Agricola, Georgius
,
De re metallica
,
1912/1950
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which the tin itself is made, and a material they dig up resembling litharge;
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of iron, iron rust. </
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<
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>Gold and copper are equally indicated by chrysocolla and
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azure; silver and lead, by the lead. </
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<
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>But, though miners rightly
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call bismuth “the roof of silver,” and though copper pyrites is the common
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parent of vitriol and
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melantería,
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still these sometimes have their own
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peculiar minerals, just as have orpiment and
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stibium.
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<
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>Now, just as certain vein materials give miners a favourable indication,
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so also do the rocks through which the
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canales
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of the veins wind their
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way, for sand discovered in a mine is reckoned among the good indications,
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especially if it is very fine. </
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<
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>In the same way schist, when it is of a
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bluish or blackish colour, and also limestone, of whatever colour it may be, is
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a good sign for a silver vein. </
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<
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>There is a rock of another kind that is a good sign;
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in it are scattered tiny black stones from which tin is smelted; especially when
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the whole space between the veins is composed of this kind of rock.
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</
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<
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>Very often indeed, this good kind of rock in conjunction with valuable
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stringers contains within its folds the
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canales
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of mineral bearing veins: if
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it descends vertically into the earth, the benefit belongs to that mine in
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which it is seen first of all; if inclined, it benefits the other neighbouring
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mines
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12
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. </
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<
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>As a result the miner who is not ignorant of geometry can calculate
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from the other mines the depth at which the
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canales
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of a vein bearing rich
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metal will wind its way through the rock into his mine. </
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<
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>So much for these
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matters.</
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<
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>I now come to the mode of working, which is varied and complex, for in
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some places they dig crumbling ore, in others hard ore, in others a harder
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ore, and in others the hardest kind of ore. </
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<
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>In the same way, in some places
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the hangingwall rock is soft and fragile, in others hard, in others harder, and
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in still others of the hardest sort. </
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<
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>I call that ore “crumbling” which is com
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posed of earth, and of soft solidified juices; that ore “hard” which is composed
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of metallic minerals and moderately hard stones, such as for the most part
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are those which easily melt in a fire of the first and second orders, like lead
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and similar materials. </
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<
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>I call that ore “harder” when with those I have already
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mentioned are combined various sorts of quartz, or stones which easily melt
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in fire of the third degree, or pyrites, or
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cadmia,
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or very hard marble. </
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<
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>I call
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that ore hardest, which is composed throughout the whole vein of these hard
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stones and compounds. </
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>
<
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>The hanging or footwalls of a vein are hard, when
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composed of rock in which there are few stringers or seams; harder, in
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which they are fewer; hardest, in which they are fewest or none at all.
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</
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<
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>When these are absent, the rock is quite devoid of water which softens
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it. </
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>
<
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>But the hardest rock of the hanging or footwall, however, is seldom as
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hard as the harder class of ore.</
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</
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<
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<
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>Miners dig out crumbling ore with the pick alone. </
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>
<
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>When the metal
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has not yet shown itself, they do not discriminate between the hangingwall
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and the veins; when it has once been found, they work with the utmost care.
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</
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<
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>For first of all they tear away the hangingwall rock separately from the vein,
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afterward with a pick they dislodge the crumbling vein from the footwall </
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>
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</
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</
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>
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