. . . . . . . "y"@en . . . . . . . . . . . . . . . . . . . . . . . . . . . "L'erosi\u00F3 en geomorfologia, \u00E9s el proc\u00E9s de degradaci\u00F3 i de transformaci\u00F3 del relleu, i de les roques, causat per tot agent extern (diferent de la tect\u00F2nica). Normalment hi ha erosi\u00F3 pel transport de sediments a trav\u00E9s del vent, aigua o gel; a favor del pendent de s\u00F2ls i altres materials sota la for\u00E7a de la gravetat; o per organismes vius com s\u00F3n els animals excavadors, que s'anomena bioerosi\u00F3. Malgrat que l'erosi\u00F3 \u00E9s un proc\u00E9s natural s'ha incrementat molt\u00EDssim per l'\u00FAs hum\u00E0 de la terra. Aproximadament un 40% de la superf\u00EDcie agr\u00EDcola mundial est\u00E0 seriosament degradada per l'erosi\u00F3. L'erosionabilitat mesura la capacitat d'un s\u00F2l de ser erosionat i dep\u00E8n de factors com la duresa, estar cobert per vegetaci\u00F3 o el seu pendent. L'erosi\u00F3 no \u00E9s el mateix que la meteoritzaci\u00F3, que \u00E9s la disgregaci\u00F3 de la roca sense despla\u00E7ament del material (si b\u00E9 la meteoritzaci\u00F3 facilita l'erosi\u00F3), ni \u00E9s el mateix que el transport dels materials erosionats, que \u00E9s el seg\u00FCent pas del cicle geol\u00F2gic, i que normalment realitza el mateix agent que ha produ\u00EFt l'erosi\u00F3. Un problema particularment seri\u00F3s \u00E9s l'erosi\u00F3 costanera propiciada pel fet de fer construccions molt a la vora de la mar, les quals pertorben el flux de sediments cap a elles."@ca . . . . . . . . . . . . . . . . "\u4FB5\u98DF\uFF08\u3057\u3093\u3057\u3087\u304F\u3001\u4FB5\u8755\u3068\u3082\u3001erosion\uFF09\u3068\u306F\u3001\u6C34\u3084\u98A8\u306A\u3069\u306E\u5916\u7684\u55B6\u529B\u306B\u3088\u308A\u5CA9\u77F3\u3084\u5730\u5C64\u304C\u524A\u3089\u308C\u308B\u3053\u3068\u3002\u6D78\u98DF\uFF08\u6D78\u8755\uFF09\u3068\u8868\u8A18\u3059\u308B\u5834\u5408\u3082\u3042\u308B\u304C\u3001\u6C34\u306B\u300C\u6D78\u308B\u300D\u3068\u306F\u9650\u3089\u306A\u3044\u305F\u3081\u3001\u5B66\u8853\u7684\u306B\u306F\u4FB5\u98DF\u306E\u8868\u8A18\u3092\u7528\u3044\u308B\u3002 \u6C34\u306E\u5834\u5408\u306F\u96E8\u6C34\u304A\u3088\u3073\u305D\u308C\u304C\u6D41\u308C\u305F\u3082\u306E\u304B\u3089\u6CB3\u5DDD\u306E\u6D41\u308C\u3001\u6D77\u3084\u6E56\u306E\u6CE2\u3001\u6C37\u6CB3\u306A\u3069\u304C\u539F\u56E0\uFF08scoring\uFF09\u3002\u6C34\u6D41\u305D\u306E\u3082\u306E\u306B\u3088\u3063\u3066\u7269\u7406\u7684\u4FB5\u98DF\u3092\u3059\u308B\u5834\u5408\u3092\u300C\u6D17\u6398\u300D\u3001\u9577\u6642\u9593\u306B\u308F\u305F\u3063\u3066\u5805\u3044\u5CA9\u76E4\u306A\u3069\u304C\u6469\u8017\u3055\u308C\u308B\u3053\u3068\u3092\u300C\u78E8\u98DF\u300D\u3068\u533A\u5225\u3059\u308B\u3053\u3068\u3082\u3042\u308B\u3002 \u98A8\u306E\u5834\u5408\u306F\u98A8\u305D\u306E\u3082\u306E\u306E\u307B\u304B\u3001\u98A8\u3067\u98DB\u3070\u3055\u308C\u3066\u304F\u308B\u7802\u7C92\u306B\u3088\u3063\u3066\u524A\u3089\u308C\u308B\uFF08\u30B5\u30F3\u30C9\u30D6\u30E9\u30B9\u30C8\u72B6\u614B\uFF09\u3053\u3068\u3082\u591A\u3044\u3002\u3053\u308C\u306F\u98A8\u98DF\uFF08deflation\uFF09\u3068\u547C\u3070\u308C\u308B\u3053\u3068\u3082\u3042\u308B\u3002\u307E\u305F\u3001\u8C9D\u985E\u3084\u30A6\u30CB\u306A\u3069\u306B\u3088\u3063\u3066\u77F3\u7070\u5CA9\u306A\u3069\u304C\u4FB5\u98DF\u3055\u308C\u308B\u3053\u3068\u3092\u751F\u7269\u4FB5\u98DF\uFF08bioerosion\uFF09\u3068\u3044\u3046\u3002"@ja . . . . . . . . . . . . . . . . . . . . . "\u4FB5\u98DF\uFF08\u3057\u3093\u3057\u3087\u304F\u3001\u4FB5\u8755\u3068\u3082\u3001erosion\uFF09\u3068\u306F\u3001\u6C34\u3084\u98A8\u306A\u3069\u306E\u5916\u7684\u55B6\u529B\u306B\u3088\u308A\u5CA9\u77F3\u3084\u5730\u5C64\u304C\u524A\u3089\u308C\u308B\u3053\u3068\u3002\u6D78\u98DF\uFF08\u6D78\u8755\uFF09\u3068\u8868\u8A18\u3059\u308B\u5834\u5408\u3082\u3042\u308B\u304C\u3001\u6C34\u306B\u300C\u6D78\u308B\u300D\u3068\u306F\u9650\u3089\u306A\u3044\u305F\u3081\u3001\u5B66\u8853\u7684\u306B\u306F\u4FB5\u98DF\u306E\u8868\u8A18\u3092\u7528\u3044\u308B\u3002 \u6C34\u306E\u5834\u5408\u306F\u96E8\u6C34\u304A\u3088\u3073\u305D\u308C\u304C\u6D41\u308C\u305F\u3082\u306E\u304B\u3089\u6CB3\u5DDD\u306E\u6D41\u308C\u3001\u6D77\u3084\u6E56\u306E\u6CE2\u3001\u6C37\u6CB3\u306A\u3069\u304C\u539F\u56E0\uFF08scoring\uFF09\u3002\u6C34\u6D41\u305D\u306E\u3082\u306E\u306B\u3088\u3063\u3066\u7269\u7406\u7684\u4FB5\u98DF\u3092\u3059\u308B\u5834\u5408\u3092\u300C\u6D17\u6398\u300D\u3001\u9577\u6642\u9593\u306B\u308F\u305F\u3063\u3066\u5805\u3044\u5CA9\u76E4\u306A\u3069\u304C\u6469\u8017\u3055\u308C\u308B\u3053\u3068\u3092\u300C\u78E8\u98DF\u300D\u3068\u533A\u5225\u3059\u308B\u3053\u3068\u3082\u3042\u308B\u3002 \u98A8\u306E\u5834\u5408\u306F\u98A8\u305D\u306E\u3082\u306E\u306E\u307B\u304B\u3001\u98A8\u3067\u98DB\u3070\u3055\u308C\u3066\u304F\u308B\u7802\u7C92\u306B\u3088\u3063\u3066\u524A\u3089\u308C\u308B\uFF08\u30B5\u30F3\u30C9\u30D6\u30E9\u30B9\u30C8\u72B6\u614B\uFF09\u3053\u3068\u3082\u591A\u3044\u3002\u3053\u308C\u306F\u98A8\u98DF\uFF08deflation\uFF09\u3068\u547C\u3070\u308C\u308B\u3053\u3068\u3082\u3042\u308B\u3002\u307E\u305F\u3001\u8C9D\u985E\u3084\u30A6\u30CB\u306A\u3069\u306B\u3088\u3063\u3066\u77F3\u7070\u5CA9\u306A\u3069\u304C\u4FB5\u98DF\u3055\u308C\u308B\u3053\u3068\u3092\u751F\u7269\u4FB5\u98DF\uFF08bioerosion\uFF09\u3068\u3044\u3046\u3002"@ja . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . "Erosion (fr\u00E5n latin ero'sio n\u00F6tning) \u00E4r nedn\u00F6tning och transport av berg, jord eller annat material p\u00E5 grund av mekanisk eller kemisk p\u00E5verkan. Erosion kan till exempel orsakas av vind, rinnande vatten, v\u00E5gor, glaci\u00E4rer, gravitationsr\u00F6relser, levande organismer, men \u00E4ven genom massr\u00F6relsernas materialtransport nedf\u00F6r sluttningar. Till skillnad fr\u00E5n vittring s\u00E5 f\u00F6ruts\u00E4tter begreppet erosion att det \u00E4ven sker en bortf\u00F6rsel. Erosion \u00E4r en utj\u00E4mnande kraft (en exogen kraft), som \"str\u00E4var\" efter att j\u00E4mna ut markytan, med ett peneplan som ett slutstadium."@sv . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 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"Erosion is the action of surface processes (such as water flow or wind) that removes soil, rock, or dissolved material from one location on the Earth's crust, and then transports it to another location where it is deposited. Erosion is distinct from weathering which involves no movement. Removal of rock or soil as clastic sediment is referred to as physical or mechanical erosion; this contrasts with chemical erosion, where soil or rock material is removed from an area by dissolution. Eroded sediment or solutes may be transported just a few millimetres, or for thousands of kilometres."@en . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . "Eros\u00E3o \u00E9 a a\u00E7\u00E3o de processos superficiais, (tal como a a\u00E7\u00E3o do fluxo de \u00E1gua ou vento) que remove solo, rochas, ou material dissolvido de um local na crosta da Terra, que ent\u00E3o o transporta para outro local. Enquanto a eros\u00E3o \u00E9 a\u00E7\u00E3o desses processos superficiais, a gliptog\u00EAnese \u00E9 a forma\u00E7\u00E3o da superf\u00EDcie terrestre como consequ\u00EAncia dos processos erosivos que provocam a destrui\u00E7\u00E3o do relevo preexistente. Os dois termos s\u00E3o ocasionalmente usados como sin\u00F4nimos mesmo na literatura acad\u00EAmica. A ruptura de part\u00EDculas provenientes de pedra e solo em sedimento cl\u00E1stico \u00E9 denominado como meteoriza\u00E7\u00E3o f\u00EDsica ou mec\u00E2nica; isso contrasta com a meteoriza\u00E7\u00E3o qu\u00EDmica, onde o solo ou material de rocha \u00E9 removido atrav\u00E9s da dissolu\u00E7\u00E3o, promovido por um solvente (tipicamente \u00E1gua), seguido pelo fluxo da solu\u00E7\u00E3o. Os sedimentos ou solutos erodidos podem ser transportados apenas por alguns mil\u00EDmetros ou para milhares de quil\u00F4metros. As taxas naturais de eros\u00E3o s\u00E3o controladas pela a\u00E7\u00E3o de agentes geom\u00F3rficos, como chuva; desgaste rochoso em rios; eros\u00E3o costeira pelo mar e ondas; delapida\u00E7\u00E3o