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Случайные фотографии
Barren Island вулкан
Стратовулкан 354 m / 1,161 ft.
Indian Ocean, 12.28°N / 93.86°E
Текущее состояние: незначительные действия или извержения предупреждение (3 из 5)
Barren Island Веб-камеры / данные в реальном времени | Reports
Barren Island volcano books
Barren Island Вулкан-извержения:
1787, 1789, 1795, 1803-04, 1852(?), 1991, 1994-95, 2005-2006, 2015, 2016, 2018, 2019
Типичный извержения стиль:
Последнее землетрясение поблизости
Latest satellite images

Sentinel hub | Landsat 8
Location map of Barren Island.
Location map of Barren Island.

Volcano news & eruption updates: Barren Island

последние (2019) | 2018 | 2017 | Архив
Ср, 6 ноя 2019, 10:44
Presence of lava in the central cone's crater of Barren Island on a recent satellite image (image: Sentinel Hub)
After a relatively calm period during the summer months with little or no activity, it seems to have picked up again since around 23 October this year. ...БОЛЬШЕ [читать все]
Сб, 16 мар 2019, 09:00
Чт, 14 мар 2019, 11:45
Спутниковое изображение вулкана Barren Island 14 Mar 2019
Чт, 7 мар 2019, 11:15
Спутниковое изображение вулкана Barren Island 7 Mar 2019
Ср, 27 фев 2019, 16:21
Santinel-2 image from 27 Feb 2019 showing erupting Barren Island
The volcano remains active as a satellite image from earlier today shows. A small ash plume can be seen which suggests that the volcano is in a phase of intermittent small strombolian-type explosions. ...БОЛЬШЕ
Вс, 27 янв 2019, 01:45
Сб, 26 янв 2019, 02:00
Спутниковое изображение вулкана Barren Island 26 Jan 2019
последние (2019) | 2018 | 2017 | Архив


Barren Island, a possession of India in the Andaman Sea about 135 km NE of Port Blair in the Andaman Islands, is the only historically active volcano along the N-S-trending volcanic arc extending between Sumatra and Burma (Myanmar).  The 354-m-high island is the emergent summit of a volcano that rises from a depth of about 2250 m.  The small, uninhabited 3-km-wide island contains a roughly 2-km-wide caldera with walls 250-350 m high.  The caldera, which is open to the sea on the west, was created during a major explosive eruption in the late Pleistocene that produced pyroclastic-flow and -surge deposits.  The morphology of a fresh pyroclastic cone that was constructed in the center of the caldera has varied during the course of historical eruptions.  Lava flows fill much of the caldera floor and have reached the sea along the western coast during eruptions in the 19th century and more recently in 1991 and 1995.
Source: GVP, Smithsonian Institution

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