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Frying Pan Lake (renamed Waimangu Cauldron in 1963 though not widely used) is the world's largest hot spring. It is located in the Echo Crater of the Waimangu Volcanic Rift Valley, New Zealand and its acidic water maintains a temperature of about 50–60 °C (122–140 °F). The Lake covers 38,000 square metres in part of the volcanic crater and the shallow lake is only 5.5 metres deep, but at vents, it can go down to 18.3 metres.

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dbo:abstract
  • بحيرة المقلاة (بالإنجليزية: Frying Pan Lake)‏Frying Pan Lake (renamed Waimangu Cauldron in 1963 though not widely used) is the largest حمة in the world. It is located in , نيوزيلندا and maintains a temperature of 50-60 °C. (ar)
  • Frying Pan Lake nebo také Waimangu Cauldron je termální pramen na Novém Zélandu. Má rozlohu 3,8 hektaru, průměrná hloubka činí šest metrů a maximální přes dvacet metrů a objem 200 000 m³, řadí se tak k největším geotermálním jezerům na světě. Pramen se nachází v kráteru Echo, který náleží k chráněné oblasti nedaleko města Rotorua (region Bay of Plenty). Horké prameny zde vznikly v důsledku erupce sopky 10. června 1886, k poslednímu výbuchu došlo 22. února 1973. Voda dosahuje teploty 55-60 °C a má pH 3,8, díky unikajícímu oxidu uhličitému a sulfanu jezero neustále bublá a hladina je zahalena oblaky páry. Ve vodě žijí termofilní organismy, jako je Cyanidium caldarium. (cs)
  • Der Frying Pan Lake (auch Waimangu-Kessel) ist ein See vulkanischen Ursprungs in Neuseeland. (de)
  • Frying Pan Lake (renamed Waimangu Cauldron in 1963 though not widely used) is the world's largest hot spring. It is located in the Echo Crater of the Waimangu Volcanic Rift Valley, New Zealand and its acidic water maintains a temperature of about 50–60 °C (122–140 °F). The Lake covers 38,000 square metres in part of the volcanic crater and the shallow lake is only 5.5 metres deep, but at vents, it can go down to 18.3 metres. Echo Crater was formed as part of the 1886 Mount Tarawera eruption, which opened several craters along a 17-kilometre (11 mi) rift stretching southwest from Mount Tarawera to the nearby Southern Crater. After this event, the crater's floor partly filled with rainwater and heated groundwater, but it was not until after a large eruption in Echo Crater on 1 April 1917 that the resulting larger crater filled up from hot springs to reach its current size by mid 1918. The most recent eruption in Echo Crater occurred on 22 February 1973, destroying the Trinity Terrace area on the south-eastern shore of Frying Pan Lake. An area of colourful sinter terraces is still visible on the western shore of the lake. To the north, the lake is bounded by the steaming Cathedral Rocks. This monolithic rock structure is composed of rhyolitic lava at least 60,000 years old and was named Gibraltar Rock until the 1917 Echo Crater eruption completely changed its shape. A fumarole known as the Devil's Blowhole in the northern wall of Echo Crater also disappeared in that event. The water of Frying Pan Lake is typically steaming and can appear to be boiling, due to carbon dioxide and hydrogen sulphide gas bubbling to the surface, but the lake's average temperature is 55 °C (131 °F). The lake and its outflow, Waimangu Stream (referred to as Hot Water Creek in the Waimangu Wanderer Guide), have an average pH level of 3.8, even though some of the boiling hot springs and vents on the lake's bed feed it with alkaline water of pH 8.2 to 8.7. This leads to various gradients of pH levels, which govern which types of algae are present, the blue-green algae Mastigocladus laminosus, or the eukaryotic algae Cyanidium caldarium. The unique cyclic nature of the hydrothermal system interconnecting Frying Pan Lake and the nearby Inferno Crater Lake has been the subject of studies since monitoring equipment was installed in 1970 at the outflow stream from Frying Pan Lake and at Inferno Crater Lake. Both lakes' water levels and overflow volumes follow a complicated rhythm that repeats itself roughly every 38 days. When the water level and temperature of Inferno Crater Lake increase, the water level and outflow of Frying Pan Lake decrease. The outflow volume of Frying Pan Lake has decreased from over 122 litres per second (4.3 cubic feet per second) in 1970 to around 100 L/s (3.5 cu ft/s), but varies by up to 20 L/s (0.7 cu ft/s) as part of the 38-day cycle. Frying Pan Lake is one of the first major attractions encountered along the wheelchair-friendly main Waimangu walking track. The site of the extinct Waimangu Geyser is located not far from its north-eastern shore. (en)
