@prefix rdfs: . @prefix dbr: . dbr:Weichselian_glaciation rdfs:label "Weichselien"@nl , "Weichselian glaciation"@en , "\u0412\u0456\u0441\u043B\u0438\u043D\u0441\u044C\u043A\u0435 \u0437\u043B\u0435\u0434\u0435\u043D\u0456\u043D\u043D\u044F"@uk , "Zlodowacenie p\u00F3\u0142nocnopolskie"@pl , "Glaciazione weichseliana"@it , "\u062A\u062C\u0645\u062F \u0641\u0627\u064A\u0633\u0644\u064A"@ar , "Weichsel (geologi)"@sv , "Weichsel-Kaltzeit"@de , "Glaciation vistulienne"@fr , "Glaciaci\u00F3n Weichseliense"@es , "\uBC14\uC774\uD750\uC824 \uBE59\uAE30"@ko ; rdfs:comment "\uBC14\uC774\uD750\uC824 \uBE59\uAE30(\uB3C5\uC77C\uC5B4: Weichsel-Eiszeit)\uB294 \uBD81\uC720\uB7FD\uC758 \uB9C8\uC9C0\uB9C9 \uBE59\uAE30\uB2E4. \uAC19\uC740 \uC2DC\uAE30\uC5D0 \uC54C\uD504\uC2A4 \uACE0\uC0B0\uC9C0\uB300\uC5D0\uC11C\uB294 \uBDD4\uB984 \uBE59\uAE30\uAC00 \uC9C4\uD589\uB418\uC5C8\uB2E4. \uC2A4\uCE78\uB514\uB098\uBE44\uC544\uC0B0\uB9E5\uC5D0\uC11C \uC290\uB808\uC2A4\uBE44\uD788\uD640\uC288\uD0C0\uC778, \uBE0C\uB780\uB374\uBD80\uB974\uD06C \uBCC0\uACBD, \uAE4C\uC9C0 \uD3BC\uCCD0\uC9C4 \uAC70\uB300\uD55C \uBE59\uC0C1\uC778 \uD398\uB178\uC2A4\uCE78\uB514\uC544 \uBE59\uC0C1(Fenno-Scandian ice sheet)\uC73C\uB85C \uADF8 \uD2B9\uC9D5\uC774 \uADDC\uC815\uB41C\uB2E4. \uBC14\uC774\uD750\uC824 \uBE59\uAE30\uB294 \uC9C0\uAE08\uC73C\uB85C\uBD80\uD130 11\uB9CC 5000\uB144 \uC804\uBD80\uD130 1\uB9CC 1700\uB144 \uC804\uAE4C\uC9C0 \uC9C4\uD589\uB418\uC5C8\uB2E4. \uBD81\uC720\uB7FD\uC5D0\uC11C \uC9C4\uD589\uB41C \uD64D\uC801\uC138 \uBE59\uD558\uAE30\uC758 \uBE59\uAE30\uB4E4 \uC911 \uAC00\uC7A5 \uCD5C\uADFC\uC758 \uBE59\uAE30\uC600\uACE0, \uBC14\uC774\uD750\uC824 \uBE59\uAE30\uAC00 \uB05D\uB09C \uC2DC\uC810\uC774 \uD64D\uC801\uC138\uC758 \uB05D\uACFC \uCDA9\uC801\uC138\uC758 \uC2DC\uC791\uC5D0 \uB300\uB7B5 \uACB9\uCE5C\uB2E4. \uBC14\uC774\uD750\uC824\uC774\uB780 \uBE44\uC2A4\uC640\uAC15\uC758 \uB3C5\uC77C\uC5B4 \uC774\uB984\uC774\uBA70, \uB3C5\uC77C \uC9C0\uC9C8\uD559\uC790 \uAC00 \uBA85\uBA85\uD588\uB2E4."@ko , "\u064A\u0634\u064A\u0631 \u062A\u062C\u0645\u062F \u0641\u0627\u064A\u0633\u0644\u064A \u0623\u0648 \u062A\u062C\u0645\u062F \u0641\u0627\u064A\u0633\u0625\u064A\u0644\u064A\u0627\u0646 \u0625\u0644\u0649 \u0627\u0644\u0639\u0635\u0631 \u0627\u0644\u062C\u0644\u064A\u062F\u064A \u0627\u0644\u0623\u062E\u064A\u0631 \u0648\u0627\u0644\u062A\u062C\u0645\u062F \u0627\u0644\u0645\u0631\u062A\u0628\u0637 \u0628\u0647 \u0641\u064A \u0627\u0644\u0623\u062C\u0632\u0627\u0621 \u0627\u0644\u0634\u0645\u0627\u0644\u064A\u0629 \u0645\u0646 \u0623\u0648\u0631\u0648\u0628\u0627. \u0648\u0641\u064A \u0645\u0646\u0637\u0642\u0629 \u062C\u0628\u0627\u0644 \u0627\u0644\u0623\u0644\u0628 \u064A\u0642\u0627\u0628\u0644 \u062A\u062C\u0645\u062F \u0648\u0648\u0631\u0645. \u064A\u062A\u0633\u0645 \u0628\u0648\u062C\u0648\u062F \u0635\u0641\u064A\u062D\u0629 \u062C\u0644\u064A\u062F\u064A\u0629 (\u0627\u0644\u0635\u0641\u064A\u062D\u0629 \u0627\u0644\u062C\u0644\u064A\u062F\u064A\u0629 \u0627\u0644\u0641\u064A\u0646\u0648\u0633\u0643\u0646\u062F\u064A\u0629) \u0627\u0644\u062A\u064A \u062A\u0646\u0628\u0633\u0637 \u0645\u0646 \u0627\u0644\u062C\u0628\u0627\u0644 \u0627\u0644\u0625\u0633\u0643\u0646\u062F\u0646\u0627\u0641\u064A\u0629 \u0648\u062A\u0645\u062A\u062F \u0628\u0639\u064A\u062F\u064B\u0627 \u0644\u062A\u0635\u0644 \u0625\u0644\u0649 \u0634\u0644\u064A\u0633\u0641\u064A\u0634 \u0647\u0648\u0644\u0634\u062A\u0627\u064A\u0646 \u0648\u0645\u0631\u063A\u0631\u064A\u0641\u064A\u0629 \u0628\u0631\u0627\u0646\u062F\u0646\u0628\u0648\u0631\u063A \u0648\u0634\u0645\u0627\u0644 \u063A\u0631\u0628 \u0631\u0648\u0633\u064A\u0627. \u0641\u064A \u0634\u0645\u0627\u0644 \u0623\u0648\u0631\u0648\u0628\u0627\u060C \u0643\u0627\u0646\u062A \u0623\u0635\u063A\u0631 \u0627\u0644\u0623\u062F\u0648\u0627\u0631 \u0627\u0644\u062C\u0644\u064A\u062F\u064A\u0629 \u0644\u0644\u0639\u0635\u0631 \u0627\u0644\u062C\u0644\u064A\u062F\u064A \u0627\u0644\u062D\u062F\u064A\u062B \u0627\u0644\u0623\u0642\u0631\u0628. \u0643\u0627\u0646\u062A \u0627\u0644\u0641\u062A\u0631\u0629 \u0627\u0644\u062F\u0627\u0641\u0626\u0629 \u0627\u0644\u0633\u0627\u0628\u0642\u0629 \u0641\u064A \u0647\u0630\u0647 \u0627\u0644\u0645\u0646\u0637\u0642\u0629 \u0647\u064A \u0627\u0644\u0641\u062A\u0631\u0629 \u0627\u0644\u0625\u064A\u0645\u064A\u0627\u0646\u064A\u0629 \u0628\u064A\u0646 \u0627\u0644\u0639\u0635\u0648\u0631 \u0627\u0644\u062C\u0644\u064A\u062F\u064A\u0629. \u0628\u062F\u0623\u062A \u0627\u0644\u0641\u062A\u0631\u0629 \u0627\u0644\u0628\u0627\u0631\u062F\u0629 \u0627\u0644\u0623\u062E\u064A\u0631\u0629 \u0645\u0646\u0630 \u0646\u062D\u0648 115.000 \u0639\u0627\u0645 \u0648\u0627\u0646\u062A\u0647\u062A \u0645\u0646\u0630 11.700. \u062A\u062A\u0642\u0627\u0628\u0644 \u0646\u0647\u0627\u064A\u062A\u0647\u0627 \u0645\u0639 \u0646\u0647\u0627\u064A\u0629 \u0627\u0644\u0639\u0635\u0631 \u0627\u0644\u062C\u0644\u064A\u062F\u064A \u0627\u0644\u062D\u062F\u064A\u062B \u0627\u0644\u0623\u0642\u0631\u0628 \u0648\u0645\u0639 \u0628\u062F\u0627\u064A\u0629 \u0639\u0635\u0631 \u0627\u0644\u0647\u0648\u0644\u0648\u0633\u064A\u0646."@ar , "La glaciaci\u00F3n Weichseliense fue el \u00FAltimo per\u00EDodo glacial y su glaciaci\u00F3n asociada en el norte de Europa. En la regi\u00F3n alpina corresponde a la glaciaci\u00F3n de W\u00FCrm. Se caracteriz\u00F3 por una gran capa de hielo (la capa de hielo Fenno- Escandinava ) que se extendi\u00F3 desde las monta\u00F1as escandinavas \u200B y se extendi\u00F3 hasta la costa este de Schleswig-Holstein, la Marcha de Brandeburgo y el noroeste de Rusia ."@es , "La glaciation vistulienne ou vistulien (ou en conservant le nom allemand weichs\u00E9lien ou glaciation weichs\u00E9lienne) est le nom donn\u00E9 \u00E0 la derni\u00E8re glaciation en Europe du Nord (Scandinavie, une grande partie de la Grande-Bretagne, la Pologne et le nord-est de l'Allemagne) et est utilis\u00E9 par extension pour parler de l'ensemble de l'inlandsis eurasiatique. Elle est l'\u00E9quivalent de la glaciation du W\u00FCrm ou W\u00FCrmien des Alpes.Le Vistulien est dat\u00E9 de l'\u00E9poque du Pl\u00E9istoc\u00E8ne sup\u00E9rieur au sein de la p\u00E9riode du Quaternaire."@fr , "Het Weichselien (Vlaanderen: Weichseliaan of Weichsel), ook wel Weichselglaciaal genoemd, is een vooral in het noordwesten van Europa gebruikt tijdperk in de geologische tijdschaal of een stratigrafische indeling met de rang van een etage. Het Weichselien bevat de afzettingen uit de laatste ijstijd en is onderdeel van het Pleistoceen. Het heeft een ouderdom van ongeveer 116 tot 11,7 ka BP (116 tot 11,7 duizend jaar geleden). Het Weichselien komt na of ligt op het Eemien en wordt gevolgd door het Holoceen. Samen met het Eemien maakt het Weichselien deel uit van het Laat Pleistoceen. De wetenschappelijke term voor een koudere periode zoals het Weichselien is glaciaal, echter in de praktijk wordt vaak ook de term \"ijstijd\" gebruikt. Gedurende het Weichselien bereikte het Scandinavische landij"@nl , "Glaciazione weichseliana (anche conosciuta come Weichseliano, glaciazione Vistuliana o Weichsel) \u00E8 il nome che si d\u00E0 all'ultimo periodo glaciale e alla glaciazione associata in Europa settentrionale. Nell'area alpina, corrisponde alla glaciazione W\u00FCrm. Era caratterizzata da una vasta calotta di ghiaccio che si estendeva dai Monti scandinavi alla costa est dello Schleswig-Holstein, alla Marca di Brandenburgo e alla Russia nord-occidentale."@it , "Als Weichsel-Kaltzeit, Weichsel-Glazial oder Weichsel-Komplex wird die letzte Kaltzeit des K\u00E4nozoischen Eiszeitalters und die damit verbundene Vergletscherung f\u00FCr Nordeuropa und das n\u00F6rdliche Mitteleuropa bezeichnet. Umgangssprachlich wird sie auch Weichsel-Eiszeit oder Weichsel-Zeit benannt, im Alpenraum dagegen W\u00FCrm-Kaltzeit. Kennzeichnend war ein gro\u00DFer Eisschild, der vom skandinavischen Hochgebirge ausging und sich bis an die schleswig-holsteinische Ostk\u00FCste, in die Mark Brandenburg und nach Nordrussland erstreckte."