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Amalgamation Machinery used in Freiberg
Section of the Amalgamation Works at Freiberg
Apparatus used for Distilling the Amalgam in Freiberg
Arany-Idka

Stamps for Crushing Ores (Molinos) in Mexico
Grinding Mills (Arrastras) in Mexico.

Apparatus for the Extraction of Silver used in Freiberg 102-105 Double Roasting Furnace used at Mansfeld

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Apparatus for Extracting Silver with Warm Water

ZINC.

Cupola Furnace having a Fire-grate used in Spain for
Calcination .

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Double Muffle Furnace for Calcination used in Przibram 417-419
Belgian Furnaces for Distillation

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Retort and Adapters used on the Continent

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Furnace for Burning Muffles used at Llansamlet, near
Swansea

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125-129 Belgian-Silesian Distillation Furnace

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Adapter used at Valentin Cocq

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Muffle and Adapter used at Borbeck

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Muffle Furnace with Two Rows of Muffles one above the
other used at Birkengang near Stolberg
Crucible Furnace used at Neath

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Pots for Re-melting Zinc used at Llansamlet near
Swansea

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Reverberatory Furnace for Re-melting Zinc used in

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Silesia

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TIN.

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Roasting Furnaces with Condensers, as used in Saxony
Brunton's Calciner

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Tin Smelting Furnace at Truro, in Cornwall.

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Apparatus for Liquating Antimony used at Wolfsberg
Furnace for Liquating Antimony used at Malbosc (France)
Reverberatory Furnace for Smelting Roasted Antimonial
Ores in France

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Distilling the Amalgam

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Section in the Clunes Gold Mining Field (Australia)
of a portion of the Ballarat Gold Field (Australia)
from the Boroondara and Balleen Gold Mines
(Australia)

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Gold Mills, used at Schemnitz.

Apparatus for Pressing the Auriferous Mercury

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Extracting Gold used at Reichenstein

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Extracting Gold used at Schemnitz

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Refining Gold used at the Lower Hartz

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Pressing the Silver used at the Lower Hartz

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PLATINUM.

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A PRACTICAL

TREATISE ON METALLURGY.

CHAPTER I.

LEAD.

PRINCIPAL ORES OF LEAD.

IN these ores the lead is contained in the form of sulphide or oxide. The principal ores are the following:

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1. Galena (sulphide of lead), PbS, containing 86.57 per cent Pb, and 13°43 per cent S. It usually contains sulphide of silver in an isomorphous state. The amount of silver varies, in most cases, between o'oï and o‘30 per cent, sometimes rising to o'50, or even I per cent. In the latter case, however, silver does not occur as isomorphous sulphide of silver, but as silver ore disseminated through the galena. Upon treating galena by reagents, it may frequently.be ascertained in what state of combination the silver exists in the ore. Malaguti and Durocher* found silver in galena, from mere traces up to more than 7 per cent. The amount of silver varies not only in different deposits of the same locality, but sometimes even in the same bed, and is found to bear no relation whatever to the structure of the ore.

* MALAGUTI and DUROCHER, in Annales des Mines, 4 ser., tom. xvii., 1805; FABRE, in Bulletin de la Société de l'Industrie Minérale, tom. iii., p. 281, 1857-1858. Berg. u. hüttenm. Ztg., 1859, p. 446, 447.

B

It appears that the period of the formation of the ore has had an essential influence upon the amount of silver contained in it; galena in veins usually possesses a greater amount than galena in beds, or when diffused through other ores. Moreover, the purest galena contains the least silver. The prevailing opinion that lamellar galena contains more silver than granular galena, and that in the latter the silver occurs as mechanically included sulphide, is not always correct. Ores containing a small amount of lead, sometimes owe their entire value to the other metals, silver, gold, and copper, which they accidentally contain. Galena is found in almost all countries, and in nearly all geological formations.* It occurs :

A. In CRYSTALLINE SLATES and UNSTRATIFIED ROCKS. a. In veins. In gneiss (Black Forest, Odenwald, Saxon Erzgebirge, Oberpfalz, Silesian Sudeten, Riesengebirge, Bleistadt in Bohemia, Central France, Kongsberg); in mica schist (Bleistadt in Bohemia, Spain, Kongsberg, Sardinia, Tuscany); in granite (Badenweiler, Sohneeberg, Linares in Spain, Wicklow in Ireland, Central France); in quartz slate (Kongsberg); in granular limestone (Schwarzenberg in Erzgebirge); in magnesian slate (Sardinia); in porphyry (Central France, i.e., Pontgibaud); in trachytic porphyry (Felsobanya, Kapnik); in greenstone (Schemnitz); in greywacke, quartz, and greenstone (Przibram).

b. In beds. In mica schist (Tuscany, Fahlun).

c. In floors. In mica schist and granular limestone (Ruszkitza in Banat); in mica schist, granular limestone, and syenite (Dognaska, in Banat); in granite (Christiania); in syenite (Christiania); in mica schist (Tuscany).

d. Impregnated, in granular limestone (Sala). B. In CAMBRIAN CLAY SLATE.

&c., in Wales).

C. In SILURIAN SLATES.

In veins (Cardiganshire,

a. In veins. In clay slate (Harzgerode on the Hartz, Mies in Bohemia, Carthagena in Spain).

Ann. d. Min., 4 ser., xvii., 83. Ueber das Vorkommen der Bleierze, see v. DECHEN, Statistik des nördl, and zollv. Deutschland, i., 750. COTTA, Lehre von den Erzlagerstätten, 1860, ii., 570 and 618.

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