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Amargosa Range
The Amargosa Range is a mountain range in Inyo County, California and Nye County, Nevada. The range runs along most of the eastern side of California's Death Valley, separating it from Nevada's Amargosa Desert. The U-shaped Amargosa River flows clockwise around the perimeter of the range, ending below sea level in the Badwater Basin. The mountain range is named after the Amargosa River, so-named for the Spanish word for bitter because of the bitter taste of the water. In order from north to south, the Grapevine Mountains (including the range's highest point, Grapevine Peak), the Funeral Mountains, and the Black Mountains form distinct sections. Many of Death Valley National Park's most well-known features, such as Zabriskie Point Zabriskie Point is a part of the Amargosa Range located east of Death Valley in Death Valley National Park in California, United States, noted for its erosional landscape. It is composed of sediments from Furnace Creek Lake, which dried up 5 ...
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Grapevine Peak (Nevada)
Grapevine Peak is the highest mountain in the Grapevine Mountains of Nye County in Nevada, United States. It is the fourth-most topographically prominent peak in Nye County and ranks seventeenth among the most topographically prominent peaks in Nevada. The peak is located within the boundaries of Death Valley National Park Death Valley National Park is an American national park that straddles the California–Nevada border, east of the Sierra Nevada. The park boundaries include Death Valley, the northern section of Panamint Valley, the southern section of Eure .... References Mountains of Nevada Mountains of Death Valley National Park Mountains of Nye County, Nevada {{NyeCountyNV-geo-stub ...
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Grapevine Mountains
The Grapevine Mountains are a mountain range located along the border of Inyo County, California and Nye County, Nevada in the United States. The mountain range is about long and lies in a northwest-southeasterly direction along the Nevada- California state line. The range reaches an elevation of at Grapevine Peak, near Phinney Canyon on the Nevada side. Daylight Pass is at the southern end of the range. Most of the Grapevine Mountain chain is in Death Valley National Park Death Valley National Park is an American national park that straddles the California–Nevada border, east of the Sierra Nevada. The park boundaries include Death Valley, the northern section of Panamint Valley, the southern section of Eure .... The range was named for the wild grapes in the area. References * See also * Mountain ranges of the Mojave Desert Mountain ranges of Esmeralda County, Nevada Mountain ranges of Nye County, Nevada Mountain ranges of Inyo County, California Death Vall ...
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Mountain Ranges Of Nevada
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 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 isolated summits, but most occur in mountain ranges. Mountains are formed through 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 slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable terrain a ...
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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 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 isolated summits, but most occur in mountain ranges. Mountains are formed through 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 slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable terrain and ...
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Mountain Ranges Of The Mojave Desert
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 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 isolated summits, but most occur in mountain ranges. Mountains are formed through 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 slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable ...
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Zabriskie Point
Zabriskie Point is a part of the Amargosa Range located east of Death Valley in Death Valley National Park in California, United States, noted for its erosional landscape. It is composed of sediments from Furnace Creek Lake, which dried up 5 million years ago—long before Death Valley came into existence. Name The location was named after Christian Brevoort Zabriskie, vice-president and general manager of the Pacific Coast Borax Company in the early 20th century. The company's twenty-mule teams were used to transport borax from its mining operations in Death Valley. History Millions of years prior to the actual sinking and widening of Death Valley and the existence of Lake Manly (see Geology of the Death Valley area), another lake covered a large portion of Death Valley including the area around Zabriskie Point. This ancient lake began forming approximately nine million years ago. During several million years of the lake's existence, sediments were collecting at the bot ...
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Death Valley National Park
Death Valley National Park is an American national park that straddles the California–Nevada border, east of the Sierra Nevada. The park boundaries include Death Valley, the northern section of Panamint Valley, the southern section of Eureka Valley and most of Saline Valley. The park occupies an interface zone between the arid Great Basin and Mojave deserts, protecting the northwest corner of the Mojave Desert and its diverse environment of salt-flats, sand dunes, badlands, valleys, canyons and mountains. Death Valley is the largest national park in the contiguous United States, as well as the hottest, driest and lowest of all the national parks in the United States. It contains Badwater Basin, the second-lowest point in the Western Hemisphere and lowest in North America at below sea level. More than 93% of the park is a designated wilderness area. The park is home to many species of plants and animals that have adapted to this harsh desert environment including creos ...
