. "( \uB2E4\uB978 \uB73B\uC5D0 \uB300\uD574\uC11C\uB294 \uC735\uAE30 (\uC5F0\uD638) \uBB38\uC11C\uB97C \uCC38\uACE0\uD558\uC2ED\uC2DC\uC624.) \uC735\uAE30(\u9686\u8D77, uplift)\uB294 \uC790\uC5F0\uC801\uC778 \uC6D0\uC778\uC5D0 \uC758\uD574 \uC5B4\uB5A4 \uC9C0\uC5ED\uC758 \uB545\uB369\uC5B4\uB9AC\uAC00 \uC8FC\uBCC0\uC5D0 \uB300\uD558\uC5EC \uC0C1\uB300\uC801\uC73C\uB85C \uC0C1\uC2B9\uD558\uB294 \uC77C\uC744 \uB9D0\uD55C\uB2E4. \uC735\uAE30\uC640 \uBC18\uB300\uB85C \uB545\uC774 \uC8FC\uBCC0\uBCF4\uB2E4 \uB0AE\uC544\uC9C0\uB294 \uD604\uC0C1\uC740 \uCE68\uAC15\uC774\uB77C\uACE0 \uD55C\uB2E4. \uC735\uAE30\uC640 \uCE68\uAC15\uC740 \uC5F0\uC57D\uAD8C \uC704\uC5D0 \uB5A0 \uC788\uB294 \uC554\uC11D\uAD8C\uC774 \uD3C9\uD615\uC744 \uC720\uC9C0\uD558\uAE30 \uC704\uD574 \uB098\uD0C0\uB098\uB294 \uD604\uC0C1\uC774\uB2E4. \uC721\uC9C0\uC5D0 \uCEE4\uB2E4\uB780 \uBE59\uD558\uAC00 \uC788\uC744 \uB54C \uC628\uB3C4\uAC00 \uC62C\uB77C\uAC00\uBA74 \uBE59\uD558\uB294 \uBAA8\uB450 \uB179\uC544\uBC84\uB9B0\uB2E4. \uB179\uC544\uBC84\uB9B0 \uBE59\uD558 \uB54C\uBB38\uC5D0 \uADF8 \uC9C0\uC5ED\uC758 \uBC00\uB3C4\uB294 \uB0AE\uC544\uC9C0\uAC8C \uB418\uACE0 \uBC00\uB3C4\uAC00 \uB0AE\uC544\uC9C0\uBA74 \uD3C9\uD615\uC744 \uB9DE\uCD94\uAE30 \uC704\uD574 \uADF8 \uC9C0\uC5ED\uC740 \uC735\uAE30\uD558\uAC8C \uB41C\uB2E4. \uC774\uB7F0 \uC735\uAE30\uC640 \uCE68\uAC15\uC774 \uB098\uD0C0\uB098\uB294 \uC774\uC720\uB294 \uD06C\uAC8C\uB294 \uC870\uB959\uC6B4\uB3D9\uACFC \uC870\uC0B0\uC6B4\uB3D9\uC774 \uC788\uB2E4. \uC870\uB959\uC6B4\uB3D9\uACFC \uC870\uC0B0\uC6B4\uB3D9\uC73C\uB85C \uC554\uC11D\uAD8C\uC740 \uBCC0\uD615\uD55C\uB2E4. \uC774\uB54C \uBC1B\uB294 \uC555\uB825\uC758 \uC601\uD5A5\uC73C\uB85C \uC77C\uBD80 \uC9C0\uC5ED\uC740 \uC735\uAE30\uD558\uACE0 \uC77C\uBD80 \uC9C0\uC5ED\uC740 \uCE68\uAC15\uD558\uAC8C \uB41C\uB2E4. \uC774\uB7EC\uD55C \uC6C0\uC9C1\uC784 \uB9D0\uACE0\uB3C4 \uD574\uC218\uBA74\uC758 \uBCC0\uD654\uC5D0 \uC758\uD574\uC11C\uB3C4 \uC0DD\uAE34\uB2E4. \uC8FC\uBCC0\uC758 \uD574\uC218\uBA74\uC774 \uB0B4\uB824\uAC00\uBA74 \uC0C1\uB300\uC801\uC73C\uB85C \uC9C0\uCE35\uC740 \uC0C1\uC2B9\uD558\uB294 \uD6A8\uACFC\uAC00 \uC0DD\uAE34\uB2E4. \uC735\uAE30\uC758 \uC99D\uAC70\uB85C \uB300\uD45C\uC801\uC778 \uC608\uAC00 \uD574\uC548\uB2E8\uAD6C\uC778\uB370, \uB300\uD55C\uBBFC\uAD6D\uC5D0\uC11C\uB294 \uBD80\uC0B0\uC758 \uD0DC\uC885\uB300\uC640 \uC815\uB3D9\uC9C4\uC774 \uC720\uBA85\uD558\uB2E4."@ko . . . "1112388931"^^ . . . . . "La surrection ou soul\u00E8vement tectonique est le processus g\u00E9ologique d'\u00E9l\u00E9vation en altitude de roches par la tectonique des plaques. Si la vitesse de soul\u00E8vement est sup\u00E9rieure \u00E0 la vitesse de l'\u00E9rosion, il y a cr\u00E9ation de reliefs (orogen\u00E8se), sinon on a simplement apparition \u00E0 l'affleurement de terrains de plus en plus profonds (isostasie). Le soul\u00E8vement peut ainsi \u00EAtre orog\u00E9nique ou isostatique. Il s'agit d'un cas particulier d'ascendance. L'oppos\u00E9 du soul\u00E8vement est la subsidence."