ALUMINA. 
325 
Colophonite —Silica 37.00, alumina 13.50, lime 29.00, oxide of iron 7.50, oxide of 
manganese 4.80, magnesia 6.50, water 1.00 (Simon). 
Allochroite —Silica 35.00, alumina 8.00, lime 30.00, oxide of iron 17.00, oxide of man¬ 
ganese 3.50 ( Vauquelin). 
Pyrope —Silica 40.00, alumina 28.50, lime 3.50, oxide of iron 16.50, oxide of manga¬ 
nese 0.3, magnesia 10.00, chromic acid 2.60 (Klaproth). 
Topazolite —Silica 37.00, alumina 2.00, lime 29.00, glucina 4.00, oxide of iron 25.00, 
oxide of manganese 2.00 (Bonvoisin). 
Essonite or Cinnamon Stone —Silica 38.80, alumina 21.26, lime 31.25, oxide of iron 
6.50 (Klaproth). 
Geological Situation. Garnet, in all its varieties, is most commonly found in primary 
rocks. Those which, in this State, afford the best specimens, are gneiss and mica slate, the 
latter of which is often thickly studded with the dodecahedral crystals. It is sometimes found 
in white limestone, but I am not aware that any of the varieties have been here observed in 
the transition rocks. 
LOCALITIES. 
Dutchess County. Near the Foss ore bed in the town of Dover, crystallized garnet occurs 
abundantly in mica slate. The colours are red and dark brown, and sometimes the crystals are 
translucent. They are usually 
small, very seldom exceeding 
the size of a pea, and occasion¬ 
ally associated with staurolite. 
The forms are the primary 
(Fig. 270); the primary with 
the edges replaced by tangent 
planes, emargine of Haiiy, Fig. 
271, P on n or n' 150° 0 / , n on 
n or n' on h' 131° 48 / 36", n on 
Fig. 273. 
Fig. 272. 
Fig. 271. 
n' 146° 26' 33"; the same with six of the sides extended, giving it the appearance of a six- 
sided prism, and with two other sides assuming a hexagonal outline, Fig. 272 ; also Fig. 273, 
in which six of the primary planes are extended, and all the edges are replaced by tangent 
planes. 
At Stone church, in the same town, is another similar locality of garnet in a light coloured 
mica-slate. The crystals are in great abundance, and are similar in form to those observed 
at the Foss ore bed. 
Essex County. In the town of Willsborough, nine miles northwest of the village of Essex, 
there is a detached mountain mass, which extends from east to west; and on its northern face, 
near the base, is a bed of the variety colophonite in gneiss. The bed is from two to five feet 
in width, and the mineral is made up of large grains of red, yellow and deep brown colours, 
which have a high resinous lustre, and are frequently irised; the single grains are highly 
translucent, and have a cleavage. Specific gravity 3.896. It is associated with the massive 
