"Agglomerat"@sv . . "Un aglomerado es una roca \u00EDgnea volc\u00E1nica formada casi totalmente de trozos angulares o redondeados de lava, de variadas formas y tama\u00F1os; est\u00E1n asociados con los flujos de lava que se expulsan durante las erupciones volc\u00E1nicas. Algunos ge\u00F3logos clasifican los aglomerados como bombas, y breccia. Parecen conglomerados sedimentarios, pero su origen es completamente diferente.[cita requerida] Las bombas volc\u00E1nicas son expelidas en estado l\u00EDquido, volvi\u00E9ndose esf\u00E9ricas en la solidificaci\u00F3n, y los bloques volc\u00E1nicos brotan como piezas s\u00F3lidas. Durante la aglomeraci\u00F3n y la solidificaci\u00F3n de los fragmentos angulosos, conocidos tambi\u00E9n como pirocl\u00E1sticos, se forman los aglomerados.[cita requerida]"@es . . . . . . . . "El terme aglomerat pot referir-se a un dip\u00F2sit detr\u00EDtic poc o gens cimentat d'element superiors o iguals als 2 mm. Tamb\u00E9 pot referir-se a una acumulaci\u00F3 de blocs no cimentats. Tamb\u00E9 s'anomenen aix\u00F2 les roques pirocl\u00E0stiques on m\u00E9s del 75% dels fragments pirocl\u00E0stics s\u00F3n majors de 64 mm i com a m\u00EDnim el 50% d'aquests s\u00F3n arrodonits."@ca . . . "\u96C6\u584A\u5CA9(\u82F1\u8A9E\uFF1AAgglomerate)\u662F\u706B\u5C71\u904B\u52D5\u6240\u7522\u751F\u7684\u706B\u6210\u5CA9\uFF0C\u901A\u5E38\u70BA\u5927\u578B\u7684\u706B\u5C71\u7269\u8CEA\u7684\u6DF7\u5408\u5CA9\u584A\uFF0C\u591A\u898B\u65BC\u706B\u5C71\u6D3B\u52D5\u7684\u4E2D\u5FC3\u5340\u57DF\u3002\u5B83\u88AB\u5B9A\u7FA9\u70BA\u81F3\u5C11\u542B75%\u7684\u706B\u5C71\u5F48\uFF08Bomb\uFF09\u7684\u5CA9\u77F3\uFF0C\u901A\u5E38\u70BA\u7C97\u7C92\u7684\u6DF7\u5408\u8CEA\u7194\u5CA9\u788E\u584A\u6DF7\u5408\u5728\u706B\u5C71\u7070\u57FA\u8CEA\u4E2D\u3002\u5806\u7A4D\u5728\u706B\u5C71\u53E3\u9644\u8FD1\u3001\u8986\u84CB\u65BC\u706B\u5C71\u5761\u9762\u6216\u6563\u4F48\u65BC\u706B\u5C71\u9644\u8FD1\u4E4B\u5EE3\u5927\u5730\u5340\u4E4B\u706B\u5C71\u788E\u5C51\u7269\uFF0C\u51DD\u56FA\u6210\u5927\u5C0F\u4E0D\u7B49\u4E4B\u5CA9\u584A\uFF0C\u7A31\u706B\u5C71\u788E\u5C51\u5CA9(volcanic breccia)\u6216\u96C6\u584A\u5CA9(agglomerates)\u3002\u96C6\u584A\u5CA9\u4E2D\u4E4B\u5927\u8005\u6BD4\u623F\u5B50\u9084\u5927\uFF0C\u5C0F\u8005\u53EF\u5145\u586B\u65BC\u5927\u5CA9\u584A\u4E4B\u9699\u7E2B\u4E2D\u3002"@zh . "Un aglomerado es una roca \u00EDgnea volc\u00E1nica formada casi totalmente de trozos angulares o redondeados de lava, de variadas formas y tama\u00F1os; est\u00E1n asociados con los flujos de lava que se expulsan durante las erupciones volc\u00E1nicas. Algunos ge\u00F3logos clasifican los aglomerados como bombas, y breccia. Parecen conglomerados sedimentarios, pero su origen es completamente diferente.