White Sands & Carlsbad Caverns — Gypsum & Limestone
Two days linking the surface geology of White Sands with the underground geology of Carlsbad Caverns — both formed from the same ancient Permian sea that covered West Texas and New Mexico 265 million years ago. The gypsum at White Sands and the limestone of Carlsbad Caverns are both products of that Permian marine environment; the Capitan Reef (the limestone formation in which Carlsbad Caverns formed) and the gypsum deposits in the San Andres Mountains (the source of the White Sands dunes) are contemporary Permian formations. The through-line is deep geological time made visually accessible: at White Sands, Permian gypsum is visible as white sand on the surface; at Carlsbad Caverns, Permian limestone dissolved by sulfuric acid created a cave system of extraordinary scale. Day one covers White Sands and the drive to Carlsbad; day two is Carlsbad Caverns with the Natural Entrance, Big Room, and bat flight.