@prefix rdf: . @prefix dbpedia: . @prefix opencyc: . dbpedia:Earthquake rdf:type opencyc:Mx4rvViq35wpEbGdrcN5Y29ycA . @prefix foaf: . dbpedia:Earthquake foaf:homepage . @prefix owl: . dbpedia:Earthquake owl:sameAs opencyc:Mx4rwQBYpZwpEbGdrcN5Y29ycA . @prefix ns5: . dbpedia:Earthquake owl:sameAs ns5:Mx4rwQBYpZwpEbGdrcN5Y29ycA , . @prefix ns6: . dbpedia:Earthquake foaf:page ns6:Earthquake . @prefix dbpprop: . dbpedia:Earthquake dbpprop:reference . @prefix ns8: . dbpedia:Earthquake dbpprop:reference ns8:earthquake , , , , , , , , , , , , , , , , , , . @prefix rdfs: . dbpedia:Earthquake rdfs:label "\u0417\u0435\u043C\u043B\u0435\u0442\u0440\u044F\u0441\u0435\u043D\u0438\u0435"@ru , "Trz\u0119sienie ziemi"@pl , "\u0417\u0435\u043C\u043B\u0435\u0442\u0440\u0443\u0441"@uk , "Cutremur"@ro , "Jordskjelv"@no , "Erdbeben"@de , "Terratr\u00E8mol"@ca , "Tremblement de terre"@fr , "\u5730\u9707"@zh , "Maanj\u00E4ristys"@fi , "Zem\u011Bt\u0159esen\u00ED"@cs , "Terremoto"@it , "Aardbeving"@nl , "\u5730\u9707"@ja , "F\u00F6ldreng\u00E9s"@hu , "Sismo"@pt , "Deprem"@tr , "Jordb\u00E4vning"@sv , "Earthquake"@en , "Terremoto"@es . @prefix dbpedia-owl: . dbpedia:Earthquake dbpedia-owl:thumbnail ; dbpprop:abstract "Un terremoto \u2014 tambi\u00E9n llamado se\u00EDsmo o sismo (del griego \"\u03C3\u03B5\u03B9\u03C3\u03BC\u03CC\u03C2\", temblor) o, simplemente, temblor de tierra (en algunas zonas se considera que un se\u00EDsmo o sismo o temblor es un terremoto de menor magnitud) \u2014 es una sacudida del terreno que se produce debido al choque de las placas tect\u00F3nicas y a la liberaci\u00F3n de energ\u00EDa en el curso de una reorganizaci\u00F3n brusca de materiales de la corteza terrestre al superar el estado de equilibrio mec\u00E1nico. Los m\u00E1s importantes y frecuentes se producen cuando se libera energ\u00EDa potencial el\u00E1stica acumulada en la deformaci\u00F3n gradual de las rocas contiguas al plano de una falla activa, pero tambi\u00E9n pueden ocurrir por otras causas, por ejemplo en torno a procesos volc\u00E1nicos, por hundimiento de cavidades c\u00E1rsticas o por movimientos de ladera."@es , "\u0417\u0435\u043C\u043B\u0435\u0442\u0440\u044F\u0441\u0435\u0301\u043D\u0438\u044F \u2014 \u043F\u043E\u0434\u0437\u0435\u043C\u043D\u044B\u0435 \u0442\u043E\u043B\u0447\u043A\u0438 \u0438 \u043A\u043E\u043B\u0435\u0431\u0430\u043D\u0438\u044F \u043F\u043E\u0432\u0435\u0440\u0445\u043D\u043E\u0441\u0442\u0438 \u0417\u0435\u043C\u043B\u0438, \u0432\u044B\u0437\u0432\u0430\u043D\u043D\u044B\u0435 \u0435\u0441\u0442\u0435\u0441\u0442\u0432\u0435\u043D\u043D\u044B\u043C\u0438 \u043F\u0440\u0438\u0447\u0438\u043D\u0430\u043C\u0438 (\u0433\u043B\u0430\u0432\u043D\u044B\u043C \u043E\u0431\u0440\u0430\u0437\u043E\u043C 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\u0441\u0438\u043B\u044C\u043D\u044B\u0435 \u0437\u0435\u043C\u043B\u0435\u0442\u0440\u044F\u0441\u0435\u043D\u0438\u044F, \u0441\u043F\u043E\u0441\u043E\u0431\u043D\u044B\u0435 \u0432\u044B\u0437\u0432\u0430\u0442\u044C \u043E\u0431\u0448\u0438\u0440\u043D\u044B\u0435 \u0440\u0430\u0437\u0440\u0443\u0448\u0435\u043D\u0438\u044F, \u0441\u043B\u0443\u0447\u0430\u044E\u0442\u0441\u044F \u043D\u0430 \u043F\u043B\u0430\u043D\u0435\u0442\u0435 \u043F\u0440\u0438\u043C\u0435\u0440\u043D\u043E \u0440\u0430\u0437 \u0432 \u0434\u0432\u0435 \u043D\u0435\u0434\u0435\u043B\u0438. \u041A \u0441\u0447\u0430\u0441\u0442\u044C\u044E, \u0431\u043E\u043B\u044C\u0448\u0430\u044F \u0438\u0445 \u0447\u0430\u0441\u0442\u044C \u043F\u0440\u0438\u0445\u043E\u0434\u0438\u0442\u0441\u044F \u043D\u0430 \u0434\u043D\u043E \u043E\u043A\u0435\u0430\u043D\u043E\u0432, \u0438 \u043F\u043E\u044D\u0442\u043E\u043C\u0443 \u043D\u0435 \u0441\u043E\u043F\u0440\u043E\u0432\u043E\u0436\u0434\u0430\u0435\u0442\u0441\u044F \u043A\u0430\u0442\u0430\u0441\u0442\u0440\u043E\u0444\u0438\u0447\u0435\u0441\u043A\u0438\u043C\u0438 \u043F\u043E\u0441\u043B\u0435\u0434\u0441\u0442\u0432\u0438\u044F\u043C\u0438 (\u0435\u0441\u043B\u0438 \u0437\u0435\u043C\u043B\u0435\u0442\u0440\u044F\u0441\u0435\u043D\u0438\u0435 \u043F\u043E\u0434 \u043E\u043A\u0435\u0430\u043D\u043E\u043C \u043E\u0431\u0445\u043E\u0434\u0438\u0442\u0441\u044F \u0431\u0435\u0437 \u0446\u0443\u043D\u0430\u043C\u0438). \u0417\u0435\u043C\u043B\u0435\u0442\u0440\u044F\u0441\u0435\u043D\u0438\u044F \u043D\u0430\u0438\u0431\u043E\u043B\u0435\u0435 \u0438\u0437\u0432\u0435\u0441\u0442\u043D\u044B \u043F\u043E \u0442\u0435\u043C \u043E\u043F\u0443\u0441\u0442\u043E\u0448\u0435\u043D\u0438\u044F\u043C, \u043A\u043E\u0442\u043E\u0440\u044B\u0435 \u043E\u043D\u0438 \u0441\u043F\u043E\u0441\u043E\u0431\u043D\u044B \u043F\u0440\u043E\u0438\u0437\u0432\u0435\u0441\u0442\u0438. \u0420\u0430\u0437\u0440\u0443\u0448\u0435\u043D\u0438\u044F \u0437\u0434\u0430\u043D\u0438\u0439 \u0438 \u0441\u043E\u043E\u0440\u0443\u0436\u0435\u043D\u0438\u0439 \u0432\u044B\u0437\u044B\u0432\u0430\u044E\u0442\u0441\u044F \u043A\u043E\u043B\u0435\u0431\u0430\u043D\u0438\u044F\u043C\u0438 \u043F\u043E\u0447\u0432\u044B \u0438\u043B\u0438 \u0433\u0438\u0433\u0430\u043D\u0442\u0441\u043A\u0438\u043C\u0438 \u043F\u0440\u0438\u043B\u0438\u0432\u043D\u044B\u043C\u0438 \u0432\u043E\u043B\u043D\u0430\u043C\u0438, \u0432\u043E\u0437\u043D\u0438\u043A\u0430\u044E\u0449\u0438\u043C\u0438 \u043F\u0440\u0438 \u0441\u0435\u0439\u0441\u043C\u0438\u0447\u0435\u0441\u043A\u0438\u0445 \u0441\u043C\u0435\u0449\u0435\u043D\u0438\u044F\u0445 \u043D\u0430 \u043C\u043E\u0440\u0441\u043A\u043E\u043C \u0434\u043D\u0435."