Landslide tsunami simulations have advanced to the point where the tsunamigenic potential
of giant submarine landslides (GSL) can be affirmed, while the subsidence history of …

The submarine flanks of volcanic islands are shaped by volcanic constructional processes,
landslides, erosion, sediment deposition and tectonic movements. We use a newly acquired …

We present models of compressional and shear velocity structure of the oceanic sediments
and upper crust surrounding the Hawaiian islands. The models were derived from analysis …

Submarine lavas recovered from the Hilina bench region, offshore Kilauea, Hawaii Island
provide information on ancient Kilauea volcano and the geochemical components of the …

The development of concepts about the giant Nuuanu and Wailau landslides have been
dependant on bathymetric surveys of the landslide region northeast of Oahu and Molokai …

The main break-in-slope on the northern submarine flank of Molokai at− 1500 to− 1250 m is
a shoreline feature that has been only modestly modified by the Wailau landslide …

Compositional and age data from offshore pillow lavas and volcaniclastic sediments, along
with on-land geologic, seismic, and deformation data, provide broad perspectives on the …

Numerous submarine landslide morphologies have been mapped aroundthe Hawaiian
islands, andthey are classified into slumps and debris avalanches fe. g., Moore et a1., 1994) …

The Mid-Atlantic Ridge near the 15 20¢ Fracture Zone has been the focus of a long-term
cooperative French-American and allied Russian research program. During the summer of …

Despite numerous above-sea-level studies, the early eruptive histories of Hawaiian
volcanoes are largely un known, because younger subaerial lavas conceal older rocks …