Relationships of fine-grained glacial sediment and total organic carbon in Glacier Bay, Alaska

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dc.contributor.authorTheiss, Aubrey
dc.date.accessioned2008-07-18T21:21:18Z
dc.date.available2008-07-18T21:21:18Z
dc.date.issued2008-06-19
dc.description.abstractThe relationship between marine geology and marine chemistry was explored in Glacier Bay by correlating sediment grain size to particulate organic carbon (POC.) Marine and alpine glaciers produce sediment in the bay. It was hypothesized that sediment from alpine glaciers would hold higher concentrations of POC because of finer grain size.en
dc.identifier.citationKeil R., Kelley D., D'Asaro E., Krembs C., and Collins R.E. [Eds.] 2008. Proceedings from the University of Washington School of Oceanography Undergraduate Thesis Research Expedition to Glacier Bay Alaska, March 2008. 296pp.en
dc.identifier.urihttp://hdl.handle.net/1773/3751
dc.language.isoen_USen
dc.publisherSchool of Oceanography, University of Washingtonen
dc.subjectMarine sediments--Alaska--Glacier Bayen
dc.subjectSedimentation analysisen
dc.titleRelationships of fine-grained glacial sediment and total organic carbon in Glacier Bay, Alaskaen
dc.typeOtheren

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