Second Supplement to Dana’s Mineralogy. 207 
On some needles of Millerite he found small ip rhombohedral crystals giving 
e angle R: R=105° 15 pata et too few for analysis, but may have been a 
ealtite containing a carbonate of nickel. 
Morerene [p. 401].—Analyses, etc., Phoenixville, Pa., J. L. Smith, xx, 248. 
Misric p. 62 ager her of Mispickel of Copiapo, a L. Smith (Gilliss’s 
Exped., ii, i 109): § 20°25, As 44°30, Fe is a Co 5:84 = 
Mispickel eciselinphione after Pyrrhotine has hg sboorvtil by Kenngott, in 
specimens from Freiberg in Saxony (Min. Not, No. 14). 
reap or Iron (?) [p. 144].—Loeality in Heard Co., Georgia, Am. J. Sci. [2], 
xix, 
MORENOSITE, A. Casares.—A — 1 vitriol occurring in Spain n(Hartm, Zeit. vii, 
37, and Kenngott’s Min. Forsch, for 1853, 16), in nee edles or thin prisms, Soluble in 
Water, solution green, Reactions indicate Ni, S, (and also H?) with mixed Cuand Fe, 
Naparaa iP. 469]—On some of the fle ponepnenia of coal Naphtha, by C. 
Greville Williams, Edinb, N. Phil. J. [21, 
Native Iron [p. 17}—The s Ls sed s ative Iron of Canaan, Ct, has been an- 
po by Dr. A. et Hayes of Boston, and proved thus to be a furnace product. It 
i sa i and affords full i se that it has been artificially reduced from 
has examined masses of iron purporting to be native, from Liberia, 
Aitiea a2 nd finds them a sce ure all a carbon, slike any artificial iron, and 
“hasta gr of quartz are disseminated through it; and the evidence from 
s 
ure iron 98°40, quartz grains, magnetic oxyd of iron, and zeolite 1:60 = 100-00. 
¢ locality is in the rg pene bore gr fsb Bassa county, Liberia. It probably 
Cccurs in large deposits 
[ rice seyyc? crystals afforded v. Kokscharov, (Min. Russl, ii, 
1 ‘a 1= 1=isse 29) 4° BHO: :1= 1350 BAe Breithaupt obtained fo 
| Biidiigee 184° 3 Scacchi, 13 
].—Mean of two analyses by C. y. eet, (Jahrb. geol. Pago 
1854, 190, sr Si - be oe 27°28, Se by H{ 18-04 = 100-08, giving the 
ceived formula Cas § 
‘ Ostaanire [p. 196] cere confirms (Min. Not. No. 15), by a eS 
awe the identity of Ostranite with Zircon. The Ostranite is from Brevig, 
eway. 
Patarrive (native).—Hofstidter, in J. f. pr. Chem., Ixiii, 410). 
Patsprrerre [p. 168).—H. Da 
mee uber (Pogg. xciv, 398), 
describes ¢ this Bae 1 —— decarring ‘a ( asia 
the 
+ a6 099 dey ident 38"; 
Angles ae== 939 2837, a’ 1179 45}', ok 148° 474, ab 111° 
an 106° 83" $n’ 149° 394, be 87°38’, b/c 92° 227 
0¢ 186° 847 95131997 sc 138° 114’, 6’ 184° OF 
me 94°36’, mle 85° 24’ = 102° 58’ ks 139° 43/ 
m8 126°11% 9 118958’ a0 107° 16", kb 76° 59" 
