"Southward view of the east-vergent Vega de los Patos anticline, cored by the Huitrín Formation evaporites and flanked by the Diamante Formation red beds, developed in a region of thin-skinned deformation of the Malargüe fold-and-thrust belt, Mendoza Province, Argentina (34°39'30''S-69°41'20''W)(Photography by M. Turienzo)".