Figure 6
From: Shelf sand supply determined by glacial-age sea-level modes, submerged coastlines and wave climate
Correlation between the (a) coastline morphology and orientation, (b) shelf slope gradient (°) along the south-east Australian shelf, and (c) the calculated paleoshoreline recession rate (m/yr) during the sea-level rise enhanced by the MWP-1B (11.45–11.1 kya B.P). Yellow bars highlight the areas with the smallest paleoshoreline recession rates coincident with highest slope gradients of ≥1°. Green dots indicate inner shelf slope, and location of the SSB is indicated (adapted from Roy (1998)).