glacial, abras\u00E3o; inunda\u00E7\u00F5es locais; abras\u00E3o do vento; processos de \u00E1gua subterr\u00E2nea; e processos de movimento de massa em paisagens \u00EDngremes como deslizamentos de terra e fluxos de detritos. As taxas a que tais processos atuam controlar\u00E3o a velocidade da eros\u00E3o de uma superf\u00EDcie. Normalmente, a eros\u00E3o f\u00EDsica prossegue mais rapidamente em superf\u00EDcies inclinadas, e as taxas tamb\u00E9m podem ser sens\u00EDveis a algumas propriedades controladas climaticamente, incluindo quantidades de \u00E1gua fornecida (por exemplo, pela chuva), a velocidade do vento, a busca da onda ou a temperatura atmosf\u00E9rica (especialmente para alguns processos relacionados ao gelo).Tamb\u00E9m s\u00E3o poss\u00EDveis entre as taxas de eros\u00E3o e a quantidade de material erodido que j\u00E1 \u00E9 transportado, por exemplo, um rio ou uma geleira. Os processos de eros\u00E3o que produzem sedimentos ou solutos de um lugar contrastam com os de deposi\u00E7\u00E3o, que controlam a chegada e coloca\u00E7\u00E3o de material em um novo local. Enquanto a eros\u00E3o \u00E9 um processo natural, as atividades humanas aumentaram entre 10-40 vezes a taxa em que a eros\u00E3o est\u00E1 ocorrendo globalmente. Em regi\u00F5es bem conhecidas da agricultura, como as Montanhas dos Apalaches, localizada nos Estados Unidos, pr\u00E1ticas agr\u00EDcolas intensivas aumentaram a taxa de eros\u00E3o em at\u00E9 100x da velocidade em rela\u00E7\u00E3o a taxa natural de eros\u00E3o na regi\u00E3o. A eros\u00E3o excessiva (ou acelerada) causa problemas \"no local\" e \"fora do local\". Os impactos no local incluem diminui\u00E7\u00E3o da produtividade agr\u00EDcola e (em paisagens naturais) colapso ecol\u00F3gico, tanto por causa da perda das camadas do solo superior ricas em nutrientes. Em alguns casos, o eventual resultado final \u00E9 a desertifica\u00E7\u00E3o. Os efeitos fora do local incluem sedimenta\u00E7\u00E3o de vias naveg\u00E1veis e eutrofiza\u00E7\u00E3o de corpos d'\u00E1gua, bem como danos causados por sedimentos em estradas e casas. A eros\u00E3o causada pela \u00E1gua e vento s\u00E3o as duas principais causas de degrada\u00E7\u00E3o da terra; que combinados, s\u00E3o respons\u00E1veis por cerca de 84% da extens\u00E3o global da terra degradada, tornando a eros\u00E3o excessiva um dos problemas ambientais mais significativos em todo o mundo. A agricultura intensiva, o desmatamento, as estradas, as mudan\u00E7as clim\u00E1ticas antropog\u00EAnicas e a expans\u00E3o urbana est\u00E3o entre as atividades humanas mais significativas em rela\u00E7\u00E3o ao seu efeito na estimula\u00E7\u00E3o da eros\u00E3o. No entanto, existem muitas pr\u00E1ticas de preven\u00E7\u00E3o e remedia\u00E7\u00E3o que podem reduzir ou limitar a eros\u00E3o de solos vulner\u00E1veis."@pt . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . "y"@en . . . . . . . . . . . . . . . . . . . . . . . . . . . "( \uD615\uD0DC\uD559\uC5D0 \uB300\uD574\uC11C\uB294 \uCE68\uC2DD (\uD615\uD0DC\uD559) \uBB38\uC11C\uB97C \uCC38\uACE0\uD558\uC2ED\uC2DC\uC624.) \uCE68\uC2DD(\u6D78\u8755, \uC601\uC5B4: erosion) \uC791\uC6A9\uC740 \uC911\uB825\uC5D0 \uB530\uB978 \uBC18\uC751\uC774\uB098 \uC0DD\uBB3C\uC5D0 \uB530\uB978 (bioerosion)\uC73C\uB85C \uBC14\uB78C, \uC720\uC218, \uC5BC\uC74C \uB530\uC704\uC758 \uC720\uB3D9\uCCB4\uC5D0 \uC758\uD558\uC5EC \uC9C0\uD45C(\uD1A0\uC591, \uBC14\uC704, )\uAC00 \uAE4E\uC784\uC73C\uB85C\uC368 \uAD11\uBB3C \uC785\uC790\uAC00 \uB5A8\uC5B4\uC9C0\uAC70\uB098 \uC774\uB3D9\uD558\uB294 \uD604\uC0C1\uC744 \uB9D0\uD55C\uB2E4. \uCE68\uC2DD \uC791\uC6A9\uC740 \uD654\uD559\uC801\uC73C\uB85C\uB098 \uBB3C\uB9AC\uC801\uC73C\uB85C \uBC14\uC704 \uC18D \uAD11\uBB3C\uC774 \uAE4E\uC774\uB294 \uACFC\uC815\uC778 \uD48D\uD654 \uC791\uC6A9\uACFC \uAD6C\uBD84\uD55C\uB2E4. \uCE68\uC2DD\uC744 \uBC1B\uC740 \uBB3C\uC9C8\uC740 \uB300\uAC1C \uC9C0\uD45C\uBA74\uC758 \uB192\uC740 \uC9C0\uC5ED\uC5D0\uC11C \uB0AE\uC740 \uC9C0\uC5ED\uC73C\uB85C \uC774\uB3D9\uD55C\uB2E4. \uADF8\uB9AC\uD558\uC5EC \uC0B0\uC744 \uAE4E\uC544 \uB0B4\uB9AC\uAC70\uB098 \uACC4\uACE1\uC744 \uBA54\uC6B0\uACE0, \uD558\uCC9C\uC744 \uC0C8\uB85C \uB9CC\uB4E4\uAC70\uB098 \uC5C6\uC560\uBA74\uC11C \uC9C0\uD615\uC744 \uBCC0\uD654\uC2DC\uD0A8\uB2E4. \uCE68\uC2DD\uC73C\uB85C \uC778\uD574 \uB18D\uC9C0\uAC00 \uD669\uD3D0\uD654\uD558\uACE0 \uB18D\uC9C0\uC758 \uBE44\uB8CC\uB97C \uC53B\uC5B4\uB0B4\uC5B4 \uD638\uC218\uC640 \uAC15\uC744 \uC624\uC5FC\uC2DC\uD0A8\uB2E4. \uB610 \uCE68\uC2DD\uB41C \uD1A0\uC591\uC740 \uB3C4\uB791\u00B7\uBABB\u00B7\uC800\uC218\uC9C0 \uB4F1\uC744 \uB9C9\uC544 \uAD00\uAC1C\uB97C \uBC29\uD574\uD55C\uB2E4. \uCE68\uC2DD \uC791\uC6A9\uC740 \uBCF8\uB798 \uC790\uC5F0\uC2A4\uB7EC\uC6B4 \uACFC\uC815\uC774\uC9C0\uB9CC \uB9CE\uC740 \uACF3\uC5D0\uC11C \uC778\uAC04\uC758 \uC5D0 \uC758\uD574 \uC774\uB7EC\uD55C \uC791\uC6A9\uC774 \uC99D\uAC00\uB418\uAE30\uB3C4 \uD55C\uB2E4. , \uACFC\uB3C4\uD55C \uBC29\uBAA9, \uBB34\uBD84\uBCC4\uD55C \uAC74\uCD95 \uD65C\uB3D9\uC744 \uBE44\uB86F\uD55C \uC9C8 \uB0AE\uC740 \uD1A0\uC9C0 \uC774\uC6A9\uC774 \uD2B9\uD788 \uC774\uB7EC\uD558\uB2E4. \uB18D\uC791\uBB3C \uC0DD\uC0B0\uC5D0 \uC4F0\uC774\uB294 \uD1A0\uC9C0\uB294 \uC790\uC5F0 \uC18D \uCC44\uC18C\uB85C \uC774\uB8E8\uC5B4\uC9C4 \uB545\uBCF4\uB2E4 \uC77C\uBC18\uC801\uC73C\uB85C \uC5C4\uCCAD\uB09C \uC591\uC758 \uCE68\uC2DD \uC791\uC6A9\uC744 \uACAA\uAC8C \uB41C\uB2E4."@ko . . "Eroze"@cs . . . . . . . . . . . "Eros\u00E3o \u00E9 a a\u00E7\u00E3o de processos superficiais, (tal como a a\u00E7\u00E3o do fluxo de \u00E1gua ou vento) que remove solo, rochas, ou material dissolvido de um local na crosta da Terra, que ent\u00E3o o transporta para outro local. Enquanto a eros\u00E3o \u00E9 a\u00E7\u00E3o desses processos superficiais, a gliptog\u00EAnese \u00E9 a forma\u00E7\u00E3o da superf\u00EDcie terrestre como consequ\u00EAncia dos processos erosivos que provocam a destrui\u00E7\u00E3o do relevo preexistente. Os dois termos s\u00E3o ocasionalmente usados como sin\u00F4nimos mesmo na literatura acad\u00EAmica. A ruptura de part\u00EDculas provenientes de pedra e solo em sedimento cl\u00E1stico \u00E9 denominado como meteoriza\u00E7\u00E3o f\u00EDsica ou mec\u00E2nica; isso contrasta com a meteoriza\u00E7\u00E3o qu\u00EDmica, onde o solo ou material de rocha \u00E9 removido atrav\u00E9s da dissolu\u00E7\u00E3o, promovido por um solvente (tipicamente \u00E1gua), seguido pelo fluxo da so"@pt . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . "1"^^ . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . "Erosie is het proces van slijtage van een vast oppervlak waarbij materiaal wordt verplaatst of geheel verdwijnt. Op Aarde gebeurt erosie vooral door de werking van wind, stromend water, ijs, maar ook ongewonere vormen van erosie zijn mogelijk als gevolg van vulkanisme en inslagen. Erosie is een fenomeen met een natuurlijke oorzaak. Menselijke activiteiten kunnen het erosieproces versterken, bijvoorbeeld door het kappen van bossen en het kaal houden van de bodem door ploegen. Erosie moet niet verward worden met verwering. Het verschil tussen erosie en verwering is dat bij erosie de grond verplaatst wordt, terwijl bij verwering de grond wel in stukjes breekt (mechanische verwering) of chemisch verandert (chemische verwering) maar op dezelfde plaats blijft. Wel is het zo dat verweerde grond vaak makkelijker erodeert."