Mineralogical processes taking place close to equilibrium, or with very slow kinetics, are difficult to quantify precisely. The determination of ultraslow dissolution/precipitation rates would reveal characteristic timing associated with these processes that are important at geological scale. We have designed an advanced high-resolution white-beam phase-shift interferometry microscope to measure growth rates of crystals at very low supersaturation values. To test this technique, we have selected the giant gypsum crystals of Naica ore mines in Chihuahua, Mexico, a challenging subject in mineral formation. They are thought to form by a self-feeding mechanism driven by solution-mediated anhydritegypsum phase transition, and therefore they must be the result of an extremely slow crystallization process close to equilibrium. To calculate the formation time of these crystals we have measured the growth rates of the f010g face of gypsum growing from current Naica waters at different temperatures. The slowest measurable growth rate was found at 55°C, 1.4 AE 0.2 × 10 −5 nm∕s, the slowest directly measured normal growth rate for any crystal growth process. At higher temperatures, growth rates increase exponentially because of decreasing gypsum solubility and higher kinetic coefficient. At 50°C neither growth nor dissolution was observed indicating that growth of giant crystals of gypsum occurred at Naica between 58°C (gypsum/anhydrite transition temperature) and the current temperature of Naica waters, confirming formation temperatures determined from fluid inclusion studies. Our results demonstrate the usefulness of applying advanced optical techniques in laboratory experiments to gain a better understanding of crystal growth processes occurring at a geological timescale.phase shifting interferometry | mineral growth D uring the last decade, the field of mineral growth has experienced important advances in analytical instrumentation (1). The development of state-of-the-art methods for nanometric observation, such as high-resolution atomic force microscopy (2), or advanced optical microscopy techniques like laser confocal differential interference contrast microscopy (3) and phase-shift interferometry (4, 5), have allowed the study at nanoscopic levels of the different growth mechanisms exhibited by crystals, emphasizing the direct relation between the morphology and the growth processes taking place on each crystal face. For example, the application of in situ nanoscale observation of calcite crystal growth in the lab have revealed the microscopic causes of the large morphological variety exhibited by natural occurring calcite crystals (6-8). These, and other works (9-11) have demonstrated the power of laboratory crystal growth studies for sharpening the picture of crystallization occurring in nature.Recently, a very striking crystal growth problem in earth sciences has emerged: the existence of giant crystals of gypsum (CaSO 4 :2H 2 O), in particular those found in the range of Naica, Mexico (12, 13). Large gypsum cryst...