348 Sixth Supplement to Dana’s Mineralogy. 
Catcrre [p. 435, 503, I, I, II, IV, V].—The calcite from Sparta, New Jer- 
sey, associated with zinci e, has been named Paice by Breithaupt. By measure- 
ment R: R=104° 5 oy; 'G.=2'808—2'818 analysis by Jenzsch is given in 
= IL—Breithaupt i in Berg. u. Hutt. Zeit. xvii i, 8. 
ARMINE SPAR p 410]. —F. Sandberger gives the following analysis (Pogg. ciii, 
3i5) of ox of carmine 
rsenic acid hs) 49°11 Fe 8 Pb 
whence the formula Por As | 5Mels—Arsenic it 485, sesquioxyd of iron 281, 
oxyd of lead 235. G=4'10 
Casstrerrre [p. 118, and V].—Tin ore occurs at Xeres in Mexico.—C. Bergemann 
in N. Jahrb, 1857, p. 395. 
ELESTINE [p. 368]—Fine crystals from Pschow in Upper Silesia have been de- 
crib by Websky i in the Zeits. G. Ges, ix, 303, The planes (arranged according 
0 the zones in the direction of f the brachy diagonal) are as follows: i-7; 7 Fi 4, 6-2; 
4a, 2-4, 2-7; $-8; $3; 4-4; 3. -8; at -24, (the tive preceding planes form- 
ing an oblique zone between J and 1-1); $12 dy 1-2, 1-3, 1-6, 1-16, 14; 4-4, 
$6, $-16, 24; 44; 47,14, 0. 
Pseudomorphs of queebene quartz after celestine are described by R. Blum and 
L. Carius, ste oe 
iad and Pee iron and magnesia carbonate affording the 
Bowe been named PY Breithaupt (Berg. u. 
hiitt. Zeit. xvii, 54) Sid. i. He gives R: R=107° 6’; G. =3616—3 660, 
Analysis of a specim Sita Péhl (of whish G.=8°616) afforded Prof. Fritasche 
(mean of two analyses), 6 41: 7. Fe 45-06, Mg 12-16; or 
MeG 2658 Fe€ 73-42 = 100 =MeC4ored. 
Traversella in Soe he and Bohmsdorf near ge are mor oe as pe locali- 
ties. [Analyses “he é 445 of Min. are of the oe com mgt 
lated compound fr ma Mitter erberg in the Tar — De Khuen (niean of two 
analyses), 6 39°83, cs 51°65, Mn 0°81, Mg 7-5 
Mg6 15°33 Fed ee re a 
Cuonproprrs [p. 186, and IT].—Hessenberg has some notes on the t of 
humite in his Min. Not., p. 14 of the Fortsetzung. [He has overlooked the view of 
the tion of humite taken in the Mineralogy, p. 186 (and Jour. Sci. [2], 
wi eualtth Uh Shcclis W's" tase 12-3 at at Aieuitiig tat te 
crystals are monoclinic, the latter two are +, iced than sae 
_—— [p. 184]—A crystal of Forsterite, from Vesuvius, is described and 
d by Hessenberg (Min. Not, p.21). It has the planes 0, 1-1, +3, 5 +-2, 1+ 
SET he 
Ctausraatrre s0)—Chanathalie te occurs at the mines of Rio Tinto near Se- 
ville, in Spain. in Berg. u. hiitt. Zeit., a 8. 
Se —Pseudomorphs of Brandisite after pyroxene (fassaite) have 
a — described b: mh Ps Verh. Nat. Ges, Basel, 4th Heft, 1857, p. 569). They 
are from Mor in the Som tals of the fassaite at that locality 
| while others have boen more or palpate ther far mete 
ying of mineral coals by the blowpipe, by E. J. Chapman.— 
