Zusammenfassung
Der Vulkanismus ist für Geologen und Petrologen von besonderem Interesse, da er einer der wenigen geologischen Prozesse ist, die sich unmittelbar beobachten lassen. Vulkane sind geologische Gebilde, die durch den Ausbruch von magmatischen Schmelzen und/oder Gasen aus dem Erdinnern an die Erdoberfläche oder auf den Meeresboden entstehen. Als Vulkane im geographischen Sinne bezeichnet man die Hügel oder Berge, die durch Anhäufung von vulkanischem Gesteinsmaterial gebildet wurden.
†Deceased
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Okrusch, M., Matthes †, S. (2010). Vulkanismus. In: Mineralogie. Springer-Lehrbuch. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-540-78201-8_12
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