|
Seneca Caverns (West Virginia)
Seneca Caverns is a karst show cave in Germany Valley near Riverton, West Virginia, USA. It has been commercially used since 1930. The largest room inside the cave is the Teter Hall, which is 60 feet tall by 60 feet wide in some areas. History A German-American settler named Phillip Teter purchased the land surrounding Seneca Caverns in the 1770s.The proprietors of the cave give the date of discovery as 1742, and having been done by Laven Teter. However, historical records indicate that the Mouth of Seneca/Germany Valley area was not settled by whites until 1761, and that no such person as Laven Teter lived in the area. He may have first entered the cave on a quest for water to supply his livestock. The first recorded entry into the cave was in 1781 by Francis Asbury. The Teter family maintained ownership until 1928, at which point it became property of the Harman family, who began the process of commercializing the cave. In 1930 the new owners opened it to the public as a sho ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Riverton, West Virginia
Riverton is an unincorporated community on the North Fork South Branch Potomac River in Pendleton County, West Virginia, United States. Riverton lies along U.S. Highway 33/West Virginia Route 28 in the Monongahela National Forest. Climate This climatic region is typified by large seasonal temperature differences, with warm to hot (and often humid) summers and cold (sometimes severely cold) winters. According to the Köppen Climate Classification system, Riverton has a humid continental climate A humid continental climate is a climatic region defined by Russo-German climatologist Wladimir Köppen in 1900, typified by four distinct seasons and large seasonal temperature differences, with warm to hot (and often humid) summers and freezing ..., abbreviated "Dfb" on climate maps. References Unincorporated communities in Pendleton County, West Virginia Unincorporated communities in West Virginia {{PendletonCountyWV-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
West Virginia
West Virginia is a state in the Appalachian, Mid-Atlantic and Southeastern regions of the United States.The Census Bureau and the Association of American Geographers classify West Virginia as part of the Southern United States while the Bureau of Labor Statistics classifies the state as a part of the Mid-Atlantic regionMid-Atlantic Home : Mid-Atlantic Information Office: U.S. Bureau of Labor Statistics" www.bls.gov. Archived. It is bordered by Pennsylvania to the north and east, Maryland to the east and northeast, Virginia to the southeast, Kentucky to the southwest, and Ohio to the northwest. West Virginia is the 10th-smallest state by area and ranks as the 12th-least populous state, with a population of 1,793,716 residents. The capital and largest city is Charleston. West Virginia was admitted to the Union on June 20, 1863, and was a key border state during the American Civil War. It was the only state to form by separating from a Confederate state, the second to sepa ... [...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] |
Karst
Karst is a topography formed from the dissolution of soluble rocks such as limestone, dolomite, and gypsum. It is characterized by underground drainage systems with sinkholes and caves. It has also been documented for more weathering-resistant rocks, such as quartzite, given the right conditions. Subterranean drainage may limit surface water, with few to no rivers or lakes. However, in regions where the dissolved bedrock is covered (perhaps by debris) or confined by one or more superimposed non-soluble rock strata, distinctive karst features may occur only at subsurface levels and can be totally missing above ground. The study of ''paleokarst'' (buried karst in the stratigraphic column) is important in petroleum geology because as much as 50% of the world's hydrocarbon reserves are hosted in carbonate rock, and much of this is found in porous karst systems. Etymology The English word ''karst'' was borrowed from German in the late 19th century, which entered German much earlier ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Show Cave
A show cave—also called tourist cave, public cave, and, in the United States, commercial cave—is a cave which has been made accessible to the public for guided visits. Definition A show cave is a cave that has been made accessible to the public for guided visits, where a cave is defined as a natural occurring void beneath the surface of the earth, per the International Show Caves Association. A show cave may be managed by a government or commercial organization and made accessible to the general public, usually for an entrance fee. Unlike wild caves, they may possess regular opening hours, guided group tours, constructed trails and stairs, color artificial illumination and other lighting, musical/video/laser shows and concerts, elevators, small trains, and boats if they contain underground water features. Some caves (mainly in Asia) open to the public have temples, monasteries and religious statues or monuments. Some caves are visited by millions of tourists annually ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Germany Valley
Germany Valley is a scenic upland valley high in the Allegheny Mountains of eastern West Virginia originally settled by German (including Pennsylvania Dutch) farmers in the mid-18th century. It is today a part of the Spruce Knob–Seneca Rocks National Recreation Area of the Monongahela National Forest, although much ownership of the Valley remains in private hands. The Valley is noted for its extensive karst and cave development, with dozens of caves and cave systems having been formally documented and mapped. The area was made a National Natural Landmark, the Germany Valley Karst Area, in 1973 by the National Park Service. The NPS cited it as "one of the largest cove or intermountain karst areas in the country, unique because all the ground water recharge and solution activities are linked with precipitation within the cove." Geography Germany Valley is situated in the upper reaches of the North Fork South Branch Potomac River in northeastern Pendleton County, West Virginia. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