@ru , "En jordb\u00E4vning, \u00E4ven kallat jordskalv, inneb\u00E4r att marken skakar och r\u00F6r sig p\u00E5 grund av pl\u00F6tsligt utl\u00F6sta r\u00F6relser i jordskorpan eller \u00F6vre delen av manteln, den s\u00E5 kallade litosf\u00E4ren. Skakningarna kan orsaka sv\u00E5ra skador p\u00E5 byggnader, och om jordb\u00E4vningen intr\u00E4ffar under havet kan en flodv\u00E5g, tsunami, utl\u00F6sas och f\u00E4rdas l\u00E5nga str\u00E4ckor och orsaka stor f\u00F6r\u00F6delse n\u00E4r den n\u00E5r land. Jordb\u00E4vningar uppkommer n\u00E4r de sp\u00E4nningar utl\u00F6ses som byggts upp p\u00E5 grund av r\u00F6relser i jordskorpan eller \u00F6vre manteln. Stora m\u00E4ngder energi frig\u00F6rs och sprids i form av seismiska v\u00E5gor genom jorden. Det \u00E4r dessa v\u00E5gor som orsakar den skakning som k\u00E4nns vid en jordb\u00E4vning. Jordb\u00E4vningar kan uppst\u00E5 under flera olika f\u00F6ruts\u00E4ttningar. De omr\u00E5den i v\u00E4rlden som \u00E4r mest jordb\u00E4vningsdrabbade ligger vid eller n\u00E4ra gr\u00E4nserna mellan de olika Plattektoniktektoniska plattorna som bygger upp jordskorpan. Jordb\u00E4vningar f\u00F6rekommer ocks\u00E5 i samband med vulkanutbrott och landh\u00F6jning. \u00C4ven k\u00E4rnvapenprov under jord utl\u00F6ser mindre jordb\u00E4vningar. Orsaken till att de flesta och kraftigaste jordb\u00E4vningarna registreras n\u00E4ra gr\u00E4nsen mellan de tektoniska plattorna \u00E4r att de st\u00F6rsta sp\u00E4nningarna byggs upp i dessa zoner. Vid plattgr\u00E4nserna \u00E5terfinns ocks\u00E5 de allra flesta vulkaner. Stora jordb\u00E4vningar f\u00F6ljs alltid av en l\u00E5ng rad efterskalv som kan h\u00E5lla p\u00E5 i m\u00E5nader och uppg\u00E5 till \u00E5tskilliga tusental. I samband med de allra kraftigaste jordb\u00E4vningarna kan det i s\u00E4llsynta fall f\u00F6rekomma enorma efterskalv som \u00E4r n\u00E4stan lika kraftiga som huvudskalvet. Ibland f\u00F6reg\u00E5s det stora skalvet av m\u00E5nga f\u00F6rskalv."@sv , "Cutremur sau seism sunt termenii folosi\u0163i pentru mi\u015Fc\u0103rile p\u0103m\u00E2ntului, ce constau \u00EEn vibra\u0163ii originate \u00EEn zonele interne ale Terrei, propagate \u00EEn form\u0103 de unde prin roci. Aceste vibra\u0163ii rezult\u0103 din mi\u015Fc\u0103rile pl\u0103cilor tectonice, fiind des cauzate de o activitate vulcanic\u0103. \u00CEn unele \u0163\u0103ri, cuv\u00E2ntul cutremur este folosit doar pentru acele mi\u015Fc\u0103ri ale pl\u0103cilor tectonice care provoac\u0103 daune majore \u015Fi seism sau mi\u015Fc\u0103ri seismice pentru cele care trec neobservate. Scara seismologic\u0103 a lui Richter este o scal\u0103 logaritmic\u0103, care este folosit\u0103 pentru a evalua intensitatea cutremurelor. Cutremure puternice ce devin catastrofe naturale, pot distruge construc\u0163ii, cl\u0103diri, chiar localit\u0103\u0163i \u00EEntregi, provoac\u0103 alunec\u0103ri de teren, chiar catastrofe naturale. Cutremurele submarine pot declan\u015Fa formarea de valuri uria\u015Fe p\u00E2n\u0103 la 30 de m \u00EEn\u0103\u0163ime ating\u00E2nd viteze nea\u015Fteptate (800 km/h), astfel \u00EEn Oceanul Pacific (Tsunami) a produs pagube foarte mari materiale, cu pierderi de vie\u0163i omene\u015Fti. \u015Etiin\u0163a care se ocup\u0103 cu studiul cutremurului (mi\u015Fc\u0103rilor seismice) se nume\u015Fte seismologie."@ro , "Als Erdbeben werden messbare Ersch\u00FCtterungen des Erdk\u00F6rpers bezeichnet. Der deutlich gr\u00F6\u00DFte Anteil aufgezeichneter Erdbeben ist zu schwach, um von Menschen wahrgenommen zu werden. Auch andere Bewegungen der Erdoberfl\u00E4che, wie etwa durch Tidenhub oder durch Eigenschwingungen der Erde sind nicht f\u00FChlbar, da sie zu langsam erfolgen oder zu schwach sind. Erdbeben bestehen in der Regel nicht aus einzelnen Ersch\u00FCtterungen, sondern ziehen meist weitere nach sich. Man spricht in diesem Zusammenhang vonNachbeben. Starke Erdbeben k\u00F6nnen H\u00E4user und Bauten zerst\u00F6ren, Tsunamis und Erdrutsche ausl\u00F6sen und dabei Menschen t\u00F6ten. Sie k\u00F6nnen die Gestalt der Erdoberfl\u00E4che ver\u00E4ndern und z\u00E4hlen zu den Naturkatastrophen. Unterseeische Erdbeben werden im Volksmund auch alsSeebeben bezeichnet. Die Wissenschaft, die sich mit Erdbeben befasst, hei\u00DFt Seismologie."@de , "\u5730\u9707\uFF08\u53C8\u79F0\u5730\u52A8\u3001\u5730\u632F\u52A8\uFF09\u662F\u5730\u6BBC\u5FEB\u901F\u91CB\u653E\u80FD\u91CF\u904E\u7A0B\u4E2D\u9020\u6210\u7684\u632F\u52D5\uFF0C\u671F\u9593\u6703\u7522\u751F\u5730\u9707\u6CE2\u3002 \u5730\u9707\u53EF\u7531\u5730\u9707\u5100\u6240\u6E2C\u91CF\uFF0C\u5730\u9707\u7684\u9707\u7D1A\u662F\u7528\u4F5C\u8868\u793A\u7531\u9707\u6E90\u91CB\u653E\u51FA\u4F86\u7684\u80FD\u91CF\uFF0C\u901A\u5E38\u4EE5\u300C\u9ECE\u514B\u7279\u5236\u5730\u9707\u9707\u7D1A\u300D\u4F86\u8868\u793A\uFF1B\u70C8\u5EA6\u5247\u900F\u904E\u300C\u4FEE\u8A02\u9EA5\u52A0\u5229\u5730\u9707\u70C8\u5EA6\u8868\u300D\u4F86\u8868\u793A\uFF0C\u67D0\u5730\u9EDE\u7684\u5730\u9707\u70C8\u5EA6\u662F\u6307\u5730\u9707\u5F15\u81F4\u8A72\u5730\u9EDE\u5730\u6BBC\u904B\u52D5\u7684\u731B\u70C8\u7A0B\u5EA6\uFF0C\u662F\u7531\u9707\u52D5\u5C0D\u500B\u4EBA\u3001\u50A2\u5177\u3001\u623F\u5C4B\u3001\u5730\u8CEA\u7D50\u69CB\u7B49\u6240\u7522\u751F\u7684\u5F71\u97FF\u4F86\u65B7\u5B9A\u3002 \u5728\u5730\u7403\u7684\u8868\u9762\uFF0C\u5730\u9707\u6703\u4F7F\u5730\u9762\u767C\u751F\u9707\u52D5\uFF0C\u6709\u6642\u5247\u6703\u767C\u751F\u5730\u9762\u79FB\u52D5\u3002\u9707\u52D5\u53EF\u80FD\u5F15\u767C\u5C71\u6CE5\u50BE\u7009\u751A\u6216\u706B\u5C71\u6D3B\u52D5\u3002\u5982\u5730\u9707\u5728\u6D77\u5E95\u767C\u751F\uFF0C\u6D77\u5E8A\u7684\u79FB\u52D5\u751A\u81F3\u6703\u5F15\u767C\u6D77\u562F\u3002 \u4E00\u822C\u800C\u8A00\uFF0C\u5730\u9707\u4E00\u8A5E\u53EF\u6307\u81EA\u7136\u73FE\u8C61\u6216\u4EBA\u70BA\u7834\u58DE\u6240\u9020\u6210\u7684\u5730\u9707\u6CE2\u3002\u4EBA\u70BA\u81EA\u7136\u5730\u5F62\u7684\u7834\u58DE\u3001\u5927\u91CF\u6C23\u9AD4\uFF08\u5C24\u5176\u662F\u6CBC\u6C23\uFF09\u9077\u79FB\u6216\u63D0\u53D6\u3001\u6C34\u5EAB\u84C4\u6C34\u3001\u63A1\u7926\u3001\u6CB9\u4E95\u6CE8\u6C34\u3001\u5730\u4E0B\u6838\u8A66\u7B49\uFF1B\u81EA\u7136\u7684\u706B\u5C71\u6D3B\u52D5\u3001\u5927\u578B\u5C71\u5D29\u3001\u5730\u4E0B\u7A7A\u6D1E\u584C\u9677\u3001\u5927\u584A\u9695\u77F3\u589C\u843D\u7B49\u5747\u53EF\u5F15\u767C\u5730\u9707\u3002 \u9707\u52D5\u7684\u767C\u6E90\u8655\u7A31\u70BA\u9707\u6E90\u3002\u5927\u591A\u6578\u9707\u6E90\u90FD\u5728\u5730\u6BBC\u548C\u4E0A\u5730\u5E54\u9802\u90E8\uFF0C\u5373\u5CA9\u77F3\u5708\u5167\u3002\u6839\u64DA\u9707\u6E90\u7684\u6DF1\u5EA6\uFF0C\u5730\u9707\u53EF\u5206\u70BA\u4E09\u985E\uFF1A\u6DFA\u6E90\u5730\u9707\uFF08\u6DF1\u5EA6\u57280-70\u516C\u91CC\uFF09\u3001\u4E2D\u6E90\u5730\u9707\uFF08\u6DF1\u5EA6\u572870-300\u516C\u91CC\uFF09\u548C\u6DF1\u6E90\u5730\u9707\uFF08\u6DF1\u5EA6\u5728300\u516C\u91CC\u4EE5\u4E0A\uFF09\u3002\u7531\u9707\u6E90\u8C4E\u4E00\u5782\u76F4\u7DDA\u81F3\u5730\u9762\u4E0A\u7684\u4F4D\u7F6E\u7A31\u70BA\u9707\u4E2D\u3002\u9707\u4E2D\u662F\u5730\u8868\u8DDD\u96E2\u9707\u6E90\u6700\u8FD1\u7684\u5730\u65B9\uFF0C\u56E0\u6B64\u5730\u9707\u6CE2\u6700\u65E9\u5230\u9054\u9019\u8655\uFF0C\u9707\u52D5\u4E5F\u6700\u70BA\u5F37\u70C8\uFF0C\u7834\u58DE\u7A0B\u5EA6\u4E5F\u6700\u5927\u3002"@zh , "Um sismo, tamb\u00E9m chamado de terremoto ou terramoto, \u00E9 um fen\u00F4meno de vibra\u00E7\u00E3o brusca e passageira da superf\u00EDcie da Terra, resultante de movimentos subterr\u00E2neos de placas rochosas, de atividade vulc\u00E2nica, ou por deslocamentos (migra\u00E7\u00E3o) de gases no interior da Terra, principalmente metano. O movimento \u00E9 causado pela libera\u00E7\u00E3o r\u00E1pida de grandes quantidades de energia sob a forma de ondas s\u00EDsmicas. A maior parte dos terremotos ocorrem nas fronteiras entre placas tect\u00F4nicas, ou em falhas entre dois blocos rochosos. O comprimento de uma falha pode variar de alguns cent\u00EDmetros at\u00E9 milhares de quil\u00F4metros, como \u00E9 o caso da falha de San Andreas na Calif\u00F3rnia, Estados Unidos. S\u00F3 nos Estados Unidos ocorrem de 12 mil a 14 mil terremotos anualmente (ou seja, aproximadamente 35 por dia). Baseado em registros hist\u00F3ricos de longo prazo, aproximadamente 18 grandes terremotos (de 7,0 a 7,9 na Escala de Richter) e um terremoto gigante (8 ou acima) podem ser esperados num ano. Entre os efeitos dos terremotos est\u00E3o a vibra\u00E7\u00E3o do solo, abertura de falhas, deslizamentos de terra, tsunamis, mudan\u00E7as na rota\u00E7\u00E3o da Terra, al\u00E9m de efeitos delet\u00E9rios em constru\u00E7\u00F5es feitas pelo homem, resultando em perda de vidas, ferimentos e altos preju\u00EDzos financeiros e sociais (como o desabrigo de popula\u00E7\u00F5es inteiras, facilitando a prolifera\u00E7\u00E3o de doen\u00E7as, fome, etc). O maior terremoto j\u00E1 registado foi o Grande Terremoto do Chile em 1960 que atingiu 9.5 na escala de Richter seguido pelo da Indon\u00E9sia em 2004 que atingiu 9.3 na mesma escala."@pt , "A f\u00F6ldreng\u00E9s a f\u00F6ldfelsz\u00EDn egy darabj\u00E1nak hirtelen bek\u00F6vetkez\u0151 \u00E9s n\u00E9ha katasztrof\u00E1lis k\u00F6vetkezm\u00E9nyekkel j\u00E1r\u00F3 mozg\u00E1sa. A f\u00F6ldreng\u00E9sek \u00E1ltal\u00E1ban a f\u00F6ldk\u00E9regben felgy\u00FClemlett energia felszabadul\u00E1sakor keletkez\u0151 l\u00F6k\u00E9shull\u00E1mok, melyek a keletkez\u00E9si pontb\u00F3l, amit a f\u00F6ldreng\u00E9s hipocentrum\u00E1nak nevez\u00FCnk, g\u00F6mbh\u00E9jszer\u0171en terjednek minden ir\u00E1nyba. A fesz\u00FClts\u00E9g t\u00F6bb okb\u00F3l halmoz\u00F3dhat fel. Ebb\u0151l k\u00F6vetkezik, hogy a f\u00F6ldreng\u00E9sek a F\u00F6ld k\u00FCl\u00F6nb\u00F6z\u0151 r\u00E9szein keletkeznek. A legnagyobb fesz\u00FClts\u00E9gek a k\u0151zetlemezek tal\u00E1lkoz\u00E1s\u00E1n\u00E1l keletkeznek, \u00E9s a f\u00F6ldreng\u00E9sek jelent\u0151s r\u00E9sze ezen a ter\u00FCleten alakul ki. (Ha megn\u00E9zz\u00FCk a k\u00E9pet nagyon j\u00F3l kirajzol\u00F3dnak rajta a lemezhat\u00E1rok. ) Ezeket a f\u00F6ldreng\u00E9seket nevezz\u00FCk interplate (lemezek k\u00F6zti) f\u00F6ldreng\u00E9seknek. Megfigyeltek f\u00F6ldreng\u00E9seket a lemezszeg\u00E9lyekt\u0151l t\u00E1vol a k\u0151zetlemezek belsej\u00E9ben is, ezeket intraplate (lemezen bel\u00FCli) f\u00F6ldreng\u00E9seknek nevezz\u00FCk, ennek kialakul\u00E1si okai m\u00E9g nem teljesen tiszt\u00E1zottak. Ezeket a f\u00F6ldreng\u00E9seket, amiket a lemezek mozg\u00E1sa okoz, tektonikus reng\u00E9seknek nevezz\u00FCk (p\u00E9ld\u00E1ul vulk\u00E1nkit\u00F6r\u00E9s hat\u00E1s\u00E1ra, amikor a f\u00F6ldreng\u00E9st a felfel\u00E9 t\u00F6rekv\u0151 magma okozza). Az ember is okozhat f\u00F6ldreng\u00E9seket a f\u00F6ld alatti k\u00EDs\u00E9rleti atomrobbant\u00E1sokkal. Ezt a hat\u00E1st haszn\u00E1lt\u00E1k fel arra, hogy az atomrobbant\u00E1sokat figyelemmel tudj\u00E1k k\u00EDs\u00E9rni, de mivel ezek mesters\u00E9gesen keltett f\u00F6ldreng\u00E9sek, nem szokt\u00E1k a f\u00F6ldreng\u00E9sek k\u00F6z\u00E9 sorolni \u0151ket. F\u00E1jl:Quake epicenters 1963-98. png A f\u00F6ldreng\u00E9sek eloszl\u00E1sa"@hu , "Maanj\u00E4ristys on Maan peruskallion t\u00E4r\u00E4htely\u00E4, joka on voimakkaana hyvin tuhoisaa rakennuksille ja ihmisille. Heikko j\u00E4ristys heiluttaa lamppuja, voimakas j\u00E4ristys romahduttaa talot, hyvin voimakas myll\u00E4\u00E4 maaper\u00E4\u00E4kin. Meren pohjassa tapahtunut maanj\u00E4ristys voi aiheuttaa voimakkaan hy\u00F6kyaallon, tsunamin. Maanj\u00E4ristyksen voimaa mitataan yleens\u00E4 Richterin asteikolla ja tuhoisuutta Mercallin asteikolla. Yli seitsem\u00E4n Richterin j\u00E4ristykset ovat hyvin tuhoisia. Maaj\u00E4ristyksi\u00E4 syntyy muun muassa mannerlaattojen liikkuessa toistensa suhteen, tulivuorenpurkauksen, asteroidit\u00F6rm\u00E4yksen, maanvy\u00F6ryn tai ydinr\u00E4j\u00E4hdyksen takia. Maanj\u00E4ristyksi\u00E4 esiintyy eniten mannerlaattojen rajoilla alueilla, joissa on runsasta tulivuoritoimintaakin. Maanj\u00E4ristyksen maanalainen tapahtumapaikka on hyposentri, ja maanpintakeskus episentri. Hyposentri voi olla satojen metrien - satojen kilometrien syvyydess\u00E4. Maanj\u00E4ristyksi\u00E4 pystyt\u00E4\u00E4n toteamaan kaukaakin seismometriksi kutsutulla laitteella. Maanj\u00E4ristysaallot jateaan pitkitt\u00E4isiin ja poikittaisiin. J\u00E4ristysaaltojen heijastumisia tutkimalla voidaan selvitt\u00E4\u00E4 jossain m\u00E4\u00E4rin peruskallion ja koko Maan rakennetta. Suomi on geologisesti katsoen hyvin rauhallista aluetta, t\u00E4\u00E4ll\u00E4 ei yleens\u00E4 esiinny maanj\u00E4ristyksi\u00E4, mutta teoriassa suurenkaan j\u00E4ristyksen mahdollisuutta eiv\u00E4t geologit pysty pois sulkemaan."