[cita requerida]"@es . . . . "\u96C6\u584A\u5CA9(\u82F1\u8A9E\uFF1AAgglomerate)\u662F\u706B\u5C71\u904B\u52D5\u6240\u7522\u751F\u7684\u706B\u6210\u5CA9\uFF0C\u901A\u5E38\u70BA\u5927\u578B\u7684\u706B\u5C71\u7269\u8CEA\u7684\u6DF7\u5408\u5CA9\u584A\uFF0C\u591A\u898B\u65BC\u706B\u5C71\u6D3B\u52D5\u7684\u4E2D\u5FC3\u5340\u57DF\u3002\u5B83\u88AB\u5B9A\u7FA9\u70BA\u81F3\u5C11\u542B75%\u7684\u706B\u5C71\u5F48\uFF08Bomb\uFF09\u7684\u5CA9\u77F3\uFF0C\u901A\u5E38\u70BA\u7C97\u7C92\u7684\u6DF7\u5408\u8CEA\u7194\u5CA9\u788E\u584A\u6DF7\u5408\u5728\u706B\u5C71\u7070\u57FA\u8CEA\u4E2D\u3002\u5806\u7A4D\u5728\u706B\u5C71\u53E3\u9644\u8FD1\u3001\u8986\u84CB\u65BC\u706B\u5C71\u5761\u9762\u6216\u6563\u4F48\u65BC\u706B\u5C71\u9644\u8FD1\u4E4B\u5EE3\u5927\u5730\u5340\u4E4B\u706B\u5C71\u788E\u5C51\u7269\uFF0C\u51DD\u56FA\u6210\u5927\u5C0F\u4E0D\u7B49\u4E4B\u5CA9\u584A\uFF0C\u7A31\u706B\u5C71\u788E\u5C51\u5CA9(volcanic breccia)\u6216\u96C6\u584A\u5CA9(agglomerates)\u3002\u96C6\u584A\u5CA9\u4E2D\u4E4B\u5927\u8005\u6BD4\u623F\u5B50\u9084\u5927\uFF0C\u5C0F\u8005\u53EF\u5145\u586B\u65BC\u5927\u5CA9\u584A\u4E4B\u9699\u7E2B\u4E2D\u3002"@zh . . "Agglomerate"@en . . "Vulkanisches Agglomerat"@de . "Ein vulkanisches Agglomerat (lateinisch agglomerare \u201Azusammenballen, anh\u00E4ufen\u2018) ist in der Petrographie ein pyroklastisches Sedimentgestein, das zu mehr als 75 Prozent aus vulkanischen Bomben, also aus den gr\u00F6bsten Pyroklasten (Komponenten > 6,4 Zentimeter), besteht; der Rest kann auch aus Lapilli oder vulkanischen Aschen bestehen. Das vulkanische Agglomerat ist durch die Komponenten, die Korngr\u00F6\u00DFe und den Modalbestand der Komponentengr\u00F6\u00DFe definiert."@de . . . "'Aglomerat (dari bahasa latin agglomerare' yang berarti 'membentuk menjadi bola') merupakan akumulasi kasar blok - blok besar material vulkanik yang mengandung setidaknya 75% . bom vulkanik berbeda dari blok vulkanik dalam hal perekaman permukaan fluidal: bom vulkanik dapat memiliki urat, cauliform, scoriaceous, terlipat, chilled margin dan spindle, bekas hujan rintik-rintik, pita, compang-camping, atau bentuk amuboid. Sebuah massa lava yang bulat mungkin telah terhempas dari kawah pada saat lava cair parsial tersingkap ke permukaan, dan sering hancur oleh ledakan uap yang terjadi secara tiba - tiba. Bom beruwujud kental pada saat keluar dan akibat rotasi di udara diperoleh-lah bentuk yang ada sekarang. Mereka umumnya berdiameter 30 hingga 60 cm, tetapi spesimen besar berukuran 3,7 meter juga telah ditemukan. Komposisinya tidak begitu bervariasi dan komposisinya mengindikasika tipe magma yang menghasilkannya."@in . "1711396"^^ . "Ein vulkanisches Agglomerat (lateinisch agglomerare \u201Azusammenballen, anh\u00E4ufen\u2018) ist in der Petrographie ein pyroklastisches Sedimentgestein, das zu mehr als 75 Prozent aus vulkanischen Bomben, also aus den gr\u00F6bsten Pyroklasten (Komponenten > 6,4 Zentimeter), besteht; der Rest kann auch aus Lapilli oder vulkanischen Aschen bestehen. Das vulkanische Agglomerat ist durch die Komponenten, die Korngr\u00F6\u00DFe und den Modalbestand der Komponentengr\u00F6\u00DFe definiert. Vulkanische Agglomerate sind aber auch h\u00E4ufig durch das Fehlen einer Grundmasse aus feink\u00F6rnigem Material gekennzeichnet, so dass das Gestein eine hohe Porosit\u00E4t aufweist. Vulkanische Bomben haben einen Durchmesser von \u00FCber 6,4 Zentimetern und weisen, anders als vulkanische Bl\u00F6cke, gerundete Formen auf, die darauf hindeuten, dass das Material zur Zeit des Auswurfs noch schmelzfl\u00FCssig war. Sind die Bestandteile beim Auftreffen auf den Boden noch \u00FCberwiegend schmelzfl\u00FCssig, so bilden sich Schwei\u00DFschlacken."