* 
Report on Meteorites. 407 
The ang “— of uae 2 
Tro : 89:00 
Niel : ? a 9-60 
. Chromium wid Ne Sa Save a 1-40 
100-00 
F flow mixture of the ey, sitseenie: in the stone, are é 
oll 
Silicic Oy... + co 3.6 Oe ‘ 
Prk sawen;.. A os...» oe 
Magnésia, .. .  . : ba 930 .. oa 
ime,. ; , 5:30 
Alumina, we 1:80 
99°73 
ay Nobleboro, Maine. 
Notices of this stone are contained in Vols. vii, p. 170, and 
1Sp-p. 400, also in Boston Journal of Philosophy and the Arts, 
and Die Meteoriten von P. Partsch, s. 29, Wien, 1843. The 
crust is a perfectly fused and shining glass, similar to the Juve- 
nas and Stannern stones. The color of the interior is a light ash- 
grey. When examined by the aid ofa lens, it is found to be 
highly composite in character, pate the small fragment i in my 
possession shows neither nickel-iron nor magnetic pyrites. The 
most — ingredient is howardite, through which are dis- 
| ns of greenish transparent olivinoid, white  par- 
ticles of ssiasbiee. black grains of chantonnite, and a red color- 
ed, vitreous, hard mineral, which ayeedie to be either garnet o1 
idocra ase. 
7. Little Ferg Missduri. ai 
Brief — of this _— ‘are contained i in Vols. xxxvii, p. 
I have so ti avored with stot additional particulars respect- 
ing its fall, from p wl ide in the vicinity of the locality. 
Bluff, on Gasconade river, 
Do te came jts size and 
to those of a blacksmith’s bellows, moving with the large 
most. A bright light or blaze: was nol om to hover sou 
ipebesetieemity: of thesinaah, ap hich 
