Figure 2.
Geological history of the components of Martinique. Two islands in (a) the older arc, Caravelle (east) and St Anne (south (s)), were subsequently joined by a further two islands at the origin of (b) the younger arc, northwest (nw) and southwest (sw). General uplifting of (c) the central area, (d) continued until the central area joined the peripheral precursor islands into (e) the present single island of Martinique.