Photo of this volcano
  • Country
  • Volcanic Region
  • Primary Volcano Type
  • Last Known Eruption
  • 14.295°S
  • 170.7°W

  • 653 m
    2142 ft

  • 244020
  • Latitude
  • Longitude

  • Summit

  • Volcano

The Global Volcanism Program has no activity reports for Tutuila.

The Global Volcanism Program has no Weekly Reports available for Tutuila.

The Global Volcanism Program has no Bulletin Reports available for Tutuila.

This compilation of synonyms and subsidiary features may not be comprehensive. Features are organized into four major categories: Cones, Craters, Domes, and Thermal Features. Synonyms of features appear indented below the primary name. In some cases additional feature type, elevation, or location details are provided.

The Global Volcanism Program is not aware of any Holocene eruptions from Tutuila. If this volcano has had large eruptions (VEI >= 4) prior to 10,000 years ago, information might be found on the Tutuila page in the LaMEVE (Large Magnitude Explosive Volcanic Eruptions) database, a part of the Volcano Global Risk Identification and Analysis Project (VOGRIPA).

Deformation History

Information about Deformation periods will be available soon.

Emission History

There is no Emissions History data is available for Tutuila.

Photo Gallery

The elongated, 32-km-long island of Tutuila in the center of the Samoan Islands is seen in this Space Shuttle view (with north to the upper right). Five Pliocene-to-Pleistocene volcanoes were constructed along rift zones, and the Pago shield volcano in the center of the island was truncated by an eroded, 9-km-wide caldera that incorporates Pago Pago harbor (right-center). Following a lengthy period of erosion, the Leone tuff cones and cinder cones were erupted during the Holocene across the southernmost portion of the island (left-center).

NASA Space Shuttle image ISS002-701-263, 2001 (http://eol.jsc.nasa.gov/).
See title for photo information.
Rocky cliffs and offshore rocky island mark the rugged coastline of Tutuila Island. The elongated, extensively eroded Tutuila Island in the center of the Samoan Islands consists of five Pliocene-to-Pleistocene volcanoes constructed along two or three rifts trending SSW-NNE. Following a lengthy period of erosion, submergence, and the construction of a barrier reef, the Leone volcanics were erupted during the Holocene along a 5-km-long N-S-trending fissure, forming a group of cinder cones that produced fresh-looking pahoehoe lava flows.

Photo by Tavita Togia, 2004 (U. S. National Park Service).
See title for photo information.

Smithsonian Sample Collections Database

The following 10 samples associated with this volcano can be found in the Smithsonian's NMNH Department of Mineral Sciences collections, and may be availble for research (contact the Rock and Ore Collections Manager). Catalog number links will open a window with more information.

Catalog Number Sample Description Lava Source Collection Date
NMNH 99715 Basalt -- --
NMNH 99716 Basalt -- --
NMNH 99717 Basalt -- --
NMNH 99718 Basalt -- --
NMNH 99719 Quartz Trachyte -- --
NMNH 99720 Trachyte -- --
NMNH 99721 Trachyte -- --
NMNH 99722 Basalt -- --
NMNH 99723 Olivine Gabbro -- --
NMNH 99724 Trachyandesite -- --

Affiliated Sites