A view of the northwest side of Taʻū Island in American Samoa. This island is a shield volcano with small scoria cones on its upper flanks and tuff cones at sea level. The history of this volcano is currently being studied to better understand the eruptions that built it. The light brown material in the foreground at sea level is part of a tuff cone at Faleāsao.
Multimedia
Multimedia of Taʻū Island in American Samoa.
Images
August 7, 2023 — View of the northwest side of Taʻū Island, American Samoa
A view of the northwest side of Taʻū Island in American Samoa. This island is a shield volcano with small scoria cones on its upper flanks and tuff cones at sea level. The history of this volcano is currently being studied to better understand the eruptions that built it. The light brown material in the foreground at sea level is part of a tuff cone at Faleāsao.
July 2023—Topography and bathymetry of the Manuʻa Islands, American Samoa
This reference map depicts the volcanoes in the Manuʻa Islands, American Samoa, the site of seismic unrest between July and September 2022. Marked on the map are the locations of Hawaiian Volcano Observatory GPS and seismometers in the islands.
This reference map depicts the volcanoes in the Manuʻa Islands, American Samoa, the site of seismic unrest between July and September 2022. Marked on the map are the locations of Hawaiian Volcano Observatory GPS and seismometers in the islands.
Map of American Samoa volcano-monitoring network.
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
linkBathymetric 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
linkBathymetric 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.
September 8, 2022 — Ta‘ū Island Coastal Tuff Cone
On the northwest coast of Ta‘ū Island (near Faleāsao village), half of a tuff cone, which is likely thousands of years old, is visible. Ocean waves have eroded away the other half of the tuff cone, which formed when hot magma interacted with either shallow groundwater or sea water. USGS image by J. Chang.
On the northwest coast of Ta‘ū Island (near Faleāsao village), half of a tuff cone, which is likely thousands of years old, is visible. Ocean waves have eroded away the other half of the tuff cone, which formed when hot magma interacted with either shallow groundwater or sea water. USGS image by J. Chang.
September 8, 2022 — Ta‘ū Island Coastal Tuff Cone
The tuff cone on the northwest coast of Ta‘ū Island (near Faleāsao village) is mostly composed of fine-grained ash with larger lithic clasts (fragments of older rock material). Some of these lithic clasts are larger than 1 meter or 3 feet in diameter and are scattered throughout the tuff cone. USGS image by J. Chang.
The tuff cone on the northwest coast of Ta‘ū Island (near Faleāsao village) is mostly composed of fine-grained ash with larger lithic clasts (fragments of older rock material). Some of these lithic clasts are larger than 1 meter or 3 feet in diameter and are scattered throughout the tuff cone. USGS image by J. Chang.