Nuclear microprobe analysis and backscattered 57Fe Mössbauer spectroscopic methods have been used to study the desert varnish surface coatings on samples of dolerite and sandstone from the Taylor Valley area of the McMurdo Dry Valley region, South Victoria Land, Antarctica. With the nuclear microprobe method the oxygen content of the varnish coating and underlying bulk rock was measured directly using the emitted protons from the 16O(d,p 1) 17O nuclear reaction, and also the 871-keV gamma rays emitted from the excited oxygen nucleus. In addition, the iron, calcium and sulphur contents were measured using their characteristic proton-induced fluorescent X-rays. The concentration profiles of these elements are presented in three- and two-dimensional diagrammatic representations. These show that in the Fe-containing dolerites, the desert varnish is formed by subsurface leaching of the Fe from the bulk rock. This is transported to the surface and deposited as a coating of hydrous ferric oxide, probably ferrihydrite, by subsequent oxidation and evaporation. In the essentially Fe-deficient sandstone, the Fe is derived externally from the overlying dolerite sills and is similarly transported and deposited as a varnish coating on the upper surfaces of the sandstone. Windblown inorganic salts, notably thenardite (Na 2SO 4) may be incorporated in the outer layers of the varnish. The backscattered 57Fe Mössbauer spectra recorded using both the conversion electrons and X-rays show that at a depth of ∼ 0.1 μm from the surface the predominant oxidation state of the Fe in the dolerite is Fe 3+, whereas at depths of 10 μm or more it is Fe 2+. For the sandstone it is present only as Fe 3+.