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Show three parts of the lake suggest that there has been a homogenization of the lake's chemistry, though salinity differences still exist between the south and north arms. REFERENCES Gwynn, J. W. and Sturm, P. A. 1987. Effects of Breaching the Southern Pacific Railroad Causeway, Great Salt Lake, Utah - Physical and Chemical Changes, August 1, 1984- July, 1986: Utah Geological and Mineral Survey Water Resources Bulletin 25, p25. Hahl, D. C. and Handy, A. H. 1969. Great Salt Lake, Utah - Chemical and Physical Variations of the Brine, 1963- 1966: Utah Geological and Mineralogical Survey Water- Resources Bulletin 12, p33. Madison, R. J. 1970. Effects of a Causeway on the Chemistry of the Brine in Great Salt Lake, Utah: Utah Geological and Mineralogical Survey Water- Resources Bulletin 14, p52. Spencer, R. J., Eugster, H. P., Jones, B. F. and Rettig, S. L. 1985. Geochemistry of Great Salt Lake, Utah - 1: Hydrochemistry since 1850: Geochimica et Cosmochimica Acta, v. 49, p. 727- 737. Whelan, J. A. 1973. Great Salt Lake, Utah - Chemical and Physical Variations of the Brine, 1966- 1972: Utah Geological and Mineralogical Survey Water- Resources Bulletin 17, p24. 377 |