De Re Metallica, Translated from the First Latin Edition of 1556 by Georg Agricola
BOOK XII.
21652 words | Chapter 29
Previously I have dealt with the methods of separating silver from
copper. There now remains the portion which treats of solidified juices;
and whereas they might be considered as alien to things metallic,
nevertheless, the reasons why they should not be separated from it I
have explained in the second book.
Solidified juices are either prepared from waters in which nature or art
has infused them, or they are produced from the liquid juices
themselves, or from stony minerals. Sagacious people, at first observing
the waters of some lakes to be naturally full of juices which thickened
on being dried up by the heat of the sun and thus became solidified
juices, drew such waters into other places, or diverted them into
low-lying places adjoining hills, so that the heat of the sun should
likewise cause them to condense. Subsequently, because they observed
that in this wise the solidified juices could be made only in summer,
and then not in all countries, but only in hot and temperate regions in
which it seldom rains in summer, they boiled them in vessels over a fire
until they began to thicken. In this manner, at all times of the year,
in all regions, even the coldest, solidified juices could be obtained
from solutions of such juices, whether made by nature or by art.
Afterward, when they saw juices drip from some roasted stones, they
cooked these in pots in order to obtain solidified juices in this wise
also. It is worth the trouble to learn the proportions and the methods
by which these are made.
I will therefore begin with salt, which is made from water either salty
by nature, or by the labour of man, or else from a solution of salt, or
from lye, likewise salty. Water which is salty by nature, is condensed
and converted into salt in salt-pits by the heat of the sun, or else by
the heat of a fire in pans or pots or trenches. That which is made salty
by art, is also condensed by fire and changed into salt. There should be
as many salt-pits dug as the circumstance of the place permits, but
there should not be more made than can be used, although we ought to
make as much salt as we can sell. The depth of salt-pits should be
moderate, and the bottom should be level, so that all the water is
evaporated from the salt by the heat of the sun. The salt-pits should
first be encrusted with salt, so that they may not suck up the water.
The method of pouring or leading sea-water into salt-pits is very old,
and is still in use in many places. The method is not less old, but less
common, to pour well-water into salt-pits, as was done in Babylon, for
which Pliny is the authority, and in Cappadocia, where they used not
only well-water, but also spring-water. In all hot countries salt-water
and lake-water are conducted, poured or carried into salt-pits, and,
being dried by the heat of the sun, are converted into salt.[1] While
the salt-water contained in the salt-pits is being heated by the sun, if
they be flooded with great and frequent showers of rain the evaporation
is hindered. If this happens rarely, the salt acquires a disagreeable[2]
flavour, and in this case the salt-pits have to be filled with other
sweet water.
[Illustration 547 (Salt Pans): A--Sea. B--Pool. C--Gate. D--Trenches.
E--Salt basins. F--Rake. G--Shovel.]
Salt from sea-water is made in the following manner. Near that part of
the seashore where there is a quiet pool, and there are wide, level
plains which the inundations of the sea do not overflow, three, four,
five, or six trenches are dug six feet wide, twelve feet deep, and six
hundred feet long, or longer if the level place extends for a longer
distance; they are two hundred feet distant from one another; between
these are three transverse trenches. Then are dug the principal pits, so
that when the water has been raised from the pool it can flow into the
trenches, and from thence into the salt-pits, of which there are numbers
on the level ground between the trenches. The salt-pits are basins dug
to a moderate depth; these are banked round with the earth which was dug
in sinking them or in cleansing them, so that between the basins, earth
walls are made a foot high, which retain the water let into them. The
trenches have openings, through which the first basins receive the
water; these basins also have openings, through which the water flows
again from one into the other. There should be a slight fall, so that
the water may flow from one basin into the other, and can thus be
replenished. All these things having been done rightly and in order, the
gate is raised that opens the mouth of the pool which contains sea-water
mixed with rain-water or river-water; and thus all of the trenches are
filled. Then the gates of the first basins are opened, and thus the
remaining basins are filled with the water from the first; when this
salt-water condenses, all these basins are incrusted, and thus made
clean from earthy matter. Then again the first basins are filled up from
the nearest trench with the same kind of water, and left until much of
the thin liquid is converted into vapour by the heat of the sun and
dissipated, and the remainder is considerably thickened. Then their
gates being opened, the water passes into the second basins; and when it
has remained there for a certain space of time the gates are opened, so
that it flows into the third basins, where it is all condensed into
salt. After the salt has been taken out, the basins are filled again and
again with sea-water. The salt is raked up with wooden rakes and thrown
out with shovels.
[Illustration 549 (Salt Wells): A--Shed. B--Painted signs. C--First
room. D--Middle room. E--Third room. F--Two little windows in the end
wall. G--Third little window in the roof. H--Well. I--Well of another
kind. K--Cask. L--Pole. M--Forked sticks in which the porters rest the
pole when they are tired.]
Salt-water is also boiled in pans, placed in sheds near the wells from
which it is drawn. Each shed is usually named from some animal or other
thing which is pictured on a tablet nailed to it. The walls of these
sheds are made either from baked earth or from wicker work covered with
thick mud, although some may be made of stones or bricks. When of
brick they are often sixteen feet high, and if the roof rises
twenty-four feet high, then the walls which are at the ends must be made
forty feet high, as likewise the interior partition walls. The roof
consists of large shingles four feet long, one foot wide, and two digits
thick; these are fixed on long narrow planks placed on the rafters,
which are joined at the upper end and slope in opposite directions. The
whole of the under side is plastered one digit thick with straw mixed
with lute; likewise the roof on the outside is plastered one and a half
feet thick with straw mixed with lute, in order that the shed should not
run any risk of fire, and that it should be proof against rain, and be
able to retain the heat necessary for drying the lumps of salt. Each
shed is divided into three parts, in the first of which the firewood and
straw are placed; in the middle room, separated from the first room by a
partition, is the fireplace on which is placed the caldron. To the right
of the caldron is a tub, into which is emptied the brine brought into
the shed by the porters; to the left is a bench, on which there is room
to lay thirty pieces of salt. In the third room, which is in the back
part of the house, there is made a pile of clay or ashes eight feet
higher than the floor, being the same height as the bench. The master
and his assistants, when they carry away the lumps of salt from the
caldrons, go from the former to the latter. They ascend from the right
side of the caldron, not by steps, but by a slope of earth. At the top
of the end wall are two small windows, and a third is in the roof,
through which the smoke escapes. This smoke, emitted from both the back
and the front of the furnace, finds outlet through a hood through which
it makes its way up to the windows; this hood consists of boards
projecting one beyond the other, which are supported by two small beams
of the roof. Opposite the fireplace the middle partition has an open
door eight feet high and four feet wide, through which there is a gentle
draught which drives the smoke into the last room; the front wall also
has a door of the same height and width. Both of these doors are large
enough to permit the firewood or straw or the brine to be carried in,
and the lumps of salt to be carried out; these doors must be closed when
the wind blows, so that the boiling will not be hindered. Indeed, glass
panes which exclude the wind but transmit the light, should be inserted
in the windows in the walls.