@de , "\u0412\u0456\u0441\u043B\u0438\u043D\u0441\u044C\u043A\u0435 \u0437\u043B\u0435\u0434\u0435\u043D\u0456\u043D\u043D\u044F \u043D\u0430\u0437\u0432\u0430 \u043E\u0441\u0442\u0430\u043D\u043D\u044C\u043E\u0433\u043E \u043B\u044C\u043E\u0434\u043E\u0432\u0438\u043A\u043E\u0432\u043E\u0433\u043E \u043F\u0435\u0440\u0456\u043E\u0434\u0443 \u0442\u0430 \u043F\u043E\u0432'\u044F\u0437\u0430\u043D\u043E\u0433\u043E \u0456\u0437 \u043D\u0438\u043C \u0437\u043B\u0435\u0434\u0435\u043D\u0456\u043D\u043D\u044F \u041F\u0456\u0432\u043D\u0456\u0447\u043D\u043E\u0457 \u0404\u0432\u0440\u043E\u043F\u0438.\u0425\u0430\u0440\u0430\u043A\u0442\u0435\u0440\u0438\u0437\u0443\u0432\u0430\u0432\u0441\u044F \u0432\u0435\u043B\u0438\u043A\u0438\u043C \u043B\u044C\u043E\u0434\u043E\u0432\u0438\u043A\u043E\u0432\u0438\u043C \u0449\u0438\u0442\u043E\u043C (\u0424\u0435\u043D\u043D\u043E-\u0441\u043A\u0430\u043D\u0434\u0438\u043D\u0430\u0432\u0441\u044C\u043A\u0438\u0439 \u043B\u044C\u043E\u0434\u043E\u0432\u0438\u043A\u043E\u0432\u0438\u0439 \u0449\u0438\u0442), \u0449\u043E \u043F\u043E\u0448\u0438\u0440\u044E\u0432\u0430\u0432\u0441\u044F \u0432\u0456\u0434 \u0421\u043A\u0430\u043D\u0434\u0438\u043D\u0430\u0432\u0441\u044C\u043A\u0438\u0445 \u0433\u0456\u0440\u0456 \u043F\u0440\u043E\u0441\u0442\u044F\u0433\u0430\u0432\u0441\u044F \u0430\u0436 \u0434\u043E \u0441\u0445\u0456\u0434\u043D\u043E\u0433\u043E \u0443\u0437\u0431\u0435\u0440\u0435\u0436\u0436\u044F \u0428\u043B\u0435\u0437\u0432\u0456\u0433-\u0413\u043E\u043B\u044C\u0448\u0442\u0435\u0439\u043D\u0443, \u0426\u0435\u043D\u0442\u0440\u0430\u043B\u044C\u043D\u043E\u0457 \u041D\u0456\u043C\u0435\u0447\u0447\u0438\u043D\u0438 \u0442\u0430 \u041F\u0456\u0432\u043D\u0456\u0447\u043D\u043E-\u0417\u0430\u0445\u0456\u0434\u043D\u043E\u0457 \u0420\u043E\u0441\u0456\u0457. \u0423 \u041F\u0456\u0432\u043D\u0456\u0447\u043D\u0456\u0439 \u0404\u0432\u0440\u043E\u043F\u0456 \u0446\u0435 \u043D\u0430\u0439\u043E\u0441\u0442\u0430\u043D\u043D\u0456\u0448\u0438\u0439 \u0437 \u043B\u044C\u043E\u0434\u043E\u0432\u0438\u043A\u0456\u0432 \u043F\u043B\u0435\u0439\u0441\u0442\u043E\u0446\u0435\u043D\u043E\u0432\u043E\u0433\u043E \u043B\u044C\u043E\u0434\u043E\u0432\u0438\u043A\u043E\u0432\u043E\u0433\u043E \u043F\u0435\u0440\u0456\u043E\u0434\u0443.\u041F\u043E\u043F\u0435\u0440\u0435\u0434\u043D\u0456\u043C \u0442\u0435\u043F\u043B\u0438\u043C \u043F\u0435\u0440\u0456\u043E\u0434\u043E\u043C \u0443 \u0446\u044C\u043E\u043C\u0443 \u0440\u0435\u0433\u0456\u043E\u043D\u0456 \u0431\u0443\u0432 \u0435\u0454\u043C\u0441\u044C\u043A\u0438\u0439 \u0456\u043D\u0442\u0435\u0440\u0433\u043B\u044F\u0446\u0456\u0430\u043B.\u041E\u0441\u0442\u0430\u043D\u043D\u0456\u0439 \u0445\u043E\u043B\u043E\u0434\u043D\u0438\u0439 \u043F\u0435\u0440\u0456\u043E\u0434 \u0440\u043E\u0437\u043F\u043E\u0447\u0430\u0432\u0441\u044F \u043F\u0440\u0438\u0431\u043B\u0438\u0437\u043D\u043E 115 000 \u0440\u043E\u043A\u0456\u0432 \u0442\u043E\u043C\u0443 \u0456 \u0437\u0430\u043A\u0456\u043D\u0447\u0438\u0432\u0441\u044F 11 700 \u0440\u043E\u043A\u0456\u0432 \u0442\u043E\u043C\u0443."@uk , "Weichsel var den senaste av de fyra stora nedisningarna (istiderna) i norra Europa under Pleistocen. Den varade i cirka 100 000 \u00E5r, n\u00E5dde sin st\u00F6rsta utbredning f\u00F6r 20 000\u201318 000 \u00E5r sedan och det mesta av isen sm\u00E4lte bort under de f\u00F6ljande 10 000 \u00E5ren. Namnet kommer fr\u00E5n det tyskspr\u00E5kiga namnet, Weichsel, p\u00E5 den flod, Wis\u0142a, i Polen dit glaci\u00E4rens maximala utbredning n\u00E5dde. Andra delar av samma nedisning g\u00E5r under ben\u00E4mningen Wisconsin (i Nordamerika), W\u00FCrm (i Alperna) och Devensian (Brittiska \u00F6arna). Nedisningen under Weichsel-istiden str\u00E4ckte sig vid maximum \u00E4nda ner till norra Tyskland och t\u00E4ckte hela Skandinavien utom de v\u00E4stra delarna av Jylland som var f\u00F6rbundna med Brittiska \u00F6arna via Doggerland (nuvarande Nordsj\u00F6n torrlagd)."