@fr . . . "\uC735\uAE30"@ko . "Hebung ist in den Geowissenschaften eine Vertikalbewegung im Zusammenhang mit endogenen Kr\u00E4ften des Erdk\u00F6rpers \u2013 etwa bei der Gebirgsbildung \u2013 und geht auf unterirdische Bewegungen wie Mantelkonvektion und Vulkanismus oder auf Keilwirkungen zur\u00FCck sowie auf Isostasie, den Kr\u00E4fteausgleich der Landmassen \u00FCber dem fl\u00FCssigen Erdmantel. Hebe- und Senkeffekte sind Teil des Bradyseismos, der langsamen Erdbewegung."@de . . . . . . . . . . "\u6784\u9020\u62AC\u5347\u6307\u5F52\u56E0\u4E8E\u677F\u5757\u6784\u9020\u7684\u4E8E\u5730\u8868\u53D1\u751F\u7684\u5730\u8D28\u62AC\u5347\u3002\u867D\u7136\u5730\u58F3\u5747\u8861\u53CD\u6620\u4E5F\u5F88\u91CD\u8981\uFF0C\u4F46\u4E00\u4E2A\u5730\u533A\u5E73\u5747\u6D77\u62D4\u7684\u589E\u52A0\u53EA\u80FD\u53D1\u751F\u5728\u5730\u58F3\u589E\u539A\u7684\u6784\u9020\u8FC7\u7A0B\u4E2D(\u5982\u9020\u5C71\u8FD0\u52A8)\u3001\u5730\u58F3\u4E0E\u4E0B\u65B9\u5730\u5E54\u7684\u5BC6\u5EA6\u5206\u5E03\u53D8\u5316\u53CA\u56E0\u521A\u6027\u5CA9\u77F3\u5708\u7684\u5F2F\u66F2\u800C\u4EA7\u751F\u7684\u5F39\u6027\u652F\u6491\u3002 \u8FD8\u5E94\u8003\u8651\u5265\u8680\u4F5C\u7528\uFF08\u78E8\u635F\u5730\u7403\u8868\u9762\u7684\u8FC7\u7A0B\uFF09\u7684\u5F71\u54CD\u3002\u672C\u4E13\u9898\u8303\u56F4\u5185\uFF0C\u9686\u8D77\u4E0E\u5265\u8680\u662F\u6709\u5173\u7684\uFF0C\u56E0\u4E3A\u5265\u8680\u80FD\u4F7F\u5730\u4E0B\u5CA9\u77F3\u66F4\u63A5\u8FD1\u5730\u8868\u3002\u8FD9\u4E2A\u8FC7\u7A0B\u53EF\u4EE5\u5C06\u5927\u7684\u8D1F\u8377\u4ECE\u9AD8\u5904\u91CD\u65B0\u5206\u914D\u5230\u5730\u5F62\u8F83\u4F4E\u7684\u5730\u533A--\u4ECE\u800C\u4FC3\u8FDB\u5265\u8680\u5730\u533A\u7684\u7B49\u9759\u529B\u53CD\u5E94\uFF08\u53EF\u80FD\u5BFC\u81F4\u5C40\u90E8\u57FA\u5CA9\u9686\u8D77\uFF09\u3002\u5730\u8D28\u5B66\u5BB6\u53EF\u901A\u8FC7\u538B\u529B-\u6E29\u5EA6\u7814\u7A76\u6765\u4F30\u8BA1\u5265\u8680\u53D1\u751F\u7684\u65F6\u95F4\u3001\u89C4\u6A21\u548C\u901F\u5EA6\u3002"@zh . . . . . . . . . . . . . . . "Landh\u00F6jning \u00E4r en h\u00F6jning av jordskorpan j\u00E4mf\u00F6rt med havsniv\u00E5n. Den kan vara av olika slag, i omr\u00E5den som varit t\u00E4ckta av inlandsis, bland annat i Skandinavien och Kanada, f\u00F6rekommer postglacial landh\u00F6jning. I andra omr\u00E5den, d\u00E4r jordskorpans plattor m\u00F6ts, f\u00F6rekommer orogenisk landh\u00F6jning. Motsatsen \u00E4r lands\u00E4nkning som resulterar i en minskning av h\u00F6jden. \u00C4ven om landh\u00F6jningen handlar om en h\u00F6jning av landytan i f\u00F6rh\u00E5llande till havsytan p\u00E5verkas kustlinjen \u00E4ven av att havsniv\u00E5n v\u00E4xlat, vilket g\u00F6r att arkeologer och andra som studerar strandniv\u00E5er ist\u00E4llet anv\u00E4nder begreppet strandf\u00F6rskjutning."