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Victoria University Antarctic Research Expedition Science and Logistics Reports 2002-03: VUWAE 47

Fig.1 Hut Point Peninsula and the McMurdo Ice Shelf to the SE, showing the bathymetry of the broad channel connecting the waters of McMurdo Sound to the NW with those beneath the Ross Ice Shelf to the east. The intersecting lines mark seismic surveys run by the Institute of Geological & Nuclear Sciences (Melhuish et al., 1995; Bannister and Naish, 2002; Horgan et al., 2003) for imaging the geometry of the strata filling the basin (see fig. 2). The red square is the current monitoring site at th…

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Fig.1 Hut Point Peninsula and the McMurdo Ice Shelf to the SE, showing the bathymetry of the broad channel connecting the waters of McMurdo Sound to the NW with those beneath the Ross Ice Shelf to the east. The intersecting lines mark seismic surveys run by the Institute of Geological & Nuclear Sciences (Melhuish et al., 1995; Bannister and Naish, 2002; Horgan et al., 2003) for imaging the geometry of the strata filling the basin (see fig. 2). The red square is the current monitoring site at the shelf edge.

Fig.1 Hut Point Peninsula and the McMurdo Ice Shelf to the SE, showing the bathymetry of the broad channel connecting the waters of McMurdo Sound to the NW with those beneath the Ross Ice Shelf to the east. The intersecting lines mark seismic surveys run by the Institute of Geological & Nuclear Sciences (Melhuish et al., 1995; Bannister and Naish, 2002; Horgan et al., 2003) for imaging the geometry of the strata filling the basin (see fig. 2). The red square is the current monitoring site at the shelf edge.

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