MARCH, 1907. IRON METEORITES —F ARRINGTON. gI 
banan group, so that the group is a transition to the finest octahe- 


drites. 
Indet.| Total. SD Gl’. Analyst. Reference. 
ts 99.97 7.525 |M. Neff & A. Stocky|1899, Prog.d.Béhm Gym.in Mahr-Ostrow 
BOS LODE] es ve tse 5's pA ric egee ee 1867, Ale odt 2), Ll, 280 
Bt FOO O21 6 aia s vin e'o 1.2 ahrentorst. «22... 1900, Meteoreisen-Studien, XI, A. N. H. XV, 
37 98% 
= Soom aeet.. 21. Durger,........,|r905, Meteoritenkunde, III, 299 
oe. Copege sees. - iti, W. Nichols. .....{1905; Field Col: Mus. Geol. Ser. IIT, 4 

a. SALTY RIVER GROUP. 
The content of nickel-cobalt is lower than in the Tazewell group, 
not exceeding 10% percent. Plessite predominates as compared with 
the Tazewell group. Schreibersite is common in numerous small, 
elongated individuals, . 





indet.| Total. Sp. Gr. Analyst. Reference. 
ms 96.285} 7.69 je.. Whitfield +: :..j1902, Proc: Roch: Acad. Sci. IV, 74 
ae 100.14 7.59 Cohen & Hildebrand/1903, Mitt. N. ee f. Neu Vorp. u. Riigen, 
XXXV, 13 
ey 100.40 7.8432 |O. Sjéstr6m......../1898, Ber. Berlin Akad., 19-22 
Bee 100.00 7.8 Mariner & Hoskins.|1898, A. J. S. (4), V, 137 
ae 99.53 7.72 PeommMiNic cate ns el OF fy Chat be OE Zee e why 2E3 
Be 100.36 |...........|W. H. Brewer......|1851, Proc. A. A. A. Sci. IV, 36-38 
ee 100.84 7.6648 |J. Fahrenhorst .....|1900, Meteoreisen-Studien, X, A. N. H. XV, 
| 76 
