"The 1808 mystery eruption is a large volcanic eruption (VEI-6) conjectured to have taken place in late 1808, possibly in the southwest Pacific. This eruption is suspected of having contributed to a period of global cooling that lasted several years, analogous to how the 1815 eruption of Mount Tambora (VEI-7) led to the Year Without a Summer in 1816. A VEI-6 eruption is comparable to the 1883 eruption of Krakatoa."@en . . . . . . "Erupci\u00F3 misteriosa del 1808"@ca . . . . . "\u064A\u064F\u0639\u062A\u0642\u062F \u0628\u062D\u062F\u0648\u062B \u062B\u0648\u0631\u0627\u0646 \u0628\u0631\u0643\u0627\u0646\u064A \u0647\u0627\u0626\u0644 \u0628\u0642\u064A\u0645\u0629 6 \u0639\u0644\u0649 \u0645\u0624\u0634\u0631 \u0627\u0644\u062A\u0641\u062C\u0631 \u0627\u0644\u0628\u0631\u0643\u0627\u0646\u064A (VEI 6) \u0641\u064A \u0623\u0648\u0627\u062E\u0631 \u0627\u0644\u0639\u0627\u0645 1808\u060C \u0648\u064A\u064F\u0634\u062A\u0628\u0647 \u0641\u064A \u0645\u0633\u0627\u0647\u0645\u062A\u0647 \u0641\u064A \u0641\u062A\u0631\u0629 \u0645\u0646 \u0627\u0644\u062A\u0628\u0631\u064A\u062F \u0627\u0644\u0639\u0627\u0644\u0645\u064A \u0627\u0644\u0630\u064A \u0627\u0633\u062A\u0645\u0631 \u0644\u0633\u0646\u0648\u0627\u062A. \u0628\u0637\u0631\u064A\u0642\u0629 \u0645\u0645\u0627\u062B\u0644\u0629 \u0644\u0644\u0643\u064A\u0641\u064A\u0629 \u0627\u0644\u062A\u064A \u0623\u062F\u0649 \u0628\u0647\u0627 \u062B\u0648\u0631\u0627\u0646 \u062C\u0628\u0644 \u062A\u0627\u0645\u0628\u0648\u0631\u0627 1815 (\u0628\u0642\u064A\u0645\u0629 7 \u0639\u0644\u0649 \u0645\u0624\u0634\u0631 \u0627\u0644\u062A\u0641\u062C\u0631 \u0627\u0644\u0628\u0631\u0643\u0627\u0646\u064A-VEI 7) \u0625\u0644\u0649 \u0633\u0646\u0629 \u0628\u0644\u0627 \u0635\u064A\u0641 \u0641\u064A 1816."@ar . . "9513"^^ . "\u062B\u0648\u0631\u0627\u0646 \u0628\u0631\u0643\u0627\u0646\u064A \u063A\u0627\u0645\u0636 \u0633\u0646\u0629 1808"@ar . "1107087315"^^ . . . . . . . . . . "Z\u00E1hadn\u00E1 sope\u010Dn\u00E1 erupce v roce 1808"@cs . . "1808 mystery eruption"@en . . . . "Z\u00E1hadn\u00E1 sope\u010Dn\u00E1 erupce v roce 1808 je nezn\u00E1m\u00E1 erupce, k n\u00ED\u017E do\u0161lo na konci roku 1808. Odehr\u00E1la se n\u011Bkde v ji\u017En\u00EDm Pacifiku, pravd\u011Bpodobn\u011B v z\u00E1padn\u00ED \u010D\u00E1sti. Na indexu vulkanick\u00E9 aktivity se jej\u00ED s\u00EDla odhaduje na VEI 6 (podobn\u00FD stupe\u0148 m\u011Bl tak\u00E9 v\u00FDbuch Krakatoy roku 1883). Ud\u00E1lost zp\u016Fsobila glob\u00E1ln\u00ED ochlazen\u00ED, trvaj\u00EDc\u00ED n\u011Bkolik let. Z\u00E1rove\u0148 p\u0159isp\u011Bla k v\u011Bt\u0161\u00EDmu glob\u00E1ln\u00EDmu ochlazen\u00ED (tzv. roku bez l\u00E9ta), kter\u00E9 nastalo o 7 let pozd\u011Bji, po v\u00FDbuchu (VEI 7) sopky Tambory."@cs . "Se cree que una colosal erupci\u00F3n volc\u00E1nica, con IEV de 6, ocurri\u00F3 a finales de 1808, contribuyendo a un periodo de disminuci\u00F3n global de la temperatura que dur\u00F3 por a\u00F1os,\u200B\u200B disminuci\u00F3n que fue exacerbada por la erupci\u00F3n del Tambora (IEV 7) en 1815."