. . . . . "Slate"@en . . . . . "Batu sabak (slate) adalah batuan metamorf homogen berbutir halus yang berfoliasi dan berasal dari batuan asal berupa batuan sedimen bertipe menyerpih yang terdiri dari lempung atau abu vulkanik yang mengalami metamorfisme regional berderajat rendah. Ini adalah batuan metamorf foliasi berbutir paling halus. Foliasi mungkin berhubungan dengan perlapisan sedimen asal, tetapi berbentuk bidang - bidang yang tegak lurus dengan arah kompresi metamorfik."@in . . . . . "La llicorella o llosa, sovint tamb\u00E9 anomenada pissarra, \u00E9s una roca metam\u00F2rfica d'origen sedimentari, de textura granular fina i homog\u00E8nia, formada per la compactaci\u00F3 d'argiles. \u00C9s d'estructura laminar o foli\u00E0cia (pissarrositat), cosa que permet obtenir-ne lloses planes i primes de forma regular. Es presenta generalment en un color opac blav\u00F3s fosc o grisenc, per\u00F2 n'existeixen varietats vermelles, verdes i d'altres tonalitats. Gr\u00E0cies de la seva impermeabilitat, la llicorella s'utilitza en la construcci\u00F3 de teulades, com a pedra de pavimentaci\u00F3 i fins i tot per a fabricaci\u00F3 d'elements decoratius. La llicorella pot contenir quantitats variables de quars, mica, minerals d'argila i feldespats. Espanya \u00E9s el major productor de llicorelles del m\u00F3n, on destaquen els jaciments d'El Bierzo, Cabrera i Valdeorras (Lle\u00F3 i Ourense), Bernardos (Seg\u00F2via) i Villar del Rey (Badajoz). \u00C9s abundant a tot el Pirineu catal\u00E0. Gal\u00B7les \u00E9s una de les zones amb m\u00E9s tradici\u00F3 i producci\u00F3. A Europa tamb\u00E9 hi ha importants pedreres a Portugal, It\u00E0lia o Alemanya. A Am\u00E8rica del Nord les zones de producci\u00F3 m\u00E9s importants es troben a Terranova (Canad\u00E0), la vall de la llicorella a Vermont i Nova York, i el comtat de Buckingham a Virg\u00EDnia. La llosa de llicorella de qu\u00E8 es fan els o cobertes de les cases \u00E9s dita llosarda al Conflent i Cerdanya."@ca . . . . . . . . "Skiffer \u00E4r en bergart som kan vara metamorf eller sediment\u00E4r. Namnet skiffer kommer av medell\u00E5gtyskans schever eller tyskans Schiefer. Den best\u00E5r av finkornigt klastiskt sediment.. Stenhuggare har anv\u00E4nt ordet skiffer i bredare betydelse \u00E4n geologer, det har syftat till all typ av sten som g\u00E5tt att klyva f\u00F6r att anv\u00E4nda till tak. Ett exempel p\u00E5 en sten som kallats skiffer av stenhuggare \u00E4r en kallad fr\u00E5n Oxfordshire i England. F\u00F6r en exakt ben\u00E4mning p\u00E5 en skiffer anv\u00E4nds namn som beskriver de viktigaste mineralen som ing\u00E5r. En vanlig typ av s\u00E5dan skiffer \u00E4r , en annan sort \u00E4r talk-tremolitmagnetitskiffer."@sv . "Ardesia"@it . . . . . . "Carraig mh\u00EDnghr\u00E1inn\u00EDneach mheiteamorfach ar f\u00E9idir a scoilteadh go foirfe mar go bhfuil ail\u00EDni\u00FA comhthreomhar ag na criostail m\u00EDoca inti. Is toradh ar strus d\u00EDrithe \u00E9 seo le linn meiteamorf\u00FA \u00E1iti\u00FAil \u00EDsealghr\u00E1id an scealla n\u00F3 na l\u00E1ibchloiche. \u00DAs\u00E1idtear i gcomhair d\u00EDonta \u00ED agus \u00ED scoilte i leath\u00E1in thana\u00ED, agus is buanseasmhach \u00E9adrom \u00ED. T\u00E1 foins\u00ED i gContae an Chl\u00E1ir agus an Bhreatain Bheag."@ga . . . "Ardoise"@fr . . . . . . . "Slate is a fine-grained, foliated, homogeneous metamorphic rock derived from an original shale-type sedimentary rock composed of clay or volcanic ash through low-grade regional metamorphism. It is the finest grained foliated metamorphic rock. Foliation may not correspond to the original sedimentary layering, but instead is in planes perpendicular to the direction of metamorphic compression."