. . . "245138"^^ . "Loess (paraula d'origen alemany en la variant de Su\u00EFssa) \u00E9s un tipus de s\u00F2l llim\u00F3s. Les part\u00EDcules que formen el loess s\u00F3n de gra molt fi (di\u00E0metre inferior a 0,05 mm), anguloses i formades de quars, feldespat, hornblenda, mica, carbonat de calci i de vegades tamb\u00E9 argila. El deu per cent de la superf\u00EDcie terrestre de la Terra est\u00E0 coberta per loess o dip\u00F2sits similars."@ca . . . . . . . . . . . . "\u0627\u0644\u0631\u0627\u0633\u0628 \u0627\u0644\u0637\u0641\u0627\u0644\u064A (\u0628\u0627\u0644\u0625\u0646\u062C\u0644\u064A\u0632\u064A\u0629: Loess) \u0647\u064A \u0639\u0628\u0627\u0631\u0629 \u0639\u0646 \u0645\u0648\u0627\u062F \u0645\u062A\u0641\u0643\u0643\u0629 \u0648\u0631\u0648\u0627\u0633\u0628 \u0628\u062D\u062C\u0645 \u0627\u0644\u0637\u0645\u064A (20 -50\u0645\u064A\u0643\u0631\u0648\u0645\u062A\u0631)\u060C \u0648\u0627\u0644\u062A\u064A \u062A\u062A\u0643\u0648\u0646 \u0645\u0646 \u062A\u0631\u0627\u0643\u0645 \u0627\u0644\u063A\u0628\u0627\u0631 \u0627\u0644\u0630\u064A \u062A\u0630\u0631\u0648\u0647 \u0627\u0644\u0631\u064A\u0627\u062D. \u0648\u0647\u064A \u0639\u0627\u062F\u0629 \u0645\u0627 \u062A\u0643\u0648\u0646 \u0645\u062A\u062C\u0627\u0646\u0633\u0629 \u0648\u0630\u0627\u062A \u0645\u0633\u0627\u0645\u064A\u0629 \u0639\u0627\u0644\u064A\u0629."@ar . . . . . . . . "(alia vorto: loeso) estas sedimenta petro, kiu ekestas per la detrui\u011Do de aliaj \u015Dtona\u0135oj. Plejparte \u011Di konsistas el pulvora kvarco. \u011Ciaj grajnoj (eroj), kiujn origine alportis vento, estas delikataj kaj egalmezuraj."@eo . . . . . . . "L\u00F6ss is een eolische afzetting van silt. Silt is de textuurfractie met een korrelgrootte die tussen die van zand en lutum in ligt. Qua samenstelling bevat l\u00F6ss voornamelijk siliciclastica (kwarts en andere silicaten), maar het kan ook een kleine fractie kleimineralen bevatten. Soms is die fractie groter geworden sinds het moment van sedimentatie als gevolg van chemische verwering. In het dagelijkse spraakgebruik wordt het begrip l\u00F6ss of Limburgse klei veelal gebruikt voor gronden die onder andere voorkomen in Nederlands en Belgisch Limburg, langs de Veluwezoom bij Rheden, in de Achterhoek en op het plateau bij Groesbeek ten zuidoosten van Nijmegen. De Nederlandse l\u00F6ss heeft een typerende geelrode kleur. Uitgestrekte l\u00F6ss-gebieden bevinden zich ook in Noord-China, het l\u00F6ssplateau langs de Gele Rivier, en in het Russische steppegebied, waar zich in de l\u00F6ss-bodem de aan organische bestanddelen zeer rijke chernozems (zwarte aarde) hebben ontwikkeld."@nl . "\u0627\u0644\u0631\u0627\u0633\u0628 \u0627\u0644\u0637\u0641\u0627\u0644\u064A (\u0628\u0627\u0644\u0625\u0646\u062C\u0644\u064A\u0632\u064A\u0629: Loess) \u0647\u064A \u0639\u0628\u0627\u0631\u0629 \u0639\u0646 \u0645\u0648\u0627\u062F \u0645\u062A\u0641\u0643\u0643\u0629 \u0648\u0631\u0648\u0627\u0633\u0628 \u0628\u062D\u062C\u0645 \u0627\u0644\u0637\u0645\u064A (20 -50\u0645\u064A\u0643\u0631\u0648\u0645\u062A\u0631)\u060C \u0648\u0627\u0644\u062A\u064A \u062A\u062A\u0643\u0648\u0646 \u0645\u0646 \u062A\u0631\u0627\u0643\u0645 \u0627\u0644\u063A\u0628\u0627\u0631 \u0627\u0644\u0630\u064A \u062A\u0630\u0631\u0648\u0647 \u0627\u0644\u0631\u064A\u0627\u062D. \u0648\u0647\u064A \u0639\u0627\u062F\u0629 \u0645\u0627 \u062A\u0643\u0648\u0646 \u0645\u062A\u062C\u0627\u0646\u0633\u0629 \u0648\u0630\u0627\u062A \u0645\u0633\u0627\u0645\u064A\u0629 \u0639\u0627\u0644\u064A\u0629."@ar . . . . . . . "\u9EC4\u571F\u3068\u306F\u3001\u9EC4\u8272\u307F\u306E\u5F37\u3044\u571F\u306E\u3053\u3068\u3067\u3042\u308B\u3002\u5C02\u9580\u7528\u8A9E\u3068\u3057\u3066\u306F2\u3064\u306E\u7528\u6CD5\u304C\u3042\u308B\u3002 1. \n* \u300C\u304D\u3065\u3061\u300D\u300C\u304D\u3064\u3061\u300D\u3068\u8AAD\u3093\u3067\u3001\u548C\u5EFA\u7BC9\u3001\u5DE6\u5B98\u3001\u65E5\u672C\u7F8E\u8853\u306A\u3069\u3067\u7528\u3044\u308B\u3001\u9EC4\u5473\u3092\u5E2F\u3073\u305F\u571F\u306E\u4E00\u7A2E\u3002 2. \n* \u30C9\u30A4\u30C4\u8A9E: L\u00F6ss\u3001\u82F1\u8A9E: loess \u306E\u8A33\u8A9E\u3002\u300C\u304A\u3046\u3069\u300D\u307E\u305F\u306F\u300C\u3053\u3046\u3069\u300D\u3068\u8AAD\u3080\u3002"@ja . . . . "32695"^^ . "Le\u016Dso"@eo . . . . . . . . . . . "Il l\u00F6ss /l\u0153s/, pi\u00F9 frequentemente trascritto come loess (la parola \u00E8 di origine tedesca), \u00E8 un tipo di sedimento eolico molto fine (delle dimensioni del limo); alle volte, il termine viene impropriamente utilizzato per indicare i suoli che su di esso si sono sviluppati. Il l\u00F6ss \u00E8 un sedimento eolico, che viene cio\u00E8 originato dal trasporto e dalla deposizione di particelle da parte del vento. Ci\u00F2 causa la particolare selezione granulometrica che lo caratterizza, la quale \u00E8 funzione della velocit\u00E0 del vento e della densit\u00E0 dei clasti trasportati. Le aree di origine del sedimento possono essere diverse: in alcuni casi, le particelle provengono da depositi inconsolidati di origine glaciale che sono molto suscettibili di erosione, soprattutto