The case-hardened crust developed on the Aztec Sandstone in the Valley of Fire,
Nevada, has been characterized by a variety of techniques, including electron microscopy
and infrared spectroscopy. The case-hardened crust consists mainly of host rock, with a
fine-grained cement and wind-deposited kaolinite. The cement is usually calcite, but in
some cases the hydrated calcium borate, colemanite, was found to be the case-hardening
cement