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Cumberland Caverns
Cumberland Caverns is a national natural landmark and show cave located in McMinnville, Tennessee. It is the second longest cave in Tennessee and makes the list of longest caves in the United States and in the world. History The main entrance was discovered by Aaron Higgenbotham in 1810 while he was surveying the nearby Chickamauga Trail on Cardwell Mountain in what is now Warren County. According to legend, Higgenbotham was the first man to enter the cave and it was named Higgenbotham Cave in his honor. Another smaller cave, also located on Cardwell Mountain, was also discovered about this time and was named Henshaw Cave. Although not nearly as big as Higgenbotham Cave, Henshaw Cave proved to be a source of saltpeter (the main ingredient of gunpowder) and was operated as a saltpeter mine during perhaps both the War of 1812 and the Civil War. Higgenbotham Cave became a favorite spot for local adventurers during the 19th century and groups would ride out to the entrance in hay ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
McMinnville, Tennessee
McMinnville is the largest city in and the county seat of Warren County, Tennessee, United States. The population was 13,605 at the 2010 census. It was named for Governor Joseph McMinn. Geography McMinnville is located at (35.686708, -85.779309), approximately south of Cookeville and northwest of Chattanooga. According to the United States Census Bureau, the city has a total area of , all land. McMinnville lies at an elevation of , as it sits along the Eastern Highland Rim near the base of the Cumberland Plateau. The city is drained primarily by the Barren Fork, a tributary of the Collins River. Nearby cities and towns Climate Demographics 2020 census As of the 2020 United States census, there were 13,788 people, 5,581 households, and 3,131 families residing in the city. 2000 census As of the census of 2000, there were 12,749 people, 5,419 households and 3,332 families residing in the city. The population density was 1,273.4 per square mile (491.7/km2). There were 5, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Gift Shop
A gift shop or souvenir shop is a store primarily selling souvenirs, memorabilia, and other items relating to a particular topic or theme. The items sold often include coffee mugs, stuffed animals, toys, t-shirts, postcards, handmade collections and other souvenirs, intended to be kept by the buyer as a memento of their visit, or given to another as a gift. Gift shops are normally found in areas visited by many tourists. Hotels and motels in Canada and the United States often feature a gift shop near their entrance. Venues such as zoos, aquariums, national parks, theme parks, and museums have their own gift shops as well; in some cases these shops sell items of higher value than gift shops not associated with a venue, as well as trinkets. These stores are sometimes a source of financial support for educational institutions. Mainstream businesses There are many mainstream shop businesses that target gift-buyers as their primary customer base. These retailers can vary in size ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cave Pearl
A cave pearl is a small, usually spherical, speleothem (cave formation) found in limestone caves. Cave pearls are formed by a concretion of calcium salts that form concentric layers around a nucleus. Exposure to moving water polishes the surface of cave pearls, making them glossy; if exposed to the air, cave pearls can degrade and appear rough. Composition A cave pearl is composed primarily of calcite (calcium carbonate aCO3. Cave pearls are generally not considered to be a type of oolite. Other minerals found in small quantities in cave pearls include quartz (silicon dioxide iO2, apatite (a group of phosphate minerals), iron, aluminum, and magnesium. Formation Cave pearls form when water dripping into a cave loses carbon dioxide and precipitates calcite. A cave pearl forms when the water is moving too vigorously to form a stalagmite. A nucleus of matter (such as a grain of sand) becomes coated with calcite, and the current then provides a rotation to the nucleus in such ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Flowstone
Flowstones are sheetlike deposits of calcite or other carbonate minerals, formed where water flows down the walls or along the floors of a cave. They are typically found in "solution caves", in limestone, where they are the most common speleothem. However, they may form in any type of cave where water enters that has picked up dissolved minerals. Flowstones are formed via the degassing of vadose percolation waters. Flowstone may also form on manmade structures as a result of calcium hydroxide being leached from concrete, lime or mortar. These secondary deposits created outside the cave environment, which mimic the shapes and forms of speleothems, are classified as "calthemites" and are associated with concrete degradation.Smith, G.K., (2016). “Calcite Straw Stalactites Growing From Concrete Structures”, Cave and Karst Science, Vol.43, No.1, P.4-10, (April 2016), British Cave Research Association, ISSN 1356-191X. Formation Flowing films of water that move along floors or do ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Helictite
A helictite is a speleothem (cave-formed mineral) found in a limestone cave that changes its axis from the vertical at one or more stages during its growth. Helictites have a curving or angular form that looks as if they were grown in zero gravity. They are most likely the result of capillary forces acting on tiny water droplets, a force often strong enough at this scale to defy gravity. Helictites are, perhaps, the most delicate of cave formations. They are usually made of needle-form calcite and aragonite. Helictite forms have been described in several types: ribbon helictites, saws, rods, butterflies, "hands", curly-fries, and "clumps of worms". They typically have radial symmetry. They can be easily crushed or broken by the slightest touch. Because of this, helictites are rarely seen within arm's reach in tourist caves. Timpanogos Cave National Monument in Utah has one of the largest collections of these formations in the world. Large numbers are also in the Jenolan Caves ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Stalactite
