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Fish Lake Valley
The Fish Lake Valley is a longNevada, DeLorme Atlas & Gazetteer, c 2010, p. 58-59. endorheic valley in southwest Nevada, one of many contiguous inward-draining basins collectively called the Great Basin. The alluvial valley lies just northwest of Death Valley and borders the southeast, and central-northeast flank of the massif of the White Mountains of California. The southwestern portion of the valley lies in California, with the southern tip at the edge of Inyo County east of the Chocolate Mountains, and a significant portion of the south end of the valley floor including the ranching community of Oasis, in Mono County. The valley is sparsely populated, primarily with ranchers and indigenous Paiute. The valley's Post Office and commercial services are located in the town of Dyer. Description Fish Lake Valley is a slightly southwest-northeast trending valley, in its northern and central section. It borders the White Mountains on the southwest and receives water from Cot ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Nevada
Nevada ( ; ) is a state in the Western region of the United States. It is bordered by Oregon to the northwest, Idaho to the northeast, California to the west, Arizona to the southeast, and Utah to the east. Nevada is the 7th-most extensive, the 32nd-most populous, and the 9th-least densely populated of the U.S. states. Nearly three-quarters of Nevada's people live in Clark County, which contains the Las Vegas–Paradise metropolitan area, including three of the state's four largest incorporated cities. Nevada's capital is Carson City. Las Vegas is the largest city in the state. Nevada is officially known as the "Silver State" because of the importance of silver to its history and economy. It is also known as the "Battle Born State" because it achieved statehood during the Civil War (the words "Battle Born" also appear on its state flag); as the " Sagebrush State", for the native plant of the same name; and as the " Sage-hen State". The name means "snowy" in Spanish, re ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Oasis, Mono County, California
Oasis is an unincorporated community in Mono County, California. It is located in Fish Lake Valley east-southeast of Mount Bancroft. Oasis is at the junction of California State Route 266 and California State Route 168 State Route 168 (SR 168) is an east-west state highway in the U.S. state of California that is separated into two distinct segments by the Sierra Nevada mountains. The western segment runs from State Routes 41 and 180 in Fresno east to Huntin .... The 2000 Census reports that Oasis had a population of 22.Mono County's government population report A post office operated at Oasis from 1873 to 1942. References [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Nevada Historical Markers ...
Nevada historical markers identify significant places of interest in Nevada's history. The Historic Marker Program was initiated by the Nevada State Legislature in 1967 to bring the state's heritage to the public's attention with on-site markers. Because of budget cuts the program became dormant in 2009. Notes {{reflist, 33em *Markers Nevada Historical markers *Historical markers Historical markers A commemorative plaque, or simply plaque, or in other places referred to as a historical marker, historic marker, or historic plaque, is a plate of metal, ceramic, stone, wood, or other material, typically attached to a wall, stone, or other ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fish Lake Hot Well
Fish Lake Hot Well, also known as Fish Lake Hot Spring and Fish Lake Valley Hot Well is a geothermal hot spring in Nevada. Location The spring is located in the Fish Lake Valley near the town of Dyer, Nevada. The White Mountains and the 13,146 foot high Boundary Peak are visible from the springs. The hot spring is surrounded by mountains, and the Boundary Peak Wilderness area is visible from the spring. History and description In the 1880s ranchers drilling for oil discovered the hot well. It was later surrounded by a well casing. Later a six-foot square concrete soaking area was added surrounded by a cement deck and wooden benches. The soaking pool over-flows into a man-made swimming hole that has been stocked with large goldfish. This warm pond flows into a second and third pond. All of the soaking pools/ponds are different temperatures, ranging from 85°F to 105°F. The main gravel-bottomed soaking pool is surrounded by a concrete deck and is 12' x 6'. The water then flows ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Coaldale, Nevada
Coaldale is a former mining town and true ghost town in Esmeralda County, Nevada, located at the junction of U.S. Route 6 and U.S. Route 95 about west of Tonopah. History Coal was discovered near Coaldale in 1894 by William Groszenger who sold 150 tons to the Columbus Marsh Borax works. In 1911, the Darms Mine and the Nevada Coal and Fuel Co. mines were in operation. Coal was found 4 miles SSE of Coaldale in the north end of the Silver Peak Range. In the early 1900s, there was renewed interest in the coal, when Dr. Frances Williams of Goldfield, Nevada personally restaked claims. At the time, Groezenger retained the majority of the claims. In November, 1917, the Darms Mining Company asked the Nevada Railroads Commission to secure a rate of $3/ton to deliver coal from Coaldale to Reno. The Tonopah and Goldfield Railroad replied that while they had grave doubts about the value of the coal, they offered two plans: 1) where one or two cars would be transported to Tonopah, Goldf ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Furnace Creek Fault Zone
The Furnace Creek Fault Zone (FCFZ) is a geological fault that is located in Eastern California and southwestern Nevada. The right lateral-moving (dextral) fault extends for some between a connection with the Death Valley Fault Zone in the Amargosa Valley and northward to a termination in the Fish Lake Valley of southwest Nevada. The northern segment of the FCFZ is also referred to as the Fish Lake Valley Fault Zone. The FCFZ is considered an integral part of the Walker Lane The Walker Lane is a geologic trough roughly aligned with the California/Nevada border southward to where Death Valley intersects the Garlock Fault, a major left lateral, or sinistral, strike-slip fault. The north-northwest end of the Walker L .... References Additional readingBaucke, W.; Cemen, I., ''Strike-Slip displacement along the Furnace Creek Fault Zone, southern Basins and Ranges, Death Valley, California,'' American Geophysical Union, Fall Meeting 2007, abstract #T31C-0594 Amargosa Dese ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Block Fault