@en . . . . . . "Slate"@en . . . . . . . . . . . "Metamorphic Rock"@en . "Pizarra (roca)"@es . . . . "\uC810\uD310\uC554(\u7C98\u677F\u5CA9)\uC740 \uC810\uD1A0\uAC00 \uAD73\uC5B4\uC11C \uB41C \uAC80\uC740 \uBE5B\uAE54\uC758 \uCE58\uBC00\uD55C \uBCC0\uC131\uC554\uC774\uB2E4. \uC2AC\uB808\uC774\uD2B8 \uC11D\uD310, \uBCBC\uB8FB\uB3CC \uB530\uC704\uC5D0 \uC0AC\uC6A9\uD55C\uB2E4."@ko . . . . . . "\u7C98\u677F\u5CA9\uFF08\u306D\u3093\u3070\u3093\u304C\u3093\u3001\u82F1: slate\u3001\u30B9\u30EC\u30FC\u30C8\uFF09\u3068\u306F\u3001\u6CE5\u5CA9\u3084\u9801\u5CA9\u304C\u306B\u3088\u308A\u30B9\u30EC\u30FC\u30C8\u5288\u958B\u3092\u6301\u3063\u305F\u3082\u306E\u3002\u5806\u7A4D\u5CA9\u304C\u3084\u3084\u5909\u6210\u4F5C\u7528\u3092\u53D7\u3051\u305F\u3082\u306E\u3002\u5143\u3005\u306E\u5806\u7A4D\u9762\u3067\u306F\u306A\u304F\u5727\u5BC6\u4F5C\u7528\u306B\u5782\u76F4\u306B\u8584\u304F\u306F\u304C\u308C\u308B\u3002\u77F3\u82F1\u30FB\u96F2\u6BCD\u30FB\u7C98\u571F\u9271\u7269\u30FB\u9577\u77F3\u30FB\u8D64\u9244\u9271\u30FB\u9EC4\u9244\u9271\u306A\u3069\u304C\u542B\u307E\u308C\u308B\u3002"@ja . . "Skiffer \u00E4r en bergart som kan vara metamorf eller sediment\u00E4r. Namnet skiffer kommer av medell\u00E5gtyskans schever eller tyskans Schiefer. Den best\u00E5r av finkornigt klastiskt sediment.. Stenhuggare har anv\u00E4nt ordet skiffer i bredare betydelse \u00E4n geologer, det har syftat till all typ av sten som g\u00E5tt att klyva f\u00F6r att anv\u00E4nda till tak. Ett exempel p\u00E5 en sten som kallats skiffer av stenhuggare \u00E4r en kallad fr\u00E5n Oxfordshire i England."@sv . . . . . . . . . "Ardezo"@eo . . . "Arbela metamorfismo gradu baxuko harri metamorfiko bat da. Pikor tamaina txikia du eta jatorrian tupa edo errautsez osatutako materialen metamorfismoaz sortu da. Arroka foliatua, baina foliazio horrek ez du zertan hasierako sedimentazio estratifikazioarekin bat egin behar."@eu . . . "Tonschiefer"@de . "\u0623\u0631\u062F\u0648\u0627\u0632"@ar . . . . . . . . . . . . . . . . . "Batu sabak"@in . . . . "L\u2019ardoise est une roche m\u00E9tamorphique issue d'une argile ayant subi un m\u00E9tamorphisme g\u00E9n\u00E9ral faible. Elle appartient \u00E0 la famille des schistes \u00E0 l'int\u00E9rieur de laquelle elle se distingue par la qualit\u00E9 de son grain, tr\u00E8s fin et homog\u00E8ne, et sa fissilit\u00E9 : sa capacit\u00E9 \u00E0 se fendre en raison de sa schistosit\u00E9 dans le sens de la s\u00E9dimentation. Ces propri\u00E9t\u00E9s font qu'on peut l'utiliser comme mat\u00E9riau de couverture. L'ardoise est r\u00E9sistante et sa couleur peut varier du blanc au noir, en passant par toutes sortes de gris, de rouges sombres et de verts. Elle a un aspect lustr\u00E9 en raison de la pr\u00E9sence de petits micas blancs embryonnaires (vari\u00E9t\u00E9 appel\u00E9e s\u00E9ricite) issus de la transformation min\u00E9ralogique des argiles en schistes ardoisiers. L'ardoise de couverture peut \u00EAtre droite (rectangulaire) ou en forme d'\u00E9caille. Son \u00E9paisseur varie de 3 \u00E0 9 mm. Entre 20 et 40 mm, il s'agit de lauze, autre schiste plus massif et moins cisaill\u00E9. La pose \u00E0 l'ancienne est la pose au clou. Fin XIXe si\u00E8cle, appara\u00EEt la pose sur crochet."@fr . . "L'ard\u00E8sia (detta anche pietra di Lavagna) \u00E8 una roccia metamorfica di origine sedimentaria (Metamarna in facies pumpellyite-attinolite). Si tratta di una variet\u00E0 di scisti calcareo-argillosi facilmente divisibili in lastre sottili, piane, leggere, impermeabili e resistenti agli agenti atmosferici, derivanti da metamorfismo di basso grado di rocce sedimentarie formate dalla deposizione di un limo finissimo (marna) dovuto all'erosione di antichi rilievi. L'ardesia \u00E8 una roccia classificata come tenera o semi-dura. \u00C8 una pietra compatta, di colore plumbeo-nerastra e facilmente lavorabile."