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Geology of the pacific sea floor

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Zusammenfassung

Als Folge von Faltungen und vulkanischen Vorgängen, die in grossem Maßstabe ablaufen, ist der Meeresboden meistens gebirgig. Lokal dagegen erscheint der Boden flach, da die Berge unter Ebenen sedimentären oder vulkanischen Ursprungs verborgen sind.

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Authors and Affiliations

  1. Scripps Institution of Oceanography, University of California, La Jolla

    H. W. Menard

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  1. H. W. Menard
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Menard, H.W. Geology of the pacific sea floor. Experientia 15, 205–213 (1959). https://doi.org/10.1007/BF02158108

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