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Sarigan

Stratovulcano · United States · 494 m

The 3-km-wide Sarigan volcano is seen here from the E during a 2003 NOAA expedition to the Marianas Islands.The cone has a 750-m-wide summit crater that forms the flat area to the right and it contains a small cone. More recent eruptions produced two lava domes from vents on and near the S crater rim, forming the island's high point at the left part of the summit. Holocene lava flows from the dome complex formed the peninsula to the far left.
The 3-km-wide Sarigan volcano is seen here from the E during a 2003 NOAA expedition to the Marianas Islands.The cone has a 750-m-wide summit crater that forms the flat area to the right and it contains a small cone. More recent eruptions produced two lava domes from vents on and near the S crater rim, forming the island's high point at the left part of the summit. Holocene lava flows from the dome complex formed the peninsula to the far left. · Foto: Image courtesy of NOAA, 2003 (http://oceanexplorer.noaa.gov/explorations/03fire/). · Wikimedia Commons
Tipo
Stratovulcano
Paese
United States
Regione
Northwestern Pacific Volcanic Regions / Mariana Volcanic Arc
Altitudine
494 m
Coordinate
16.699, 145.780
Ultima eruzione
Sconosciuto
Contesto tettonico
Subduction zone / Crustal thickness unknown
Forma vulcanica
Composite
Roccia principale
Andesite / Basaltic Andesite
Sintesi geologica

Sarigan volcano forms an irregular 3-km-long island consisting of a low truncated cone with a 750-m-wide summit crater that contains a small ash cone. The most recent eruptions produced two lava domes from vents above and near the south crater rim. Lava flows from each dome reached the coast and extended out to sea. The northern flow overtopped the crater rim on the N and NW sides. The sparse vegetation on the flows indicated to Meijer and Reagan (1981) that they are of Holocene age.

Sintesi da Wikipedia

Sarigan è un'isola vulcanica dell'oceano Pacifico dell'arcipelago delle Isole Marianne.

Wikipedia · CC BY-SA · Leggi l'articolo completo

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