They construct the greater part of the fireplace of rock-salt and of
clay mixed with salt and moistened with brine, for such walls are
greatly hardened by the fire. These fireplaces are made eight and a half
feet long, seven and three quarters feet wide, and, if wood is burned in
them, nearly four feet high; but if straw is burned in them, they are
six feet high. An iron rod, about four feet long, is engaged in a hole
in an iron foot, which stands on the base of the middle of the furnace
mouth. This mouth is three feet in width, and has a door which opens
inward; through it they throw in the straw.
[Illustration 551 (Salt Caldron): A--Fireplace. B--Mouth of fireplace.
C--Caldron. D--Posts sunk into the ground. E--Cross-beams. F--Shorter
bars. G--Iron hooks. H--Staples. I--Longer bars. K--Iron rod bent to
support the caldron.]
The caldrons are rectangular, eight feet long, seven feet wide, and half
a foot high, and are made of sheets of iron or lead, three feet long and
of the same width, all but two digits. These plates are not very thick,
so that the water is heated more quickly by the fire, and is boiled
away rapidly. The more salty the water is, the sooner it is condensed
into salt. To prevent the brine from leaking out at the points where the
metal plates are fastened with rivets, the caldrons are smeared over
with a cement made of ox-liver and ox-blood mixed with ashes. On each
side of the middle of the furnace two rectangular posts, three feet
long, and half a foot thick and wide are set into the ground, so that
they are distant from each other only one and a half feet. Each of them
rises one and a half feet above the caldron. After the caldron has been
placed on the walls of the furnace, two beams of the same width and
thickness as the posts, but four feet long, are laid on these posts, and
are mortised in so that they shall not fall. There rest transversely
upon these beams three bars, three feet long, three digits wide, and two
digits thick, distant from one another one foot. On each of these hang
three iron hooks, two beyond the beams and one in the middle; these are
a foot long, and are hooked at both ends, one hook turning to the right,
the other to the left. The bottom hook catches in the eye of a staple,
whose ends are fixed in the bottom of the caldron, and the eye projects
from it. There are besides, two longer bars six feet long, one palm
wide, and three digits thick, which pass under the front beam and rest
upon the rear beam. At the rear end of each of the bars there is an iron
hook two feet and three digits long, the lower end of which is bent so
as to support the caldron. The rear end of the caldron does not rest on
the two rear corners of the fireplace, but is distant from the fireplace
two thirds of a foot, so that the flame and smoke can escape; this rear
end of the fireplace is half a foot thick and half a foot higher than
the caldron. This is also the thickness and height of the wall between
the caldron and the third room of the shed, to which it is adjacent.
This back wall is made of clay and ashes, unlike the others which are
made of rock-salt. The caldron rests on the two front corners and sides
of the fireplace, and is cemented with ashes, so that the flames shall
not escape. If a dipperful of brine poured into the caldron should flow
into all the corners, the caldron is rightly set upon the fireplace.
The wooden dipper holds ten Roman _sextarii_, and the cask holds eight
dippers full[3]. The brine drawn up from the well is poured into such
casks and carried by porters, as I have said before, into the shed and
poured into a tub, and in those places where the brine is very strong it
is at once transferred with the dippers into the caldron. That brine
which is less strong is thrown into a small tub with a deep ladle, the
spoon and handle of which are hewn out of one piece of wood. In this tub
rock-salt is placed in order that the water should be made more salty,
and it is then run off through a launder which leads into the caldron.
From thirty-seven dippersful of brine the master or his deputy, at Halle
in Saxony,[4] makes two cone-shaped pieces of salt. Each master has a
helper, or in the place of a helper his wife assists him in his work,
and, in addition, a youth who throws wood or straw under the caldron.
He, on account of the great heat of the workshop, wears a straw cap on
his head and a breech cloth, being otherwise quite naked. As soon as the
master has poured the first dipperful of brine into the caldron the
youth sets fire to the wood and straw laid under it. If the firewood is
bundles of faggots or brushwood, the salt will be white, but if straw is
burned, then it is not infrequently blackish, for the sparks, which are
drawn up with the smoke into the hood, fall down again into the water
and colour it black.
[Illustration 553 (Salt Caldron): A--Wooden dipper. B--Cask. C--Tub.
D--Master. E--Youth. F--Wife. G--Wooden spade. H--Boards. I--Baskets.
K--Hoe. L--Rake. M--Straw. N--Bowl. O--Bucket containing the blood.
P--Tankard which contains beer.]
In order to accelerate the condensation of the brine, when the master
has poured in two casks and as many dippersful of brine, he adds about a
Roman _cyathus_ and a half of bullock's blood, or of calf's blood, or
buck's blood, or else he mixes it into the nineteenth dipperful of
brine, in order that it may be dissolved and distributed into all the
corners of the caldron; in other places the blood is dissolved in beer.
When the boiling water seems to be mixed with scum, he skims it with a
ladle; this scum, if he be working with rock-salt, he throws into the
opening in the furnace through which the smoke escapes, and it is dried
into rock-salt; if it be not from rock-salt, he pours it on to the floor
of the workshop. From the beginning to the boiling and skimming is the
work of half-an-hour; after this it boils down for another
quarter-of-an-hour, after which time it begins to condense into salt.
