. . . . "La deriva continental es el desplazamiento de las masas continentales unas respecto a otras. Esta teor\u00EDa fue desarrollada en 1912 por el alem\u00E1n Alfred Wegener a partir de diversas observaciones emp\u00EDrico-racionales, pero no fue hasta la d\u00E9cada de 1960, con el desarrollo de la tect\u00F3nica de placas, cuando pudo explicarse de manera adecuada el movimiento de los continentes.\u200B"@es . . . . . . "Deriva dei continenti"@it . . . . . "Die Theorie der Kontinentaldrift, auch Kontinentalverschiebung genannt, beschreibt die langsame Bewegung, Aufspaltung und Vereinigung von Kontinenten. Erste Hypothesen zur Kontinentaldrift gab es bereits im 18. und 19. Jahrhundert. Jedoch f\u00FChrte erst die Arbeit von Alfred Wegener zu einer allm\u00E4hlichen Abkehr vom Fixismus hin zum Mobilismus. Die Bewegung der Erdteile ist heute Bestandteil der Theorie der Plattentektonik."@de . . "Continentverschuiving"@nl . . . . . . . . . . . . . . . . . "( \uBBF8\uAD6D\uC758 \uC560\uB2C8\uBA54\uC774\uC158\uC5D0 \uB300\uD574\uC11C\uB294 \uC544\uC774\uC2A4 \uC5D0\uC774\uC9C0 4: \uB300\uB959 \uC774\uB3D9\uC124 \uBB38\uC11C\uB97C \uCC38\uACE0\uD558\uC2ED\uC2DC\uC624.) \uB300\uB959 \uC774\uB3D9\uC124(\u5927\u9678 \u79FB\u52D5\u8AAA, Continental drift theory)\uC740 \uB3C5\uC77C\uC758 \uAE30\uC0C1\uD559\uC790\uC778 \uC54C\uD504\uB808\uD2B8 \uBCA0\uAC8C\uB108\uAC00 \uC81C\uCC3D\uD55C \uD559\uC124\uB85C, \uC6D0\uB798 \uD558\uB098\uC758 \uCD08\uB300\uB959\uC73C\uB85C \uC774\uB904\uC838 \uC788\uB358 \uB300\uB959\uB4E4\uC774 \uAC08\uB77C\uC838 \uC774\uB3D9\uD558\uBA74\uC11C \uD604\uC7AC\uC640 \uAC19\uC740 \uB300\uB959\uB4E4\uC774 \uB9CC\uB4E4\uC5B4\uC84C\uB2E4\uB294 \uC774\uB860\uC774\uB2E4. 1912\uB144\uC5D0 \uADF8\uC758 \uC800\uC11C \u300A\uB300\uB959\uC758 \uAE30\uC6D0\u300B(Die Entstehung der Kontinente)\uC5D0\uC11C \uBCA0\uAC8C\uB108\uB294 \uC9C0\uC9C8, \uACE0\uC0DD\uBB3C, \uACE0\uAE30\uD6C4 \uB4F1\uC758 \uC790\uB8CC\uB97C \uBC14\uD0D5\uC73C\uB85C \uD0DC\uACE0\uC5D0\uB294 \uB300\uC11C\uC591\uC758 \uC591\uCABD\uC758 \uB300\uB959\uC774 \uAC01\uAC01\uC758 \uBC29\uD5A5\uC73C\uB85C \uD45C\uB958\uD588\uB2E4\uB294 \uB300\uB959\uC774\uB3D9\uC124\uC744 \uC8FC\uC7A5\uD558\uC600\uB2E4. 1915\uB144\uC5D0\uB294 \u300A\uB300\uB959\uACFC \uD574\uC591\uC758 \uAE30\uC6D0\u300B(Die Entstehung der Kontinente und Ozeane)\uC5D0\uC11C \u2018\uD310\uAC8C\uC544\u2019\uB77C\uB294 \uCD08\uB300\uB959(\uAC70\uB300\uD55C \uC721\uAD34)\uC774 \uC874\uC7AC\uD558\uC600\uACE0 \uC57D 2\uC5B5\uB144 \uC804\uC5D0 \uBD84\uC5F4\uD55C \uB4A4 \uD45C\uB958\uD558\uC5EC \uD604\uC7AC\uC758 \uC704\uCE58\uC640 \uBAA8\uC2B5\uC744 \uAC00\uC9C0\uAC8C \uB418\uC5C8\uB2E4\uACE0 \uBC1C\uD45C\uD558\uC600\uB2E4. \uADF8\uB7EC\uB098 \uBCA0\uAC8C\uB108\uB294 \uB300\uB959 \uC774\uB3D9\uC758 \uC6D0\uB3D9\uB825\uC744 \uC124\uBA85\uD560 \uC218 \uC5C6\uC5B4 \uADF8\uC758 \uD559\uC124\uC740 \uD559\uACC4\uB85C\uBD80\uD130 \uC778\uC815\uBC1B\uC9C0 \uBABB\uD588\uB2E4. \uB300\uB959\uC744 \uC774\uB3D9\uC2DC\uD0A4\uB294 \uD798\uC740 \uBCA0\uAC8C\uB108 \uC774\uD6C4 \uB2E4\uB978 \uD559\uC790\uB4E4\uC5D0 \uC758\uD574 \uB9E8\uD2C0\uC758 \uB300\uB958\uB85C \uC81C\uC2DC\uB418\uC5C8\uC73C\uBA70, \uB300\uB959 \uC774\uB3D9\uC124\uC740 \uD310 \uAD6C\uC870\uB860\uC73C\uB85C \uBC1C\uC804\uB41C\uB2E4. \uB300\uB959 \uC774\uB3D9\uC758 \uC99D\uAC70"@ko . . . . . . . . . . . "\u5927\u9678\u79FB\u52D5\u8AAC\uFF08\u305F\u3044\u308A\u304F\u3044\u3069\u3046\u305B\u3064\u3001\u82F1: continental drift theory, theory of continental drift\uFF09\u306F\u3001\u5927\u9678\u306F\u5730\u7403\u8868\u9762\u4E0A\u3092\u79FB\u52D5\u3057\u3066\u305D\u306E\u4F4D\u7F6E\u3084\u5F62\u72B6\u3092\u5909\u3048\u308B\u3068\u3044\u3046\u5B66\u8AAC\u3002\u5927\u9678\u6F02\u79FB\u8AAC\uFF08\u305F\u3044\u308A\u304F\u3072\u3087\u3046\u3044\u305B\u3064\uFF09\u3068\u3082\u3044\u3046\u3002 \u767A\u60F3\u81EA\u4F53\u306F\u53E4\u304F\u304B\u3089\u3042\u308A\u69D8\u3005\u306A\u4EBA\u7269\u304C\u8FF0\u3079\u3066\u3044\u308B\u304C\u3001\u4E00\u822C\u306B\u306F\u30C9\u30A4\u30C4\u306E\u6C17\u8C61\u5B66\u8005\u30A2\u30EB\u30D5\u30EC\u30FC\u30C8\u30FB\u30F4\u30A7\u30FC\u30B2\u30CA\u30FC\u304C1912\u5E74\u306B\u63D0\u5531\u3057\u305F\u8AAC\u3092\u6307\u3059\u3002\u30F4\u30A7\u30FC\u30B2\u30CA\u30FC\u306E\u5927\u9678\u79FB\u52D5\u8AAC\u306F\u767A\u8868\u5F8C\u9577\u304F\u53D7\u5BB9\u3055\u308C\u306A\u304B\u3063\u305F\u304C\u3001\u73FE\u5728\u306F\u30D7\u30EC\u30FC\u30C8\u30C6\u30AF\u30C8\u30CB\u30AF\u30B9\u7406\u8AD6\u306E\u5E30\u7D50\u306E\u3072\u3068\u3064\u3068\u3057\u3066\u5B9F\u8A3C\u3055\u308C\u53D7\u3051\u5165\u308C\u3089\u308C\u3066\u3044\u308B\u3002"@ja . . . . . . . "Kontinent\u00E1ln\u00ED drift (pohyb sv\u011Btad\u00EDl\u016F) je teorie navr\u017Een\u00E1 v roce 1912 n\u011Bmeck\u00FDm meteorologem a geofyzikem Alfredem Wegenerem vysv\u011Btluj\u00EDc\u00ED vznik kontinent\u016F rozpadem p\u016Fvodn\u00EDho superkontinentu Pangea. P\u016Fvodn\u00ED my\u0161lenku, \u017Ee kontinenty do sebe \u201Ezapadaj\u00ED\u201C, kterou vyslovil u\u017E vl\u00E1msk\u00FD kartograf Abraham Ortelius (1527-1598), podpo\u0159il Wegener srovn\u00E1n\u00EDm geologick\u00FDch a paleontologick\u00FDch n\u00E1lez\u016F p\u0159edev\u0161\u00EDm z pob\u0159e\u017E\u00ED Afriky a Ji\u017En\u00ED Ameriky. Z\u00E1sadn\u00ED chybou Wegnerova pojet\u00ED bylo, \u017Ee pova\u017Eoval za hnac\u00ED s\u00EDlu pohybu kontinent\u016F Coriolisovu s\u00EDlu (ta je mnoha\u0159\u00E1dov\u011B nedostate\u010Dn\u00E1 pro takov\u00FD proces).Dnes je teorie kontinent\u00E1ln\u00EDho driftu sou\u010D\u00E1st\u00ED teorie deskov\u00E9 tektoniky, kter\u00E1 vysv\u011Btluje nejen pohyb kontinent\u016F, ale i dynamiku zemsk\u00E9ho pl\u00E1\u0161t\u011B. Teorie deskov\u00E9 tektoniky tvrd\u00ED, \u017Ee zemsk\u00E1 k\u016Fra je slo\u017Eena z tuh\u00FDch desek. Tyto desky se pak pohybuj\u00ED po vrchn\u00ED vrstv\u011B pl\u00E1\u0161t\u011B a vz\u00E1jemn\u011B do sebe zapadaj\u00ED tak, \u017Ee mezi nimi neexistuj\u00ED \u017E\u00E1dn\u00E9 propadliny, kter\u00E9 by umo\u017E\u0148ovaly kontakt s pl\u00E1\u0161t\u011Bm. Pohyby tektonick\u00FDch desek zp\u016Fsobuj\u00ED zem\u011Bt\u0159esen\u00ED."@cs . . . "Die Theorie der Kontinentaldrift, auch Kontinentalverschiebung genannt, beschreibt die langsame Bewegung, Aufspaltung und Vereinigung von Kontinenten. Erste Hypothesen zur Kontinentaldrift gab es bereits im 18. und 19. Jahrhundert. Jedoch f\u00FChrte erst die Arbeit von Alfred Wegener zu einer allm\u00E4hlichen Abkehr vom Fixismus hin zum Mobilismus. Die Bewegung der Erdteile ist heute Bestandteil der Theorie der Plattentektonik."