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National News<br />

Figure 1: New AUV for German ridge studies.<br />

Other major activities include the delivery of the 6000-m capable<br />

AUV for ridge studies by the company Hydroid LLC<br />

of Massachusetts, USA (Fig. 1). The vehicle is presently undergoing<br />

seatrials before being put into action at Logatchev in<br />

January 2009. Fig. 1 shows the vehicle aboard R/V Poseidon<br />

during these trials. The vehicle can be operated in three different<br />

configurations, either with a Reson 7125D multibeam,<br />

a black and white camera and flash, or a sub-bottom profiler.<br />

Common to all configurations is an Edgetech 2200 side-scan<br />

sonar, a Seabird CTD, an Ecotech backscattering detector, and<br />

an Eh sensor, the latter kindly provided by Koichi Nakamura<br />

of AIST, Japan. On the research front, the German Ridge community<br />

is initiating a proposal to G-cubed for a thematic issue<br />

on slow-spreading ridges. Colin Devey, Nadine Le Bris, Nicole<br />

Dubilier, Jian Lin and Doug Connelly will be put forward as<br />

guest editors.<br />

India<br />

K.A. Kamesh Raju<br />

Recent cruise onboard R/V Sonne to the Carlsberg<br />

Ridge and the Andaman Sea<br />

The NIO-RVS2 cruise from 17 Oct. - 1 Dec. 2007 was conducted<br />

as the second phase field program of the CSIR (India)<br />

- Network Program, “Tectonic and oceanic processes along the<br />

Indian ridge system and the back arc basins.” The main objective<br />

of the cruise was to acquire multiparameter<br />

data together with deep-tow and seafloor imaging<br />

over segments of the Carlsberg Ridge (CR) and the<br />

Andaman Backarc Spreading Center (ABSC; Fig.<br />

1). The cruise was conducted onboard the German<br />

research vessel R/V Sonne (Fig. 2) chartered by the<br />

National Institute of Oceanography (NIO). We also<br />

collaborated with the Hawaii Mapping Research<br />

Group (HMRG), University of Hawaii, and hired<br />

equipment (MAPRs) from PMEL, NOAA (USA).<br />

Observations included multibeam mapping, magnetics,<br />

deep-tow surveys along the rift valley, ocean<br />

floor imaging with OFOS (Ocean Floor Observing<br />

System, Fig. 3) at selected locations, and seabed sampling using<br />

a TV-guided-grab (Fig. 4), dredge, spade core and gravity core.<br />

Water column sampling, CTD and MAPR observations were<br />

also carried out over the CR and ABSC segments.<br />

Figure 1: Cruise track.<br />

<strong>InterRidge</strong> News 34 Vol. 17, 2008

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