Recently, scientists have described what is being called the largest volcano on the planet. In an article in the journal Nature Geoscience, Dr. William Sager and his coauthors present evidence from
multichannel seismic and core data indicating that the province known as the Tamu Massif is a shield volcano several hundred kilometers across.
The site, one of three provinces of the massive Shatsky
Rise plateau, is located roughly 1000 km east of Japan in the northwest Pacific Ocean. As part of their investigation, scientists conducted research cruises in 2010 and 2012 aboard the R/V Marcus G. Langseth,
a geophysical research vessel operated by the Lamont-Doherty Earth Observatory, of Columbia University. In addition to multichannel seismic survey capabilities, the Langseth is equipped with an EM122
1° x 1° multibeam echo sounder system. The large extent of this site is such that it would take a substantial effort to collect bathymetry and backscatter for the entire structure, across depths of 2000-5000
Data from the EM122 aboard R/V Langseth collected during cruise MGL 1004, over the shallowest portion of the Tamu Massif, 2000-4000m. Data used in this image was downloaded from the National Geophysical
Data Center and processed by Kongsberg Underwater Technology.
Multichannel seismic and core data was critical in defining the subsurface expressions that helped characterize the nature of the site. However, it is clear that the multibeam data presents morphological
features worthy of further investigation.
In the meantime, regional bathymetry must be assembled by merging high resolution multibeam data with coarse satellite altimetry and sparse single beam data, as has been common practice for most of
the deep ocean. We hope KONGSBERG systems will contribute to a more detailed understanding of this, and other large discoveries, in the future.
Image courtesy of Dr. William Sager, University of Houston