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NOAA Vents Program expeditions Neovolcanic activity in the NE Lau Basin

NOAA Vents Program expeditions Neovolcanic activity in the NE Lau Basin. May 10, 2010. Final 2010 expedition posting Tofa Soifua. Tofa Soifua and Goodbye from Samoa and the Kilo Moana. Joe Resing Chief Scientist. That we were able to accomplish so much. This area of the seafloor appears to be opening and cracking, allowing more magmatic activity, making these volcanoes very different from those that we find along the mid-ocean ridge, back arc spreading centers, and even those found along the arcs.
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Participating Scientists

Monday, April 27, 2009. 2010 Participating Scientists and Affiliations. Joseph Resing - Chief Scientist, University of Washington. Richard Arculus - Australian National University. NOAA Pacific Marine Environmental Lab. University of Washington grad student. Institute of Geological and Nuclear Sciences. NOAA Pacific Marine Environmental Lab. Institute of Geological and Nuclear Sciences. NOAA Pacific Marine Environmental Laboratory. Eric Olson - University of Washington.

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NOAA Vents Program expeditions Neovolcanic activity in the NE Lau Basin

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NOAA Vents Program expeditions Neovolcanic activity in the NE Lau Basin. May 10, 2010. Final 2010 expedition posting Tofa Soifua. Tofa Soifua and Goodbye from Samoa and the Kilo Moana. Joe Resing Chief Scientist. That we were able to accomplish so much. This area of the seafloor appears to be opening and cracking, allowing more magmatic activity, making these volcanoes very different from those that we find along the mid-ocean ridge, back arc spreading centers, and even those found along the arcs.

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This web page laueruptions.blogspot.com states the following, "NOAA Vents Program expeditions Neovolcanic activity in the NE Lau Basin." We saw that the webpage said " Final 2010 expedition posting Tofa Soifua." It also said " Tofa Soifua and Goodbye from Samoa and the Kilo Moana. That we were able to accomplish so much. This area of the seafloor appears to be opening and cracking, allowing more magmatic activity, making these volcanoes very different from those that we find along the mid-ocean ridge, back arc spreading centers, and even those found along the arcs."

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