@de . . . "Kontinenta drivo estas la movi\u011Do de la kontinentoj relative al la reciproka situo. La hipotezo, ke kontinentoj ne estas fiksaj, sed \u201Edrivas\u201C sur la surfaco de la tero, estis unuafoje proponita de Abraham Ortelius en 1596 kaj plene evoluigita de Alfred Wegener en 1912. La teorioj de Wegener siatempe ne estis akceptitaj, \u0109ar je tiu tempo neniu povis vidi ian \u201Emotoron\u201C por peli tiel gigantajn amasojn. Tiu ideo venis nur en la 1960-aj jaroj, kiam proponis la teorion de platotektoniko: la mem movi\u011Das: la \u201Enaskas\u201C novan kontinentan materialon kaj tiel dis\u015Dovas la kontinentajn platojn."@eo . . . . . . "\u5927\u9678\u79FB\u52D5\u8AAC"@ja . "Continental drift is the hypothesis that the Earth's continents have moved over geologic time relative to each other, thus appearing to have \"drifted\" across the ocean bed. The idea of continental drift has been subsumed into the science of plate tectonics, which studies the movement of the continents as they ride on plates of the Earth's lithosphere. The speculation that continents might have 'drifted' was first put forward by Abraham Ortelius in 1596. A pioneer of the modern view of mobilism was the Austrian geologist Otto Ampferer. The concept was independently and more fully developed by Alfred Wegener in 1912, but the hypothesis was rejected by many for lack of any motive mechanism. The English geologist Arthur Holmes later proposed mantle convection for that mechanism."@en . . "Kontinent\u00E1ln\u00ED drift"@cs . . . . . . . . . "On appelle d\u00E9rive des continents l'ensemble des d\u00E9placements horizontaux des continents (ou des blocs continentaux) les uns par rapport aux autres. L'hypoth\u00E8se de la d\u00E9rive des continents a \u00E9t\u00E9 sugg\u00E9r\u00E9e d\u00E8s 1596. Elle a ensuite \u00E9t\u00E9 d\u00E9velopp\u00E9e et popularis\u00E9e, mais mal d\u00E9fendue, par Alfred Wegener en 1912. Apr\u00E8s la d\u00E9couverte des anomalies magn\u00E9tiques du fond des oc\u00E9ans dans les ann\u00E9es 1960, la d\u00E9rive des continents est devenue une r\u00E9alit\u00E9 attest\u00E9e par des observations directes et indirectes, et que l'on comprend dans le cadre plus g\u00E9n\u00E9ral de la th\u00E9orie de la tectonique des plaques."@fr . "\u5927\u9646\u6F02\u79FB\u5B66\u8BF4\u662F\u89E3\u91CA\u5927\u9646\u548C\u6D77\u6D0B\u7684\u5206\u5E03\u4EE5\u53CA\u5927\u9646\u4E4B\u95F4\u5B58\u5728\u7684\u6784\u9020\u3001\u5730\u8D28\u548C\u7269\u7406\u76F8\u4F3C\u6027\u7684\u5047\u8BF4\uFF0C\u8BA4\u4E3A\u5404\u5927\u9646\u662F\u7531\u4E00\u4E2A\u5DE8\u5927\u7684\u9646\u5757\u6F02\u79FB\u3001\u5206\u5F00\u800C\u5F62\u6210\u7684\u3002\u6700\u521D\u7531\u4E9E\u4F2F\u62C9\u7F55\u00B7\u5967\u7279\u67F3\u65AF\u57281596\u5E74\u63D0\u51FA\uFF0C\u5F8C\u4F86\u5FB7\u56FD\u79D1\u5B66\u5BB6\u963F\u5C14\u5F17\u96F7\u5FB7\u00B7\u9B4F\u683C\u7EB3\u57281912\u5E74\u52A0\u4EE5\u95E1\u8FF0\uFF0C\u4E2D\u6587\u4E2D\u201C\u5927\u9646\u6F02\u79FB\u8BF4\u201D\u3001\u201C\u5927\u9646\u6F02\u79FB\u5047\u8BF4\u201D\u5747\u6307\u540C\u4E00\u6982\u5FF5\u3002\u9019\u500B\u5927\u81BD\u7684\u5B78\u8AAA\u4E00\u76F4\u88AB\u5B78\u754C\u5FFD\u8996\uFF0C\u76F4\u81F31960\u5E74\u4EE3\u6D77\u6D0B\u64F4\u5F35\u8AAA\u51FA\u73FE\uFF0C\u4EE4\u5927\u9678\u98C4\u79FB\u8AAA\u5F97\u4EE5\u767C\u5C55\uFF0C\u5F8C\u4F86\u66F4\u95E1\u8FF0\u70BA\u677F\u584A\u69CB\u9020\u7406\u8AD6\u3002\u5927\u9646\u6F02\u79FB\u7684\u60F3\u6CD5\u5DF2\u7ECF\u88AB\u677F\u5757\u6784\u9020\u7406\u8BBA\u7EB3\u5165\uFF0C\u89E3\u91CA\u5927\u9646\u5982\u4F55\u79FB\u52A8\u3002 \u4E3B\u8981\u5185\u5BB9\u4E3A\u8FDC\u53E4\u65F6\u4EE3\u7684\u5730\u7403\u53EA\u6709\u4E00\u5757\u201C\u6CDB\u53E4\u9646\u201D\u6216\u7A31\u76E4\u53E4\u5927\u9678\u7684\u5E9E\u5927\u9646\u5730\uFF0C\u88AB\u79F0\u4E3A\u201C\u6CDB\u5927\u6D0B\u201D\u7684\u6C34\u57DF\u5305\u56F4\uFF0C\u5927\u7EA6\u4E8E2\u4EBF\u5E74\u4EE5\u524D\u201C\u6CDB\u5927\u9646\u201D\u5F00\u59CB\u7834\u88C2\uFF0C\u5230\u8DDD\u4ECA\u7EA6\u4E8C\u3001\u4E09\u767E\u4E07\u5E74\u4EE5\u524D\uFF0C\u6F02\u79FB\u7684\u5927\u9646\u5F62\u6210\u73B0\u5728\u7684\u4E03\u5927\u6D32\u548C\u4E94\u5927\u6D0B\u7684\u57FA\u672C\u5730\u8C8C\u3002 \u503C\u5F97\u4E00\u63D0\u7684\u662F\u5927\u9678\u6F02\u79FB\u5B78\u8AAA\u8207\u677F\u584A\u69CB\u9020\u5B78\u8AAA\u6709\u4E9B\u6839\u672C\u7684\u4E0D\u540C\uFF0C\u524D\u8005\u5047\u8A2D\u63A8\u52D5\u529B\u662F\u6F6E\u6C50\uFF0C\u5F8C\u8005\u5047\u60F3\u63A8\u52D5\u529B\u662F\u7531\u65BC\u5730\u5E54\u51FA\u73FE\u5C0D\u6D41\uFF0C\u62D6\u52D5\u677F\u584A\u3002\u4F46\u5728\u9B4F\u683C\u7EB31929\u5E74\u7B2C\u56DB\u7248\u7684\u300A\u5927\u9646\u548C\u6D77\u6D0B\u7684\u5F62\u6210\u300B\u4E2D\uFF0C\u4ED6\u5DF2\u7ECF\u63A5\u53D7\u4E86\u5730\u5E54\u5BF9\u6D41\u63D0\u4F9B\u52A8\u529B\u7684\u601D\u60F3\u3002"@zh . . . . "\u5927\u9678\u79FB\u52D5\u8AAC\uFF08\u305F\u3044\u308A\u304F\u3044\u3069\u3046\u305B\u3064\u3001\u82F1: continental drift theory, theory of continental drift\uFF09\u306F\u3001\u5927\u9678\u306F\u5730\u7403\u8868\u9762\u4E0A\u3092\u79FB\u52D5\u3057\u3066\u305D\u306E\u4F4D\u7F6E\u3084\u5F62\u72B6\u3092\u5909\u3048\u308B\u3068\u3044\u3046\u5B66\u8AAC\u3002\u5927\u9678\u6F02\u79FB\u8AAC\uFF08\u305F\u3044\u308A\u304F\u3072\u3087\u3046\u3044\u305B\u3064\uFF09\u3068\u3082\u3044\u3046\u3002 \u767A\u60F3\u81EA\u4F53\u306F\u53E4\u304F\u304B\u3089\u3042\u308A\u69D8\u3005\u306A\u4EBA\u7269\u304C\u8FF0\u3079\u3066\u3044\u308B\u304C\u3001\u4E00\u822C\u306B\u306F\u30C9\u30A4\u30C4\u306E\u6C17\u8C61\u5B66\u8005\u30A2\u30EB\u30D5\u30EC\u30FC\u30C8\u30FB\u30F4\u30A7\u30FC\u30B2\u30CA\u30FC\u304C1912\u5E74\u306B\u63D0\u5531\u3057\u305F\u8AAC\u3092\u6307\u3059\u3002\u30F4\u30A7\u30FC\u30B2\u30CA\u30FC\u306E\u5927\u9678\u79FB\u52D5\u8AAC\u306F\u767A\u8868\u5F8C\u9577\u304F\u53D7\u5BB9\u3055\u308C\u306A\u304B\u3063\u305F\u304C\u3001\u73FE\u5728\u306F\u30D7\u30EC\u30FC\u30C8\u30C6\u30AF\u30C8\u30CB\u30AF\u30B9\u7406\u8AD6\u306E\u5E30\u7D50\u306E\u3072\u3068\u3064\u3068\u3057\u3066\u5B9F\u8A3C\u3055\u308C\u53D7\u3051\u5165\u308C\u3089\u308C\u3066\u3044\u308B\u3002"@ja . . . . . "\u5927\u9646\u6F02\u79FB\u5B66\u8BF4\u662F\u89E3\u91CA\u5927\u9646\u548C\u6D77\u6D0B\u7684\u5206\u5E03\u4EE5\u53CA\u5927\u9646\u4E4B\u95F4\u5B58\u5728\u7684\u6784\u9020\u3001\u5730\u8D28\u548C\u7269\u7406\u76F8\u4F3C\u6027\u7684\u5047\u8BF4\uFF0C\u8BA4\u4E3A\u5404\u5927\u9646\u662F\u7531\u4E00\u4E2A\u5DE8\u5927\u7684\u9646\u5757\u6F02\u79FB\u3001\u5206\u5F00\u800C\u5F62\u6210\u7684\u3002\u6700\u521D\u7531\u4E9E\u4F2F\u62C9\u7F55\u00B7\u5967\u7279\u67F3\u65AF\u57281596\u5E74\u63D0\u51FA\uFF0C\u5F8C\u4F86\u5FB7\u56FD\u79D1\u5B66\u5BB6\u963F\u5C14\u5F17\u96F7\u5FB7\u00B7\u9B4F\u683C\u7EB3\u57281912\u5E74\u52A0\u4EE5\u95E1\u8FF0\uFF0C\u4E2D\u6587\u4E2D\u201C\u5927\u9646\u6F02\u79FB\u8BF4\u201D\u3001\u201C\u5927\u9646\u6F02\u79FB\u5047\u8BF4\u201D\u5747\u6307\u540C\u4E00\u6982\u5FF5\u3002\u9019\u500B\u5927\u81BD\u7684\u5B78\u8AAA\u4E00\u76F4\u88AB\u5B78\u754C\u5FFD\u8996\uFF0C\u76F4\u81F31960\u5E74\u4EE3\u6D77\u6D0B\u64F4\u5F35\u8AAA\u51FA\u73FE\uFF0C\u4EE4\u5927\u9678\u98C4\u79FB\u8AAA\u5F97\u4EE5\u767C\u5C55\uFF0C\u5F8C\u4F86\u66F4\u95E1\u8FF0\u70BA\u677F\u584A\u69CB\u9020\u7406\u8AD6\u3002\u5927\u9646\u6F02\u79FB\u7684\u60F3\u6CD5\u5DF2\u7ECF\u88AB\u677F\u5757\u6784\u9020\u7406\u8BBA\u7EB3\u5165\uFF0C\u89E3\u91CA\u5927\u9646\u5982\u4F55\u79FB\u52A8\u3002 \u4E3B\u8981\u5185\u5BB9\u4E3A\u8FDC\u53E4\u65F6\u4EE3\u7684\u5730\u7403\u53EA\u6709\u4E00\u5757\u201C\u6CDB\u53E4\u9646\u201D\u6216\u7A31\u76E4\u53E4\u5927\u9678\u7684\u5E9E\u5927\u9646\u5730\uFF0C\u88AB\u79F0\u4E3A\u201C\u6CDB\u5927\u6D0B\u201D\u7684\u6C34\u57DF\u5305\u56F4\uFF0C\u5927\u7EA6\u4E8E2\u4EBF\u5E74\u4EE5\u524D\u201C\u6CDB\u5927\u9646\u201D\u5F00\u59CB\u7834\u88C2\uFF0C\u5230\u8DDD\u4ECA\u7EA6\u4E8C\u3001\u4E09\u767E\u4E07\u5E74\u4EE5\u524D\uFF0C\u6F02\u79FB\u7684\u5927\u9646\u5F62\u6210\u73B0\u5728\u7684\u4E03\u5927\u6D32\u548C\u4E94\u5927\u6D0B\u7684\u57FA\u672C\u5730\u8C8C\u3002 \u503C\u5F97\u4E00\u63D0\u7684\u662F\u5927\u9678\u6F02\u79FB\u5B78\u8AAA\u8207\u677F\u584A\u69CB\u9020\u5B78\u8AAA\u6709\u4E9B\u6839\u672C\u7684\u4E0D\u540C\uFF0C\u524D\u8005\u5047\u8A2D\u63A8\u52D5\u529B\u662F\u6F6E\u6C50\uFF0C\u5F8C\u8005\u5047\u60F3\u63A8\u52D5\u529B\u662F\u7531\u65BC\u5730\u5E54\u51FA\u73FE\u5C0D\u6D41\uFF0C\u62D6\u52D5\u677F\u584A\u3002\u4F46\u5728\u9B4F\u683C\u7EB31929\u5E74\u7B2C\u56DB\u7248\u7684\u300A\u5927\u9646\u548C\u6D77\u6D0B\u7684\u5F62\u6210\u300B\u4E2D\uFF0C\u4ED6\u5DF2\u7ECF\u63A5\u53D7\u4E86\u5730\u5E54\u5BF9\u6D41\u63D0\u4F9B\u52A8\u529B\u7684\u601D\u60F3\u3002"@zh . . . "Continentverschuiving, continentale drift of continentendrift (van het Engelse continental drift) is het geologische verschijnsel waarbij continenten bewegen. Deze bewegingen met snelheden van enkele centimeters per jaar kunnen sinds de opkomst van de satellietgeodesie ook daadwerkelijk gemeten worden. De beweging van continenten wordt veroorzaakt door platentektoniek."@nl . . . "S\u00EDobghluaiseacht ilchr\u00EDochach"@ga . . . . . "\u0414\u0440\u0438\u0444\u0442\u043E\u0432\u0430 \u0433\u0456\u043F\u043E\u0442\u0435\u0437\u0430, \u0442\u0435\u043E\u0440\u0456\u044F \u0434\u0440\u0435\u0439\u0444\u0443 \u043C\u0430\u0442\u0435\u0440\u0438\u043A\u0456\u0432 (\u0440\u043E\u0441. \u0434\u0440\u0438\u0444\u0442\u043E\u0432\u0430\u044F \u0433\u0438\u043F\u043E\u0442\u0435\u0437\u0430, \u0430\u043D\u0433\u043B. drift hypothesis, \u043D\u0456\u043C. Drifthypothese) \u2014 \u0433\u0456\u043F\u043E\u0442\u0435\u0437\u0430 \u0433\u043E\u0440\u0438\u0437\u043E\u043D\u0442\u0430\u043B\u044C\u043D\u043E\u0433\u043E \u043F\u0435\u0440\u0435\u043C\u0456\u0449\u0435\u043D\u043D\u044F (\u0434\u0440\u0438\u0444\u0442\u0443, \u0430\u0431\u043E \u0434\u0440\u0435\u0439\u0444\u0443) \u043C\u0430\u0442\u0435\u0440\u0438\u043A\u0456\u0432 \u043F\u043E \u043F\u043B\u0430\u0441\u0442\u0438\u0447\u043D\u043E\u043C\u0443 \u0431\u0430\u0437\u0430\u043B\u044C\u0442\u043E\u0432\u043E\u043C\u0443 \u0448\u0430\u0440\u0443 \u0437\u0435\u043C\u043D\u043E\u0457 \u043A\u043E\u0440\u0438. \u0490\u0440\u0443\u043D\u0442\u0443\u0454\u0442\u044C\u0441\u044F \u043D\u0430 \u043F\u043E\u0434\u0456\u0431\u043D\u043E\u0441\u0442\u0456 \u043E\u0431\u0440\u0438\u0441\u0456\u0432 \u043C\u0430\u0442\u0435\u0440\u0438\u043A\u0456\u0432, \u0457\u0445 \u0433\u0435\u043E\u043B\u043E\u0433\u0456\u0447\u043D\u043E\u0457 \u0431\u0443\u0434\u043E\u0432\u0438 \u0439 \u043E\u0440\u0433\u0430\u043D\u0456\u0447\u043D\u0438\u0445 \u0440\u0435\u0448\u0442\u043E\u043A \u0443 \u043F\u043E\u0440\u043E\u0434\u0430\u0445. \u0417\u0430 \u0434\u0440\u0438\u0444\u0442\u043E\u0432\u043E\u044E \u0433\u0456\u043F\u043E\u0442\u0435\u0437\u043E\u044E \u0441\u0443\u0447\u0430\u0441\u043D\u0456 \u043C\u0430\u0442\u0435\u0440\u0438\u043A\u0438 \u0443\u0442\u0432\u043E\u0440\u044E\u044E\u0442\u044C\u0441\u044F \u0437 \u0454\u0434\u0438\u043D\u043E\u0433\u043E \u0441\u0443\u043F\u0435\u0440\u043C\u0430\u0442\u0435\u0440\u0438\u043A\u0430 \u2014 \u041F\u0430\u043D\u0433\u0435\u0457, \u044F\u043A\u0438\u0439 \u0440\u043E\u0437\u043A\u043E\u043B\u043E\u0432\u0441\u044F \u043D\u0430 \u043F\u043E\u0447\u0430\u0442\u043A\u0443 \u043C\u0435\u0437\u043E\u0437\u043E\u044E. \u0412\u0438\u0441\u0443\u043D\u0443\u0432 \u0446\u044E \u0433\u0456\u043F\u043E\u0442\u0435\u0437\u0443 \u0432 \u0434\u0440\u0443\u0433\u0456\u0439 \u043F\u043E\u043B\u043E\u0432\u0438\u043D\u0456 XIX \u0441\u0442. \u0440\u043E\u0441\u0456\u0439\u0441\u044C\u043A\u0438\u0439 \u0430\u0441\u0442\u0440\u043E\u043D\u043E\u043C-\u0430\u043C\u0430\u0442\u043E\u0440 \u0404. \u0412. \u0411\u0438\u0445\u0430\u043D\u043E\u0432; \u043D\u0430 \u043F\u043E\u0447\u0430\u0442\u043A\u0443 XX \u0441\u0442. \u0457\u0457 \u0440\u043E\u0437\u0432\u0438\u043D\u0443\u0432 \u043D\u0456\u043C\u0435\u0446\u044C\u043A\u0438\u0439 \u0433\u0435\u043E\u0444\u0456\u0437\u0438\u043A \u0410.\u0412\u0435\u0433\u0435\u043D\u0435\u0440. \u0423 60-\u0445 \u0440\u043E\u043A\u0430\u0445 XX \u0441\u0442. \u0434\u0440\u0438\u0444\u0442\u043E\u0432\u0430 \u0433\u0456\u043F\u043E\u0442\u0435\u0437\u0430 \u0434\u043E\u043F\u043E\u0432\u043D\u0435\u043D\u0430 \u043D\u0430 \u043E\u0441\u043D\u043E\u0432\u0456 \u043D\u043E\u0432\u0438\u0445 \u0434\u0430\u043D\u0438\u0445 \u0433\u0435\u043E\u0444\u0456\u0437\u0438\u0447\u043D\u0438\u0445 \u0434\u043E\u0441\u043B\u0456\u0434\u0436\u0435\u043D\u044C \u0456 \u0431\u0443\u0440\u0456\u043D\u043D\u044F \u0434\u043D\u0430 \u043E\u043A\u0435\u0430\u043D\u0456\u0432."@uk . "\u0422\u0435\u043E\u0301\u0440\u0438\u044F \u0434\u0440\u0435\u0301\u0439\u0444\u0430 \u043C\u0430\u0442\u0435\u0440\u0438\u043A\u043E\u0301\u0432 \u0431\u044B\u043B\u0430 \u043F\u0440\u0435\u0434\u043B\u043E\u0436\u0435\u043D\u0430 \u0432 1912 \u0433\u043E\u0434\u0443 \u043D\u0435\u043C\u0435\u0446\u043A\u0438\u043C \u0433\u0435\u043E\u0433\u0440\u0430\u0444\u043E\u043C \u0410\u043B\u044C\u0444\u0440\u0435\u0434\u043E\u043C \u0412\u0435\u0433\u0435\u043D\u0435\u0440\u043E\u043C \u043D\u0430 \u043E\u0441\u043D\u043E\u0432\u0435 \u043D\u0430\u043A\u043E\u043F\u0438\u0432\u0448\u0438\u0445\u0441\u044F \u043D\u0430\u0443\u0447\u043D\u044B\u0445 \u0434\u0430\u043D\u043D\u044B\u0445. \u0412\u0435\u0433\u0435\u043D\u0435\u0440 \u043D\u0435 \u0431\u044B\u043B \u043F\u0435\u0440\u0432\u044B\u043C, \u043A\u0442\u043E \u043F\u0440\u0438\u0448\u0451\u043B \u043A \u043F\u043E\u0434\u043E\u0431\u043D\u043E\u0439 \u043C\u044B\u0441\u043B\u0438. \u0421\u043E\u0432\u043F\u0430\u0434\u0435\u043D\u0438\u0435 \u043E\u0447\u0435\u0440\u0442\u0430\u043D\u0438\u0439 \u043F\u043E\u0431\u0435\u0440\u0435\u0436\u044C\u044F \u0410\u0444\u0440\u0438\u043A\u0438 \u0438 \u042E\u0436\u043D\u043E\u0439 \u0410\u043C\u0435\u0440\u0438\u043A\u0438 \u0431\u044B\u043B\u043E \u0437\u0430\u043C\u0435\u0447\u0435\u043D\u043E \u0424\u0440\u044D\u043D\u0441\u0438\u0441\u043E\u043C \u0411\u044D\u043A\u043E\u043D\u043E\u043C \u0435\u0449\u0451 \u0432 1620-\u0445 \u0433\u043E\u0434\u0430\u0445. \u0418\u0434\u0435\u044E \u043E \u0434\u0432\u0438\u0436\u0435\u043D\u0438\u0438 \u043C\u0430\u0442\u0435\u0440\u0438\u043A\u043E\u0432 \u0432\u044B\u0434\u0432\u0438\u043D\u0443\u043B \u0432 1668 \u0444\u0440\u0430\u043D\u0446\u0443\u0437\u0441\u043A\u0438\u0439 \u0442\u0435\u043E\u043B\u043E\u0433 \u0424\u0440\u0430\u043D\u043A\u043E \u041F\u043B\u0430\u043A\u0435. \u041D\u0435\u043C\u0435\u0446\u043A\u0438\u0439 \u0442\u0435\u043E\u043B\u043E\u0433 \u0422\u0435\u043E\u0434\u043E\u0440 \u041B\u0438\u043B\u0438\u0435\u043D\u0442\u0430\u043B\u044C \u043F\u043E\u0448\u0451\u043B \u0434\u0430\u043B\u044C\u0448\u0435 \u0411\u044D\u043A\u043E\u043D\u0430, \u043A\u043E\u0433\u0434\u0430 \u0432 1756 \u043F\u0440\u0435\u0434\u043F\u043E\u043B\u043E\u0436\u0438\u043B, \u0447\u0442\u043E \u043F\u043E\u0431\u0435\u0440\u0435\u0436\u044C\u044F \u0410\u0444\u0440\u0438\u043A\u0438 \u0438 \u042E\u0436\u043D\u043E\u0439 \u0410\u043C\u0435\u0440\u0438\u043A\u0438 \u0442\u043E\u0447\u043D\u043E \u0441\u043E\u043E\u0442\u0432\u0435\u0442\u0441\u0442\u0432\u0443\u044E\u0442 \u0434\u0440\u0443\u0433 \u0434\u0440\u0443\u0433\u0443. \u0410\u043D\u0442\u043E\u043D\u0438\u043E \u0421\u043D\u0438\u0434\u0435\u0440, \u0436\u0438\u0432\u0448\u0438\u0439 \u0432 \u041F\u0430\u0440\u0438\u0436\u0435 \u0430\u043C\u0435\u0440\u0438\u043A\u0430\u043D\u0435\u0446, \u0432 1858 \u0433\u043E\u0434\u0443 \u043F\u0440\u0435\u0434\u043F\u043E\u043B\u043E\u0436\u0438\u043B, \u0447\u0442\u043E \u043A\u043E\u0433\u0434\u0430 \u0417\u0435\u043C\u043B\u044F \u043E\u0441\u0442\u044B\u0432\u0430\u043B\u0430, \u043E\u043D\u0430 \u0441\u0436\u0438\u043C\u0430\u043B\u0430\u0441\u044C \u043D\u0435\u0440\u0430\u0432\u043D\u043E\u043C\u0435\u0440\u043D\u043E, \u0438 \u043F\u043E \u044D\u0442\u043E\u0439 \u043F\u0440\u0438\u0447\u0438\u043D\u0435 \u0432\u0435\u0449\u0435\u0441\u0442\u0432\u043E \u043D\u0430 \u043F\u043E\u0432\u0435\u0440\u0445\u043D\u043E\u0441\u0442\u0438 \u0440\u0430\u0441\u043A\u043E\u043B\u043E\u043B\u043E\u0441\u044C \u043D\u0430 \u0447\u0430\u0441\u0442\u0438. \u041E\u043D \u043F\u0440\u0435\u0434\u0441\u0442\u0430\u0432\u0438\u043B, \u043A\u0440\u043E\u043C\u0435 \u0442\u043E\u0433\u043E, \u043E\u0431\u0449\u0438\u0435 \u0434\u043B\u044F \u0434\u0432\u0443\u0445 \u043C\u0430\u0442\u0435\u0440\u0438\u043A\u043E\u0432 \u0433\u043E\u0440\u043D\u044B\u0435 \u043F\u043E\u0440\u043E\u0434\u044B \u0438 \u0438\u0441\u043A\u043E\u043F\u0430\u0435\u043C\u044B\u0435 \u043E\u0441\u0442\u0430\u0442\u043A\u0438. \u0415\u0432\u0433\u0440\u0430\u0444 \u0411\u044B"@ru . . . . . . . . . "( \uBBF8\uAD6D\uC758 \uC560\uB2C8\uBA54\uC774\uC158\uC5D0 \uB300\uD574\uC11C\uB294 \uC544\uC774\uC2A4 \uC5D0\uC774\uC9C0 4: \uB300\uB959 \uC774\uB3D9\uC124 \uBB38\uC11C\uB97C \uCC38\uACE0\uD558\uC2ED\uC2DC\uC624.) \uB300\uB959 \uC774\uB3D9\uC124(\u5927\u9678 \u79FB\u52D5\u8AAA, Continental drift theory)\uC740 \uB3C5\uC77C\uC758 \uAE30\uC0C1\uD559\uC790\uC778 \uC54C\uD504\uB808\uD2B8 \uBCA0\uAC8C\uB108\uAC00 \uC81C\uCC3D\uD55C \uD559\uC124\uB85C, \uC6D0\uB798 \uD558\uB098\uC758 \uCD08\uB300\uB959\uC73C\uB85C \uC774\uB904\uC838 \uC788\uB358 \uB300\uB959\uB4E4\uC774 \uAC08\uB77C\uC838 \uC774\uB3D9\uD558\uBA74\uC11C \uD604\uC7AC\uC640 \uAC19\uC740 \uB300\uB959\uB4E4\uC774 \uB9CC\uB4E4\uC5B4\uC84C\uB2E4\uB294 \uC774\uB860\uC774\uB2E4. 1912\uB144\uC5D0 \uADF8\uC758 \uC800\uC11C \u300A\uB300\uB959\uC758 \uAE30\uC6D0\u300B(Die Entstehung der Kontinente)\uC5D0\uC11C \uBCA0\uAC8C\uB108\uB294 \uC9C0\uC9C8, \uACE0\uC0DD\uBB3C, \uACE0\uAE30\uD6C4 \uB4F1\uC758 \uC790\uB8CC\uB97C \uBC14\uD0D5\uC73C\uB85C \uD0DC\uACE0\uC5D0\uB294 \uB300\uC11C\uC591\uC758 \uC591\uCABD\uC758 \uB300\uB959\uC774 \uAC01\uAC01\uC758 \uBC29\uD5A5\uC73C\uB85C \uD45C\uB958\uD588\uB2E4\uB294 \uB300\uB959\uC774\uB3D9\uC124\uC744 \uC8FC\uC7A5\uD558\uC600\uB2E4. 1915\uB144\uC5D0\uB294 \u300A\uB300\uB959\uACFC \uD574\uC591\uC758 \uAE30\uC6D0\u300B(Die Entstehung der Kontinente und Ozeane)\uC5D0\uC11C \u2018\uD310\uAC8C\uC544\u2019\uB77C\uB294 \uCD08\uB300\uB959(\uAC70\uB300\uD55C \uC721\uAD34)\uC774 \uC874\uC7AC\uD558\uC600\uACE0 \uC57D 2\uC5B5\uB144 \uC804\uC5D0 \uBD84\uC5F4\uD55C \uB4A4 \uD45C\uB958\uD558\uC5EC \uD604\uC7AC\uC758 \uC704\uCE58\uC640 \uBAA8\uC2B5\uC744 \uAC00\uC9C0\uAC8C \uB418\uC5C8\uB2E4\uACE0 \uBC1C\uD45C\uD558\uC600\uB2E4. \uADF8\uB7EC\uB098 \uBCA0\uAC8C\uB108\uB294 \uB300\uB959 \uC774\uB3D9\uC758 \uC6D0\uB3D9\uB825\uC744 \uC124\uBA85\uD560 \uC218 \uC5C6\uC5B4 \uADF8\uC758 \uD559\uC124\uC740 \uD559\uACC4\uB85C\uBD80\uD130 \uC778\uC815\uBC1B\uC9C0 \uBABB\uD588\uB2E4. \uB300\uB959\uC744 \uC774\uB3D9\uC2DC\uD0A4\uB294 \uD798\uC740 \uBCA0\uAC8C\uB108 \uC774\uD6C4 \uB2E4\uB978 \uD559\uC790\uB4E4\uC5D0 \uC758\uD574 \uB9E8\uD2C0\uC758 \uB300\uB958\uB85C \uC81C\uC2DC\uB418\uC5C8\uC73C\uBA70, \uB300\uB959 \uC774\uB3D9\uC124\uC740 \uD310 \uAD6C\uC870\uB860\uC73C\uB85C \uBC1C\uC804\uB41C\uB2E4. \uB300\uB959 \uC774\uB3D9\uC758 \uC99D\uAC70 1. \n* \uC544\uD504\uB9AC\uCE74 \uB300\uB959\uC758 \uC11C\uD574\uC548\uACFC \uB0A8\uC544\uBA54\uB9AC\uCE74 \uB300\uB959\uC758 \uB3D9\uD574\uC548\uC758 \uD574\uC548\uC120\uC774 \uC720\uC0AC\uD558\uB2E4. 2. \n* \uAC19\uC740 \uC885\uC758 \uACE0\uC0DD\uBB3C\uC774 \uC11C\uB85C \uB2E4\uB978 \uB300\uB959\uC5D0\uC11C \uBC1C\uACAC\uB41C\uB2E4. 3. \n* \uC5EC\uB7EC \uB300\uB959\uC5D0 \uBD84\uD3EC\uD55C \uBE59\uD558\uC758 \uD754\uC801\uACFC \uC774\uB3D9 \uBC29\uD5A5\uC774 \uB300\uB959\uC744 \uD558\uB098\uB85C \uBAA8\uC73C\uBA74 \uC798 \uC124\uBA85\uB41C\uB2E4. 4. \n* \uBA40\uB9AC \uB5A8\uC5B4\uC9C4 \uB300\uB959\uC5D0\uC11C \uC9C0\uC9C8\uAD6C\uC870\uAC00 \uC5F0\uC18D\uC801\uC774\uACE0 \uAC19\uC740 \uC9C0\uCE35\uC758 \uBD84\uD3EC\uAC00 \uBC1C\uACAC\uB41C\uB2E4. 5. \n* \uC11C\uB85C \uBA40\uB9AC \uB5A8\uC5B4\uC9C4 \uC9C0\uC5ED\uC758 \uC11D\uD0C4\uCE35\uC774 \uC5F0\uACB0\uB418\uC5B4 \uC788\uB294 \uAC83\uC774 \uBCF4\uC774\uB294\uB370, \uC774\uAC83\uC740 \uD574\uB2F9 \uC9C0\uC5ED\uC774 \uBA3C \uACFC\uAC70\uC5D4 \uC800\uC704\uB3C4 \uC9C0\uC5ED\uC5D0\uC11C \uC11C\uB85C \uC5F0\uACB0\uB418\uC5B4 \uC788\uB358 \uC9C0\uC5ED\uC774\uB77C\uACE0 \uAC00\uC815\uD558\uBA74 \uC124\uBA85\uB41C\uB2E4. 