178 NATURAL HISTORY. [NORTH 
and Saxony.— Fluoride of calcium, yttrium, and cerium;—yttrocerite; 
and some related minerals from Finbo and Brodbo near Fahlun in Swe¬ 
den.— Fluoride of sodium and aluminum, called cryolite, found in West 
Greenland: pure and mixed with brown iron stone, Gelena, &c. 
Case 59 contains the chlorides.—Chloride of sodium ( muriate of soda), 
or rock salt: the most interesting specimens here deposited of this im¬ 
portant mineral substance are the crystallized varieties; the massive and 
fibrous coloured varieties, the red chiefly from Hallein in Tyrol, the 
blue and violet from Ischel in Upper Austria; the stalactical rock salt from 
Mexico, &c— Chloride of ammonium or sal-ammoniac, from Vesuvius, I 
Saint Etienne en Forez, &c. — Chlorides of lead: to these belong, the I 
cotunnite from Vesuvius; the basic muriate of lead from Mendip ; and 
the murio-carbonate of lead from Derbyshire, of which most rare sub¬ 
stance very perfect specimens are deposited in this glass Case.—Chlo¬ 
ride of copper or atacamite, in crystallized splendid groups, chiefly from 
Remolinos, Soli dad and Veta negra della Pampa larga, in Chili; what 
was originally termed Peruvian green sand, or atacamite (being obtained 
from the desert of Atacama between Chili and Peru) is now known to 
be artificially produced by pounding the crystallized and laminar va¬ 
rieties for the purpose of using the sand (arenilla) in lieu of blotting 
paper. — Chloride of silver, called also horn-silver and corneous silver: 
amorphous, botryoidal, in laminae, and crystallized in minute cubes and 
octahedrons, from Veta Negra in Chili, the Saxon Erzgebirge, &c_ 
Chloride of mercury, or horn-quicksilver , with native mercury from 
Moschel-Landsberg, Almaden, &c. 
Case 60 contains a small collection of organieo-chemical, or such 
mineralized substances as are composed after the manner of organic 
bodies, from which they derive their origin. They are divided into salts, 
resins, bitumen, and coal. To the salts belong—the mellate of alumina, 
also called mellite or honey-stone, found in the beds of brown coal at 
Artern in Thuringia; and the oxalate of iron, formerly known by the name 
of resinous iron, but to which that of humboldtite is now generally ap¬ 
plied—To the resins may be referred—the amber, of the* varieties of 
which a considerable suite is deposited, many of them enclosing insects, 
&c. ; to which, for the sake of comparison, are added, specimens of re¬ 
cent copal, likewise containing insects fossil copal or Highgate resin; 
— retinite or retinasphalt, found at Bovey; together with some other re¬ 
lated resinous substances;—the idrialite, to which the bituminous cin¬ 
nabar or brand-ertz is partly referable. To the bitumina belong the 
varieties of mineral pitch of all degrees of consistence, from the fluid 
naphtha and mineral oil or petroleum, to the solid and hard asphalt and 
jet ox pitch coal; the elaterite or elastic bitumen of Derbyshire, (a suite 
of specimens exhibiting all degrees of solidity, from that of honey to 
that of a compact ligneous substance). With these is also placed the 
dapeche, an inflammable fossil substance found by Humboldt in South 
America, having several properties of the common caoutchouc or Indian 
rubber ;—the liatchettine, a bituminous substance from Merthyr Tydvil 
in South Wales, the scheererite, &c.—Coal: black coal, and brown coal 
—of these a few specimens only are deposited, their different varieties 
being rather objects for a geological collection. 
