For the first time complete swath bathymetric maps of central and eastern Bransfield basins are presented at a medium scale and detailed morphological descriptions are provided. Bathymetry reveals morphological structures which provide important information about the structure, volcanism, and kinematics of these basins, The central basin is dominated by two roughly orthogonal sets of extensional faults (N065" the main set and N145" the secondary set), displays several discontinuous along-axis large volcanic cones and ridges trending about N059", and undergoes extension roughly normal to the basin. The structure of the eastern basin has a roughly rhomboidal pattern (fault sets along N053" and N103"), displays four deep troughs and a much smaller amount of volcanism than the central basin, and is affected by extension with a significant sinistral strike-slip component.
A B -Wrlud inslrumnenls and advances in networking technology make if possible lo implemrnl m o d d u r dislribulrd measuremenis and compuilng syslems. Sharing resources ond the eliminvlion of obsrocles inrroduced by communimlion networks could be the k q Io open lhe doors IO a new measuremen1 philosophy, in which vinuol instrumenis will ploy an imporlon1 role. Thanks Io lhis workingprinciple, il is possible lo correloie doin from diflerennr experimenls or eomplemenr one experiment wifh information gorhered from the local environmenl 01 m y orher remole sire. This paper describes f h i a m d 11a1us of the LobYir projeer that we arc carrying out i* order lo model o l d implemenl dirlribuled meoreh in lhe Sponish oeeoaographic vessels.Userinlerfveer based on Web leehnologv, will allow fdcndly accessibility from onyploee wifh HTTPcmnecIivi@. Experimenis fools will br oceerrible using m y kind of the ovdnble internet browsers.
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