@fi , "Zem\u011Bt\u0159esen\u00ED je n\u00E1hl\u00FD pohyb zemsk\u00E9 k\u016Fry, vyvolan\u00FD uvoln\u011Bn\u00EDm nap\u011Bt\u00ED \u2013 nap\u0159. z neust\u00E1l\u00FDch pohyb\u016F zemsk\u00FDch desek \u2013 pod\u00E9l zlom\u016F. V\u011Bt\u0161\u00ED zem\u011Bt\u0159esen\u00ED se proto obvykle vyskytuj\u00ED v t\u011Bch oblastech sv\u011Bta, kter\u00FDmi v\u00FDznamn\u00E9 zlomy proch\u00E1zej\u00ED Studiu zem\u011Bt\u0159esen\u00ED se v\u011Bnuje geofyzika konkr\u00E9tn\u011B jej\u00ED sou\u010D\u00E1st seismologie. M\u00EDsto vzniku zem\u011Bt\u0159esen\u00ED se naz\u00FDv\u00E1 ohnisko neboli hypocentrum, jeho kolm\u00FD pr\u016Fm\u011Bt na zemsk\u00E9m povrchu se naz\u00FDv\u00E1 epicentrum. K vyj\u00E1d\u0159en\u00ED s\u00EDly ot\u0159es\u016F se pou\u017E\u00EDvaj\u00ED dv\u011B rozd\u00EDln\u00E9 veli\u010Diny, magnitudo a makroseismick\u00E1 intenzita. Magnitudo se ur\u010Duje z maxim\u00E1ln\u00ED v\u00FDchylky seismometru, zat\u00EDmco makroseismick\u00E1 intenzita se ur\u010Duje ze statistick\u00E9ho vyhodnocen\u00ED \u00FA\u010Dink\u016F zem\u011Bt\u0159esen\u00ED na osoby, budovy a krajinu. Ka\u017Ed\u00E9 zem\u011Bt\u0159esen\u00ED je charakterizov\u00E1no jednou hodnotou magnituda, ale v\u00EDce hodnotami makroseismick\u00E9 intenzity v z\u00E1vislosti na poloze v\u016F\u010Di hypocentru. Nap\u0159\u00EDklad zem\u011Bt\u0159esen\u00ED v rakousk\u00E9m Ebreichsdorfu 11. \u010Dervence 2000 m\u011Blo magnitudo 4,8 a makroseismickou intenzitu v epicentru VI stup\u0148\u016F EMS-98, v Brn\u011B bylo poc\u00EDt\u011Bno jako IV. stupe\u0148 EMS-98. Slab\u00E1 zem\u011Bt\u0159esen\u00ED, kter\u00E1 \u010Dlov\u011Bk bu\u010F v\u016Fbec nepoc\u00EDt\u00ED, nebo kter\u00E1 se projev\u00ED na nestabiln\u00EDch p\u0159edm\u011Btech v dom\u00E1cnosti (skleni\u010Dky na polic\u00EDch, lustr, hodiny na stole), jsou velmi \u010Dast\u00E1 i v seismicky klidn\u011Bj\u0161\u00EDch oblastech \u2013 nap\u0159. seismick\u00E9 roje v z\u00E1padn\u00EDch \u010Cech\u00E1ch mohou v\u00E9st a\u017E k lehk\u00E9mu poprask\u00E1n\u00ED zd\u00ED, na Ostravsku doch\u00E1z\u00ED \u010Dasto k slab\u00FDm ot\u0159es\u016Fm v souvislosti s d\u016Fln\u00ED \u010Dinnost\u00ED. Siln\u011Bj\u0161\u00ED zem\u011Bt\u0159esen\u00ED jsou pak v\u00E1z\u00E1na v\u011Bt\u0161inou na aktivn\u00ED tektonick\u00E9 oblasti a jejich v\u00FDskyt je m\u00E9n\u011B \u010Dast\u00FD, av\u0161ak celosv\u011Btov\u011B nejde o v\u00FDjime\u010Dn\u00FD \u00FAkaz. Jednou za n\u011Bkolik let v\u0161ak dojde k siln\u00E9mu zem\u011Bt\u0159esen\u00ED v nejchud\u0161\u00EDch st\u00E1tech sv\u011Bta, kter\u00E9 m\u016F\u017Ee p\u0159ipravit o \u017Eivot stovky \u010Di tis\u00EDce lid\u00ED a zp\u016Fsob\u00ED mnohamiliardov\u00E9 \u0161kody na majetku. Podmo\u0159sk\u00E1 zem\u011Bt\u0159esen\u00ED pak mohou vyvolat tak\u00E9 velmi ni\u010Div\u00E9 vlny tsunami."@cs , "Een aardbeving is een trilling of schokkende beweging van de aardkorst. Aardbevingen vinden plaats als er in de aardkorst plotseling veel energie vrijkomt. De energie plant zich dan in een golfbeweging vanuit het centrum naar de omgeving voort. Het denkbeeldige punt waar de beving ontstaat, het zwaartepunt van de energiedichtheid, heet het hypocentrum. Het punt aan het aardoppervlak daar loodrecht boven wordt het epicentrum genoemd. Een lijn van gelijke bevingintensiteit rond een epicentrum heet een isoseist. Seismologie is de wetenschap van aardbevingen. Tijdens een aardbeving treden Tribo-elektrisch effecten op in de vorm van lichtflitsen. De meeste aardbevingen komen voor in de aardkorst tot op een diepte van ongeveer 30 kilometer. Er komen echter ook bevingen voor op dieptes tot ongeveer 700 kilometer. De meeste aardbevingen komen voor rondom de Grote Oceaan, in het Middellandse Zeegebied, in de Himalaya en Indonesi\u00EB. Ook midden in oceanen komen bevingen voor. Aardbevingen die ontstaan onder de zeespiegel worden, minder correct, ook wel zeebevingen genoemd; een vloedgolf of tsunami kan dan het gevolg zijn. Zware aardbevingen en / of tsunami's veroorzaken vaak veel slachtoffers en grote schade."@nl , "Un terratr\u00E8mol, - tamb\u00E9 anomenat sisme (del grec \"\u03C3\u03B5\u03B9\u03C3\u03BC\u03CC\u03C2\", tremolor) o, simplement, tremolor de terra (en algunes zones es considera que un sisme \u00E9s un terratr\u00E8mol de menor magnitud) - resulta de l'alliberament brusc d'energia acumulada pels despla\u00E7aments i les friccions de les diferents plaques de l'escor\u00E7a terrestre (fen\u00F2mens reagrupats sota el nom de plaques tect\u00F2niques). La majoria dels terratr\u00E8mols s\u00F3n localitzats sobre falles. M\u00E9s rars s\u00F3n els sismes deguts a l'activitat volc\u00E0nia o d'origen artificial (explosions per exemple). Es produeixen nombrosos sismes tots els dies, per\u00F2 la majoria no s\u00F3n sentits pels humans. Aproximadament cent mil sismes s\u00F3n gravats anualment sobre el planeta. Els m\u00E9s poderosos d'ells compten entre les cat\u00E0strofes naturals m\u00E9s destructores. La ci\u00E8ncia que estudia aquests fen\u00F2mens \u00E9s la sismologia i l'instrument d'estudi principal el sism\u00F2graf."