coloured, or any other. Sometimes quartz, schist, or marble is of this quality also, if much native or rudis silver adheres to it. But that ore is considered of poor quality if three librae of silver at the utmost are found in each one hundred librae of it[1]. Silver ore usually contains a greater quantity
- ↑ Three librae of silver per centumpondium would be equal to 875 ounces per short ton.
| Cadmia fossilis | Calmei; lapis calaminaris | Calamine | Calamine |
| Cadmia metallica | Kobelt | Part cobalt | *Cadmia metallica |
| Cadmia fornacis | Mitlere und obere offenbrüche | Furnace accretions or furnace calamine | Furnace accretions |
| Bituminosa cadmia | Kobelt des bergwachl | (Mansfeld copper schists) | Bituminosa cadmia (see note 4, p. 273) |
| Galena inanis | Blende | Sphalerite* (ZuS) | *Blende |
| Cobaltum cineraceum | Smallite* | Cadmia metallica (CoAs2) | |
| Cobaltum nigrum | Abolite* | ||
| Cobaltum ferri colore | Cobaltite (CoAsA) | ||
| Zincum | Zinck | Zinc | Zinc |
| Liquor Candidus ex fornace... etc | Conterfei | Zinc | See note 48, p. 408 |
| Atramentum sutorium, candidum, polissimum reperitur Goselariae | Goslarite (ZnSO4) | *Native white vitriol | |
| Spodos subtenanea cinerea | Geeler zechen rauch | Either natural or artificial zinc oxides, no doubt containing arsenical oxides | Grey spodos |
| Spodos subtenanea nigra | Schwartzer zechen rauch, auff dem, Altenberge nennet man in kis | Black spodos | |
| Spodos subtenanea viridis | Grauer zechen rauch | Green spodos | |
| Pompholyx | Hüttenrauch | Pompholyx (see note 26, p. 394) |
As seen from the following quotations from Agricola, on cadmia and cobalt, there was infinite confusion as to the zinc, cobalt, and arsenic minerals; nor do we think any good purpose is served by adding to the already lengthy discussion of these passages, the obscurity of which is natural to the state of knowledge; but we reproduce them as giving a fairly clear idea of the amount of confusion then existing. It is, however, desirable to bear in mind that the mines familiar to Agricola abounded in complex mixtures of cobalt, nickel, arsenic, bismuth, zinc, and antimony. Agricola frequently mentions the garlic odour from cadmia metallica, which, together with the corrosive qualities mentioned below, would obviously be due to arsenic. Bermannus (p. 459). “This kind of pyrites miners call cobaltum, if it be allowed to me to use our German name. The Greeks call it cadmia. The juices, however, out of which pyrites and silver are formed, appear to solidify into one body, and thus is produced what they call cobaltum. There are some who consider this the same as pyrites, because it is almost the same. There are some who distinguish it as a species, which pleases me, for it has the distinctive property of being extremely corrosive, so that it consumes the hands and feet of the workmen, unless they are well protected, which I do not believe that pyrites can do. Three kinds are found, and distinguished more by the colour than by other properties; they are black (abolite?), grey (smallite?), and iron colour (cobalt glance?). Moreover, it contains more silver than does pyrites...” Bermannus (p. 431). “It (a sort of pyrites) is so like the colour of galena that not without cause might anybody have doubt in deciding whether it be pyrites or galena Perhaps this kind is neither pyrites nor galena, but has a genus of its own. For it has not the colour of pyrites, nor the hardness. It is almost the colour of galena, but of entirely different components. From it there is made gold and silver, and a great quantity is dug out from Reichenstein which is in Silesia, as was lately reported to me. Much more is found at Raurici, which they call zincum; which species differs from pyrites, for the latter contains more silver than gold, the former only gold, or hardly any silver.”
(De Natura Fossilium, p. 170). “Cadmia fossilis has an odour like garlic”.. (p. 367). We now proceed with cadmia, not the cadmia fornacis (furnace accretions) of which I spoke in the last book, nor the cadmia fossilis (calamine) devoid of metal, which is used to colour copper, whose nature I explained in Book V, but the metallic mineral (fossilis metallica), which Pliny states to be an ore from which copper is made. The Ancients have left no record that another metal could be smelted from it. Yet it is a fact
