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290 SILICATES. It has also been obtained by fusing in a crucible lime and silica in the required proportions. In the Phil. Mag. for Sept. 1831, Mr. Brooke has given the form and angles of a mineral from Vesuvius which he received as wollastonite. This particular specimen has not been ana lyzed, but it resembles others received in this country under the same name. The fragment figured by W. Phiilips as tabular spar was taken from a specimen stated on its ticket to be from Vermont, U. S. The supposed tabular spar is in large grains, and is accompanied by small grains of coccolite ; but we do not find any notice in the American works on Mineralogy of such an association of minerals having been found in Vermont. 161. AUGrlTE.—Augite, Pyroxene; Phillips. Pyroxene; Hauy. Paratomer Augit-Spath; Mohs. Diopsid, Amianth, Malacolith, Augit; Hausmann. Augit; Haidinger. v ^ C iu i Oblique. 101,100=49° 50'; 101,001=24° 19'-8 ; 111,010=66° 4l'’7. a ioo, b oio, c ooi, e oil, z 021, x 041, p 101, 101, n 102, ■ 2 111, 0 221, K ya 49° 50' ca 73 59 net 89 20 pa 106 24 qa 144 28 xb 23 42 zb 41 17 eb 60 20 cb 90 0 ib 17 35 pb 25 25 no. 311. / 310, 9 210, U 111, d 131 mb 43° 33' 9 b 62 15 fl 70 40 ab 90 0 \b 44 4 oh 47 45 sb 60 16 db 36 28 lib 65 42 v b 55 36 <pb 37 49 Eia. 312. 110, fi 120, i 130, 221, f 483, <f> 162. Co ie‘ 5 24' uc 33 51 VC 49 64 me 79 3 cV 103 26 CO 114 28 cs 137 49 mm 87 6 00' 95 30 ss' 120 31 zz' 82 33 FIG. 313.
