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- W2019915480 abstract "This special section is the outcome of a symposium held at the Lamont-Doherty Geological Observatory November 17–19, 1982, on the origin and evolution of seamounts. The topic for the symposium arose from the realization that although there is now a wealth of new ideas on the geology, geophysics, and geochemistry of the ocean floor, the study of seamounts has been relatively neglected despite their great importance to plate tectonics. One of the most interesting features of the ocean floor is the large number of small volcanoes or seamounts. Usually, these features are circular in plan view and have a sharp summit. There has been extensive debate in the literature about the significance of the different morphological types of seamounts. A traditional view has been that flattopped seamounts (e.g., guyots) formed as a result of subaerial erosion when the volcanoes were above sea level. Seamounts covered by fringing reefs or sediments (e.g., atolls), on the other hand, are believed to have formed when the original volcanic foundation subsided below sea level." @default.
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- W2019915480 date "1984-12-10" @default.
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- W2019915480 title "Introduction to Seamount Special Section" @default.
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- W2019915480 doi "https://doi.org/10.1029/jb089ib13p11066" @default.
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