@sv . . "Levantamiento (geolog\u00EDa)"@es . . . "\u6784\u9020\u62AC\u5347"@zh . "Hebung ist in den Geowissenschaften eine Vertikalbewegung im Zusammenhang mit endogenen Kr\u00E4ften des Erdk\u00F6rpers \u2013 etwa bei der Gebirgsbildung \u2013 und geht auf unterirdische Bewegungen wie Mantelkonvektion und Vulkanismus oder auf Keilwirkungen zur\u00FCck sowie auf Isostasie, den Kr\u00E4fteausgleich der Landmassen \u00FCber dem fl\u00FCssigen Erdmantel. Hebe- und Senkeffekte sind Teil des Bradyseismos, der langsamen Erdbewegung."@de . . . . . . . . . "Tektona levo estas la parto de la totala geologia levo de la \u0109efa surfaco de la Tero kiu ne estas atribuebla simple al izostaza reago al ebeni\u011Do. En geologio, levo estas la alti\u011Do de la grundo en la tuto de regiono pro efiko de fortoj \u0109u tektonaj a\u016D izostaza. Sekvo estas falto kaj kreado de montaro (Orogenezo)."@eo . . "Tektona levo"@eo . . . . "\u0627\u0644\u0631\u0641\u0639 \u0627\u0644\u062A\u0643\u062A\u0648\u0646\u064A \u0623\u0648 \u0627\u0644\u062A\u0642\u0628\u0628 \u0627\u0644\u062A\u0643\u062A\u0648\u0646\u064A \u0647\u0648 \u062C\u0632\u0621 \u0645\u0646 \u0627\u0644\u062A\u0642\u0628\u0628 \u0623\u0648 \u0627\u0644\u0625\u0631\u062A\u0641\u0627\u0639 \u0627\u0644\u062C\u064A\u0648\u0644\u0648\u062C\u064A \u0644\u0633\u0637\u062D \u0627\u0644\u0623\u0631\u0636 \u0648\u0627\u0644\u0630\u064A \u0644\u0645 \u064A\u062D\u062F\u062B \u0646\u062A\u064A\u062C\u0629 \u0627\u0633\u062A\u062C\u0627\u0628\u0629 \u062A\u0648\u0627\u0632\u0646\u064A\u0629 \u0644\u062D\u0627\u0644\u0629 \u0627\u0644\u062A\u0641\u0631\u064A\u063A. \u0641\u064A \u062D\u064A\u0646 \u0623\u0646 \u0627\u0644\u0625\u0633\u062A\u062C\u0627\u0628\u0629 \u0627\u0644\u0645\u062A\u0648\u0627\u0632\u0646\u0629 \u0645\u0647\u0645\u0629\u060C \u0641\u0625\u0646 \u0627\u0644\u0632\u064A\u0627\u062F\u0629 \u0641\u064A \u0645\u062A\u0648\u0633\u0637 \u0627\u0644\u0623\u0631\u062A\u0641\u0627\u0639 \u0644\u0645\u0646\u0637\u0642\u0629 \u0645\u0627 \u064A\u0645\u0643\u0646 \u0623\u0646 \u062A\u062D\u062F\u062B \u0641\u0642\u0637 \u0625\u0633\u062A\u062C\u0627\u0628\u0629\u064B \u0644\u0644\u0639\u0645\u0644\u064A\u0627\u062A \u0627\u0644\u062A\u0643\u062A\u0648\u0646\u064A\u0629 (\u0645\u062B\u0644 \u0623\u062D\u062F\u0627\u062B \u0628\u0646\u0627\u0621 \u0627\u0644\u062C\u0628\u0627\u0644)\u060C \u0648\u0627\u0644\u062A\u063A\u064A\u0631\u0627\u062A \u0641\u064A \u062A\u0648\u0632\u064A\u0639 \u0643\u062B\u0627\u0641\u0629 \u0627\u0644\u0642\u0634\u0631\u0629 \u0648\u0627\u0644\u0648\u0634\u0627\u062D \u0627\u0644\u0643\u0627\u0645\u0646\u0629\u060C \u0648\u062F\u0639\u0645 \u0627\u0644\u0627\u0646\u062D\u0646\u0627\u0621 \u0628\u0633\u0628\u0628 \u0637\u064A \u0627\u0644\u063A\u0644\u0627\u0641 \u0627\u0644\u0635\u062E\u0631\u064A \u0627\u0644\u0635\u0644\u0628. \u064A\u0624\u062F\u064A \u0627\u0644\u0625\u0631\u062A\u0641\u0627\u0639 \u0627\u0644\u062A\u0643\u062A\u0648\u0646\u064A \u0625\u0644\u0649 (\u0639\u0645\u0644\u064A\u0627\u062A \u062A\u0622\u0643\u0644 \u0633\u0637\u062D \u0627\u0644\u0623\u0631\u0636) \u0639\u0646 \u0637\u0631\u064A\u0642 \u0631\u0641\u0639 \u0627\u0644\u0635\u062E\u0648\u0631 \u0627\u0644\u0645\u062F\u0641\u0648\u0646\u0629 \u0628\u0627\u0644\u0642\u0631\u0628 \u0645\u0646 \u0627\u0644\u0633\u0637\u062D. \u064A\u0645\u0643\u0646 \u0644\u0647\u0630\u0647 \u0627\u0644\u0639\u0645\u0644\u064A\u0629 \u0625\u0639\u0627\u062F\u0629 \u062A\u0648\u0632\u064A\u0639 \u0627\u0644\u0623\u062D\u0645\u0627\u0644 \u0627\u0644\u0643\u0628\u064A\u0631\u0629 \u0645\u0646 \u0645\u0646\u0637\u0642\u0629 \u0645\u0631\u062A\u0641\u0639\u0629 \u0625\u0644\u0649 \u0645\u0646\u0637\u0642\u0629 \u0645\u0646\u062E\u0641\u0636\u0629 \u0637\u0628\u0648\u063A\u0631\u0627\u0641\u064A\u064B\u0627 \u0623\u064A\u0636\u064B\u0627 - \u0648\u0628\u0627\u0644\u062A\u0627\u0644\u064A \u062A\u0639\u0632\u064A\u0632 \u0627\u0633\u062A\u062C\u0627\u0628\u0629 \u0645\u062A\u0648\u0627\u0632\u0646\u0629 \u0641\u064A \u0645\u0646\u0637\u0642\u0629 \u0627\u0644\u062A\u0639\u0631\u064A\u0629 (\u0648\u0627\u0644\u062A\u064A \u064A\u0645\u0643\u0646 \u0623\u0646 \u062A\u0633\u0628\u0628 \u0631\u0641\u0639 \u0627\u0644\u0635\u062E\u0648\u0631 \u0627\u0644\u0645\u062D\u0644\u064A\u0629). \u064A\u0645\u0643\u0646 \u062A\u0642\u062F\u064A\u0631 \u062A\u0648\u0642\u064A\u062A \u0648\u062D\u062C\u0645 \u0648\u0645\u0639\u062F\u0644 \u0627\u0644\u062A\u0639\u0631\u064A\u0629 \u0628\u0648\u0627\u0633\u0637\u0629 \u0627\u0644\u062C\u064A\u0648\u0644\u0648\u062C\u064A\u064A\u0646 \u0628\u0627\u0633\u062A\u062E\u062F\u0627\u0645 \u062F\u0631\u0627\u0633\u0627\u062A \u0627\u0644\u0636\u063A\u0637 \u0648\u062F\u0631\u062C\u0629 \u0627\u0644\u062D\u0631\u0627\u0631\u0629."@ar . "Tectonic uplift"@en . "Tektonische opheffing (Engels: uplift) is in de geologie het proces waarbij de bodem omhoog beweegt als gevolg van tektoniek, bewegingen in de aardkorst. Door tektonische processen wordt gesteente zo dichter naar de oppervlakte gebracht. Dit is het tegengestelde proces van tektonische daling, waarbij sediment of gesteente juist neerwaarts beweegt, hetgeen meestal samengaat met begraving."@nl . "Surrection (g\u00E9ologie)"@fr . . . . . . . . "Soerguimento tect\u00F3nico (portugu\u00EAs europeu) ou soerguimento tect\u00F4nico (portugu\u00EAs brasileiro) \u00E9 um processo geol\u00F3gico normalmente causado devido \u00E0 tect\u00F3nica de placas. Neste processo, uma por\u00E7\u00E3o da crosta terrestre \u00E9 elevada da sua posi\u00E7\u00E3o original. O oposto deste fen\u00F3meno \u00E9 a subsid\u00EAncia, da qual resulta a diminui\u00E7\u00E3o da eleva\u00E7\u00E3o. O levantamento pode ter origem orog\u00E9nica ou isost\u00E1tica."