208 J. L. Smith—New Wisconsin Meteoric Stone. 
tones. Examined with a glass the grains are of a dirty green 
through the mass, and particles of troilite are also visible. 
Its specific gravity is 3°66 and it is composed of: 
t rites ts EL Cee ee 78°33 per cent. 
Metallic particles _............2... 1707 “ 
WONNNSO Ss 200 i ee Sale. 460 * 
100°00 
The stony matter treated with aqua regia furnished : 
Permittee SS OE 47°20 per cent. 
Ensoluble matter... 52°80 “ 
100°00 
The composition of these two portions are: 
Soluble. Insoluble. 
32°5 57 
ee es 5 “£1 
Lrotosiaes of an 2 30°40 9°50 
ic NeoPa nia’ ape viele UaRGE ae tae trace. 4°00 
pee a eae 35°80 22°80 
ime Se ee ee 3°70 
Bi re tee 60 2:01 
99°35 99°42 
The metallic particles, completely separated from the stony 
portion, are composed of: 
eo 92°15 
ON ae 7°37 
Ee 0G 28 
Copper very minute quantity ; ae eee 
Phosphorus hes estimated. 99°80 
In regarding the above analyses, it is very evident that the 
meteorite is made up of 
ronzite, with probably a little anorthite -.-. 41°35 
ite (olivine) --- 36°98 
on 
=< 
As I was not Pee a find analysis of the Meno (Alt 
Strelitz Mecklenburg) meteorite, which fell Oct. 1st, i 
midday, and as the physical aspects of the one just descr! 
eee gee 
