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Global Volcanism Program | Image GVP-09659

This view of Vailulu'u seamount to the NW displays three major rifts toward the W, SE, and W. The lower slopes of Vailulu'u and Ta'u merge along the W ridge, with a saddle at 3,200 m and a diameter of ~35 km at its base. An earthquake swarm in 1995 may have been related to an eruption at Vailulu'u, which was not discovered until 1975. It rises 4,200 m from the sea floor to a depth of about 600 m between Ta'u and Rose islands at the eastern end of the American Samoas. Image by Hart and others (Global Volcanism Network Bulletin, 2001).

This view of Vailulu'u seamount to the NW displays three major rifts toward the W, SE, and W. The lower slopes of Vailulu'u and Ta'u merge along the W ridge, with a saddle at 3,200 m and a diameter of ~35 km at its base. An earthquake swarm in 1995 may have been related to an eruption at Vailulu'u, which was not discovered until 1975. It rises 4,200 m from the sea floor to a depth of about 600 m between Ta'u and Rose islands at the eastern end of the American Samoas.

Image by Hart and others (Global Volcanism Network Bulletin, 2001).

Keywords: submarine volcano | stratovolcano | remote sensing | technology | DEM | map | bathymetry


Vailulu'u