Kaʻū News Briefs, Sunday, Nov. 13, 2022

Rangers teach Volcano School  keiki about nēnē. Photo from VSAS

PRE-K STUDENTS AT VOLCANO SCHOOL OF ARTS & SCIENCES recently received rangers from Hawai'i Volcanoes National Park, along with some nene friends. The rangers taught students about the differences between the extinct giant Hawaiian goose and nēnē, the Hawai'i state bird.  Students enjoyed comparing their sizes to the height of the giant Hawaiian goose and learned about the nēnē habitat and keeping the nēnē safe.  Students performed their Nēnē Mele, took turns petting the nēnē, and observed `ohelo berries, the bird's favorite food.  A statement from the school said, "PreK students would like to say mahalo to the rangers for helping them learn about the nēnē and celebrate the letter 'n.'"

A RESEARCH GEOLOGIST NAMED DREW DOWNS writes about American Samoa volcano activity in Volcano Watch, the  weekly article and activity update by U.S. Geological Survey Hawaiian Volcano Observatory scientists and affiliates. He focuses on Ta‘ū volcano's unrest in the form of an earthquake swarm that was felt throughout the Manuʻa Islands (Ofu-Olosega and Ta‘ū Islands) from late July through early September 2022. He writes:

     American Samoa comprises the easternmost islands of the Samoan archipelago in the south Pacific. These include the islands of Tutuila (the population center) and the Manuʻa Islands about 60 miles (100 km) to the east. These islands are the tops of shield volcanoes, which are mostly submerged to 15,000 ft (4,500 m) beneath the ocean surface. Other volcanoes created by the Samoan hotspot are still completely below the ocean, such as the Vailuluʻu seamount located about 25 miles (40 km) east of Ta‘ū.
    Despite being near the Pacific’s famed ‘Ring of Fire,’ the volcanoes of the Samoan Islands were created by a hotspot in much the same way as the Hawaiian Islands. This type of volcanism tends to produce shield volcanoes known for their distinctive broad shape. The volcanoes in nearby Tonga are of a different type related to subduction at the Tonga Trench, and consequently, an eruption like the one that occurred at Hunga.

Bathymetric data from the National Oceanic and Atmospheric Administrationcollected 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. The Samoan hotspot has created volcanoes along two tracks, the Vai (to the north) and Malu (to the south) trends, but with most of the volcanoes remaining below sea level as seamounts. The Samoan hotspot is thought to be near the easternmost seamount of Vailuluʻu.

    Vailuluʻu is the most recently active volcano, within American Samoa, with three eruptions since the 1970s. These eruptions occurred nearly 2,000 ft (600 m) below the ocean surface and produced lava flows. It is difficult to confirm Vailuluʻu eruptions without ship-based ocean floor mapping. Occasional sea-floor mapping, from time-to-time, looks for changes in topography of the volcano.
    Most eruptions in American Samoa produce relatively slow moving lava flows that are similar to eruptions in Hawaiʻi. Rarer are small explosions where magma and water interact. There is evidence, in the past, of small explosive eruptions that threw out bombs of molten rock and colder, dense rock a few hundred yards (few hundred meters) away from their volcanic vents. These bombs can reach over a yard (meter) in size and are usually in tuff cones that are mostly made of volcanic glass shards with a texture similar to sand and flour. These types of eruptions occur when magma comes into contact with shallow groundwater or near the coast in the shallow marine environment.
    Such an eruption happened about two miles (3 km) offshore to the east of Ofu-Olosega in 1866. On September 7, 1866, residents of the Manuʻa Islands began feeling earthquakes. Five days later, an eruption started and continued for at least two months. The most dramatic of the volcanic activity occurred about 3 days into the eruption, when there was so much volcanic ash ejected that people on Taʻū Island could not see Ofu-Olosega. The cone at the site of the eruption remains submerged below the ocean, but at the time of the eruption, volcanic ash reached 2,000 ft (600 m) above sea level. Earthquakes were felt throughout the two months of the event, and the surrounding ocean was agitated with an occasional sulfur yellow hue and dead fish washing ashore.
    Tutuila is the westernmost, and most populous, island of American Samoa, it too has been impacted by eruptions. Volcanic ash deposited above soils, containing ceramic shards, indicate that people likely witnessed eruptions on Tutuila about 1,400–1,700 years ago. Youthful-looking lava flows on Tutuila, Ofu-Olosega, and Taʻū suggests there have been other eruptions within the past 10,000 years.
    Since September, there has been little earthquake activity beneath Taʻū Island. The monitoring network that HVO set-up across American Samoa in response to the earthquakes earlier this year will help assess potential future volcanic unrest in American Samoa, and associated hazards.
    Read more about the volcanoes of American Samoa on the following U.S. Geological Survey’s webpage: https://www.usgs.gov/observatories/hvo/volcanoes-american-samoa.

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