@sv , "The Weichselian glaciation was the last glacial period and its associated glaciation in northern parts of Europe. In the Alpine region it corresponds to the W\u00FCrm glaciation. It was characterized by a large ice sheet (the Fenno-Scandian ice sheet) that spread out from the Scandinavian Mountains and extended as far as the east coast of Schleswig-Holstein, northern Poland and Northwest Russia. This glaciation is also known as the Weichselian ice age (German: Weichsel-Eiszeit), Vistulian glaciation, Weichsel or, less commonly, the Weichsel glaciation, Weichselian cold period (Weichsel-Kaltzeit), Weichselian glacial (Weichsel-Glazial), Weichselian Stage or, rarely, the Weichselian complex (Weichsel-Komplex)."@en , "Zlodowacenie p\u00F3\u0142nocnopolskie, zlodowacenie ba\u0142tyckie, ostatnie zlodowacenie, vistulian \u2013 najm\u0142odsze ze zlodowace\u0144 plejstoce\u0144skich. Trwa\u0142o od 115 tys. lat temu do 11,7 tys. lat b2k (przed rokiem 2000). Poprzedzi\u0142 je interglacja\u0142 eemski, a po nim nast\u0105pi\u0142 holocen \u2013 uznawany za otwarty interglacja\u0142."@pl . @prefix foaf: . dbr:Weichselian_glaciation foaf:depiction , , , , . @prefix dcterms: . @prefix dbc: . dbr:Weichselian_glaciation dcterms:subject dbc:Last_Glacial_Maximum , dbc:Last_Glacial_Period , dbc:Pleistocene_events . @prefix dbo: . dbr:Weichselian_glaciation dbo:wikiPageID 20930890 ; dbo:wikiPageRevisionID 1123789001 ; dbo:wikiPageWikiLink dbr:Pleistocene , dbr:White_Sea , dbr:Kiloannus , dbr:Glacial , , dbr:Europe , dbr:Sommen , dbr:Novaya_Zemlya , dbr:Spruce , dbr:South_Norway , dbr:Ice_field , dbr:Baltic_states , dbr:Mysis , dbr:Northern_Europe , dbr:Glaciation , , dbr:Larch , dbr:Joint_valley_landscape , dbr:Heliophyte , dbr:Kandalaksha_Gulf , dbr:Ice_divide , , dbr:Schalkholz , dbr:Glacier , dbr:Oldest_Dryas , dbr:Baltic_Ice_Lake , dbr:Glacial_relict , dbr:Alder , dbr:Salvelinus , , dbr:Landslide , dbr:Willow , dbr:Great_Britain , dbr:Glacial_lake_outburst_flood , dbc:Last_Glacial_Maximum , , dbr:Ice_cap , dbr:Norrland , , dbr:North_Atlantic_Deep_Water , dbr:Northwest_Russia , dbr:Year , dbr:Lake_Ladoga , dbr:Jan_Mangerud , dbr:Holocene , , dbr:Ice_age , dbr:German-language , dbr:Skuleberget , dbr:Sagebrush , dbr:Northwestern_Russia , , dbr:Interglacial , , dbr:Schleswig-Holstein , dbr:Vistula , dbr:Dithmarschen , dbr:Timeline_of_glaciation , dbr:Astrid_Cleve , dbr:Dwarf_birch , dbr:Last_glacial_period , , dbr:Bothnian_Sea , , dbr:Toba_catastrophe_theory , dbr:Fennoscandian_Ice_Sheet , dbr:Groundwater_recharge , dbr:Cyperaceae , , dbr:Lake_Onega , dbr:Glaciology , dbr:Last_Glacial_Maximum , dbr:Barents_Sea , , dbr:Outwash_plain , dbr:Ice_sheet , dbr:Greenland , dbr:Esker , dbr:Scandinavian_Mountains , dbr:Proglacial_lake , dbr:Isostatic_rebound , dbr:Kola_Peninsula , dbr:Eemian_interglacial , , dbr:Ernst_Antevs , , dbr:Stockholm_archipelago , , dbr:Sarek_National_Park , dbr:Meiendorf_Interstadial , dbr:Thousand , dbr:Ireland , dbr:Canadian_Arctic_Archipelago , dbr:Ice-dammed_lake , dbr:High_Coast , dbr:Pore_pressure , dbr:Sandthorn , dbr:Patagonia , dbr:Deglaciation , dbr:Alps , dbr:Norra_Kvarken , dbr:Quaternary , dbr:Bornholm , , dbr:Devensian_glaciation , dbr:Interstadial , dbc:Last_Glacial_Period , dbr:Wisconsin_glaciation , dbr:Bering_Strait , dbr:Younger_Dryas , dbc:Pleistocene_events , , dbr:Mollusc_shell , dbr:Pskov_Oblast , dbr:Poland , dbr:Before_Present , , dbr:Gotland , dbr:Juniper , dbr:Andes , dbr:Sommen_charr , dbr:Older_Dryas ; dbo:wikiPageExternalLink . @prefix owl: . @prefix dbpedia-it: . dbr:Weichselian_glaciation owl:sameAs dbpedia-it:Glaciazione_weichseliana . @prefix ns8: . dbr:Weichselian_glaciation owl:sameAs ns8:UA5K , , , , . @prefix dbpedia-fr: . dbr:Weichselian_glaciation owl:sameAs dbpedia-fr:Glaciation_vistulienne . @prefix dbpedia-da: . dbr:Weichselian_glaciation owl:sameAs dbpedia-da:Weichsel-istiden , , , , . @prefix yago-res: . dbr:Weichselian_glaciation owl:sameAs yago-res:Weichselian_glaciation , , . @prefix dbpedia-nl: . dbr:Weichselian_glaciation owl:sameAs dbpedia-nl:Weichselien . @prefix dbpedia-de: . dbr:Weichselian_glaciation owl:sameAs dbpedia-de:Weichsel-Kaltzeit , , . @prefix wikidata: . dbr:Weichselian_glaciation owl:sameAs wikidata:Q14664222 . @prefix dbp: . @prefix dbt: . dbr:Weichselian_glaciation dbp:wikiPageUsesTemplate dbt:Reflist , dbt:Farblegende , dbt:Short_description , dbt:North_German_glaciations , dbt:ISBN , dbt:Evolution_of_the_Baltic_Sea , dbt:Citation , dbt:Notelist-ua , dbt:Efn-ua , dbt:Ill ; dbo:thumbnail ; dbo:abstract "\u0412\u0456\u0441\u043B\u0438\u043D\u0441\u044C\u043A\u0435 \u0437\u043B\u0435\u0434\u0435\u043D\u0456\u043D\u043D\u044F \u043D\u0430\u0437\u0432\u0430 \u043E\u0441\u0442\u0430\u043D\u043D\u044C\u043E\u0433\u043E \u043B\u044C\u043E\u0434\u043E\u0432\u0438\u043A\u043E\u0432\u043E\u0433\u043E \u043F\u0435\u0440\u0456\u043E\u0434\u0443 \u0442\u0430 \u043F\u043E\u0432'\u044F\u0437\u0430\u043D\u043E\u0433\u043E \u0456\u0437 \u043D\u0438\u043C \u0437\u043B\u0435\u0434\u0435\u043D\u0456\u043D\u043D\u044F \u041F\u0456\u0432\u043D\u0456\u0447\u043D\u043E\u0457 \u0404\u0432\u0440\u043E\u043F\u0438.\u0425\u0430\u0440\u0430\u043A\u0442\u0435\u0440\u0438\u0437\u0443\u0432\u0430\u0432\u0441\u044F \u0432\u0435\u043B\u0438\u043A\u0438\u043C \u043B\u044C\u043E\u0434\u043E\u0432\u0438\u043A\u043E\u0432\u0438\u043C \u0449\u0438\u0442\u043E\u043C (\u0424\u0435\u043D\u043D\u043E-\u0441\u043A\u0430\u043D\u0434\u0438\u043D\u0430\u0432\u0441\u044C\u043A\u0438\u0439 \u043B\u044C\u043E\u0434\u043E\u0432\u0438\u043A\u043E\u0432\u0438\u0439 \u0449\u0438\u0442), \u0449\u043E \u043F\u043E\u0448\u0438\u0440\u044E\u0432\u0430\u0432\u0441\u044F \u0432\u0456\u0434 \u0421\u043A\u0430\u043D\u0434\u0438\u043D\u0430\u0432\u0441\u044C\u043A\u0438\u0445 \u0433\u0456\u0440\u0456 \u043F\u0440\u043E\u0441\u0442\u044F\u0433\u0430\u0432\u0441\u044F \u0430\u0436 \u0434\u043E \u0441\u0445\u0456\u0434\u043D\u043E\u0433\u043E \u0443\u0437\u0431\u0435\u0440\u0435\u0436\u0436\u044F \u0428\u043B\u0435\u0437\u0432\u0456\u0433-\u0413\u043E\u043B\u044C\u0448\u0442\u0435\u0439\u043D\u0443, \u0426\u0435\u043D\u0442\u0440\u0430\u043B\u044C\u043D\u043E\u0457 \u041D\u0456\u043C\u0435\u0447\u0447\u0438\u043D\u0438 \u0442\u0430 \u041F\u0456\u0432\u043D\u0456\u0447\u043D\u043E-\u0417\u0430\u0445\u0456\u0434\u043D\u043E\u0457 \u0420\u043E\u0441\u0456\u0457. \u0423 \u041F\u0456\u0432\u043D\u0456\u0447\u043D\u0456\u0439 \u0404\u0432\u0440\u043E\u043F\u0456 \u0446\u0435 \u043D\u0430\u0439\u043E\u0441\u0442\u0430\u043D\u043D\u0456\u0448\u0438\u0439 \u0437 \u043B\u044C\u043E\u0434\u043E\u0432\u0438\u043A\u0456\u0432 \u043F\u043B\u0435\u0439\u0441\u0442\u043E\u0446\u0435\u043D\u043E\u0432\u043E\u0433\u043E \u043B\u044C\u043E\u0434\u043E\u0432\u0438\u043A\u043E\u0432\u043E\u0433\u043E \u043F\u0435\u0440\u0456\u043E\u0434\u0443.\u041F\u043E\u043F\u0435\u0440\u0435\u0434\u043D\u0456\u043C \u0442\u0435\u043F\u043B\u0438\u043C \u043F\u0435\u0440\u0456\u043E\u0434\u043E\u043C \u0443 \u0446\u044C\u043E\u043C\u0443 \u0440\u0435\u0433\u0456\u043E\u043D\u0456 \u0431\u0443\u0432 \u0435\u0454\u043C\u0441\u044C\u043A\u0438\u0439 \u0456\u043D\u0442\u0435\u0440\u0433\u043B\u044F\u0446\u0456\u0430\u043B.\u041E\u0441\u0442\u0430\u043D\u043D\u0456\u0439 \u0445\u043E\u043B\u043E\u0434\u043D\u0438\u0439 \u043F\u0435\u0440\u0456\u043E\u0434 \u0440\u043E\u0437\u043F\u043E\u0447\u0430\u0432\u0441\u044F \u043F\u0440\u0438\u0431\u043B\u0438\u0437\u043D\u043E 115 000 \u0440\u043E\u043A\u0456\u0432 \u0442\u043E\u043C\u0443 \u0456 \u0437\u0430\u043A\u0456\u043D\u0447\u0438\u0432\u0441\u044F 11 700 \u0440\u043E\u043A\u0456\u0432 \u0442\u043E\u043C\u0443."@uk , "The Weichselian glaciation was the last glacial period and its associated glaciation in northern parts of Europe. In the Alpine region it corresponds to the W\u00FCrm glaciation. It was characterized by a large ice sheet (the Fenno-Scandian ice sheet) that spread out from the Scandinavian Mountains and extended as far as the east coast of Schleswig-Holstein, northern Poland and Northwest Russia. This glaciation is also known as the Weichselian ice age (German: Weichsel-Eiszeit), Vistulian glaciation, Weichsel or, less commonly, the Weichsel glaciation, Weichselian cold period (Weichsel-Kaltzeit), Weichselian glacial (Weichsel-Glazial), Weichselian Stage or, rarely, the Weichselian complex (Weichsel-Komplex). In Northern Europe it was the youngest of the glacials of the Pleistocene ice age. The preceding warm period in this region was the Eemian interglacial. The last cold period began about 115,000 years ago and ended 11,700 years ago. Its end corresponds with the end of the Pleistocene epoch and the start of the Holocene. The German geologist (1858\u20131944) named it using the German name (Weichsel) of the Vistula (Polish: Wis\u0142a) in present-day Poland."