Zeolites commonly occur as microscopic crystals and are often overlooked. However, we benefit from these minerals in many unrecognized ways. Their distinctive crystal structures result in their ability to hydrate/dehydrate reversibly, to exchange cations with aqueous solutions, and to act as molecular sieves. These structure-related physicochemical properties make zeolites an important group of industrial minerals. In nature, they form as one of the first alteration products of continental and oceanic crust under low-temperature conditions. The distribution and occurrence of zeolites can provide important constraints on the spatial and temporal evolution of geological systems within the shallow crust.
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