Little Colorado River Plateau

Arizona State Land Department, 1974, Arizona Lower Colorado River Resource Area: Arizona State Land Department, Report to President of Senate and Speaker of House, Pursuant to Senate Bill 1331, Thirty First Legislature, First Regular Session, April 1974, [345] p., 12 sheets, approx. scale 1:25,000.

Richard, S.M., Reynolds, S.J., Spencer, J.E., and Pearthree, P.A., comps., 2000, Geologic Map of Arizona: Arizona Geological Survey Map M-35, 1 sheet, scale 1:1,000,000.

Ward, John, 2002, Groundwater on the plateau: Southwest Hydrology, v. 1, no. 4, p. 8, 35.

U.S. Geological Survey, 1973, Availability of ground water in the Navajo and Hopi Indian Reservations, in Geological Survey research 1973: U.S. Geological Survey Professional Paper 850, p. 102.

Allis, R.G., Moore, J.N., Chidsey, T., Morgan, C., Gwynn, W., Doelling, H., Adams, M., Rauzi, S., and White, S., 2002, CO2 geysers, springs and massive travertine deposits on the Colorado Plateau: Examples of natural leakage of fluids saturated in CO2 [abs.]: Geological Society of America Abstracts with Programs, v. 34, p. 392.

Rauzi, S.L., 2002, Arizona has salt!: Arizona Geological Survey, Circular 30, 36 p.

Catlin, C.N., 1926, Character of the ground-water resources of Arizona: Tucson, University of Arizona, College of Agriculture, Agricultural Experiment Station, Bulletin no. 114, p. 173-293.

Smith, H.V., Caster, A.B., Fuller, W.H., Breazeale, E.L., and Draper, George, 1949, The chemical composition of representative Arizona waters: Tucson, University of Arizona, College of Agriculture, Agricultural Experiment Station, Bulletin 225, 76 p.

Weitzman, Morley, 2002, Geology and hydrology of the Payson-Strawberry-Diamond Rim area, Gila and Coconino Counties, central Arizona: Arizona Geological Survey Contributed Report CR-02-B, 17 p., 3 sheets, scale 1:62,500.

Ligner, J.J., White, N.D., Kister, L.R., and Moss, M.E., 1969, Water resources: Part II of Mineral and water resources of Arizona: Arizona Bureau of Mines Bulletin 180, p. 471-580.