"250"^^ . . . . . . . . "8"^^ . . . "490"^^ . "11"^^ . . . . . . . . . "Auckland volcanic field map"@en . "-36.877 174.764" . . . . . . . . . . "250"^^ . . . . . . . . . . . . . . . . . . . . "Volcanic field"@en . . "\u041E\u043A\u043B\u0435\u043D\u0434 (\u0432\u0443\u043B\u043A\u0430\u043D\u0438\u0447\u0435\u0441\u043A\u043E\u0435 \u043F\u043E\u043B\u0435)"@ru . . . "Das Auckland Volcanic Field ist ein bis zu 250.000 Jahre altes monogenetisches Vulkanfeld im Stadtgebiet von Auckland in Neuseeland, auf dem sich nach letzten Erkenntnissen aus dem Jahr 2011 53 ehemals aktive Vulkane befinden. Zuvor ging man noch von 49 Vulkanen aus."@de . "Pleistocene and Holocene"@en . . . . . . . "Auckland (vulkanick\u00E9 pole)"@cs . . . . . . . . . . "Map data/Auckland faults and volcanoes"@en . . . . . . "490"^^ . . . . "-36.9"^^ . "174.7640075683594"^^ . . . . . . . . . . . . . . "\u041E\u043A\u043B\u0435\u043D\u0434 \u2014 \u0432\u0443\u043B\u043A\u0430\u043D\u0438\u0447\u0435\u0441\u043A\u043E\u0435 \u043F\u043E\u043B\u0435 \u0432 \u041D\u043E\u0432\u043E\u0439 \u0417\u0435\u043B\u0430\u043D\u0434\u0438\u0438, \u0440\u0435\u0433\u0438\u043E\u043D \u041E\u043A\u043B\u0435\u043D\u0434. \u0412\u0443\u043B\u043A\u0430\u043D\u0438\u0447\u0435\u0441\u043A\u043E\u0435 \u043F\u043E\u043B\u0435 \u043D\u0435\u0432\u044B\u0441\u043E\u043A\u043E\u0435, \u0441\u043E\u0441\u0442\u043E\u044F\u0449\u0438\u0435 \u043F\u0440\u0435\u0438\u043C\u0443\u0449\u0435\u0441\u0442\u0432\u0435\u043D\u043D\u043E \u0438\u0437 \u0445\u043E\u043B\u043C\u043E\u0432. \u041D\u0430\u0438\u0432\u044B\u0441\u0448\u0430\u044F \u0442\u043E\u0447\u043A\u0430 260 \u043C\u0435\u0442\u0440\u043E\u0432. \u041D\u0430 \u0434\u0430\u043D\u043D\u043E\u043C \u043F\u043E\u043B\u0435 \u0441\u0442\u043E\u0438\u0442 \u044D\u043A\u043E\u043D\u043E\u043C\u0438\u0447\u0435\u0441\u043A\u0438\u0439 \u0446\u0435\u043D\u0442\u0440 \u041D\u043E\u0432\u043E\u0439 \u0417\u0435\u043B\u0430\u043D\u0434\u0438\u0438 \u2014 \u041E\u043A\u043B\u0435\u043D\u0434. \u041E\u043A\u043B\u0435\u043D\u0434 \u0437\u0430\u043D\u0438\u043C\u0430\u0435\u0442 \u0442\u0435\u0440\u0440\u0438\u0442\u043E\u0440\u0438\u044E \u043D\u0430 \u0441\u0435\u0432\u0435\u0440\u0435 \u0421\u0435\u0432\u0435\u0440\u043D\u043E\u0433\u043E \u043E\u0441\u0442\u0440\u043E\u0432\u0430 \u043F\u043B\u043E\u0449\u0430\u0434\u044C\u044E 360 \u043A\u043C\u00B2. \u041E\u0431\u044A\u0451\u043C \u0438\u0437\u0432\u0435\u0440\u0436\u0435\u043D\u043D\u043E\u0439 \u043B\u0430\u0432\u044B \u0441\u043E\u0441\u0442\u0430\u0432\u043B\u044F\u0435\u0442 75 \u043A\u043C\u00B3. \u0421\u0430\u043C\u044B\u0439 \u0434\u043B\u0438\u043D\u043D\u044B\u0439 \u0437\u0430\u0441\u0442\u044B\u0432\u0448\u0438\u0439 \u043F\u043E\u0442\u043E\u043A \u043F\u0440\u043E\u0442\u044F\u043D\u0443\u043B\u0441\u044F \u043D\u0430 10 \u043A\u043C. \u0422\u0435\u0440\u0440\u0438\u0442\u043E\u0440\u0438\u044E \u043F\u043E\u043A\u0440\u044B\u0432\u0430\u044E\u0442 \u043C\u0430\u0430\u0440\u044B, \u0432\u0443\u043B\u043A\u0430\u043D\u0438\u0447\u0435\u0441\u043A\u0438\u0435 \u0442\u0443\u0444\u044B, \u043D\u0435\u0431\u043E\u043B\u044C\u0448\u0438\u0435 \u0449\u0438\u0442\u043E\u0432\u044B\u0435 \u043E\u0431\u0440\u0430\u0437\u043E\u0432\u0430\u043D\u0438\u044F, \u0432\u0443\u043B\u043A\u0430\u043D\u0438\u0447\u0435\u0441\u043A\u0438\u0435 \u043E\u0437\u0451\u0440\u0430, \u043D\u0435\u0432\u044B\u0441\u043E\u043A\u0438\u0435 \u0448\u043B\u0430\u043A\u043E\u0432\u044B\u0435 \u043A\u043E\u043D\u0443\u0441\u044B, \u043A\u043E\u0442\u043E\u0440\u044B\u0445 \u043D\u0430\u0441\u0447\u0438\u0442\u044B\u0432\u0430\u0435\u0442\u0441\u044F \u043F\u043E\u0440\u044F\u0434\u043A\u0430 49 \u0448\u0442\u0443\u043A. \u0412\u0443\u043B\u043A\u0430\u043D\u0438\u0447\u0435\u0441\u043A\u0430\u044F \u0430\u043A\u0442\u0438\u0432\u043D\u043E\u0441\u0442\u044C \u043D\u0430\u0447\u0430\u043B\u0430\u0441\u044C \u0432 \u043F\u043E\u0437\u0434\u043D\u0435\u043C \u043F\u043B\u0435\u0439\u0441\u0442\u043E\u0446\u0435\u043D\u0435 \u043F\u0440\u0438\u043C\u0435\u0440\u043D\u043E 140 \u0442\u044B\u0441\u044F\u0447 \u043B\u0435\u0442 \u0442\u043E\u043C\u0443 \u043D\u0430\u0437\u0430\u0434 \u0438 \u0437\u0430\u043A\u043E\u043D\u0447\u0438\u043B\u0430\u0441\u044C \u0441\u0440\u0430\u0432\u043D\u0438\u0442\u0435\u043B\u044C\u043D\u043E \u043D\u0435\u0434\u0430\u0432\u043D\u043E \u0432 \u0441\u043E\u0432\u0440\u0435\u043C\u0435\u043D\u043D\u044B\u0439 \u043F\u0435\u0440\u0438\u043E\u0434 \u043E\u043A\u043E\u043B\u043E 600\u2014700 \u043B\u0435\u0442. \u0412 \u044D\u043F\u043E\u0445\u0443 \u0433\u043E\u043B\u043E\u0446\u0435\u043D\u0430 \u0438\u0437\u0432\u0435\u0440\u0436\u0435\u043D\u0438\u044F \u043C\u043E\u0433\u043B\u0438 \u0434\u043B\u0438\u0442\u044C\u0441\u044F \u043E\u0442 10 \u0434\u043E 100 \u043B\u0435\u0442. \u0420\u0435\u0437\u0443\u043B\u044C\u0442\u0430\u0442\u043E\u043C \u043F\u043E\u0441\u043B\u0435\u0434\u043D\u0435\u0433\u043E \u0438\u0437\u0432\u0435\u0440\u0436\u0435\u043D\u0438\u044F \u0431\u044B\u043B\u043E \u043E\u0431\u0440\u0430\u0437\u043E\u0432\u0430\u043D\u0438\u0435 \u043E\u0441\u0442\u0440\u043E\u0432\u0430 \u0420\u0430\u043D\u0433\u0438\u0442\u043E\u0442\u043E \u043F\u043B\u043E\u0449\u0430\u0434\u044C\u044E 23 \u043A\u043C\u00B2 \u0438 \u0432\u043E\u0437\u043D\u0438\u043A\u043D\u043E\u0432\u0435\u043D\u0438\u0435\u043C \u043E\u0434\u043D\u043E\u0438\u043C\u0451\u043D\u043D\u043E\u0433\u043E \u0448\u043B\u0430\u043A\u043E\u0432\u043E\u0433\u043E \u043A\u043E\u043D\u0443\u0441\u0430 \u0432\u044B\u0441\u043E\u0442\u043E\u0439 260 \u043C\u0435\u0442\u0440\u043E\u0432, \u043D\u0430\u0438\u0431\u043E\u043B\u0435\u0435 \u0432\u044B\u0441\u043E\u043A\u043E\u0433\u043E \u0432 \u0434\u0430\u043D\u043D\u043E\u0439 \u043C\u0435\u0441\u0442\u043D\u043E\u0441\u0442\u0438. \u0412 \u0433\u043E\u043B\u043E\u0446\u0435\u043D\u0435 \u0431\u044B\u043B\u043E \u043F\u043E\u0440\u044F\u0434\u043A\u0430 20 \u0438\u0437\u0432\u0435\u0440\u0436\u0435\u043D\u0438\u0439. \u041F\u043E\u0440\u043E\u0434\u044B \u043F\u0440\u0435\u0438\u043C\u0443\u0449\u0435\u0441\u0442\u0432\u0435\u043D\u043D\u043E \u0441\u043B\u043E\u0436\u0435\u043D\u044B \u0431\u0430\u0437\u0430\u043B\u044C\u0442\u0430\u043C\u0438. \u0412 \u043D\u0430\u0441\u0442\u043E\u044F\u0449\u0438\u0439 \u043F\u0435\u0440\u0438\u043E\u0434 \u0432 \u0440\u0430\u0439\u043E\u043D\u0435 \u041E\u043A\u043B\u0435\u043D\u0434\u0430 \u0441\u0435\u0439\u0441\u043C\u0438\u0447\u0435\u0441\u043A\u0430\u044F \u0430\u043A\u0442\u0438\u0432\u043D\u043E\u0441\u0442\u044C \u0441\u043F\u043E\u043A\u043E\u0439\u043D\u0430\u044F \u0438 \u043F\u0440\u0438\u0437\u043D\u0430\u043A\u043E\u0432 \u0432\u0443\u043B\u043A\u0430\u043D\u0438\u0447\u0435\u0441\u043A\u043E\u0439 \u0430\u043A\u0442\u0438\u0432\u043D\u043E\u0441\u0442\u0438 \u043D\u0435\u0442."@ru . . . . . . . "no"@en . . . "-36.96"^^ . . . . . . "43445"^^ . . . . . . . . . . . . "right"@en . . . "174.8"^^ . "\u041E\u043A\u043B\u0435\u043D\u0434 \u2014 \u0432\u0443\u043B\u043A\u0430\u043D\u0438\u0447\u0435\u0441\u043A\u043E\u0435 \u043F\u043E\u043B\u0435 \u0432 \u041D\u043E\u0432\u043E\u0439 \u0417\u0435\u043B\u0430\u043D\u0434\u0438\u0438, \u0440\u0435\u0433\u0438\u043E\u043D \u041E\u043A\u043B\u0435\u043D\u0434. \u0412\u0443\u043B\u043A\u0430\u043D\u0438\u0447\u0435\u0441\u043A\u043E\u0435 \u043F\u043E\u043B\u0435 \u043D\u0435\u0432\u044B\u0441\u043E\u043A\u043E\u0435, \u0441\u043E\u0441\u0442\u043E\u044F\u0449\u0438\u0435 \u043F\u0440\u0435\u0438\u043C\u0443\u0449\u0435\u0441\u0442\u0432\u0435\u043D\u043D\u043E \u0438\u0437 \u0445\u043E\u043B\u043C\u043E\u0432. \u041D\u0430\u0438\u0432\u044B\u0441\u0448\u0430\u044F \u0442\u043E\u0447\u043A\u0430 260 \u043C\u0435\u0442\u0440\u043E\u0432. \u041D\u0430 \u0434\u0430\u043D\u043D\u043E\u043C \u043F\u043E\u043B\u0435 \u0441\u0442\u043E\u0438\u0442 \u044D\u043A\u043E\u043D\u043E\u043C\u0438\u0447\u0435\u0441\u043A\u0438\u0439 \u0446\u0435\u043D\u0442\u0440 \u041D\u043E\u0432\u043E\u0439 \u0417\u0435\u043B\u0430\u043D\u0434\u0438\u0438 \u2014 \u041E\u043A\u043B\u0435\u043D\u0434. \u041E\u043A\u043B\u0435\u043D\u0434 \u0437\u0430\u043D\u0438\u043C\u0430\u0435\u0442 \u0442\u0435\u0440\u0440\u0438\u0442\u043E\u0440\u0438\u044E \u043D\u0430 \u0441\u0435\u0432\u0435\u0440\u0435 \u0421\u0435\u0432\u0435\u0440\u043D\u043E\u0433\u043E \u043E\u0441\u0442\u0440\u043E\u0432\u0430 \u043F\u043B\u043E\u0449\u0430\u0434\u044C\u044E 360 \u043A\u043C\u00B2. \u041E\u0431\u044A\u0451\u043C \u0438\u0437\u0432\u0435\u0440\u0436\u0435\u043D\u043D\u043E\u0439 \u043B\u0430\u0432\u044B \u0441\u043E\u0441\u0442\u0430\u0432\u043B\u044F\u0435\u0442 75 \u043A\u043C\u00B3. \u0421\u0430\u043C\u044B\u0439 \u0434\u043B\u0438\u043D\u043D\u044B\u0439 \u0437\u0430\u0441\u0442\u044B\u0432\u0448\u0438\u0439 \u043F\u043E\u0442\u043E\u043A \u043F\u0440\u043E\u0442\u044F\u043D\u0443\u043B\u0441\u044F \u043D\u0430 10 \u043A\u043C. \u0422\u0435\u0440\u0440\u0438\u0442\u043E\u0440\u0438\u044E \u043F\u043E\u043A\u0440\u044B\u0432\u0430\u044E\u0442 \u043C\u0430\u0430\u0440\u044B, \u0432\u0443\u043B\u043A\u0430\u043D\u0438\u0447\u0435\u0441\u043A\u0438\u0435 \u0442\u0443\u0444\u044B, \u043D\u0435\u0431\u043E\u043B\u044C\u0448\u0438\u0435 \u0449\u0438\u0442\u043E\u0432\u044B\u0435 \u043E\u0431\u0440\u0430\u0437\u043E\u0432\u0430\u043D\u0438\u044F, \u0432\u0443\u043B\u043A\u0430\u043D\u0438\u0447\u0435\u0441\u043A\u0438\u0435 \u043E\u0437\u0451\u0440\u0430, \u043D\u0435\u0432\u044B\u0441\u043E\u043A\u0438\u0435 \u0448\u043B\u0430\u043A\u043E\u0432\u044B\u0435 \u043A\u043E\u043D\u0443\u0441\u044B, \u043A\u043E\u0442\u043E\u0440\u044B\u0445 \u043D\u0430\u0441\u0447\u0438\u0442\u044B\u0432\u0430\u0435\u0442\u0441\u044F \u043F\u043E\u0440\u044F\u0434\u043A\u0430 49 \u0448\u0442\u0443\u043A."@ru . . . . . . . . . . . . "Auckland Volcanic Field"@en . "Auckland volcanic field"@en . . . . . . . . "POINT(174.76400756836 -36.876998901367)"^^ . . . . "174.86"^^ . . . . . . . . . "AucklandMapHochstetter1859.JPG"@en . . . . . . . . . . . . "Campo volc\u00E1nico de Auckland"@es . . "954076"^^ . "The Auckland volcanic field is an area of monogenetic volcanoes covered by much of the metropolitan area of Auckland, New Zealand's largest city, located in the North Island. The approximately in the field have produced a diverse array of maars (explosion craters), tuff rings, scoria cones, and lava flows. With the exception of Rangitoto, no volcano has erupted more than once, but the other eruptions lasted for various periods ranging from a few weeks to several years. Rangitoto erupted several times and recently twice; in an eruption that occurred about 600 years ago, followed by a second eruption approximately 50 years later. The field is fuelled entirely by basaltic magma, unlike the explosive subduction-driven volcanism in the central North Island, such as at Mount Ruapehu and Lake Taup\u014D. The field is currently dormant, but could become active again."@en . . "The Auckland volcanic field is an area of monogenetic volcanoes covered by much of the metropolitan area of Auckland, New Zealand's largest city, located in the North Island. The approximately in the field have produced a diverse array of maars (explosion craters), tuff rings, scoria cones, and lava flows. With the exception of Rangitoto, no volcano has erupted more than once, but the other eruptions lasted for various periods ranging from a few weeks to several years. Rangitoto erupted several times and recently twice; in an eruption that occurred about 600 years ago, followed by a second eruption approximately 50 years later. The field is fuelled entirely by basaltic magma, unlike the explosive subduction-driven volcanism in the central North Island, such as at Mount Ruapehu and Lake Ta"@en . . . "Map of the field drawn by Hochstetter in 1859 and published in English in 1864"@en . . . . "Auckland je neaktivn\u00ED vulkanick\u00E9 pole, rozkl\u00E1daj\u00EDc\u00ED se na plo\u0161e p\u0159es 140 km\u00B2 v okol\u00ED nejv\u011Bt\u0161\u00EDho