@ca , "Trz\u0119sienie ziemi - gwa\u0142towne roz\u0142adowanie napr\u0119\u017Ce\u0144 powsta\u0142ych w skorupie ziemskiej w czasie ruch\u00F3w fragment\u00F3w litosfery. Z miejsca uwolnienia tych napr\u0119\u017Ce\u0144 (hipocentrum – ogniska trz\u0119sienia ziemi) rozchodz\u0105 si\u0119 fale sejsmiczne. Punkt na powierzchni Ziemi po\u0142o\u017Cony nad ogniskiem to miejsce, gdzie fale docieraj\u0105 najwcze\u015Bniej i gdzie straty s\u0105 najwi\u0119ksze. Si\u0142a wstrz\u0105s\u00F3w maleje w miar\u0119 oddalania si\u0119 od epicentrum. Badaniem trz\u0119sie\u0144 ziemi zajmuje si\u0119 sejsmologia."@pl , "\u0417\u0435\u043C\u043B\u0435\u0442\u0440\u0443\u0301\u0441 (\u0430\u043D\u0433\u043B. earthquake, earth shock, \u043D\u0456\u043C. Erdbeben n, unterirdische St\u00F6\u00DF m) \u2014 \u043A\u043E\u0440\u043E\u0442\u043A\u043E\u0442\u0440\u0438\u0432\u0430\u043B\u0456, \u0440\u0430\u043F\u0442\u043E\u0432\u0456 \u0441\u0442\u0440\u0443\u0441\u0438 \u0437\u0435\u043C\u043D\u043E\u0457 \u043A\u043E\u0440\u0438, \u0432\u0438\u043A\u043B\u0438\u043A\u0430\u043D\u0456 \u043F\u0435\u0440\u0435\u043C\u0456\u043D\u043D\u0438\u043C \u043F\u0435\u0440\u0435\u043C\u0456\u0449\u0435\u043D\u043D\u044F\u043C \u043C\u0430\u0441 \u0433\u0456\u0440\u0441\u044C\u043A\u0438\u0445 \u043F\u043E\u0440\u0456\u0434 \u0443 \u043D\u0430\u0434\u0440\u0430\u0445 \u0417\u0435\u043C\u043B\u0456, \u0447\u043E\u043C\u0443 \u0441\u043F\u0440\u0438\u044F\u0454 \u043F\u043E\u0440\u0443\u0448\u0435\u043D\u043D\u044F \u0440\u043E\u0437\u0442\u044F\u0436\u043D\u043E\u0441\u0442\u0456 \u043E\u0441\u0435\u0440\u0435\u0434\u043A\u0430 \u0433\u0456\u0440\u0441\u044C\u043A\u0438\u0445 \u043F\u043E\u0440\u0456\u0434 \u0456 \u0432\u0438\u043D\u0438\u043A\u043D\u0435\u043D\u043D\u044F \u0441\u0435\u0439\u0441\u043C\u0456\u0447\u043D\u0438\u0445 \u0445\u0432\u0438\u043B\u044C; \u043F\u0456\u0434 \u0447\u0430\u0441 \u0441\u0438\u043B\u044C\u043D\u0438\u0445 \u0437\u0435\u043C\u043B\u0435\u0442\u0440\u0443\u0441\u0456\u0432, \u043D\u0430 \u043F\u043E\u0432\u0435\u0440\u0445\u043D\u0456 \u0417\u0435\u043C\u043B\u0456 \u0447\u0430\u0441\u0442\u043E \u0432\u0438\u043D\u0438\u043A\u0430\u044E\u0442\u044C \u0449\u0456\u043B\u0438\u043D\u0438, \u0441\u043A\u0438\u0434\u0438, \u0437\u0441\u0443\u0432\u0438, \u0446\u0443\u043D\u0430\u043C\u0456; \u0447\u0430\u0441\u043E\u043C \u0437\u0435\u043C\u043B\u0435\u0442\u0440\u0443\u0441\u0438 \u0441\u043F\u0440\u0438\u0447\u0438\u043D\u044E\u044E\u0442\u044C \u0432\u0435\u043B\u0438\u043A\u0456 \u0440\u0443\u0439\u043D\u0443\u0432\u0430\u043D\u043D\u044F. \u041D\u0430\u0441\u043B\u0456\u0434\u043A\u0438 \u0437\u0435\u043C\u043B\u0435\u0442\u0440\u0443\u0441\u0443. JPG \u0421\u0435\u0440\u0435\u0434 \u0443\u0441\u0456\u0445 \u0441\u0442\u0438\u0445\u0456\u0439\u043D\u0438\u0445 \u043B\u0438\u0445, \u0437\u0430 \u0434\u0430\u043D\u0438\u043C\u0438 \u042E\u041D\u0415\u0421\u041A\u041E, \u0437\u0435\u043C\u043B\u0435\u0442\u0440\u0443\u0441\u0438 \u0437\u0430\u0439\u043C\u0430\u044E\u0442\u044C \u043F\u0435\u0440\u0448\u0435 \u043C\u0456\u0441\u0446\u0435 \u0432 \u0441\u0432\u0456\u0442\u0456 \u0437\u0430 \u0437\u0430\u043F\u043E\u0434\u0456\u044F\u043D\u043E\u044E \u0435\u043A\u043E\u043D\u043E\u043C\u0456\u0447\u043D\u043E\u044E \u0448\u043A\u043E\u0434\u043E\u044E \u0456 \u043A\u0456\u043B\u044C\u043A\u0456\u0441\u0442\u044E \u0437\u0430\u0433\u0438\u0431\u043B\u0438\u0445."@uk , "Deprem, yerkabu\u011Fu i\u00E7indeki k\u0131r\u0131lmalar nedeniyle ani olarak ortaya \u00E7\u0131kan titre\u015Fimlerin dalgalar halinde yay\u0131larak ge\u00E7tikleri ortamlar\u0131 ve yery\u00FCzeyini sarsma olay\u0131d\u0131r. Magma \u00FCzerinde y\u00FCzen levhalar konveksiyonel ak\u0131m sayesinde s\u00FCrekli hareket halindedir. K\u0131talar\u0131n hareketi ile plato s\u0131n\u0131rlar\u0131nda kaynama ve ayr\u0131lmadaki s\u00FCrt\u00FCnmeden olu\u015Fan kinetik enerjinin aniden b\u00FCy\u00FCk bir g\u00FC\u00E7le bo\u015Falabilir. Yer katmanlar\u0131nda olu\u015Fan \u015Fok dalgalar\u0131n\u0131n sebep oldu\u011Fu do\u011Fa olay\u0131na deprem denir. Depremin nas\u0131l olu\u015Ftu\u011Funu, deprem dalgalar\u0131n\u0131n yeryuvar\u0131 i\u00E7inde ne \u015Fekilde yay\u0131ld\u0131klar\u0131n\u0131, \u00F6l\u00E7\u00FC aletleri ve y\u00F6ntemlerini, kay\u0131tlar\u0131n de\u011Ferlendirilmesini ve deprem ile ilgili di\u011Fer konular\u0131 inceleyen bilim dal\u0131na \"Sismoloji\" denir. Sismik \u015Fok dalgalar\u0131, yer kabu\u011Funda dikey veya yatay olarak hareket edebilirler. Deprem b\u00F6lgesinin jeolojik yap\u0131s\u0131 sonucu killi veya kumlu arazilerde yer alt\u0131 su kaynaklar\u0131 aniden yery\u00FCz\u00FCne \u00E7\u0131kabilir. Arazide seviye kayb\u0131 veya tersi olu\u015Fabilir. Deprem, insan\u0131n hareketsiz kabul etti\u011Fi ve g\u00FCvenle aya\u011F\u0131n\u0131 bast\u0131\u011F\u0131 topra\u011F\u0131n da oynad\u0131\u011F\u0131 ve \u00FCzerinde bulunan t\u00FCm yap\u0131lar\u0131n da hasar g\u00F6r\u00FCp, can kayb\u0131na u\u011Frayacak \u015Fekilde y\u0131k\u0131labileceklerini g\u00F6steren bir do\u011Fa olay\u0131d\u0131r. \u0130stanbul Kandilli Rasathanesi T\u00FCrkiye depremlerini ara\u015Ft\u0131rma ve bilgi merkezidir."@tr , "Un tremblement de terre, ou s\u00E9isme, r\u00E9sulte de la lib\u00E9ration brusque d'\u00E9nergie accumul\u00E9e par les d\u00E9placements et les frictions des diff\u00E9rentes plaques de la cro\u00FBte terrestre (ph\u00E9nom\u00E8nes regroup\u00E9s sous le nom de tectonique des plaques). La plupart des tremblements de terre sont localis\u00E9s sur des failles. Plus rares sont les s\u00E9ismes dus \u00E0 l'activit\u00E9 volcanique ou d'origine artificielle (explosions par exemple). Il se produit de tr\u00E8s nombreux s\u00E9ismes tous les jours, mais la plupart ne sont pas ressentis par les humains. Environ cent mille s\u00E9ismes sont enregistr\u00E9s par an sur la plan\u00E8te. Les plus puissants d'entre eux comptent parmi les catastrophes naturelles les plus destructrices. La science qui \u00E9tudie ces ph\u00E9nom\u00E8nes est la sismologie et l'instrument d'\u00E9tude principal est le sismographe."