da parte del vento; tuttavia le aree di ablazione dei maggiori depositi l\u00F6ssici come l'altopiano del Loess sono costituite dalle ampie aree desertiche del deserto del Gobi. Dopo la rideposizione, i depositi l\u00F6ssici rimangono spesso instabili e possono essere erosi in tempi relativamente brevi; questo destino si compie generalmente anche in mancanza di azioni perturbatrici di origine antropica. Le deposizioni di l\u00F6ss si estendono spesso su vaste aree: celeberrimi e molto importanti sono l'altopiano del Loess, nella Cina centro-settentrionale e i suoli neri di steppa (Chernozem, Mollisol) della Russia europea meridionale, della Siberia sudoccidentale e delle Grandi Pianure nordamericane. L'altopiano del Loess, nella Cina centro-settentrionale, \u00E8 uno dei depositi di l\u00F6ss pi\u00F9 estesi e pi\u00F9 studiati. Questi sedimenti si sono accumulati durante l'ultimo milione di anni con spessori variabili fino a qualche centinaio di metri e sono caratterizzati da una alternanza di strati di l\u00F6ss veri e propri e suoli. I primi si accumulano durante i periodi glaciali, secchi e ventosi; i secondi si sviluppano durante i periodi interglaciali con clima caldo e umido."@it . . . "\u9EC4\u571F\u9AD8\u539F"@en . "\u9EC4\u571F"@ja . "L\u00F6ss"@de . . . . . . . . . . . . "El loess (del alem\u00E1n de Suiza l\u00F6sch, en alem\u00E1n com\u00FAn: L\u00F6ss) son dep\u00F3sitos sedimentarios limosos de origen e\u00F3lico."@es . . "L\u00F6ss (Hauptschreibweise) oder L\u00F6\u00DF ist ein homogenes, ungeschichtetes, hellgelblich-graues Sediment, das vorwiegend aus Schluff besteht. H\u00E4ufig wird daneben ein gewisser Karbonatanteil als wichtiges Kriterium zur Charakterisierung angesehen. L\u00F6ss wurde \u00FCberwiegend von Wind abgelagert, ver\u00E4nderte sich danach aber meist weiter."@de . . "\u9EC3\u571F\u4E00\u79CD\u6D45\u9EC4\u6216\u8910\u9EC4\u8272\u7684\u571F\uFF0C\u9897\u7C92\u6210\u5206\u4EE5\u7C92\u7EA7\u4E3A\u4E3B\uFF08\u542B\u91CF\uFF1E50%\uFF09\uFF0C\u7269\u8D28\u7C92\u5F84\u5747\u4E00\uFF0C\u5177\u5B54\u9699\uFF0C\u65E0\u5C42\u7406\uFF0C\u758F\u677E\uFF0C\u5782\u76F4\u8282\u7406\u767C\u80B2\u3002\u5BCC\u542B\u78B3\u9178\u9499,\u6709\u65F6\u542B\u786B\u9178\u76D0\u6216\u6C2F\u5316\u7269\u76D0\u7C7B\uFF0C\u5177\u6709\u8089\u773C\u53EF\u89C1\u5B54\u9699\u7684\u7B2C\u56DB\u7EAA\u9646\u76F8\u6C89\u79EF\u7269\u3002\u9EC4\u571F\u6709\u65F6\u5177\u6709\u6E7F\u9677\u6027\u3002\u53E6\u5916\uFF0C\u5176\u5728\u77FF\u7269\u6210\u5206\u65B9\u9762\u9AD8\u5EA6\u590D\u6742\uFF0C\u591A\u8FBE60\u591A\u79CD\u77FF\u7269\uFF0C\u5305\u62EC\u5CA9\u6D46\u5CA9\u3001\u53D8\u8D28\u5CA9\u548C\u6C89\u79EF\u5CA9\u7684\u77FF\u7269\u6210\u5206\uFF0C\u800C\u4E14\u4E0E\u5176\u4E2D\u4EFB\u4F55\u4E00\u79CD\u5CA9\u77F3\u7684\u77FF\u7269\u6210\u5206\u90FD\u4E0D\u76F8\u540C\u3002\u5404\u5730\u533A\u9EC4\u571F\u77FF\u7269\u6210\u5206\u5927\u4F53\u76F8\u540C\uFF0C\u65E0\u8BBA\u77FF\u7269\u79CD\u7C7B\u8FD8\u662F\u767E\u5206\u542B\u91CF\u90FD\u57FA\u672C\u76F8\u4F3C\uFF0C\u5E76\u6709\u6BD4\u8F83\u591A\u7684\u6613\u98CE\u5316\u4E0D\u7A33\u5B9A\u77FF\u7269\u3002\u5728\u5316\u5B66\u6210\u5206\u4E2D\u542B\u91CF\u6700\u591A\u7684\u662FSiO2\u3001Al2O3\u3001CaO\u3001Na2O\uFF0C\u542B\u6709\u6BD4\u8F83\u591A\u7684\u6613\u6EB6\u76D0\u7C7B\uFF0C\u4E3B\u8981\u662F\uFF1A\u6C27\u5316\u7269\u3001\u78B3\u9178\u76D0\u3001\u786B\u9178\u76D0\u3001CaCO3,\u542B\u91CF\u572810\uFF05-16\uFF05\u4E4B\u95F4\u3002\u5728\u6240\u542B\u751F\u7269\u5316\u77F3\u65B9\u9762\u4EE5\u8010\u65F1\u8349\u672C\u690D\u7269\u82B1\u7C89\u548C\u8010\u5E72\u65F1\u52A8\u7269\u5316\u77F3\u4E3A\u4E3B\uFF0C\u800C\u4E14\u542B\u6709\u559C\u6696\u6E7F\u7684\u52A8\u690D\u7269\u5316\u77F3\u3002\u6700\u65E9\u674E\u5E0C\u970D\u82AC\uFF081877\u5E74\uFF09\u5BF9\u6B27\u6D32\u83B1\u8335\u6CB3\u6D41\u57DF\u53CA\u4E2D\u56FD\u5927\u9646\u7684\u9EC4\u571F\u63D0\u51FA\u7684\u5B9A\u4E49\u4E3A\uFF1A\u9EC4\uFF0D\u8910\u8272\uFF0C\u542B\u77F3\u7070\u8D28\uFF0C\u4EE5\u7C89\u571F\u4E3A\u4E3B\u7684\u7C89\u72B6\u571F\uFF1B\u6CA1\u6709\u5C42\u7406\uFF0C\u542B\u9646\u751F\u8717\u725B\uFF0C\u6709\u5782\u76F4\u8282\u7406\u3002\u5386\u53F2\u65B9\u9762\uFF0C\u201C\u9EC4\u571F\u201D\u4E00\u8BCD\uFF0C\u5728\u4E2D\u56FD\u53E4\u4EE3\u6587\u732E\u4E2D\u53CA\u6C11\u95F4\u5C31\u5DF2\u51FA\u73B0\u3002 \u6709\u6642\u56E0\u6DCB\u6D17\u4F5C\u7528\u8F03\u5F37\u800C\u4F7F\u7C98\u7C92\u660E\u986F\u5F80\u5256\u9762\u4E0B\u5C64\u79FB\u52D5\uFF0C\u990A\u5206\u6709\u7684\u5DF2\u6D41\u5931\u800C\u5448\u9EC3\u3001\u9EC3\u68D5\u6216\u7D05\u68D5\u8272\u3002\u591A\u751F\u6210\u65BC\u4E18\u9675\u5730\u4E0A\u4E4B\u76F8\u5C0D\u5730\u5F62\u8F03\u5B89\u5B9A\u3001\u5761\u5EA6\u8D77\u4F0F\u8F03\u7DE9\u548C\u8655\u3002\u571F\u58E4\u591A\u5448\u5F31\u9178\u6027\uFF0C\u80A5\u6C83\u5EA6\u504F\u4F4E\uFF0C\u9808\u9032\u884C\u65BD\u80A5\u7BA1\u7406\u53CA\u6C34\u571F\u4FDD\u6301\uFF0C\u624D\u53EF\u505A\u8FB2\u7267\u7528\u5730\u3002\u6B64\u571F\u58E4\u5728\u65B0\u5206\u985E\u4E0A\u5C6C\u6216\u6DCB\u6EB6\u571F\u3002\u3002"@zh . . . "L\u00F6ss"@it . . . "L\u00F6ss is een eolische afzetting van silt. Silt is de textuurfractie met een korrelgrootte die tussen die van zand en lutum in ligt. Qua samenstelling bevat l\u00F6ss voornamelijk siliciclastica (kwarts en andere silicaten), maar het kan ook een kleine fractie kleimineralen bevatten. Soms is die fractie groter geworden sinds het moment van sedimentatie als gevolg van chemische verwering."