6. \n* \uACE0\uC9C0\uC790\uAE30\uC801\uC73C\uB85C \uBD84\uC11D\uD558\uBA74 \uC815\uC790\uADF9\uACFC \uC5ED\uC790\uADF9\uC774 \uBC18\uBCF5\uB418\uB294 \uAC83\uC744 \uD1B5\uD574 \uC0C8\uB85C\uC6B4 \uC9C0\uAC01\uC774 \uC0DD\uAE30\uBA74\uC11C \uB300\uB959\uC774 \uC774\uB3D9\uD558\uACE0 \uC788\uB2E4\uB294 \uAC83\uC744 \uC54C \uC218 \uC788\uB2E4."@ko . . "Deriva dels continents"@ca . "La deriva dei continenti \u00E8 una teoria geologica secondo la quale i continenti migrano, spostandosi analogamente a zattere galleggianti sullo strato inferiore della crosta terrestre. Fu introdotta nel 1912 da Alfred Wegener, il quale credeva che i continenti in passato fossero tutti uniti in un unico blocco e che, nel corso dei secoli, con il movimento interno della Terra, si siano pian piano allontanati. Nella scienza moderna la teoria della deriva dei continenti \u00E8 stata migliorata e sostituita dalla teoria della tettonica delle placche. La litosfera \u00E8 suddivisa in tanti frammenti definiti placche, che si muovono in varie direzioni. Le placche sono circa venti e hanno dimensioni pi\u00F9 o meno diverse. Tra queste ve ne sono sette principali: \n* Placca nordamericana; \n* Placca sudamericana; \n* Placca africana; \n* Placca euroasiatica; \n* Placca indo-australiana; \n* Placca antartica; \n* Placca pacifica. Le placche si spostano molto lentamente, ma, nella scala dei tempi geologici, tali movimenti modificano il volto del nostro pianeta. Per comprendere le principali conseguenze dei movimenti delle placche, bisogna analizzare come quelle adiacenti interagiscano lungo i margini. \n* Margini divergenti: due placche adiacenti si allontanano l'una dall'altra. Allontanandosi, il magma che fuoriesce dal mantello solidifica e forma nuova litosfera. Questo processo, con il passare del tempo, pu\u00F2 portare alla formazioni di nuovi oceani. \n* Margini convergenti: due placche adiacenti si muovono l'una verso l'altra, Scontrandosi distruggono porzioni di litosfera che sprofonda nel mantello. Questo fenomeno \u00E8 noto come subduzione. \n* Margini trasformi: due placche si muovono in senso opposta l'una al fianco dell'altra. In questo modo non creano e non distruggono litosfera. Lungo questi margini, a causa dello sfregamento, vengono evidenziate le faglie. Il movimento di ogni placca \u00E8 indipendente, ma influenza il movimento di quelle adiacenti. Le forze che permettono alle placche di muoversi sono i moti convettivi. All'interno della litosfera il calore non \u00E8 distribuito in modo omogeneo: infatti, esistono zone pi\u00F9 calde e zone pi\u00F9 fredde. Il materiale pi\u00F9 caldo sale dall'interno del mantello verso la superficie e, quando si raffredda, affonda nuovamente. Alcune parti di questo materiale riescono, per\u00F2, ad attraversare la litosfera lacerandola. Il materiale che si raffredda d\u00E0 vita ad un nuovo strato di litosfera."@it . . . . "\u039C\u03B5\u03C4\u03B1\u03C4\u03CC\u03C0\u03B9\u03C3\u03B7 \u03C4\u03C9\u03BD \u03B7\u03C0\u03B5\u03AF\u03C1\u03C9\u03BD"@el . . . . . . "1123044501"^^ . . "\u0414\u0440\u0438\u0444\u0442\u043E\u0432\u0430 \u0433\u0456\u043F\u043E\u0442\u0435\u0437\u0430"@uk . . . "En geologia, la deriva dels continents \u00E9s el despla\u00E7ament de les masses continentals unes respecte a les altres. Aquesta teoria segons la qual el cient\u00EDfic alemany Alfred Wegener hi afirmava que els continents actuals van estar units fa uns 250 milions d'anys en un supercontinent al qual anomen\u00E0 Pangea, rodejat per un \u00FAnic oce\u00E0, Pantalassa. La forma moderna d'aquesta teoria va ser plantejada el 1912, per\u00F2 no va ser completament explicada fins a la formulaci\u00F3 de la teoria de les plaques tect\u00F2niques, cap als anys 60 del segle xx."@ca . "W\u0119dr\u00F3wka kontynent\u00F3w"@pl . "Kontinenta drivo"@eo . . . . . . . . "\u0627\u0644\u0627\u0646\u062C\u0631\u0627\u0641 \u0627\u0644\u0642\u0627\u0631\u064A \u0623\u0648 \u062A\u0632\u062D\u0632\u062D \u0627\u0644\u0642\u0627\u0631\u0627\u062A \u0623\u0648 \u0632\u062D\u0641 \u0627\u0644\u0642\u0627\u0631\u0627\u062A \u0647\u064A \u0646\u0634\u0627\u0637 \u062C\u064A\u0648\u0644\u0648\u062C\u064A \u062A\u0642\u0648\u0645 \u0628\u0647 \u0627\u0644\u0635\u0641\u0627\u0626\u062D \u0627\u0644\u062A\u0643\u062A\u0648\u0646\u064A\u0629 \u0644\u0644\u0643\u0631\u0629 \u0627\u0644\u0623\u0631\u0636\u064A\u0629 \u0648\u062A\u062A\u0645\u062B\u0644 \u0641\u064A \u062D\u0631\u0643\u0627\u062A \u062A\u0643\u062A\u0648\u0646\u064A\u0629 \u0625\u0645\u0627 \u0627\u0644\u062A\u0628\u0627\u0639\u062F \u0623\u0648 \u0627\u0644\u062A\u0642\u0627\u0631\u0628 \u0623\u0648 \u0627\u0644\u0627\u062D\u062A\u0643\u0627\u0643 \u0645\u0627 \u0628\u064A\u0646 \u0635\u0641\u064A\u062D\u062A\u064A\u0646\u060C \u0644\u062A\u0628\u062F\u0648 \u0648\u0643\u0623\u0646\u0647\u0627 \u062A\u062A\u0632\u062D\u0632\u062D \u0639\u0628\u0631 \u0642\u0627\u0639 \u0627\u0644\u0628\u062D\u0631. \u0643\u0627\u0646 \u0623\u0628\u0631\u0627\u0647\u0627\u0645 \u0623\u0648\u0631\u062A\u064A\u0644\u064A\u0648\u0633 \u0623\u0648\u0644 \u0645\u0646 \u0627\u0641\u062A\u0631\u0636 \u0623\u0646 \u0627\u0644\u0642\u0627\u0631\u0627\u062A \u0642\u062F \u062A\u0643\u0648\u0646 \u00AB\u062A\u062A\u0632\u062D\u0632\u062D\u00BB\u060C \u0648\u0630\u0644\u0643 \u0633\u0646\u0629 1596 \u0645. \u0625\u0644\u0627 \u0623\u0646 \u0647\u0630\u0647 \u0627\u0644\u0641\u0631\u0636\u064A\u0629 \u062A\u0637\u0648\u0631\u062A \u0648\u0627\u0643\u062A\u0645\u0644\u062A \u0628\u0634\u0643\u0644 \u0645\u0633\u062A\u0642\u0644 \u0639\u0644\u0649 \u064A\u062F \u0623\u0644\u0641\u0631\u064A\u062F \u0641\u064A\u062C\u0646\u0631 \u0633\u0646\u0629 1912 \u0645\u060C \u0644\u0643\u0646 \u0646\u0638\u0631\u064A\u062A\u0647 \u0631\u0641\u0636\u0647\u0627 \u0627\u0644\u0628\u0639\u0636 \u0644\u0639\u062F\u0645 \u0634\u0631\u062D\u0647\u0627 \u0644\u0644\u0622\u0644\u064A\u0629 \u0627\u0644\u062A\u064A \u062A\u0645 \u0628\u0647\u0627 \u0630\u0644\u0643\u060C \u0648\u0631\u0641\u0636\u0647\u0627 \u0627\u0644\u0628\u0639\u0636 \u0627\u0644\u0622\u062E\u0631 \u0644\u0645\u0627 \u062A\u0636\u0645\u0646\u062A\u0647 \u0645\u0646 \u0627\u0641\u062A\u0631\u0627\u0636\u0627\u062A \u0646\u0638\u0631\u064A\u0629. \u062B\u0645 \u0644\u0627\u0642\u062A \u0642\u0628\u0648\u0644\u0627\u064B \u0628\u0639\u062F \u0623\u0646 \u0642\u062F\u0645\u062A \u0646\u0638\u0631\u064A\u0629 \u0627\u0644\u0635\u0641\u0627\u0626\u062D \u0627\u0644\u062A\u0643\u062A\u0648\u0646\u064A\u0629 \u0634\u0631\u062D\u064B\u0627 \u0644\u0622\u0644\u064A\u0629 \u062D\u0631\u0643\u0629 \u0627\u0644\u0642\u0627\u0631\u0627\u062A."