Fault blocks are very large blocks of rock, sometimes hundreds of kilometres in extent, created by tectonic and localized stresses in Earth's crust. Large areas of bedrock are broken up into blocks by faults. Blocks are characterized by relatively uniform lithology. The largest of these fault blocks are called crustal blocks. Large crustal blocks broken off from tectonic plates are called terranes. Those terranes which are the full thickness of the lithosphere are called microplates. Continent-sized blocks are called variously ''microcontinents, continental ribbons, H-blocks, extensional allochthons and outer highs.'' Because most stresses relate to the tectonic activity of moving plates, most motion between blocks is horizontal, that is parallel to the Earth's crust by strike-slip faults. However vertical movement of blocks produces much more dramatic results. Landforms (mountains, hills, ridges, lakes, valleys, etc.) are sometimes formed when the faults have a large v ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Nevada State Route 264
State Route 264 (SR 264) is a state highway in Esmeralda County, Nevada, United States. It connects California State Route 266 to U.S. Route 6 (US 6) via the town of Dyer, Nevada. The majority of the route is known as Fish Lake Valley Road, with the northern portion referred to as the ''Dicalite Cutoff''. A majority of the route was originally designated State Route 3A. Route description SR 264 begins at the California State line approximately north of Oasis, California on California State Route 266. From there, the highway follows Fish Lake Valley Road north to pass through the small community of Dyer. As the route heads north from Dyer through Fish Lake Valley, Boundary Peak, the highest point in the state of Nevada, comes into view on the west side of the highway. About north of Dyer is a junction with State Route 773, where Fish Lake Valley Road turns off of the route. At this point, SR 264 curves northwest to follow the Dicalite Cutoff. The route reaches ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Alluvial Fan
An alluvial fan is an accumulation of sediments that fans outwards from a concentrated source of sediments, such as a narrow canyon emerging from an escarpment. They are characteristic of mountainous terrain in arid to semiarid climates, but are also found in more humid environments subject to intense rainfall and in areas of modern glaciation. They range in area from less than to almost . Alluvial fans typically form where flow emerges from a confined channel and is free to spread out and infiltrate the surface. This reduces the carrying capacity of the flow and results in deposition of sediments. The flow can take the form of infrequent debris flows or one or more ephemeral or perennial streams. Alluvial fans are common in the geologic record, such as in the Triassic basins of eastern North America and the New Red Sandstone of south Devon. Such fan deposits likely contain the largest accumulations of gravel in the geologic record. Alluvial fans have also been found on Mar ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dry Lake
A dry lake bed, also known as a playa, is a basin or depression that formerly contained a standing surface water body, which disappears when evaporation processes exceeds recharge. If the floor of a dry lake is covered by deposits of alkaline compounds, it is known as an alkali flat. If covered with salt, it is known as a '' salt flat.'' Terminology If its basin is primarily salt, then a dry lake bed is called a '' salt pan'', ''pan'', or ''salt flat'' (the latter being a remnant of a salt lake). ''Hardpan'' is the dry terminus of an internally drained basin in a dry climate, a designation typically used in the Great Basin of the western United States. Another term for dry lake bed is ''playa''. The Spanish word ''playa'' () literally means "beach". Dry lakes are known by this name in some parts of Mexico and the western United States. This term is used e.g. on the Llano Estacado and other parts of the Southern High Plains and is commonly used to address paleolake sediment ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Borax
Borax is a salt ( ionic compound), a hydrated borate of sodium, with chemical formula often written . It is a colorless crystalline solid, that dissolves in water to make a basic solution. It is commonly available in powder or granular form, and has many industrial and household uses, including as a pesticide, as a metal soldering flux, as a component of glass, enamel, and pottery glazes, for tanning of skins and hides, for artificial aging of wood, as a preservative against wood fungus, and as a pharmaceutic alkalizer. In chemical laboratories, it is used as a buffering agent. The compound is often called sodium tetraborate decahydrate, but that name is not consistent with its structure. The anion is not tetraborate but tetrahydroxy tetraborate , so the more correct formula should be . Informally, the product is often called sodium borate decahydrate or just sodium borate. The terms tincal "tinkle" and tincar "tinker" refer to native borax, historically mine ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cottonwood Creek (Inyo County, California)
Cottonwood Creek originates in the Ancient Bristlecone Pine Forests of the White Mountains of eastern California. The creek flows eastward from below the alpine crest of the White Mountains and descends through groves of bristlecone pine, aspen and mountain mahogany, then a woodland of pinyon pine and juniper, and finally into sagebrush as the stream ends in endorheic Fish Lake Valley which is one of the contiguous collection of inward-draining basins that make up the Great Basin. Cottonwood Creek has no native fish, however its North Fork is a refuge for the threatened Paiute cutthroat trout, one of the rarest trout in North America. This subspecies was transplanted from its very limited native range, upper Silver King Creek in the Carson River basin. The remainder of the stream hosts (originally) transplanted brook, brown and rainbow A rainbow is a meteorological phenomenon that is caused by reflection, refraction and dispersion of light in water droplets resultin ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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