range east of the Sierra Nevada in eastern California in the United States. The range separates the Owens Valley to the west from Saline Valley to the east, extending for approximately south-southeast from the southern end of the White Mountains, from which they are separated by Westgard Pass, to the east of Owens Lake. Geologically, the mountains are a fault block range in the Basin and Range Province, at the western end of the Great Basin. They are considered to be among the most important and best-known Late Proterozoic to Cambrian sections in the United States. Wilderness Most of the mountain range () is designated as the Inyo Mountain Wilderness, managed by the Bureau of Land Management in the south and the United States Forest Service in the north. The USFS manages of the wilderness all within Inyo National Forest. Wildlife in the area includes the endangered Inyo Mountains salamander and the desert bighorn sheep. Plant co ...
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Coso Range
The Coso Range of eastern California is located immediately south of Owens Lake, east of the Sierra Nevada, and west of the Argus Range. The southern part of the range lies in the restricted Naval Air Weapons Station China Lake and the northern part of the range is designated as the Coso Range Wilderness. The mountains include Coso Peak, at above sea level, as well as Silver Peak and Silver Mountain, both more than in height. The range is underlain principally by Mesozoic granitic rocks that are partly veneered by upper Cenozoic volcanic rocks of the Coso Volcanic Field. The volcanic units (in apparent decreasing age) include (1) widespread basaltic flows, (2) dacitic flows and tuff, and (3) rhyolitic domes and flows and basaltic cones and flows. These volcanic rocks are encompassed by an oval-shaped zone of late Cenozoic ring faulting that measures about east to west and north to south and that defines a structural basin. Most of the Coso Range and a slice of the adjacent ...
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Hidden Valley Dolomite
The Hidden Valley Dolomite is a Silurian−Devonian geologic formation in the northern Mojave Desert of California, in the western United States. Locations where it is exposed include sections of the southern Inyo Mountains and the Talc City Hills. Hidden Valley Dolomite overlies the Ely Springs Dolomite formation, and underlies the Lost Burro Formation. Paleontology Outcrops of the Hidden Valley Dolomite formation's ''Lippincott Member'' in Death Valley National Park have produced fossils of the fishes '' Panamintaspis snowi'' and '' Blieckaspis priscillae'' along with the remains of other jawless fishes Agnatha (, Ancient Greek 'without jaws') is an infraphylum of jawless fish in the phylum Chordata, subphylum Vertebrata, consisting of both present (cyclostomes) and extinct ( conodonts and ostracoderms) species. Among recent animals, cyclosto ... and a small arthrodire placoderm."Death Valley National Park," Hunt, Santucci, and Kenworthy (2006); page 63.Hunt, ReBe ...
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Lost Burro Formation
The Lost Burro Formation is a Middle to Upper/Late Devonian geologic formation in the Mojave Desert of California in the Western United States. Geology The Dolomite formation is exposed in sections of the Darwin Hills, the Santa Rosa Hills, the Talc City Hills, the Inyo Mountains near the Cerro Gordo Mines, the Panamint Range near Towne Pass, and the Argus Range. Fossils Outcrops of the formation in Death Valley National Park have produced fossils of the placoderm ''Dunkleosteus terrelli'', a small cladodont shark, the crushing tooth of a cochliodont, and the pteraspidid Pteraspididae is an extinct family of heterostracan vertebrates. It is an Early Devonian-aged family that contains the stereotypical, torpedo-shaped pteraspidids, such as the type genus, ''Pteraspis'', and its close relatives '' Errivaspis'' and ... '' Blieckaspis priscillae''."Death Valley National Park," Hunt, Santucci, and Kenworthy (2006); page 63. Hunt, ReBecca K., Vincent L. Santucci and Jason ...
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Mountain Ranges Of Inyo County, California
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited Summit (topography), summit area, and is usually higher than a hill, typically rising at least 300 metres (1,000 feet) above the surrounding land. A few mountains are Monadnock, isolated summits, but most occur in mountain ranges. Mountain formation, Mountains are formed through Tectonic plate, tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through Slump (geology), slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce Alpine climate, colder climates than at sea level at similar latitude. These colder climates strongly affect the Montane ecosystems, ecosys ...
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