Muri Spring
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Muri Spring
Muri Spring (, ) is a chalybeate mineral spring on the Austrian side of the Austria-Slovenia border, on the slope of a hill named Goli Vrh. The spring is next to the main road leading from Seeberg Saddle, Jezersko towards the village of Bad Vellach. The water arises from Paleozoic schists, which contain a high concentration of iron minerals. Due to the high mineral content, the water leaves a marked trace. During the rain, the fallen water runs underground and mixes with carbon dioxide, which emerges from deeper parts of the Earth's crust. Such water dissolves iron minerals present in the rock of this area. The source disappears during drought and low rain. References External links * Uroš Grabnar, Ognjeno rdeča voda...
Springs of Austria Völkermarkt District Landforms of Carinthia {{Carinthia-geo-stub ...
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Muri Quelle
Muri Spring (, ) is a chalybeate mineral spring on the Austrian side of the Austria-Slovenia border, on the slope of a hill named Goli Vrh. The spring is next to the main road leading from Jezersko towards the village of Bad Vellach. The water arises from Paleozoic schists, which contain a high concentration of iron minerals. Due to the high mineral content, the water leaves a marked trace. During the rain, the fallen water runs underground and mixes with carbon dioxide, which emerges from deeper parts of the Earth's crust Earth's crust is its thick outer shell of rock, referring to less than one percent of the planet's radius and volume. It is the top component of the lithosphere, a solidified division of Earth's layers that includes the crust and the upper .... Such water dissolves iron minerals present in the rock of this area. The source disappears during drought and low rain. References External links * Uroš Grabnar, Ognjeno rdeča voda... Springs ...
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Muri Spring
Muri Spring (, ) is a chalybeate mineral spring on the Austrian side of the Austria-Slovenia border, on the slope of a hill named Goli Vrh. The spring is next to the main road leading from Seeberg Saddle, Jezersko towards the village of Bad Vellach. The water arises from Paleozoic schists, which contain a high concentration of iron minerals. Due to the high mineral content, the water leaves a marked trace. During the rain, the fallen water runs underground and mixes with carbon dioxide, which emerges from deeper parts of the Earth's crust. Such water dissolves iron minerals present in the rock of this area. The source disappears during drought and low rain. References External links * Uroš Grabnar, Ognjeno rdeča voda...
Springs of Austria Völkermarkt District Landforms of Carinthia {{Carinthia-geo-stub ...
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Bad Vellach
Bad or BAD may refer to: Common meanings *Evil, the opposite of moral good * Erroneous, inaccurate or incorrect * Unhealthy, or counter to well-being *Antagonist, the threat or obstacle of moral good Acronyms * BAD-2, a Soviet armored trolley car * Bank account debits tax, an Australian tax * Bcl-2-associated death promoter, a pro-apoptotic protein * Team B.A.D., a professional wrestling tag team Films * ''Andy Warhol's Bad'', a 1977 film * ''Bad'', an unfinished film by Theo van Gogh * ''Bad'' (2025 film), an Indian Kannada-language action thriller film Music Performers * B. A. D., the Taiwanese boy band, who formed in 1998 * Big Audio Dynamite, Mick Jones' post-Clash band, from London * Royce da 5'9", the American rapper known as Bad, in the group Bad Meets Evil Albums * ''Bad'' (album), a 1987 album by Michael Jackson * ''BAD'', or '' Bigger and Deffer'', the second album by LL Cool J, 1987 Songs * "Bad" (U2 song), 1984 * "Bad" (Michael Jackson song), 1987 * "Ba ...
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Springs Of Austria
Spring(s) may refer to: Common uses * Spring (season), a season of the year * Spring (device), a mechanical device that stores energy * Spring (hydrology), a natural source of water * Spring (mathematics), a geometric surface in the shape of a helically coiled tube * Spring (political terminology), often used to name periods of political liberalization * Springs (tide), in oceanography, the maximum tide, occurs twice a month during the full and new moon Places * Spring (Milz), a river in Thuringia, Germany * Spring, Alabel, a barangay unit in Alabel, Sarangani Province, Philippines * Șpring, a commune in Alba County, Romania * Șpring (river), a river in Alba County, Romania * Springs, Gauteng, South Africa * Springs, the location of Dubai British School, Dubai * Spring Village, Saint Vincent and the Grenadines * Spring Village, Shropshire, England United States * Springs, New York, a part of East Hampton, New York * Springs, Pennsylvania, an unincorporated community * Spring, ...
