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Crystal, Colorado
Crystal (also known as Crystal City) is a ghost town on the upper Crystal River in Gunnison County, Colorado, United States. It is located in the Elk Mountains along a four-wheel-drive road east of Marble and northwest of Crested Butte. Crystal was a mining camp established in 1881 and after several decades of robust existence, was all but abandoned by 1917. Many buildings still stand in Crystal, but its few residents live there only in the summer. History In 1874, geologist Sylvester Richardson discovered promising deposits of silver near the confluence of the North Fork and South Fork of the Crystal River in Gunnison County. In the years that followed, the aboriginal Ute people were removed from the area and prospectors began mining operations, creating a new mining camp in 1880. A year later, on August 6, 1881, the Gunnison County court held a session and voted for the incorporation of Crystal City, made official as of June 8, 1881. At the height of its prosperity in the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ghost Town
Ghost Town(s) or Ghosttown may refer to: * Ghost town, a town that has been abandoned Film and television * Ghost Town (1936 film), ''Ghost Town'' (1936 film), an American Western film by Harry L. Fraser * Ghost Town (1956 film), ''Ghost Town'' (1956 film), an American Western film by Allen H. Miner * Ghost Town (1988 film), ''Ghost Town'' (1988 film), an American horror film by Richard McCarthy (as Richard Governor) * Ghost Town (2008 film), ''Ghost Town'' (2008 film), an American fantasy comedy film by David Koepp * ''Ghost Town'', a 2008 TV film featuring Billy Drago * ''Derek Acorah's Ghost Towns'', a 2005–2006 British paranormal reality television series * Ghost Town (CSI: Crime Scene Investigation), "Ghost Town" (''CSI: Crime Scene Investigation''), a 2009 TV episode Literature * Ghost Town (Lucky Luke), ''Ghost Town'' (''Lucky Luke'') or ''La Ville fantôme'', a 1965 ''Lucky Luke'' comic *''Ghost Town'', a Beacon Street Girls novel by Annie Bryant *''Ghost Town'', a 199 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cue Sports
Cue sports are a wide variety of games of skill played with a cue, which is used to strike billiard balls and thereby cause them to move around a cloth-covered table bounded by elastic bumpers known as . There are three major subdivisions of games within cue sports: *Carom billiards, played on tables without , typically 10 feet in length, including straight rail, balkline, one-cushion carom, three-cushion billiards, artistic billiards, and four-ball *Pool, played on six-pocket tables of 7-, 8-, 9-, or 10-foot length, including among others eight-ball (the world's most widely played cue sport), nine-ball (the dominant professional game), ten-ball, straight pool (the formerly dominant pro game), one-pocket, and bank pool *Snooker, English billiards, and Russian pyramid, played on a large, six-pocket table (dimensions just under 12 ft by 6 ft), all of which are classified separately from pool based on distinct development histories, player culture, rules, and termi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sandstone
Sandstone is a clastic sedimentary rock composed mainly of sand-sized (0.0625 to 2 mm) silicate grains. Sandstones comprise about 20–25% of all sedimentary rocks. Most sandstone is composed of quartz or feldspar (both silicates) because they are the most resistant minerals to weathering processes at the Earth's surface. Like uncemented sand, sandstone may be any color due to impurities within the minerals, but the most common colors are tan, brown, yellow, red, grey, pink, white, and black. Since sandstone beds often form highly visible cliffs and other topographic features, certain colors of sandstone have been strongly identified with certain regions. Rock formations that are primarily composed of sandstone usually allow the percolation of water and other fluids and are porous enough to store large quantities, making them valuable aquifers and petroleum reservoirs. Quartz-bearing sandstone can be changed into quartzite through metamorphism, usually related to ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Maroon Bells–Snowmass Wilderness
The Maroon Bells–Snowmass Wilderness is a U.S. Wilderness Area located in the Elk Mountains (Colorado), Elk Mountains of central Colorado. The wilderness was established in 1980 in the Gunnison National Forest, Gunnison and White River National Forest, White River national forests. Within its boundaries are of trails, six of Colorado's fourteeners and nine passes over . The wilderness is named after the two peaks known as the Maroon Bells, and the Snowmass Mountain. References Wilderness areas of Colorado Protected areas of Pitkin County, Colorado Protected areas of Gunnison County, Colorado Protected areas established in 1980 Gunnison National Forest White River National Forest 1980 establishments in Colorado {{Colorado-protected-area-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Igneous Rock
Igneous rock (derived from the Latin word ''ignis'' meaning fire), or magmatic rock, is one of the three main The three types of rocks, rock types, the others being Sedimentary rock, sedimentary and metamorphic rock, metamorphic. Igneous rock is formed through the cooling and solidification of magma or lava. The magma can be derived from Partial melting, partial melts of existing rocks in either a Terrestrial planet, planet's mantle (geology), mantle or crust (geology), crust. Typically, the melting is caused by one or more of three processes: an increase in temperature, a decrease in pressure, or a change in composition. Solidification into rock occurs either below the surface as intrusive rocks or on the surface as extrusive (geology), extrusive rocks. Igneous rock may form with crystallization to form granular, crystalline rocks, or without crystallization to form Volcanic glass, natural glasses. Igneous rocks occur in a wide range of geological settings: shields, platforms ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Limestone
Limestone ( calcium carbonate ) is a type of carbonate sedimentary rock which is the main source of the material lime. It is composed mostly of the minerals calcite and aragonite, which are different crystal forms of . Limestone forms when these minerals precipitate out of water containing dissolved calcium. This can take place through both biological and nonbiological processes, though biological processes, such as the accumulation of corals and shells in the sea, have likely been more important for the last 540 million years. Limestone often contains fossils which provide scientists with information on ancient environments and on the evolution of life. About 20% to 25% of sedimentary rock is carbonate rock, and most of this is limestone. The remaining carbonate rock is mostly dolomite, a closely related rock, which contains a high percentage of the mineral dolomite, . ''Magnesian limestone'' is an obsolete and poorly-defined term used variously for dolomite, for limes ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Shale