@nl . . . . . . . . . . . . . "Erosion is the action of surface processes (such as water flow or wind) that removes soil, rock, or dissolved material from one location on the Earth's crust, and then transports it to another location where it is deposited. Erosion is distinct from weathering which involves no movement. Removal of rock or soil as clastic sediment is referred to as physical or mechanical erosion; this contrasts with chemical erosion, where soil or rock material is removed from an area by dissolution. Eroded sediment or solutes may be transported just a few millimetres, or for thousands of kilometres. Agents of erosion include rainfall; bedrock wear in rivers; coastal erosion by the sea and waves; glacial plucking, abrasion, and scour; areal flooding; wind abrasion; groundwater processes; and mass movement processes in steep landscapes like landslides and debris flows. The rates at which such processes act control how fast a surface is eroded. Typically, physical erosion proceeds the fastest on steeply sloping surfaces, and rates may also be sensitive to some climatically-controlled properties including amounts of water supplied (e.g., by rain), storminess, wind speed, wave fetch, or atmospheric temperature (especially for some ice-related processes). Feedbacks are also possible between rates of erosion and the amount of eroded material that is already carried by, for example, a river or glacier. The transport of eroded materials from their original location is followed by deposition, which is arrival and emplacement of material at a new location. While erosion is a natural process, human activities have increased by 10-40 times the rate at which soil erosion is occurring globally. At agriculture sites in the Appalachian Mountains, intensive farming practices have caused erosion at up to 100 times the natural rate of erosion in the region. Excessive (or accelerated) erosion causes both \"on-site\" and \"off-site\" problems. On-site impacts include decreases in agricultural productivity and (on natural landscapes) ecological collapse, both because of loss of the nutrient-rich upper soil layers. In some cases, this leads to desertification. Off-site effects include sedimentation of waterways and eutrophication of water bodies, as well as sediment-related damage to roads and houses. Water and wind erosion are the two primary causes of land degradation; combined, they are responsible for about 84% of the global extent of degraded land, making excessive erosion one of the most significant environmental problems worldwide. Intensive agriculture, deforestation, roads, anthropogenic climate change and urban sprawl are amongst the most significant human activities in regard to their effect on stimulating erosion. However, there are many practices that can curtail or limit erosion of vulnerable soils."@en . . . . . . . . . . . . . . . . . . "Sa gheola\u00EDocht, athr\u00FA i bhfoirmeacha na tal\u00FAn tr\u00ED aistri\u00FA is iompar \u00E1bhair ag uisce, gaoth, gluaiseacht oighir, domhantarraingt is/n\u00F3 org\u00E1naigh bheo. Is iad aibhneacha na gn\u00EDomhaithe cna\u00EDte is \u00E9ifeachta\u00ED, ag cruth\u00FA patr\u00FAin cnoc is gleannta, agus crutha\u00EDonn gn\u00EDomha\u00EDocht na dtonnta imeallbhord an ch\u00F3sta. M\u00E1 aistr\u00EDonn cna\u00ED an bharrithir, is f\u00E9idir go leanfaidh tortha\u00ED suntasacha eacnama\u00EDocha."@ga . . . . . . . . . . . . . . . . . . . . . . . . . . "Sa gheola\u00EDocht, athr\u00FA i bhfoirmeacha na tal\u00FAn tr\u00ED aistri\u00FA is iompar \u00E1bhair ag uisce, gaoth, gluaiseacht oighir, domhantarraingt is/n\u00F3 org\u00E1naigh bheo. Is iad aibhneacha na gn\u00EDomhaithe cna\u00EDte is \u00E9ifeachta\u00ED, ag cruth\u00FA patr\u00FAin cnoc is gleannta, agus crutha\u00EDonn gn\u00EDomha\u00EDocht na dtonnta imeallbhord an ch\u00F3sta. M\u00E1 aistr\u00EDonn cna\u00ED an bharrithir, is f\u00E9idir go leanfaidh tortha\u00ED suntasacha eacnama\u00EDocha."@ga . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . "Erozja \u2013 proces niszczenia powierzchni terenu przez wod\u0119, wiatr, s\u0142o\u0144ce, si\u0142\u0119 grawitacji i dzia\u0142alno\u015B\u0107 organizm\u00F3w."@pl . . . . . . . . . . . . . . . . . "Erosione"@it . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . "\u4FB5\u8680\u4F5C\u7528"@zh . . . . . . . . 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"@ar . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . "\u039C\u03B5 \u03C4\u03BF\u03BD \u03CC\u03C1\u03BF \u03B1\u03C0\u03BF\u03C3\u03AC\u03B8\u03C1\u03C9\u03C3\u03B7 \u03B5\u03BD\u03BD\u03BF\u03BF\u03CD\u03BC\u03B5 \u03C4\u03B7\u03BD \u03C0\u03C1\u03BF\u03BF\u03B4\u03B5\u03C5\u03C4\u03B9\u03BA\u03AE \u03BA\u03B1\u03B9 \u03C3\u03C4\u03B1\u03B4\u03B9\u03B1\u03BA\u03AE \u03B1\u03C0\u03BF\u03C3\u03CD\u03BD\u03B8\u03B5\u03C3\u03B7 \u03C4\u03C9\u03BD \u03C5\u03BB\u03B9\u03BA\u03CE\u03BD \u03C4\u03C9\u03BD \u03B5\u03B4\u03B1\u03C6\u03CE\u03BD, \u03C4\u03C9\u03BD \u03C0\u03B5\u03C4\u03C1\u03C9\u03BC\u03AC\u03C4\u03C9\u03BD, \u03C4\u03B7\u03C2 \u03B1\u03BB\u03BB\u03AC \u03BA\u03B1\u03B9 \u03C4\u03B5\u03C7\u03BD\u03B7\u03C4\u03CE\u03BD \u03C5\u03BB\u03B9\u03BA\u03CE\u03BD \u03BC\u03B5 \u03C4\u03B7\u03BD \u03C0\u03AC\u03C1\u03BF\u03B4\u03BF \u03C4\u03BF\u03C5 \u03C7\u03C1\u03CC\u03BD\u03BF\u03C5 \u03C5\u03C0\u03CC \u03C4\u03B7\u03BD \u03B5\u03C0\u03AF\u03B4\u03C1\u03B1\u03C3\u03B7 \u03C0\u03B1\u03C1\u03B1\u03B3\u03CC\u03BD\u03C4\u03C9\u03BD \u03C4\u03BF\u03C5 \u03C0\u03B5\u03C1\u03B9\u03B2\u03AC\u03BB\u03BB\u03BF\u03BD\u03C4\u03BF\u03C2, \u03CC\u03C0\u03C9\u03C2 \u03C4\u03BF\u03C5 \u03B1\u03BD\u03AD\u03BC\u03BF\u03C5, \u03C4\u03BF\u03C5 \u03BD\u03B5\u03C1\u03BF\u03CD, \u03C4\u03BF\u03C5 \u03C0\u03AC\u03B3\u03BF\u03C5 \u03AE \u03B1\u03BA\u03CC\u03BC\u03B7 \u03BA\u03B1\u03B9 \u03C4\u03C9\u03BD \u03B6\u03C9\u03BD\u03C4\u03B1\u03BD\u03CE\u03BD \u03BF\u03C1\u03B3\u03B1\u03BD\u03B9\u03C3\u03BC\u03CE\u03BD, \u03B1\u03BB\u03BB\u03AC \u03BA\u03B1\u03B9 \u03C4\u03B7 \u03B4\u03B9\u03AC\u03B2\u03C1\u03C9\u03C3\u03B7."@el . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . "Erozio la\u016D la lingva\u0135o de fizika geografio estas la forporto de solida materio (ekzemple tero a\u016D roka\u0135o) fare de vento, akvo kaj gravito. Erozio povas esti komplete natura procezo, sed multloke pliigas \u011Din homaj aktivecoj kiel ekzemple senarbarigo kaj tropa\u015Dti\u011Do. Aliflanke homoj klopodas malhelpi al la erozio konstruante terasojn, firmigante deklivojn kaj dunojn ekzemple per kaj plantante arbojn, arbustojn a\u016D herbojn. En iuj cirkonstancoj, la uzo de dispecigita frondara ligno povas kontribui al regenerado de eroziitaj terenoj."@eo . . . . . . . . . . . . . . . . . . . . . . . . . . . . "\uCE68\uC2DD"@ko . . . . . . . . . . . . . . . "L'erosi\u00F3 en geomorfologia, \u00E9s el proc\u00E9s de degradaci\u00F3 i de transformaci\u00F3 del relleu, i de les roques, causat per tot agent extern (diferent de la tect\u00F2nica). Normalment hi ha erosi\u00F3 pel transport de sediments a trav\u00E9s del vent, aigua o gel; a favor del pendent de s\u00F2ls i altres materials sota la for\u00E7a de la gravetat; o per organismes vius com s\u00F3n els animals excavadors, que s'anomena bioerosi\u00F3. Malgrat que l'erosi\u00F3 \u00E9s un proc\u00E9s natural s'ha incrementat molt\u00EDssim per l'\u00FAs hum\u00E0 de la terra. Aproximadament un 40% de la superf\u00EDcie agr\u00EDcola mundial est\u00E0 seriosament degradada per l'erosi\u00F3."@ca . . . . . . . "Eros\u00E3o"@pt . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . "( \uD615\uD0DC\uD559\uC5D0 \uB300\uD574\uC11C\uB294 \uCE68\uC2DD (\uD615\uD0DC\uD559) \uBB38\uC11C\uB97C \uCC38\uACE0\uD558\uC2ED\uC2DC\uC624.) \uCE68\uC2DD(\u6D78\u8755, \uC601\uC5B4: erosion) \uC791\uC6A9\uC740 \uC911\uB825\uC5D0 \uB530\uB978 \uBC18\uC751\uC774\uB098 \uC0DD\uBB3C\uC5D0 \uB530\uB978 (bioerosion)\uC73C\uB85C \uBC14\uB78C, \uC720\uC218, \uC5BC\uC74C \uB530\uC704\uC758 \uC720\uB3D9\uCCB4\uC5D0 \uC758\uD558\uC5EC \uC9C0\uD45C(\uD1A0\uC591, \uBC14\uC704, )\uAC00 \uAE4E\uC784\uC73C\uB85C\uC368 \uAD11\uBB3C \uC785\uC790\uAC00 \uB5A8\uC5B4\uC9C0\uAC70\uB098 \uC774\uB3D9\uD558\uB294 \uD604\uC0C1\uC744 \uB9D0\uD55C\uB2E4. \uCE68\uC2DD \uC791\uC6A9\uC740 \uD654\uD559\uC801\uC73C\uB85C\uB098 \uBB3C\uB9AC\uC801\uC73C\uB85C \uBC14\uC704 \uC18D \uAD11\uBB3C\uC774 \uAE4E\uC774\uB294 \uACFC\uC815\uC778 \uD48D\uD654 \uC791\uC6A9\uACFC \uAD6C\uBD84\uD55C\uB2E4. \uCE68\uC2DD\uC744 \uBC1B\uC740 \uBB3C\uC9C8\uC740 \uB300\uAC1C \uC9C0\uD45C\uBA74\uC758 \uB192\uC740 \uC9C0\uC5ED\uC5D0\uC11C \uB0AE\uC740 \uC9C0\uC5ED\uC73C\uB85C \uC774\uB3D9\uD55C\uB2E4. \uADF8\uB9AC\uD558\uC5EC \uC0B0\uC744 \uAE4E\uC544 \uB0B4\uB9AC\uAC70\uB098 \uACC4\uACE1\uC744 \uBA54\uC6B0\uACE0, \uD558\uCC9C\uC744 \uC0C8\uB85C \uB9CC\uB4E4\uAC70\uB098 \uC5C6\uC560\uBA74\uC11C \uC9C0\uD615\uC744 \uBCC0\uD654\uC2DC\uD0A8\uB2E4. \uCE68\uC2DD\uC73C\uB85C \uC778\uD574 \uB18D\uC9C0\uAC00 \uD669\uD3D0\uD654\uD558\uACE0 \uB18D\uC9C0\uC758 \uBE44\uB8CC\uB97C \uC53B\uC5B4\uB0B4\uC5B4 \uD638\uC218\uC640 \uAC15\uC744 \uC624\uC5FC\uC2DC\uD0A8\uB2E4. \uB610 \uCE68\uC2DD\uB41C \uD1A0\uC591\uC740 \uB3C4\uB791\u00B7\uBABB\u00B7\uC800\uC218\uC9C0 \uB4F1\uC744 \uB9C9\uC544 \uAD00\uAC1C\uB97C \uBC29\uD574\uD55C\uB2E4. \uCE68\uC2DD \uC791\uC6A9\uC740 \uBCF8\uB798 \uC790\uC5F0\uC2A4\uB7EC\uC6B4 \uACFC\uC815\uC774\uC9C0\uB9CC \uB9CE\uC740 \uACF3\uC5D0\uC11C \uC778\uAC04\uC758 \uC5D0 \uC758\uD574 \uC774\uB7EC\uD55C \uC791\uC6A9\uC774 \uC99D\uAC00\uB418\uAE30\uB3C4 \uD55C\uB2E4. , \uACFC\uB3C4\uD55C \uBC29\uBAA9, \uBB34\uBD84\uBCC4\uD55C \uAC74\uCD95 \uD65C\uB3D9\uC744 \uBE44\uB86F\uD55C \uC9C8 \uB0AE\uC740 \uD1A0\uC9C0 \uC774\uC6A9\uC774 \uD2B9\uD788 \uC774\uB7EC\uD558\uB2E4. \uB18D\uC791\uBB3C \uC0DD\uC0B0\uC5D0 \uC4F0\uC774\uB294 \uD1A0\uC9C0\uB294 \uC790\uC5F0 \uC18D \uCC44\uC18C\uB85C \uC774\uB8E8\uC5B4\uC9C4 \uB545\uBCF4\uB2E4 \uC77C\uBC18\uC801\uC73C\uB85C \uC5C4\uCCAD\uB09C \uC591\uC758 \uCE68\uC2DD \uC791\uC6A9\uC744 \uACAA\uAC8C \uB41C\uB2E4."