@pt . . . . . . . . . . "Tektonische opheffing"@nl . . "En geolog\u00EDa, un levantamiento[cita requerida] es la elevaci\u00F3n del suelo en un \u00E1rea por efecto de fuerzas tect\u00F3nicas o isost\u00E1ticas. Las dos causas principales de las deformaciones positivas (hacia arriba) de un terreno son tanto el plegamiento, debido a empujes laterales del contenido de un geosinclinal, cuya consecuencia es la formaci\u00F3n de un sistema monta\u00F1oso; como al reajuste isost\u00E1tico debido a que todo un compartimiento de la corteza terrestre ha perdido una parte importante de su peso al fundirse el hielo de los inlandsis cuaternarios, Como sucedi\u00F3 en los Acantilados de Dover[cita requerida] o bien por haber sufrido una erosi\u00F3n muy significativa."@es . . . . . . . "La surrection ou soul\u00E8vement tectonique est le processus g\u00E9ologique d'\u00E9l\u00E9vation en altitude de roches par la tectonique des plaques. Si la vitesse de soul\u00E8vement est sup\u00E9rieure \u00E0 la vitesse de l'\u00E9rosion, il y a cr\u00E9ation de reliefs (orogen\u00E8se), sinon on a simplement apparition \u00E0 l'affleurement de terrains de plus en plus profonds (isostasie). Le soul\u00E8vement peut ainsi \u00EAtre orog\u00E9nique ou isostatique. Il s'agit d'un cas particulier d'ascendance. L'oppos\u00E9 du soul\u00E8vement est la subsidence. Le soul\u00E8vement orog\u00E9nique est le r\u00E9sultat de la collision des plaques tectoniques et aboutit \u00E0 des cha\u00EEnes de montagnes ou \u00E0 un modeste soul\u00E8vement d'une large r\u00E9gion. L'Himalaya, par exemple a \u00E9t\u00E9 (et est encore) form\u00E9e par la collision de deux plaques continentales : la plaque indienne et la plaque eurasiatique. Cette collision a produit le plateau tib\u00E9tain, ainsi que l'Himalaya et les cha\u00EEnes associ\u00E9es. Le plateau du Colorado avec ses spectaculaires canyons donc le fameux Grand Canyon est aussi le r\u00E9sultat d'un large soul\u00E8vement suivi par l'\u00E9rosion fluviale. Le Massif central en France est une cha\u00EEne de montagne ancienne (orogen\u00E8se varisque) qui a subi un soul\u00E8vement tectonique, li\u00E9 \u00E0 l'orogen\u00E8se alpine, on dit que le massif a \u00E9t\u00E9 \u00AB rajeuni \u00BB. Le soul\u00E8vement isostatique inclut le soul\u00E8vement progressif suivant la rapide \u00E9rosion, enlevant de la mati\u00E8re \u00E0 une cha\u00EEne de montagne. Le sol monte \u00E0 la suite de son all\u00E9gement. Un autre exemple de soul\u00E8vement isostatique est le rebond post-glaciaire qui suit la fonte des glaciers continentaux et des calottes glaciaires. La baie d'Hudson et les Grands Lacs au Canada sont actuellement en train de se soulever, en r\u00E9ponse \u00E0 la fonte des calottes glaciaires il y a 10 000 ans. Ce m\u00EAme effet s'observe en p\u00E9ninsule Scandinave, o\u00F9 par exemple la Haute C\u00F4te s'est \u00E9lev\u00E9e de 285 m depuis la derni\u00E8re glaciation."@fr . "Tectonic uplift is the geologic uplift of Earth's surface that is attributed to plate tectonics. While isostatic response is important, an increase in the mean elevation of a region can only occur in response to tectonic processes of crustal thickening (such as mountain building events), changes in the density distribution of the crust and underlying mantle, and flexural support due to the bending of rigid lithosphere."