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  1. No Access

    Article

    Trace element abundances of high-MgO glasses from Kilauea, Mauna Loa and Haleakala volcanoes, Hawaii

    We performed an ion-microprobe study of eleven high-MgO (6.7–14.8 wt%) tholeiite glasses from the Hawaiian volcanoes Kilauea, Mauna Loa and Haleakala. We determined the rare earth (RE), high field strength, a...

    T. P. Wagner, D. A. Clague, E. H. Hauri… in Contributions to Mineralogy and Petrology (1998)

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    Article

    Role of olivine cumulates in destabilizing the flanks of Hawaiian volcanoes

    The south flank of Kilauea Volcano is unstable and has the structure of a huge landslide; it is one of at least 17 enormous catastrophic landslides shed from the Hawaiian Islands. Mechanisms previously propose...

    D. A. Clague, R. P. Denlinger in Bulletin of Volcanology (1994)

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    Article

    Ages, rare-earth element enrichment, and petrogenesis of tholeiitic and alkalic basalts from Kahoolawe Island, Hawaii

    Kahoolawe Island, Hawaii (18×11 km), is a basaltic shield volcano with caldera-filling lavas, seven identified postshield vents, and at least two occurrences of apparent rejuvenated-stage eruptive. We examined...

    R. V. Fodor, F. A. Frey, G. R. Bauer… in Contributions to Mineralogy and Petrology (1992)

  4. Article

    Terrestrial primordial neon

    M. HONDA, I. MCDOUGALL, D. B. PATTERSON, A. DOULGERIS, D. A. CLAGUE in Nature (1991)

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    Article

    Petrology of Hualalai volcano, Hawaii: Implication for mantle composition

    Hualalai is one of five volcanoes whose eruptions built the island of Hawaii. The historic 1800–1801 flows and the analyzed prehistoric flows exposed at the surface are alkalic basalts except for a trachyte co...

    D. A. Clague, E. D. Jackson, T. L. Wright in Bulletin Volcanologique (1980)