@de . . . "Ceirtle\u00E1n"@ga . . "Carraig gharbh bholc\u00E1nach is ea ceirtle\u00E1n, measc\u00E1n de bhl\u00FAir\u00ED den iliomad m\u00E9id is cruth. B\u00EDonn s\u00E9 fosaithe de ghn\u00E1th mar chuid de ch\u00F3n an bholc\u00E1in, d\u00EDorthaithe \u00F3 na carraigeacha ar thaisteal an magma tr\u00EDothu ar a bhealach tr\u00EDd an maintl\u00EDn don dromchla."@ga . . . "Agglomerate (from the Latin agglomerare meaning \"to form into a ball\") is a coarse accumulation of large blocks of volcanic material that contains at least 75% bombs. Volcanic bombs differ from volcanic blocks in that their shape records fluidal surfaces: they may, for example, have ropy, cauliform, scoriaceous, folded, spindle, spatter, ribbon, ragged, or amoeboid shapes. Globular masses of lava may have been shot from the crater at a time when partly molten lava was exposed, and was frequently shattered by sudden outbursts of steam. These bombs were viscous at the moment of ejection and by rotation in the air acquired their shape. They are commonly 1 to 2 feet (30 to 60 cm) in diameter, but specimens as large as 12 feet (3.7 m) have been observed. There is less variety in their composition at any one volcanic centre than in the case of the lithic blocks, and their composition indicates the type of magma being erupted. Agglomerates are typically found near volcanic vents and within volcanic conduits, where they may be associated with pyroclastic or intrusive volcanic breccias. Older (pre-1970) publications, particularly in Scotland, referred to any coarse-grained volcaniclastic rock as 'agglomerate', which led to debris flow deposits, talus deposits and other types of breccia being mistaken for vents. Agglomerates are typically poorly sorted, may contain a fine ash or tuff matrix and vary from matrix to clast support. They may be monolithologic or heterolithic, and may contain some blocks of various igneous rocks. There are various differences between agglomerates and ordinary ash beds or tuffs. Agglomerates are coarser and less frequently well-bedded. Agglomerates can be non-welded or welded, such as coarse basaltic 'spatter'. They typically form proximally during Strombolian eruptions, and are common at strongly peralkaline volcanoes. Some large agglomerate deposits are deposited from pyroclastic density currents during explosive caldera-forming eruptions, such as at Santorini, Taal, and Campi Flegrei. They may be massive to crudely bedded, and can attain great thicknesses. Crystalline masses of a different kind occur in some numbers in certain agglomerates. They consist of volcanic minerals very much the same as those formed in the lava, but exhibiting certain peculiarities which indicate that they have formed slowly under pressure at considerable depths. They bear a resemblance to plutonic igneous rocks, but are more correctly to be regarded as agglomerations of crystals formed within the liquid lava as it slowly rose towards the surface, and at a subsequent period cast out by violent steam explosions. The sanidinites of the Eifel belong to this group. At Vesuvius, Ascension, St Vincent and many other volcanoes, they form a considerable part of the coarser ash-beds. Their commonest minerals are olivine, anorthite, hornblende, augite, biotite and leucite."