@en . "Tectonic uplift is the geologic uplift of Earth's surface that is attributed to plate tectonics. While isostatic response is important, an increase in the mean elevation of a region can only occur in response to tectonic processes of crustal thickening (such as mountain building events), changes in the density distribution of the crust and underlying mantle, and flexural support due to the bending of rigid lithosphere. Tectonic uplift results in denudation (processes that wear away the earth's surface) by raising buried rocks closer to the surface. This process can redistribute large loads from an elevated region to a topographically lower area as well \u2013 thus promoting an isostatic response in the region of denudation (which can cause local bedrock uplift). The timing, magnitude, and rate of denudation can be estimated by geologists using pressure-temperature studies."@en . . . . . . . . . . . . . . . . . . . . "Hebung (Geologie)"@de . . . . . . . "12218"^^ . . "\u0631\u0641\u0639 \u062A\u0643\u062A\u0648\u0646\u064A"@ar . . . . . "Tektona levo estas la parto de la totala geologia levo de la \u0109efa surfaco de la Tero kiu ne estas atribuebla simple al izostaza reago al ebeni\u011Do. En geologio, levo estas la alti\u011Do de la grundo en la tuto de regiono pro efiko de fortoj \u0109u tektonaj a\u016D izostaza. Sekvo estas falto kaj kreado de montaro (Orogenezo)."@eo . "Landh\u00F6jning \u00E4r en h\u00F6jning av jordskorpan j\u00E4mf\u00F6rt med havsniv\u00E5n. Den kan vara av olika slag, i omr\u00E5den som varit t\u00E4ckta av inlandsis, bland annat i Skandinavien och Kanada, f\u00F6rekommer postglacial landh\u00F6jning. I andra omr\u00E5den, d\u00E4r jordskorpans plattor m\u00F6ts, f\u00F6rekommer orogenisk landh\u00F6jning. Motsatsen \u00E4r lands\u00E4nkning som resulterar i en minskning av h\u00F6jden. \u00C4ven om landh\u00F6jningen handlar om en h\u00F6jning av landytan i f\u00F6rh\u00E5llande till havsytan p\u00E5verkas kustlinjen \u00E4ven av att havsniv\u00E5n v\u00E4xlat, vilket g\u00F6r att arkeologer och andra som studerar strandniv\u00E5er ist\u00E4llet anv\u00E4nder begreppet strandf\u00F6rskjutning."@sv . . . . . "Tektonische opheffing (Engels: uplift) is in de geologie het proces waarbij de bodem omhoog beweegt als gevolg van tektoniek, bewegingen in de aardkorst. Door tektonische processen wordt gesteente zo dichter naar de oppervlakte gebracht. Dit is het tegengestelde proces van tektonische daling, waarbij sediment of gesteente juist neerwaarts beweegt, hetgeen meestal samengaat met begraving. In de geologie worden gebieden onderscheiden waar de aardkorst zich uitrekt (extensie) en gebieden waar in de aardkorst verdikking door compressie plaatsvindt. Compressie