. . . . . "\u0646\u0648\u0627\u0632\u0644 \u0628\u0644\u0648\u0631\u064A\u0629"@ar . . . . . . . . . . . . "Une fistuleuse (du latin fistulosus, \u00AB creux \u00BB) est une concr\u00E9tion tubiforme monocristalline qui s'allonge suivant la verticale et au sein de laquelle circule l'eau d'infiltration. Il s'agit le plus souvent d'un tube de calcite creux, allong\u00E9, translucide, de diam\u00E8tre \u00E9gal (8 mm) \u00E0 celui des gouttes d\u2019eau qui sont \u00E0 l'origine de sa formation par le processus de concr\u00E9tionnement. La fistuleuse qui fait partie des sp\u00E9l\u00E9oth\u00E8mes classiques, est parfois appel\u00E9e famili\u00E8rement \u00AB macaroni \u00BB."@fr . . . "\u0627\u0644\u0646\u0651\u0648\u0627\u0632\u0644 \u0627\u0644\u0628\u0644\u0651\u0648\u0631\u064A\u0651\u0629 \u0647\u064A \u0646\u0648\u0627\u0632\u0644 \u0631\u0641\u064A\u0639\u0629 \u062A\u0645\u062B\u0651\u0644 \u0623\u0646\u0627\u0628\u064A\u0628 \u0637\u0628\u064A\u0639\u064A\u0651\u0629 \u062A\u0634\u0643\u0651\u0644\u062A \u0645\u0646 \u062A\u0631\u0633\u0651\u0628\u0627\u062A \u0627\u0644\u0643\u0627\u0644\u0633\u064A\u062A \u0627\u0644\u0651\u062A\u064A \u064A\u062D\u0645\u0644\u0647\u0627 \u0645\u0639\u0647 \u0627\u0644\u0645\u0627\u0621 \u0627\u0644\u0645\u062A\u0631\u0634\u0651\u062D. \u0645\u0648\u0642\u0639 \u062A\u0648\u0627\u062C\u062F\u0647\u0627 \u0627\u0644\u0637\u0651\u0628\u064A\u0639\u064A\u0651 \u0647\u0648 \u0627\u0644\u0643\u0647\u0648\u0641 \u0648\u0627\u0644\u0645\u063A\u0627\u0631\u0627\u062A."@ar . . . . . . "Br\u010Dko je prim\u00E1rn\u00ED krasov\u00FD jev. Jedn\u00E1 se o prvotn\u00ED st\u00E1dium stalaktitu, kter\u00FD vznik\u00E1 vysr\u00E1\u017Een\u00EDm uhli\u010Ditanu v\u00E1penat\u00E9ho z vodn\u00EDho roztoku. Nejdel\u0161\u00ED zn\u00E1m\u00E9 br\u010Dko dosahovalo d\u00E9lky 9 metr\u016F. Ze stropn\u00EDch dutinek prosakuje kapka vody, kter\u00E1 b\u011Bhem prosakov\u00E1n\u00ED horninou j\u00ED rozkl\u00E1d\u00E1 a obohacuje se o miner\u00E1ln\u00ED slo\u017Eky. P\u0159i zm\u011Bn\u011B tlaku na p\u0159echodu mezi horninou a vzduchem, doch\u00E1z\u00ED ke sr\u00E1\u017Een\u00ED miner\u00E1l\u016F. Postupn\u00FDm p\u0159\u00EDsunem dal\u0161\u00ED vody dos\u00E1hne vznikaj\u00EDc\u00ED kapka velikosti, p\u0159i kter\u00E9 jej\u00ED v\u00E1ha p\u0159em\u016F\u017Ee p\u0159ilnavost vody ke stropu a kapka vlivem gravitace odk\u00E1pne. Tento proces m\u016F\u017Ee trvat i n\u011Bkolik hodin, b\u011Bhem kter\u00FDch doch\u00E1z\u00ED k odpa\u0159ov\u00E1n\u00ED z povrchu kapky. T\u00EDm se zahu\u0161\u0165uje obsah rozpu\u0161t\u011Bn\u00E9ho uhli\u010Ditanu v\u00E1penat\u00E9ho a doch\u00E1z\u00ED ke vzniku molekulov\u00FDch vlo\u010Dek krystal\u016F v\u00E1pence, kter\u00E9 se pohybuj\u00ED v povrchov\u00E9 blance kapky a hromad\u00ED se v tenk\u00E9m prstenci kolem horn\u00EDho okraje kapky, kde se usazuj\u00ED a tvo\u0159\u00ED prstenec, j\u00EDm\u017E st\u00E1le prokap\u00E1v\u00E1 voda. Prstenec nar\u016Fst\u00E1 v dut\u00FD v\u00E1pencov\u00FD