@ko . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . "\u4FB5\u8680\u4F5C\u7528\uFF08\u82F1\u8A9E\uFF1Aerosion\uFF09\u6216\u6C34\u571F\u6D41\u5931\uFF08\u82F1\u8A9E\uFF1Asoil erosion\uFF09\u662F\u81EA\u7136\u754C\u7684\u4E00\u79CD\u73B0\u8C61\uFF0C\u662F\u6307\u5730\u7403\u7684\u8868\u9762\u4E0D\u65AD\u53D7\u5230\u98CE\u3001\u6C34\u7684\u78E8\u635F\u3002\u8FD9\u4E2A\u8FC7\u7A0B\uFF0C\u9646\u5730\u9664\u4E86\u88AB\u4FB5\u8680\u4E4B\u5916\uFF0C\u8680\u51FA\u7684\u7269\u8D28\u9084\u6703\u88AB\u5E26\u8D70\uFF0C\u5806\u79EF\u5728\u5176\u4ED6\u5730\u65B9\uFF0C\u4E3B\u8981\u5806\u79EF\u5728\u6D77\u88E1\u3002 \u4FB5\u8680\u7531\u6C34\u6D41\u3001\u51B0\u79FB\u6216\u98CE\u5439\u9020\u6210\u3002 \u800C\u7531\u96EA\u3001\u971C\u3001\u9633\u5149\u3001\u96E8\u6C34\u5BF9\u5730\u8868\u7684\u4F5C\u7528\u5247\u53EB\u505A\u98CE\u5316\u4F5C\u7528\uFF0C\u66B4\u9732\u5728\u7A7A\u6C14\u4E2D\u7684\u5CA9\u77F3\u4F1A\u53D7\u5230\u5929\u6C14\u5F71\u54CD\uFF0C\u957F\u671F\u51B7\u70ED\u4EA4\u66FF\uFF0C\u6709\u4E9B\u5CA9\u77F3\u4F1A\u56E0\u800C\u5F00\u88C2\u3002\u5CA9\u77F3\u4E2D\u7684\u6C34\u7ED3\u51B0\u65F6\u4F1A\u81A8\u80C0\uFF0C\u8FD9\u4E2A\u4E5F\u4F1A\u4F7F\u5CA9\u77F3\u5F00\u88C2\u3002\u77F3\u5934\u53D7\u5230\u91CD\u529B\u7684\u6324\u538B\u540E\u7A81\u7136\u51CF\u538B\uFF0C\u4E5F\u4F1A\u4F7F\u5CA9\u77F3\u788E\u88C2\u3002\u96E8\u6C34\u662F\u7A00\u9178\uFF0C\u53EF\u6EB6\u5316\u6216\u6539\u53D8\u5CA9\u77F3\u5185\u7684\u5316\u5B66\u7269\u8D28\u3002\u690D\u7269\u7684\u6839\u548C\u7A74\u5C45\u52A8\u7269\u4E5F\u4F1A\u52A0\u901F\u98CE\u5316\u3002 \u56E0\u4E3A\u98CE\u5316\u800C\u788E\u88C2\u7684\u77F3\u5757\u4F1A\u7531\u6C34\u3001\u51B0\u3001\u98CE\u5E26\u8D70\uFF0C\u800C\u5982\u679C\u6C34\u3001\u51B0\u3001\u98CE\u5185\u5982\u6709\u77F3\u5757\uFF0C\u5373\u4F7F\u975E\u5E38\u7EC6\u5C0F\uFF0C\u4E5F\u80FD\u5927\u5927\u52A0\u5F3A\u4FB5\u8680\u7684\u4F5C\u7528\uFF0C\u6539\u53D8\u5730\u8C8C\u3002 \u6210\u56E0\u6C34\u571F\u6D41\u5931\u53EF\u80FD\u662F\u7531\u4E8E\u81EA\u7136\u73AF\u5883\u5F15\u8D77\u7684\uFF0C\u8B6C\u5982\u5730\u52BF\u9661\u5CED\uFF0C\u7A81\u53D1\u5927\u91CF\u964D\u6C34\uFF0C\u6216\u8005\u5730\u8D28\u53D8\u5316\u3002\u4F46\u66F4\u591A\u7684\u662F\u7531\u4E8E\u4EBA\u7C7B\u6D3B\u52A8\u5BFC\u81F4\u7684\uFF0C\u8B6C\u5982\u8FC7\u5EA6\u653E\u7267\uFF0C\u5F00\u57A6\u571F\u5730\uFF0C\u91C7\u4F10\u68EE\u6797\uFF0C\u9032\u884C\u5404\u9805\u5DE5\u7A0B\u5EFA\u8A2D\u7B49\u7B49\u3002 \u5BB3\u8655\u4FB5\u8680\u662F\u81EA\u7136\u73AF\u5883\u6076\u5316\u7684\u91CD\u8981\u539F\u56E0\u3002\u7531\u4E8E\u6C34\u7684\u6D41\u52A8\uFF0C\u5E26\u8D70\u4E86\u5730\u7403\u8868\u9762\u7684\u571F\u58E4\uFF0C\u4F7F\u5F97\u571F\u5730\u53D8\u5F97\u8D2B\u7620\uFF0C\u5CA9\u77F3\u88F8\u9732\uFF0C\u690D\u88AB\u7834\u574F\uFF0C\u751F\u6001\u6076\u5316\u3002 \u8FD9\u79CD\u81EA\u7136\u73B0\u8C61\u53EF\u4EE5\u662F\u5FAA\u73AF\u4F5C\u7528\u7684\uFF0C\u751F\u6001\u6076\u5316\u5F15\u8D77\u6C34\u571F\u6D41\u5931\uFF0C\u6C34\u571F\u6D41\u5931\u53C8\u4F7F\u5F97\u751F\u6001\u66F4\u52A0\u6076\u5316\u3002\u4E8E\u662F\u571F\u5730\u9000\u5316\uFF0C\u65E0\u6CD5\u8015\u79CD\u3002\u690D\u7269\u6B7B\u4EA1\uFF0C\u5730\u8868\u88F8\u9732\u3002\u6076\u52A3\u7684\u751F\u6001\u53C8\u66F4\u5BFC\u81F4\u6C14\u5019\u7684\u53D8\u5316\uFF0C\u4F7F\u5F97\u751F\u7269\u53EF\u751F\u5B58\u7684\u73AF\u5883\u53D8\u574F\u3002 \u98CE\u5316\u4E0E\u4FB5\u8680\u7684\u533A\u522B\u3002\u98CE\u5316\u662F\u7834\u574F\u540E\u6539\u53D8\u7269\u4F53\u5F62\u72B6\uFF0C\u800C\u4FB5\u8680\u662F\u8F6C\u79FB\u7269\u4F53\uFF0C\u4ECE\u800C\u6539\u53D8\u5730\u8C8C\u3002"@zh . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . "y"@en . . . . . . . . . . . . . . . . . . . . . . . . "Cna\u00ED"@ga . . "Erosie is het proces van slijtage van een vast oppervlak waarbij materiaal wordt verplaatst of geheel verdwijnt. Op Aarde gebeurt erosie vooral door de werking van wind, stromend water, ijs, maar ook ongewonere vormen van erosie zijn mogelijk als gevolg van vulkanisme en inslagen. Erosie is een fenomeen met een natuurlijke oorzaak. Menselijke activiteiten kunnen het erosieproces versterken, bijvoorbeeld door het kappen van bossen en het kaal houden van de bodem door ploegen."@nl . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . "Erosi (dari bahasa Latin erosionem \"menggerogoti\") atau disebut juga pengikisan adalah suatu peristiwa yang terjadi secara alami oleh pengikisan padatan (sedimen, tanah, batuan, dan partikel lainnya) akibat transportasi oleh angin, tanah dan material lain di bawah pengaruh gravitasi atau oleh makhluk hidup semisal hewan yang membuat liang atau pertumbuhan akar tanaman yang mengakibatkan retakan tanah dalam hal ini disebut . Erosi tidak sama dengan pelapukan akibat cuaca, yang mana merupakan proses penghancuran mineral batuan dengan proses kimiawi maupun fisik, atau gabungan keduanya. Secara umum erosi melibatkan tiga proses yaitu pelepasan (detachment), transformasi (transformation), dan pengendapan (sedimentation). Erosi yang terjadi dapat membentuk banyak penampakan alam menarik seperti puncak gunung, lembah dan garis pantai. Erosi sebenarnya merupakan proses alami yang mudah dikenali, namun di kebanyakan tempat kejadian ini diperparah oleh aktivitas manusia dalam tata guna lahan yang buruk, penggundulan hutan, kegiatan pertambangan, perkebunan dan , kegiatan konstruksi atau pembangunan yang tidak tertata dengan baik dan pembangunan jalan. Tanah yang digunakan untuk menghasilkan tanaman pertanian biasanya mengalami erosi yang jauh lebih besar dari tanah dengan vegetasi alaminya. Alih fungsi hutan menjadi ladang pertanian meningkatkan erosi, karena struktur akar tanaman hutan yang kuat mengikat tanah digantikan dengan struktur akar tanaman pertanian yang lebih lemah."@in . . . . . . . . . . . . . . . "Erosion"@en . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . "Erosion"@sv . . . . . . . . . . . . . . . "Erozja \u2013 proces niszczenia powierzchni terenu przez wod\u0119, wiatr, s\u0142o\u0144ce, si\u0142\u0119 grawitacji i dzia\u0142alno\u015B\u0107 organizm\u00F3w."@pl . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . "\u062A\u0639\u0631\u064A\u0629"@ar . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . "Erosi\u00F3n"@es . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . "\u0627\u0644\u062A\u0639\u0631\u064A\u0629 \u0623\u0648 \u0627\u0644\u062D\u062A\u0651\u060C \u0641\u064A \u0639\u0644\u0645 \u0627\u0644\u0623\u0631\u0636\u060C \u0647\u064A \u0639\u0645\u0644\u064A\u0629 \u0645\u0646 \u0627\u0644\u0639\u0645\u0644\u064A\u0627\u062A \u0627\u0644\u062A\u064A \u062A\u062D\u062F\u062B \u0639\u0644\u0649 \u0633\u0637\u062D \u0627\u0644\u0643\u0631\u0629 \u0627\u0644\u0623\u0631\u0636\u064A\u0629 (\u0645\u062B\u0644 \u062A\u062F\u0641\u0642 \u0627\u0644\u0645\u064A\u0627\u0647 \u0623\u0648 \u0627\u0644\u0631\u064A\u0627\u062D)\u060C \u0648\u0627\u0644\u062A\u064A \u062A\u0632\u064A\u0644 \u0627\u0644\u062A\u0631\u0628\u0629 \u0623\u0648 \u0627\u0644\u0635\u062E\u0648\u0631 \u0623\u0648 \u0627\u0644\u0645\u0648\u0627\u062F \u0627\u0644\u0630\u0627\u0626\u0628\u0629 \u0645\u0646 \u0645\u0648\u0642\u0639 \u0639\u0644\u0649 \u0627\u0644\u0642\u0634\u0631\u0629 \u0627\u0644\u0623\u0631\u0636\u064A\u0629 \u0648\u062A\u0646\u0642\u0644\u0647\u0627 \u0625\u0644\u0649 \u0645\u0648\u0642\u0639 \u0622\u062E\u0631 (\u0644\u0627 \u064A\u062C\u0628 \u0627\u0644\u062E\u0644\u0637 \u0628\u064A\u0646\u0647\u0627 \u0648\u0628\u064A\u0646 \u0627\u0644\u062A\u062C\u0648\u064A\u0629 \u0627\u0644\u062A\u064A \u0644\u0627 \u062A\u0634\u0645\u0644 \u062D\u0631\u0643\u0629). \u062A\u0646\u062A\u062C \u0647\u0630\u0647 \u0627\u0644\u0639\u0645\u0644\u064A\u0629 \u0627\u0644\u0637\u0628\u064A\u0639\u064A\u0629 \u0639\u0646 \u0627\u0644\u0646\u0634\u0627\u0637 \u0627\u0644\u062F\u064A\u0646\u0627\u0645\u064A\u0643\u064A \u0644\u0644\u0639\u0648\u0627\u0645\u0644 \u0627\u0644\u0645\u0633\u0628\u0628\u0629 \u0644\u0644\u062A\u0639\u0631\u064A\u0629\u060C \u0623\u064A \u0627\u0644\u0645\u0627\u0621 \u0648\u0627\u0644\u062C\u0644\u064A\u062F (\u0627\u0644\u0623\u0646\u0647\u0627\u0631 \u0627\u0644\u062C\u0644\u064A\u062F\u064A\u0629) \u0648\u0627\u0644\u062B\u0644\u0648\u062C \u0648\u0627\u0644\u0647\u0648\u0627\u0621 (\u0627\u0644\u0631\u064A\u0627\u062D) \u0648\u0627\u0644\u0646\u0628\u0627\u062A\u0627\u062A \u0648\u0627\u0644\u062D\u064A\u0648\u0627\u0646\u0627\u062A \u0648\u0627\u0644\u0628\u0634\u0631. \u062A\u0646\u0642\u0633\u0645 \u0627\u0644\u062A\u0639\u0631\u064A\u0629 \u0648\u0641\u0642\u064B\u0627 \u0644\u0647\u0630\u0647 \u0627\u0644\u0639\u0648\u0627\u0645\u0644 \u0623\u062D\u064A\u0627\u0646\u064B\u0627 \u0625\u0644\u0649 \u0627\u0644\u062A\u0639\u0631\u064A\u0629 \u0627\u0644\u0645\u0627\u0626\u064A\u0629\u060C \u0648\u0627\u0644\u062C\u0644\u064A\u062F\u064A\u0629\u060C \u0648\u0627\u0644\u062B\u0644\u062C\u064A\u0629\u060C \u0648\u0627\u0644\u0647\u0648\u0627\u0626\u064A\u0629\u060C \u0648\u0627\u0644\u062D\u064A\u0648\u0627\u0646\u064A\u0629\u060C \u0648\u0627\u0644\u0645\u0631\u062A\u0628\u0637\u0629 \u0628\u0627\u0644\u0646\u0634\u0627\u0637 \u0627\u0644\u0628\u0634\u0631\u064A. \u064A\u0634\u0627\u0631 \u0625\u0644\u0649 \u0627\u0646\u0647\u064A\u0627\u0631 \u0627\u0644\u062C\u0633\u064A\u0645\u0627\u062A \u0645\u0646 \u0627\u0644\u0635\u062E\u0648\u0631 \u0623\u0648 \u0627\u0644\u062A\u0631\u0628\u0629 \u0625\u0644\u0649 \u0631\u0648\u0627\u0633\u0628 \u0641\u062A\u0627\u062A\u064A\u0629 \u0628\u0627\u0644\u062A\u0639\u0631\u064A\u0629 \u0627\u0644\u0645\u0627\u062F\u064A\u0629 \u0623\u0648 \u0627\u0644\u0645\u064A\u0643\u0627\u0646\u064A\u0643\u064A\u0629. \u064A\u062A\u0646\u0627\u0642\u0636 \u0647\u0630\u0627 \u0645\u0639 \u0627\u0644\u062A\u0639\u0631\u064A\u0629 \u0627\u0644\u0643\u064A\u0645\u064A\u0627\u0626\u064A\u0629 \u062D\u064A\u062B \u062A\u064F\u0632\u0627\u0644 \u0627\u0644\u062A\u0631\u0628\u0629 \u0623\u0648 \u0627\u0644\u0645\u0648\u0627\u062F \u0627\u0644\u0635\u062E\u0631\u064A\u0629 \u0645\u0646 \u0645\u0646\u0637\u0642\u0629 \u0645\u0627 \u0639\u0646 \u0637\u0631\u064A\u0642 \u0625\u0630\u0627\u0628\u062A\u0647\u0627 \u0641\u064A \u0645\u064F\u0630\u064A\u0628 (\u0639\u0627\u062F\u0629\u064B \u0645\u0627\u0621)\u060C \u0648\u0645\u0646 \u062B\u0645 \u062A\u062F\u0641\u0642 \u0647\u0630\u0627 \u0627\u0644\u0645\u062D\u0644\u0648\u0644 \u0628\u0639\u064A\u062F\u064B\u0627. \u064A\u0645\u0643\u0646 \u0646\u0642\u0644 \u0627\u0644\u0631\u0648\u0627\u0633\u0628 \u0627\u0644\u0645\u062A\u0622\u0643\u0644\u0629 \u0623\u0648 \u0627\u0644\u0630\u0627\u0626\u0628\u0629 \u0644\u0645\u0633\u0627\u0641\u0629 \u0628\u0636\u0639\u0629 \u0645\u0644\u0644\u064A\u0645\u062A\u0631\u0627\u062A \u0641\u0642\u0637 \u0623\u0648 \u0644\u0622\u0644\u0627\u0641 \u0627\u0644\u0643\u064A\u0644\u0648\u0645\u062A\u0631\u0627\u062A."@ar . . . . . . . "Erosi\u00F3"@ca . . . . . "\u0415\u0440\u043E\u0301\u0437\u0456\u044F (\u0432\u0456\u0434 \u043B\u0430\u0442. erosio) \u2014 \u043F\u0440\u043E\u0446\u0435\u0441 \u0440\u0443\u0439\u043D\u0443\u0432\u0430\u043D\u043D\u044F \u0491\u0440\u0443\u043D\u0442\u0443 \u0430\u0431\u043E \u0433\u0456\u0440\u0441\u044C\u043A\u0438\u0445 \u043F\u043E\u0440\u0456\u0434 \u0432\u043E\u0434\u043D\u0438\u043C \u043F\u043E\u0442\u043E\u043A\u043E\u043C (\u0432\u043E\u0434\u043D\u0430 \u0435\u0440\u043E\u0437\u0456\u044F), \u0432\u0456\u0442\u0440\u043E\u043C (\u0432\u0456\u0442\u0440\u043E\u0432\u0430 \u0435\u0440\u043E\u0437\u0456\u044F, \u0430\u0431\u043E \u0434\u0435\u0444\u043B\u044F\u0446\u0456\u044F), \u043B\u044C\u043E\u0434\u043E\u043C. \u0415\u0440\u043E\u0437\u0456\u044F \u2014 \u043E\u0434\u0438\u043D \u0437 \u0433\u043E\u043B\u043E\u0432\u043D\u0438\u0445 \u0437\u043E\u0432\u043D\u0456\u0448\u043D\u0456\u0445 (\u0435\u043A\u0437\u043E\u0433\u0435\u043D\u043D\u0438\u0445) \u0447\u0438\u043D\u043D\u0438\u043A\u0456\u0432 \u0444\u043E\u0440\u043C\u0443\u0432\u0430\u043D\u043D\u044F \u0440\u0435\u043B\u044C\u0454\u0444\u0443 \u0437\u0435\u043C\u043D\u043E\u0457 \u043F\u043E\u0432\u0435\u0440\u0445\u043D\u0456. \u0427\u0430\u0441\u0442\u0438\u043D\u0430 \u043F\u0440\u043E\u0446\u0435\u0441\u0443 \u0434\u0435\u043D\u0443\u0434\u0430\u0446\u0456\u0457. \u0420\u043E\u0437\u0440\u0456\u0437\u043D\u044F\u044E\u0442\u044C \u0441\u0445\u0438\u043B\u043E\u0432\u0443 \u0439 \u0440\u0443\u0441\u043B\u043E\u0432\u0443 \u0432\u043E\u0434\u043D\u0443 \u0435\u0440\u043E\u0437\u0456\u044E. \u0423 \u0440\u0435\u0437\u0443\u043B\u044C\u0442\u0430\u0442\u0456 \u0432\u043E\u0434\u043D\u043E\u0457 \u0435\u0440\u043E\u0437\u0456\u0457 \u0443\u0442\u0432\u043E\u0440\u044E\u044E\u0442\u044C\u0441\u044F \u044F\u0440\u0438, \u0431\u0430\u043B\u043A\u0438, \u0440\u0456\u0447\u043A\u043E\u0432\u0456 \u0434\u043E\u043B\u0438\u043D\u0438 \u0442\u043E\u0449\u043E. \u041A\u0440\u0456\u043C \u0417\u0435\u043C\u043B\u0456, \u044F\u0432\u0438\u0449\u0430 \u0435\u0440\u043E\u0437\u0456\u0457 \u0441\u043F\u043E\u0441\u0442\u0435\u0440\u0456\u0433\u0430\u044E\u0442\u044C\u0441\u044F \u0439 \u043D\u0430 \u0456\u043D\u0448\u0438\u0445 \u043F\u043B\u0430\u043D\u0435\u0442\u0430\u0445 \u0421\u043E\u043D\u044F\u0447\u043D\u043E\u0457 \u0441\u0438\u0441\u0442\u0435\u043C\u0438, \u0437\u043E\u043A\u0440\u0435\u043C\u0430 \u043D\u0430 \u041C\u0430\u0440\u0441\u0456."@uk . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . "Higadura lurrazaleko gaien karraskatze eta suntsitzea da (lurra, lokatza, arroka eta beste) agente geologikoen eraginpean. Etengabeko marruskatze-lana ibaiek, euri urek, haizeak, izotzak edo itsasoak eragiten dute, grabitazioa edo izaki biziek direla-eta. Higaduraren ondorioz askatutako harri puskak ez dira toki berean gelditzen, agente berak egiten duen mugimenduari esker lekualdatzen dira, hau da, garraiatu. Garraioa burutzen duten agenteak honako hauek dira: grabitatea, ibaiak, errekak eta uharrek daramaten ura, glaziarretako izotza, itsasoko ura eta haizea. Azkenik harri zati horiek malda edo agentearen abiadura txikitzen delako leku egonkorrago batera iristen direnean, bertan metatzen dira. Prozesu horri sedimentazioa edo jalkitzea deritzo. Higatutako mineralak, gehienetan uretan disolbaturik, gerora garraiatzea eragile indartsuenetako bat da lurrak sortzeko orduan, eta harri sedimentarioak eratzeko lehen urratsa izango genuke. Beraz, eragile geologiko motel baino indartsu hau erliebearen modelatzaile nagusienetako bat dugu."@eu . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . "\u0415\u0440\u043E\u0301\u0437\u0456\u044F (\u0432\u0456\u0434 \u043B\u0430\u0442. erosio) \u2014 \u043F\u0440\u043E\u0446\u0435\u0441 \u0440\u0443\u0439\u043D\u0443\u0432\u0430\u043D\u043D\u044F \u0491\u0440\u0443\u043D\u0442\u0443 \u0430\u0431\u043E \u0433\u0456\u0440\u0441\u044C\u043A\u0438\u0445 \u043F\u043E\u0440\u0456\u0434 \u0432\u043E\u0434\u043D\u0438\u043C \u043F\u043E\u0442\u043E\u043A\u043E\u043C (\u0432\u043E\u0434\u043D\u0430 \u0435\u0440\u043E\u0437\u0456\u044F), \u0432\u0456\u0442\u0440\u043E\u043C (\u0432\u0456\u0442\u0440\u043E\u0432\u0430 \u0435\u0440\u043E\u0437\u0456\u044F, \u0430\u0431\u043E \u0434\u0435\u0444\u043B\u044F\u0446\u0456\u044F), \u043B\u044C\u043E\u0434\u043E\u043C. \u0415\u0440\u043E\u0437\u0456\u044F \u2014 \u043E\u0434\u0438\u043D \u0437 \u0433\u043E\u043B\u043E\u0432\u043D\u0438\u0445 \u0437\u043E\u0432\u043D\u0456\u0448\u043D\u0456\u0445 (\u0435\u043A\u0437\u043E\u0433\u0435\u043D\u043D\u0438\u0445) \u0447\u0438\u043D\u043D\u0438\u043A\u0456\u0432 \u0444\u043E\u0440\u043C\u0443\u0432\u0430\u043D\u043D\u044F \u0440\u0435\u043B\u044C\u0454\u0444\u0443 \u0437\u0435\u043C\u043D\u043E\u0457 \u043F\u043E\u0432\u0435\u0440\u0445\u043D\u0456. \u0427\u0430\u0441\u0442\u0438\u043D\u0430 \u043F\u0440\u043E\u0446\u0435\u0441\u0443 \u0434\u0435\u043D\u0443\u0434\u0430\u0446\u0456\u0457. \u0420\u043E\u0437\u0440\u0456\u0437\u043D\u044F\u044E\u0442\u044C \u0441\u0445\u0438\u043B\u043E\u0432\u0443 \u0439 \u0440\u0443\u0441\u043B\u043E\u0432\u0443 \u0432\u043E\u0434\u043D\u0443 \u0435\u0440\u043E\u0437\u0456\u044E. \u0423 \u0440\u0435\u0437\u0443\u043B\u044C\u0442\u0430\u0442\u0456 \u0432\u043E\u0434\u043D\u043E\u0457 \u0435\u0440\u043E\u0437\u0456\u0457 \u0443\u0442\u0432\u043E\u0440\u044E\u044E\u0442\u044C\u0441\u044F \u044F\u0440\u0438, \u0431\u0430\u043B\u043A\u0438, \u0440\u0456\u0447\u043A\u043E\u0432\u0456 \u0434\u043E\u043B\u0438\u043D\u0438 \u0442\u043E\u0449\u043E. \u041A\u0440\u0456\u043C \u0417\u0435\u043C\u043B\u0456, \u044F\u0432\u0438\u0449\u0430 \u0435\u0440\u043E\u0437\u0456\u0457 \u0441\u043F\u043E\u0441\u0442\u0435\u0440\u0456\u0433\u0430\u044E\u0442\u044C\u0441\u044F \u0439 \u043D\u0430 \u0456\u043D\u0448\u0438\u0445 \u043F\u043B\u0430\u043D\u0435\u0442\u0430\u0445 \u0421\u043E\u043D\u044F\u0447\u043D\u043E\u0457 \u0441\u0438\u0441\u0442\u0435\u043C\u0438, \u0437\u043E\u043A\u0440\u0435\u043C\u0430 \u043D\u0430 \u041C\u0430\u0440\u0441\u0456."@uk . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . "\u0391\u03C0\u03BF\u03C3\u03AC\u03B8\u03C1\u03C9\u03C3\u03B7"@el . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . "Erozio la\u016D la lingva\u0135o de fizika geografio estas la forporto de solida materio (ekzemple tero a\u016D roka\u0135o) fare de vento, akvo kaj gravito. Erozio povas esti komplete natura procezo, sed multloke pliigas \u011Din homaj aktivecoj kiel ekzemple senarbarigo kaj tropa\u015Dti\u011Do. Aliflanke homoj klopodas malhelpi al la erozio konstruante terasojn, firmigante deklivojn kaj dunojn ekzemple per kaj plantante arbojn, arbustojn a\u016D herbojn. En iuj cirkonstancoj, la uzo de dispecigita frondara ligno povas kontribui al regenerado de eroziitaj terenoj."@eo . . . . . . . . . . . . . . . . . . . . . . . . . . . . "62250"^^ . . . . . . . . . . . . . . . . . . . . . . . . . . . . . "En g\u00E9omorphologie, l\u2019\u00E9rosion est le processus de d\u00E9gradation et de transformation du relief, et donc des sols, roches, berges et littoraux qui est caus\u00E9 par tout agent externe (donc autre que la tectonique). Un relief dont le model\u00E9 s'explique principalement par l'\u00E9rosion est dit \u00AB \u00BB. Les facteurs d'\u00E9rosion sont : L'\u00E9rosion agit \u00E0 diff\u00E9rents rythmes et peut, sur plusieurs dizaines de millions d'ann\u00E9es, araser des montagnes, creuser des vall\u00E9es, faire reculer des falaises."@fr . . . . . . . . . . . . . . . . . . . . . . . . . . . "Erosie"@nl . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . "L'erosione \u00E8 una fase del processo sedimentario e consiste nella separazione fisica, da suoli e rocce affioranti, e successivo allontanamento di frammenti, chiamati \"clasti\", e di soluti generati dalla fase di degradazione meteorica. Il termine viene applicato non solo al processo fisico-chimico in s\u00E9, ma anche agli effetti che l'erosione produce sul territorio. L'erosione tende a portare la superficie terrestre verso un profilo di equilibrio, raggiunto il quale le forze che la determinano sono insufficienti a farla proseguire o questa rallenta in modo significativo la sua azione. Si usa distinguere l'erosione in \"senso stretto\", un processo che muove piccole quantit\u00E0 di materia in modo costante nel tempo, dai movimenti di massa, come frane e smottamenti, che invece movimentano grandi quantit\u00E0 di materiale in pochissimo tempo, ma sono discontinui."@it . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . "\u042D\u0440\u043E\u0437\u0438\u044F"@ru . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . "Erosion (Geologie)"@de . . . . . . . . . "\u4FB5\u98DF"@ja . . . . . . . . . . . . . . . . . "Die Erosion (von lateinisch erodere \u201Aabnagen\u2018) ist ein grundlegender Prozess im exogenen Teil des Gesteinskreislaufes. Er beinhaltet die Abtragung von mehr oder weniger stark verwitterten Gesteinen (Regolith) oder Lockersedimenten einschlie\u00DFlich der B\u00F6den (siehe Bodenerosion). So erschafft die Erosion einerseits Gel\u00E4ndeformen wie Berg und Tal, zerst\u00F6rt selbige jedoch schlie\u00DFlich bei anhaltendem Wirken vollst\u00E4ndig, insofern ihr keine endogenen Prozesse (insbesondere Tektonik), die eine Anhebung der Landoberfl\u00E4che hervorrufen, entgegenwirken. Erosion ist das Gegenst\u00FCck zur Sedimentation. Der Prozess, der zwischen Erosion und Sedimentation vermittelt, hei\u00DFt Transport (siehe Hjulstr\u00F6m-Diagramm)."@de . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . "La erosi\u00F3n es el desgaste o denudaci\u00F3n de suelos y rocas que producen distintos procesos en la superficie de la Tierra.\u200B La erosi\u00F3n implica movimiento, transporte del material, en contraste con la alteraci\u00F3n y disgregaci\u00F3n de las rocas, fen\u00F3meno conocido como meteorizaci\u00F3n y es uno de los principales factores del ciclo geogr\u00E1fico. Entre los agentes erosivos est\u00E1n la circulaci\u00F3n de agua o hielo, el viento, o los cambios t\u00E9rmicos.\u200B\u200B La erosi\u00F3n produce el relieve de los valles, gargantas, ca\u00F1ones, cavernas y mesas, y puede ser incrementada por actividades humanas."@es . . . . . . . . . . "\u042D\u0440\u043E\u0301\u0437\u0438\u044F (\u043E\u0442 \u043B\u0430\u0442. erosio \u00AB\u0440\u0430\u0437\u044A\u0435\u0434\u0430\u043D\u0438\u0435\u00BB) \u2014 \u0440\u0430\u0437\u0440\u0443\u0448\u0435\u043D\u0438\u0435 \u0433\u043E\u0440\u043D\u044B\u0445 \u043F\u043E\u0440\u043E\u0434 \u0438 \u043F\u043E\u0447\u0432 \u043F\u043E\u0432\u0435\u0440\u0445\u043D\u043E\u0441\u0442\u043D\u044B\u043C\u0438 \u0432\u043E\u0434\u043D\u044B\u043C\u0438 \u043F\u043E\u0442\u043E\u043A\u0430\u043C\u0438, \u0432\u043A\u043B\u044E\u0447\u0430\u044E\u0449\u0435\u0435 \u0432 \u0441\u0435\u0431\u044F \u043E\u0442\u0440\u044B\u0432 \u0438 \u0432\u044B\u043D\u043E\u0441 \u043E\u0431\u043B\u043E\u043C\u043A\u043E\u0432 \u043C\u0430\u0442\u0435\u0440\u0438\u0430\u043B\u0430 \u0438 \u0441\u043E\u043F\u0440\u043E\u0432\u043E\u0436\u0434\u0430\u044E\u0449\u0435\u0435\u0441\u044F \u0438\u0445 \u043E\u0442\u043B\u043E\u0436\u0435\u043D\u0438\u0435\u043C. \u042D\u0440\u043E\u0437\u0438\u044F \u044F\u0432\u043B\u044F\u0435\u0442\u0441\u044F \u043F\u0440\u0438\u0447\u0438\u043D\u043E\u0439 \u043E\u0431\u0440\u0430\u0437\u043E\u0432\u0430\u043D\u0438\u044F \u043F\u0440\u043E\u043C\u043E\u0438\u043D, \u043E\u0432\u0440\u0430\u0433\u043E\u0432, \u0440\u0435\u0447\u043D\u044B\u0445 \u0434\u043E\u043B\u0438\u043D. \u042D\u0440\u043E\u0437\u0438\u044F \u043F\u043E\u0447\u0432\u044B \u2014 \u0440\u0430\u0437\u0440\u0443\u0448\u0435\u043D\u0438\u0435 (\u0440\u0430\u0437\u044A\u0435\u0434\u0430\u043D\u0438\u0435) \u043F\u043E\u0447\u0432\u044B. \u041F\u043E \u043F\u0440\u0438\u0447\u0438\u043D\u0430\u043C \u0432\u044B\u0434\u0435\u043B\u044F\u044E\u0442 \u0435\u0441\u0442\u0435\u0441\u0442\u0432\u0435\u043D\u043D\u0443\u044E \u0438 \u0430\u043D\u0442\u0440\u043E\u043F\u043E\u0433\u0435\u043D\u043D\u0443\u044E \u044D\u0440\u043E\u0437\u0438\u044E. \u0410\u043D\u0442\u0440\u043E\u043F\u043E\u0433\u0435\u043D\u043D\u0430\u044F \u044D\u0440\u043E\u0437\u0438\u044F \u043D\u0435 \u0432\u0441\u0435\u0433\u0434\u0430 \u044F\u0432\u043B\u044F\u0435\u0442\u0441\u044F \u0443\u0441\u043A\u043E\u0440\u0435\u043D\u043D\u043E\u0439 \u0438 \u043D\u0430\u043E\u0431\u043E\u0440\u043E\u0442. \u041F\u0440\u043E\u0446\u0435\u0441\u0441\u044B \u044D\u0440\u043E\u0437\u0438\u0438 \u0440\u0430\u0441\u043F\u0440\u043E\u0441\u0442\u0440\u0430\u043D\u0435\u043D\u044B \u043D\u0430 \u0417\u0435\u043C\u043B\u0435 \u043F\u043E\u0432\u0441\u0435\u043C\u0435\u0441\u0442\u043D\u043E \u0432 \u0443\u0441\u043B\u043E\u0432\u0438\u044F\u0445 \u0433\u0443\u043C\u0438\u0434\u043D\u043E\u0433\u043E \u043A\u043B\u0438\u043C\u0430\u0442\u0430."