@nl . "Loess"@eu . . . "Loessa (Suitzako alemanieratik l\u00F6sch) material geologiko sedimentario eolikoa da. 10 eta 50 mikrometro arteko tamaina duten partikula metaketen lupetz metaketek osatzen dute. Milaka urtean zehar, hauts erauntsiek garraiaturikoak dira. Hori kolorekoa da, labaingarria eta ez du estratifikaziorik. Batipat, silizioz kaltzio karbonatoz (kareharria), detritu organiko finez eta buztinez eratuta dago. Nekazaritzarako, lurzoru sakon eta emankorra osatzen dute. Partikula sendoenak, eratzen dituzten hareak dira."@eu . . "\u041B\u0435\u0441"@uk . . . . . "( \uC601\uD654\uC5D0 \uB300\uD574\uC11C\uB294 \uD669\uD1A0 (\uC601\uD654) \uBB38\uC11C\uB97C \uCC38\uACE0\uD558\uC2ED\uC2DC\uC624.) \uD669\uD1A0(\u9EC3\u571F), \uB8B0\uC2A4(loess)\uB294 \uC77C\uBC18\uC801\uC73C\uB85C \uBC14\uB78C\uC5D0 \uC758\uD574 \uC6B4\uBC18\uB418\uC5B4 \uD1F4\uC801\uB41C \uD669\uAC08\uC0C9\uC774\uB098 \uC758 \uBBF8\uC138\uD55C \uBAA8\uB798\uC640 \uC810\uD1A0\uB97C \uAC00\uB9AC\uD0A4\uBA70, \uC8FC\uB85C \uC2E4\uD2B8 \uD06C\uAE30\uC758 \uC785\uC790\uB4E4\uB85C \uAD6C\uC131\uB418\uC5B4 \uC788\uB2E4. \uD0C4\uC0B0\uCE7C\uC298\uC5D0 \uC758\uD574 \uB290\uC2A8\uD558\uAC8C \uC811\uCC29\uB418\uC5B4 \uB300\uAC1C \uADE0\uC9C8\uD558\uACE0 \uCE35\uB9AC\uAC00 \uBC1C\uB2EC\uB418\uC5B4 \uC788\uC9C0 \uC54A\uC73C\uBA70 \uB2E4\uACF5\uC9C8\uC774\uB2E4. \uD604\uC7AC \uC911\uAD6D \uBD81\uBD80, \uC720\uB7FD \uC911\uBD80, \uBD81\uC544\uBA54\uB9AC\uCE74\uC758 \uBBF8\uC2DC\uC2DC\uD53C \uACC4\uACE1, \uC544\uB974\uD5E8\uD2F0\uB098\uC758 \uC0C1\uB2F9 \uBD80\uBD84, \uD0C0\uC9C0\uD0A4\uC2A4\uD0C4 \uB0A8\uBD80\uC5D0\uC11C \uCE74\uC790\uD750\uC2A4\uD0C4\uC5D0 \uAC78\uCE58\uB294 \uC911\uC559\uC544\uC2DC\uC544 \uB4F1\uC5D0 \uB110\uB9AC \uBD84\uD3EC\uB418\uC5B4 \uC788\uC73C\uBA70, \uC804\uCCB4 \uC9C0\uD45C\uBA74 \uC911 \uC57D 10%\uB97C \uCC28\uC9C0\uD558\uACE0 \uC788\uB2E4. \uD669\uD1A0\uB294 \uC7BF\uBE5B\uC774 \uB098\uB294 \uD669\uC0C9\uC758 \uC11D\uC601(\u77F3\u82F1)\uC774\uB098 \uC7A5\uC11D(\u9577\u77F3) \uB4F1\uC758 \uBBF8\uB9BD(\u5FAE\u7C92)\uC758 \uD1F4\uC801\uC73C\uB85C\uC11C, \uB545\uC774 \uBE44\uC625\uD558\uACE0 \uBD80\uB4DC\uB7EC\uC6CC\uC11C \uB18D\uACBD \uC0DD\uD65C\uC744 \uD558\uAE30\uC5D0\uB294 \uC544\uC8FC \uC801\uD569\uD588\uB2E4. \uD669\uD1A0 \uC548\uC5D0 \uD568\uC720\uD558\uACE0 \uC788\uB294 \uC720\uAE30\uBB3C\uC9C8\uC774 \uC0C1\uB300\uC801\uC73C\uB85C \uBE48\uC57D\uD568\uC5D0\uB3C4 \uD1A0\uC9C8\uC774 \uBE44\uC625\uD55C \uC774\uC720\uB85C\uB294, \uC591\uC774\uC628 \uAD50\uD658 \uC6A9\uB7C9\uACFC \uD22C\uACFC\uC131\uC774 \uB192\uAE30 \uB54C\uBB38\uC774\uB77C\uB294 \uC774\uB860\uC774 \uC81C\uC2DC\uB418\uC5B4 \uC788\uB2E4. \uC774 \uD669\uD1A0 \uC9C0\uB300\uC5D0\uC11C \uB18D\uC5C5 \uC0DD\uC0B0\uB825\uC758 \uBC1C\uC804\uC744 \uAE30\uCD08\uB85C \uBB38\uBA85\uC774 \uC131\uB9BD\uB418\uC5C8\uB2E4."@ko . . . . . "Hu\u00E1ngt\u01D4 G\u0101oyu\u00E1n"@en . . . . . . . . . "L\u00F6ssjord"@sv . "\u041B\u0435\u0441 (\u043D\u0456\u043C. L\u00F6ss, L\u00F6\u00DF, \u0432\u0456\u0434 \u0430\u043B\u0435\u043C. l\u00F6sch \u2014 \u00AB\u043A\u0440\u0438\u0445\u043A\u0438\u0439, \u0441\u0438\u043F\u043A\u0438\u0439\u00BB) \u2014 \u043A\u043E\u043D\u0442\u0438\u043D\u0435\u043D\u0442\u0430\u043B\u044C\u043D\u0430 \u0491\u0440\u0443\u043D\u0442\u043E\u0443\u0442\u0432\u043E\u0440\u044E\u0432\u0430\u043B\u044C\u043D\u0430 \u0433\u0456\u0440\u0441\u044C\u043A\u0430 \u043E\u0441\u0430\u0434\u043E\u0432\u0430 \u043F\u043E\u0440\u043E\u0434\u0430 \u0441\u0456\u0440\u0443\u0432\u0430\u0442\u043E-\u0436\u043E\u0432\u0442\u043E\u0433\u043E, \u0456\u043D\u043E\u0434\u0456 \u0431\u0443\u0440\u043E\u0433\u043E \u0430\u0431\u043E \u0447\u0435\u0440\u0432\u043E\u043D\u0443\u0432\u0430\u0442\u043E-\u0431\u0443\u0440\u043E\u0433\u043E \u043A\u043E\u043B\u044C\u043E\u0440\u0443. \u041F\u043E\u0442\u0443\u0436\u043D\u0456\u0441\u0442\u044C \u043B\u0435\u0441\u043E\u0432\u0438\u0445 \u043D\u0430\u0448\u0430\u0440\u0443\u0432\u0430\u043D\u044C \u0441\u0442\u0430\u043D\u043E\u0432\u0438\u0442\u044C \u0432\u0456\u0434 \u043A\u0456\u043B\u044C\u043A\u043E\u0445 \u0434\u0435\u0441\u044F\u0442\u043A\u0456\u0432 \u0441\u0430\u043D\u0442\u0438\u043C\u0435\u0442\u0440\u0456\u0432 \u0434\u043E \u043A\u0456\u043B\u044C\u043A\u043E\u0445 \u0434\u0435\u0441\u044F\u0442\u043A\u0456\u0432 \u043C\u0435\u0442\u0440\u0456\u0432 \u043D\u0430 \u0432\u043E\u0434\u043E\u0434\u0456\u043B\u0430\u0445 \u0442\u0430 \u0441\u0445\u0438\u043B\u0430\u0445 \u0442\u0435\u0440\u0430\u0441 \u0434\u0430\u0432\u043D\u0456\u0445 \u0434\u043E\u043B\u0438\u043D."@uk . . . . . . "Loess (US: /\u02C8l\u025Bs, \u02C8l\u028Cs, \u02C8lo\u028A.\u0259s/, UK: /\u02C8lo\u028A.\u0259s, \u02C8l\u025C\u02D0s/; from German: L\u00F6ss [l\u0153s]) is a clastic, predominantly silt-sized sediment that is formed by the accumulation of wind-blown dust. Ten percent of Earth's land area is covered by loess or similar deposits."