@it . . "\u0627\u0644\u0623\u0631\u062F\u0648\u0627\u0632 \u0623\u0648 \u062D\u062C\u0631 \u0633\u062C\u064A\u0644 (\u0628\u0627\u0644\u0625\u0646\u062C\u0644\u064A\u0632\u064A\u0629: Slate)\u200F \u0647\u0648 \u0635\u062E\u0631 \u0635\u0641\u0627\u0626\u062D\u064A\u060C \u0623\u0648 \u062D\u0628\u064A\u0628\u0627\u062A \u0645\u0646 \u0627\u0644\u0635\u062E\u0631 \u0627\u0644\u0645\u0631\u0642\u0642\u060C \u0648\u0647\u0648 \u0646\u0648\u0639 \u0645\u0646 \u0627\u0644\u0635\u062E\u0648\u0631 \u0627\u0644\u0645\u062A\u062D\u0648\u0644\u0629\u060C \u062A\u0643\u0648\u0646\u062A \u0645\u0646 \u0627\u0644\u0637\u064A\u0646\u060C \u0623\u0648 \u0645\u0646 \u0627\u0644\u0631\u0645\u0627\u062F \u0627\u0644\u0628\u0631\u0643\u0627\u0646\u064A\u060C \u0639\u0628\u0631 \u0645\u0644\u0627\u064A\u064A\u0646 \u0627\u0644\u0633\u0646\u064A\u0646. \u0648\u0627\u0644\u0646\u062A\u064A\u062C\u0629 \u0647\u064A \u0635\u062E\u0648\u0631 \u0645\u0631\u0642\u0642\u0629 \u0643\u0623\u0648\u0631\u0627\u0642 \u0627\u0644\u0634\u062C\u0631 . \u0641\u064A \u0643\u062B\u064A\u0631 \u0645\u0646 \u0627\u0644\u0623\u062D\u064A\u0627\u0646 \u0631\u0645\u0627\u062F\u064A \u0627\u0644\u0644\u0648\u0646. \u0646\u0633\u062A\u062E\u062F\u0645\u0647 \u0641\u064A \u0635\u0646\u0627\u0639\u0629 \u0623\u0644\u0648\u0627\u062D \u0627\u0644\u0623\u0631\u062F\u0648\u0627\u0632 . \u0648\u0641\u064A \u0627\u0644\u0645\u0646\u0627\u0637\u0642 \u0627\u0644\u0623\u0648\u0631\u0648\u0628\u064A\u0629 \u0627\u0644\u062A\u064A \u064A\u0643\u062B\u0631 \u0641\u064A\u0647\u0627 \u064A\u0633\u062A\u062E\u062F\u0645 \u0643\u0623\u0644\u0648\u0627\u062D \u0645\u0646\u062A\u0638\u0645\u0629 \u0644\u062A\u063A\u0637\u064A\u0629 \u0623\u0633\u0642\u0641 \u0627\u0644\u0645\u0646\u0627\u0632\u0644\u060C \u0648\u0623\u062D\u064A\u0627\u0646\u0627\u064B \u064A\u063A\u0637\u0649 \u0645\u0628\u0646\u0649 \u0627\u0644\u0628\u064A\u062A \u0643\u0644\u0647 \u0645\u0646\u0647\u0627. \u064A\u0648\u062C\u062F \u0627\u0644\u0633\u062C\u064A\u0644 \u0627\u0644\u0646\u0641\u0637\u064A \u0641\u064A \u0627\u0644\u0648\u0644\u0627\u064A\u0627\u062A \u0627\u0644\u0645\u062A\u062D\u062F\u0629 \u0648\u0641\u064A \u0643\u0646\u062F\u0627 \u0648\u064A\u0633\u062A\u062E\u0631\u062C \u0645\u0646\u0647 \u0627\u0644\u0646\u0641\u0637 \u0648\u0627\u0644\u063A\u0627\u0632 \u0627\u0644\u0637\u0628\u064A\u0639\u064A."@ar . . . . . . "Batu sabak (slate) adalah batuan metamorf homogen berbutir halus yang berfoliasi dan berasal dari batuan asal berupa batuan sedimen bertipe menyerpih yang terdiri dari lempung atau abu vulkanik yang mengalami metamorfisme regional berderajat rendah. Ini adalah batuan metamorf foliasi berbutir paling halus. Foliasi mungkin berhubungan dengan perlapisan sedimen asal, tetapi berbentuk bidang - bidang yang tegak lurus dengan arah kompresi metamorfik. Foliasi yang sangat kuat disebut juga \"Belahan sabak\". Foliasi ini disebabkan oleh kompresi yang kuat yang menyebabkan lempung berbutir halus menyerpih dan tumbuh kembali dalam bentuk bidang - bidang yang tegak lurus dengan kompresi. Ketika para ahli memotong tepat sejajar dengan foliasi menggunakan alat - alat khusus, banyak batusabak akan membentuk lapisan - lapisan datar batuan yang telah sejak lama digunakan sebagai bahan atap, ubin lantai, dan tujuan lain. Batusabak biasanya berwarna abu - abu, terutama yang biasa terlihat sebagai penutup atap. Meskipun begitu, batusabak dapat terbentuk dalam warna yang bermacam - macam bahkan dapat berwarna khas pada satu tempat saja. Batusabak berbeda dengan batuserpih."