Ruby Submarine Volcano

May 3, 2006

Bob Embley
Geophysicist
NOAA Vents Program, Pacific Marine Environmental Laboratory

The wonderful opportunity we had to observe and sample the active eruption at NW Rota-1 volcano provides a new basis for understanding submarine eruptions on arc volcanoes. It also raises new questions about how these volcanoes work. For example, how often do these volcanoes erupt, how long do they remain active, and how much material is produced during a typical eruptive episode?

In order to better understand these volcanoes, we looked for another example that had a recent eruptive history. In the 1960s, hydrophones picked up sounds from a point lying northwest of Saipan. Subsequent mapping showed a shallow volcano in the correct location that was named Ruby. Ruby has had several eruptive episodes since than - the most recent one occurred in 1995. Although the CTD measurements during our expedition here in 2003 (SRof'03) did not show any evidence of a hydrothermal plume, a tow-yo conducted on this expedition (SROF'06) did find evidence of hydrothermal emissions. The explorations we made during Jason dive 194 found evidence of low level emission of hydrothermal heat and chemicals characterized by extensive iron oxide crusts and deposits. We also discovered a unique ecosystem living on the upper flank of this volcano, consisting largely of numerous brown/red crabs and small limpets that colonize the small rocks and sand within the iron oxide zone. Has this community survived the last volcanic eruption on the summit of Ruby or has it developed since? We don't know from our present data, but we now have a good baseline of information that will be invaluable for future investigators studying the aftermath of the next eruption of Ruby volcano.

Stalked crinoids clinging to the steep, basaltic terrain at Ruby volcano. These crinoids can slowly crawl around on the rocks, but cannot swim. Click image for larger view and image credit.

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A unique ecosystem lives on the upper flank of Ruby volcano, consisting largely of numerous small brown/red crabs and small limpets that colonize the small rocks and sand within the iron oxide zone. The inset is a zoomed-in view of one of the crabs, which were hard to distinguish from the surrounding red rocks and sediment. The red circles outline some of the crabs in the image. Click image for larger view and image credit.

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