@en . . . . . . . . . . . . . . . . "Loess (US: /\u02C8l\u025Bs, \u02C8l\u028Cs, \u02C8lo\u028A.\u0259s/, UK: /\u02C8lo\u028A.\u0259s, \u02C8l\u025C\u02D0s/; from German: L\u00F6ss [l\u0153s]) is a clastic, predominantly silt-sized sediment that is formed by the accumulation of wind-blown dust. Ten percent of Earth's land area is covered by loess or similar deposits. Loess is a periglacial or aeolian (windborne) sediment, defined as an accumulation of 20% or less of clay and a balance of roughly equal parts sand and silt (with a typical grain size from 20 to 50 micrometers), often loosely cemented by calcium carbonate. It is usually homogeneous and highly porous and is traversed by vertical capillaries that permit the sediment to fracture and form vertical bluffs."@en . . "Le l\u0153ss (ou loess) est une roche s\u00E9dimentaire d\u00E9tritique meuble form\u00E9e par l'accumulation de limons issus de l'\u00E9rosion \u00E9olienne, dans les r\u00E9gions d\u00E9sertiques et p\u00E9riglaciaires (ceintures p\u00E9rid\u00E9sertique et p\u00E9riglaciaire). Les d\u00E9p\u00F4ts \u00E9oliens de couverture r\u00E9sultent du transport par le vent \u00E0 moyenne et longue distance et du pi\u00E9geage de ces particules fines par une v\u00E9g\u00E9tation herbac\u00E9e dense. Ils s'\u00E9tendent en couverture sur plus de 10 % de la surface des continents et concernent les sables fins (sables de couverture) et les limons (l\u0153ss)."@fr . . . "(alia vorto: loeso) estas sedimenta petro, kiu ekestas per la detrui\u011Do de aliaj \u015Dtona\u0135oj. Plejparte \u011Di konsistas el pulvora kvarco. \u011Ciaj grajnoj (eroj), kiujn origine alportis vento, estas delikataj kaj egalmezuraj."@eo . . "\u041B\u0451\u0441\u0441 (\u043D\u0435\u043C. L\u00F6\u00DF \u0438\u043B\u0438 L\u00F6ss \u2014 \u0440\u044B\u0445\u043B\u044B\u0439, \u043E\u0441\u044B\u043F\u0430\u044E\u0449\u0438\u0439\u0441\u044F) \u2014 \u043E\u0441\u0430\u0434\u043E\u0447\u043D\u0430\u044F \u0433\u043E\u0440\u043D\u0430\u044F \u043F\u043E\u0440\u043E\u0434\u0430, \u043D\u0435\u0441\u043B\u043E\u0438\u0441\u0442\u0430\u044F, \u0441\u0443\u0433\u043B\u0438\u043D\u0438\u0441\u0442\u043E-\u0441\u0443\u043F\u0435\u0441\u0447\u0430\u043D\u0430\u044F, \u0438\u043C\u0435\u0435\u0442 \u0441\u0432\u0435\u0442\u043B\u043E-\u0436\u0451\u043B\u0442\u044B\u0439 \u0438\u043B\u0438 \u043F\u0430\u043B\u0435\u0432\u044B\u0439 \u0446\u0432\u0435\u0442, \u0441\u043B\u043E\u0436\u0435\u043D\u0430 \u043F\u0440\u0435\u0438\u043C\u0443\u0449\u0435\u0441\u0442\u0432\u0435\u043D\u043D\u043E \u043F\u044B\u043B\u0435\u0432\u0430\u0442\u044B\u043C\u0438 \u0437\u0451\u0440\u043D\u0430\u043C\u0438. \u0417\u0430\u043B\u0435\u0433\u0430\u0435\u0442 \u0432 \u0432\u0438\u0434\u0435 \u043F\u043E\u043A\u0440\u043E\u0432\u0430 \u043E\u0442 \u043D\u0435\u0441\u043A\u043E\u043B\u044C\u043A\u0438\u0445 \u043C\u0435\u0442\u0440\u043E\u0432 \u0434\u043E 50\u2014100 \u043C \u2014 \u043D\u0430 \u0432\u043E\u0434\u043E\u0440\u0430\u0437\u0434\u0435\u043B\u0430\u0445, \u0441\u043A\u043B\u043E\u043D\u0430\u0445 \u0438 \u0434\u0440\u0435\u0432\u043D\u0438\u0445 \u0442\u0435\u0440\u0440\u0430\u0441\u0430\u0445 \u0434\u043E\u043B\u0438\u043D."@ru . . . . . . "O loesse (do alem\u00E3o L\u00F6ss) \u00E9 um sedimento f\u00E9rtil de colora\u00E7\u00E3o amarelada. \u00C9 formado por sedimentos depositados pelo vento\u02D0 basicamente, part\u00EDculas de quartzito, calc\u00E1rio e calcita. Sua colora\u00E7\u00E3o amarela se deve \u00E0 presen\u00E7a de \u00F3xido de ferro. \u00C9 encontrado em parte da Europa (Fran\u00E7a e Pa\u00EDses Baixos), em plan\u00EDcies fluviais e glaciais, nos pampas argentino e uruguaio, e principalmente na China, onde encontra-se o Rio Amarelo, importante rio na cultura do arroz chin\u00EAs. Loessito \u00E9 o nome dado \u00E0 rocha sedimentar composta por loesse consolidado."@pt . . . . "Loess"@en . . . . "Le l\u0153ss (ou loess) est une roche s\u00E9dimentaire d\u00E9tritique meuble form\u00E9e par l'accumulation de limons issus de l'\u00E9rosion \u00E9olienne, dans les r\u00E9gions d\u00E9sertiques et p\u00E9riglaciaires (ceintures p\u00E9rid\u00E9sertique et p\u00E9riglaciaire). Les d\u00E9p\u00F4ts \u00E9oliens de couverture r\u00E9sultent du transport par le vent \u00E0 moyenne et longue distance et du pi\u00E9geage de ces particules fines par une v\u00E9g\u00E9tation herbac\u00E9e dense. Ils s'\u00E9tendent en couverture sur plus de 10 % de la surface des continents et concernent les sables fins (sables de couverture) et les limons (l\u0153ss)."@fr . . . . . . . . . . . . . . . . . . . . . . . "O loesse (do alem\u00E3o L\u00F6ss) \u00E9 um sedimento f\u00E9rtil de colora\u00E7\u00E3o amarelada. \u00C9 formado por sedimentos depositados pelo vento\u02D0 basicamente, part\u00EDculas de quartzito, calc\u00E1rio e calcita. Sua colora\u00E7\u00E3o amarela se deve \u00E0 presen\u00E7a de \u00F3xido de ferro. \u00C9 encontrado em parte da Europa (Fran\u00E7a e Pa\u00EDses Baixos), em plan\u00EDcies fluviais e glaciais, nos pampas argentino e uruguaio, e principalmente na China, onde encontra-se o Rio Amarelo, importante rio na cultura do arroz chin\u00EAs. Loessito \u00E9 o nome dado \u00E0 rocha sedimentar composta por loesse consolidado."