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Prince Edward Island

Gunung api perisai · South Africa · 672 m

The 10-km-wide Prince Edward Island is around 300 km S of the SW Indian Ocean Ridge and is shown in this 24 May 2019 Sentinel-2 satellite image (N is at the top). Seven tuff cones have been identified and scoria cones have also formed across the island, as well as lava flows. A large portion of the island has been submerged through faulting.
The 10-km-wide Prince Edward Island is around 300 km S of the SW Indian Ocean Ridge and is shown in this 24 May 2019 Sentinel-2 satellite image (N is at the top). Seven tuff cones have been identified and scoria cones have also formed across the island, as well as lava flows. A large portion of the island has been submerged through faulting. · Foto: Satellite image courtesy of Copernicus Sentinel Data, 2019. · Wikimedia Commons
Tipe
Gunung api perisai
Negara
South Africa
Wilayah
Somalian-Antarctic Volcanic Regions / Marion Hotspot Volcano Group
Ketinggian
672 m
Koordinat
-46.630, 37.950
Letusan terakhir
Tidak diketahui
Kondisi tektonik
Rift zone / Oceanic crust (< 15 km)
Bentuk lahan
Shield
Batuan utama
Basalt / Picro-Basalt
Ringkasan geologi

Uninhabited 5 x 10-km-wide Prince Edward Island lies opposite Marion Island at the N end of a submarine plateau on the Antarctic Plate immediately S of the SW Indian Ocean Ridge. It is a low-angle remnant of a large shield volcano formerly centered off the current NW shore of the island. Pleistocene and Holocene scoria cones and tuff cones are located throughout the unglaciated island, which was active contemporaneously with nearby Marion Island. Fifteen of the scoria cones and four tuff cones on the coastal plain were active during the Holocene.

Ringkasan Wikipedia

Ringkasan Inggris

The Prince Edward Islands are two small uninhabited subantarctic volcanic islands in the southern Indian Ocean that are administered by South Africa. They are named Marion Island and Prince Edward Island.

Wikipedia · CC BY-SA · Baca artikel lengkap

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