Gypsum megacrystals from chemistry notes

picture taken from Garcia-Ruiz, J.M. et al. 2007 Geology 35(4), 327.

Although this isn't exactly a chemistry article, it is most certainly chemistry related, and I hope that you will agree that these pictures are too awesome to believe. The gigantic crystals pictured above made the cover of this month's Geology. Almost 80 years ago, the excavation of caves and tunnels at the Naica mine (112km Southeast of Chihuahua, Mexico) led to the discovery of meter-sized single crystals of selenite, which is one of the four crystal forms of gypsum. (The other three forms are satin spar, desert rose, and gypsum flower. As a side note, when I was younger I had a great collection of rocks and minerals that included a very nice sample of desert rose). Often these crystals of calcium sulfate dihydrate are found coated in calcite (calcium carbonate), celestite (strontium sulfate), or trace amounts of iron oxide, which give the crystals either a white or slightly red hue; selenite is colorless/transparent in its pure form. Amazingly, the Cueva de los Cristales (Cave of Crystals) contains selenite crystals up to 11 meters in length and 1 meter thick, with minimal contamination from other minerals.

While several have made conjectures as to how these crystals formed, none had been investigated carefully until now. Garcia-Ruiz and coworkers set out to explain the formation and growth of the Naica megacrystals after closely considering several factors. First, gypsum is slightly soluble in water, with a maximal solubility observed at 58 degrees C; conveniently, water samples from the Naica mines have temperatures ranging from 48-59 degrees C. Thus, the water found in the area is slightly supersaturated for gypsum and slightly undersaturated for the anhydrite form of calcium sulfate, suggesting a self-feeding mechanism. In other words, crystal growth might have been driven by a solution controlled anhydrite-gypsum phase transition. Calculation of the nucleation rate indicated that this suggested mechanism is a probable one, but only within a very narrow range of temperatures--46 to 60 degrees C. Such calculations indicate that these crystals have been growing in the caves at Naica for over one million years!

For more information:

The Largest Crystals on Earth

More pictures