Pharm 
PSS We el ee ene tee — lee te 
Be eee 
Fifth Supplement to Dana's Mineralogy. 407 
being the ae and ¢ the orthodiagonal) = 0 8558:1:0°5503. 1-i:4i=— 
154° 34/, 1-1 O17’, 1-€: b=e126° 26’, J: 11619 13’, Clora: 5) = =648 18’. 
Hesenterg ts ninerak on crystals from Zermatt and St. Gothard the new planes 
$ 4, -4, -},-7, -7-7, 44 (Lieb. u. Kopp, 1856, p. 849). 
RYTHRINE or Cobalt Bloom [p. ae wo of a specimen from Joachimsthal 
by Lindaker (Vogl’s Min. Joach. , Pp. 160): 
As 
% Ni e H 
3642 O86 «8875 «1126 «S51 42852997 
giving the usual fcrmula, 
Evcrrorre (p- 421].—A mineral, not yet determined, but resembling euchroite 
has been observed ot gn ot (Frogs. cii, feed — with the Dioptase of the 
irghis stepp 
Metres high and thick + tr aadiAe. plan es ef Ae 1; =F plates ined had 
the summit angle of the dome 1.3 nearly a right sie, that of m-i more obtuse, 
Planes J yer rtically striated. 
Evxourre [p, 42 ,and I cal 
grounds (Ann, d. M. iy oe, 26 a) a TRakolite is poner oad near Piradialye “ tat 
has a negative axis, while Eudialyte has a 
Fanortite or Mesole [p. 828, and IV].—Aceording to Dr. Heddle (Phil. Mag., (41, 
Xv, 28), the globules of faroelite from Farée (cave in Naalsée) consist of crystals ; 
and he has found on me easurement that they are right rectangu oe prisms, with highly 
Perfect pearly cleavage, stilBite-like, parallel to one of the lateral faces of this prism. 
There are planes on the edges of the prism, and they are inclined to the ¢ onal 
Pema [p. 479), —A memoir on ts species is published in the Ann. d. Ch. u 
J. Sci re “hi ciii, 236; and also, revised by the author, in this volume (aun. 
bias 64). 
Garver RT [p. 199, and T, IT, III, [V}.—A whitish compact garnet rock occurs in the 
Green Mountains t to the north, along with euphotides, according to o Pro of. T. S. Hunt 
(Logan's Canada Geol. Rep., and Phil. Mag., [4], xiv, 388). It is distinguished from 
4g by its 8 tog i ity, which is 8 a3. It_ is mixed with gate 
r. 
Position ‘seuonding 4 Hemt ee n’s he, 1847, p- 4 
ae | Ca g FBe,Mn Na,K ign. ; 
1. Orford, 38-70 29-71 34-83 oa 160 0-47 1:10==99-90. G.==3-522-3-536 
A relted rock, from St. a was found to correspond in composition to 57-72 
and 40-71] 
The “Ap ag Sodalite, _ Hanyne, ge Ittnerite and Helvin are referred to the 
b n (J. f. pr. C , Ixx, 834). [This relation of Helvin is 
1e Mice, rs 194 and Suppl Hi and the similar ratio of 1;1 Ngee 
ases ani silica in’ these species rnet; and the accessory oe ee ~ the 
the ¢ and su “oe ogg ag in the sodalite ssvlan, is also remarked upon in the chapter on 
‘lassification of Mine rals, yol. i, p. 244) 
Gorn. —~Native gold has been found on Clarke’s fork of the Columbia river, a few 
miles above Fort Colville. 
Gtaver —Oce ith Hayesine in cavities in the Gypsum 
of Nova Scotia a bg eat rs 7d. ei v, 230. Analysis afforded, Sulphate of 
toda 4454, water 56°46, 
Harcenrre + {p. 413). oe. states (Min. 2g p- 186) that Joachimsthal was 
filial 
gis. 
ese 
Probably the original locality of the Haidingerit 