v\u00E1le\u010Dek o pr\u016Fm\u011Bru odpov\u00EDdaj\u00EDc\u00EDmu velikosti vodn\u00ED kapky a dosahuj\u00EDc\u00ED d\u00E9lky a\u017E n\u011Bkolik metr\u016F zvan\u00FD br\u010Dko. Br\u010Dko m\u00E1 tenk\u00E9 k\u0159ehk\u00E9 pr\u016Fsvitn\u00E9 st\u011Bny a v\u011Bt\u0161inou rovn\u00FD tvar, jen v\u00FDjime\u010Dn\u011B zak\u0159iven\u00FD (zak\u0159iven\u00ED zp\u016Fsobuje nej\u010Dast\u011Bji proud\u00EDc\u00ED vzduch). Po st\u011Bn\u00E1ch br\u010Dka st\u00E9k\u00E1 voda, vypa\u0159uje se a br\u010Dko dor\u016Fst\u00E1 soust\u0159edn\u00FDmi vrstvi\u010Dkami v ko\u0159enovit\u00E9 tvary naz\u00FDvan\u00E9 stalaktity. Br\u010Dka jsou prvn\u00EDm \u00FAtvarem, kter\u00FD za\u010D\u00EDn\u00E1 vznikat vlivem vypa\u0159ov\u00E1n\u00ED vody a mineralizace. \u010Casto se s nimi d\u00E1 setkat i na \u00FA\u010Delov\u00FDch stavb\u00E1ch jako pod oblouky most\u016F."@cs . . . "1023946859"^^ . "A soda straw (or simply straw) is a speleothem in the form of a hollow mineral cylindrical tube. They are also known as tubular stalactites. Soda straws grow in places where water leaches slowly through cracks in rock, such as on the roofs of caves. Soda straws in caves rarely grow more than a few millimetres per year and may average one tenth of a millimetre per year. A soda straw can turn into a stalactite if the hole at the bottom is blocked, or if the water begins flowing on the outside surface of the hollow tube. Soda straws can also form outside the cave environment on exposed concrete surfaces as a type of calthemite, growing significantly faster than those formed on rock."@en . "Br\u010Dko (geologie)"@cs . . "Un macarr\u00F3, o estalactita fistulosa, \u00E9s un espeleotema consistent en una fina i delicada estalactita en el qual no existeix creixement secundari de cristalls perpendicular al canal primari, cosa que passa quan el degoteig de l'aigua \u00E9s lent per\u00F2 constant. La gruixa no passa habitualment dels 8 mm i la gruixa de les parets oscil\u00B7la entre els 0,1 mm i els 0,5 mm, i pot arribar a longituds de diversos metres."@ca . . . . . . . "Soda straw"@en . . . "A soda straw (or simply straw) is a speleothem in the form of a hollow mineral cylindrical tube. They are also known as tubular stalactites. Soda straws grow in places where water leaches slowly through cracks in rock, such as on the roofs of caves. Soda straws in caves rarely grow more than a few millimetres per year and may average one tenth of a millimetre per year. A soda straw can turn into a stalactite if the hole at the bottom is blocked, or if the water begins flowing on the outside surface of the hollow tube. Soda straws can also form outside the cave environment on exposed concrete surfaces as a type of calthemite, growing significantly faster than those formed on rock."