@fr , "I terremoti (dal latino terrae motus), detti anche sismi o scosse telluriche, sono movimenti improvvisi e rapidi della crosta terrestre, provocati dalla liberazione di energia in un punto interno, detto ipocentro; di qui, una serie di onde elastiche, dette \"onde sismiche\", si propagano in tutte le direzioni, anche all'interno della Terra stessa; il luogo della superficie terrestre posto sulla verticale dell'ipocentro, si chiama epicentro ed \u00E8 generalmente quello pi\u00F9 interessato dal fenomeno. La superficie terrestre \u00E8 in lento ma costante movimento e i terremoti si verificano quando la tensione risultante eccede la capacit\u00E0 del materiale roccioso di sopportarla. Questa condizione occorre molto spesso ai confini delle placche tettoniche nelle quali la litosfera terrestre pu\u00F2 essere suddivisa. Gli eventi sismici che si verificano ai confini tra placche sono detti terremoti interplacca; quelli meno frequenti che avvengono all'interno delle placche della litosfera sono detti terremoti intraplacca. Ogni giorno sulla Terra si verificano migliaia di terremoti; solo qualche decina sono percepiti dalla popolazione e la maggior parte di questi ultimi causano poco o nessun danno. La durata media di una scossa \u00E8 molto al di sotto dei 30 secondi; per i terremoti pi\u00F9 forti, per\u00F2, pu\u00F2 arrivare fino a qualche minuto. Le onde elastiche che si propagano durante un terremoto sono di diverso tipo e in alcuni casi possono risultare in un movimento prevalentemente orizzontale o verticale del terreno (scossa ondulatoria o sussultoria). Un terremoto pu\u00F2 essere accompagnato da forti rumori che possono ricordare boati, rombi, tuoni, sequenze di spari, eccetera; questi suoni sono dovuti al passaggio delle onde sismiche all'atmosfera e sono pi\u00F9 intensi in vicinanza dell'epicentro. Alcuni terremoti, specialmente i pi\u00F9 forti, sono anche accompagnati, preceduti o seguiti da fenomeni naturali, come: bagliori o lampi; modificazioni improvvise del campo magnetico, elettrico o della radioattivit\u00E0 locale; nervosismo degli animali; variazione del livello delle falde o delle acque costiere; attivit\u00E0 vulcanica. Tutte queste manifestazioni hanno trovato riscontro nelle osservazioni e nelle testimonianze, e sono state studiate e confermate dalla ricerca scientifica che \u00E8 giunta alla spiegazione di ognuna di esse, anche se, in mancanza di consenso unanime, non costituiscono di fatto misure effettivamente riconosciute o adottate sul fronte della previsione."@it , "An earthquake (also known as a tremor or temblor) is the result of a sudden release of energy in the Earth's crust that creates seismic waves. Earthquakes are recorded with a seismometer, also known as a seismograph. The moment magnitude of an earthquake is conventionally reported, or the related and mostly obsolete Richter magnitude, with magnitude 3 or lower earthquakes being mostly and magnitude 7 causing serious damage over large areas. Intensity of shaking is measured on the modified Mercalli scale. At the Earth's surface, earthquakes manifest themselves by shaking and sometimes displacing the ground. When a large earthquake epicenter is located offshore, the seabed sometimes suffers sufficient displacement to cause a tsunami. The shaking in earthquakes can also trigger landslides and occasionally volcanic activity. In its most generic sense, the word earthquake is used to describe any seismic event \u2014 whether a natural phenomenon or an event caused by humans \u2014 that generates seismic waves. Earthquakes are caused mostly by rupture of geological faults, but also by volcanic activity, landslides, mine blasts, and nuclear experiments. An earthquake's point of initial rupture is called its focus or hypocenter. The term epicenter refers to the point at ground level directly above the hypocenter."@en , "\u5730\u9707\uFF08\u3058\u3057\u3093\uFF09\u3068\u306F\u3001\u666E\u6BB5\u306F\u56FA\u304F\u5BC6\u7740\u3057\u3066\u3044\u308B\u5730\u4E0B\u306E\u5730\u76E4\u3084\u5CA9\u76E4\u304C\u3001\u4E00\u5B9A\u306E\u90E8\u5206\u3092\u5883\u76EE\u306B\u3057\u3066\u3001\u6025\u306B\u305A\u308C\u52D5\u304F\u3053\u3068\u3002\u307E\u305F\u3001\u305D\u308C\u306B\u3088\u3063\u3066\u5F15\u304D\u8D77\u3053\u3055\u308C\u308B\u5730\u9762\u306E\u632F\u52D5\u3002\u6B63\u78BA\u306B\u306F\u3001\u524D\u8005\u3092\u300C\u5730\u9707\uFF08\u3058\u3057\u3093\uFF09\u300D\u3068\u547C\u3073\u3001\u5F8C\u8005\u3092\u300C\u5730\u9707\u52D5\uFF08\u3058\u3057\u3093\u3069\u3046\uFF09\u300D\u3068\u3044\u3046\u3002\u4E00\u822C\u306B\u306F\u3069\u3061\u3089\u3082\u5730\u9707\u3068\u547C\u3076\u3002\u901A\u5E38\u306F\u5730\u9707\u3068\u3044\u3046\u3068\u5730\u9707\u52D5\u3092\u610F\u5473\u3059\u308B\u3053\u3068\u304C\u591A\u3044\u3002 \u6708\u3067\u767A\u751F\u3059\u308B\u5730\u9707\u306F\u6708\u9707\u3068\u547C\u3070\u308C\u308B\u3002"@ja , "Jordskjelv skyldes langsomme bevegelser i jordskorpen som over tid skaper spenninger i jordskorpen som kan bli s\u00E5 store at den aktuelle bergarten til slutt gir etter, og plutselige forskyvninger oppst\u00E5r. Denne typen jordskjelv kalles tektoniske jordskjelv og er de mest vanlige, mens jordskjelv som skyldes vulkanutbrudd forekommer langt sjeldnere. Senteret for et skjelv kalles hyposentrum i jordens indre, mens det samme punktet (loddrett over) p\u00E5 jordoverflaten kalles episentrum. Et jordskjelvs st\u00F8rrelse kan m\u00E5les i seismisk moment, magnitude, intensitet eller fysisk st\u00F8rrelse. De tre st\u00F8rste jordskjelvene gjennom tidene \u2013 og de eneste som har m\u00E5lt 9,0 eller mer p\u00E5 Richters skala \u2013 var langfredagsjordskjelvet i Alaska 27. mars 1964 (m\u00E5lt til 9,2), i Chile 22. mai 1960 (m\u00E5lt til 9,5) og jordskjelvet i Indiahavet 26. desember 2004 (m\u00E5lt til 9,0). De siste hundre \u00E5rene har over \u00E9n million mennesker omkommet p\u00E5 grunn av jordskjelv."