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GSCI 340 - Environmental Geology
Fort Hays State University
Fall 2008

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Lecture #13

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Clerical:

  • It's Volcano Video Week!
  • Homework #5 is posted. It will be completed in class today (10/2).
  • Before Thursday's class, take a virtual field trip to Haimey. Then watch this 30 minute CBC video of the eruption.

    Themes of the Day:

    • Types of Volcanoes
    • Felsic Magmas
    • Stratovolcanoes
    • Pyroclastic Eruptions

    Types of Volcanoes

    • volcanoes, lava flows
    • Profile of a volcano, and types of eruption dictated by composition of the magma (lava) - Types of Igneous Rocks
    • Main types of volcanoes and volcanic products:
      • Shield Volcanoes - low viscosity basaltic magmas - lava lakes and flows common - not explosive - flood basalts and submarine pillow lavas are basaltic, too
      • Cinder Cones - variable composition, often basaltic - usually a single batch of magma - steep cones formed by cinders piled around vent at angle of repose
      • Composite Volcanoes (Stratovolcanoes) - interayered lava flows and pyroclastic deposits - ranges from intermediate to felsic in composition (andesite-dacite-rhyolite) - in volcanic arcs above subduction zones
      • Dome Volcanoes - similar in composition and often genetically related to composite volcanoes - usually more viscous (more silicic) magma type (dacite/rhyolite) - pyroclastic flows abundant - explosive eruptions common
      • Continantal Calderas - in continental regions the result of the largest types of volcanic eruptions - large, shallow, silicic magma chambers empty catastrophically with unparalleled violence; roof of magma chamber collapses into emptied portion of magma chamber
    • Crater vs. Caldera - Aniakchak Volcano
    • USGS Photo Glossary of Volcanic Terms - lots of good illustrations of volcanoes and volcanic features

    Felsic Magmas

    • formed by evolution of mafic magmas and melting of the crust
    • Generally formed at subduction zones, by fractional crystallization and evolution of mafic magmas. Evolve into intermediate to felsic composition magmas before crystallizing as diorite/andesite or granite/rhyolite.
    • high viscosity - gas rich - explosive

    Stratovolcanoes

    Pyroclastic Eruptions

    Mt. Pinatubo Overview
    Mt Pinatubo Ash CloudThe goal of this exercise is to get you to think about the very real links between geology and society. Mount Pinatubo in the Philippines erupted spectacularly in 1991 - it was the second largest eruption of the 20th century. The video that we will watch on Monday details the monitoring and prediction efforts of US Geological Survey (USGS) volcanologists and their colleagues at the Philippine Institute for Volcanology and Seismology (PHIVOLCS). Thousands of lives were saved because geologists were able to accurately predict the timing and magnitude of the eruption - the Mt. Pinatubo eruption is considered one of the greatest success stories of modern volcanology. As further evidence of its impact on our culture, consider that the movie Dante's Peak draws much of its scientific inspiration from the story portrayed in this video.

    For further surfing...

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    GSCI 340 - Environmental Geology
    Dr. Ron Schott, Assistant Professor of Geology
    Fort Hays State University - Geosciences Dept.
    600 Park Street, Hays, KS  67601-4099
    Phone: (785)628-5348  Fax: (785)628-4096
    E-mail: rschott@fhsu.edu
    Web: http://hays.outcrop.org/schott/
    Page content last revised on: 14 October 2008