49 
in large flat octoliedral crystals from Norway, with 
epidote, &c. also the variety called, by Sanssiire, 
rayoniiante en gouttiere, from St. Gothard, on feld¬ 
spar, with chlorite, &c.— 2\tan'shorl^ also called 
rutile; massive, crystallized, and fibrous, to which 
latter belongs the variety with golden tarnish, from 
Moutier, near the Montblanc; the acicular crsytals 
of rutile in rock crystal, &c.; the ferrlftrous ox¬ 
ides (siderotitanium of Klaproth), some varieties 
of which may be considered as titaniferous oxides 
of iron, and to which may be referred the black sand- 
called menachanite^ and the iserine, in loose grains 
and imbedded;—specimens of anatase, or octohe- 
drite, from Dauphine;—the scarce substance called 
craitonite {crichto?iite), by the Comte de Bournon, 
likewise from Dauphind, in very acute octohedral 
crystals, and in thin lamince. 
The remainder of this table case contains the 
ores of antimony: native antimomj, hom Ailemont, 
and from Sala in Sweden, some varieties of which 
are arseniferous;— sidphuret of antimony, or grey 
antimony (the most common ore of this metal), oc¬ 
curs compact, foliated, radiated, and plumose: the 
more remarkable among these are the specimens of 
crystallized radiated antimony in fine groups, espe¬ 
cially from Transylvania; radiated grey antimony 
with barytes, realgar, &c.; the plumose grey anti¬ 
mony, some varieties of which, appearing like deli¬ 
cate wool or down, display a fine iridescent blue, 
E yellow'. 
SALOON. 
Nat. Hist, 
