Berkeley Springs State Park
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Berkeley Springs State Park
Berkeley Springs State Park is situated in the center of Berkeley Springs, West Virginia, USA. The centerpiece of the Park is its historic mineral spa. These waters were celebrated for their medicinal or restorative powers and were generally taken internally for digestive disorders, or bathed in for stress relief. Native peoples visited these springs as did George Washington. Berkeley Springs is the only state-run spa in the United States and is operated by the West Virginia Division of Natural Resources. History The Park is located on land which has been used as a health resort since the 1750s as the property of Lord Fairfax. On 18 March 1748, George Washington, then 16, visited the spa for the first time. An annual event is held to commemorate this historic visit, but the tub where Washington supposedly bathed was rebuilt in the 1930s. Colonial maps dating as early as 1740 credit medicinal properties to the springs' waters. The land was officially granted to Virginia in 177 ...
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Morgan County, West Virginia
Morgan County is a county located in the U.S. state of West Virginia. As of the 2020 census, the population was 17,063. Its county seat is Berkeley Springs. The county was formed in 1820 from parts of Hampshire and Berkeley Counties and named in honor of General Daniel Morgan, prominent soldier of the American Revolutionary War. The county and town of Bath are considered an excellent jumping off point for exploring the Potomac and Cacapon Rivers valleys just to the north and west. Along with also being a tourist destination hosting numerous local artists, mineral water spas, and a large amount of outdoor recreation that includes fishing, boating, wildlife, hunting, and mountain scenery. The region is known for the famed Apple Butter Festival held annually in October. Morgan County is also the home of an important silica mine, part of U.S. Silica. History Morgan County was created by an act of the Virginia General Assembly in February 1820 from parts of Berkeley and Hampshire c ...
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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 ...
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Destination Spas
Destination may refer to: Music *Destination (group), a disco studio group from New York * ''Destination'' (Eloy album), 1992 * ''Destination'' (FictionJunction Yuuka album), 2005 * ''Destination'' (Ronan Keating album), 2002 * ''Destination'' (EP), by SS501, 2010 *''The Destination'', an EP by Vonthongchai Intarawat, 2008 *''Destination'', an album by Akina Nakamori, 2006 *"Destination", a song by The Church from ''Starfish'' Other uses * ''Destination'' (game), a board game * ''Destination'' (magazine), a monthly lifestyle magazine published in Saudi Arabia *Destination Films, a division of Sony Pictures * Tourist destination, a place commercially dedicated to tourism See also *Destiny (other) Destiny is a predetermined course of events or fixed natural order of the universe. Destiny may also refer to: People * Destiny (given name), with a list of people so called * Destiny (streamer) (born 1988), former Twitch streamer and political ...
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Warm Spring Run
Warm Spring Run is an U.S. Geological Survey. National Hydrography Dataset high-resolution flowline dataThe National Map accessed August 15, 2011 non-navigable tributary stream of the Potomac River in Morgan County of West Virginia's Eastern Panhandle. It rises on the eastern side of Warm Springs Ridge (1,115 feet) and parallels U.S. Route 522 for most of its course. Warm Spring Run enters the Potomac River at Hancock. Warm Spring Run is primarily fed by springs on Warm Springs Ridge, the best-known of these being the springs at Berkeley Springs State Park in Berkeley Springs through which it flows. Tributaries *Dry Run List of cities and towns along Warm Spring Run * Berkeley Springs * Berryville * Burnt Factory *Hancock * Jimtown * North Berkeley See also *List of rivers of West Virginia This is a list of rivers in the U.S. state of West Virginia. List of West Virginia rivers includes streams formally designated as rivers. There are also smaller streams (i.e., branche ...
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List Of West Virginia State Parks
There are 37 state parks in the U.S. state of West Virginia . The West Virginia Division of Natural Resources (WVDNR) Parks and Recreation Section is the governing body for all 37 state parks and directly operates all but one of them. In addition to state parks, the WVDNR Parks and Recreation Section governs eight state forests. The first West Virginia state park, Droop Mountain Battlefield, was acquired in 1928 and dedicated in 1929; and the newest state parks, Stonewall Jackson Lake and North Bend Rail Trail, were opened in 1990 and 1991, respectively. Four parks that later joined the state park system were established prior to Droop Mountain, the earliest being the Point Pleasant Monument (now Tu-Endie-Wei) in 1901. There are seven former West Virginia state parks: one state park was transferred to the National Park Service (NPS), one to the West Virginia Division of Culture and History, one to the West Virginia Division of Highways, and one to a municipality, and three ...