When it begins to thicken with the heat, he and his helper stir it
assiduously with a wooden spatula, and then he allows it to boil for an
hour. After this he pours in a _cyathus_ and a half of beer. In order
that the wind should not blow into the caldron, the helper covers the
front with a board seven and a half feet long and one foot high, and
covers each of the sides with boards three and three quarters feet long.
In order that the front board may hold more firmly, it is fitted into
the caldron itself, and the side-boards are fixed on the front board and
upon the transverse beam. Afterward, when the boards have been lifted
off, the helper places two baskets, two feet high and as many wide at
the top, and a palm wide at the bottom, on the transverse beams, and
into them the master throws the salt with a shovel, taking half-an-hour
to fill them. Then, replacing the boards on the caldron, he allows the
brine to boil for three quarters of an hour. Afterward the salt has
again to be removed with a shovel, and when the baskets are full, they
pile up the salt in heaps.
In different localities the salt is moulded into different shapes. In
the baskets the salt assumes the form of a cone; it is not moulded in
baskets alone, but also in moulds into which they throw the salt, which
are made in the likeness of many objects, as for instance tablets.
These tablets and cones are kept in the higher part of the third room of
the house, or else on the flat bench of the same height, in order that
they may dry better in the warm air. In the manner I have described, a
master and his helper continue one after the other, alternately boiling
the brine and moulding the salt, day and night, with the exception only
of the annual feast days. No caldron is able to stand the fire for more
than half a year. The master pours in water and washes it out every
week; when it is washed out he puts straw under it and pounds it; new
caldrons he washes three times in the first two weeks, and afterward
twice. In this manner the incrustations fall from the bottom; if they
are not cleared off, the salt would have to be made more slowly over a
fiercer fire, which requires more brine and burns the plates of the
caldron. If any cracks make their appearance in the caldron they are
filled up with cement. The salt made during the first two weeks is not
so good, being usually stained by the rust at the bottom where
incrustations have not yet adhered.
Although salt made in this manner is prepared only from the brine of
springs and wells, yet it is also possible to use this method in the
case of river-, lake-, and sea-water, and also of those waters which are
artificially salted. For in places where rock-salt is dug, the impure
and the broken pieces are thrown into fresh water, which, when boiled,
condenses into salt. Some, indeed, boil sea-salt in fresh water again,
and mould the salt into the little cones and other shapes.
[Illustration 554 (Salt Boiling): A--Pool. B--Pots. C--Ladle. D--Pans.
E--Tongs.]
Some people make salt by another method, from salt water which flows
from hot springs that issue boiling from the earth. They set earthenware
pots in a pool of the spring-water, and into them they pour water
scooped up with ladles from the hot spring until they are half full. The
perpetual heat of the waters of the pool evaporates the salt water just
as the heat of the fire does in the caldrons. As soon as it begins to
thicken, which happens when it has been reduced by boiling to a third or
more, they seize the pots with tongs and pour the contents into small
rectangular iron pans, which have also been placed in the pool. The
interior of these pans is usually three feet long, two feet wide, and
three digits deep, and they stand on four heavy legs, so that the water
flows freely all round, but not into them. Since the water flows
continuously from the pool through the little canals, and the spring
always provides a new and copious supply, always boiling hot, it
condenses the thickened water poured into the pans into salt; this is at
once taken out with shovels, and then the work begins all over again. If
the salty water contains other juices, as is usually the case with hot
springs, no salt should be made from them.
[Illustration 555 (Salt Boiling): A--Pots. B--Tripod. C--Deep ladle.]
Others boil salt water, and especially sea-water, in large iron pots;
this salt is blackish, for in most cases they burn straw under them.
Some people boil in these pots the brine in which fish is pickled. The
salt which they make tastes and smells of fish.
[Illustration 556 (Salt evaporated on faggots): A--Trench. B--Vat into
which the salt water flows. C--Ladle. D--Small bucket with pole fastened
into it.]
Those who make salt by pouring brine over firewood, lay the wood in
trenches which are twelve feet long, seven feet wide, and two and one
half feet deep, so that the water poured in should not flow out. These
trenches are constructed of rock-salt wherever it is to be had, in order
that they should not soak up the water, and so that the earth should not
fall in on the front, back and sides. As the charcoal is turned into
salt at the same time as the salt liquor, the Spaniards think, as
Pliny writes[5], that the wood itself turns into salt. Oak is the best
wood, as its pure ash yields salt; elsewhere hazel-wood is lauded. But
with whatever wood it be made, this salt is not greatly appreciated,
being black and not quite pure; on that account this method of
salt-making is disdained by the Germans and Spaniards.
[Illustration 557 (Lye Making): A--Large vat. B--Plug. C--Small tub.
D--Deep ladle. E--Small vat. F--Caldron.]
The solutions from which salt is made are prepared from salty earth or
from earth rich in salt and saltpetre. Lye is made from the ashes of
reeds and rushes. The solution obtained from salty earth by boiling,
makes salt only; from the other, of which I will speak more a little
later, salt and saltpetre are made; and from ashes is derived lye, from
which its own salt is obtained. The ashes, as well as the earth, should
first be put into a large vat; then fresh water should be poured over
the ashes or earth, and it should be stirred for about twelve hours with
a stick, so that it may dissolve the salt. Then the plug is pulled out
of the large vat; the solution of salt or the lye is drained into a
small tub and emptied with ladles into small vats; finally, such a
solution is transferred into iron or lead caldrons and boiled, until the
water having evaporated, the juices are condensed into salt. The above
are the various methods for making salt. (Illustration p. 557.)
[Illustration 559 (Nitrum-pits): A--Nile. B--Nitrum-pits, such as I
conjecture them to be.[7]]
_Nitrum_[6] is usually made from _nitrous_ waters, or from solutions or
from lye. In the same manner as sea-water or salt-water is poured into
salt-pits and evaporated by the heat of the sun and changed into salt,
so the _nitrous_ Nile is led into _nitrum_ pits and evaporated by the
heat of the sun and converted into _nitrum_. Just as the sea, in
flowing of its own will over the soil of this same Egypt, is changed
into salt, so also the Nile, when it overflows in the dog days, is
converted into _nitrum_ when it flows into the _nitrum_ pits. The
solution from which _nitrum_ is produced is obtained from fresh water
percolating through _nitrous_ earth, in the same manner as lye is made
from fresh water percolating through ashes of oak or hard oak. Both
solutions are taken out of vats and poured into rectangular copper
caldrons, and are boiled until at last they condense into _nitrum_.
