On 17 October 1970, the thermocline in the mixolimnion of Big Soda Lake, Nev., was located between 15 and 20 m below the surface. The chemocline was found to lie between 30 and 35 m depth. Significant dilution of the lake has occurred since 23 July 1933.
Koenig, Ervon R.; Baker, John R.; Paulson, Larry J.; and Tew, Richard W.
"Limnological status of Big Soda Lake, Nevada, October 1970,"
Great Basin Naturalist: Vol. 31
, Article 12.
Available at: https://scholarsarchive.byu.edu/gbn/vol31/iss2/12