Enc pay o eee a 
C. U. Shepard on Meteoric Iron in South Africa. 213 
Ww eobtire, see peyote: 
(tin, Not., No. 1‘ rity rane prisms, affording a planes, @, a-a, 
i % O04 E738 - 
O, or # Ie iigee: J, it, mi, m’%, ==98° 80’, O:: mi=1464°, O: a wee pte 
proxim: ==5°828, e form is near that of Bournonite, but the composition 
pens . “a different. adie sis by Schrotter, recaleulated by Kenngott. 
Sb Cu Pb Fe 
28° ma 6 of 16 65 17°35 29°98 1:35==99°79 
corresponding to 17°83 sulphur, 0°8 As?, 1:3 Sb%, 2°7 Su, 2°9 Pb, 0-5 Fe, or 178 S, 
21 As?-++Sb?, 6:1 €u+-Pb-+Fe. Kenngot takes the ratio as at “% 1 (As?, Sb?,) 
:8(€u, Fe, Pb). It is more nearly 9:1:3; but the mineral requires a new investi- 
ce ae 
am [p. 851],—The — Suppl. [, p. 18 (this Jour., vol, xix, p. 370) is 
by P Petzold 1 in a notice by Schn 
Wottastonirz |p. 1 561—Anaiss of Wollastonite from the Morne Mts., by Mr. 
F, Heddle (Phil. Mag., te ix, 452): 
i Ca Mg H 6 
1, 51°36 0-98 42°50 048 148 undet. 
2. 50°43 0°84 43°92 0:40 1°36 2:37 99°82 
The mineral contains a little mixed carbonate of lime. 
Wourenrre [(p. 849]. —-Analysis and crystal of Wulfenite from Phcenixville, Pa., 
J. L, Smith, xx, 245, 
aren (p- 401]—T'win of Xenotime with Malacone, Zschau, Am. J. Sci., xx, 
ZAMTITE, .A. Casares pF in a sed to be a hydrous hae of nickel, but n 
bit t analyzed. sheng ee e emerald nickel, and is from Spain. Color dull oe 
Not 
Ww r , 
soda a a ane borax affords a metallic globule of a dull yellow perry which j is 
magnetic and has the pr Spates. of nickel. In a tube yields water, Kenngott’s 
Min. Forsch, for 1853, p. ri [See Min., piste 0] 
Zeuxrrz [p. 270].—See e. 
PS acearak Gl A ni Zino oe {p. 110].—Isomorphism with Greenockite, Kenngott, 
een 
Art. XXV.—On a new locality of Meteoric pst in the Cramps 
River Country, South Africa, and a ed new 
of the same, in Mexico; by CuarLes foe Sueparp, M. D. 
it Was purchased ; and a few days subse ily Ww, 
to my possession this being the second large metallic meteorite 
from Africa, which I owe to the same source, 
Its weight is 328 pounds. Its figure in one position, as shown 
by the drawing of Mr. Robert Bakewell here given, is somewhat 
cubical or block-like, though exhibiting very blunt edge S, and 
Upon one side, a very remarkable gash, or reéntering an; 
