“…Before and between the two caldera-forming eruptions, activity consisted largely of basaltic lava effusion, (Byers, 1959;Nye and Reid, 1986;Miller and others, 1992;Kay and Kay, 1994) including the ~2-million-year-old Ashishik basalt (Bingham and Stone, 1972). A sequence of high-MgO picritic lavas likely older than the Ashishik basalts are exposed along Cape Idak northeast of the caldera (for example, Byers, 1959;Nye and Reid, 1986).…”