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JOHNSON LAKES GEO MAP ( OFR-584) Birds Late Pleistocene Lake Bonneville sediments

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Late Pleistocene Lake Bonneville sediments and related shorelines dominate the landscape

oxygen and hydrogen isotopic analyses of water samples indicate that the thermal fluid is a mixture of meteoric water derived from recharge areas in the Pine Valley Mountains and cold

Pages: 243

dry salt lakes

• Brunton EverNorth Magnet resists demagnetization over time

JOHNSON LAKES GEO MAP ( OFR-584) Birds Late Pleistocene Lake Bonneville sedimentsNULL

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