THE BOND SPRINGS STONY METEORITE 
57 
Limonite. Limonite due to weatliering is present in very 
small amounts as occasional narrow seams which enclose 
small chondrules and infill cracks, but neither nickel-iron 
nor pyrrhotite have given rise to limonite. 
References. 
1. Bradley, A. J., and H. J. Goldschmidt. An X-Ray Investigation of the 
Iron-Rich Nickel-Iron Alloys. Journ. Iron Steel Inst., vol. cxl, No. II, 
11, 1939. 
2. Bullard, F. M. The Rosebud Meteorite, Milam County, Texas. Ameri- 
can Mineralo^st, vol. 24, No. 4, pp. 242-254, 1939. 
3. Campbell Smith, W. A New Meteoric Stone from Suwahib, Arabia. 
Mjn. Mag. xxiii, pp. 290-304, 1932. 
4. Dunn, J. A. The Rangala Meteorite. Records Geol. Surv. India, vol. 
74, pp. 260-276, 1939. 
5. Farnham, C. M. Determination of the Opaque Minerals. McGraw- 
Hill, 1931. 
6. Fletcher, L. An Introduction to the Study of Meteorites. British 
Museum (Natural History) Guide Book, 10th edition, 1908. 
7. Hodge-Smith, T. Australian Meteorites. Australian Museum Memoir, 
vii, 1939 . 
8. Hutton, C. O. The Morven Meteorite; An Aerolite from South 
Canterbury, New Zealand. Min. Mag. xxiv, pp. 265-275, 1936. 
9. Johnston, R. A. A., and Ellsworth, H. V. The Annaheim Meteorite. 
Trans. Roy. Soc. Canada, vol. xv, section IV, 1921. 
10. Short, M. N. Microscopic Determination of the Ore Minerals. Geol. 
Surv. U.S.A., Bull, 825, 1931. 
11. Stillwell, F. L. The Caroline Stony Meteorite. This Memoir, pp. 41-47. 
12. Vanick, J. S. Microstructural Features of Several Meteorites. Trans. 
Amer. Soc. Steel Treatment, vol. 7, 1925. 
