March, 1907. Iron Meteorites — Farrington. 



OUP. 



OUP. 



anomalous composition. It may however for the present be included 

 among- meteorites. 



>s. 



Undet. 



Total 



99.19 

 100.40 



Sp. Gr. 



6.854 



Analyst. 



W. J. Taylor 

 E. Cohen . . . 



Reference. 



1S57, A. J. S. (2), XXIV, 294 



1892, Meteoreisen-Studien, 11, A. N. fl., VII, m 



lies between the nickel-rich and nickel-poor ataxites. On etching, 

 irregularly shaped areas appear, 0.2-2 cm. in area, which under the 

 microscope have a spotted look and are generally bordered, as are 



! most of the silicate grains, by narrow, zigzag bands the nature of 



which cannot be further determined. 



:essory Forsterite. 