@in . . "Ard\u00F3sia"@pt . . . . . . . . "\uC810\uD310\uC554"@ko . "\u0627\u0644\u0623\u0631\u062F\u0648\u0627\u0632 \u0623\u0648 \u062D\u062C\u0631 \u0633\u062C\u064A\u0644 (\u0628\u0627\u0644\u0625\u0646\u062C\u0644\u064A\u0632\u064A\u0629: Slate)\u200F \u0647\u0648 \u0635\u062E\u0631 \u0635\u0641\u0627\u0626\u062D\u064A\u060C \u0623\u0648 \u062D\u0628\u064A\u0628\u0627\u062A \u0645\u0646 \u0627\u0644\u0635\u062E\u0631 \u0627\u0644\u0645\u0631\u0642\u0642\u060C \u0648\u0647\u0648 \u0646\u0648\u0639 \u0645\u0646 \u0627\u0644\u0635\u062E\u0648\u0631 \u0627\u0644\u0645\u062A\u062D\u0648\u0644\u0629\u060C \u062A\u0643\u0648\u0646\u062A \u0645\u0646 \u0627\u0644\u0637\u064A\u0646\u060C \u0623\u0648 \u0645\u0646 \u0627\u0644\u0631\u0645\u0627\u062F \u0627\u0644\u0628\u0631\u0643\u0627\u0646\u064A\u060C \u0639\u0628\u0631 \u0645\u0644\u0627\u064A\u064A\u0646 \u0627\u0644\u0633\u0646\u064A\u0646. \u0648\u0627\u0644\u0646\u062A\u064A\u062C\u0629 \u0647\u064A \u0635\u062E\u0648\u0631 \u0645\u0631\u0642\u0642\u0629 \u0643\u0623\u0648\u0631\u0627\u0642 \u0627\u0644\u0634\u062C\u0631 . \u0641\u064A \u0643\u062B\u064A\u0631 \u0645\u0646 \u0627\u0644\u0623\u062D\u064A\u0627\u0646 \u0631\u0645\u0627\u062F\u064A \u0627\u0644\u0644\u0648\u0646. \u0646\u0633\u062A\u062E\u062F\u0645\u0647 \u0641\u064A \u0635\u0646\u0627\u0639\u0629 \u0623\u0644\u0648\u0627\u062D \u0627\u0644\u0623\u0631\u062F\u0648\u0627\u0632 . \u0648\u0641\u064A \u0627\u0644\u0645\u0646\u0627\u0637\u0642 \u0627\u0644\u0623\u0648\u0631\u0648\u0628\u064A\u0629 \u0627\u0644\u062A\u064A \u064A\u0643\u062B\u0631 \u0641\u064A\u0647\u0627 \u064A\u0633\u062A\u062E\u062F\u0645 \u0643\u0623\u0644\u0648\u0627\u062D \u0645\u0646\u062A\u0638\u0645\u0629 \u0644\u062A\u063A\u0637\u064A\u0629 \u0623\u0633\u0642\u0641 \u0627\u0644\u0645\u0646\u0627\u0632\u0644\u060C \u0648\u0623\u062D\u064A\u0627\u0646\u0627\u064B \u064A\u063A\u0637\u0649 \u0645\u0628\u0646\u0649 \u0627\u0644\u0628\u064A\u062A \u0643\u0644\u0647 \u0645\u0646\u0647\u0627. \u0645\u0646 \u0646\u0648\u0639 \u062D\u062C\u0631 \u0627\u0644\u0633\u062C\u064A\u0644 \u064A\u0648\u062C\u062F \u0633\u062C\u064A\u0644 \u0632\u064A\u062A\u064A \u0648\u0647\u0648 \u0645\u0627\u062F\u0629 \u0635\u0644\u0628\u0629 \u062A\u062D\u062A\u0648\u064A \u0628\u0630\u0627\u062A\u0647\u0627 \u0639\u0644\u0649 \u0645\u0648\u0627\u062F \u0639\u0636\u0648\u064A\u0629 \u0646\u0628\u0627\u062A\u064A\u0629 \u0648\u062D\u064A\u0648\u0627\u0646\u064A\u0629 \u062A\u0633\u0645\u0649 \u0627\u0644\u0643\u064A\u0631\u0648\u062C\u064A\u0646\u060C \u0648\u064A\u062A\u062D\u0648\u0644 \u0628\u0627\u0644\u062A\u0633\u062E\u064A\u0646 \u0625\u0644\u0649 \u0646\u0641\u0637 \u063A\u064A\u0631 \u062A\u0642\u0644\u064A\u062F\u064A. \u064A\u062F\u062E\u0644 \u0641\u064A \u062A\u0631\u0643\u064A\u0628 \u0627\u0644\u0633\u062C\u064A\u0644 \u0627\u0644\u0632\u064A\u062A\u064A \u0645\u0639\u0638\u0645 \u0645\u0643\u0648\u0646\u0627\u062A \u0627\u0644\u0646\u0641\u0637 \u0628\u062F\u0621\u0627\u064B \u0645\u0646 \u0627\u0644\u063A\u0627\u0632 \u0648\u0627\u0646\u062A\u0647\u0627\u0621\u064B \u0628\u0627\u0644\u0628\u064A\u062A\u0648\u0645\u064A\u0646\u060C \u0645\u0639\u062A\u0628\u0631\u0627\u064B \u0623\u0646\u0647 \u0645\u0646 \u0623\u0647\u0645 \u0627\u0644\u0628\u062F\u0627\u0626\u0644 \u0627\u0644\u0645\u0633\u062A\u0642\u0628\u0644\u064A\u0629 \u0644\u0625\u0646\u062A\u0627\u062C \u0627\u0644\u0637\u0627\u0642\u0629 \u0648\u0642\u064A\u0627\u0645 \u0627\u0644\u0635\u0646\u0627\u0639\u0627\u062A \u0627\u0644\u0628\u062A\u0631\u0648\u0643\u064A\u0645\u0627\u0648\u064A\u0629. \u064A\u0648\u062C\u062F \u0627\u0644\u0633\u062C\u064A\u0644 \u0627\u0644\u0646\u0641\u0637\u064A \u0641\u064A \u0627\u0644\u0648\u0644\u0627\u064A\u0627\u062A \u0627\u0644\u0645\u062A\u062D\u062F\u0629 \u0648\u0641\u064A \u0643\u0646\u062F\u0627 \u0648\u064A\u0633\u062A\u062E\u0631\u062C \u0645\u0646\u0647 \u0627\u0644\u0646\u0641\u0637 \u0648\u0627\u0644\u063A\u0627\u0632 \u0627\u0644\u0637\u0628\u064A\u0639\u064A."