Page 82 - Volcanic Textures A Guide To The Interpretation of Textures In Volcanic Rocks
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Plate 11 — Hyaloclastite
                                                                  1. Feeder dyke-hyaloclastite in rhyolite

                                                                  This exposure shows the gradational contact between
                                                                  dark grey, coherent obsidian (Ob) in a feeder  dyke
                                                                  and adjacent matrix-rich, in situ hyaloclastite (Hy) in
                                                                  rhyolitic lava erupted on the sea floor. The transition
                                                                  zone consists of altered, tan, in situ hyaloclastite
                                                                  (Ahy). The matrix-rich hyaloclastite is unaltered and
                                                                  composed of dark grey rhyolite blocks embedded in
                                                                  white, sand-sized hyaloclastite  matrix. Rucksack
                                                                  foreground for scale.



                                                                  Rhyolite, Pleistocene; Chiaia di Luna, Ponza, Italy.
                                                                  2. In situ rhyolitic hyaloclastite

                                                                  There is a gradation  from  comparatively coherent,
                                                                  flow-banded lava (below the pen) into matrix-rich in
                                                                  situ hyaloclastite. Clasts in the hyaloclastite have
                                                                  curviplanar margins  (Cp) and  groups of  clasts
                                                                  display jigsaw-fit texture (dashed line). The granular
                                                                  matrix (M) is composed  of  glassy particles and
                                                                  phenocryst fragments derived from thorough quench
                                                                  fragmentation of the lava.



                                                                  Glassy  rhyolite, Pleistocene; Cala del  Gaetano,
                                                                  Ponza, Italy.

                                                                  3. In situ rhyolitic hyaloclastite
                                                                  A brecciated lobe of flow-banded rhyolite comprises
                                                                  jigsaw-fit to slightly rotated blocks of dark grey lava
                                                                  separated by narrow seams of finer matrix. The lobe
                                                                  has sharp contacts with enclosing pale grey, matrix-
                                                                  rich in situ  hyaloclastite (Hy). Autobrecciation  and
                                                                  quench fragmentation probably  operated  together
                                                                  during disintegration of the lobe. It may represent a
                                                                  pulse of lava emplaced into cogenetic, freshly formed
                                                                  in situ hyaloclastite.


                                                                  Glassy  rhyolite, Pleistocene; Cala del  Gaetano,
                                                                  Ponza, Italy.

                                                                  4. In situ andesitic hyaloclastite
                                                                  This monomict andesitic breccia shows  the clast
                                                                  shapes and  jigsaw-fit texture typical of in situ
                                                                  hyaloclastite. White, silicic pumiceous sandstone that
                                                                  fills the spaces between the andesite clasts filtered
                                                                  down from overlying  pumiceous volcaniclastic
                                                                  deposits.





                                                                  Matsuzaki Volcanics,  Late Miocene—Pliocene;
                                                                  Matsuzaki, Izu Peninsula, Honshu, Japan.
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