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Magma und Lava

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Zusammenfassung

Wie wir gesehen haben, werden bei Vulkanausbrüchen glutheiße Gesteinsschmelzen aus dem Erdinnern gefördert, die unter stürmischer Entgasung ausfließen oder explosiv herausgeschleudert werden. Man muss daraus schließen, dass im Erdinnern heiße Schmelzen existieren, in denen leichtflüchtige (volatile) Komponenten gelöst sind. Die meisten Laven, die an die Erdoberfläche gefördert werden, enthalten bereits Kristalle, die in einer Magmakammer oder beim Aufstieg gewachsen sind; sie bilden Einsprenglinge in vulkanischen Gesteinen.

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Authors and Affiliations

  1. Institut für Geographie und Geologie, Universität Würzburg, Würzburg, Deutschland

    Martin Okrusch & Hartwig E. Frimmel

  2. Department of Geological Sciences, University of Cape Town, Rondebosch, Südafrika

    Hartwig E. Frimmel

Authors
  1. Martin Okrusch
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  2. Hartwig E. Frimmel
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Correspondence to Martin Okrusch .

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Okrusch, M., Frimmel, H.E. (2022). Magma und Lava. In: Mineralogie. Springer Spektrum, Berlin, Heidelberg. https://doi.org/10.1007/978-3-662-64064-7_16

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