Sediment accumulation rates in the West Arm of Glacier Bay, Alaska based on Lead-210 analysis

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Sediment accumulation rates in the West Arm of Glacier Bay, Alaska based on Lead-210 analysis

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dc.contributor.author Bergquist, Justin
dc.date.accessioned 2008-07-23T18:30:11Z
dc.date.available 2008-07-23T18:30:11Z
dc.date.issued 2008-06-19
dc.identifier.citation Keil 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.uri http://hdl.handle.net/1773/3760
dc.description.abstract The 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.iso en_US en
dc.publisher School of Oceanography, University of Washington en
dc.subject Sedimentation and deposition--Alaska--Glacier Bay en
dc.subject Sedimentation and deposition--measurement en
dc.title Sediment accumulation rates in the West Arm of Glacier Bay, Alaska based on Lead-210 analysis en
dc.type Other en


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