Pago is a shield volcano in the center of Tutuila Island, the largest island of American Samoa in the South Pacific Ocean. The volcano was formed by subaerial eruptions between 1.54 and 1.28 million years ago. It has been estimated that the volcano was as high as 3,937 feet (1,200 m) above sea level. Activity on Pago Volcano ended with emplacement of trachyte bodies with ages of 1.03 ± 0.01 Ma.
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