Zircon
                This crystal is from the sand collected on a beach of Big
                  Talbot Island, Florida. The heavy minerals, including zircon,
                  were concentrated by density for analysis using lithium heteropolytunstantes.
              
              
                Transmitted Circular Polarized Light
                
Definition/Function:
                Zircon is Zirconium Silicate (ZrSiO4). It is a very durable mineral and some
                grains have been dated back to at least 4.4
                billion years based on the decay of uranium included in the crystals matrix. The Oxygen
                isotope ratio is used to assess the nature of
                the environment at the time of the formation of the crystals.
                Significance in the Environment:
                Characteristic Features:
                Zircon belongs to the tetragonal crystal system and is optically positive. Its
                refractive indices are 1.922-1.960 and 1.961-2.015.
                Its birefringence ranges from 0.042 to 0.065. The density of Zircon is about 4.6
                grams/cc. Small grains tend to be
                colorless. Zircons are often found in soils and sands as well formed crystals or as
                rounded ellipses.
                Associated Particles:
                Zircons are common in igneous rocks and in sedimentary deposits. It is one of the
                minerals used to characterize soils,
                sediments, and conditions at the time of formation and age of igneous rocks.
                References:
                Deer, W. A., R. A. Howie, and J. Zussman, AN INTRODCUTION TO THE ROCK-FORMING MINERALS,
                ISBN 0-582-30094-0, pp. 22-6, 1992.
                Wilde, Simon A., John W. Valley, William H. Peck, and Colin M. Graham, "Evidence from
                detrital zircons for the existence of continental
                crust and ocieans on the Earth 4.4 Gyr ago", NATURE, vol. 409, pp. 175-178, 11 Jan.
                2001.
                Hanchar, J. M. and C. F. Miller, "Zircon sonation patterns as revealed by
                chattodoluminescence and backscattered electron images:
                implications for interpretation of complex crustal histories", CHEMICAL GEOLOGY (ISSN
                OOO9-2541),PP. 1-13, 1993.
                Bowen, Andrew, "Individualizing minerals: a proposed approach for forensic soil
                comparison", MICROSCOPE, vol. 55, no. 2, pp. 59-73, 2007.
                Hanchar, J.M. and P.O.W. Hoskin, (ed.), ZIRCON, Reviews in Mineralogy & Geochmistry,
                vol. 53, 2003.