@ar . . "45768"^^ . . . . . . "Pergeseran benua"@in . "A teoria da deriva continental foi apresentada pelo ge\u00F3logo e meteorologista alem\u00E3o Alfred Wegener em 1913, com a publica\u00E7\u00E3o de sua obra cl\u00E1ssica \"A Origem dos Continentes e Oceanos\" (Die Entstehung der Kontinente und Ozeane). Wegener afirmava que os continentes, hoje separados por oceanos, estiveram unidos numa \u00FAnica massa de terra no passado, por ele denominado de Pangeia (do grego \"Terra \u00FAnica\"), do Carbon\u00EDfero superior, h\u00E1 cerca de 335 milh\u00F5es de anos, ao Jur\u00E1ssico superior, h\u00E1 cerca de 190 milh\u00F5es de anos, quando a Laur\u00E1sia (atuais Am\u00E9rica do Norte e Eur\u00E1sia) separou-se do Gondwana, que depois tamb\u00E9m dividiu-se, j\u00E1 no Cret\u00E1ceo inferior."@pt . "Deriva continental"@es . "An tsl\u00ED a ngluaiseann na hilchr\u00EDocha ar dhromchla an Domhain mar a bheadh cnoic ollmh\u00F3ra oighir iontu. S\u00EDobghluaiseacht na m\u00F3r-ranna, n\u00F3 teoiric na bpl\u00E1ta\u00ED teicteonacha, cur s\u00EDos eile ar an bhfeinim\u00E9an. Ceintim\u00E9adar n\u00F3 dh\u00F3 sa bhliain a ghluaiseann siad. Ar l\u00E9arsc\u00E1il an Domhain n\u00F3 an chruinneog, is l\u00E9ir go n-oiri\u00FAna\u00EDonn costa thoir Mheirice\u00E1 do ch\u00F3sta thiar na hEorpa is na hAfraice mar mh\u00EDreanna meara\u00ED. Ag cur san \u00E1ireamh na scairbheacha ilchr\u00EDochacha faoin bhfarraige, is fearr f\u00F3s an t-oiri\u00FAn\u00FA. De r\u00E9ir na teoirice seo, n\u00ED raibh ach meall amh\u00E1in tal\u00FAn ar Domhan, Pangaea, go luath i stair an Domhain timpeall 200 milli\u00FAn bliain \u00F3 shin. Scoilt Pangaea ina hilchr\u00EDocha de r\u00E9ir a ch\u00E9ile, ghluais siad seo amach \u00F3na ch\u00E9ile go dt\u00ED na h\u00E1iteanna a bhfuil siad inniu, agus t\u00E1 an ts\u00EDobghluaiseacht seo ag dul ar aghaidh an t-am ar fad. Luaitear an coincheap seo le Alfred Wegener a thairg ar dt\u00FAs \u00ED i 1912 agus a chuir s\u00EDos go cuimsitheach uirthi ina leabhar Die Entstehung der Kontinente und Ozeane (Bun\u00FAs na nIlchr\u00EDoch is na nAig\u00E9an, 1922), ach nach bhfuair taca\u00EDocht ar fi\u00FA tr\u00E1cht uirthi go dt\u00ED na 1960id\u00ED nuair a cuireadh teoiric na bpl\u00E1ta\u00ED teicteonacha chun cinn."@ga . . . "Hipotesis pergeseran benua (bahasa Inggris: continental drift) merupakan gagasan bahwa benua-benua di Bumi berpindah, terlihat seperti \"bergeser\" di dasar laut. Meski telah dikemukakan sejak abad ke-16, hipotesis ini baru disampaikan secara ilmiah oleh Alfred L. Wegener dalam buku berjudul The Origin of Continent and Oceans (1912). Isinya, benua tersusun dari batuan sial yang terapung pada batuan sima yang lebih besar berat jenisnya. Pergerakan benua itu menuju khatulistiwa dan juga ke arah barat. Wegener mendapati bahwa timur Amerika Selatan cocok jika dihubungkan dengan barat Afrika, memberi petunjuk bahwa semua benua dahulu pernah bersatu. Wegener mencari bebatuan dan fosil di dua sisi benua yang berbatasan dengan Samudra Atlantik untuk membuktikan hipotesisnya. Dia berhasil menemukan bukti-bukti tersebut tetapi tidak dapat menjelaskan mekanisme pergerakan benua dan gagasannya ditentang oleh organisasi seperti American Petroleum Society. Hipotesisnya tidak diacuhkan hingga kematiannya pada 1930. Hipotesis utamanya adalah di bumi pernah ada satu benua raksasa yang disebut Pangaea (artinya \"semua daratan\") yang dikelilingi oleh Panthalassa (\"semua lautan\"). Selanjutnya, 200 juta tahun yang lalu Pangaea pecah menjadi benua-benua yang lebih kecil yang kemudian bergerak menuju ke tempatnya seperti yang dijumpai saat ini. Beberapa ilmuwan dapat menerima konsep ini namun sebagian besar lainnya tidak dapat membayangkan bagaimana satu massa benua yang besar dapat mengapung di atas bumi yang padat dan mengapa ini terjadi. Pemahaman para ilmuwan pengkritik adalah bahwa gaya yang bekerja pada bumi adalah gaya vertikal. Tidaklah mungkin gaya vertikal ini mampu menyebabkan benua yang besar tersebut pecah. Pada masa itu belum dijumpai bukti-bukti yang meyakinkan. Wegener mengumpulkan bukti lainnya berupa kesamaan garis pantai, persamaaan fosil, struktur dan batuan. Namun, tetap saja usaha Wegener sia-sia karena Wagener tidak mampu menjelaskan dan meyakinkan para ahli bahwa gaya utama yang bekerja adalah gaya lateral bukan gaya vertikal. Pada tahun 1960-an, ditemukan bahwa magma berada di sepanjang garis lempeng tektonik, menandakan dasar laut bergeser seperti yang diperkirakan Wegener."@in . . . . "Kontinenteen jitoa"@eu . . . . . . "Kontinentaldrift \u00E4r f\u00F6rflyttningen av jordens kontinenter i f\u00F6rh\u00E5llande till varandra. Hypotesen att kontinenter \"driver\" lades f\u00F6rst fram av Abraham Ortelius 1596 och teorin utvecklades av Alfred Wegener 1912. N\u00E4r han lade fram teorin fanns det dock ingen f\u00F6rklaring till hur en s\u00E5dan drift skulle kunna uppst\u00E5, och det var inte f\u00F6rr\u00E4n utvecklingen av teorin om plattektoniken p\u00E5 1960-talet som en tillr\u00E4cklig geologisk f\u00F6rklaring till r\u00F6relserna kunde ges."@sv . . . . . . . . . "Hipotesis pergeseran benua (bahasa Inggris: continental drift) merupakan gagasan bahwa benua-benua di Bumi berpindah, terlihat seperti \"bergeser\" di dasar laut. Meski telah dikemukakan sejak abad ke-16, hipotesis ini baru disampaikan secara ilmiah oleh Alfred L. Wegener dalam buku berjudul The Origin of Continent and Oceans (1912). Isinya, benua tersusun dari batuan sial yang terapung pada batuan sima yang lebih besar berat jenisnya. Pergerakan benua itu menuju khatulistiwa dan juga ke arah barat."@in . "Continental drift is the hypothesis that the Earth's continents have moved over geologic time relative to each other, thus appearing to have \"drifted\" across the ocean bed. The idea of continental drift has been subsumed into the science of plate tectonics, which studies the movement of the continents as they ride on plates of the Earth's lithosphere."