@en . . . . "Agglomerat, kantigt s\u00F6nderspr\u00E4ngda st\u00F6rre och mindre stenar, som tillsammans med aska och splittrade sm\u00E5korn slungats ut ur en vulkan vid utbrott. Stenarna och sm\u00E5kornen har b\u00E4ddats in i askan, vilken s\u00E5 sm\u00E5ningom h\u00E5rdnat till bergart. Man skiljer mellan monomikta agglomerat med bara ett slags kantiga stenar och polymikta agglomerat med flera olika slags bergarts bitar. Agglomerat som bildats genom f\u00F6rflyttning av stenbitar fr\u00E5n vulkanutbrott med hj\u00E4lp av slamstr\u00F6mmar eller vattenfl\u00F6den kallas vulkaniska konglomerat. De k\u00E4nnetecknas av att bitarna ofta blivit rundade genom n\u00F6tning under f\u00F6rflyttningen."@sv . . . . . . . . . "Aglomerado, ou aglomerado vulc\u00E2nico, \u00E9 um tipo de rocha \u00EDgnea vulc\u00E2nica formada quase totalmente por piroclastos, dos quais mais de 75% devem ser bombas vulc\u00E2nicas, e outros fragmentos angulares ou arredondados de lava consolidada, de variadas formas e tamanhos, que se forma em associa\u00E7\u00E3o a escoadas l\u00E1vicas."@pt . "374"^^ . "3669"^^ . . "Agglomeraten (van het Latijnse 'agglomerare', betekent \"te vormen tot een bol\") zijn grove opeenhopingen van grote brokken vulkanoclastisch sediment, die voor ten minste 75% bestaan uit vulkanische bommen. De vulkanische brokken zijn gewoonlijk \u00E9\u00E9n of twee voet in diameter, maar er zijn ook exemplaren van twaalf meter waargenomen. Er is weinig variatie in hun samenstelling. Agglomeraten worden meestal gevonden in de buurt van vulkanische openingen en binnen vulkanische leidingen."@nl . . . . "El terme aglomerat pot referir-se a un dip\u00F2sit detr\u00EDtic poc o gens cimentat d'element superiors o iguals als 2 mm. Tamb\u00E9 pot referir-se a una acumulaci\u00F3 de blocs no cimentats. Tamb\u00E9 s'anomenen aix\u00F2 les roques pirocl\u00E0stiques on m\u00E9s del 75% dels fragments pirocl\u00E0stics s\u00F3n majors de 64 mm i com a m\u00EDnim el 50% d'aquests s\u00F3n arrodonits."@ca . "1021995513"^^ . "Aglomerat"@in . "Aglomerado, ou aglomerado vulc\u00E2nico, \u00E9 um tipo de rocha \u00EDgnea vulc\u00E2nica formada quase totalmente por piroclastos, dos quais mais de 75% devem ser bombas vulc\u00E2nicas, e outros fragmentos angulares ou arredondados de lava consolidada, de variadas formas e tamanhos, que se forma em associa\u00E7\u00E3o a escoadas l\u00E1vicas."@pt . . . . "Aglomerado"@es . "1"^^ . . . . . . . . "Agglomerate (from the Latin agglomerare meaning \"to form into a ball\") is a coarse accumulation of large blocks of volcanic material that contains at least 75% bombs. Volcanic bombs differ from volcanic blocks in that their shape records fluidal surfaces: they may, for example, have ropy, cauliform, scoriaceous, folded, spindle, spatter, ribbon, ragged, or amoeboid shapes. Globular masses of lava may have been shot from the crater at a time