@es . "\u064A\u064F\u0639\u062A\u0642\u062F \u0628\u062D\u062F\u0648\u062B \u062B\u0648\u0631\u0627\u0646 \u0628\u0631\u0643\u0627\u0646\u064A \u0647\u0627\u0626\u0644 \u0628\u0642\u064A\u0645\u0629 6 \u0639\u0644\u0649 \u0645\u0624\u0634\u0631 \u0627\u0644\u062A\u0641\u062C\u0631 \u0627\u0644\u0628\u0631\u0643\u0627\u0646\u064A (VEI 6) \u0641\u064A \u0623\u0648\u0627\u062E\u0631 \u0627\u0644\u0639\u0627\u0645 1808\u060C \u0648\u064A\u064F\u0634\u062A\u0628\u0647 \u0641\u064A \u0645\u0633\u0627\u0647\u0645\u062A\u0647 \u0641\u064A \u0641\u062A\u0631\u0629 \u0645\u0646 \u0627\u0644\u062A\u0628\u0631\u064A\u062F \u0627\u0644\u0639\u0627\u0644\u0645\u064A \u0627\u0644\u0630\u064A \u0627\u0633\u062A\u0645\u0631 \u0644\u0633\u0646\u0648\u0627\u062A. \u0628\u0637\u0631\u064A\u0642\u0629 \u0645\u0645\u0627\u062B\u0644\u0629 \u0644\u0644\u0643\u064A\u0641\u064A\u0629 \u0627\u0644\u062A\u064A \u0623\u062F\u0649 \u0628\u0647\u0627 \u062B\u0648\u0631\u0627\u0646 \u062C\u0628\u0644 \u062A\u0627\u0645\u0628\u0648\u0631\u0627 1815 (\u0628\u0642\u064A\u0645\u0629 7 \u0639\u0644\u0649 \u0645\u0624\u0634\u0631 \u0627\u0644\u062A\u0641\u062C\u0631 \u0627\u0644\u0628\u0631\u0643\u0627\u0646\u064A-VEI 7) \u0625\u0644\u0649 \u0633\u0646\u0629 \u0628\u0644\u0627 \u0635\u064A\u0641 \u0641\u064A 1816."@ar . . . . . "Erupci\u00F3n misteriosa de 1808"@es . . . . . . . "Es creu que una colossal erupci\u00F3 volc\u00E0nica, amb un \u00EDndex d'explosivitat volc\u00E0nica (IEV) de 6, es produ\u00ED a finals del 1808 i contribu\u00ED a un per\u00EDode de baixada global de la temperatura que dur\u00E0 diversos anys i fou exacerbada per l'erupci\u00F3 del Tambora (IEV 7) el 1815."@ca . . . . . . "\u00C9ruption myst\u00E9rieuse de 1808"@fr . . . . "44662223"^^ . . . . "The 1808 mystery eruption is a large volcanic eruption (VEI-6) conjectured to have taken place in late 1808, possibly in the southwest Pacific. This eruption is suspected of having contributed to a period of global cooling that lasted several years, analogous to how the 1815 eruption of Mount Tambora (VEI-7) led to the Year Without a Summer in 1816. A VEI-6 eruption is comparable to the 1883 eruption of Krakatoa."@en . . "Z\u00E1hadn\u00E1 sope\u010Dn\u00E1 erupce v roce 1808 je nezn\u00E1m\u00E1 erupce, k n\u00ED\u017E do\u0161lo na konci roku 1808. Odehr\u00E1la se n\u011Bkde v ji\u017En\u00EDm Pacifiku, pravd\u011Bpodobn\u011B v z\u00E1padn\u00ED \u010D\u00E1sti. Na indexu vulkanick\u00E9 aktivity se jej\u00ED s\u00EDla odhaduje na VEI 6 (podobn\u00FD stupe\u0148 m\u011Bl tak\u00E9 v\u00FDbuch Krakatoy roku 1883). Ud\u00E1lost zp\u016Fsobila glob\u00E1ln\u00ED ochlazen\u00ED, trvaj\u00EDc\u00ED n\u011Bkolik let. Z\u00E1rove\u0148 p\u0159isp\u011Bla k v\u011Bt\u0161\u00EDmu glob\u00E1ln\u00EDmu ochlazen\u00ED (tzv. roku bez l\u00E9ta), kter\u00E9 nastalo o 7 let pozd\u011Bji, po v\u00FDbuchu (VEI 7) sopky Tambory."@cs . . "Es creu que una colossal erupci\u00F3 volc\u00E0nica, amb un \u00EDndex d'explosivitat volc\u00E0nica (IEV) de 6, es produ\u00ED a finals del 1808 i contribu\u00ED a un per\u00EDode de baixada global de la temperatura que dur\u00E0 diversos anys i fou exacerbada per l'erupci\u00F3 del Tambora (IEV 7) el 1815."@ca . . . . . . . . . "L'\u00E9ruption de 1808 est un \u00E9v\u00E8nement volcanique majeur (d'Indice d'explosivit\u00E9 volcanique 6) dont la localisation g\u00E9ographique reste, en 2021, inconnue."@fr . . . . . . . "L'\u00E9ruption de 1808 est un \u00E9v\u00E8nement volcanique majeur (d'Indice d'explosivit\u00E9 volcanique 6) dont la localisation g\u00E9ographique reste, en 2021, inconnue."@fr . . . . "Se cree que una colosal erupci\u00F3n volc\u00E1nica, con IEV de 6, ocurri\u00F3 a finales de 1808, contribuyendo a un periodo de disminuci\u00F3n global de la temperatura que dur\u00F3 por a\u00F1os,\u200B\u200B disminuci\u00F3n que fue exacerbada por la erupci\u00F3n del Tambora (IEV 7) en 1815."@es .