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Magnetic Properties of Sediments in Cores BL96-1, -2, and -3 from Bear Lake, Utah and Idaho

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As part of an ongoing study to derive records of past environmental change from lake sediments in the western United States, a set of three cores was collected from Bear Lake, Utah, in 1996. The three cores, BL96-1, -2, and -3, form an east-west profile and are located in about 50, 40 , and 30 m of water, respectively. The cores range in length from 4 m to 5 m, but because sediments thin markedly to the west (Colman, 2005) the maximum age of sediments penetrated increases from east to west. Together the cores provide a record from the last glacial period through the Holocene. This report presents magnetic property data acquired from these cores. [Summary provided by the USGS.]
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