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Sudafrica · Vulcano a scudo

Prince Edward Island

Tipo
Vulcano a scudo
Altitudine
672 m
Ultima eruzione
Sconosciuto
Prince Edward Island
Foto: NASA Earth Observatory image created by Jesse Allen, using EO-1 ALI data provided courtesy of the NASA EO-1 team and the United States Geological Survey. Caption by Michon Scott. · Public domain · Wikimedia Commons
Tipo
Vulcano a scudo
Paese
Sudafrica
Regione
Somalia e Antartide / Marion Hotspot Volcano Group
Altitudine
672 m
Coordinate
-46.630, 37.950
Ultima eruzione
Sconosciuto
Contesto tettonico
Zona di rift / Crosta oceanica (< 15 km)
Forma vulcanica
A scudo
Roccia principale
Basalto / Picrobasalto
Sintesi geologica

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.

Sintesi da Wikipedia

Riassunto in inglese

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.

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