when partly molten lava was exposed, and was frequently shattered by sudden outbursts of steam. These bombs were viscous at the moment of ejection and by rotation in the air acquired their shape. They are commonly 1 to 2 feet (30 to 60 cm) in diameter, but specimens as large as 12 feet (3.7 m) have been observed. There is less variety in their compositi"@en . . . . . . . . . "\u96C6\u584A\u5CA9"@zh . . . "'Aglomerat (dari bahasa latin agglomerare' yang berarti 'membentuk menjadi bola') merupakan akumulasi kasar blok - blok besar material vulkanik yang mengandung setidaknya 75% . bom vulkanik berbeda dari blok vulkanik dalam hal perekaman permukaan fluidal: bom vulkanik dapat memiliki urat, cauliform, scoriaceous, terlipat, chilled margin dan spindle, bekas hujan rintik-rintik, pita, compang-camping, atau bentuk amuboid. Sebuah massa lava yang bulat mungkin telah terhempas dari kawah pada saat lava cair parsial tersingkap ke permukaan, dan sering hancur oleh ledakan uap yang terjadi secara tiba - tiba. Bom beruwujud kental pada saat keluar dan akibat rotasi di udara diperoleh-lah bentuk yang ada sekarang. Mereka umumnya berdiameter 30 hingga 60 cm, tetapi spesimen besar berukuran 3,7 meter j"@in . "Carraig gharbh bholc\u00E1nach is ea ceirtle\u00E1n, measc\u00E1n de bhl\u00FAir\u00ED den iliomad m\u00E9id is cruth. B\u00EDonn s\u00E9 fosaithe de ghn\u00E1th mar chuid de ch\u00F3n an bholc\u00E1in, d\u00EDorthaithe \u00F3 na carraigeacha ar thaisteal an magma tr\u00EDothu ar a bhealach tr\u00EDd an maintl\u00EDn don dromchla."@ga . "Agglomeraten (van het Latijnse 'agglomerare', betekent \"te vormen tot een bol\") zijn grove opeenhopingen van grote brokken vulkanoclastisch sediment, die voor ten minste 75% bestaan uit vulkanische bommen. De vulkanische brokken zijn gewoonlijk \u00E9\u00E9n of twee voet in diameter, maar er zijn ook exemplaren van twaalf meter waargenomen. Er is weinig variatie in hun samenstelling. Agglomeraten worden meestal gevonden in de buurt van vulkanische openingen en binnen vulkanische leidingen."@nl . . . . . . "Agglomeraat"@nl . . . . "Agglomerate"@en . "Aglomerat (roca)"@ca . . "Aglomerado (rocha)"@pt . "Agglomerat, kantigt s\u00F6nderspr\u00E4ngda st\u00F6rre och mindre stenar, som tillsammans med aska och splittrade sm\u00E5korn slungats ut ur en vulkan vid utbrott. Stenarna och sm\u00E5kornen har b\u00E4ddats in i askan, vilken s\u00E5 sm\u00E5ningom h\u00E5rdnat till bergart. Man skiljer mellan monomikta agglomerat med bara ett slags kantiga stenar och polymikta agglomerat med flera olika slags bergarts bitar. Agglomerat som bildats genom f\u00F6rflyttning av stenbitar fr\u00E5n vulkanutbrott med hj\u00E4lp av slamstr\u00F6mmar eller vattenfl\u00F6den kallas vulkaniska konglomerat. De k\u00E4nnetecknas av att bitarna ofta blivit rundade genom n\u00F6tning under f\u00F6rflyttningen. Ordet agglomerat anv\u00E4nds \u00E4ven i tillverkningsprocessen f\u00F6r l\u00F6sligt kaffe, d\u00E4r agglomerat kaffe \u00E4r d\u00E4r fina partiklar av spraytorkat kaffe bearbetas till st\u00F6rre runda partiklar med en omtorkningsprocess som ger en mer l\u00F6slig form av snabbkaffe."@sv .