  • Le Frying Pan Lake (renommé chaudron de Waimangu en 1963 bien que ce nom soit moins utilisé) est un lac volcanique qui constitue la plus vaste source chaude du monde. Il est situé dans la (en), en Nouvelle-Zélande. Sa température est entre 50 et 60 °C. (fr)
  • Frying Pan Lake adalah mata air panas terbesar di dunia. Danau ini terletak di , Selandia Baru. (in)
  • Il lago Frying Pan (ribattezzato Waimangu Cauldron nel 1963 anche se questo nome non viene ampiamente utilizzato) è la più grande sorgente termale del mondo. Il lago è situato nell'Echo Crater della Waimangu Volcanic Rift Valley, in Nuova Zelanda e le sue acque acide rimangono sempre ad una temperatura di circa 50-60 °C . Il lago copre 38000 m² del cratere e rimane profondo 5,5 m, anche se alle bocche può scendere fino a 18,3 metri. L'Echo Crater si è formato con l'eruzione del monte Tarawera del 1886, che ha aperto diversi crateri lungo una faglia lunga 17 km. A seguito di questo evento eruttivo, il fondo del cratere si riempì di acqua piovana e di acque sotterranee, ma fu solo dopo una grande eruzione nell'Echo Crater il 1 aprile 1917 che il cratere più grande si riempì di sorgenti termali per raggiungere le dimensioni attuali entro la metà del 1918. L'eruzione più recente dell'Echo Crater si è verificata il 22 febbraio 1973, distruggendo l'area di Trinity Terrace sulla sponda sud-orientale del lago Frying Pan. Sulla sponda occidentale del lago, rimane visibile un'area di terrazze colorate per sinterizzazione. A nord, il lago è delimitato dalle fumanti Cathedral Rocks. Questa struttura rocciosa monolitica è composta da lava riolitica antica di almeno 60 000 anni ed era stata chiamata Gibraltar Rock fino a quando l'eruzione dell'Echo Crater del 1917 ha completamente cambiato la sua forma. In quell'evento scomparve anche una fumarola nota come Devil's Blowhole sulla parete settentrionale dell'Echo Crater. L'acqua del lago Frying Pan è abitualmente fumante a causa dell'anidride carbonica e del gas acido solfidrico che gorgogliano in superficie, e può sembrare in ebollizione, anche se la temperatura media del lago è di 55 °C. Il lago e il suo emissario, il Waimangu Stream (che si trova indicato come Hot Water Creek nella Waimangu Wanderer Guide), hanno un livello medio di 3,8 pH anche se alcune sorgenti termali bollenti lo alimentano con acqua alcalina di pH da 8,2 a 8,7. In questo ambiente acido, vivono alcuni tipi di alghe: l'alga blu-verde Mastigocladus laminosus e l'alga eucariotica Cyanidium caldarium. L'unicità della ciclicità del sistema idrotermale che collega il Frying Pan e il vicino lago Inferno Crater è stata oggetto di studi da quando, nel 1970, sono state installate apparecchiature di monitoraggio presso l'emissario il Waimangu Stream e nel Inferno Crater. Il livello dell'acqua e i volumi di straripamento dei laghi seguono un ritmo complicato che si ripete all'incirca ogni 38 giorni. Quando il livello dell'acqua e la temperatura dell'Inferno Crater aumentano, il livello dell'acqua e il deflusso del Frying Pan diminuiscono. Il lago Frying Pan è una delle prime grandi attrazioni incontrate lungo il percorso pedonale di Waimangu. Il sito dell'estinto Waimangu Geyser si trova non lontano dalla sua sponda nord-orientale. (it)
  • Jezioro Frying Pan jest największym gorącym źródłem na świecie. Położone jest w Waimangu Volcanic Rift Valley znajdującym się na Wyspie Północnej w Nowej Zelandii. W swoim najgłębszym punkcie woda osiąga tam 200 °C. (pl)
