Transmitted Linear Polarized Light, Darkfield Dispersion Staining Illumination Mounted in 1.662 Refractive Index Medium
Definition/Function:
Tourmaline has the general formula of (Na,Ca)(Mg,Fe,Mn,Li,Al)3(Al,Mg,Fe)6[Si6O18](BO3)3(O,OH)3(OH,F).
It is a common mineral in some granites or metamorphic deposits.
Sand is a large accumulation of small rock and/or mineral particles in the size range of from 20 micrometers to 2,000
micrometers in diameter. Sand may include small shells or shell fragments and oolitic deposits. Sand is a size and
density segregated material that is the result of air or water action.
Significance in the Environment:
This is an example of a dense sand where wave and current action has removed most of the lighter minerals, such as quartz
and feldspars, from the beach.
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Characteristic Features:
Tourmaline belongs to the trigonal crystal system and is optically negative. Its refractive indices are 1.612-1.650 for epsilon and
1.633-1.671 for Omega. Its birefringence ranges from 0.017 to 0.035. The density of tourmaline ranges from about 2.9 to 3.22 grams/cc.
Small grains may be colorless to black. Their pleochroism is strong if they are strongly colored. The absorption is always strongest along
omega, the highest refractive index. The long axis of the grains tends to be the epsilon direction.
Associated Particles:
References:
Deer, W. A., R. A. Howie, and J. Zussman, AN INTRODCUTION TO THE ROCK-FORMING MINERALS, ISBN 0-582-30094-0, pp. 130-7, 1992.