Fig. 7: Thematic maps of identified volcanic cones.
From: Seafloor evidence for pre-shield volcanism above the Tristan da Cunha mantle plume
a Bathymetry for the central area with identified volcanic cones. b Bathymetry for the western area with identified volcanic cones. The hillshade is illuminated by an azimuth of 315°. Smt. Seamount; TTFZ Tristan da Cunha Transform Fault And Fracture Zone System.