@no ; rdfs:comment "I terremoti (dal latino terrae motus), detti anche sismi o scosse telluriche, sono movimenti improvvisi e rapidi della crosta terrestre, provocati dalla liberazione di energia in un punto interno, detto ipocentro; di qui, una serie di onde elastiche, dette \"onde sismiche\", si propagano in tutte le direzioni, anche all'interno della Terra stessa; il luogo della superficie terrestre posto sulla verticale dell'ipocentro, si chiama epicentro ed \u00E8 generalmente quello pi\u00F9 interessato dal fenomeno."@it , ""@ja , "A f\u00F6ldreng\u00E9s a f\u00F6ldfelsz\u00EDn egy darabj\u00E1nak hirtelen bek\u00F6vetkez\u0151 \u00E9s n\u00E9ha katasztrof\u00E1lis k\u00F6vetkezm\u00E9nyekkel j\u00E1r\u00F3 mozg\u00E1sa. A f\u00F6ldreng\u00E9sek \u00E1ltal\u00E1ban a f\u00F6ldk\u00E9regben felgy\u00FClemlett energia felszabadul\u00E1sakor keletkez\u0151 l\u00F6k\u00E9shull\u00E1mok, melyek a keletkez\u00E9si pontb\u00F3l, amit a f\u00F6ldreng\u00E9s hipocentrum\u00E1nak nevez\u00FCnk, g\u00F6mbh\u00E9jszer\u0171en terjednek minden ir\u00E1nyba. A fesz\u00FClts\u00E9g t\u00F6bb okb\u00F3l halmoz\u00F3dhat fel."@hu , "Un tremblement de terre, ou s\u00E9isme, r\u00E9sulte de la lib\u00E9ration brusque d'\u00E9nergie accumul\u00E9e par les d\u00E9placements et les frictions des diff\u00E9rentes plaques de la cro\u00FBte terrestre (ph\u00E9nom\u00E8nes regroup\u00E9s sous le nom de tectonique des plaques). La plupart des tremblements de terre sont localis\u00E9s sur des failles. Plus rares sont les s\u00E9ismes dus \u00E0 l'activit\u00E9 volcanique ou d'origine artificielle (explosions par exemple)."@fr , ""@zh , "Als Erdbeben werden messbare Ersch\u00FCtterungen des Erdk\u00F6rpers bezeichnet. Der deutlich gr\u00F6\u00DFte Anteil aufgezeichneter Erdbeben ist zu schwach, um von Menschen wahrgenommen zu werden. Auch andere Bewegungen der Erdoberfl\u00E4che, wie etwa durch Tidenhub oder durch Eigenschwingungen der Erde sind nicht f\u00FChlbar, da sie zu langsam erfolgen oder zu schwach sind. Erdbeben bestehen in der Regel nicht aus einzelnen Ersch\u00FCtterungen, sondern ziehen meist weitere nach sich."@de , "\u0417\u0435\u043C\u043B\u0435\u0442\u0440\u0443\u0301\u0441 (\u0430\u043D\u0433\u043B. earthquake, earth shock, \u043D\u0456\u043C."@uk , "Trz\u0119sienie ziemi - gwa\u0142towne roz\u0142adowanie napr\u0119\u017Ce\u0144 powsta\u0142ych w skorupie ziemskiej w czasie ruch\u00F3w fragment\u00F3w litosfery. Z miejsca uwolnienia tych napr\u0119\u017Ce\u0144 (hipocentrum – ogniska trz\u0119sienia ziemi) rozchodz\u0105 si\u0119 fale sejsmiczne. Punkt na powierzchni Ziemi po\u0142o\u017Cony nad ogniskiem to miejsce, gdzie fale docieraj\u0105 najwcze\u015Bniej i gdzie straty s\u0105 najwi\u0119ksze. Si\u0142a wstrz\u0105s\u00F3w maleje w miar\u0119 oddalania si\u0119 od epicentrum. Badaniem trz\u0119sie\u0144 ziemi zajmuje si\u0119 sejsmologia."@pl , "Un terremoto \u2014 tambi\u00E9n llamado se\u00EDsmo o sismo (del griego \"\u03C3\u03B5\u03B9\u03C3\u03BC\u03CC\u03C2\", temblor) o, simplemente, temblor de tierra (en algunas zonas se considera que un se\u00EDsmo o sismo o temblor es un terremoto de menor magnitud) \u2014 es una sacudida del terreno que se produce debido al choque de las placas tect\u00F3nicas y a la liberaci\u00F3n de energ\u00EDa en el curso de una reorganizaci\u00F3n brusca de materiales de la corteza terrestre al superar el estado de equilibrio mec\u00E1nico."@es , "Jordskjelv skyldes langsomme bevegelser i jordskorpen som over tid skaper spenninger i jordskorpen som kan bli s\u00E5 store at den aktuelle bergarten til slutt gir etter, og plutselige forskyvninger oppst\u00E5r. Denne typen jordskjelv kalles tektoniske jordskjelv og er de mest vanlige, mens jordskjelv som skyldes vulkanutbrudd forekommer langt sjeldnere. Senteret for et skjelv kalles hyposentrum i jordens indre, mens det samme punktet (loddrett over) p\u00E5 jordoverflaten kalles episentrum."@no , "An earthquake (also known as a tremor or temblor) is the result of a sudden release of energy in the Earth's crust that creates seismic waves. Earthquakes are recorded with a seismometer, also known as a seismograph. The moment magnitude of an earthquake is conventionally reported, or the related and mostly obsolete Richter magnitude, with magnitude 3 or lower earthquakes being mostly and magnitude 7 causing serious damage over large areas."@en , "Zem\u011Bt\u0159esen\u00ED je n\u00E1hl\u00FD pohyb zemsk\u00E9 k\u016Fry, vyvolan\u00FD uvoln\u011Bn\u00EDm nap\u011Bt\u00ED \u2013 nap\u0159. z neust\u00E1l\u00FDch pohyb\u016F zemsk\u00FDch desek \u2013 pod\u00E9l zlom\u016F. V\u011Bt\u0161\u00ED zem\u011Bt\u0159esen\u00ED se proto obvykle vyskytuj\u00ED v t\u011Bch oblastech sv\u011Bta, kter\u00FDmi v\u00FDznamn\u00E9 zlomy proch\u00E1zej\u00ED Studiu zem\u011Bt\u0159esen\u00ED se v\u011Bnuje geofyzika konkr\u00E9tn\u011B jej\u00ED sou\u010D\u00E1st seismologie. M\u00EDsto vzniku zem\u011Bt\u0159esen\u00ED se naz\u00FDv\u00E1 ohnisko neboli hypocentrum, jeho kolm\u00FD pr\u016Fm\u011Bt na zemsk\u00E9m povrchu se naz\u00FDv\u00E1 epicentrum."