novoz\u00E9landsk\u00E9ho m\u011Bsta Auckland. Pole je tvo\u0159eno v\u00EDce ne\u017E pades\u00E1ti vulkanick\u00FDmi centry (struskov\u00FDmi ku\u017Eely a maary), m\u00E1 eliptick\u00FD tvar (nejv\u011Bt\u0161\u00ED \u0161\u00ED\u0159ka je 29 km) a jeho v\u011Bk je datov\u00E1n na pozdn\u00ED pleistoc\u00E9n. V horninov\u00E9m slo\u017Een\u00ED p\u0159evl\u00E1daj\u00ED alkalick\u00E9 bazalty a\u017E bazanity. B\u011Bhem posledn\u00ED erupce vznik ostrov ."@cs . . . . . . . . . . . . . . . "Map of the Auckland Volcanic Field from 1859"@en . . . "Auckland je neaktivn\u00ED vulkanick\u00E9 pole, rozkl\u00E1daj\u00EDc\u00ED se na plo\u0161e p\u0159es 140 km\u00B2 v okol\u00ED nejv\u011Bt\u0161\u00EDho novoz\u00E9landsk\u00E9ho m\u011Bsta Auckland. Pole je tvo\u0159eno v\u00EDce ne\u017E pades\u00E1ti vulkanick\u00FDmi centry (struskov\u00FDmi ku\u017Eely a maary), m\u00E1 eliptick\u00FD tvar (nejv\u011Bt\u0161\u00ED \u0161\u00ED\u0159ka je 29 km) a jeho v\u011Bk je datov\u00E1n na pozdn\u00ED pleistoc\u00E9n. V horninov\u00E9m slo\u017Een\u00ED p\u0159evl\u00E1daj\u00ED alkalick\u00E9 bazalty a\u017E bazanity. B\u011Bhem posledn\u00ED erupce vznik ostrov ."@cs . . . . . . "260"^^ . . . . . . . . . . . "Auckland Volcanic Field"@en . . . . . . . . . . "c. 1400 CE"@en . "Basalt"@en . "yes"@en . . . . . . . . . . . . . . . . . . . . . . . . . . "0.0"^^ . . . . . "Map of faults and Quaternary volcanoes in the Auckland region. To show well the volcanoes in relation to fault lines you have to click on the map to enlarge and then zoom and pan. This also enables mouse over of the volcano and fault names. Definite active faults are shown in red. Well characterised inactive fault segments are in dark grey and other faults are shown in grey. A number of faults characterised by sea floor studies off the west coast of North Island are not shown. The type of volcanic eruption is indicated by basalt shield type eruption , scoria cone , or phreatomagmatic eruptions tuff ring and maar . Volcanoes from both the Auckland volcanic field and South Auckland volcanic field are displayed. Miocene volcanoes are not shown."@en . . . . "Map data/Auckland Volcanic Field"@en . . . . "260.0"^^ . "-36.87699890136719"^^ . . . . "1122923880"^^ . "Map of selected volcanic features of the Auckland Volcanic Field. Clicking on the map enlarges it, and enables mouseover of volcano name/wikilink. The type of volcanic eruption is indicated by scoria cone , or phreatomagmatic eruptions tuff ring , maar and basaltic volcano activity ."@en . . . . . . . . . . . "1400"^^ . . . "Auckland Volcanic Field"@de . . . . . "Das Auckland Volcanic Field ist ein bis zu 250.000 Jahre altes monogenetisches Vulkanfeld im Stadtgebiet von Auckland in Neuseeland, auf dem sich nach letzten Erkenntnissen aus dem Jahr 2011 53 ehemals aktive Vulkane befinden. Zuvor ging man noch von 49 Vulkanen aus."@de . . . . . . . . . . . "Location and extent of the Auckland volcanic field"@en . . . . . . . . . . . . .