@en , "Het Weichselien (Vlaanderen: Weichseliaan of Weichsel), ook wel Weichselglaciaal genoemd, is een vooral in het noordwesten van Europa gebruikt tijdperk in de geologische tijdschaal of een stratigrafische indeling met de rang van een etage. Het Weichselien bevat de afzettingen uit de laatste ijstijd en is onderdeel van het Pleistoceen. Het heeft een ouderdom van ongeveer 116 tot 11,7 ka BP (116 tot 11,7 duizend jaar geleden). Het Weichselien komt na of ligt op het Eemien en wordt gevolgd door het Holoceen. Samen met het Eemien maakt het Weichselien deel uit van het Laat Pleistoceen. De wetenschappelijke term voor een koudere periode zoals het Weichselien is glaciaal, echter in de praktijk wordt vaak ook de term \"ijstijd\" gebruikt. Gedurende het Weichselien bereikte het Scandinavische landijs het noorden van Duitsland en Denemarken, maar het kwam niet in Belgi\u00EB of Nederland."@nl , "\u064A\u0634\u064A\u0631 \u062A\u062C\u0645\u062F \u0641\u0627\u064A\u0633\u0644\u064A \u0623\u0648 \u062A\u062C\u0645\u062F \u0641\u0627\u064A\u0633\u0625\u064A\u0644\u064A\u0627\u0646 \u0625\u0644\u0649 \u0627\u0644\u0639\u0635\u0631 \u0627\u0644\u062C\u0644\u064A\u062F\u064A \u0627\u0644\u0623\u062E\u064A\u0631 \u0648\u0627\u0644\u062A\u062C\u0645\u062F \u0627\u0644\u0645\u0631\u062A\u0628\u0637 \u0628\u0647 \u0641\u064A \u0627\u0644\u0623\u062C\u0632\u0627\u0621 \u0627\u0644\u0634\u0645\u0627\u0644\u064A\u0629 \u0645\u0646 \u0623\u0648\u0631\u0648\u0628\u0627. \u0648\u0641\u064A \u0645\u0646\u0637\u0642\u0629 \u062C\u0628\u0627\u0644 \u0627\u0644\u0623\u0644\u0628 \u064A\u0642\u0627\u0628\u0644 \u062A\u062C\u0645\u062F \u0648\u0648\u0631\u0645. \u064A\u062A\u0633\u0645 \u0628\u0648\u062C\u0648\u062F \u0635\u0641\u064A\u062D\u0629 \u062C\u0644\u064A\u062F\u064A\u0629 (\u0627\u0644\u0635\u0641\u064A\u062D\u0629 \u0627\u0644\u062C\u0644\u064A\u062F\u064A\u0629 \u0627\u0644\u0641\u064A\u0646\u0648\u0633\u0643\u0646\u062F\u064A\u0629) \u0627\u0644\u062A\u064A \u062A\u0646\u0628\u0633\u0637 \u0645\u0646 \u0627\u0644\u062C\u0628\u0627\u0644 \u0627\u0644\u0625\u0633\u0643\u0646\u062F\u0646\u0627\u0641\u064A\u0629 \u0648\u062A\u0645\u062A\u062F \u0628\u0639\u064A\u062F\u064B\u0627 \u0644\u062A\u0635\u0644 \u0625\u0644\u0649 \u0634\u0644\u064A\u0633\u0641\u064A\u0634 \u0647\u0648\u0644\u0634\u062A\u0627\u064A\u0646 \u0648\u0645\u0631\u063A\u0631\u064A\u0641\u064A\u0629 \u0628\u0631\u0627\u0646\u062F\u0646\u0628\u0648\u0631\u063A \u0648\u0634\u0645\u0627\u0644 \u063A\u0631\u0628 \u0631\u0648\u0633\u064A\u0627. \u0641\u064A \u0634\u0645\u0627\u0644 \u0623\u0648\u0631\u0648\u0628\u0627\u060C \u0643\u0627\u0646\u062A \u0623\u0635\u063A\u0631 \u0627\u0644\u0623\u062F\u0648\u0627\u0631 \u0627\u0644\u062C\u0644\u064A\u062F\u064A\u0629 \u0644\u0644\u0639\u0635\u0631 \u0627\u0644\u062C\u0644\u064A\u062F\u064A \u0627\u0644\u062D\u062F\u064A\u062B \u0627\u0644\u0623\u0642\u0631\u0628. \u0643\u0627\u0646\u062A \u0627\u0644\u0641\u062A\u0631\u0629 \u0627\u0644\u062F\u0627\u0641\u0626\u0629 \u0627\u0644\u0633\u0627\u0628\u0642\u0629 \u0641\u064A \u0647\u0630\u0647 \u0627\u0644\u0645\u0646\u0637\u0642\u0629 \u0647\u064A \u0627\u0644\u0641\u062A\u0631\u0629 \u0627\u0644\u0625\u064A\u0645\u064A\u0627\u0646\u064A\u0629 \u0628\u064A\u0646 \u0627\u0644\u0639\u0635\u0648\u0631 \u0627\u0644\u062C\u0644\u064A\u062F\u064A\u0629. \u0628\u062F\u0623\u062A \u0627\u0644\u0641\u062A\u0631\u0629 \u0627\u0644\u0628\u0627\u0631\u062F\u0629 \u0627\u0644\u0623\u062E\u064A\u0631\u0629 \u0645\u0646\u0630 \u0646\u062D\u0648 115.000 \u0639\u0627\u0645 \u0648\u0627\u0646\u062A\u0647\u062A \u0645\u0646\u0630 11.700. \u062A\u062A\u0642\u0627\u0628\u0644 \u0646\u0647\u0627\u064A\u062A\u0647\u0627 \u0645\u0639 \u0646\u0647\u0627\u064A\u0629 \u0627\u0644\u0639\u0635\u0631 \u0627\u0644\u062C\u0644\u064A\u062F\u064A \u0627\u0644\u062D\u062F\u064A\u062B \u0627\u0644\u0623\u0642\u0631\u0628 \u0648\u0645\u0639 \u0628\u062F\u0627\u064A\u0629 \u0639\u0635\u0631 \u0627\u0644\u0647\u0648\u0644\u0648\u0633\u064A\u0646. \u0623\u0637\u0644\u0642 \u0639\u0627\u0644\u0645 \u0627\u0644\u062C\u064A\u0648\u0644\u0648\u062C\u064A\u0627 \u0627\u0644\u0623\u0644\u0645\u0627\u0646\u064A \u0643\u0648\u0646\u0631\u0627\u062F \u0643\u064A\u0644\u0647\u0627\u0643 (1858-1944) \u0627\u0633\u0645 \u062A\u062C\u0645\u062F \u0641\u0627\u064A\u0633\u0625\u064A\u0644\u064A\u0627\u0646 \u0645\u0633\u062A\u062E\u062F\u0645\u064B\u0627 \u0627\u0644\u0627\u0633\u0645 \u0627\u0644\u0645\u0648\u062C\u0648\u062F \u0641\u064A \u0627\u0644\u0644\u063A\u0629 \u0627\u0644\u0623\u0644\u0645\u0627\u0646\u064A\u0629 (\u0641\u0627\u064A\u0633\u0644) \u0644\u0646\u0647\u0631 \u0641\u064A\u0633\u062A\u0648\u0644\u0627 \u0641\u064A \u0628\u0648\u0644\u0646\u062F\u0627 \u0627\u0644\u062D\u0627\u0644\u064A\u0629."@ar , "Glaciazione weichseliana (anche conosciuta come Weichseliano, glaciazione Vistuliana o Weichsel) \u00E8 il nome che si d\u00E0 all'ultimo periodo glaciale e alla glaciazione associata in Europa settentrionale. Nell'area alpina, corrisponde alla glaciazione W\u00FCrm. Era caratterizzata da una vasta calotta di ghiaccio che si estendeva dai Monti scandinavi alla costa est dello Schleswig-Holstein, alla Marca di Brandenburgo e alla Russia nord-occidentale. Nell'Europa settentrionale si tratta del pi\u00F9 recente dei periodi glaciali dell'era glaciale pleistocenica. Il precedente periodo caldo in questa regione fu l'interglaciazione Riss-W\u00FCrm. L'ultimo periodo freddo \u00E8 iniziato circa 115 000 anni fa e si \u00E8 concluso 11 700 anni BP. La sua fine corrisponde alla fine dell'epoca pleistocenica e inizio dell'Olocene. Il nome di glaciazione weichseliana fu dato dal geologo tedesco . In altre regioni, le glaciazioni dell'ultimo periodo glaciale sono note con altri nomi: W\u00FCrm nell'arco alpino, glaciazione Devensiana nelle Isole britanniche e glaciazione del Wisconsin in Nordamerica."@it , "\uBC14\uC774\uD750\uC824 \uBE59\uAE30(\uB3C5\uC77C\uC5B4: Weichsel-Eiszeit)\uB294 \uBD81\uC720\uB7FD\uC758 \uB9C8\uC9C0\uB9C9 \uBE59\uAE30\uB2E4. \uAC19\uC740 \uC2DC\uAE30\uC5D0 \uC54C\uD504\uC2A4 \uACE0\uC0B0\uC9C0\uB300\uC5D0\uC11C\uB294 \uBDD4\uB984 \uBE59\uAE30\uAC00 \uC9C4\uD589\uB418\uC5C8\uB2E4. \uC2A4\uCE78\uB514\uB098\uBE44\uC544\uC0B0\uB9E5\uC5D0\uC11C \uC290\uB808\uC2A4\uBE44\uD788\uD640\uC288\uD0C0\uC778, \uBE0C\uB780\uB374\uBD80\uB974\uD06C \uBCC0\uACBD, \uAE4C\uC9C0 \uD3BC\uCCD0\uC9C4 \uAC70\uB300\uD55C \uBE59\uC0C1\uC778 \uD398\uB178\uC2A4\uCE78\uB514\uC544 \uBE59\uC0C1(Fenno-Scandian ice sheet)\uC73C\uB85C \uADF8 \uD2B9\uC9D5\uC774 \uADDC\uC815\uB41C\uB2E4. \uBC14\uC774\uD750\uC824 \uBE59\uAE30\uB294 \uC9C0\uAE08\uC73C\uB85C\uBD80\uD130 11\uB9CC 5000\uB144 \uC804\uBD80\uD130 1\uB9CC 1700\uB144 \uC804\uAE4C\uC9C0 \uC9C4\uD589\uB418\uC5C8\uB2E4. \uBD81\uC720\uB7FD\uC5D0\uC11C \uC9C4\uD589\uB41C \uD64D\uC801\uC138 \uBE59\uD558\uAE30\uC758 \uBE59\uAE30\uB4E4 \uC911 \uAC00\uC7A5 \uCD5C\uADFC\uC758 \uBE59\uAE30\uC600\uACE0, \uBC14\uC774\uD750\uC824 \uBE59\uAE30\uAC00 \uB05D\uB09C \uC2DC\uC810\uC774 \uD64D\uC801\uC138\uC758 \uB05D\uACFC \uCDA9\uC801\uC138\uC758 \uC2DC\uC791\uC5D0 \uB300\uB7B5 \uACB9\uCE5C\uB2E4. \uBC14\uC774\uD750\uC824\uC774\uB780 \uBE44\uC2A4\uC640\uAC15\uC758 \uB3C5\uC77C\uC5B4 \uC774\uB984\uC774\uBA70, \uB3C5\uC77C \uC9C0\uC9C8\uD559\uC790 \uAC00 \uBA85\uBA85\uD588\uB2E4."