@ar . . . "1122991749"^^ . "Carraig mh\u00EDnghr\u00E1inn\u00EDneach mheiteamorfach ar f\u00E9idir a scoilteadh go foirfe mar go bhfuil ail\u00EDni\u00FA comhthreomhar ag na criostail m\u00EDoca inti. Is toradh ar strus d\u00EDrithe \u00E9 seo le linn meiteamorf\u00FA \u00E1iti\u00FAil \u00EDsealghr\u00E1id an scealla n\u00F3 na l\u00E1ibchloiche. \u00DAs\u00E1idtear i gcomhair d\u00EDonta \u00ED agus \u00ED scoilte i leath\u00E1in thana\u00ED, agus is buanseasmhach \u00E9adrom \u00ED. T\u00E1 foins\u00ED i gContae an Chl\u00E1ir agus an Bhreatain Bheag."@ga . . "La llicorella o llosa, sovint tamb\u00E9 anomenada pissarra, \u00E9s una roca metam\u00F2rfica d'origen sedimentari, de textura granular fina i homog\u00E8nia, formada per la compactaci\u00F3 d'argiles. \u00C9s d'estructura laminar o foli\u00E0cia (pissarrositat), cosa que permet obtenir-ne lloses planes i primes de forma regular. Es presenta generalment en un color opac blav\u00F3s fosc o grisenc, per\u00F2 n'existeixen varietats vermelles, verdes i d'altres tonalitats. La llosa de llicorella de qu\u00E8 es fan els o cobertes de les cases \u00E9s dita llosarda al Conflent i Cerdanya."@ca . . . . . . . . . . . . "A ard\u00F3sia \u00E9 uma rocha metam\u00F3rfica s\u00EDlico-argilosa formada pela transforma\u00E7\u00E3o da argila sob press\u00E3o e temperatura, endurecida em finas lamelas. De baixo grau metam\u00F3rfico, a ard\u00F3sia \u00E9 formada sob as menores press\u00F5es e temperaturas dentre as rochas metam\u00F3rficas. Algumas das mais finas ard\u00F3sias do mundo t\u00EAm origem em Campo (Valongo) em Portugal, Pequim na China, Esc\u00F3cia, em Vermont e Nova York nos Estados Unidos."@pt . . . . "La pizarra es una roca metam\u00F3rfica homog\u00E9nea de grano fino formada por la compactaci\u00F3n por metamorfismo de bajo grado de lutitas.\u200B Se presenta generalmente de color opaco azulado oscuro y estructurada en lajas u hojas planas por una esquistosidad bien desarrollada (pizarrosidad), siendo, por esta caracter\u00EDstica, utilizada en cubiertas y como antiguo elemento de escritura. Debido a su impermeabilidad, la pizarra se utiliza en la construcci\u00F3n de tejados, como piedra de pavimentaci\u00F3n, mesas de billar,\u200B e incluso para fabricaci\u00F3n de elementos decorativos.\u200B"@es . "Llicorella"@ca . . . . . . "Ardezo estas speco de roko, fendi\u011Danta en platajn tavolojn, uzatajn i.a. por fari tegmenton. \u011Cia koloro estas grizblua. Ardeza tabuleto estis uzata iam de junaj lernantoj por skribado. La\u016D Francisko Azor\u00EDn Ardezo estas Duonenigra \u015Dtono facile disigebla en tavoloj, uzata por kovri tegmentojn, k.c. Li indikas etimologion el Ardeso, propra nomo de Irlanda regiono."@eo . "Slinn"@ga . "44214"^^ . . "\u677F\u5CA9\uFF0C\u5176\u7ED3\u6784\u6709\u3001\uFF0C\u6784\u9020\u4E3A\u3002\u57FA\u672C\u6CA1\u6709\u91CD\u7ED3\u6676\u7684\u5CA9\u77F3\uFF0C\u662F\u4E00\u79CD\u53D8\u8D28\u5CA9\uFF0C\u539F\u5CA9\u4E3A\u9875\u5CA9\u3001\u6CE5\u5CA9\u3001\u7C89\u7802\u5CA9\u6216\u4E2D\u6027\u51DD\u7070\u5CA9\uFF0C\u6CBF\u65B9\u5411\u53EF\u4EE5\u5265\u6210\u8584\u7247\u3002\u677F\u5CA9\u7684\u989C\u8272\u968F\u5176\u6240\u542B\u6709\u7684\u7926\u7269\u4E0D\u540C\u800C\u53D8\u5316\uFF0C\u542B\u94C1\u7684\u4E3A\u7EA2\u8272\u6216\u9EC4\u8272\uFF1B\u542B\u78B3\u8D28\u7684\u4E3A\u9ED1\u8272\u6216\u7070\u8272\uFF1B\u542B\u9499\u8CEA\u7684\u9047\u76D0\u9178\u4F1A\u8D77\u6CE1\u3002\u4E00\u822C\u4EE5\u5176\u989C\u8272\u6216\u6210\u5206\u547D\u540D\u5206\u985E\uFF0C\u4EE5\u989C\u8272\u5206\u7C7B\u5982\uFF1A\u7EFF\u8272\u677F\u5CA9\u3001\u9ED1\u8272\u677F\u5CA9\u7B49\uFF0C\u4EE5\u6210\u5206\u5206\u7C7B\u5982\uFF1A\u9499\u8D28\u677F\u5CA9\u3001\u70AD\u8D28\u677F\u5CA9\u3001\u51DD\u7070\u8D28\u677F\u5CA9\u7B49\u3002 \u5728\u677F\u5CA9\u542B\u91CF\u8C50\u5BCC\u7684\u5730\u533A\uFF0C\u677F\u5CA9\u7D93\u5E38\u7528\u6765\u4F5C\u4E3A\u5C4B\u9876\u7684\u74E6\u4F7F\u7528\uFF0C\u4E5F\u53EF\u88FD\u6210\u66F8\u5BEB\u7528\u7684\u5C0F\u9ED1\u677F\u3002"@zh . . . . . . . . "A ard\u00F3sia \u00E9 uma rocha metam\u00F3rfica s\u00EDlico-argilosa formada pela transforma\u00E7\u00E3o da argila sob press\u00E3o e temperatura, endurecida em finas lamelas. De baixo grau metam\u00F3rfico, a ard\u00F3sia \u00E9 formada sob as menores press\u00F5es e temperaturas dentre as rochas metam\u00F3rficas. A ard\u00F3sia pode ser transformada em soletos, porque tem duas linhas de folhabilidade: clivagem e gr\u00E3o. Isto torna poss\u00EDvel que se divida em finas folhas. Coberturas sint\u00E9ticas e manufaturadas podem, inicialmente, ser mais baratas no acto da coloca\u00E7\u00E3o, mas os soletos de ard\u00F3sia durar\u00E3o muitos e muitos anos, fazendo deste material uma escolha de futuro mais econ\u00F4mica. A ard\u00F3sia \u00E9 uma rocha metam\u00F3rfica.Outras aplica\u00E7\u00F5es da ard\u00F3sia: pavimentos, fachadas, tampos de laborat\u00F3rios, e em decora\u00E7\u00F5es interiores e exteriores. Folhas finas de ard\u00F3sia preta ou cinza escuro eram o material mais usado na produ\u00E7\u00E3o de quadros negros, ou lousa. Hoje em dia, com o surgimento de materiais mais adequados, a ard\u00F3sia deixou de ser usada para esse prop\u00F3sito. Algumas das mais finas ard\u00F3sias do mundo t\u00EAm origem em Campo (Valongo) em Portugal, Pequim na China, Esc\u00F3cia, em Vermont e Nova York nos Estados Unidos."@pt . . . . . . . . . . . "Leisteen"@nl . . . . . . . "Slate is a fine-grained, foliated, homogeneous metamorphic rock derived from an original shale-type sedimentary rock composed of clay or volcanic ash through low-grade regional metamorphism. It is the finest grained foliated metamorphic rock. Foliation may not correspond to the original sedimentary layering, but instead is in planes perpendicular to the direction of metamorphic compression. The foliation in slate is called \"slaty cleavage\". It is caused by strong compression causing fine grained clay flakes to regrow in planes perpendicular to the compression. When expertly \"cut\" by striking parallel to the foliation, with a specialized tool in the quarry, many slates will display a property called fissility, forming smooth flat sheets of stone which have long been used for roofing, floor tiles, and other purposes. Slate is frequently grey in color, especially when seen, en masse, covering roofs. However, slate occurs in a variety of colors even from a single locality; for example, slate from North Wales can be found in many shades of grey, from pale to dark, and may also be purple, green or cyan. Slate is not to be confused with shale, from which it may be formed, or schist. The word \"slate\" is also used for certain types of object made from slate rock. It may mean a single roofing tile made of slate, or a writing slate. They were traditionally a small, smooth piece of the rock, often framed in wood, used with chalk as a notepad or notice board, and especially for recording charges in pubs and inns. The phrases \"clean slate\" and \"blank slate\" come from this usage."@en . "Skiffer"@sv . . . . . . "\u677F\u5CA9"@zh . . . "Ardezo estas speco de roko, fendi\u011Danta en platajn tavolojn, uzatajn i.a. por fari tegmenton. \u011Cia koloro estas grizblua. Ardeza tabuleto estis uzata iam de junaj lernantoj por skribado. La\u016D Francisko Azor\u00EDn Ardezo estas Duonenigra \u015Dtono facile disigebla en tavoloj, uzata por kovri tegmentojn, k.c. Li indikas etimologion el Ardeso, propra nomo de Irlanda regiono."