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Black Mountains (California)
The Black Mountains are a mountain range located in the southeastern part of Inyo County, California, within southeastern Death Valley National Park. Geography The Black Mountains are a southern range of the Amargosa Range System and lie in a generally north–south direction at their southwestern end. Their formation has been classified as the Amargosa Chaos. Lower Death Valley lies to the west & southwest of the Black Mountains section, with Greenwater Valley and the Greenwater Range to the northeast. The Black Mountains and Greenwater Range abut the Funeral Mountains on the north, also at the southern terminus of the Amargosa Range. The Amargosa River turns south-southwest, around the three sub-ranges, then northwest into Death Valley. The Owlshead Mountains are to the south across the Amargosa River and its steep descent into Death Valley. ;Features The range reaches an elevation of above sea level at Funeral Peak. Dante's View and Coffin Peak lie at the northern end ...
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Funeral Mountains
The Funeral Mountains are a short, arid mountain range in the United States along the California-Nevada border approximately 100 mi (160 km) west of Las Vegas. The mountains are considered a subrange of the Amargosa Range that form the eastern wall of Death Valley. The crest of the range is within Death Valley National Park. The range is separated from the Grapevine Mountains to the northwest by the narrow Boundary Canyon''Beatty, Nevada–California,'' 30x60 Minute Topographic Quadrangle, USGS, 1986 and is separated from the Black Mountains by Furnace Creek Wash on the southwest and from the Greenwater Range at the narrow Travertine Point on the south. The broad flats of the Amargosa Desert lie across the border to the northeast in Nevada. The highest point in the range is Pyramid Peak, at 6703 ft (2043 m).''East of Echo Canyon, Calif.–Nev.,'' 7.5 Minute Topographic Quadrangle, USGS, 1987 The first movement of Ferde Grofé's ''Death Valley Suite The ''Deat ...
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Spanish Language
Spanish ( or , Castilian) is a Romance language of the Indo-European language family that evolved from colloquial Latin spoken on the Iberian peninsula. Today, it is a global language with more than 500 million native speakers, mainly in the Americas and Spain. Spanish is the official language of 20 countries. It is the world's second-most spoken native language after Mandarin Chinese; the world's fourth-most spoken language overall after English, Mandarin Chinese, and Hindustani (Hindi-Urdu); and the world's most widely spoken Romance language. The largest population of native speakers is in Mexico. Spanish is part of the Ibero-Romance group of languages, which evolved from several dialects of Vulgar Latin in Iberia after the collapse of the Western Roman Empire in the 5th century. The oldest Latin texts with traces of Spanish come from mid-northern Iberia in the 9th century, and the first systematic written use of the language happened in Toledo, a prominent city of ...
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Mountain Range
A mountain range or hill range is a series of mountains or hills arranged in a line and connected by high ground. A mountain system or mountain belt is a group of mountain ranges with similarity in form, structure, and alignment that have arisen from the same cause, usually an orogeny. Mountain ranges are formed by a variety of geological processes, but most of the significant ones on Earth are the result of plate tectonics. Mountain ranges are also found on many planetary mass objects in the Solar System and are likely a feature of most terrestrial planets. Mountain ranges are usually segmented by highlands or mountain passes and valleys. Individual mountains within the same mountain range do not necessarily have the same geologic structure or petrology. They may be a mix of different orogenic expressions and terranes, for example thrust sheets, uplifted blocks, fold mountains, and volcanic landforms resulting in a variety of rock types. Major ranges Most ge ...
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Badwater Basin
Badwater Basin is an endorheic basin in Death Valley National Park, Death Valley, Inyo County, California, noted as the lowest point in North America and the United States, with a depth of below sea level. Mount Whitney, the highest point in the contiguous United States, is only to the northwest. The site itself consists of a small spring-fed pool of "bad water" next to the road in a sink; the accumulated salts of the surrounding basin make it undrinkable, thus giving it the name. The pool does have animal and plant life, including pickleweed, aquatic insects, and the Badwater snail. Adjacent to the pool, where water is not always present at the surface, repeated freeze–thaw and evaporation cycles gradually push the thin salt crust into hexagonal honeycomb shapes. The pool is not the lowest point of the basin: the lowest point (which is only slightly lower) is several miles to the west and varies in position, depending on rainfall and evaporation patterns. The sa ...
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