@pt . . "\uD669\uD1A0"@ko . . "Loess"@in . . "L\u00F6ss (Hauptschreibweise) oder L\u00F6\u00DF ist ein homogenes, ungeschichtetes, hellgelblich-graues Sediment, das vorwiegend aus Schluff besteht. H\u00E4ufig wird daneben ein gewisser Karbonatanteil als wichtiges Kriterium zur Charakterisierung angesehen. L\u00F6ss wurde \u00FCberwiegend von Wind abgelagert, ver\u00E4nderte sich danach aber meist weiter. L\u00F6ss bedeckt etwa zehn Prozent der Erdoberfl\u00E4che und ist vor allem in der gem\u00E4\u00DFigten Klimazone verbreitet. Er wurde zum gr\u00F6\u00DFten Teil in den quart\u00E4ren Kaltzeiten gebildet und ist Ausgangssubstrat f\u00FCr die ackerbaulich g\u00FCnstigsten B\u00F6den weltweit. Dar\u00FCber hinaus werden L\u00F6sse und darin eingeschaltete fossile B\u00F6den (Pal\u00E4ob\u00F6den) als Archive f\u00FCr die Rekonstruktion quart\u00E4rer Umweltver\u00E4nderungen erforscht."@de . . . . . . . . . . . . . "Spra\u0161"@cs . . . . . . . "Loess"@es . . . . . . . . . . "\u9EC3\u571F"@zh . . . . . . . . . . . . "L\u00F6ssjordar \u00E4r en l\u00F6s vindavsatt avlagring som till st\u00F6rsta delen best\u00E5r av silt som domineras av kvarts. L\u00F6ssjordar, liksom andra sediment med h\u00F6ga kvartshalter har sitt ursprung i erosion av den blottade underliggande berggrunden. Detta kan till exempel ske mekaniskt med hj\u00E4lp av en stor ismassa (glaci\u00E4r) d\u00E4r silten transporteras och avs\u00E4tts med hj\u00E4lp av vinden, eller genom att vinden eroderar ned berggrunden, s\u00E5som till exempel l\u00F6ssjordarna i Kina har bildats. L\u00F6ssjordarna kan bli flera hundra meter tjocka och p\u00E5 vissa h\u00E5ll i v\u00E4rlden har man byggt bost\u00E4der i dessa. P\u00E5 m\u00E5nga h\u00E5ll bildar l\u00F6ssjordarna vertikala branter, som kan bli riktigt stora. L\u00F6ssjordar finns p\u00E5 m\u00E5nga platser i v\u00E4rlden, framf\u00F6rallt i USA, Argentina, Kina, centrala Europa och Asien, men \u00E4ven i bland annat Nordafrika och Australien."@sv . . "L\u0153ss"@fr . . . . . . . . . . . . "Il l\u00F6ss /l\u0153s/, pi\u00F9 frequentemente trascritto come loess (la parola \u00E8 di origine tedesca), \u00E8 un tipo di sedimento eolico molto fine (delle dimensioni del limo); alle volte, il termine viene impropriamente utilizzato per indicare i suoli che su di esso si sono sviluppati. Il l\u00F6ss \u00E8 un sedimento eolico, che viene cio\u00E8 originato dal trasporto e dalla deposizione di particelle da parte del vento. Ci\u00F2 causa la particolare selezione granulometrica che lo caratterizza, la quale \u00E8 funzione della velocit\u00E0 del vento e della densit\u00E0 dei clasti trasportati."@it . . "L\u00F6ssjordar \u00E4r en l\u00F6s vindavsatt avlagring som till st\u00F6rsta delen best\u00E5r av silt som domineras av kvarts. L\u00F6ssjordar, liksom andra sediment med h\u00F6ga kvartshalter har sitt ursprung i erosion av den blottade underliggande berggrunden. Detta kan till exempel ske mekaniskt med hj\u00E4lp av en stor ismassa (glaci\u00E4r) d\u00E4r silten transporteras och avs\u00E4tts med hj\u00E4lp av vinden, eller genom att vinden eroderar ned berggrunden, s\u00E5som till exempel l\u00F6ssjordarna i Kina har bildats."@sv . . "\u9EC3\u571F\u9AD8\u539F"@en . "\u9EC4\u571F\u3068\u306F\u3001\u9EC4\u8272\u307F\u306E\u5F37\u3044\u571F\u306E\u3053\u3068\u3067\u3042\u308B\u3002\u5C02\u9580\u7528\u8A9E\u3068\u3057\u3066\u306F2\u3064\u306E\u7528\u6CD5\u304C\u3042\u308B\u3002 1. \n* \u300C\u304D\u3065\u3061\u300D\u300C\u304D\u3064\u3061\u300D\u3068\u8AAD\u3093\u3067\u3001\u548C\u5EFA\u7BC9\u3001\u5DE6\u5B98\u3001\u65E5\u672C\u7F8E\u8853\u306A\u3069\u3067\u7528\u3044\u308B\u3001\u9EC4\u5473\u3092\u5E2F\u3073\u305F\u571F\u306E\u4E00\u7A2E\u3002 2. \n* \u30C9\u30A4\u30C4\u8A9E: L\u00F6ss\u3001\u82F1\u8A9E: loess \u306E\u8A33\u8A9E\u3002\u300C\u304A\u3046\u3069\u300D\u307E\u305F\u306F\u300C\u3053\u3046\u3069\u300D\u3068\u8AAD\u3080\u3002"@ja . "1117745106"^^ . . . . . . . . . . "\u041B\u0435\u0441 (\u043D\u0456\u043C. L\u00F6ss, L\u00F6\u00DF, \u0432\u0456\u0434 \u0430\u043B\u0435\u043C. l\u00F6sch \u2014 \u00AB\u043A\u0440\u0438\u0445\u043A\u0438\u0439, \u0441\u0438\u043F\u043A\u0438\u0439\u00BB) \u2014 \u043A\u043E\u043D\u0442\u0438\u043D\u0435\u043D\u0442\u0430\u043B\u044C\u043D\u0430 \u0491\u0440\u0443\u043D\u0442\u043E\u0443\u0442\u0432\u043E\u0440\u044E\u0432\u0430\u043B\u044C\u043D\u0430 \u0433\u0456\u0440\u0441\u044C\u043A\u0430 \u043E\u0441\u0430\u0434\u043E\u0432\u0430 \u043F\u043E\u0440\u043E\u0434\u0430 \u0441\u0456\u0440\u0443\u0432\u0430\u0442\u043E-\u0436\u043E\u0432\u0442\u043E\u0433\u043E, \u0456\u043D\u043E\u0434\u0456 \u0431\u0443\u0440\u043E\u0433\u043E \u0430\u0431\u043E \u0447\u0435\u0440\u0432\u043E\u043D\u0443\u0432\u0430\u0442\u043E-\u0431\u0443\u0440\u043E\u0433\u043E \u043A\u043E\u043B\u044C\u043E\u0440\u0443. \u041F\u043E\u0442\u0443\u0436\u043D\u0456\u0441\u0442\u044C \u043B\u0435\u0441\u043E\u0432\u0438\u0445 \u043D\u0430\u0448\u0430\u0440\u0443\u0432\u0430\u043D\u044C \u0441\u0442\u0430\u043D\u043E\u0432\u0438\u0442\u044C \u0432\u0456\u0434 \u043A\u0456\u043B\u044C\u043A\u043E\u0445 \u0434\u0435\u0441\u044F\u0442\u043A\u0456\u0432 \u0441\u0430\u043D\u0442\u0438\u043C\u0435\u0442\u0440\u0456\u0432 \u0434\u043E \u043A\u0456\u043B\u044C\u043A\u043E\u0445 \u0434\u0435\u0441\u044F\u0442\u043A\u0456\u0432 \u043C\u0435\u0442\u0440\u0456\u0432 \u043D\u0430 \u0432\u043E\u0434\u043E\u0434\u0456\u043B\u0430\u0445 \u0442\u0430 \u0441\u0445\u0438\u043B\u0430\u0445 \u0442\u0435\u0440\u0430\u0441 \u0434\u0430\u0432\u043D\u0456\u0445 \u0434\u043E\u043B\u0438\u043D."