@eo . . . . . . . . . . . . . . . . "La pizarra es una roca metam\u00F3rfica homog\u00E9nea de grano fino formada por la compactaci\u00F3n por metamorfismo de bajo grado de lutitas.\u200B Se presenta generalmente de color opaco azulado oscuro y estructurada en lajas u hojas planas por una esquistosidad bien desarrollada (pizarrosidad), siendo, por esta caracter\u00EDstica, utilizada en cubiertas y como antiguo elemento de escritura. La pizarra es una roca densa, de grano fino, formada a partir de rocas sedimentarias arcillosas y, en algunas ocasiones, de rocas \u00EDgneas. La principal caracter\u00EDstica de la pizarra es su divisi\u00F3n en finas l\u00E1minas o capas (fisibilidad). Los minerales que la forman son principalmente sericita, moscovita, clorita y cuarzo.\u200B Suele ser de color negro azulado o negro gris\u00E1ceo, pero existen variedades rojas, verdes y otros tonos. Debido a su impermeabilidad, la pizarra se utiliza en la construcci\u00F3n de tejados, como piedra de pavimentaci\u00F3n, mesas de billar,\u200B e incluso para fabricaci\u00F3n de elementos decorativos.\u200B La launa es una arcilla magn\u00E9sica de estructura pizarrosa y color gris azulado, que resulta de la descomposici\u00F3n de las pizarras arcillosas."@es . . "\uC810\uD310\uC554(\u7C98\u677F\u5CA9)\uC740 \uC810\uD1A0\uAC00 \uAD73\uC5B4\uC11C \uB41C \uAC80\uC740 \uBE5B\uAE54\uC758 \uCE58\uBC00\uD55C \uBCC0\uC131\uC554\uC774\uB2E4. \uC2AC\uB808\uC774\uD2B8 \uC11D\uD310, \uBCBC\uB8FB\uB3CC \uB530\uC704\uC5D0 \uC0AC\uC6A9\uD55C\uB2E4."@ko . . . . . . "26208"^^ . . . . . . "\u0410\u0441\u043F\u0438\u0434\u043D\u044B\u0439 \u0441\u043B\u0430\u043D\u0435\u0446"@ru . . . . "Leisteen of schiefer (Engels: slate; Duits: Schiefer) is een metamorf gesteente dat gekenmerkt wordt door een duidelijke, dominante foliatie van afwisselende laagjes kwarts met veldspaat en laagjes mica. Dankzij deze foliatie heeft leisteen een sterke splijting en verbrokkelt het in dunne, plaatvormige brokken. Leisteen wordt in de natuur gevormd door de metamorfose van kleirijk sediment, zoals schalie of kleisteen. Het wordt veel als dakbedekking gebruikt, zeker in gebieden waar het aan het oppervlak voorkomt, zoals in het zuiden van Belgi\u00EB en aangrenzende delen van Duitsland. Leisteen is daar gemakkelijk te winnen."@nl . . . . . . "Arbel"@eu . . . . . "Slate"@en . . . . . . "\u7C98\u677F\u5CA9"@ja . . . . . . . . . . . "L'ard\u00E8sia (detta anche pietra di Lavagna) \u00E8 una roccia metamorfica di origine sedimentaria (Metamarna in facies pumpellyite-attinolite). Si tratta di una variet\u00E0 di scisti calcareo-argillosi facilmente divisibili in lastre sottili, piane, leggere, impermeabili e resistenti agli agenti atmosferici, derivanti da metamorfismo di basso grado di rocce sedimentarie formate dalla deposizione di un limo finissimo (marna) dovuto all'erosione di antichi rilievi. L'ardesia \u00E8 una roccia classificata come tenera o semi-dura. \u00C8 una pietra compatta, di colore plumbeo-nerastra e facilmente lavorabile. L'ardesia tende a schiarirsi dal momento dell'estrazione fino ad assumere una pigmentazione grigio chiara, la tonalit\u00E0 scura essendo dovuta a residui carboniosi che si ossidano una volta a contatto con ossigeno, umidit\u00E0 e radiazioni ultraviolette. In virt\u00F9 della propria scistosit\u00E0 (ovvero la capacit\u00E0 di dividersi in lastre secondo i piani di clivaggio dovuti alla sua foliazione) e propriet\u00E0, pu\u00F2 essere impiegata in vari segmenti artigianali e industriali tanto dell'architettura e dell'edilizia (per la realizzazione di tetti, pavimentazioni, gradoni di scale) quanto in arte nel design e dell'oggettistica di uso quotidiano."