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Papua Nuova Guinea · Stratovulcano

Hargy

Tipo
Stratovulcano
Altitudine
1148 m
Ultima eruzione
950
Lake Hargy (lower right) lies in the SE corner of the 10 x 12 km wide Hargy caldera. The Lobu River drains the lake through a notch in the northern caldera rim. The post-caldera cone of Galloseulo lies beneath the large cloud bank in the center of the image, about halfway from the lake to the Bismarck Sea. The Toiru River cuts across the bottom of the image. Small eruptions have taken place at Galloseulo over the past 7,000 years, the last occurring about 1,000 years ago.
Lake Hargy (lower right) lies in the SE corner of the 10 x 12 km wide Hargy caldera. The Lobu River drains the lake through a notch in the northern caldera rim. The post-caldera cone of Galloseulo lies beneath the large cloud bank in the center of the image, about halfway from the lake to the Bismarck Sea. The Toiru River cuts across the bottom of the image. Small eruptions have taken place at Galloseulo over the past 7,000 years, the last occurring about 1,000 years ago. · Foto: NASA Landsat image, 2000 (courtesy of Hawaii Synergy Project, Univ. of Hawaii Institute of Geophysics & Planetology).
Tipo
Stratovulcano
Paese
Papua Nuova Guinea
Regione
Pacifico sud-occidentale / Bismarck Volcanic Arc
Altitudine
1148 m
Coordinate
-5.330, 151.100
Ultima eruzione
950
Contesto tettonico
Zona di subduzione / Crosta continentale (> 25 km)
Forma vulcanica
Composito
Roccia principale
Dacite
Sintesi geologica

This little-known volcano is one of several major calderas on the island of New Britain. The 10 x 12 km Hargy caldera, whose floor is 150 m above sea level, contains an inner caldera with a steep west-facing wall. A caldera lake on the SE side drains through a narrow gap in the northern caldera wall. The latest caldera-forming eruption of Hargy volcano took place about 11,000 years ago. The dacitic Galloseulo lava cone rises above and partially overtops the western rim of the caldera. A double crater occupies a larger 700-m-wide crater. Numerous small eruptions have taken place at Galloseulo over the past 7000 years, the last occurring about 1000 years ago.

Storia delle eruzioni

2 registrateGlossario
Riepilogo (VEI nel tempo)
Fai clic su una barra per vedere le singole eruzioni · Usa le frecce per spostarti tra le barre, Invio per aprire
5050 a.C.~4850 a.C. · 1 eruzioni · VEI max. ?750~950 · 1 eruzioni · VEI max. ?5050 a.C.3650 a.C.2050 a.C.650 a.C.750

Cronologia dettagliata

  1. 950VEI ?Stima geologica
    950 – fine sconosciuta
    Galloseulo
  2. 5050 a.C.VEI ?Stima geologica
    5050 a.C. – fine sconosciuta
    Galloseulo

Vulcani nelle vicinanze

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