  • Frying Pan Lake ("Stekpannesjön") är världens största heta källa och ligger i Echo-kratern i den vulkaniska sprickdalen i Nya Zeeland. Kratern bildades, liksom resten av sprickdalen, efter vulkanen utbrott 1886, även om själva sjön bildades 1918 i efterdyningarna av ett utbrott i kratern året innan. Sjön, som är 3,8 hektar stor, är 200 meter tvärs över på längsta stället, har ett medeldjup på 6 meter och ett maxdjup på cirka 20 meter. Källan har ett pH på 3,5 och medeltemperaturen är runt 50°C, även om vattnet är nära kokpunkten i de varmaste delarna. (sv)
  • 煎锅湖是世界上最大的温泉,位于新西兰北島。 (zh)
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  • Frying Pan Lake (en)
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  • New Zealand (en)
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  • Frying Pan Lake (en)
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  • (en)
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  • Frying Pan Lake (en)
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  • Waimangu Stream (en)
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  • Location of Frying Pan Lake (en)
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  • بحيرة المقلاة (بالإنجليزية: Frying Pan Lake)‏Frying Pan Lake (renamed Waimangu Cauldron in 1963 though not widely used) is the largest حمة in the world. It is located in , نيوزيلندا and maintains a temperature of 50-60 °C. (ar)
  • Der Frying Pan Lake (auch Waimangu-Kessel) ist ein See vulkanischen Ursprungs in Neuseeland. (de)
  • Le Frying Pan Lake (renommé chaudron de Waimangu en 1963 bien que ce nom soit moins utilisé) est un lac volcanique qui constitue la plus vaste source chaude du monde. Il est situé dans la (en), en Nouvelle-Zélande. Sa température est entre 50 et 60 °C. (fr)
  • Frying Pan Lake adalah mata air panas terbesar di dunia. Danau ini terletak di , Selandia Baru. (in)
  • Jezioro Frying Pan jest największym gorącym źródłem na świecie. Położone jest w Waimangu Volcanic Rift Valley znajdującym się na Wyspie Północnej w Nowej Zelandii. W swoim najgłębszym punkcie woda osiąga tam 200 °C. (pl)
  • Frying Pan Lake ("Stekpannesjön") är världens största heta källa och ligger i Echo-kratern i den vulkaniska sprickdalen i Nya Zeeland. Kratern bildades, liksom resten av sprickdalen, efter vulkanen utbrott 1886, även om själva sjön bildades 1918 i efterdyningarna av ett utbrott i kratern året innan. Sjön, som är 3,8 hektar stor, är 200 meter tvärs över på längsta stället, har ett medeldjup på 6 meter och ett maxdjup på cirka 20 meter. Källan har ett pH på 3,5 och medeltemperaturen är runt 50°C, även om vattnet är nära kokpunkten i de varmaste delarna. (sv)
  • 煎锅湖是世界上最大的温泉,位于新西兰北島。 (zh)
  • Frying Pan Lake nebo také Waimangu Cauldron je termální pramen na Novém Zélandu. Má rozlohu 3,8 hektaru, průměrná hloubka činí šest metrů a maximální přes dvacet metrů a objem 200 000 m³, řadí se tak k největším geotermálním jezerům na světě. (cs)
  • Frying Pan Lake (renamed Waimangu Cauldron in 1963 though not widely used) is the world's largest hot spring. It is located in the Echo Crater of the Waimangu Volcanic Rift Valley, New Zealand and its acidic water maintains a temperature of about 50–60 °C (122–140 °F). The Lake covers 38,000 square metres in part of the volcanic crater and the shallow lake is only 5.5 metres deep, but at vents, it can go down to 18.3 metres. (en)
  • Il lago Frying Pan (ribattezzato Waimangu Cauldron nel 1963 anche se questo nome non viene ampiamente utilizzato) è la più grande sorgente termale del mondo. Il lago è situato nell'Echo Crater della Waimangu Volcanic Rift Valley, in Nuova Zelanda e le sue acque acide rimangono sempre ad una temperatura di circa 50-60 °C . Il lago copre 38000 m² del cratere e rimane profondo 5,5 m, anche se alle bocche può scendere fino a 18,3 metri. (it)
rdfs:label
  • بحيرة المقلاة (ar)
  • Frying Pan Lake (cs)
  • Frying Pan Lake (de)
  • Frying Pan Lake (en)
  • Frying Pan Lake (in)
  • Frying Pan Lake (fr)
  • Lago Frying Pan (it)
  • Frying Pan (pl)
  • Frying Pan Lake (sv)
  • 煎锅湖 (zh)
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