196 Second Supplement to Dana's Mineralogy. 
ANO: 234],—Analysis of anorthite from I. St. Eustache, by Deville, (Aan. 
nea i Phys [3] [3]al , 286 and Lieb. u. Kopp., 1854, 832); specific gravity 2°78: 
Si458 213850 6al77 Mgoo Nai0=1004 
Antmony GLANcE [p. 33].—Loe. in California, Am. J. Sci. [2], xx, 82. 
Apvatire [p. 396]—Kokscharev, in Min. Russl., ii, i, 89, » BES ) raat Bp new 
of crys- 
planes 3 and 3. He figures many new crystals. Fro measuremen 
rom the Ural Emerald mine, O: foe oa th as an" the same as 
friedersdorf cry erystals fi == 139 NB te 4 same 2g 
e Lake Laach crystals. The Spates arn ‘ors 139° 4 
Analyses: 1. Y apatite from Miask, by G. von Rath, (Pes. xcvi, wees 2, 
— the a ee R. Bluhme (Verh, nat. ve, than 1855, 111, and Ann. 
Pharm., x se 
p fe Gs Fe me 0 h 2am 
1° 4208 4975. 887 O16 —— ee TO 
2, 8738 4750 —— 828 270 220 350 165 1:84==100 . 
Tn ro * as 3°87 Ca require 3-62 fluorine, the loss is probably all fluorine ex- 
5 a Oe 
ARA sare tg —An Aragonite in columnar crystallization of unknown lo- 
cality, ponew oe poe: afforded G. Jenzsch, (Pogg., xevi, 145): 
OG $6 MeG KG NaC Cam CaP CaS 
91°17 0°27 0°48 0°62 0°59 3:27 1:24 086 2:°26= 10076 
Color snow-white. G.—=2°830. Fluor was detected i in the Aragonite of Volterra, ete. 
Avarre, see Pyroxene. ) 
AvrRIcHALcrTE [p. 460].—Loe. in Lancaster, Pa., W. J. Taylor, Am. J. Sci., xx, 412. 
ares k [p. 459].—Analysis of Azurite from Pheenixville, Pa. J. L. Smith, Am. J. 
BaBINGTONITE Ep 178 ].—Babingtonite is penal by Dauber into close connection 
with the Paisbergite (Pogg., xciv, Kah “je ls orga of 82 crystals, he 
arrives at the wets ab=112° 12’, ac==92° Roe . Referred to tithe form 
of anes (see figure under Paisbuagite) ere’ angles ar ! ['=112? 12’, 0: [= 
92° 82’, 7: P’=87° 24’. Cleavage parallel to ¢ (Z), fate so Spurn to & (1). 
ara ytes [p.366]—Crystallographic ne oe nes crystals as ascertained by erosion 
: sith acid, Leydolt, Acad, Wiss, Wien, May, 1 
Berry [p. 178]—Many figures of Russian Sie by Kokscharov, Min. Russl., 
1854, p.147. One onal affords the plane 1242, Specific gee’ of transparent 
_ erystals: from Mursinka, yellow, 2694; ib. gre nish-yellow, 2 2°683 ; ib. greenish- 
saa 2681: from Sehaitanka, ¢ ~olorless ss, 2°694, 2 ; pale cone pt apple- 
” green, 2°710: from Adun- Tschilon, bluish-green, 261 ve: from Urulga, n, 2702. 
POP is160° 3/ 24 
- ‘The Emera lof tie Ural afforded A. B, Kammerer, sp. gr. =2°710—2°759; 2742, 
of the best results, 
Brromen [p. 469]. — Locality in California, W. P. Blake, Am. J. Sci. [2], xix, 433, 
f Trinidad, N.S. Manross, Am. J. Sci. [2], xx, 158. 
ysis ; from Phenixville, Pa., J. peRntS Sci. xx, 250. 
massive boracite of Stassfurth, which occurs in large oF 
Tanlnce and Segeberg.. When pulverized the particles show electric 
those of the crystallized si (G. H. O. V: # note Mon, d. 
