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Tephra from the 1979 soufriere explosive eruption.

H Sigurdsson

    Science (New York, N.Y.)
    |June 4, 1982
    PubMed
    Summary
    This summary is machine-generated.

    The 1979 Soufriere eruption ejected tephra composed of juvenile and nonjuvenile materials. Particle aggregation and accretionary lapilli formation in a wet eruption column explain the deposit's fine grain size and poor sorting.

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    Area of Science:

    • Volcanology
    • Geochemistry

    Background:

    • The 1979 Soufriere eruption produced a significant volume of tephra.
    • The tephra deposit comprised both juvenile and nonjuvenile components.

    Purpose of the Study:

    • To analyze the composition and characteristics of the tephra from the 1979 Soufriere eruption.
    • To understand the processes responsible for the deposit's unique grain size and sorting.

    Main Methods:

    • Analysis of tephra deposit composition (juvenile vs. nonjuvenile).
    • Grain size and sorting analysis of the tephra.
    • Interpretation of particle aggregation and accretionary lapilli formation.

    Main Results:

    • The tephra was 40% juvenile basaltic andesite and 60% nonjuvenile material.

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  • The deposit exhibited fine grain size, poor sorting, and bimodality.
  • Evidence suggests particle aggregation and accretionary lapilli formation.
  • Conclusions:

    • Phreatomagmatic explosions fragmented the 1971-1972 lava island, contributing nonjuvenile material.
    • A wet eruption column facilitated particle aggregation and accretionary lapilli formation.
    • These processes explain the unusual deposit characteristics of the 1979 Soufriere eruption.