[Illustration 561 (Soda Making): A--Vat in which the soda is mixed.
B--Caldron. C--Tub in which _chrysocolla_ is condensed. D--Copper wires.
E--Mortar.]
Native as well as manufactured _nitrum_ is mixed in vats with urine and
boiled in the same caldrons; the decoction is poured into vats in which
are copper wires, and, adhering to them, it hardens and becomes
_chrysocolla_, which the Moors call _borax_. Formerly _nitrum_ was
compounded with Cyprian verdigris, and ground with Cyprian copper in
Cyprian mortars, as Pliny writes. Some _chrysocolla_ is made of
rock-alum and sal-ammoniac.[8]
[Illustration 563 (Saltpetre Making): A--Caldron. B--Large vat into
which sand is thrown. C--Plug. D--Tub. E--Vat containing the rods.]
Saltpetre[9] is made from a dry, slightly fatty earth, which, if it be
retained for a while in the mouth, has an acrid and salty taste. This
earth, together with a powder, are alternately put into a vat in layers
a palm deep. The powder consists of two parts of unslaked lime and three
parts of ashes of oak, or holmoak, or Italian oak, or Turkey oak, or of
some similar kind. Each vat is filled with alternate layers of these to
within three-quarters of a foot of the top, and then water is poured in
until it is full. As the water percolates through the material it
dissolves the saltpetre; then, the plug being pulled out from the vat,
the solution is drained into a tub and ladled out into small vats. If
when tested it tastes very salty, and at the same time acrid, it is
good; but, if not, then it is condemned, and it must be made to
percolate again through the same material or through a fresh lot. Even
two or three waters may be made to percolate through the same earth and
become full of saltpetre, but the solutions thus obtained must not be
mixed together unless all have the same taste, which rarely or never
happens. The first of these solutions is poured into the first vat, the
next into the second, the third into the third vat; the second and third
solutions are used instead of plain water to percolate through fresh
material; the first solution is made in this manner from both the second
and third. As soon as there is an abundance of this solution it is
poured into the rectangular copper caldron and evaporated to one half by
boiling; then it is transferred into a vat covered with a lid, in which
the earthy matter settles to the bottom. When the solution is clear it
is poured back into the same pan, or into another, and re-boiled. When
it bubbles and forms a scum, in order that it should not run over and
that it may be greatly purified, there is poured into it three or four
pounds of lye, made from three parts of oak or similar ash and one of
unslaked lime. But in the water, prior to its being poured in, is
dissolved rock-alum, in the proportion of one hundred and twenty
_librae_ of the former to five _librae_ of the latter. Shortly
afterward the solution will be found to be clear and blue. It is boiled
until the waters, which are easily volatile (_subtiles_), are
evaporated, and then the greater part of the salt, after it has settled
at the bottom of the pan, is taken out with iron ladles. Then the
concentrated solution is transferred to the vat in which rods are placed
horizontally and vertically, to which it adheres when cold, and if there
be much, it is condensed in three or four days into saltpetre. Then the
solution which has not congealed, is poured out and put on one side or
re-boiled. The saltpetre being cut out and washed with its own solution,
is thrown on to boards that it may drain and dry. The yield of saltpetre
will be much or little in proportion to whether the solution has
absorbed much or little; when the saltpetre has been obtained from lye,
which purifies itself, it is somewhat clear and pure.
The purest and most transparent, because free from salt, is made if it
is drawn off at the thickening stage, according to the following method.
There are poured into the caldron the same number of _amphorae_ of the
solution as of _congii_ of the lye of which I have already spoken, and
into the same caldron is thrown as much of the already made saltpetre as
the solution and lye will dissolve. As soon as the mixture effervesces
and forms scum, it is transferred to a vat, into which on a cloth has
been thrown washed sand obtained from a river. Soon afterward the plug
is drawn out of the hole at the bottom, and the mixture, having
percolated through the sand, escapes into a tub. It is then reduced by
boiling in one or another of the caldrons, until the greater part of the
solution has evaporated; but as soon as it is well boiled and forms
scum, a little lye is poured into it. Then it is transferred to another
vat in which there are small rods, to which it adheres and congeals in
two days if there is but little of it, or if there is much in three
days, or at the most in four days; if it does not condense, it is poured
back into the caldron and re-boiled down to half; then it is transferred
to the vat to cool. The process must be repeated as often as is
necessary.
Others refine saltpetre by another method, for with it they fill a pot
made of copper, and, covering it with a copper lid, set it over live
coals, where it is heated until it melts. They do not cement down the
lid, but it has a handle, and can be lifted for them to see whether or
not the melting has taken place. When it has melted, powdered sulphur is
sprinkled in, and if the pot set on the fire does not light it, the
sulphur kindles, whereby the thick, greasy matter floating on the
saltpetre burns up, and when it is consumed the saltpetre is pure. Soon
afterward the pot is removed from the fire, and later, when cold, the
purest saltpetre is taken out, which has the appearance of white marble,
the earthy residue then remains at the bottom. The earths from which the
solution was made, together with branches of oak or similar trees, are
exposed under the open sky and sprinkled with water containing
saltpetre. After remaining thus for five or six years, they are again
ready to be made into a solution.
Pure saltpetre which has rested many years in the earth, and that which
exudes from the stone walls of wine cellars and dark places, is mixed
with the first solution and evaporated by boiling.
Thus far I have described the methods of making _nitrum_, which are not
less varied or multifarious than those for making salt. Now I propose to
describe the methods of making alum,[10] which are likewise neither all
alike, nor simple, because it is made from boiling aluminous water until
it condenses to alum, or else from boiling a solution of alum which is
obtained from a kind of earth, or from rocks, or from pyrites, or other
minerals.
[Illustration 567 (Vitriol Making): A--Tanks. B--Stirring poles.
C--Plug. D--Trough. E--Reservoir. F--Launder. G--lead caldron. H--Wooden
tubs sunk into the earth. I--Vats in which twigs are fixed.]