@uk . "\u041B\u0451\u0441\u0441"@ru . "Loesse"@pt . . "Loess (paraula d'origen alemany en la variant de Su\u00EFssa) \u00E9s un tipus de s\u00F2l llim\u00F3s. Les part\u00EDcules que formen el loess s\u00F3n de gra molt fi (di\u00E0metre inferior a 0,05 mm), anguloses i formades de quars, feldespat, hornblenda, mica, carbonat de calci i de vegades tamb\u00E9 argila. El deu per cent de la superf\u00EDcie terrestre de la Terra est\u00E0 coberta per loess o dip\u00F2sits similars. El loess \u00E9s un sediment e\u00F2lic (transm\u00E8s pel vent) que acumula un vint per cent o menys d'argila i l'equilibri \u00E9s principalment de parts iguals de sorra i llim t\u00EDpicament de 20 a 50 micr\u00F2metres per part\u00EDcula sovint cimentada de manera fluida pel carbonat c\u00E0lcic. Normalment \u00E9s homogeni i altament por\u00F3s i est\u00E0 travessat per capil\u00B7lars verticals que permeten el sediment fracturar-se i formar esclats verticals."@ca . . . . . "Spra\u0161 je \u00FAlomkovit\u00E1 usazen\u00E1 hornina v\u011Btrem (\u010Dili v odborn\u00E9 terminologii klastick\u00FD sediment eolick\u00E9ho p\u016Fvodu). Hlavn\u00ED slo\u017Ekou je jemn\u00FD k\u0159emit\u00FD prach (k\u0159emen, \u017Eivec a sl\u00EDda; typick\u00E1 velikost \u010D\u00E1stic 0,03-0,06 mm) s p\u0159\u00EDm\u011Bs\u00ED uhli\u010Ditanu v\u00E1penat\u00E9ho, vytv\u00E1\u0159ej\u00EDc\u00EDho sra\u017Een\u00E9 hrudky (\u201Ecicv\u00E1ry\u201C), a j\u00EDlu. Typickou sv\u011Btle okrovou barvu maj\u00ED na sv\u011Bdom\u00ED oxidy \u017Eeleza."@cs . "Loessa (Suitzako alemanieratik l\u00F6sch) material geologiko sedimentario eolikoa da. 10 eta 50 mikrometro arteko tamaina duten partikula metaketen lupetz metaketek osatzen dute. Milaka urtean zehar, hauts erauntsiek garraiaturikoak dira. Hori kolorekoa da, labaingarria eta ez du estratifikaziorik. Batipat, silizioz kaltzio karbonatoz (kareharria), detritu organiko finez eta buztinez eratuta dago. Nekazaritzarako, lurzoru sakon eta emankorra osatzen dute. Klima idorreko lurraldeetan, loessaren metaketak, landarediak, eskasa izan arren, bere finkatzea errezten duen tokietan eratzen dira. Klima hotzeko lurraldeetan, hautsa, lupetz bankuetatik erauzia izan da, eta, ondoren, lurraldeen elur geruza gainean utzia. Fenomeno honek, laugarren aroko glaziazio garaietan jarraitu duenez, 300 metrorarteko sendoera duten metaketa handiak sortu ditu europar lautada handian. Lurralde honetako tokirik emankorrena, hain zuzen ere, loessak eratuta dagoelako da hain emankorra. Lurralde hauetako hainbat tokitan, urak, metaketa hauen goiko geruzako karea disolbatu eta tarrasean eraman du denboran zehar, deskarbonatatu eta bihurtuz. Partikula sendoenak, eratzen dituzten hareak dira."@eu . "Less \u2013 pylasta ska\u0142a osadowa, wyselekcjonowana i deponowana na drodze eolicznej, a wi\u0119c w warunkach wzgl\u0119dnie suchego klimatu, na co wskazuje m.in. rozmieszczenie strefowe lub zwi\u0105zek lessu z okre\u015Blonym pi\u0119trem hipsometrycznym. W obszarach wilgotniejszych osad o takich cechach nie wyodr\u0119bnia si\u0119 spo\u015Br\u00F3d innych piaszczysto-gliniastych produkt\u00F3w denudacji i akumulacji. Dominuje w nim frakcja py\u0142\u00F3w (0,002\u20130,063 mm) z\u0142o\u017Cona przede wszystkim z kwarcu z domieszk\u0105 skaleni, w\u0119glan\u00F3w, rzadziej innych minera\u0142\u00F3w. We frakcji podstawowej less\u00F3w dominuj\u0105 py\u0142y \u015Brednie (0,02\u20130,063 mm). Zr\u00F3\u017Cnicowanie wielko\u015Bci ziaren w ska\u0142ach jest bardzo ma\u0142e, jest to wi\u0119c ska\u0142a dobrze wysortowana. Zazwyczaj bezstrukturalna (homogeniczna), makro- i mikroporowata. Barwa przewa\u017Cnie \u017C\u00F3\u0142tawoszara, jasno\u017C\u00F3\u0142ta, a nawet p\u0142owa. Less jest sk\u0142onny do osiadania pod wp\u0142ywem zawilgocenia wzgl\u0119dnie dodatkowego obci\u0105\u017Cenia. W stanie suchym wykazuje sk\u0142onno\u015B\u0107 do p\u0119kania i tworzenia pionowych obrywisk, kt\u00F3re zanikaj\u0105, gdy jest wilgotny. Mamy do czynienia z lessami w\u0142a\u015Bciwymi, gdy frakcja 0,02\u20130,05 mm stanowi powy\u017Cej 50% analizowanej pr\u00F3by. Wyr\u00F3\u017Cnia si\u0119 ponadto lessy w\u0142a\u015Bciwe piaszczyste oraz less gliniasty. Lessy w\u0142a\u015Bciwe powstaj\u0105 w wyniku proces\u00F3w eolicznych (wiatrowych), je\u015Bli w fazie sedymentacji ich rola by\u0142a mniejsza, mamy do czynienia z utworami lessopodobnymi."