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Multimedia of Tutuila Island in American Samoa.
A view of Rainmaker Mountain to the east of Pago Pago harbor on Tutuila Island, American Samoa. Rainmaker Mountain was mapped in the 1940s as a trachyte plug by geologist Harold Stearns. Dense jungle, the highest annual rainfall in American Samoa, and its steep cliffs make it a formidable mountain to summit. USGS photo by D. Downs.
A view of Rainmaker Mountain to the east of Pago Pago harbor on Tutuila Island, American Samoa. Rainmaker Mountain was mapped in the 1940s as a trachyte plug by geologist Harold Stearns. Dense jungle, the highest annual rainfall in American Samoa, and its steep cliffs make it a formidable mountain to summit. USGS photo by D. Downs.
A view to the west across Pago Pago harbor at Matafao Peak on Tutuila Island, American Samoa. Matafao Peak is the highest part of Tutuila Island at an elevation of 2,142 feet (653 meters) above sea level. It is part of the Matafao Peak National Natural Landmark. USGS photo by D. Downs.
A view to the west across Pago Pago harbor at Matafao Peak on Tutuila Island, American Samoa. Matafao Peak is the highest part of Tutuila Island at an elevation of 2,142 feet (653 meters) above sea level. It is part of the Matafao Peak National Natural Landmark. USGS photo by D. Downs.
A view looking at the basalt lava flows that make cliffs along the southwestern part of Tutuila Island, American Samoa. These flows are part of the Leone volcanic series and form the flattest part of Tutuila Island, where the airport and population center of Tafuna are located. USGS photo by D. Downs.
A view looking at the basalt lava flows that make cliffs along the southwestern part of Tutuila Island, American Samoa. These flows are part of the Leone volcanic series and form the flattest part of Tutuila Island, where the airport and population center of Tafuna are located. USGS photo by D. Downs.
The view looks south along the basalt cliffs and beaches at Tula point on the eastern end of Tutuila Island, American Samoa. Tutuila Island is a shield volcano, formed by basalt flows that are 1-1.5 million years old.
The view looks south along the basalt cliffs and beaches at Tula point on the eastern end of Tutuila Island, American Samoa. Tutuila Island is a shield volcano, formed by basalt flows that are 1-1.5 million years old.
Map of the American Samoa volcano-monitoring network (top). Data from Wake Island hydrograph (located about 4,500 km, or 2,900 miles, northwest of Taʻū Island) shows the general trend in the number of events during the 2022 earthquake swarm (bottom left). Locations for larger earthquakes (M2.5 and greater) are available starting August 20, 2022 (bottom right).
Map of the American Samoa volcano-monitoring network (top). Data from Wake Island hydrograph (located about 4,500 km, or 2,900 miles, northwest of Taʻū Island) shows the general trend in the number of events during the 2022 earthquake swarm (bottom left). Locations for larger earthquakes (M2.5 and greater) are available starting August 20, 2022 (bottom right).
Bathymetric data from the National Oceanic and Atmospheric Administration (NOAA) collected around American Samoa. Light gray areas are the islands of Tutuila, Ofu-Olosega, and Taʻū. Black lines are 1,640 ft (500 m) contour intervals below sea level.
Bathymetric data from the National Oceanic and Atmospheric Administration (NOAA) collected around American Samoa. Light gray areas are the islands of Tutuila, Ofu-Olosega, and Taʻū. Black lines are 1,640 ft (500 m) contour intervals below sea level.