@ko , "La glaciaci\u00F3n Weichseliense fue el \u00FAltimo per\u00EDodo glacial y su glaciaci\u00F3n asociada en el norte de Europa. En la regi\u00F3n alpina corresponde a la glaciaci\u00F3n de W\u00FCrm. Se caracteriz\u00F3 por una gran capa de hielo (la capa de hielo Fenno- Escandinava ) que se extendi\u00F3 desde las monta\u00F1as escandinavas \u200B y se extendi\u00F3 hasta la costa este de Schleswig-Holstein, la Marcha de Brandeburgo y el noroeste de Rusia . En el norte de Europa fue el per\u00EDodo glaciar m\u00E1s temprano de la edad de hielo del Pleistoceno. El per\u00EDodo c\u00E1lido anterior en esta regi\u00F3n fue el interglaciar Riss-W\u00FCrm. El \u00FAltimo per\u00EDodo fr\u00EDo comenz\u00F3 hace unos 115.000 a\u00F1os y termin\u00F3 hace 11.700 a\u00F1os. \u200B Su final corresponde con el final de la \u00E9poca del Pleistoceno y el inicio del Holoceno. El nombre de glaciaci\u00F3n Weichseliense o de Weichselian le fue dado por el ge\u00F3logo alem\u00E1n Konrad Keilhack ."@es , "La glaciation vistulienne ou vistulien (ou en conservant le nom allemand weichs\u00E9lien ou glaciation weichs\u00E9lienne) est le nom donn\u00E9 \u00E0 la derni\u00E8re glaciation en Europe du Nord (Scandinavie, une grande partie de la Grande-Bretagne, la Pologne et le nord-est de l'Allemagne) et est utilis\u00E9 par extension pour parler de l'ensemble de l'inlandsis eurasiatique. Elle est l'\u00E9quivalent de la glaciation du W\u00FCrm ou W\u00FCrmien des Alpes.Le Vistulien est dat\u00E9 de l'\u00E9poque du Pl\u00E9istoc\u00E8ne sup\u00E9rieur au sein de la p\u00E9riode du Quaternaire."@fr , "Weichsel var den senaste av de fyra stora nedisningarna (istiderna) i norra Europa under Pleistocen. Den varade i cirka 100 000 \u00E5r, n\u00E5dde sin st\u00F6rsta utbredning f\u00F6r 20 000\u201318 000 \u00E5r sedan och det mesta av isen sm\u00E4lte bort under de f\u00F6ljande 10 000 \u00E5ren. Namnet kommer fr\u00E5n det tyskspr\u00E5kiga namnet, Weichsel, p\u00E5 den flod, Wis\u0142a, i Polen dit glaci\u00E4rens maximala utbredning n\u00E5dde. Andra delar av samma nedisning g\u00E5r under ben\u00E4mningen Wisconsin (i Nordamerika), W\u00FCrm (i Alperna) och Devensian (Brittiska \u00F6arna). Nedisningen under Weichsel-istiden str\u00E4ckte sig vid maximum \u00E4nda ner till norra Tyskland och t\u00E4ckte hela Skandinavien utom de v\u00E4stra delarna av Jylland som var f\u00F6rbundna med Brittiska \u00F6arna via Doggerland (nuvarande Nordsj\u00F6n torrlagd)."@sv , "Zlodowacenie p\u00F3\u0142nocnopolskie, zlodowacenie ba\u0142tyckie, ostatnie zlodowacenie, vistulian \u2013 najm\u0142odsze ze zlodowace\u0144 plejstoce\u0144skich. Trwa\u0142o od 115 tys. lat temu do 11,7 tys. lat b2k (przed rokiem 2000). Poprzedzi\u0142 je interglacja\u0142 eemski, a po nim nast\u0105pi\u0142 holocen \u2013 uznawany za otwarty interglacja\u0142."@pl , "Als Weichsel-Kaltzeit, Weichsel-Glazial oder Weichsel-Komplex wird die letzte Kaltzeit des K\u00E4nozoischen Eiszeitalters und die damit verbundene Vergletscherung f\u00FCr Nordeuropa und das n\u00F6rdliche Mitteleuropa bezeichnet. Umgangssprachlich wird sie auch Weichsel-Eiszeit oder Weichsel-Zeit benannt, im Alpenraum dagegen W\u00FCrm-Kaltzeit. Kennzeichnend war ein gro\u00DFer Eisschild, der vom skandinavischen Hochgebirge ausging und sich bis an die schleswig-holsteinische Ostk\u00FCste, in die Mark Brandenburg und nach Nordrussland erstreckte. Sie war im n\u00F6rdlichen Europa die j\u00FCngste der Vergletscherungsphasen (Glaziale) im Pleistoz\u00E4n. Die vorangegangene Warmzeit wird im selben Bereich als Eem-Warmzeit bezeichnet. Die letzte Kaltzeit begann vor ca. 115.000 Jahren und endete vor 11.600 Jahren. Nach der internationalen Gliederung, die auf den Sauerstoff-Isotopenstufen beruht, beginnt die Letzte Gro\u00DFe Vereisung (englisch Last glacial period) in der Stufe MIS 5d und endet mit der Isotopenstufe MIS 2. Mit ihrem Ende endet das Pleistoz\u00E4n und beginnt das Holoz\u00E4n."@de . @prefix prov: . dbr:Weichselian_glaciation prov:wasDerivedFrom . @prefix xsd: . dbr:Weichselian_glaciation dbo:wikiPageLength "27782"^^xsd:nonNegativeInteger . @prefix wikipedia-en: . dbr:Weichselian_glaciation foaf:isPrimaryTopicOf wikipedia-en:Weichselian_glaciation .