26 
SALOON. 
Nat. Hist. 
(called grenatite in Switzerland) : besides seve¬ 
ral varieties of the cruciform and other crystals 
from Britany, we have modifications of the simple 
crystals in mica-slate from St. Gothard, accom¬ 
panied by prisms of kyanite perfectly similar to 
those of the staurolite, and sometimes longitu¬ 
dinally grown together with them. 
Case 14. The contents of this table-case 
are ;— chrysolite and olivine (peridot of Haiiy), 
the former crystallized, and in cut and polished 
pieces ; the latter as grains, in basaltic rocks and 
separate : to which is added some of the olivine¬ 
like substance found in the cells of the Siberian 
meteoric iron (Case 49). —The substances which 
have been described under the names of thallite, 
arendalite5akantikone5delphinite3&c.are Haiiy’s 
epidote, and Yferner’s pistacite : of which several 
specimens are deposited in this case. Among 
these is also the violet manganesiferous epidote^ 
referred by some to the ores of manganese.— 
Zuisite.—Axinite^ variously crystallized, from 
Danphinej&c.—The pyroxene tribe, comprising 
the aiigite^ in separate crystals and imbedded in 
Vesuvian lava, together with groups of well de¬ 
fined crystals from Arendahl in Norway, where 
this substance occurs in primitive rocks, and the 
granular augite or coccolite ; the varieties of diop- 
side (now pyroxene) called alalite and miissite ; 
the saliteov malacolite, a species perfectly distinct 
from the common augite or pyroxene ; the fu¬ 
sible augite called euchysiderite, — Jejfersonite^ 
a mineral from New York, related to pyroxene. 
The 
