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dc.contributor.authorBergquist, Justin
dc.date.accessioned2008-07-23T18:30:11Z
dc.date.available2008-07-23T18:30:11Z
dc.date.issued2008-06-19
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/1773/3760
dc.description.abstractThe rate of sedimentation in Glacier Bay is considerably higher than in similar environments. Because of glacier melt, sedimentation rate is an important indicator of climate change. This study measured 210Pb in sediment cores from the bay.en
dc.language.isoen_USen
dc.publisherSchool of Oceanography, University of Washingtonen
dc.subjectSedimentation and deposition--Alaska--Glacier Bayen
dc.subjectSedimentation and deposition--measurementen
dc.titleSediment accumulation rates in the West Arm of Glacier Bay, Alaska based on Lead-210 analysisen
dc.typeOtheren


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