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East Pacific Rise: Hot Springs and Geophysical Experiments
Science, 1980Hydrothermal vents jetting out water at 380° ± 30°C have been discovered on the axis of the East Pacific Rise. The hottest waters issue from mineralized chimneys and are blackened by sulfide precipitates. These hydrothermal springs are the sites of actively forming massive sulfide mineral deposits.
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East Pacific Rise and Westward Drift of North America
Nature, 1968There is some evidence for an ancestral East Pacific Rise which was overridden by North America in Mesozoic time.
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Tertiary Sediment from the East Pacific Rise
Science, 1967More than 50 cores ranging in age from Pliocene to Lower Miocene have been recovered from the East Pacific Rise. Near the crestal regions the sediment cover is thin or lacking, and only Pleistocene sediments were recovered. On the flanks, the sediment thickness increases and pre-Pleistocene sediments are encountered.
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