SUNKLANDS OF PORT PHILLIP BAY AND BASS STRAIT 
91 
FIG. 7. 
Bathymetrical Chart of King Bay showing the Outer Face of the Upper Dune Series 
resting on a Mature Surface of Fluviatile Erosion. 
30-fathom outlets. There are two outlets, in close proximity, 3 
miles west of Cape Schanck. The bent contours point northwards 
to the approximate position of the relatively recent Tootgarook 
Tideway, and open towards the 45-fathom depression; like the 
Tootgarook Tideway, they entered King Bay near to where 
Selwyn’s Fault intersects the coast line. There is little doubt 
that the drift at 186 feet in Bore No. 4, Wannaeue, was deposited 
in a tideway that led to one of these outlets. 