Shale is a fine-grained, clastic sedimentary rock formed from mud that is a mix of flakes of clay minerals (hydrous aluminium phyllosilicates, e.g. kaolin, Al2 Si2 O5( OH)4) and tiny fragments (silt-sized particles) of other minerals, especially quartz and calcite.Blatt, Harvey and Robert J. Tracy (1996) ''Petrology: Igneous, Sedimentary and Metamorphic'', 2nd ed., Freeman, pp. 281–292 Shale is characterized by its tendency to split into thin layers ( laminae) less than one centimeter in thickness. This property is called '' fissility''. Shale is the most common sedimentary rock. The term ''shale'' is sometimes applied more broadly, as essentially a synonym for mudrock, rather than in the more narrow sense of clay-rich fissile mudrock. Texture Shale typically exhibits varying degrees of fissility. Because of the parallel orientation of clay mineral flakes in shale, it breaks into thin layers, often splintery and usually parallel to the otherwise indistinguishable beddin ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sedimentary Rock
Sedimentary rocks are types of rock that are formed by the accumulation or deposition of mineral or organic particles at Earth's surface, followed by cementation. Sedimentation is the collective name for processes that cause these particles to settle in place. The particles that form a sedimentary rock are called sediment, and may be composed of geological detritus (minerals) or biological detritus (organic matter). The geological detritus originated from weathering and erosion of existing rocks, or from the solidification of molten lava blobs erupted by volcanoes. The geological detritus is transported to the place of deposition by water, wind, ice or mass movement, which are called agents of denudation. Biological detritus was formed by bodies and parts (mainly shells) of dead aquatic organisms, as well as their fecal mass, suspended in water and slowly piling up on the floor of water bodies (marine snow). Sedimentation may also occur as dissolved minerals precipitate from ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Aspen, Colorado
Aspen is a home rule municipality that is the county seat and the most populous municipality of Pitkin County, Colorado, United States. The city population was 7,004 at the 2020 United States Census. Aspen is in a remote area of the Rocky Mountains' Sawatch Range and Elk Mountains, along the Roaring Fork River at an elevation just below above sea level on the Western Slope, west of the Continental Divide. Aspen is now a part of the Glenwood Springs, CO Micropolitan Statistical Area. Founded as a mining camp during the Colorado Silver Boom and later named Aspen for the abundance of aspen trees in the area, the city boomed during the 1880s, its first decade. The boom ended when the Panic of 1893 led to a collapse of the silver market. For the next half-century, known as "the quiet years", the population steadily declined, reaching a nadir of fewer than 1000 by 1930. Aspen's fortunes recovered in the mid-20th century when neighboring Aspen Mountain was developed into a ski ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Panic Of 1893
The Panic of 1893 was an economic depression in the United States that began in 1893 and ended in 1897. It deeply affected every sector of the economy, and produced political upheaval that led to the political realignment of 1896 and the presidency of William McKinley. Causes The Panic of 1893 has been traced to many causes, one of those points to Argentina; investment was encouraged by the Argentine agent bank, Baring Brothers. However, the 1890 wheat crop failure and a failed coup in Buenos Aires ended further investments. In addition, speculations in South African and Australian properties also collapsed. Because European investors were concerned that these problems might spread, they started a run on gold in the U.S. Treasury. Specie was considered more valuable than paper money; when people were uncertain about the future, they hoarded specie and rejected paper notes.Nelson, Scott Reynolds. 2012. A Nation of Deadbeats. New York: Alfred Knopf, p. 189. During the Gi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mule
The mule is a domestic equine hybrid between a donkey and a horse. It is the offspring of a male donkey (a jack) and a female horse (a mare). The horse and the donkey are different species, with different numbers of chromosomes; of the two possible first-generation hybrids between them, the mule is easier to obtain and more common than the hinny, which is the offspring of a female donkey (a jenny) and a male horse (a stallion). Mules vary widely in size, and may be of any color. They are more patient, hardier and longer-lived than horses, and are perceived as less obstinate and more intelligent than donkeys. Terminology A female mule that has oestrus cycles, and which could thus in theory carry a foetus, is called a "molly" or "Molly mule", though the term is sometimes used to refer to female mules in general. A male mule is properly called a "horse mule", though often called a "john mule", which is the correct term for a gelded mule. A young male mule is called a "mule co ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Carbondale, Colorado
The Town of Carbondale is a home rule municipality located in Garfield County, Colorado, United States. The town population was 6,434 at the 2020 United States Census. Carbondale is a part of the Glenwood Springs, CO Micropolitan Statistical Area. The town is located in the Roaring Fork Valley, downstream from Aspen and upstream from the mouth of the Roaring Fork River at Glenwood Springs. The town proper sits on the south bank of the river, at the confluence of the Crystal River. Carbondale's horizon is dominated by the 12,953 ft (3,952 m) tall Mount Sopris several miles to the south of town. It also boasts a rodeo, the Carbondale Wild West Rodeo, held every Thursday night, 7:30-9:00 pm, from June 3rd-August 19th. Everything from bronc riding to a calf scramble is there, with events such as hide racing and ribbon roping falling into the schedule. History Carbondale takes its name from Carbondale, Pennsylvania, hometown of some of Carbondale's early settlers. Carbondale ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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