@pl . . . "\u0631\u0627\u0633\u0628 \u0637\u0641\u0627\u0644\u064A"@ar . "( \uC601\uD654\uC5D0 \uB300\uD574\uC11C\uB294 \uD669\uD1A0 (\uC601\uD654) \uBB38\uC11C\uB97C \uCC38\uACE0\uD558\uC2ED\uC2DC\uC624.) \uD669\uD1A0(\u9EC3\u571F), \uB8B0\uC2A4(loess)\uB294 \uC77C\uBC18\uC801\uC73C\uB85C \uBC14\uB78C\uC5D0 \uC758\uD574 \uC6B4\uBC18\uB418\uC5B4 \uD1F4\uC801\uB41C \uD669\uAC08\uC0C9\uC774\uB098 \uC758 \uBBF8\uC138\uD55C \uBAA8\uB798\uC640 \uC810\uD1A0\uB97C \uAC00\uB9AC\uD0A4\uBA70, \uC8FC\uB85C \uC2E4\uD2B8 \uD06C\uAE30\uC758 \uC785\uC790\uB4E4\uB85C \uAD6C\uC131\uB418\uC5B4 \uC788\uB2E4. \uD0C4\uC0B0\uCE7C\uC298\uC5D0 \uC758\uD574 \uB290\uC2A8\uD558\uAC8C \uC811\uCC29\uB418\uC5B4 \uB300\uAC1C \uADE0\uC9C8\uD558\uACE0 \uCE35\uB9AC\uAC00 \uBC1C\uB2EC\uB418\uC5B4 \uC788\uC9C0 \uC54A\uC73C\uBA70 \uB2E4\uACF5\uC9C8\uC774\uB2E4. \uD604\uC7AC \uC911\uAD6D \uBD81\uBD80, \uC720\uB7FD \uC911\uBD80, \uBD81\uC544\uBA54\uB9AC\uCE74\uC758 \uBBF8\uC2DC\uC2DC\uD53C \uACC4\uACE1, \uC544\uB974\uD5E8\uD2F0\uB098\uC758 \uC0C1\uB2F9 \uBD80\uBD84, \uD0C0\uC9C0\uD0A4\uC2A4\uD0C4 \uB0A8\uBD80\uC5D0\uC11C \uCE74\uC790\uD750\uC2A4\uD0C4\uC5D0 \uAC78\uCE58\uB294 \uC911\uC559\uC544\uC2DC\uC544 \uB4F1\uC5D0 \uB110\uB9AC \uBD84\uD3EC\uB418\uC5B4 \uC788\uC73C\uBA70, \uC804\uCCB4 \uC9C0\uD45C\uBA74 \uC911 \uC57D 10%\uB97C \uCC28\uC9C0\uD558\uACE0 \uC788\uB2E4. \uD669\uD1A0\uB294 \uC7BF\uBE5B\uC774 \uB098\uB294 \uD669\uC0C9\uC758 \uC11D\uC601(\u77F3\u82F1)\uC774\uB098 \uC7A5\uC11D(\u9577\u77F3) \uB4F1\uC758 \uBBF8\uB9BD(\u5FAE\u7C92)\uC758 \uD1F4\uC801\uC73C\uB85C\uC11C, \uB545\uC774 \uBE44\uC625\uD558\uACE0 \uBD80\uB4DC\uB7EC\uC6CC\uC11C \uB18D\uACBD \uC0DD\uD65C\uC744 \uD558\uAE30\uC5D0\uB294 \uC544\uC8FC \uC801\uD569\uD588\uB2E4. \uD669\uD1A0 \uC548\uC5D0 \uD568\uC720\uD558\uACE0 \uC788\uB294 \uC720\uAE30\uBB3C\uC9C8\uC774 \uC0C1\uB300\uC801\uC73C\uB85C \uBE48\uC57D\uD568\uC5D0\uB3C4 \uD1A0\uC9C8\uC774 \uBE44\uC625\uD55C \uC774\uC720\uB85C\uB294, \uC591\uC774\uC628 \uAD50\uD658 \uC6A9\uB7C9\uACFC \uD22C\uACFC\uC131\uC774 \uB192\uAE30 \uB54C\uBB38\uC774\uB77C\uB294 \uC774\uB860\uC774 \uC81C\uC2DC\uB418\uC5B4 \uC788\uB2E4. \uC774 \uD669\uD1A0 \uC9C0\uB300\uC5D0\uC11C \uB18D\uC5C5 \uC0DD\uC0B0\uB825\uC758 \uBC1C\uC804\uC744 \uAE30\uCD08\uB85C \uBB38\uBA85\uC774 \uC131\uB9BD\uB418\uC5C8\uB2E4."@ko . . . . "L\u00F6ss"@nl . . . . "Spra\u0161 je \u00FAlomkovit\u00E1 usazen\u00E1 hornina v\u011Btrem (\u010Dili v odborn\u00E9 terminologii klastick\u00FD sediment eolick\u00E9ho p\u016Fvodu). Hlavn\u00ED slo\u017Ekou je jemn\u00FD k\u0159emit\u00FD prach (k\u0159emen, \u017Eivec a sl\u00EDda; typick\u00E1 velikost \u010D\u00E1stic 0,03-0,06 mm) s p\u0159\u00EDm\u011Bs\u00ED uhli\u010Ditanu v\u00E1penat\u00E9ho, vytv\u00E1\u0159ej\u00EDc\u00EDho sra\u017Een\u00E9 hrudky (\u201Ecicv\u00E1ry\u201C), a j\u00EDlu. Typickou sv\u011Btle okrovou barvu maj\u00ED na sv\u011Bdom\u00ED oxidy \u017Eeleza. Spra\u0161e jako prvn\u00ED definoval Charles Lyell. Porovn\u00E1val spra\u0161e z \u00FAdol\u00ED Mississippi se spra\u0161emi v \u00FAdol\u00ED R\u00FDna. P\u016Fvodn\u011B byl p\u0159esv\u011Bd\u010Den, \u017Ee jsou fluvi\u00E1ln\u00EDmi (\u0159\u00ED\u010Dn\u00EDmi) sedimenty. A\u017E v roce 1877 Ferdinand von Richthofen pouk\u00E1zal na eolick\u00FD (nav\u00E1t\u00FD) p\u016Fvod."@cs . . . "Loess"@ca . . . . "\u9EC3\u571F\u4E00\u79CD\u6D45\u9EC4\u6216\u8910\u9EC4\u8272\u7684\u571F\uFF0C\u9897\u7C92\u6210\u5206\u4EE5\u7C92\u7EA7\u4E3A\u4E3B\uFF08\u542B\u91CF\uFF1E50%\uFF09\uFF0C\u7269\u8D28\u7C92\u5F84\u5747\u4E00\uFF0C\u5177\u5B54\u9699\uFF0C\u65E0\u5C42\u7406\uFF0C\u758F\u677E\uFF0C\u5782\u76F4\u8282\u7406\u767C\u80B2\u3002\u5BCC\u542B\u78B3\u9178\u9499,\u6709\u65F6\u542B\u786B\u9178\u76D0\u6216\u6C2F\u5316\u7269\u76D0\u7C7B\uFF0C\u5177\u6709\u8089\u773C\u53EF\u89C1\u5B54\u9699\u7684\u7B2C\u56DB\u7EAA\u9646\u76F8\u6C89\u79EF\u7269\u3002\u9EC4\u571F\u6709\u65F6\u5177\u6709\u6E7F\u9677\u6027\u3002\u53E6\u5916\uFF0C\u5176\u5728\u77FF\u7269\u6210\u5206\u65B9\u9762\u9AD8\u5EA6\u590D\u6742\uFF0C\u591A\u8FBE60\u591A\u79CD\u77FF\u7269\uFF0C\u5305\u62EC\u5CA9\u6D46\u5CA9\u3001\u53D8\u8D28\u5CA9\u548C\u6C89\u79EF\u5CA9\u7684\u77FF\u7269\u6210\u5206\uFF0C\u800C\u4E14\u4E0E\u5176\u4E2D\u4EFB\u4F55\u4E00\u79CD\u5CA9\u77F3\u7684\u77FF\u7269\u6210\u5206\u90FD\u4E0D\u76F8\u540C\u3002\u5404\u5730\u533A\u9EC4\u571F\u77FF\u7269\u6210\u5206\u5927\u4F53\u76F8\u540C\uFF0C\u65E0\u8BBA\u77FF\u7269\u79CD\u7C7B\u8FD8\u662F\u767E\u5206\u542B\u91CF\u90FD\u57FA\u672C\u76F8\u4F3C\uFF0C\u5E76\u6709\u6BD4\u8F83\u591A\u7684\u6613\u98CE\u5316\u4E0D\u7A33\u5B9A\u77FF\u7269\u3002\u5728\u5316\u5B66\u6210\u5206\u4E2D\u542B\u91CF\u6700\u591A\u7684\u662FSiO2\u3001Al2O3\u3001CaO\u3001Na2O\uFF0C\u542B\u6709\u6BD4\u8F83\u591A\u7684\u6613\u6EB6\u76D0\u7C7B\uFF0C\u4E3B\u8981\u662F\uFF1A\u6C27\u5316\u7269\u3001\u78B3\u9178\u76D0\u3001\u786B\u9178\u76D0\u3001CaCO3,\u542B\u91CF\u572810\uFF05-16\uFF05\u4E4B\u95F4\u3002\u5728\u6240\u542B\u751F\u7269\u5316\u77F3\u65B9\u9762\u4EE5\u8010\u65F1\u8349\u672C\u690D\u7269\u82B1\u7C89\u548C\u8010\u5E72\u65F1\u52A8\u7269\u5316\u77F3\u4E3A\u4E3B\uFF0C\u800C\u4E14\u542B\u6709\u559C\u6696\u6E7F\u7684\u52A8\u690D\u7269\u5316\u77F3\u3002\u6700\u65E9\u674E\u5E0C\u970D\u82AC\uFF081877\u5E74\uFF09\u5BF9\u6B27\u6D32\u83B1\u8335\u6CB3\u6D41\u57DF\u53CA\u4E2D\u56FD\u5927\u9646\u7684\u9EC4\u571F\u63D0\u51FA\u7684\u5B9A\u4E49\u4E3A\uFF1A\u9EC4\uFF0D\u8910\u8272\uFF0C\u542B\u77F3\u7070\u8D28\uFF0C\u4EE5\u7C89\u571F\u4E3A\u4E3B\u7684\u7C89\u72B6\u571F\uFF1B\u6CA1\u6709\u5C42\u7406\uFF0C\u542B\u9646\u751F\u8717\u725B\uFF0C\u6709\u5782\u76F4\u8282\u7406\u3002\u5386\u53F2\u65B9\u9762\uFF0C\u201C\u9EC4\u571F\u201D\u4E00\u8BCD\uFF0C\u5728\u4E2D\u56FD\u53E4\u4EE3\u6587\u732E\u4E2D\u53CA\u6C11\u95F4\u5C31\u5DF2\u51FA\u73B0\u3002 \u897F\u65B9\u56FD\u5BB6\u572819\u4E16\u7EAA\u540E\u671F\u5C06\u5FB7\u56FD\u83B1\u8335\u6CB3\u6D41\u57DF\u7684\u9EC4\u8272\u677E\u6563\u5806\u79EF\u7269\u547D\u540D\u4E3A\u201Cl\u0153ss\u201D\uFF0C\u7531\u6B64\u97F3\u8BD1\u51FA\u82F1\uFF08loess\uFF09\u3001\u4FC4\uFF08\u041B\u0451\u0441\u0441\uFF09\u7B49\u6587\uFF0C\u4E0D\u540C\u5B66\u8005\u66FE\u4EE5\u4E0D\u540C\u89C2\u70B9\u63D0\u51FA\u9EC4\u571F\u7684\u5B9A\u4E49\u30021933\u5E74\u5965\u5E03\u9C81\u5207\u592B(\u0392.\u0391. \u041E\u0431\u0440\u0443\u0447\u0435\u0432)\u5C06\u6CA1\u6709\u5C42\u7406\u7684\u9EC4\u571F\u79F0\u4E3A\u539F\u751F\u9EC4\u571F\uFF0C\u5E76\u8BA4\u4E3A\u662F\u98CE\u6210\u6210\u56E0\u7684\uFF1B\u6B21\u751F\u9EC4\u571F\u662F\u5176\u4ED6\u5404\u79CD\u6210\u56E0\u5F62\u6210\u7684\u3002\u7531\u65BC\u51B0\u5DDD\u7684\u6D3B\u52D5\uFF0C\u628A\u56DB\u5468\u7684\u5CA9\u77F3\u7814\u78E8\u6210\u975E\u5E38\u5FAE\u7D30\u3001\u50CF\u9EB5\u7C89\u4E00\u6A23\u5E7C\u7D30\u7684\u5875\u571F\u3002\u9019\u4E9B\u5875\u571F\u4E7E\u4E86\u4EE5\u5F8C\uFF0C\u5F88\u5BB9\u6613\u88AB\u98A8\u5E36\u8D70\uFF0C\u9001\u5230\u5F88\u9060\u7684\u5730\u65B9\u53BB\uFF0C\u4E26\u7D2F\u7A4D\u8D77\u4F86\u3002\u7576\u9019\u4E9B\u5FAE\u7D30\u7684\u6CE5\u571F\u4E0D\u65B7\u7684\u6C89\u7A4D\uFF0C\u53EF\u4EE5\u5806\u6210\u5F88\u9AD8\u7684\u5C71\u3002 \u6709\u6642\u56E0\u6DCB\u6D17\u4F5C\u7528\u8F03\u5F37\u800C\u4F7F\u7C98\u7C92\u660E\u986F\u5F80\u5256\u9762\u4E0B\u5C64\u79FB\u52D5\uFF0C\u990A\u5206\u6709\u7684\u5DF2\u6D41\u5931\u800C\u5448\u9EC3\u3001\u9EC3\u68D5\u6216\u7D05\u68D5\u8272\u3002\u591A\u751F\u6210\u65BC\u4E18\u9675\u5730\u4E0A\u4E4B\u76F8\u5C0D\u5730\u5F62\u8F03\u5B89\u5B9A\u3001\u5761\u5EA6\u8D77\u4F0F\u8F03\u7DE9\u548C\u8655\u3002\u571F\u58E4\u591A\u5448\u5F31\u9178\u6027\uFF0C\u80A5\u6C83\u5EA6\u504F\u4F4E\uFF0C\u9808\u9032\u884C\u65BD\u80A5\u7BA1\u7406\u53CA\u6C34\u571F\u4FDD\u6301\uFF0C\u624D\u53EF\u505A\u8FB2\u7267\u7528\u5730\u3002\u6B64\u571F\u58E4\u5728\u65B0\u5206\u985E\u4E0A\u5C6C\u6216\u6DCB\u6EB6\u571F\u3002\u3002"@zh . . . . . "Less \u2013 pylasta ska\u0142a osadowa, wyselekcjonowana i deponowana na drodze eolicznej, a wi\u0119c w warunkach wzgl\u0119dnie suchego klimatu, na co wskazuje m.in. rozmieszczenie strefowe lub zwi\u0105zek lessu z okre\u015Blonym pi\u0119trem hipsometrycznym. W obszarach wilgotniejszych osad o takich cechach nie wyodr\u0119bnia si\u0119 spo\u015Br\u00F3d innych piaszczysto-gliniastych produkt\u00F3w denudacji i akumulacji. Less jest sk\u0142onny do osiadania pod wp\u0142ywem zawilgocenia wzgl\u0119dnie dodatkowego obci\u0105\u017Cenia. W stanie suchym wykazuje sk\u0142onno\u015B\u0107 do p\u0119kania i tworzenia pionowych obrywisk, kt\u00F3re zanikaj\u0105, gdy jest wilgotny."@pl . "Less"@pl . . "El loess (del alem\u00E1n de Suiza l\u00F6sch, en alem\u00E1n com\u00FAn: L\u00F6ss) son dep\u00F3sitos sedimentarios limosos de origen e\u00F3lico."@es . . . . . . . "\u041B\u0451\u0441\u0441 (\u043D\u0435\u043C. L\u00F6\u00DF \u0438\u043B\u0438 L\u00F6ss \u2014 \u0440\u044B\u0445\u043B\u044B\u0439, \u043E\u0441\u044B\u043F\u0430\u044E\u0449\u0438\u0439\u0441\u044F) \u2014 \u043E\u0441\u0430\u0434\u043E\u0447\u043D\u0430\u044F \u0433\u043E\u0440\u043D\u0430\u044F \u043F\u043E\u0440\u043E\u0434\u0430, \u043D\u0435\u0441\u043B\u043E\u0438\u0441\u0442\u0430\u044F, \u0441\u0443\u0433\u043B\u0438\u043D\u0438\u0441\u0442\u043E-\u0441\u0443\u043F\u0435\u0441\u0447\u0430\u043D\u0430\u044F, \u0438\u043C\u0435\u0435\u0442 \u0441\u0432\u0435\u0442\u043B\u043E-\u0436\u0451\u043B\u0442\u044B\u0439 \u0438\u043B\u0438 \u043F\u0430\u043B\u0435\u0432\u044B\u0439 \u0446\u0432\u0435\u0442, \u0441\u043B\u043E\u0436\u0435\u043D\u0430 \u043F\u0440\u0435\u0438\u043C\u0443\u0449\u0435\u0441\u0442\u0432\u0435\u043D\u043D\u043E \u043F\u044B\u043B\u0435\u0432\u0430\u0442\u044B\u043C\u0438 \u0437\u0451\u0440\u043D\u0430\u043C\u0438. \u0417\u0430\u043B\u0435\u0433\u0430\u0435\u0442 \u0432 \u0432\u0438\u0434\u0435 \u043F\u043E\u043A\u0440\u043E\u0432\u0430 \u043E\u0442 \u043D\u0435\u0441\u043A\u043E\u043B\u044C\u043A\u0438\u0445 \u043C\u0435\u0442\u0440\u043E\u0432 \u0434\u043E 50\u2014100 \u043C \u2014 \u043D\u0430 \u0432\u043E\u0434\u043E\u0440\u0430\u0437\u0434\u0435\u043B\u0430\u0445, \u0441\u043A\u043B\u043E\u043D\u0430\u0445 \u0438 \u0434\u0440\u0435\u0432\u043D\u0438\u0445 \u0442\u0435\u0440\u0440\u0430\u0441\u0430\u0445 \u0434\u043E\u043B\u0438\u043D."@ru . . . .