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• W228476918 startingPage "261" @default.
• W228476918 abstract "Intraoceanic arcs of the world are dominated by submarine volcanoes, many of which host active hydrothermal systems. A considerable number of the morphological features common to subaerial volcanoes are also present on the submarine edifices, including summit craters. Surprisingly, some of the craters, such as at Daikoku and Nikko volcanoes of the Mariana Arc, and Macauley Cone of the Kermadec Arc, are host to lakes of molten sulfur, both ancient and modern. These lakes, up to ~200 m in diameter, act as condensers of gases that derive from the underlying magmas. Volcanic vents beneath these lakes provide a steady outflow of hot gases that continuously generate molten sulfur. At Daikoku, an extraordinary lake of liquid sulfur is in constant convective and gas escape-driven motion. Smaller pools of molten sulfur occur on Nikko, and there is evidence of older, larger lakes on both this volcano and Macauley, based on the accumulation of large quantities of sulfur in the subsurface. The elemental S at these sites is produced largely by the reaction 2H2S + SO2 = 3S + 2H2O and the disproportionation of magmatic SO2. Anomalous concentrations of Au and Cu in the lakes are most likely transported by vapor." @default.
• W228476918 created "2016-06-24" @default.
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• W228476918 date "2015-01-01" @default.
• W228476918 modified "2023-10-17" @default.
• W228476918 title "Molten Sulfur Lakes of Intraoceanic Arc Volcanoes" @default.
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• W228476918 doi "https://doi.org/10.1007/978-3-642-36833-2_11" @default.
• W228476918 hasPublicationYear "2015" @default.
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