Hydrothermal systems in Hawaii

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dc.contributor.authorThomas, Donald M.
dc.date.accessioned2014-11-17T23:14:21Z
dc.date.available2014-11-17T23:14:21Z
dc.date.issued1989
dc.description.abstractIntroduction: "One consequence of the volcanism that formed the islands of the Hawaiian archipelago is the evolution of hydrothermal activity. Surface manifestations of active hydrothermal systems are evident on the young, eruptively active volcanoes on the island of Hawaii; even on the older, long dormant volcanoes of Maui and Oahu, geophysical and geochemical evidence has been found for lower temperature hydrothermal systems. The physical and chemical characteristics of these systems span a broad range and depend heavily upon the geologic and hydrologic conditions of their formation and evolution."
dc.description.abstractFrom The Geology of North America Volume N, The Eastern Pacific Ocean and Hawaii, p. 271-277.
dc.format.extent8 pages
dc.identifier.citationThomas DM. 1989. Hydrothermal Systems in Hawaii: in The Geology of North America Volume N, The Eastern Pacific Ocean and Hawaii, p. 271-277.
dc.identifier.urihttp://hdl.handle.net/10524/47079
dc.language.isoen-US
dc.publisherGeological Society of America
dc.subjecthydrology
dc.subjectvolcanoes
dc.subjectlegal
dc.subjectKilauea East Rift Zone
dc.subjectKilauea
dc.subjectPuna
dc.subjectHawaii
dc.subject.lcshGroundwater flow--Hawaii--Kilauea Volcano Region
dc.titleHydrothermal systems in Hawaii
dc.typeReport
dc.type.dcmiText
local.identifier.callnumberQE71 .G48 1986

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