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Earth's Crust
Earth's crust is its thick outer shell of rock, referring to less than one percent of the planet's radius and volume. It is the top component of the lithosphere, a solidified division of Earth's layers that includes the crust and the upper part of the mantle. The lithosphere is broken into tectonic plates whose motion allows heat to escape the interior of Earth into space. The crust lies on top of the mantle, a configuration that is stable because the upper mantle is made of peridotite and is therefore significantly denser than the crust. The boundary between the crust and mantle is conventionally placed at the Mohorovičić discontinuity, a boundary defined by a contrast in seismic velocity. The temperature of the crust increases with depth, reaching values typically in the range from about at the boundary with the underlying mantle. The temperature increases by as much as for every kilometer locally in the upper part of the crust. Composition File:Elementa ...
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Carbon Dioxide
Carbon dioxide is a chemical compound with the chemical formula . It is made up of molecules that each have one carbon atom covalent bond, covalently double bonded to two oxygen atoms. It is found in a gas state at room temperature and at normally-encountered concentrations it is odorless. As the source of carbon in the carbon cycle, atmospheric is the primary carbon source for life on Earth. In the air, carbon dioxide is transparent to visible light but absorbs infrared, infrared radiation, acting as a greenhouse gas. Carbon dioxide is soluble in water and is found in groundwater, lakes, ice caps, and seawater. It is a trace gas Carbon dioxide in Earth's atmosphere, in Earth's atmosphere at 421 parts per million (ppm), or about 0.042% (as of May 2022) having risen from pre-industrial levels of 280 ppm or about 0.028%. Burning fossil fuels is the main cause of these increased concentrations, which are the primary cause of climate change.IPCC (2022Summary for pol ...
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Schists
Schist ( ) is a medium-grained metamorphic rock generally derived from fine-grained sedimentary rock, like shale. It shows pronounced ''schistosity'' (named for the rock). This means that the rock is composed of mineral grains easily seen with a low-power hand lens, oriented in such a way that the rock is easily split into thin flakes or plates. This texture reflects a high content of platy minerals, such as mica, talc, chlorite, or graphite. These are often interleaved with more granular minerals, such as feldspar or quartz. Schist typically forms during regional metamorphism accompanying the process of mountain building (orogeny) and usually reflects a medium grade of metamorphism. Schist can form from many different kinds of rocks, including sedimentary rocks such as mudstones and igneous rocks such as tuffs. Schist metamorphosed from mudstone is particularly common and is often very rich in mica (a ''mica schist''). Where the type of the original rock (the protolith ...
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Paleozoic
The Paleozoic ( , , ; or Palaeozoic) Era is the first of three Era (geology), geological eras of the Phanerozoic Eon. Beginning 538.8 million years ago (Ma), it succeeds the Neoproterozoic (the last era of the Proterozoic Eon) and ends 251.9 Ma at the start of the Mesozoic Era. The Paleozoic is subdivided into six period (geology), geologic periods (from oldest to youngest), Cambrian, Ordovician, Silurian, Devonian, Carboniferous and Permian. Some geological timescales divide the Paleozoic informally into early and late sub-eras: the Early Paleozoic consisting of the Cambrian, Ordovician and Silurian; the Late Paleozoic consisting of the Devonian, Carboniferous and Permian. The name ''Paleozoic'' was first used by Adam Sedgwick (1785–1873) in 1838 to describe the Cambrian and Ordovician periods. It was redefined by John Phillips (geologist), John Phillips (1800–1874) in 1840 to cover the Cambrian to Permian periods. It is derived from the Ancient Greek, Greek ''palaiós'' (π ...
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Seeberg Saddle
Seeberg Saddle (, ), also just Seeberg (''Jezersko'') is a high mountain pass connecting Bad Eisenkappel in the Austrian state of Carinthia with Jezersko in the Slovenian region of Carinthia. It is located in the Southern Limestone Alps, between the Karawanks range in the west and the Kamnik–Savinja Alps in the east. The road across the pass is probably of Roman origin, leading from the Drava valley in the Noricum province towards the city of Aquileia. The border at the summit was implemented after the dissolution of Austria-Hungary by the 1919 Treaty of Saint-Germain. Today the Seeberg Highway (B 82) heads from the Austrian side up to the border crossing on the pass. Directly behind the Slovenian border station is an inn. On the Slovenian side, the state road No. 210 descends from the Seeberg down to Jezersko, offering a panoramic view of the Kamnik Alps. Seeberg Saddle is also known as the ''Carinthian Seeberg'' to distinguish it from the Styrian Seeberg Pass in the Northern ...
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