Mo iron 
| = chan meteorite vielded the following results :— 
Rr Iron 91°25 
Nickel and co 7°20 
Sor meant: ag a deventevosees LOG 
— 
* 
; their publicati 
~ When at Paris in 1878, 3 same 0 sections 0 
Prof. C 
[Three plates.] 
scot above became somewhat oxidized nS the 
ma the metallic portion from a different part — 
In the oad case the cobalt and nickel eT ae by the 
nitrite 
‘ayer were made to estimate the amounts of schreibersite, — 
&e., ag none were sufliciently a paaeuRce! to warrant 
be 