A stalactite (, ; from the Greek 'stalaktos' ('dripping') via ''stalassein'' ('to drip') is a mineral formation that hangs from the ceiling of caves, hot springs, or man-made structures such as bridges and mines. Any material that is soluble and that can be deposited as a colloid, or is in suspension, or is capable of being melted, may form a stalactite. Stalactites may be composed of lava, minerals, mud, peat, pitch, sand, sinter, and amberat (crystallized urine of pack rats). A stalactite is not necessarily a speleothem, though speleothems are the most common form of stalactite because of the abundance of limestone caves. The corresponding formation on the floor of the cave is known as a stalagmite. Mnemonics have been developed for which word refers to which type of formation; one is that ''stalactite'' has a C for "ceiling", and ''stalagmite'' has a G for "ground". Another example is that ''stalactites'' "hang on ''T''ight" and ''stalagmites'' "''M''ight grow up" ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Stalagmite
A stalagmite (, ; from the Greek , from , "dropping, trickling") is a type of rock formation that rises from the floor of a cave due to the accumulation of material deposited on the floor from ceiling drippings. Stalagmites are typically composed of calcium carbonate, but may consist of lava, mud, peat, pitch, sand, sinter, and amberat (crystallized urine of pack rats). The corresponding formation hanging down from the ceiling of a cave is a stalactite. Mnemonics have been developed for which word refers to which type of formation; one is that ''stalactite'' has a C for "ceiling", and ''stalagmite'' has a G for "ground", another is that, as with ants in the pants, the mites go up and the tights (tites) come down. Formation and type Limestone stalagmites The most common stalagmites are speleothems, which usually form in limestone caves. Stalagmite formation occurs only under certain pH conditions within the cavern. They form through deposition of calcium carbonate ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cumberland Plateau
The Cumberland Plateau is the southern part of the Appalachian Plateau in the Appalachian Mountains of the United States. It includes much of eastern Kentucky and Tennessee, and portions of northern Alabama and northwest Georgia. The terms "Allegheny Plateau" and the "Cumberland Plateau" both refer to the dissected plateau lands lying west of the main Appalachian Mountains. The terms stem from historical usage rather than geological difference, so there is no strict dividing line between the two. Two major rivers share the names of the plateaus, with the Allegheny River rising in the Allegheny Plateau and the Cumberland River rising in the Cumberland Plateau in Harlan County, Kentucky. Geography The Cumberland Plateau is a deeply dissected plateau, with topographic relief commonly of about , and frequent sandstone outcroppings and bluffs. At Kentucky's Pottsville Escarpment, which is the transition from the Cumberland Plateau to the Bluegrass in the north and the Pennyril ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Escarpment
An escarpment is a steep slope or long cliff that forms as a result of faulting or erosion and separates two relatively level areas having different elevations. The terms ''scarp'' and ''scarp face'' are often used interchangeably with ''escarpment''. Some sources differentiate the two terms, with ''escarpment'' referring to the margin between two landforms, and ''scarp'' referring to a cliff or a steep slope. In this usage an escarpment is a ridge which has a gentle slope on one side and a steep scarp on the other side. More loosely, the term ''scarp'' also describes a zone between a coastal lowland and a continental plateau which shows a marked, abrupt change in elevation caused by coastal erosion at the base of the plateau. Formation and description Scarps are generally formed by one of two processes: either by differential erosion of sedimentary rocks, or by movement of the Earth's crust at a geologic fault. The first process is the more common type: the escarpment is a t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mississippian (geology)
The Mississippian ( , also known as Lower Carboniferous or Early Carboniferous) is a subperiod in the geologic timescale or a subsystem of the geologic record. It is the earlier of two subperiods of the Carboniferous period lasting from roughly 358.9 to 323.2 million years ago. As with most other geochronologic units, the rock beds that define the Mississippian are well identified, but the exact start and end dates are uncertain by a few million years. The Mississippian is so named because rocks with this age are exposed in the Mississippi Valley. The Mississippian was a period of marine transgression in the Northern Hemisphere: the sea level was so high that only the Fennoscandian Shield and the Laurentian Shield were dry land. The cratons were surrounded by extensive delta systems and lagoons, and carbonate sedimentation on the surrounding continental platforms, covered by shallow seas. In North America, where the interval consists primarily of marine limestones, it is treate ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Deer Tick (band)
Deer Tick is an American alternative rock-folk band from Providence, Rhode Island, composed of singer-songwriter John J. McCauley, guitarist Ian O'Neil, bassist Christopher Ryan and drummer Dennis Ryan. The band's music has been described as rock with folk, blues and country influences, although the band actively rebels against the country tag, stating "We’re proud not to sing with a twang". The band regularly performs cover versions in their live sets, including songs by the likes of The Replacements, Nirvana, John Prine, Hank Williams, the Beastie Boys, Warren Zevon and Sonny West. They have also performed entire sets as Deervana, a Nirvana tribute band, including a show in September 2013 to mark the 20th anniversary of the band's third album ''In Utero''. McCauley explained that inspiration for the name "Deer Tick" came while hiking in summer 2005 in the Morgan–Monroe State Forest near Bloomington, Indiana, where he found a deer tick on his scalp one evening, having nev ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kip Moore
Kipling Christian Moore (born April 2, 1980) is an American country music singer and songwriter signed to MCA Nashville. He has released a total of four studio albums for the label: '' Up All Night'', '' Wild Ones'', ''Slowheart'', and '' Wild World''. Moore has charted a total of twelve entries on ''Billboard'' Hot Country Songs and Country Airplay including the number-one "Somethin' 'Bout a Truck" and four additional top-ten hits. He has also written songs for Frankie Ballard, Thompson Square, and James Wesley. Biography Kip Moore was born in Tifton, Georgia, to Bonnie (Mann) and Stan Moore. He has two brothers and three sisters. Their father died in September 2011, just months before the release of Moore's debut album. He began playing guitar while attending Wallace State Community College in Hanceville, Alabama, and made his first public performance at a Mellow Mushroom restaurant in Valdosta, Georgia. After college, he moved to a "little hut" in Hawaii, where he also took ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