This kind of earth having first been dug up in such quantity as would
make three hundred wheelbarrow loads, is thrown into two tanks; then the
water is turned into them, and if it (the earth) contains vitriol it
must be diluted with urine. The workmen must many times a day stir the
ore with long, thick sticks in order that the water and urine may be
mixed with it; then the plugs having been taken out of both tanks, the
solution is drawn off into a trough, which is carved out of one or two
trees. If the locality is supplied with an abundance of such ore, it
should not immediately be thrown into the tanks, but first conveyed into
open spaces and heaped up, for the longer it is exposed to the air and
the rain, the better it is; after some months, during which the ore has
been heaped up in open spaces into mounds, there are generated veinlets
of far better quality than the ore. Then it is conveyed into six or more
tanks, nine feet in length and breadth and five in depth, and afterward
water is drawn into them of similar solution. After this, when the water
has absorbed the alum, the plugs are pulled out, and the solution
escapes into a round reservoir forty feet wide and three feet deep. Then
the ore is thrown out of the tanks into other tanks, and water again
being run into the latter and the urine added and stirred by means of
poles, the plugs are withdrawn and the solution is run off into the same
reservoir. A few days afterward, the reservoirs containing the solution
are emptied through a small launder, and run into rectangular lead
caldrons; it is boiled in them until the greater part of the water has
evaporated. The earthy sediment deposited at the bottom of the caldron
is composed of fatty and aluminous matter, which usually consists of
small incrustations, in which there is not infrequently found a very
white and very light powder of asbestos or gypsum. The solution now
seems to be full of meal. Some people instead pour the partly evaporated
solution into a vat, so that it may become pure and clear; then pouring
it back into the caldron, they boil it again until it becomes mealy. By
whichever process it has been condensed, it is then poured into a wooden
tub sunk into the earth in order to cool it. When it becomes cold it is
poured into vats, in which are arranged horizontal and vertical twigs,
to which the alum clings when it condenses; and thus are made the small
white transparent cubes, which are laid to dry in hot rooms.
If vitriol forms part of the aluminous ore, the material is dissolved in
water without being mixed with urine, but it is necessary to pour that
into the clear and pure solution when it is to be re-boiled. This
separates the vitriol from the alum, for by this method the latter sinks
to the bottom of the caldron, while the former floats on the top; both
must be poured separately into smaller vessels, and from these into vats
to condense. If, however, when the solution was re-boiled they did not
separate, then they must be poured from the smaller vessels into larger
vessels and covered over; then the vitriol separating from the alum, it
condenses. Both are cut out and put to dry in the hot room, and are
ready to be sold; the solution which did not congeal in the vessels
and vats is again poured back into the caldron to be re-boiled. The
earth which settled at the bottom of the caldron is carried back to the
tanks, and, together with the ore, is again dissolved with water and
urine. The earth which remains in the tanks after the solution has been
drawn off is emptied in a heap, and daily becomes more and more
aluminous in the same way as the earth from which saltpetre was made,
but fuller of its juices, wherefore it is again thrown into the tanks
and percolated by water.
[Illustration 571 (Alum Making): A--Furnace. B--Enclosed space.
C--Aluminous rock. D--Deep ladle. E--Caldron. F--Launder. G--Troughs.]
Aluminous rock is first roasted in a furnace similar to a lime kiln. At
the bottom of the kiln a vaulted fireplace is made of the same kind of
rock; the remainder of the empty part of the kiln is then entirely
filled with the same aluminous rocks. Then they are heated with fire
until they are red hot and have exhaled their sulphurous fumes, which
occurs, according to their divers nature, within the space of ten,
eleven, twelve, or more hours. One thing the master must guard against
most of all is not to roast the rock either too much or too little, for
on the one hand they would not soften when sprinkled with water, and on
the other they either would be too hard or would crumble into ashes;
from neither would much alum be obtained, for the strength which they
have would be decreased. When the rocks are cooled they are drawn out
and conveyed into an open space, where they are piled one upon the other
in heaps fifty feet long, eight feet wide, and four feet high, which are
sprinkled for forty days with water carried in deep ladles. In spring
the sprinkling is done both morning and evening, and in summer at noon
besides. After being moistened for this length of time the rocks begin
to fall to pieces like slaked lime, and there originates a certain new
material of the future alum, which is soft and similar to the _liquidae
medullae_ found in the rocks. It is white if the stone was white before
it was roasted, and rose-coloured if red was mixed with the white; from
the former, white alum is obtained, and from the latter, rose-coloured.
A round furnace is made, the lower part of which, in order to be able to
endure the force of the heat, is made of rock that neither melts nor
crumbles to powder by the fire. It is constructed in the form of a
basket, the walls of which are two feet high, made of the same rock. On
these walls rests a large round caldron made of copper plates, which is
concave at the bottom, where it is eight feet in diameter. In the empty
space under the bottom they place the wood to be kindled with fire.
Around the edge of the bottom of the caldron, rock is built in
cone-shaped, and the diameter of the bottom of the rock structure is
seven feet, and of the top ten feet; it is eight feet deep. The inside,
after being rubbed over with oil, is covered with cement, so that it may
be able to hold boiling water; the cement is composed of fresh lime, of
which the lumps are slaked with wine, of iron-scales, and of sea-snails,
ground and mixed with the white of eggs and oil. The edges of the
caldron are surmounted with a circle of wood a foot thick and half a
foot high, on which the workmen rest the wooden shovels with which they
cleanse the water of earth and of the undissolved lumps of rock that
remain at the bottom of the caldron. The caldron, being thus prepared,
is entirely filled through a launder with water, and this is boiled with
a fierce fire until it bubbles. Then little by little eight wheelbarrow
loads of the material, composed of roasted rock moistened with water,
are gradually emptied into the caldron by four workmen, who, with their
shovels which reach to the bottom, keep the material stirred and mixed
with water, and by the same means they lift the lumps of undissolved
rock out of the caldron. In this manner the material is thrown in, in
three or four lots, at intervals of two or three hours more or less;
during these intervals, the water, which has been cooled by the rock and
material, again begins to boil. The water, when sufficiently purified
and ready to congeal, is ladled out and run off with launders into
thirty troughs. These troughs are made of oak, holm oak, or Turkey oak;
their interior is six feet long, five feet deep, and four feet wide. In
these the water congeals and condenses into alum, in the spring in the
space of four days, and in summer in six days. Afterward the holes at
the bottom of the oak troughs being opened, the water which has not
congealed is drawn off into buckets and poured back into the caldron; or
it may be preserved in empty troughs, so that the master of the workmen,
having seen it, may order his helpers to pour it into the caldron, for
the water which is not altogether wanting in alum, is considered better
than that which has none at all. Then the alum is hewn out with a knife
or a chisel. It is thick and excellent according to the strength of the
rock, either white or pink according to the colour of the rock. The
earthy powder, which remains three to four digits thick as the residue
of the alum at the bottom of the trough is again thrown into the caldron
and boiled with fresh aluminous material. Lastly, the alum cut out is
washed, and dried, and sold.