@it . . . . . . "L\u2019ardoise est une roche m\u00E9tamorphique issue d'une argile ayant subi un m\u00E9tamorphisme g\u00E9n\u00E9ral faible. Elle appartient \u00E0 la famille des schistes \u00E0 l'int\u00E9rieur de laquelle elle se distingue par la qualit\u00E9 de son grain, tr\u00E8s fin et homog\u00E8ne, et sa fissilit\u00E9 : sa capacit\u00E9 \u00E0 se fendre en raison de sa schistosit\u00E9 dans le sens de la s\u00E9dimentation. Ces propri\u00E9t\u00E9s font qu'on peut l'utiliser comme mat\u00E9riau de couverture."@fr . "\u7C98\u677F\u5CA9\uFF08\u306D\u3093\u3070\u3093\u304C\u3093\u3001\u82F1: slate\u3001\u30B9\u30EC\u30FC\u30C8\uFF09\u3068\u306F\u3001\u6CE5\u5CA9\u3084\u9801\u5CA9\u304C\u306B\u3088\u308A\u30B9\u30EC\u30FC\u30C8\u5288\u958B\u3092\u6301\u3063\u305F\u3082\u306E\u3002\u5806\u7A4D\u5CA9\u304C\u3084\u3084\u5909\u6210\u4F5C\u7528\u3092\u53D7\u3051\u305F\u3082\u306E\u3002\u5143\u3005\u306E\u5806\u7A4D\u9762\u3067\u306F\u306A\u304F\u5727\u5BC6\u4F5C\u7528\u306B\u5782\u76F4\u306B\u8584\u304F\u306F\u304C\u308C\u308B\u3002\u77F3\u82F1\u30FB\u96F2\u6BCD\u30FB\u7C98\u571F\u9271\u7269\u30FB\u9577\u77F3\u30FB\u8D64\u9244\u9271\u30FB\u9EC4\u9244\u9271\u306A\u3069\u304C\u542B\u307E\u308C\u308B\u3002"@ja . . . . . . . . "biotite, chlorite, hematite, pyrite\nSpecific gravity: 2.7 \u2013 2.8,2.9"@en . . . . . . . . . . . . . . . . "Arbela metamorfismo gradu baxuko harri metamorfiko bat da. Pikor tamaina txikia du eta jatorrian tupa edo errautsez osatutako materialen metamorfismoaz sortu da. Arroka foliatua, baina foliazio horrek ez du zertan hasierako sedimentazio estratifikazioarekin bat egin behar."@eu . . . "Metamorphic"@en . . . . . . . . "\u677F\u5CA9\uFF0C\u5176\u7ED3\u6784\u6709\u3001\uFF0C\u6784\u9020\u4E3A\u3002\u57FA\u672C\u6CA1\u6709\u91CD\u7ED3\u6676\u7684\u5CA9\u77F3\uFF0C\u662F\u4E00\u79CD\u53D8\u8D28\u5CA9\uFF0C\u539F\u5CA9\u4E3A\u9875\u5CA9\u3001\u6CE5\u5CA9\u3001\u7C89\u7802\u5CA9\u6216\u4E2D\u6027\u51DD\u7070\u5CA9\uFF0C\u6CBF\u65B9\u5411\u53EF\u4EE5\u5265\u6210\u8584\u7247\u3002\u677F\u5CA9\u7684\u989C\u8272\u968F\u5176\u6240\u542B\u6709\u7684\u7926\u7269\u4E0D\u540C\u800C\u53D8\u5316\uFF0C\u542B\u94C1\u7684\u4E3A\u7EA2\u8272\u6216\u9EC4\u8272\uFF1B\u542B\u78B3\u8D28\u7684\u4E3A\u9ED1\u8272\u6216\u7070\u8272\uFF1B\u542B\u9499\u8CEA\u7684\u9047\u76D0\u9178\u4F1A\u8D77\u6CE1\u3002\u4E00\u822C\u4EE5\u5176\u989C\u8272\u6216\u6210\u5206\u547D\u540D\u5206\u985E\uFF0C\u4EE5\u989C\u8272\u5206\u7C7B\u5982\uFF1A\u7EFF\u8272\u677F\u5CA9\u3001\u9ED1\u8272\u677F\u5CA9\u7B49\uFF0C\u4EE5\u6210\u5206\u5206\u7C7B\u5982\uFF1A\u9499\u8D28\u677F\u5CA9\u3001\u70AD\u8D28\u677F\u5CA9\u3001\u51DD\u7070\u8D28\u677F\u5CA9\u7B49\u3002 \u5728\u677F\u5CA9\u542B\u91CF\u8C50\u5BCC\u7684\u5730\u533A\uFF0C\u677F\u5CA9\u7D93\u5E38\u7528\u6765\u4F5C\u4E3A\u5C4B\u9876\u7684\u74E6\u4F7F\u7528\uFF0C\u4E5F\u53EF\u88FD\u6210\u66F8\u5BEB\u7528\u7684\u5C0F\u9ED1\u677F\u3002"@zh . . . . . . "Leisteen of schiefer (Engels: slate; Duits: Schiefer) is een metamorf gesteente dat gekenmerkt wordt door een duidelijke, dominante foliatie van afwisselende laagjes kwarts met veldspaat en laagjes mica. Dankzij deze foliatie heeft leisteen een sterke splijting en verbrokkelt het in dunne, plaatvormige brokken. Leisteen wordt in de natuur gevormd door de metamorfose van kleirijk sediment, zoals schalie of kleisteen. Het wordt veel als dakbedekking gebruikt, zeker in gebieden waar het aan het oppervlak voorkomt, zoals in het zuiden van Belgi\u00EB en aangrenzende delen van Duitsland. Leisteen is daar gemakkelijk te winnen."@nl . . . . . .