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Gosu Cave
Gosu Cave (고수동굴 - Kosu is also still found as an alternate spelling) is a huge limestone cave near Danyang, Chungcheongbuk-do, Danyang (North Chungcheong Province), South Korea formed over 450 million years ago. It is among the best known natural caves in Korea, and is known as the "underground palace". Gosu Cave is listed as the country's "Natural Monument No. 256". "Gosu" means "field of tall reeds," and comes from the fact that the area used to be filled with fields of tall grasses. After the cave was discovered in the early 1970s, rough stone instruments were excavated from the cave's entrance, showing that this used to be a home to prehistoric people. Features of the cave The cave, 1,300 m/4,264 ft deep, is inhabited by 25 species of insects and animals. About 120 different stalactites and stalagmites are found here. Some of the formations resemble animals or human figures, such as Lion Rock, Octopus Rock, Eagle Rock, and even the Virgin Mary Rock. The Lion Rock ... [...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] |
Danyang, Chungcheongbuk-do
Danyang County (''Danyang-gun'') is in North Chungcheong Province, South Korea. Symbols *County tree: Yew tree *County bird: Magpie *County flower: Royal Azalea Geography The geographical terrain is 83.7% mountainous and 11.2% cultivable. It is very rugged, except in some of the urban areas and villages that can be found in the valleys and hills. The main water system ranges from the upper stream of the long Namhan River, which flows through the county. Pyeongchang River, one of the streams flowing from Odaesan, joins several streams at Jungnyeong, Danyang, and Geumgok, originating from Sobaeksan. Danyang Stream, which has its source in Hakseongsan, Gyeongsangbuk-do, joins the Namhan River at Habang-ri, Danseong-myeon, together with Jungnyeong Stream flowing from Jungnyeong and Dosolsan to Hyeoncholli, Danyang-eup, Maepo Stream from Geumsusan to Dodam, and Geumgok Stream from Biro Peak to Gosu-ri, Danyang-eup.Official page of Danyang county http://english.dy21.net/english/ Cli ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
North Chungcheong Province
North Chungcheong Province ( ko, 충청북도, ''Chungcheongbuk-do''), also known as Chungbuk, is a province of South Korea. North Chungcheong has a population of 1,578,934 (2014) and has a geographic area of located in the Hoseo region in the south-center of the Korean Peninsula. North Chungcheong borders the provinces of Gyeonggi and Gangwon to the north, North Gyeongsang to the east, North Jeolla to the south and South Chungcheong, Sejong Special Autonomous City and Daejeon Metropolitan City to the west. Cheongju is the capital and largest city of North Chungcheong, with other major cities including Chungju and Jecheon. North Chungcheong was established in 1896 from the province of Chungcheong, one of the Eight Provinces of Korea, consisting of the northeastern half of the territory, and is South Korea's only landlocked province. North Chungcheong was known as Chūsei-hoku Prefecture during the Japanese Colonial Period from 1910 and became part of South Korea following the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
South Korea
South Korea, officially the Republic of Korea (ROK), is a country in East Asia, constituting the southern part of the Korea, Korean Peninsula and sharing a Korean Demilitarized Zone, land border with North Korea. Its western border is formed by the Yellow Sea, while its eastern border is defined by the Sea of Japan. South Korea claims to be the sole legitimate government of the entire peninsula and List of islands of South Korea, adjacent islands. It has a Demographics of South Korea, population of 51.75 million, of which roughly half live in the Seoul Capital Area, the List of metropolitan areas by population, fourth most populous metropolitan area in the world. Other major cities include Incheon, Busan, and Daegu. The Korean Peninsula was inhabited as early as the Lower Paleolithic period. Its Gojoseon, first kingdom was noted in Chinese records in the early 7th century BCE. Following the unification of the Three Kingdoms of Korea into Unified Silla, Silla and Balhae in the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Stalactites
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] |
Stalagmites
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] |
Speleothems
A speleothem (; ) is a geological formation by mineral deposition (geology), deposits that accumulate over time in natural caves. Speleothems most commonly form in calcareous caves due to carbonate dissolution reactions. They can take a variety of forms, depending on their depositional history and environment. Their chemical composition, gradual growth, and preservation in caves make them useful paleoclimatology, paleoclimatic proxies. Chemical and physical characteristics More than 300 variations of cave mineral deposits have been identified. The vast majority of speleothems are calcareous, composed of calcium carbonate (CaCO3) minerals (calcite or aragonite). Less commonly, speleothems are made of calcium sulfate (gypsum or mirabilite) or opal. Speleothems of pure calcium carbonate or calcium sulfate are translucent and colorless. The presence of iron oxide or copper provides a reddish brown color. The presence of manganese oxide can create darker colors such as black or dark b ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cave Popcorn
Cave popcorn, or coralloids, are small nodes of calcite, aragonite or gypsum that form on surfaces in caves, especially limestone caves. They are a common type of speleothem. Appearance The individual nodules of cave popcorn range in size from 5 to 20 mm and may be decorated by other speleothems, especially aragonite needles or frostwork. The nodules tend to grow in clusters on bedrock or the sides of other speleothems. These clusters may terminate suddenly in either an upward or downward direction, forming a stratographic layer. When they terminate in a downward direction, they may appear as flat bottomed formations known as trays. Individual nodes of popcorn can assume a variety of shapes from round to flattened ear or button like shapes. The color of cave popcorn is usually white, but various other colors are possible depending on the composition. Formation Cave popcorn can form by precipitation. Water seeping through limestone walls or splashing onto them leaves depo ... [...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] |
Aragonite
Aragonite is a carbonate mineral, one of the three most common naturally occurring crystal forms of calcium carbonate, (the other forms being the minerals calcite and vaterite). It is formed by biological and physical processes, including precipitation from marine and freshwater environments. The crystal lattice of aragonite differs from that of calcite, resulting in a different crystal shape, an orthorhombic crystal system with acicular crystal. Repeated twinning results in pseudo-hexagonal forms. Aragonite may be columnar or fibrous, occasionally in branching helictitic forms called ''flos-ferri'' ("flowers of iron") from their association with the ores at the Carinthian iron mines. Occurrence The type location for aragonite is Molina de Aragón in the Province of Guadalajara in Castilla-La Mancha, Spain, for which it was named in 1797. Aragonite is found in this locality as cyclic twins inside gypsum and marls of the Keuper facies of the Triassic. This type of arago ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Caves Of South Korea
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, microorganisms ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