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National Register Of Historic Places Listings In West Virginia
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Tap (valve)
A tap (also spigot or faucet: see usage variations) is a valve controlling the release of a liquid or gas. Nomenclature United Kingdom * Tap is used in the United Kingdom and most of the Commonwealth for any everyday type of valve, particularly the fittings that control water supply to bathtubs and sinks. United States * Faucet is the most common term in the US, similar in use to "tap" in British English, e.g. "water faucet" (although the term "tap" is also used in the US). * Spigot is used by professionals in the trade (such as plumbers), and typically refers to an outdoor fixture. * Silcock (and sillcock), same as "spigot", referring to a "cock" (as in stopcock and petcock) that penetrates a foundation sill. * Bib (bibcock, and hose bib or hosebibb), usually a freeze-resistant version of a "spigot". * Wall hydrant, same as "hosebibb". * Tap generally refers to a keg or barrel tap, though also commonly refers to a faucet that supplies either hot or cold water and not ...
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Fountain
A fountain, from the Latin "fons" (genitive "fontis"), meaning source or Spring (hydrology), spring, is a decorative reservoir used for discharging water. It is also a structure that jets water into the air for a decorative or dramatic effect. Fountains were originally purely functional, connected to springs or aqueduct (watercourse), aqueducts and used to provide drinking water and water for bathing and washing to the residents of cities, towns and villages. Until the late 19th century most fountains operated by gravity, and needed a source of water higher than the fountain, such as a reservoir or aqueduct, to make the water flow or jet into the air. In addition to providing drinking water, fountains were used for decoration and to celebrate their builders. Roman fountains were decorated with bronze or stone masks of animals or heroes. In the Middle Ages, Moorish and Muslim garden designers used fountains to create miniature versions of the gardens of paradise. King Louis XIV ...
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Public Bathing
Public baths originated when most people in population centers did not have access to private bathing facilities. Though termed "public", they have often been restricted according to gender, religious affiliation, personal membership, and other criteria. In addition to their hygienic function, public baths have also been social meeting places. They have included saunas, massages, and other relaxation therapies, as are found in modern day spas. As the percentage of dwellings containing private bathrooms has increased in some societies, the need for public baths has diminished, and they are now almost exclusively used recreationally. History Public facilities for bathing were constructed, as excavations have provided evidence for, in the 3rd millennium BC, as with the Great Bath, Mohenjo-daro. Ancient Greece In Greece by the sixth century BC men and women washed in basins near places of physical and intellectual exercise. Later gymnasia had indoor basins set overhead, the open ...
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Discharge (hydrology)
In hydrology, discharge is the volumetric flow rate of water that is transported through a given cross-sectional area. It includes any suspended solids (e.g. sediment), dissolved chemicals (e.g. CaCO3(aq)), or biologic material (e.g. diatoms) in addition to the water itself. Terms may vary between disciplines. For example, a fluvial hydrologist studying natural river systems may define discharge as streamflow, whereas an engineer operating a reservoir system may equate it with outflow, contrasted with inflow. Theory and calculation A discharge is a measure of the quantity of any fluid flow over unit time. The quantity may be either volume or mass. Thus the water discharge of a tap (faucet) can be measured with a measuring jug and a stopwatch. Here the discharge might be 1 litre per 15 seconds, equivalent to 67 ml/second or 4 litres/minute. This is an average measure. For measuring the discharge of a river we need a different method and the most common is the 'area-velocity' method. ...
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Magnesium Carbonate
Magnesium carbonate, (archaic name magnesia alba), is an inorganic salt that is a colourless or white solid. Several hydrated and basic forms of magnesium carbonate also exist as minerals. Forms The most common magnesium carbonate forms are the anhydrous salt called magnesite (), and the di, tri, and pentahydrates known as barringtonite (), nesquehonite (), and lansfordite (), respectively. Some basic forms such as artinite (), hydromagnesite (), and dypingite () also occur as minerals. All of those minerals are colouress or white. Magnesite consists of colourless or white trigonal crystals. The anhydrous salt is practically insoluble in water, acetone, and ammonia. All forms of magnesium carbonate react with acids. Magnesite crystallizes in the calcite structure wherein is surrounded by six oxygen atoms. The dihydrate has a triclinic structure, while the trihydrate has a monoclinic structure. References to "light" and "heavy" magnesium carbonates actually refer to ...
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Carbonate
A carbonate is a salt of carbonic acid (H2CO3), characterized by the presence of the carbonate ion, a polyatomic ion with the formula . The word ''carbonate'' may also refer to a carbonate ester, an organic compound containing the carbonate group C(=O)(O–)2. The term is also used as a verb, to describe carbonation: the process of raising the concentrations of carbonate and bicarbonate ions in water to produce carbonated water and other carbonated beverageseither by the addition of carbon dioxide gas under pressure or by dissolving carbonate or bicarbonate salts into the water. In geology and mineralogy, the term "carbonate" can refer both to carbonate minerals and carbonate rock (which is made of chiefly carbonate minerals), and both are dominated by the carbonate ion, . Carbonate minerals are extremely varied and ubiquitous in chemically precipitated sedimentary rock. The most common are calcite or calcium carbonate, CaCO3, the chief constituent of limestone (as well a ...
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