@cs , "\u0417\u0435\u043C\u043B\u0435\u0442\u0440\u044F\u0441\u0435\u0301\u043D\u0438\u044F \u2014 \u043F\u043E\u0434\u0437\u0435\u043C\u043D\u044B\u0435 \u0442\u043E\u043B\u0447\u043A\u0438 \u0438 \u043A\u043E\u043B\u0435\u0431\u0430\u043D\u0438\u044F \u043F\u043E\u0432\u0435\u0440\u0445\u043D\u043E\u0441\u0442\u0438 \u0417\u0435\u043C\u043B\u0438, \u0432\u044B\u0437\u0432\u0430\u043D\u043D\u044B\u0435 \u0435\u0441\u0442\u0435\u0441\u0442\u0432\u0435\u043D\u043D\u044B\u043C\u0438 \u043F\u0440\u0438\u0447\u0438\u043D\u0430\u043C\u0438 (\u0433\u043B\u0430\u0432\u043D\u044B\u043C \u043E\u0431\u0440\u0430\u0437\u043E\u043C \u0442\u0435\u043A\u0442\u043E\u043D\u0438\u0447\u0435\u0441\u043A\u0438\u043C\u0438 \u043F\u0440\u043E\u0446\u0435\u0441\u0441\u0430\u043C\u0438) \u0438\u043B\u0438 \u0438\u0441\u043A\u0443\u0441\u0441\u0442\u0432\u0435\u043D\u043D\u044B\u043C\u0438 \u043F\u0440\u043E\u0446\u0435\u0441\u0441\u0430\u043C\u0438 (\u0432\u0437\u0440\u044B\u0432\u044B, \u0437\u0430\u043F\u043E\u043B\u043D\u0435\u043D\u0438\u0435 \u0432\u043E\u0434\u043E\u0445\u0440\u0430\u043D\u0438\u043B\u0438\u0449, \u043E\u0431\u0440\u0443\u0448\u0435\u043D\u0438\u0435\u043C \u043F\u043E\u0434\u0437\u0435\u043C\u043D\u044B\u0445 \u043F\u043E\u043B\u043E\u0441\u0442\u0435\u0439 \u0433\u043E\u0440\u043D\u044B\u0445 \u0432\u044B\u0440\u0430\u0431\u043E\u0442\u043E\u043A)."@ru , "Maanj\u00E4ristys on Maan peruskallion t\u00E4r\u00E4htely\u00E4, joka on voimakkaana hyvin tuhoisaa rakennuksille ja ihmisille. Heikko j\u00E4ristys heiluttaa lamppuja, voimakas j\u00E4ristys romahduttaa talot, hyvin voimakas myll\u00E4\u00E4 maaper\u00E4\u00E4kin. Meren pohjassa tapahtunut maanj\u00E4ristys voi aiheuttaa voimakkaan hy\u00F6kyaallon, tsunamin. Maanj\u00E4ristyksen voimaa mitataan yleens\u00E4 Richterin asteikolla ja tuhoisuutta Mercallin asteikolla. Yli seitsem\u00E4n Richterin j\u00E4ristykset ovat hyvin tuhoisia."@fi , "Deprem, yerkabu\u011Fu i\u00E7indeki k\u0131r\u0131lmalar nedeniyle ani olarak ortaya \u00E7\u0131kan titre\u015Fimlerin dalgalar halinde yay\u0131larak ge\u00E7tikleri ortamlar\u0131 ve yery\u00FCzeyini sarsma olay\u0131d\u0131r. Magma \u00FCzerinde y\u00FCzen levhalar konveksiyonel ak\u0131m sayesinde s\u00FCrekli hareket halindedir. K\u0131talar\u0131n hareketi ile plato s\u0131n\u0131rlar\u0131nda kaynama ve ayr\u0131lmadaki s\u00FCrt\u00FCnmeden olu\u015Fan kinetik enerjinin aniden b\u00FCy\u00FCk bir g\u00FC\u00E7le bo\u015Falabilir."@tr , "Cutremur sau seism sunt termenii folosi\u0163i pentru mi\u015Fc\u0103rile p\u0103m\u00E2ntului, ce constau \u00EEn vibra\u0163ii originate \u00EEn zonele interne ale Terrei, propagate \u00EEn form\u0103 de unde prin roci. Aceste vibra\u0163ii rezult\u0103 din mi\u015Fc\u0103rile pl\u0103cilor tectonice, fiind des cauzate de o activitate vulcanic\u0103. \u00CEn unele \u0163\u0103ri, cuv\u00E2ntul cutremur este folosit doar pentru acele mi\u015Fc\u0103ri ale pl\u0103cilor tectonice care provoac\u0103 daune majore \u015Fi seism sau mi\u015Fc\u0103ri seismice pentru cele care trec neobservate."@ro , "En jordb\u00E4vning, \u00E4ven kallat jordskalv, inneb\u00E4r att marken skakar och r\u00F6r sig p\u00E5 grund av pl\u00F6tsligt utl\u00F6sta r\u00F6relser i jordskorpan eller \u00F6vre delen av manteln, den s\u00E5 kallade litosf\u00E4ren. Skakningarna kan orsaka sv\u00E5ra skador p\u00E5 byggnader, och om jordb\u00E4vningen intr\u00E4ffar under havet kan en flodv\u00E5g, tsunami, utl\u00F6sas och f\u00E4rdas l\u00E5nga str\u00E4ckor och orsaka stor f\u00F6r\u00F6delse n\u00E4r den n\u00E5r land."@sv , "Un terratr\u00E8mol, - tamb\u00E9 anomenat sisme (del grec \"\u03C3\u03B5\u03B9\u03C3\u03BC\u03CC\u03C2\", tremolor) o, simplement, tremolor de terra (en algunes zones es considera que un sisme \u00E9s un terratr\u00E8mol de menor magnitud) - resulta de l'alliberament brusc d'energia acumulada pels despla\u00E7aments i les friccions de les diferents plaques de l'escor\u00E7a terrestre (fen\u00F2mens reagrupats sota el nom de plaques tect\u00F2niques). La majoria dels terratr\u00E8mols s\u00F3n localitzats sobre falles."@ca , "Um sismo, tamb\u00E9m chamado de terremoto ou terramoto, \u00E9 um fen\u00F4meno de vibra\u00E7\u00E3o brusca e passageira da superf\u00EDcie da Terra, resultante de movimentos subterr\u00E2neos de placas rochosas, de atividade vulc\u00E2nica, ou por deslocamentos (migra\u00E7\u00E3o) de gases no interior da Terra, principalmente metano. O movimento \u00E9 causado pela libera\u00E7\u00E3o r\u00E1pida de grandes quantidades de energia sob a forma de ondas s\u00EDsmicas."@pt , "Een aardbeving is een trilling of schokkende beweging van de aardkorst. Aardbevingen vinden plaats als er in de aardkorst plotseling veel energie vrijkomt. De energie plant zich dan in een golfbeweging vanuit het centrum naar de omgeving voort. Het denkbeeldige punt waar de beving ontstaat, het zwaartepunt van de energiedichtheid, heet het hypocentrum. Het punt aan het aardoppervlak daar loodrecht boven wordt het epicentrum genoemd."@nl ; foaf:depiction . @prefix skos: . @prefix ns12: . dbpedia:Earthquake skos:subject ns12:Geological_hazards , ns12:Earthquakes , ns12:Earthquake_engineering , ns12:Seismology . @prefix ns13: . dbpedia:Earthquake dbpprop:wikiPageUsesTemplate ns13:convert ; dbpprop:convertProperty "ft"@en , "m"@en , 0 , 1650 . @prefix ns14: . dbpedia:Earthquake dbpprop:hasPhotoCollection ns14:Earthquake . dbpedia:Agatha_of_Sicily dbpprop:patronage dbpedia:Earthquake . dbpedia:Az-Zalzala dbpprop:meaningOfTheName dbpedia:Earthquake . dbpprop:disambiguates dbpedia:Earthquake . dbpedia:Geology dbpprop:columnsListProperty dbpedia:Earthquake . dbpprop:disambiguates dbpedia:Earthquake . dbpedia:Earth_quakes dbpprop:redirect dbpedia:Earthquake . dbpedia:Earth_tremor dbpprop:redirect dbpedia:Earthquake . dbpedia:Seismic_activity dbpprop:redirect dbpedia:Earthquake . dbpedia:Tectonic_earthquake dbpprop:redirect dbpedia:Earthquake . dbpedia:Seism dbpprop:redirect dbpedia:Earthquake . dbpprop:redirect dbpedia:Earthquake . dbpedia:Earth_quake dbpprop:redirect dbpedia:Earthquake . dbpedia:Earthquakes dbpprop:redirect dbpedia:Earthquake . dbpedia:Seaquake dbpprop:redirect dbpedia:Earthquake . dbpedia:Causes_of_earthquakes dbpprop:redirect dbpedia:Earthquake . dbpedia:The_kinds_of_earthquakes dbpprop:redirect dbpedia:Earthquake .