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dc.contributor.authorMin, Brian
dc.date.accessioned2012-03-30T23:39:55Z
dc.date.available2012-03-30T23:39:55Z
dc.date.issued2011-03
dc.identifier.urihttp://hdl.handle.net/1773/19685
dc.descriptionSenior thesis written for Oceanography 444en_US
dc.description.abstractManganese (Mn) in hydrothermal vent plumes is an indicator of the vent characteristics that spawned the plume. Mn concentrations in Pele's Pit in Hawaii and the Cleft segment in the Juan de Fuca Ridge were compared. Mn was lower in Pele's Pit, an indication of weaker seismic activity.en_US
dc.language.isoen_USen_US
dc.subjectHydrothermal vents--Loihi seamount--Observationsen_US
dc.subjectChemical oceanography--Loihi seamounten_US
dc.titleManganese concentration of hydrothermal plume at Pele’s Pit, Loihi Seamount, Hawaiien_US
dc.typeOtheren_US


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