@ru . . . . . . "La erosi\u00F3n es el desgaste o denudaci\u00F3n de suelos y rocas que producen distintos procesos en la superficie de la Tierra.\u200B La erosi\u00F3n implica movimiento, transporte del material, en contraste con la alteraci\u00F3n y disgregaci\u00F3n de las rocas, fen\u00F3meno conocido como meteorizaci\u00F3n y es uno de los principales factores del ciclo geogr\u00E1fico. Entre los agentes erosivos est\u00E1n la circulaci\u00F3n de agua o hielo, el viento, o los cambios t\u00E9rmicos.\u200B\u200B La erosi\u00F3n produce el relieve de los valles, gargantas, ca\u00F1ones, cavernas y mesas, y puede ser incrementada por actividades humanas."@es . . . . . "Eroze (z latinsk\u00E9ho erosio; erodere = vyhlodat) je p\u0159irozen\u00FD proces rozru\u0161ov\u00E1n\u00ED a transportu objekt\u016F na zemsk\u00E9m povrchu (p\u016Fda, horniny, sk\u00E1ly atd.). P\u0159\u00ED\u010Dinou eroze je mechanick\u00E9 p\u016Fsoben\u00ED pohybuj\u00EDc\u00EDch se okoln\u00EDch l\u00E1tek \u2013 p\u0159edev\u0161\u00EDm v\u011Btru, proud\u00EDc\u00ED nebo vln\u00EDc\u00ED se vody, ledu, sn\u011Bhu, pohybliv\u00FDch zv\u011Btralin a nezpevn\u011Bn\u00FDch usazenin. Eroze byla v\u017Edy existuj\u00EDc\u00EDm p\u0159\u00EDrodn\u00EDm procesem. Ur\u010Dit\u00FD stupe\u0148 eroze jako p\u0159\u00EDrodn\u00EDho jevu m\u016F\u017Ee b\u00FDt prosp\u011B\u0161n\u00FD ekosyst\u00E9m\u016Fm, ov\u0161em zejm\u00E9na od 20. stolet\u00ED se \u010Dinnost\u00ED \u010Dlov\u011Bka zvy\u0161uje eroze p\u016Fd, co\u017E se projevuje rostouc\u00EDm odnosem p\u016Fdy. Eroze nen\u00ED chemick\u00E9 rozpou\u0161t\u011Bn\u00ED hornin (koroze). V\u011Bda o erozi a protierozn\u00ED ochran\u011B se naz\u00FDv\u00E1 ."@cs . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . "Eroze (z latinsk\u00E9ho erosio; erodere = vyhlodat) je p\u0159irozen\u00FD proces rozru\u0161ov\u00E1n\u00ED a transportu objekt\u016F na zemsk\u00E9m povrchu (p\u016Fda, horniny, sk\u00E1ly atd.). P\u0159\u00ED\u010Dinou eroze je mechanick\u00E9 p\u016Fsoben\u00ED pohybuj\u00EDc\u00EDch se okoln\u00EDch l\u00E1tek \u2013 p\u0159edev\u0161\u00EDm v\u011Btru, proud\u00EDc\u00ED nebo vln\u00EDc\u00ED se vody, ledu, sn\u011Bhu, pohybliv\u00FDch zv\u011Btralin a nezpevn\u011Bn\u00FDch usazenin. Eroze byla v\u017Edy existuj\u00EDc\u00EDm p\u0159\u00EDrodn\u00EDm procesem. Ur\u010Dit\u00FD stupe\u0148 eroze jako p\u0159\u00EDrodn\u00EDho jevu m\u016F\u017Ee b\u00FDt prosp\u011B\u0161n\u00FD ekosyst\u00E9m\u016Fm, ov\u0161em zejm\u00E9na od 20. stolet\u00ED se \u010Dinnost\u00ED \u010Dlov\u011Bka zvy\u0161uje eroze p\u016Fd, co\u017E se projevuje rostouc\u00EDm odnosem p\u016Fdy."@cs . . . . . "1122864498"^^ . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . "9696"^^ . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . "\u039C\u03B5 \u03C4\u03BF\u03BD \u03CC\u03C1\u03BF \u03B1\u03C0\u03BF\u03C3\u03AC\u03B8\u03C1\u03C9\u03C3\u03B7 \u03B5\u03BD\u03BD\u03BF\u03BF\u03CD\u03BC\u03B5 \u03C4\u03B7\u03BD \u03C0\u03C1\u03BF\u03BF\u03B4\u03B5\u03C5\u03C4\u03B9\u03BA\u03AE \u03BA\u03B1\u03B9 \u03C3\u03C4\u03B1\u03B4\u03B9\u03B1\u03BA\u03AE \u03B1\u03C0\u03BF\u03C3\u03CD\u03BD\u03B8\u03B5\u03C3\u03B7 \u03C4\u03C9\u03BD \u03C5\u03BB\u03B9\u03BA\u03CE\u03BD \u03C4\u03C9\u03BD \u03B5\u03B4\u03B1\u03C6\u03CE\u03BD, \u03C4\u03C9\u03BD \u03C0\u03B5\u03C4\u03C1\u03C9\u03BC\u03AC\u03C4\u03C9\u03BD, \u03C4\u03B7\u03C2 \u03B1\u03BB\u03BB\u03AC \u03BA\u03B1\u03B9 \u03C4\u03B5\u03C7\u03BD\u03B7\u03C4\u03CE\u03BD \u03C5\u03BB\u03B9\u03BA\u03CE\u03BD \u03BC\u03B5 \u03C4\u03B7\u03BD \u03C0\u03AC\u03C1\u03BF\u03B4\u03BF \u03C4\u03BF\u03C5 \u03C7\u03C1\u03CC\u03BD\u03BF\u03C5 \u03C5\u03C0\u03CC \u03C4\u03B7\u03BD \u03B5\u03C0\u03AF\u03B4\u03C1\u03B1\u03C3\u03B7 \u03C0\u03B1\u03C1\u03B1\u03B3\u03CC\u03BD\u03C4\u03C9\u03BD \u03C4\u03BF\u03C5 \u03C0\u03B5\u03C1\u03B9\u03B2\u03AC\u03BB\u03BB\u03BF\u03BD\u03C4\u03BF\u03C2, \u03CC\u03C0\u03C9\u03C2 \u03C4\u03BF\u03C5 \u03B1\u03BD\u03AD\u03BC\u03BF\u03C5, \u03C4\u03BF\u03C5 \u03BD\u03B5\u03C1\u03BF\u03CD, \u03C4\u03BF\u03C5 \u03C0\u03AC\u03B3\u03BF\u03C5 \u03AE \u03B1\u03BA\u03CC\u03BC\u03B7 \u03BA\u03B1\u03B9 \u03C4\u03C9\u03BD \u03B6\u03C9\u03BD\u03C4\u03B1\u03BD\u03CE\u03BD \u03BF\u03C1\u03B3\u03B1\u03BD\u03B9\u03C3\u03BC\u03CE\u03BD, \u03B1\u03BB\u03BB\u03AC \u03BA\u03B1\u03B9 \u03C4\u03B7 \u03B4\u03B9\u03AC\u03B2\u03C1\u03C9\u03C3\u03B7."@el . . . . . . . . . . . . . . . . . . . . "Erosi (dari bahasa Latin erosionem \"menggerogoti\") atau disebut juga pengikisan adalah suatu peristiwa yang terjadi secara alami oleh pengikisan padatan (sedimen, tanah, batuan, dan partikel lainnya) akibat transportasi oleh angin, tanah dan material lain di bawah pengaruh gravitasi atau oleh makhluk hidup semisal hewan yang membuat liang atau pertumbuhan akar tanaman yang mengakibatkan retakan tanah dalam hal ini disebut . Erosi tidak sama dengan pelapukan akibat cuaca, yang mana merupakan proses penghancuran mineral batuan dengan proses kimiawi maupun fisik, atau gabungan keduanya. Secara umum erosi melibatkan tiga proses yaitu pelepasan (detachment), transformasi (transformation), dan pengendapan (sedimentation)."@in . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . "Higadura"@eu . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . "Erosi"@in . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . "\u0415\u0440\u043E\u0437\u0456\u044F"@uk . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . "\u4FB5\u8680\u4F5C\u7528\uFF08\u82F1\u8A9E\uFF1Aerosion\uFF09\u6216\u6C34\u571F\u6D41\u5931\uFF08\u82F1\u8A9E\uFF1Asoil erosion\uFF09\u662F\u81EA\u7136\u754C\u7684\u4E00\u79CD\u73B0\u8C61\uFF0C\u662F\u6307\u5730\u7403\u7684\u8868\u9762\u4E0D\u65AD\u53D7\u5230\u98CE\u3001\u6C34\u7684\u78E8\u635F\u3002\u8FD9\u4E2A\u8FC7\u7A0B\uFF0C\u9646\u5730\u9664\u4E86\u88AB\u4FB5\u8680\u4E4B\u5916\uFF0C\u8680\u51FA\u7684\u7269\u8D28\u9084\u6703\u88AB\u5E26\u8D70\uFF0C\u5806\u79EF\u5728\u5176\u4ED6\u5730\u65B9\uFF0C\u4E3B\u8981\u5806\u79EF\u5728\u6D77\u88E1\u3002 \u4FB5\u8680\u7531\u6C34\u6D41\u3001\u51B0\u79FB\u6216\u98CE\u5439\u9020\u6210\u3002 \u800C\u7531\u96EA\u3001\u971C\u3001\u9633\u5149\u3001\u96E8\u6C34\u5BF9\u5730\u8868\u7684\u4F5C\u7528\u5247\u53EB\u505A\u98CE\u5316\u4F5C\u7528\uFF0C\u66B4\u9732\u5728\u7A7A\u6C14\u4E2D\u7684\u5CA9\u77F3\u4F1A\u53D7\u5230\u5929\u6C14\u5F71\u54CD\uFF0C\u957F\u671F\u51B7\u70ED\u4EA4\u66FF\uFF0C\u6709\u4E9B\u5CA9\u77F3\u4F1A\u56E0\u800C\u5F00\u88C2\u3002\u5CA9\u77F3\u4E2D\u7684\u6C34\u7ED3\u51B0\u65F6\u4F1A\u81A8\u80C0\uFF0C\u8FD9\u4E2A\u4E5F\u4F1A\u4F7F\u5CA9\u77F3\u5F00\u88C2\u3002\u77F3\u5934\u53D7\u5230\u91CD\u529B\u7684\u6324\u538B\u540E\u7A81\u7136\u51CF\u538B\uFF0C\u4E5F\u4F1A\u4F7F\u5CA9\u77F3\u788E\u88C2\u3002\u96E8\u6C34\u662F\u7A00\u9178\uFF0C\u53EF\u6EB6\u5316\u6216\u6539\u53D8\u5CA9\u77F3\u5185\u7684\u5316\u5B66\u7269\u8D28\u3002\u690D\u7269\u7684\u6839\u548C\u7A74\u5C45\u52A8\u7269\u4E5F\u4F1A\u52A0\u901F\u98CE\u5316\u3002 \u56E0\u4E3A\u98CE\u5316\u800C\u788E\u88C2\u7684\u77F3\u5757\u4F1A\u7531\u6C34\u3001\u51B0\u3001\u98CE\u5E26\u8D70\uFF0C\u800C\u5982\u679C\u6C34\u3001\u51B0\u3001\u98CE\u5185\u5982\u6709\u77F3\u5757\uFF0C\u5373\u4F7F\u975E\u5E38\u7EC6\u5C0F\uFF0C\u4E5F\u80FD\u5927\u5927\u52A0\u5F3A\u4FB5\u8680\u7684\u4F5C\u7528\uFF0C\u6539\u53D8\u5730\u8C8C\u3002 \u6210\u56E0\u6C34\u571F\u6D41\u5931\u53EF\u80FD\u662F\u7531\u4E8E\u81EA\u7136\u73AF\u5883\u5F15\u8D77\u7684\uFF0C\u8B6C\u5982\u5730\u52BF\u9661\u5CED\uFF0C\u7A81\u53D1\u5927\u91CF\u964D\u6C34\uFF0C\u6216\u8005\u5730\u8D28\u53D8\u5316\u3002\u4F46\u66F4\u591A\u7684\u662F\u7531\u4E8E\u4EBA\u7C7B\u6D3B\u52A8\u5BFC\u81F4\u7684\uFF0C\u8B6C\u5982\u8FC7\u5EA6\u653E\u7267\uFF0C\u5F00\u57A6\u571F\u5730\uFF0C\u91C7\u4F10\u68EE\u6797\uFF0C\u9032\u884C\u5404\u9805\u5DE5\u7A0B\u5EFA\u8A2D\u7B49\u7B49\u3002 \u5BB3\u8655\u4FB5\u8680\u662F\u81EA\u7136\u73AF\u5883\u6076\u5316\u7684\u91CD\u8981\u539F\u56E0\u3002\u7531\u4E8E\u6C34\u7684\u6D41\u52A8\uFF0C\u5E26\u8D70\u4E86\u5730\u7403\u8868\u9762\u7684\u571F\u58E4\uFF0C\u4F7F\u5F97\u571F\u5730\u53D8\u5F97\u8D2B\u7620\uFF0C\u5CA9\u77F3\u88F8\u9732\uFF0C\u690D\u88AB\u7834\u574F\uFF0C\u751F\u6001\u6076\u5316\u3002 \u8FD9\u79CD\u81EA\u7136\u73B0\u8C61\u53EF\u4EE5\u662F\u5FAA\u73AF\u4F5C\u7528\u7684\uFF0C\u751F\u6001\u6076\u5316\u5F15\u8D77\u6C34\u571F\u6D41\u5931\uFF0C\u6C34\u571F\u6D41\u5931\u53C8\u4F7F\u5F97\u751F\u6001\u66F4\u52A0\u6076\u5316\u3002\u4E8E\u662F\u571F\u5730\u9000\u5316\uFF0C\u65E0\u6CD5\u8015\u79CD\u3002\u690D\u7269\u6B7B\u4EA1\uFF0C\u5730\u8868\u88F8\u9732\u3002\u6076\u52A3\u7684\u751F\u6001\u53C8\u66F4\u5BFC\u81F4\u6C14\u5019\u7684\u53D8\u5316\uFF0C\u4F7F\u5F97\u751F\u7269\u53EF\u751F\u5B58\u7684\u73AF\u5883\u53D8\u574F\u3002 \u6C34\u571F\u6D41\u5931\u8FD8\u4F1A\u4F7F\u5F97\u6CE5\u6C99\u6DE4\u79EF\uFF0C\u6CB3\u5E8A\u62AC\u9AD8\uFF0C\u5F15\u8D77\u6C34\u6D41\u4E0D\u7545\uFF0C\u6C34\u8D28\u6DF7\u6D4A\uFF0C\u751A\u81F3\u5BFC\u81F4\u6D2A\u6C34\u6CDB\u6EE5\uFF0C\u6CB3\u6D41\u6539\u9053\uFF0C\u5C31\u5982\u4E2D\u56FD\u7684\u9EC4\u6CB3\u3002 \u98CE\u5316\u4E0E\u4FB5\u8680\u7684\u533A\u522B\u3002\u98CE\u5316\u662F\u7834\u574F\u540E\u6539\u53D8\u7269\u4F53\u5F62\u72B6\uFF0C\u800C\u4FB5\u8680\u662F\u8F6C\u79FB\u7269\u4F53\uFF0C\u4ECE\u800C\u6539\u53D8\u5730\u8C8C\u3002"@zh . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . "\u00C9rosion"@fr . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . "Die Erosion (von lateinisch erodere \u201Aabnagen\u2018) ist ein grundlegender Prozess im exogenen Teil des Gesteinskreislaufes. Er beinhaltet die Abtragung von mehr oder weniger stark verwitterten Gesteinen (Regolith) oder Lockersedimenten einschlie\u00DFlich der B\u00F6den (siehe Bodenerosion). So erschafft die Erosion einerseits Gel\u00E4ndeformen wie Berg und Tal, zerst\u00F6rt selbige jedoch schlie\u00DFlich bei anhaltendem Wirken vollst\u00E4ndig, insofern ihr keine endogenen Prozesse (insbesondere Tektonik), die eine Anhebung der Landoberfl\u00E4che hervorrufen, entgegenwirken. Erosion ist das Gegenst\u00FCck zur Sedimentation. Der Prozess, der zwischen Erosion und Sedimentation vermittelt, hei\u00DFt Transport (siehe Hjulstr\u00F6m-Diagramm). Bei Erosion wird im Wesentlichen zwischen linienhafter (linearer) und fl\u00E4chenhafter Erosion unterschieden. Unter linienhafter Erosion versteht man die Eintiefung der Erdoberfl\u00E4che durch abflie\u00DFendes Wasser in kleinen, kurzlebigen Rinnsalen (Rillenerosion) oder in Flie\u00DFgew\u00E4ssern (dann als fluviatile oder Flusserosion bezeichnet). Eine andere und derzeit auf der Erde weniger weit verbreitete Form linienhafter Erosion erfolgt durch Gebirgsgletscher (Exaration oder Glazialerosion). Die entstehenden Talformen sind V-f\u00F6rmig (Kerbtal) bei fluviatiler und U-f\u00F6rmig (Trogtal) bei glazialer Erosion. Hingegen erfolgt fl\u00E4chenhafte Erosion \u00E4olisch (durch Wind), marin (durch Meeresbrandung und -Str\u00F6mung), glazial durch Inlandeis und gelegentlich auch direkt durch Niederschl\u00E4ge (siehe Absp\u00FClung). Lineare und fl\u00E4chenhafte Erosion sind nicht vollst\u00E4ndig voneinander abgrenzbar und ma\u00DFstabsabh\u00E4ngig. So wirkt Rillenerosion im kleinen Ma\u00DFstab linienhaft, im gro\u00DFen Ma\u00DFstab jedoch fl\u00E4chenhaft (insbesondere z. B. bei Bodenerosion). Auch geht z. B. in Eiszeiten oder in besonders hohen Breiten die lineare Erosion von Gebirgsgletschern in die fl\u00E4chenhafte Erosion von Inlandeisgletschern \u00FCber. Die gro\u00DFfl\u00E4chige Abtragung und Einebnung ganzer Landoberfl\u00E4chen wird als Denudation bezeichnet."@de . . . . . . "L'erosione \u00E8 una fase del processo sedimentario e consiste nella separazione fisica, da suoli e rocce affioranti, e successivo allontanamento di frammenti, chiamati \"clasti\", e di soluti generati dalla fase di degradazione meteorica. Il termine viene applicato non solo al processo fisico-chimico in s\u00E9, ma anche agli effetti che l'erosione produce sul territorio. L'erosione tende a portare la superficie terrestre verso un profilo di equilibrio, raggiunto il quale le forze che la determinano sono insufficienti a farla proseguire o questa rallenta in modo significativo la sua azione."@it . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . "Higadura lurrazaleko gaien karraskatze eta suntsitzea da (lurra, lokatza, arroka eta beste) agente geologikoen eraginpean. Etengabeko marruskatze-lana ibaiek, euri urek, haizeak, izotzak edo itsasoak eragiten dute, grabitazioa edo izaki biziek direla-eta. Higaduraren ondorioz askatutako harri puskak ez dira toki berean gelditzen, agente berak egiten duen mugimenduari esker lekualdatzen dira, hau da, garraiatu. Garraioa burutzen duten agenteak honako hauek dira: grabitatea, ibaiak, errekak eta uharrek daramaten ura, glaziarretako izotza, itsasoko ura eta haizea."@eu . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . "Erosion (fr\u00E5n latin ero'sio n\u00F6tning) \u00E4r nedn\u00F6tning och transport av berg, jord eller annat material p\u00E5 grund av mekanisk eller kemisk p\u00E5verkan. Erosion kan till exempel orsakas av vind, rinnande vatten, v\u00E5gor, glaci\u00E4rer, gravitationsr\u00F6relser, levande organismer, men \u00E4ven genom massr\u00F6relsernas materialtransport nedf\u00F6r sluttningar. Till skillnad fr\u00E5n vittring s\u00E5 f\u00F6ruts\u00E4tter begreppet erosion att det \u00E4ven sker en bortf\u00F6rsel. Erosion \u00E4r en naturlig process. Den har tillsammans med de tektoniska processerna format jordytan. P\u00E5 m\u00E5nga st\u00E4llen har m\u00E4nniskan p\u00E5verkat den (jordbruk, avskogning, \u00F6verbetning, v\u00E4g- och j\u00E4rnv\u00E4gsbygge), vilket oftast inneburit en h\u00F6gre erosionstakt, speciellt \u00F6kad vinderosion. Jorderosion kan medf\u00F6ra att odlingsyta och n\u00E4rings\u00E4mnen f\u00F6rsvinner. Detta kan leda till igenslamning av vattendrag, \u00F6kad risk f\u00F6r \u00F6versv\u00E4mningar men ocks\u00E5 skador p\u00E5 fisk och korallrev. Erosion \u00E4r en utj\u00E4mnande kraft (en exogen kraft), som \"str\u00E4var\" efter att j\u00E4mna ut markytan, med ett peneplan som ett slutstadium. Ett av de allvarligaste problemen n\u00E4r det g\u00E4ller erosion som orsakas av rinnande vatten finns i Kina p\u00E5 de centrala delarna av Gula floden samt i Yangtzeflodens \u00F6vre lopp. 1,6 miljarder ton sediment fl\u00F6dar varje \u00E5r fr\u00E5n Gula floden ut i havet. Sedimenten kommer ursprungligen fr\u00E5n vattenerosion i l\u00F6ss-plat\u00E5 regionen i nordv\u00E4stra Kina. Kina var f\u00F6rut ett l\u00F6vskogrikt land, men nu \u00E4r det mesta av skogen \u00E4r sk\u00F6vlad f\u00F6r \u00E5kermarkens skull. Man f\u00F6rs\u00F6ker dock \u00E5terplantera skog f\u00F6r att motverka jorderosion."@sv . . . . . . . . . . . . . . . . . . . . . . . . . . "Erozja"@pl . . . . . . . . "En g\u00E9omorphologie, l\u2019\u00E9rosion est le processus de d\u00E9gradation et de transformation du relief, et donc des sols, roches, berges et littoraux qui est caus\u00E9 par tout agent externe (donc autre que la tectonique). Un relief dont le model\u00E9 s'explique principalement par l'\u00E9rosion est dit \u00AB \u00BB. Les facteurs d'\u00E9rosion sont : \n* le climat ; \n* le relief ; \n* la physique (duret\u00E9) et la chimie (solubilit\u00E9 par exemple) de la roche ; \n* des facteurs \u00E9cologiques et p\u00E9dologiques (pr\u00E9sence/absence de faune, fonge, couverture v\u00E9g\u00E9tale et lich\u00E9nique\u2026) et leur nature ; \n* l'histoire tectonique (fracturation par exemple) ; \n* l'action humaine (pratiques agricoles telle que labours, surp\u00E2turage, min\u00E9ralisation des sols, cultures sur pentes\u2026), d\u00E9forestation, imperm\u00E9abilisation, artificialisation, urbanisation qui dans le monde prend une importance croissante et pr\u00E9occupante. L'\u00E9rosion agit \u00E0 diff\u00E9rents rythmes et peut, sur plusieurs dizaines de millions d'ann\u00E9es, araser des montagnes, creuser des vall\u00E9es, faire reculer des falaises. Des ph\u00E9nom\u00E8nes naturels violents tels qu'une avalanche, un j\u00F6kulhlaup, un lahar ou un orage peuvent modifier consid\u00E9rablement le paysage en quelques heures, voire en quelques minutes."@fr . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . "Erozio"@eo . . . . . . . . . . . .