en extensie zijn het gevolg van spanningen in de aardkorst, die bijvoorbeeld kunnen worden veroorzaakt door bewegingen van tektonische platen, vulkanisme, of het accumuleren van grote hoeveelheden sediment in een bepaald gebied. Als de korst uitrekt zal (door het principe van isostasie) de bodem dalen, als de korst verdikt zal tektonische opheffing plaatsvinden. Voorbeelden van gebieden waar tektonische opheffing plaatsvond of -vindt zijn de Ardennen, de Eifel en de Vogezen. Hier is een deel van de Europese plaat omhoog bewogen ten opzichte van andere delen, zoals de Boven-Rijnslenk in Zuid-Duitsland of het Noordzeebekken."@nl . "1415891"^^ . . "En geolog\u00EDa, un levantamiento[cita requerida] es la elevaci\u00F3n del suelo en un \u00E1rea por efecto de fuerzas tect\u00F3nicas o isost\u00E1ticas. Las dos causas principales de las deformaciones positivas (hacia arriba) de un terreno son tanto el plegamiento, debido a empujes laterales del contenido de un geosinclinal, cuya consecuencia es la formaci\u00F3n de un sistema monta\u00F1oso; como al reajuste isost\u00E1tico debido a que todo un compartimiento de la corteza terrestre ha perdido una parte importante de su peso al fundirse el hielo de los inlandsis cuaternarios, Como sucedi\u00F3 en los Acantilados de Dover[cita requerida] o bien por haber sufrido una erosi\u00F3n muy significativa."@es . . . 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"\u6784\u9020\u62AC\u5347\u6307\u5F52\u56E0\u4E8E\u677F\u5757\u6784\u9020\u7684\u4E8E\u5730\u8868\u53D1\u751F\u7684\u5730\u8D28\u62AC\u5347\u3002\u867D\u7136\u5730\u58F3\u5747\u8861\u53CD\u6620\u4E5F\u5F88\u91CD\u8981\uFF0C\u4F46\u4E00\u4E2A\u5730\u533A\u5E73\u5747\u6D77\u62D4\u7684\u589E\u52A0\u53EA\u80FD\u53D1\u751F\u5728\u5730\u58F3\u589E\u539A\u7684\u6784\u9020\u8FC7\u7A0B\u4E2D(\u5982\u9020\u5C71\u8FD0\u52A8)\u3001\u5730\u58F3\u4E0E\u4E0B\u65B9\u5730\u5E54\u7684\u5BC6\u5EA6\u5206\u5E03\u53D8\u5316\u53CA\u56E0\u521A\u6027\u5CA9\u77F3\u5708\u7684\u5F2F\u66F2\u800C\u4EA7\u751F\u7684\u5F39\u6027\u652F\u6491\u3002 \u8FD8\u5E94\u8003\u8651\u5265\u8680\u4F5C\u7528\uFF08\u78E8\u635F\u5730\u7403\u8868\u9762\u7684\u8FC7\u7A0B\uFF09\u7684\u5F71\u54CD\u3002\u672C\u4E13\u9898\u8303\u56F4\u5185\uFF0C\u9686\u8D77\u4E0E\u5265\u8680\u662F\u6709\u5173\u7684\uFF0C\u56E0\u4E3A\u5265\u8680\u80FD\u4F7F\u5730\u4E0B\u5CA9\u77F3\u66F4\u63A5\u8FD1\u5730\u8868\u3002\u8FD9\u4E2A\u8FC7\u7A0B\u53EF\u4EE5\u5C06\u5927\u7684\u8D1F\u8377\u4ECE\u9AD8\u5904\u91CD\u65B0\u5206\u914D\u5230\u5730\u5F62\u8F83\u4F4E\u7684\u5730\u533A--\u4ECE\u800C\u4FC3\u8FDB\u5265\u8680\u5730\u533A\u7684\u7B49\u9759\u529B\u53CD\u5E94\uFF08\u53EF\u80FD\u5BFC\u81F4\u5C40\u90E8\u57FA\u5CA9\u9686\u8D77\uFF09\u3002\u5730\u8D28\u5B66\u5BB6\u53EF\u901A\u8FC7\u538B\u529B-\u6E29\u5EA6\u7814\u7A76\u6765\u4F30\u8BA1\u5265\u8680\u53D1\u751F\u7684\u65F6\u95F4\u3001\u89C4\u6A21\u548C\u901F\u5EA6\u3002"@zh . . . . "( \uB2E4\uB978 \uB73B\uC5D0 \uB300\uD574\uC11C\uB294 \uC735\uAE30 (\uC5F0\uD638) \uBB38\uC11C\uB97C \uCC38\uACE0\uD558\uC2ED\uC2DC\uC624.) \uC735\uAE30(\u9686\u8D77, uplift)\uB294 \uC790\uC5F0\uC801\uC778 \uC6D0\uC778\uC5D0 \uC758\uD574 \uC5B4\uB5A4 \uC9C0\uC5ED\uC758 \uB545\uB369\uC5B4\uB9AC\uAC00 \uC8FC\uBCC0\uC5D0 \uB300\uD558\uC5EC \uC0C1\uB300\uC801\uC73C\uB85C \uC0C1\uC2B9\uD558\uB294 \uC77C\uC744 \uB9D0\uD55C\uB2E4. \uC735\uAE30\uC640 \uBC18\uB300\uB85C \uB545\uC774 \uC8FC\uBCC0\uBCF4\uB2E4 \uB0AE\uC544\uC9C0\uB294 \uD604\uC0C1\uC740 \uCE68\uAC15\uC774\uB77C\uACE0 \uD55C\uB2E4. \uC735\uAE30\uC640 \uCE68\uAC15\uC740 \uC5F0\uC57D\uAD8C \uC704\uC5D0 \uB5A0 \uC788\uB294 \uC554\uC11D\uAD8C\uC774 \uD3C9\uD615\uC744 \uC720\uC9C0\uD558\uAE30 \uC704\uD574 \uB098\uD0C0\uB098\uB294 \uD604\uC0C1\uC774\uB2E4. \uC721\uC9C0\uC5D0 \uCEE4\uB2E4\uB780 \uBE59\uD558\uAC00 \uC788\uC744 \uB54C \uC628\uB3C4\uAC00 \uC62C\uB77C\uAC00\uBA74 \uBE59\uD558\uB294 \uBAA8\uB450 \uB179\uC544\uBC84\uB9B0\uB2E4. \uB179\uC544\uBC84\uB9B0 \uBE59\uD558 \uB54C\uBB38\uC5D0 \uADF8 \uC9C0\uC5ED\uC758 \uBC00\uB3C4\uB294 \uB0AE\uC544\uC9C0\uAC8C \uB418\uACE0 \uBC00\uB3C4\uAC00 \uB0AE\uC544\uC9C0\uBA74 \uD3C9\uD615\uC744 \uB9DE\uCD94\uAE30 \uC704\uD574 \uADF8 \uC9C0\uC5ED\uC740 \uC735\uAE30\uD558\uAC8C \uB41C\uB2E4. \uC774\uB7F0 \uC735\uAE30\uC640 \uCE68\uAC15\uC774 \uB098\uD0C0\uB098\uB294 \uC774\uC720\uB294 \uD06C\uAC8C\uB294 \uC870\uB959\uC6B4\uB3D9\uACFC \uC870\uC0B0\uC6B4\uB3D9\uC774 \uC788\uB2E4. \uC870\uB959\uC6B4\uB3D9\uACFC \uC870\uC0B0\uC6B4\uB3D9\uC73C\uB85C \uC554\uC11D\uAD8C\uC740 \uBCC0\uD615\uD55C\uB2E4. \uC774\uB54C \uBC1B\uB294 \uC555\uB825\uC758 \uC601\uD5A5\uC73C\uB85C \uC77C\uBD80 \uC9C0\uC5ED\uC740 \uC735\uAE30\uD558\uACE0 \uC77C\uBD80 \uC9C0\uC5ED\uC740 \uCE68\uAC15\uD558\uAC8C \uB41C\uB2E4. \uC774\uB7EC\uD55C \uC6C0\uC9C1\uC784 \uB9D0\uACE0\uB3C4 \uD574\uC218\uBA74\uC758 \uBCC0\uD654\uC5D0 \uC758\uD574\uC11C\uB3C4 \uC0DD\uAE34\uB2E4. \uC8FC\uBCC0\uC758 \uD574\uC218\uBA74\uC774 \uB0B4\uB824\uAC00\uBA74 \uC0C1\uB300\uC801\uC73C\uB85C \uC9C0\uCE35\uC740 \uC0C1\uC2B9\uD558\uB294 \uD6A8\uACFC\uAC00 \uC0DD\uAE34\uB2E4. \uC735\uAE30\uC758 \uC99D\uAC70\uB85C \uB300\uD45C\uC801\uC778 \uC608\uAC00 \uD574\uC548\uB2E8\uAD6C\uC778\uB370, \uB300\uD55C\uBBFC\uAD6D\uC5D0\uC11C\uB294 \uBD80\uC0B0\uC758 \uD0DC\uC885\uB300\uC640 \uC815\uB3D9\uC9C4\uC774 \uC720\uBA85\uD558\uB2E4."@ko . "Soerguimento tect\u00F3nico (portugu\u00EAs europeu) ou soerguimento tect\u00F4nico (portugu\u00EAs brasileiro) \u00E9 um processo geol\u00F3gico normalmente causado devido \u00E0 tect\u00F3nica de placas. Neste processo, uma por\u00E7\u00E3o da crosta terrestre \u00E9 elevada da sua posi\u00E7\u00E3o original. O oposto deste fen\u00F3meno \u00E9 a subsid\u00EAncia, da qual resulta a diminui\u00E7\u00E3o da eleva\u00E7\u00E3o. O levantamento pode ter origem orog\u00E9nica ou isost\u00E1tica."@pt . "Soerguimento tect\u00F3nico"@pt . . . . "Landh\u00F6jning"@sv . . .