Abstract
The satellite, fully 150 kilometers in diameter, was close enough to Euterpe to shine like a brilliant dot of sparkling light. It was so close to the planet that one could see it sweep west to east across the sky, outstrip** the planet’s slow rotational motion. It brightened as it rose towards zenith, and dimmed as it dropped towards the horizon again. One watched it with fascination the first night; with less the second; and with a vague discontent the third – assuming the sky was clear on those nights, which it usually wasn’t.
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Suggestion for Further Reading
Dowty, E., 1976, Crystal Structure and Crystal Growth: I. The influence of internal structure on morphology, Amer. Mineral, 61, 448-459.
Emmons, R.C. and Gates, R.M., 1948, The use of Becke line colors in refractive index determinations, Amer. Mineral, 33, 612-618.
Hecht, E., 1987, Optics, Addison-Wesley.
Hurlbut, C.S., 1984, The jeweler’s refractometer as a mineralogical tool, Amer. Mineral, 69, 391-398.
Laskowski, T.E., Scotford, D.M. and Laskowski, D.E., 1979, Measurement of refractive index in thin sections using dispersion staining and oil immersion techniques, Amer. Mineral, 64, 440-445.
Nesse, W.D., 1986, Introduction to Optical Mineralogy, Oxford University Press, Oxford UK, 325p.
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Verma, P.K. (2023). Refractometry. In: Optical Mineralogy. Springer, Cham. https://doi.org/10.1007/978-3-031-40765-9_3
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DOI: https://doi.org/10.1007/978-3-031-40765-9_3
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