CAL CITES’ OF NEW YORK oI 
SUMMARY OF MEASURED AND CALCULATED ANGLES (conttuued) 
LETTER SYMBOL TYPE ANGLE Ne: Le MEASURED | CALCULATED 
READINGS 
° , ° c 
U: 5491 | I 5491 : BOT 7 66 464 | 66 422 
I 5491 : 9451 10 mm Sh Be in 
IV 5491 : 9451 1 a OR | 6 in 
I 5491 : 4591 [ese 16-29. 1G. 80 
ale Wn 0231 :8.14.29.3| 6 7 |) Be ar 
[PEL | Sele 3) 148.223 | 2 As OR OR ae 
q 2461 | IL 2461 : 2641 3 Sm | eo i 
Il 2461 : 6421 5 a7 Bl VY By. BO 
IV 2461 : 6421 1 27 98 | Sr gO 
V 2461 : 6421 3 a7 OG | Sy a, 20 
II 2461 : 426T 9 30 49 | 3) so 
IV 2461 : 4261 2 20 dik | aD a0 
Vv 4261 : 2131 1 md I Sl | 
# | 2670 1 i |) 2.6 TO eG Za 4 46 29 | 46 30 
| tat | 4.6410. orga 2 2 | Oy 0 
WU (14.12.36.5) IIT |14.12.96.5:14.26.13.5| 2 a | GS) 
IIT |14.12.26.5:26.12.14.5) 4 53 384 | 53 34 
IID |14.12.56.5:12.14.36.5) 5 98 Gli 93 ae 
IV |14.12.96.5:12.14.20.5, 1 95 48 | 25 46 
Ge | Go| Ae) ez eim at sibs 1 sai ge 2 
Vv | 8.4 1s eau 1 DA lp | OR OF 
W | 6.418.113 2iem 1 1 B70 | 1B. BO 
c EO 3472 : 3742 2 65 03a) 65 12k 
Vv 3472 : 4372 2 a G3 dip | Ae. 
ARNOLD HILL, CLINTON CO 
Plate 13, figures 1-4 
A few specimens of crystallized calcite were obtained from the Arnold 
Hill mines. At this locality the calcite occurs in veins traversing 
the syenitic gneiss which constitutes the country rock and is commonly 
associated with pyrite in small crystals and with red jasper, which latter 
mineral marks an earlier stage of vein deposition. Small brilliant scales 
