CLARKE.] 
STONY METEORITES. 
285 
This meteorite also contained a dark vein of sp. gr., 3.585, which 
carried 2.30 per cent of metallic iron. Analyses, made on less than 
0.4 gram of material, gave as follows, recalculated to 100 per cent: 
E. Soluble in hydrochloric acid, metal deducted. 
F. Insoluble. 
E. 
F. 
Si0 2 - 
27. 63 
2.41 
34.31 
3.27 
trace 
32.12 
.52 
56. 52 
A1 2 3 
1.51 
FeO 
12.35 
NiO-4-CoO 
4.09 
CaO 
trace 
MgO 
25.53 
s 
100. 26 
.26 
100.00 
Lees =S 
100. 00 
E represents 51 per cent and F 44 per cent of the vein. 
10, SAN BERNARDINO COUNTY, CALIFORNIA. 
Found in the San Emigdio Mountains. Analyzed by J. E. Whit- 
field, record Nos. 804 and 936, and described in Bull. 60, p. 114. In 
fragments, badly altered. 
Approximate composition of the mass. 
Nickel-iron 6. 21 
Soluble silicates, etc : 51. 26 
Insoluble silicates 42. 23 
99.70 
The soluble part was probably olivine and pyrrhotite, with secondary 
iron oxide. The insoluble part was enstatite, essentially. 
A. The nickel-iron. 
B. The enstatite. 
A. 
B. 
Fe .. 
88.25 
11.27 
.48 
Si(), 
54.42 
Ni 
FeO 
14.03 
Co 
CaO 
2.46 
MgO 
29.11 
100. 00 
100. 02 