@en . . "\u0414\u0440\u0438\u0444\u0442\u043E\u0432\u0430 \u0433\u0456\u043F\u043E\u0442\u0435\u0437\u0430, \u0442\u0435\u043E\u0440\u0456\u044F \u0434\u0440\u0435\u0439\u0444\u0443 \u043C\u0430\u0442\u0435\u0440\u0438\u043A\u0456\u0432 (\u0440\u043E\u0441. \u0434\u0440\u0438\u0444\u0442\u043E\u0432\u0430\u044F \u0433\u0438\u043F\u043E\u0442\u0435\u0437\u0430, \u0430\u043D\u0433\u043B. drift hypothesis, \u043D\u0456\u043C. Drifthypothese) \u2014 \u0433\u0456\u043F\u043E\u0442\u0435\u0437\u0430 \u0433\u043E\u0440\u0438\u0437\u043E\u043D\u0442\u0430\u043B\u044C\u043D\u043E\u0433\u043E \u043F\u0435\u0440\u0435\u043C\u0456\u0449\u0435\u043D\u043D\u044F (\u0434\u0440\u0438\u0444\u0442\u0443, \u0430\u0431\u043E \u0434\u0440\u0435\u0439\u0444\u0443) \u043C\u0430\u0442\u0435\u0440\u0438\u043A\u0456\u0432 \u043F\u043E \u043F\u043B\u0430\u0441\u0442\u0438\u0447\u043D\u043E\u043C\u0443 \u0431\u0430\u0437\u0430\u043B\u044C\u0442\u043E\u0432\u043E\u043C\u0443 \u0448\u0430\u0440\u0443 \u0437\u0435\u043C\u043D\u043E\u0457 \u043A\u043E\u0440\u0438. \u0490\u0440\u0443\u043D\u0442\u0443\u0454\u0442\u044C\u0441\u044F \u043D\u0430 \u043F\u043E\u0434\u0456\u0431\u043D\u043E\u0441\u0442\u0456 \u043E\u0431\u0440\u0438\u0441\u0456\u0432 \u043C\u0430\u0442\u0435\u0440\u0438\u043A\u0456\u0432, \u0457\u0445 \u0433\u0435\u043E\u043B\u043E\u0433\u0456\u0447\u043D\u043E\u0457 \u0431\u0443\u0434\u043E\u0432\u0438 \u0439 \u043E\u0440\u0433\u0430\u043D\u0456\u0447\u043D\u0438\u0445 \u0440\u0435\u0448\u0442\u043E\u043A \u0443 \u043F\u043E\u0440\u043E\u0434\u0430\u0445. \u0417\u0430 \u0434\u0440\u0438\u0444\u0442\u043E\u0432\u043E\u044E \u0433\u0456\u043F\u043E\u0442\u0435\u0437\u043E\u044E \u0441\u0443\u0447\u0430\u0441\u043D\u0456 \u043C\u0430\u0442\u0435\u0440\u0438\u043A\u0438 \u0443\u0442\u0432\u043E\u0440\u044E\u044E\u0442\u044C\u0441\u044F \u0437 \u0454\u0434\u0438\u043D\u043E\u0433\u043E \u0441\u0443\u043F\u0435\u0440\u043C\u0430\u0442\u0435\u0440\u0438\u043A\u0430 \u2014 \u041F\u0430\u043D\u0433\u0435\u0457, \u044F\u043A\u0438\u0439 \u0440\u043E\u0437\u043A\u043E\u043B\u043E\u0432\u0441\u044F \u043D\u0430 \u043F\u043E\u0447\u0430\u0442\u043A\u0443 \u043C\u0435\u0437\u043E\u0437\u043E\u044E. \u0412\u0438\u0441\u0443\u043D\u0443\u0432 \u0446\u044E \u0433\u0456\u043F\u043E\u0442\u0435\u0437\u0443 \u0432 \u0434\u0440\u0443\u0433\u0456\u0439 \u043F\u043E\u043B\u043E\u0432\u0438\u043D\u0456 XIX \u0441\u0442. \u0440\u043E\u0441\u0456\u0439\u0441\u044C\u043A\u0438\u0439 \u0430\u0441\u0442\u0440\u043E\u043D\u043E\u043C-\u0430\u043C\u0430\u0442\u043E\u0440 \u0404. \u0412. \u0411\u0438\u0445\u0430\u043D\u043E\u0432; \u043D\u0430 \u043F\u043E\u0447\u0430\u0442\u043A\u0443 XX \u0441\u0442. \u0457\u0457 \u0440\u043E\u0437\u0432\u0438\u043D\u0443\u0432 \u043D\u0456\u043C\u0435\u0446\u044C\u043A\u0438\u0439 \u0433\u0435\u043E\u0444\u0456\u0437\u0438\u043A \u0410.\u0412\u0435\u0433\u0435\u043D\u0435\u0440. \u0423 60-\u0445 \u0440\u043E\u043A\u0430\u0445 XX \u0441\u0442. \u0434\u0440\u0438\u0444\u0442\u043E\u0432\u0430 \u0433\u0456\u043F\u043E\u0442\u0435\u0437\u0430 \u0434\u043E\u043F\u043E\u0432\u043D\u0435\u043D\u0430 \u043D\u0430 \u043E\u0441\u043D\u043E\u0432\u0456 \u043D\u043E\u0432\u0438\u0445 \u0434\u0430\u043D\u0438\u0445 \u0433\u0435\u043E\u0444\u0456\u0437\u0438\u0447\u043D\u0438\u0445 \u0434\u043E\u0441\u043B\u0456\u0434\u0436\u0435\u043D\u044C \u0456 \u0431\u0443\u0440\u0456\u043D\u043D\u044F \u0434\u043D\u0430 \u043E\u043A\u0435\u0430\u043D\u0456\u0432."@uk . . . . "Continentverschuiving, continentale drift of continentendrift (van het Engelse continental drift) is het geologische verschijnsel waarbij continenten bewegen. Deze bewegingen met snelheden van enkele centimeters per jaar kunnen sinds de opkomst van de satellietgeodesie ook daadwerkelijk gemeten worden. De beweging van continenten wordt veroorzaakt door platentektoniek."@nl . . "Kontinenteen jitoa masa kontinentalak elkarrekiko mugitu egiten direla esaten duen teoria da. Kontinenteak mugitzen zirela Abraham Orteliusek proposatu zuen eta Alfred Wegener meteorologo alemaniarrak teoria garatu zuen 1912an. Baina, 70. hamarkada arte, noiz plaken tektonikaren teoria proposatu zen, ez zen egoki azaldu jitoaren zergatia. Teoria berri hau Wegenerren teorian eta lurrazal ozeanikoaren hedapenean oinarritu zen."@eu . "Kontinenta drivo estas la movi\u011Do de la kontinentoj relative al la reciproka situo. La hipotezo, ke kontinentoj ne estas fiksaj, sed \u201Edrivas\u201C sur la surfaco de la tero, estis unuafoje proponita de Abraham Ortelius en 1596 kaj plene evoluigita de Alfred Wegener en 1912. La teorioj de Wegener siatempe ne estis akceptitaj, \u0109ar je tiu tempo neniu povis vidi ian \u201Emotoron\u201C por peli tiel gigantajn amasojn. Tiu ideo venis nur en la 1960-aj jaroj, kiam proponis la teorion de platotektoniko: la mem movi\u011Das: la \u201Enaskas\u201C novan kontinentan materialon kaj tiel dis\u015Dovas la kontinentajn platojn. \u0108i-artikolo donas superrigardon de la evoluo de la hipotezo pri kontinenta drivo \u011Dis 1950. Informojn pri la hodia\u016Da stato de la teorio donas artikolo platotektoniko.)"@eo . . 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"On appelle d\u00E9rive des continents l'ensemble des d\u00E9placements horizontaux des continents (ou des blocs continentaux) les uns par rapport aux autres. L'hypoth\u00E8se de la d\u00E9rive des continents a \u00E9t\u00E9 sugg\u00E9r\u00E9e d\u00E8s 1596. Elle a ensuite \u00E9t\u00E9 d\u00E9velopp\u00E9e et popularis\u00E9e, mais mal d\u00E9fendue, par Alfred Wegener en 1912. Apr\u00E8s la d\u00E9couverte des anomalies magn\u00E9tiques du fond des oc\u00E9ans dans les ann\u00E9es 1960, la d\u00E9rive des continents est devenue une r\u00E9alit\u00E9 attest\u00E9e par des observations directes et indirectes, et que l'on comprend dans le cadre plus g\u00E9n\u00E9ral de la th\u00E9orie de la tectonique des plaques."@fr . . . . . . "D\u00E9rive des continents"@fr . . . . . . "Kontinentaldrift \u00E4r f\u00F6rflyttningen av jordens kontinenter i f\u00F6rh\u00E5llande till varandra. Hypotesen att kontinenter \"driver\" lades f\u00F6rst fram av Abraham Ortelius 1596 och teorin utvecklades av Alfred Wegener 1912. N\u00E4r han lade fram teorin fanns det dock ingen f\u00F6rklaring till hur en s\u00E5dan drift skulle kunna uppst\u00E5, och det var inte f\u00F6rr\u00E4n utvecklingen av teorin om plattektoniken p\u00E5 1960-talet som en tillr\u00E4cklig geologisk f\u00F6rklaring till r\u00F6relserna kunde ges."@sv . . . . . "An tsl\u00ED a ngluaiseann na hilchr\u00EDocha ar dhromchla an Domhain mar a bheadh cnoic ollmh\u00F3ra oighir iontu. S\u00EDobghluaiseacht na m\u00F3r-ranna, n\u00F3 teoiric na bpl\u00E1ta\u00ED teicteonacha, cur s\u00EDos eile ar an bhfeinim\u00E9an. Ceintim\u00E9adar n\u00F3 dh\u00F3 sa bhliain a ghluaiseann siad. Ar l\u00E9arsc\u00E1il an Domhain n\u00F3 an chruinneog, is l\u00E9ir go n-oiri\u00FAna\u00EDonn costa thoir Mheirice\u00E1 do ch\u00F3sta thiar na hEorpa is na hAfraice mar mh\u00EDreanna meara\u00ED. Ag cur san \u00E1ireamh na scairbheacha ilchr\u00EDochacha faoin bhfarraige, is fearr f\u00F3s an t-oiri\u00FAn\u00FA. De r\u00E9ir na teoirice seo, n\u00ED raibh ach meall amh\u00E1in tal\u00FAn ar Domhan, Pangaea, go luath i stair an Domhain timpeall 200 milli\u00FAn bliain \u00F3 shin. Scoilt Pangaea ina hilchr\u00EDocha de r\u00E9ir a ch\u00E9ile, ghluais siad seo amach \u00F3na ch\u00E9ile go dt\u00ED na h\u00E1iteanna a bhfuil siad inniu, agus t\u00E1 an ts\u00EDobghluaiseacht seo ag"@ga . . . . . . . . . "Kontinent\u00E1ln\u00ED drift (pohyb sv\u011Btad\u00EDl\u016F) je teorie navr\u017Een\u00E1 