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The downthrown sides of faults are marked bv ticks. CHAPTER 3 The cinder cones postdate Middle Pumice, since a small remnant of Middle Pumice fallout and lithic breccia crops out below ap4a in the northeast corner of the caldera (Fig. 34). The breccia is recognized by its distinctive fragments of juvenile welded tuff and accidental orange tuff found in no other pyroclastic deposit on Santorini (Druitt 1983). The stratigraphic position relative to Vourvoulos and Upper Scoriae 1 are unknown. 1). The deposits of Cape Columbos tuff ring (ap4c) overlie a lava a old, and are themselves overlain by Upper Scoriae 2 (ap5).

40. The caldera cliff beneath Oia. showing the Lower Pumice 2 Tuff (rp3), the Middle Tuff sequence (ap4). 50m thick spatter agglomerates and lithic breccias of Upper Scoriae 2 (ap5). the thin Andesites of Oia (ao). and the Minoan Tuff (rp7a). The spatter agglomerates of Upper Scoriae 1 and Upper Scoriae 2 are similar both lithologically and chemically. They are distinguished by their different stratigraphic positions (separated by the Skaros shield), and by the different nature of their underlying tephra: intercalated scoria fall and base-surge ashes in Upper Scoriae 1 and a thin, white pumice fall in Upper Scoriae 2.

The remnant of the Skaros shield at Cape Tourlos. The unconformity (U) between Skaros and the Middle Tuff sequence (ap4) represents the wall of ancient caldera 2. The basal lavas of Skaros are dacites (dsl). and the main lavas are thin andesites and basalts (as2). The succession is capped by the welded spatter agglomerate of Upper Scoriae 2 (ap5). which in turn is overlain by the Therasia rhyodacites (rt) and Minoan Tuff (rp7a). Fig. 37. Caldera cliff at Cape Heptapedio. Lavas and tuffs of Peristeria 3 (av3) onlap the eroded remains of Peristeria 1 (avl) from the west.

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Channeling and related effects in the motion of charged particles through crystals by S. Gemmell


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