@en . . "\u0627\u0644\u0646\u0651\u0648\u0627\u0632\u0644 \u0627\u0644\u0628\u0644\u0651\u0648\u0631\u064A\u0651\u0629 \u0647\u064A \u0646\u0648\u0627\u0632\u0644 \u0631\u0641\u064A\u0639\u0629 \u062A\u0645\u062B\u0651\u0644 \u0623\u0646\u0627\u0628\u064A\u0628 \u0637\u0628\u064A\u0639\u064A\u0651\u0629 \u062A\u0634\u0643\u0651\u0644\u062A \u0645\u0646 \u062A\u0631\u0633\u0651\u0628\u0627\u062A \u0627\u0644\u0643\u0627\u0644\u0633\u064A\u062A \u0627\u0644\u0651\u062A\u064A \u064A\u062D\u0645\u0644\u0647\u0627 \u0645\u0639\u0647 \u0627\u0644\u0645\u0627\u0621 \u0627\u0644\u0645\u062A\u0631\u0634\u0651\u062D. \u0645\u0648\u0642\u0639 \u062A\u0648\u0627\u062C\u062F\u0647\u0627 \u0627\u0644\u0637\u0651\u0628\u064A\u0639\u064A\u0651 \u0647\u0648 \u0627\u0644\u0643\u0647\u0648\u0641 \u0648\u0627\u0644\u0645\u063A\u0627\u0631\u0627\u062A."@ar . . "Une fistuleuse (du latin fistulosus, \u00AB creux \u00BB) est une concr\u00E9tion tubiforme monocristalline qui s'allonge suivant la verticale et au sein de laquelle circule l'eau d'infiltration. Il s'agit le plus souvent d'un tube de calcite creux, allong\u00E9, translucide, de diam\u00E8tre \u00E9gal (8 mm) \u00E0 celui des gouttes d\u2019eau qui sont \u00E0 l'origine de sa formation par le processus de concr\u00E9tionnement. La fistuleuse qui fait partie des sp\u00E9l\u00E9oth\u00E8mes classiques, est parfois appel\u00E9e famili\u00E8rement \u00AB macaroni \u00BB."@fr . . "Fistuleuse"@fr . "5592"^^ . . . . . . "Br\u010Dko je prim\u00E1rn\u00ED krasov\u00FD jev. Jedn\u00E1 se o prvotn\u00ED st\u00E1dium stalaktitu, kter\u00FD vznik\u00E1 vysr\u00E1\u017Een\u00EDm uhli\u010Ditanu v\u00E1penat\u00E9ho z vodn\u00EDho roztoku. Nejdel\u0161\u00ED zn\u00E1m\u00E9 br\u010Dko dosahovalo d\u00E9lky 9 metr\u016F. Ze stropn\u00EDch dutinek prosakuje kapka vody, kter\u00E1 b\u011Bhem prosakov\u00E1n\u00ED horninou j\u00ED rozkl\u00E1d\u00E1 a obohacuje se o miner\u00E1ln\u00ED slo\u017Eky. P\u0159i zm\u011Bn\u011B tlaku na p\u0159echodu mezi horninou a vzduchem, doch\u00E1z\u00ED ke sr\u00E1\u017Een\u00ED miner\u00E1l\u016F. Postupn\u00FDm p\u0159\u00EDsunem dal\u0161\u00ED vody dos\u00E1hne vznikaj\u00EDc\u00ED kapka velikosti, p\u0159i kter\u00E9 jej\u00ED v\u00E1ha p\u0159em\u016F\u017Ee p\u0159ilnavost vody ke stropu a kapka vlivem gravitace odk\u00E1pne. Tento proces m\u016F\u017Ee trvat i n\u011Bkolik hodin, b\u011Bhem kter\u00FDch doch\u00E1z\u00ED k odpa\u0159ov\u00E1n\u00ED z povrchu kapky. T\u00EDm se zahu\u0161\u0165uje obsah rozpu\u0161t\u011Bn\u00E9ho uhli\u010Ditanu v\u00E1penat\u00E9ho a doch\u00E1z\u00ED ke vzniku molekulov\u00FDch vlo\u010Dek krystal\u016F v\u00E1pence, kter\u00E9 se pohybuj\u00ED v povrchov\u00E9 blance kapky a hrom"@cs . "Macarr\u00F3 (espeleotema)"@ca . "Un macarr\u00F3, o estalactita fistulosa, \u00E9s un espeleotema consistent en una fina i delicada estalactita en el qual no existeix creixement secundari de cristalls perpendicular al canal primari, cosa que passa quan el degoteig de l'aigua \u00E9s lent per\u00F2 constant. La gruixa no passa habitualment dels 8 mm i la gruixa de les parets oscil\u00B7la entre els 0,1 mm i els 0,5 mm, i pot arribar a longituds de diversos metres."@ca . . . . . . "594913"^^ . . . . . .