v roce 1912 n\u011Bmeck\u00FDm meteorologem a geofyzikem Alfredem Wegenerem vysv\u011Btluj\u00EDc\u00ED vznik kontinent\u016F rozpadem p\u016Fvodn\u00EDho superkontinentu Pangea. P\u016Fvodn\u00ED my\u0161lenku, \u017Ee kontinenty do sebe \u201Ezapadaj\u00ED\u201C, kterou vyslovil u\u017E vl\u00E1msk\u00FD kartograf Abraham Ortelius (1527-1598), podpo\u0159il Wegener srovn\u00E1n\u00EDm geologick\u00FDch a paleontologick\u00FDch n\u00E1lez\u016F p\u0159edev\u0161\u00EDm z pob\u0159e\u017E\u00ED Afriky a Ji\u017En\u00ED Ameriky. Z\u00E1sadn\u00ED chybou Wegnerova pojet\u00ED bylo, \u017Ee pova\u017Eoval za hnac\u00ED s\u00EDlu pohybu kontinent\u016F Coriolisovu s\u00EDlu (ta je mnoha\u0159\u00E1dov\u011B nedostate\u010Dn\u00E1 pro takov\u00FD proces).Dnes je teorie kontinent\u00E1ln\u00EDho driftu sou\u010D\u00E1st\u00ED teorie deskov\u00E9 tektoniky, kter\u00E1 vysv\u011Btluje nejen pohyb kontinent\u016F, ale i dynamiku zemsk\u00E9ho pl\u00E1\u0161t\u011B. Teorie deskov\u00E9 tektoniky tvrd\u00ED, \u017Ee zemsk\u00E1 k\u016Fra je slo\u017Eena z tuh\u00FDch desek. Tyt"@cs . . "Kontinenteen jitoa masa kontinentalak elkarrekiko mugitu egiten direla esaten duen teoria da. Kontinenteak mugitzen zirela Abraham Orteliusek proposatu zuen eta Alfred Wegener meteorologo alemaniarrak teoria garatu zuen 1912an. Baina, 70. hamarkada arte, noiz plaken tektonikaren teoria proposatu zen, ez zen egoki azaldu jitoaren zergatia. Teoria berri hau Wegenerren teorian eta lurrazal ozeanikoaren hedapenean oinarritu zen."@eu . "La deriva continental es el desplazamiento de las masas continentales unas respecto a otras. Esta teor\u00EDa fue desarrollada en 1912 por el alem\u00E1n Alfred Wegener a partir de diversas observaciones emp\u00EDrico-racionales, pero no fue hasta la d\u00E9cada de 1960, con el desarrollo de la tect\u00F3nica de placas, cuando pudo explicarse de manera adecuada el movimiento de los continentes.\u200B"@es . "\uB300\uB959 \uC774\uB3D9\uC124"@ko . "A teoria da deriva continental foi apresentada pelo ge\u00F3logo e meteorologista alem\u00E3o Alfred Wegener em 1913, com a publica\u00E7\u00E3o de sua obra cl\u00E1ssica \"A Origem dos Continentes e Oceanos\" (Die Entstehung der Kontinente und Ozeane). Wegener afirmava que os continentes, hoje separados por oceanos, estiveram unidos numa \u00FAnica massa de terra no passado, por ele denominado de Pangeia (do grego \"Terra \u00FAnica\"), do Carbon\u00EDfero superior, h\u00E1 cerca de 335 milh\u00F5es de anos, ao Jur\u00E1ssico superior, h\u00E1 cerca de 190 milh\u00F5es de anos, quando a Laur\u00E1sia (atuais Am\u00E9rica do Norte e Eur\u00E1sia) separou-se do Gondwana, que depois tamb\u00E9m dividiu-se, j\u00E1 no Cret\u00E1ceo inferior. Muito tempo antes de Wegener, outros cientistas notaram este fato. A ideia da deriva continental surgiu pela primeira vez no final do s\u00E9culo XVI, com o trabalho do cart\u00F3grafo Abraham Ortelius. Na sua obra de , , Ortelius sugeriu que os continentes estiveram unidos no passado. A sua sugest\u00E3o teve origem apenas na similaridade geom\u00E9trica das costas atuais da Europa e \u00C1frica com as costas da Am\u00E9rica do Norte e do Sul; mesmo para os mapas relativamente imperfeitos da \u00E9poca, ficava evidente que havia um bom encaixe entre os continentes. A ideia, evidentemente, n\u00E3o passou de uma curiosidade que n\u00E3o produziu consequ\u00EAncias. Outro ge\u00F3grafo, Antonio Snider-Pellegrini, utilizou o mesmo m\u00E9todo de Ortelius para desenhar o seu mapa, com os continentes encaixados, em 1847. Como nenhuma prova adicional foi apresentada, al\u00E9m da considera\u00E7\u00E3o geom\u00E9trica, a ideia foi novamente esquecida. A similaridade entre os f\u00F3sseis encontrados em diferentes continentes, bem como entre forma\u00E7\u00F5es geol\u00F3gicas, levou alguns ge\u00F3logos do hemisf\u00E9rio sul a acreditar que todos os continentes j\u00E1 estiveram unidos, na forma de um supercontinente. A hip\u00F3tese da deriva continental tornou-se parte de uma teoria maior, a teoria da tect\u00F4nica de placas. Este artigo trata do desenvolvimento da teoria da deriva continental antes de 1959."@pt . . . "\u5927\u9646\u6F02\u79FB\u5B66\u8BF4"@zh . . . . . "Kontinentaldrift"@sv . . . . . "W\u0119dr\u00F3wka kontynent\u00F3w, epejroforeza (od stgr. \u1F24\u03C0\u03B5\u03B9\u03C1\u03BF\u03C2 \u0113peiros \u2013 \u2018l\u0105d, kontynent\u2019 oraz \u03C6\u03CC\u03C1\u03B7\u03C3\u03B9\u03C2 ph\u00F3r\u0113sis \u2013 \u2018noszenie\u2019) \u2013 ruch kontynent\u00F3w powoduj\u0105cy zmian\u0119 ich po\u0142o\u017Cenia wzgl\u0119dem siebie oraz wzgl\u0119dem biegun\u00F3w geograficznych i magnetycznych."@pl . 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"W\u0119dr\u00F3wka kontynent\u00F3w, epejroforeza (od stgr. \u1F24\u03C0\u03B5\u03B9\u03C1\u03BF\u03C2 \u0113peiros \u2013 \u2018l\u0105d, kontynent\u2019 oraz \u03C6\u03CC\u03C1\u03B7\u03C3\u03B9\u03C2 ph\u00F3r\u0113sis \u2013 \u2018noszenie\u2019) \u2013 ruch kontynent\u00F3w powoduj\u0105cy zmian\u0119 ich po\u0142o\u017Cenia wzgl\u0119dem siebie oraz wzgl\u0119dem biegun\u00F3w geograficznych i magnetycznych."@pl . . . "\u0646\u0638\u0631\u064A\u0629 \u0627\u0644\u0627\u0646\u062C\u0631\u0627\u0641 \u0627\u0644\u0642\u0627\u0631\u064A"@ar . . "En geologia, la deriva dels continents \u00E9s el despla\u00E7ament de les masses continentals unes respecte a les altres. Aquesta teoria segons la qual el cient\u00EDfic alemany Alfred Wegener hi afirmava que els continents actuals van estar units fa uns 250 milions d'anys en un supercontinent al qual anomen\u00E0 Pangea, rodejat per un \u00FAnic oce\u00E0, Pantalassa. La forma moderna d'aquesta teoria va ser plantejada el 1912, per\u00F2 no va ser completament explicada fins a la formulaci\u00F3 de la teoria de les plaques tect\u00F2niques, cap als anys 60 del segle xx."@ca . . . . . . . . . "Kontinentaldrift"@de . "Continental drift"@en . . . "Deriva continental"@pt . . . . . . "6056"^^ . . . "La deriva dei continenti \u00E8 una teoria geologica secondo la quale i continenti migrano, spostandosi analogamente a zattere galleggianti sullo strato inferiore della crosta terrestre. Fu introdotta nel 1912 da Alfred Wegener, il quale credeva che i continenti in passato fossero tutti uniti in un unico blocco e che, nel corso dei secoli, con il movimento interno della Terra, si siano pian piano allontanati. Nella scienza moderna la teoria della deriva dei continenti \u00E8 stata migliorata e sostituita dalla teoria della tettonica delle placche."@it . . . "\u0422\u0435\u043E\u0440\u0438\u044F \u0434\u0440\u0435\u0439\u0444\u0430 \u043C\u0430\u0442\u0435\u0440\u0438\u043A\u043E\u0432"@ru . . . . .