German-American
German Americans (german: Deutschamerikaner, ) are Americans who have full or partial German ancestry. With an estimated size of approximately 43 million in 2019, German Americans are the largest of the self-reported ancestry groups by the United States Census Bureau in its American Community Survey. German Americans account for about one third of the total population of people of German ancestry in the world. Very few of the German states had colonies in the new world. In the 1670s, the first significant groups of German immigrants arrived in the British colonies, settling primarily in Pennsylvania, New York and Virginia. The Mississippi Company of France moved thousands of Germans from Europe to Louisiana and to the German Coast, Orleans Territory between 1718 and 1750. Immigration ramped up sharply during the 19th century. There is a "German belt" that extends all the way across the United States, from eastern Pennsylvania to the Oregon coast. Pennsylvania, with 3.5 millio ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mouth Of Seneca
Seneca Rocks is an unincorporated community located in Pendleton County, West Virginia, United States. The community of Seneca Rocks — formerly known as Mouth of Seneca — lies at the junction of US 33, WV 28 and WV 55 near the confluence of Seneca Creek and the North Fork South Branch Potomac River. The community also lies near Seneca Rocks, the crag from which it takes its name. Both lie within the Spruce Knob–Seneca Rocks National Recreation Area of the Monongahela National Forest. Located at Seneca Rocks is the Sites Homestead (c. 1839), now part of the Seneca Rocks Visitor Center and listed on the National Register of Historic Places The National Register of Historic Places (NRHP) is the United States federal government's official list of districts, sites, buildings, structures and objects deemed worthy of preservation for their historical significance or "great artistic v ... in 2004. Located nearby is the Boggs Mill (c. 1830), listed in 2004. References ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Francis Asbury
Francis Asbury (August 20 or 21, 1745 – March 31, 1816) was one of the first two bishops of the Methodist Episcopal Church in the United States. During his 45 years in the colonies and the newly independent United States, he devoted his life to ministry, traveling on horseback and by carriage thousands of miles to those living on the frontier. Asbury spread Methodism in British colonial America as part of the Second Great Awakening. He also founded several schools during his lifetime, although his own formal education was limited. His journal is valuable to scholars for its account of frontier society, with references to many towns and villages in Colonial America. Biography Childhood and adolescence Francis Asbury was born at Hamstead Bridge, Staffordshire, England on August 20 or 21, 1745, to Elizabeth and Joseph Asbury. The family moved to a cottage at Great Barr, Sandwell, the next year. His boyhood home still stands and is open as Bishop Asbury Cottage museum. Soon a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Smoke Hole Caverns
Smoke Hole Caverns (SHC) is a picturesque show cave in Grant County in West Virginia's Eastern Panhandle. SHC were opened to the public on 30 May 1940. They are located near the Smoke Hole Canyon from which the cave takes its name. They are located on WV 28 13 km west of Petersburg. Local lore has it that the cave was utilized during Prohibition by moonshiners. There is only one entrance into the caverns which made it secure and with an ever present supply of fresh water it was a perfect place to produce moonshine. SHC is owned and operated by Jerry and Janet Hedrick. Smoke Hole Caverns has a feature called "The World's Largest Ribbon Stalactite", Gunns Plains Cave, in northwest Tasmania ) , nickname = , image_map = Tasmania in Australia.svg , map_caption = Location of Tasmania in AustraliaCoordinates: , subdivision_type = Country , subdi ..., also claims to have the world's lar ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Seneca Caverns (Ohio)
Seneca Caverns is a show cave located in northeastern Seneca County, Ohio, USA, just outside Flat Rock. The cave is designated as a Registered Natural Landmark by the Ohio Department of Natural Resources. History The cave was discovered in June 1872 by two boys named Peter Rutan and Henry Homer while they were hunting rabbits with their dog. The dog chased a rabbit into a brush pile, where they then disappeared. While searching through the brush pile, the two boys found an opening, fell through it, and landed in the first level of the cave, where they found their dog. The boys returned home and told everyone about their discovery. The cave became known as Good's Cave, named for Emmanuel Good, the owner of the farm on which the cave was located. In 1931, Don Bell, a lawyer from |
Caves Of West Virginia
A cave or cavern is a natural void in the ground, specifically a space large enough for a human to enter. Caves often form by the weathering of rock and often extend deep underground. The word ''cave'' can refer to smaller openings such as sea caves, rock shelters, and grottos, that extend a relatively short distance into the rock and they are called ''exogene'' caves. Caves which extend further underground than the opening is wide are called ''endogene'' caves. Speleology is the science of exploration and study of all aspects of caves and the cave environment. Visiting or exploring caves for recreation may be called ''caving'', ''potholing'', or ''spelunking''. Formation types The formation and development of caves is known as ''speleogenesis''; it can occur over the course of millions of years. Caves can range widely in size, and are formed by various geological processes. These may involve a combination of chemical processes, erosion by water, tectonic forces, microorganism ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
.jpg "Click for more on -> Karst")