Alum is also made from crude pyrites and other aluminous mixtures. It is
first roasted in an enclosed area; then, after being exposed for some
months to the air in order to soften it, it is thrown into vats and
dissolved. After this the solution is poured into the leaden rectangular
pans and boiled until it condenses into alum. The pyrites and other
stones which are not mixed with alum alone, but which also contain
vitriol, as is most usually the case, are both treated in the manner
which I have already described. Finally, if metal is contained in the
pyrites and other rock, this material must be dried, and from it either
gold, silver, or copper is made in a furnace.
Vitriol[11] can be made by four different methods; by two of these
methods from water containing vitriol; by one method from a solution of
_melanteria_, _sory_ and _chalcitis_; and by another method from earth
or stones mixed with vitriol.
[Illustration 574 (Vitriol Making): A--Tunnel. B--Bucket. C--Pit.]
The vitriol water is collected into pools, and if it cannot be drained
into them, it must be drawn up and carried to them in buckets by a
workman. In hot regions or in summer, it is poured into out-of-door
pits which have been dug to a certain depth, or else it is extracted
from shafts by pumps and poured into launders, through which it flows
into the pits, where it is condensed by the heat of the sun. In cold
regions and in winter these vitriol waters are boiled down with equal
parts of fresh water in rectangular leaden caldrons; then, when cold,
the mixture is poured into vats or into tanks, which Pliny calls wooden
fish-tanks. In these tanks light cross-beams are fixed to the upper
part, so that they may be stationary, and from them hang ropes stretched
with little stones; to these the contents of the thickened solutions
congeal and adhere in transparent cubes or seeds of vitriol, like
bunches of grapes.
[Illustration 575 (Vitriol Making): A--Caldron. B--Tank. C--Cross-bars.
D--Ropes. E--Little stones.]
By the third method vitriol is made out of _melanteria_ and _sory_. If
the mines give an abundant supply of _melanteria_ and _sory_, it is
better to reject the _chalcitis_, and especially the _misy_, for from
these the vitriol is impure, particularly from the _misy_. These
materials having been dug and thrown into the tanks, they are first
dissolved with water; then, in order to recover the pyrites from which
copper is not rarely smelted and which forms a sediment at the bottom of
the tanks, the solution is transferred to other vats, which are nine
feet wide and three feet deep. Twigs and wood which float on the surface
are lifted out with a broom made of twigs, and afterward all the
sediment settles at the bottom of this vat. The solution is poured into
a rectangular leaden caldron eight feet long, three feet wide, and the
same in depth. In this caldron it is boiled until it becomes thick and
viscous, when it is poured into a launder, through which it runs into
another leaden caldron of the same size as the one described before.
When cold, the solution is drawn off through twelve little launders, out
of which it flows into as many wooden tubs four and a half feet deep and
three feet wide. Upon these tubs are placed perforated crossbars distant
from each other from four to six digits, and from the holes hang thin
laths, which reach to the bottom, with pegs or wedges driven into them.
The vitriol adheres to these laths, and within the space of a few days
congeals into cubes, which are taken away and put into a chamber having
a sloping board floor, so that the moisture which drips from the vitriol
may flow into a tub beneath. This solution is re-boiled, as is also that
solution which was left in the twelve tubs, for, by reason of its having
become too thin and liquid, it did not congeal, and was thus not
converted into vitriol.
[Illustration 576 (Vitriol Making): A--Wooden tub. B--Cross-bars.
C--Laths. D--Sloping floor of the chamber. E--Tub placed under it.]
[Illustration 577 (Vitriol Making): A--Caldron. B--Moulds. C--Cakes.]
The fourth method of making vitriol is from vitriolous earth or stones.
Such ore is at first carried and heaped up, and is then left for five or
six months exposed to the rain of spring and autumn, to the heat of
summer, and to the rime and frost of winter. It must be turned over
several times with shovels, so that the part at the bottom may be
brought to the top, and it is thus ventilated and cooled; by this means
the earth crumbles up and loosens, and the stone changes from hard to
soft. Then the ore is covered with a roof, or else it is taken away and
placed under a roof, and remains in that place six, seven, or eight
months. Afterward as large a portion as is required is thrown into a
vat, which is half-filled with water; this vat is one hundred feet
long, twenty-four feet wide, eight feet deep. It has an opening at the
bottom, so that when it is opened the dregs of the ore from which the
vitriol comes may be drawn off, and it has, at the height of one foot
from the bottom, three or four little holes, so that, when closed, the
water may be retained, and when opened the solution flows out. Thus the
ore is mixed with water, stirred with poles and left in the tank until
the earthy portions sink to the bottom and the water absorbs the juices.
Then the little holes are opened, the solution flows out of the vat, and
is caught in a vat below it; this vat is of the same length as the
other, but twelve feet wide and four feet deep. If the solution is not
sufficiently vitriolous it is mixed with fresh ore; but if it contains
enough vitriol, and yet has not exhausted all of the ore rich in
vitriol, it is well to dissolve the ore again with fresh water. As soon
as the solution becomes clear, it is poured into the rectangular leaden
caldron through launders, and is boiled until the water is evaporated.
