Titlebook: Geology and Offshore Mineral Resources of the Central Pacific Basin; Barbara H. Keating,Barrie R. Bolton Book 1992 Circum-Pacific Council

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The Foundations of Atolls: First Explorations,ere made in the Tuamotus in 1840–1841 by E. Belcher and R. E. Johnson. The prevailing belief was that atoll reefs were superficial veneers on the rims of volcanic craters. Specific knowledge of ocean depths surrounding atolls was lacking. The boring technology then available (for drilling water well

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Morphology and Geology of the Magellan trough Area in the Central Pacific,trough axis exceeds 6600 m. Compilations and analyses of bathymetric, seismic, and geologic data of the trough and its adjacent areas reveal three discriminate acoustic layers: a transparent layer (Unit I), a semi-opaque layer (Unit II), and an opaque layer (acoustic basement) in descending order. I

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Southwest Pacific Seamounts Revealed by Satellite Altimetry,as undertaken during research cruises of HMNZS . and R/V . during 1986–87. Four large seamounts were located and mapped by a variety of shipboard recording systems including 12-kHz and 3.5-kHz echo sounders, seismic, gravity, magnetics, and SeaMARC II..Of the three seamounts located in the southern

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Insular Geology of the Line Islands,unts form the longest intraplate submarine mountain chain in any ocean, rising from a sea floor in excess of 5000 m deep. Only twelve seamounts reach sea level to form low islands or atolls; all are presently bordered by fringing reefs. Some seamounts extend above sea level to form typical atolls, h

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The Geology of the Samoan Islands,ual, particularly when compared with the Hawaiian chain, because the islands are volcanically active on both the eastern and western ends of the chain, the islands are larger westward, the easternmost edifice is an atoll not an active seamount, and the chain consists dominantly of alkali rather than

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Sedimentation and Hiatuses in the Central Pacific Basin: Their Relationship to Manganese Nodule Forp to topography and the occurrence of deep-sea manganese nodules. The results of core studies and of detailed examination of two selected areas in the Central Pacific Basin led to the following conclusions..(1) Hiatuses of Neogene through Quaternary age occur widely in the Central Pacific Basin. A c