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Mount Erebus (/ ˈ ɛr ɪ b ə s /) is the southernmost active volcano on Earth, located on Ross Island in the Ross Dependency in Antarctica.With a summit elevation of 3,792 metres (12,441 ft), it is the second most prominent mountain in Antarctica (after Mount Vinson) and the second-highest volcano in Antarctica (after the dormant Mount Sidley).
The following other wikis use this file: Usage on ar.wikipedia.org جبل إريباص; Usage on de.wikipedia.org Mount Erebus; Usage on en.wikivoyage.org
The Mount Erebus disaster occurred on 28 November 1979 when Air New Zealand Flight 901 (TE901) [nb 1] flew into Mount Erebus on Ross Island, Antarctica, killing all 237 passengers and 20 crew on board. [1] [2] Air New Zealand had been operating scheduled Antarctic sightseeing flights since 1977.
The Erebus hotspot is a volcanic hotspot responsible for the high volcanic activity on Ross Island in the western Ross Sea of Antarctica. Its current eruptive zone, Mount Erebus, has erupted continuously since its discovery in 1841. Magmas of the Erebus hotspot are similar to those erupted from hotspots at the active East African Rift in ...
Three subprovinces comprise the McMurdo Volcanic Group, namely the Hallett, Melbourne and Erebus volcanic provinces. [1] The Balleny Volcanic Province along the Balleny fracture zone in the Southern Ocean was originally defined as a part of the McMurdo Volcanic Group but it is now excluded due to its location on oceanic crust with no obvious geographic or tectonic relationship to the other ...
In early July, a rift in Antarctica's Larsen C ice shelf caused the third-largest iceberg ever recorded to break off. Incredible new photos reveal Antarctica's huge iceberg in stunning detail Skip ...
Satellite picture showing the lava lake of Mount Erebus, Antarctica. Aerial view of a lava lake in Pu’u ’Ō’ō crater, east rift zone of Kīlauea. The crater is about 820 ft (250 m) in diameter. Aerial view of a lava lake atop the Kūpaʻianahā vent on the east rift zone of Kīlauea volcano.
Tramway Ridge is a ridge that rises to about 3450 m above sea level in the north-west part of the summit caldera of Mount Erebus on Ross Island, Antarctica. The ridge is formed by the levees (banks) on the side of a young lava flow. The appearance of the feature is suggestive of a set of railway or tram lines.