Afterward as many thin strips of iron as the nature of the solution
requires, are thrown in, and then it is boiled again until it is thick
enough, when cold, to congeal into vitriol. Then it is poured into tanks
or vats, or any other receptacle, in which all of it that is apt to
congeal does so within two or three days. The solution which does not
congeal is either poured back into the caldron to be boiled again, or
it is put aside for dissolving the new ore, for it is far preferable to
fresh water. The solidified vitriol is hewn out, and having once more
been thrown into the caldron, is re-heated until it liquefies; when
liquid, it is poured into moulds that it may be made into cakes. If the
solution first poured out is not satisfactorily thickened, it is
condensed two or three times, and each time liquefied in the caldron and
re-poured into the moulds, in which manner pure cakes, beautiful to look
at, are made from it.
The vitriolous pyrites, which are to be numbered among the mixtures
(_mistura_), are roasted as in the case of alum, and dissolved with
water, and the solution is boiled in leaden caldrons until it condenses
into vitriol. Both alum and vitriol are often made out of these, and it
is no wonder, for these juices are cognate, and only differ in the one
point,--that the former is less, the latter more, earthy. That pyrites
which contains metal must be smelted in the furnace. In the same manner,
from other mixtures of vitriolic and metalliferous material are made
vitriol and metal. Indeed, if ores of vitriolous pyrites abound, the
miners split small logs down the centre and cut them off in lengths as
long as the drifts and tunnels are wide, in which they lay them down
transversely; but, that they may be stable, they are laid on the ground
with the wide side down and the round side up, and they touch each other
at the bottom, but not at the top. The intermediate space is filled with
pyrites, and the same crushed are scattered over the wood, so that,
coming in or going out, the road is flat and even. Since the drifts or
tunnels drip with water, these pyrites are soaked, and from them are
freed the vitriol and cognate things. If the water ceases to drip, these
dry and harden, and then they are raised from the shafts, together with
the pyrites not yet dissolved in the water, or they are carried out from
the tunnels; then they are thrown into vats or tanks, and boiling water
having been poured over them, the vitriol is freed and the pyrites are
dissolved. This green solution is transferred to other vats or tanks,
that it may be made clear and pure; it is then boiled in the lead
caldrons until it thickens; afterward it is poured into wooden tubs,
where it condenses on rods, or reeds, or twigs, into green vitriol.
Sulphur is made from sulphurous waters, from sulphurous ores, and from
sulphurous mixtures. These waters are poured into the leaden caldrons
and boiled until they condense into sulphur. From this latter, heated
together with iron-scales, and transferred into pots, which are
afterward covered with lute and refined sulphur, another sulphur is
made, which we call _caballinum_.[12]
[Illustration 579 (Sulphur Making): A--Pots having spouts. B--Pots
without spouts. C--Lids.]
The ores[13] which consist mostly of sulphur and of earth, and rarely of
other minerals, are melted in big-bellied earthenware pots. The
furnaces, which hold two of these pots, are divided into three parts;
the lowest part is a foot high, and has an opening at the front for the
draught; the top of this is covered with iron plates, which are
perforated near the edges, and these support iron rods, upon which the
firewood is placed. The middle part of the furnace is one and a half
feet high, and has a mouth in front, so that the wood may be inserted;
the top of this has rods, upon which the bottom of the pots stand. The
upper part is about two feet high, and the pots are also two feet high
and one digit thick; these have below their mouths a long, slender
spout. In order that the mouth of the pot may be covered, an earthenware
lid is made which fits into it. For every two of these pots there must
be one pot of the same size and shape, and without a spout, but having
three holes, two of which are below the mouth and receive the spouts of
the two first pots; the third hole is on the opposite side at the
bottom, and through it the sulphur flows out. In each furnace are placed
two pots with spouts, and the furnace must be covered by plates of iron
smeared over with lute two digits thick; it is thus entirely closed in,
but for two or three vent-holes through which the mouths of the pots
project. Outside of the furnace, against one side, is placed the pot
without a spout, into the two holes of which the two spouts of the other
pots penetrate, and this pot should be built in at both sides to keep it
steady. When the sulphur ore has been placed in the pots, and these
placed in the furnace, they are closely covered, and it is desirable to
smear the joint over with lute, so that the sulphur will not exhale, and
for the same reason the pot below is covered with a lid, which is also
smeared with lute. The wood having been kindled, the ores are heated
until the sulphur is exhaled, and the vapour, arising through the spout,
penetrates into the lower pot and thickens into sulphur, which falls to
the bottom like melted wax. It then flows out through the hole, which,
as I said, is at the bottom of this pot; and the workman makes it into
cakes, or thin sticks or thin pieces of wood are dipped in it. Then he
takes the burning wood and glowing charcoal from the furnace, and when
it has cooled, he opens the two pots, empties the residues, which, if
the ores were composed of sulphur and earth, resemble naturally
extinguished ashes; but if the ores consisted of sulphur and earth and
stone, or sulphur and stone only, they resemble earth completely dried
or stones well roasted. Afterward the pots are re-filled with ore, and
the whole work is repeated.
[Illustration 581 (Sulphur Making): A--Long wall. B--High walls. C--Low
walls. D--Plates. E--Upper pots. F--Lower pots.]
The sulphurous mixture, whether it consists of stone and sulphur only,
or of stone and sulphur and metal, may be heated in similar pots, but
with perforated bottoms. Before the furnace is constructed, against the
"second" wall of the works two lateral partitions are built seven feet
high, three feet long, one and a half feet thick, and these are distant
from each other twenty-seven feet. Between them are seven low brick
walls, that measure but two feet and the same number of digits in
height, and, like the other walls, are three feet long and one foot
thick; these little walls are at equal distances from one another,
consequently they will be two and one half feet apart. At the top, iron
bars are fixed into them, which sustain iron plates three feet long and
wide and one digit thick, so that they can bear not only the weight of
the pots, but also the fierceness of the fire. These plates have in the
middle a round hole one and a half digits wide; there must not be more
than eight of these, and upon them as many pots are placed. These pots
are perforated at the bottom, and the same number of whole pots are
placed underneath them; the former contain the mixture, and are covered
with lids; the latter contain water, and their mouths are under the
holes in the plates. After wood has been arranged round the upper pots
and ignited, the mixture being heated, red, yellow, or green sulphur
drips from it and flows down through the hole, and is caught by the pots
placed underneath the plates, and is at once cooled by the water. If the
mixture contains metal, it is reserved for smelting, and, if not, it is
thrown away. The sulphur from such a mixture can best be extracted if
the upper pots are placed in a vaulted furnace, like those which I
described among other metallurgical subjects in Book VIII., which has no
floor, but a grate inside; under this the lower pots are placed in the
same manner, but the plates must have larger holes.
