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Случайные фотографии
Satellite image showing the plume from Puyehue yesterday (thanks to Sergio Abarca Delgad ‏@sergio_raptor / Twitter)
Friday, Jan 17, 2014
Небольшой выбросов газа и некоторые пепла сообщили VAAC Буэнос-Айрес. В самом деле разреженных шлейфа газа, пара и возможно некоторые вулканического пепла виден на спутниковых снимках со вчера и сегодня утром. ... [подробнее]
MODIS / Terra satellite image 14 Dec showing a plume drifting N from Puyehue
Sunday, Dec 15, 2013
Значительное ash(?) шлейф был замечен на Терра в спутниковых изображений вчера днем. Поскольку Есть никаких других сообщений о том, что (больше в данном случае) извержение произошло (например, сигналы тепла, очевидцев, веб-камера), представляется вероятным, что шлейф от ветра мобилизованы пепла от извержения 2011-12. ... [подробнее]
 

Puyehue-Cordón Caulle вулкан

ВУЛКАН 2236 m / 7,336 ft
Central Chile and Argentina, Южная Америка, -40.59°S / -72.12°W
Текущее состояние: normal or dormant (1 из 5)
Puyehue-Cordón Caulle Веб-камеры / данные в реальном времени | Reports
Puyehue-Cordón Caulle volcano books
Last update: 19 Aug 2018
Типичный извержения стиль: explosive
Puyehue-Cordón Caulle Вулкан-извержения: 2011 (4 June)- 2012, 1960, 1934, 1929, 1921-22, 1905(?), 1893(?) Puyehue-Cordón Caulle with the steam and ash plume from the rift zone eruption seen from space on 26 January 2012 (NASA Earth Observatory)Нет недавних землетрясений
ВремяМагнитный / ГлубинаРасстояниеМестоположение
Puyehue-Cordón Caulle volcano in Central Chile is a complex of 2 volcanoes: Puyehue volcano and the fissure system of Cordón Caulle. Puyehue volcano has a 2.4 km wide summit caldera, but historical eruptions occurred at the Cordón Caulle rift zone.
The Cordón Caulle geothermal area occupies a 6 x 13 km wide depression and is the largest active geothermal area in the southern Andes.
Neighboring Calbuco and Puyehue volcanoes lie on the same traverse fault and is has been noted that they tend at the same time or within only few years distance.

Справочная информация:

The Puyehue-Cordón Caulle volcanic complex (PCCVC) is a large NW-SE-trending late-Pleistocene to Holocene basaltic-to-rhyolitic transverse volcanic chain SE of Lago Ranco.
The 1799-m-high Pleistocene Cordillera Nevada caldera lies at the NW end, separated from Puyehue stratovolcano at the SE end by the Cordón Caulle fissure complex. The Pleistocene Mencheca volcano with Holocene flank cones lies NE of Puyehue.
The basaltic-to-rhyolitic Puyehue volcano is the most geochemically diverse of the PCCVC. The flat-topped, 2236-m-high Puyehue volcano was constructed above a 5-km-wide caldera and is capped by a 2.4-km-wide summit caldera of Holocene age.
Lava flows and domes of mostly rhyolitic composition are found on the eastern flank of Puyehue. Historical eruptions originally attributed to Puyehue, including major eruptions in 1921-22 and 1960, are now known to be from the Cordón Caulle rift zone.
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Source: USGS / GVP

1960 eruption following the great Chile earthquake
Puyehue-Cordón Caulle Volcano started erupting on 24 May 1960. It is possible, that the eruption was triggered by the great earthquake in Chile (magnitude 9.5; the largest measured earthquake in history) on 22 May 1960. The eruption started with a powerful explosive (subplinian) phase, which formed an ash column 8 km high.

2011 eruption of Puyehue-Cordón Caulle
A new eruption started at the complex of Puyehue-Cordón Caulle volcano in Chile on Saturday 4 June 2011 after 51 years of inactivity.
...БОЛЬШЕ

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See also: Sentinel hub | Landsat 8
 

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