[Illustration 582 (Bitumen Making): A--Lower pot. B--Upper pot. C--Lid.]
Others bury a pot in the ground, and place over it another pot with a
hole at the bottom, in which pyrites or _cadmia_, or other sulphurous
stones are so enclosed that the sulphur cannot exhale. A fierce fire
heats the sulphur, and it drips away and flows down into the lower pot,
which contains water. (Illustration p. 582).
[Illustration 583 (Bitumen Making): A--Bituminous spring. B--Bucket.
C--Pot. D--Lid.]
Bitumen[14] is made from bituminous waters, from liquid bitumen, and
from mixtures of bituminous substances. The water, bituminous as well as
salty, at Babylon, as Pliny writes, was taken from the wells to the
salt works and heated by the great heat of the sun, and condensed partly
into liquid bitumen and partly into salt. The bitumen being lighter,
floats on the top, while the salt being heavier, sinks to the bottom.
Liquid bitumen, if there is much floating on springs, streams and
rivers, is drawn up in buckets or other vessels; but, if there is
little, it is collected with goose wings, pieces of linen, _ralla_,
shreds of reeds, and other things to which it easily adheres, and it is
boiled in large brass or iron pots by fire and condensed. As this
bitumen is put to divers uses, some mix pitch with the liquid, others
old cart-grease, in order to temper its viscosity; these, however long
they are boiled in the pots, cannot be made hard. The mixtures
containing bitumen are also treated in the same manner as those
containing sulphur, in pots having a hole in the bottom, and it is rare
that such bitumen is not highly esteemed.
[Illustration 585 (Chrysocolla Making): A--Mouth of the tunnel.
B--Trough. C--Tanks. D--Little trough.]
Since all solidified juices and earths, if abundantly and copiously
mixed with the water, are deposited in the beds of springs, streams or
rivers, and the stones therein are coated by them, they do not require
the heat of the sun or fire to harden them. This having been pondered
over by wise men, they discovered methods by which the remainder of
these solidified juices and unusual earths can be collected. Such
waters, whether flowing from springs or tunnels, are collected in many
wooden tubs or tanks arranged in consecutive order, and deposit in them
such juices or earths; these being scraped off every year, are
collected, as _chrysocolla_[15] in the Carpathians and as ochre in the
Harz.
There remains glass, the preparation of which belongs here, for the
reason that it is obtained by the power of fire and subtle art from
certain solidified juices and from coarse or fine sand. It is
transparent, as are certain solidified juices, gems, and stones; and can
be melted like fusible stones and metals. First I must speak of the
materials from which glass is made; then of the furnaces in which it is
melted; then of the methods by which it is produced.
It is made from fusible stones and from solidified juices, or from other
juicy substances which are connected by a natural relationship. Stones
which are fusible, if they are white and translucent, are more excellent
than the others, for which reason crystals take the first place. From
these, when pounded, the most excellent transparent glass was made in
India, with which no other could be compared, as Pliny relates. The
second place is accorded to stones which, although not so hard as
crystal, are yet just as white and transparent. The third is given to
white stones, which are not transparent. It is necessary, however, first
of all to heat all these, and afterward they are subjected to the pestle
in order to break and crush them into coarse sand, and then they are
passed through a sieve. If this kind of coarse or fine sand is found by
the glass-makers near the mouth of a river, it saves them much labour in
burning and crushing. As regards the solidified juices, the first place
is given to soda; the second to white and translucent rock-salt; the
third to salts which are made from lye, from the ashes of the musk ivy,
or from other salty herbs. Yet there are some who give to this latter,
and not to the former, the second place. One part of coarse or fine sand
made from fusible stones should be mixed with two parts of soda or of
rock-salt or of herb salts, to which are added minute particles of
_magnes_.[16] It is true that in our day, as much as in ancient times,
there exists the belief in the singular power of the latter to attract
to itself the vitreous liquid just as it does iron, and by attracting it
to purify and transform green or yellow into white; and afterward fire
consumes the _magnes_. When the said juices are not to be had, two parts
of the ashes of oak or holmoak, or of hard oak or Turkey oak, or if
these be not available, of beech or pine, are mixed with one part of
coarse or fine sand, and a small quantity of salt is added, made from
salt water or sea-water, and a small particle of _magnes_; but these
make a less white and translucent glass. The ashes should be made from
old trees, of which the trunk at a height of six feet is hollowed out
and fire is put in, and thus the whole tree is consumed and converted
into ashes. This is done in winter when the snow lies long, or in summer
when it does not rain, for the showers at other times of the year, by
mixing the ashes with earth, render them impure; for this reason, at
such times, these same trees are cut up into many pieces and burned
under cover, and are thus converted into ashes.
[Illustration 587 (Glass-making Furnace): A--Lower chamber of the first
furnace. B--Upper chamber. C--Vitreous mass.]
Some glass-makers use three furnaces, others two, others only one. Those
who use three, melt the material in the first, re-melt it in the second,
and in the third they cool the glowing glass vessels and other
articles. Of these the first furnace must be vaulted and similar to an
oven. In the upper chamber, which is six feet long, four feet wide, and
two feet high, the mixed materials are heated by a fierce fire of dry
wood until they melt and are converted into a vitreous mass. And if they
are not satisfactorily purified from dross, they are taken out and
cooled and broken into pieces; and the vitreous pieces are heated in
pots in the same furnace.
[Illustration 588 (Glass-making Furnace): A--Arches of the second
furnace. B--Mouth of the lower chamber. C--Windows of the upper chamber.
D--Big-bellied pots. E--Mouth of the third furnace. F--Recesses for the
receptacles. G--Openings in the upper chamber. H--Oblong receptacles.]
The second furnace is round, ten feet in diameter and eight feet high,
and on the outside, so that it may be stronger, it is encompassed by
five arches, one and one half feet thick; it consists in like manner of
two chambers, of which the lower one is vaulted and is one and one half
feet thick. In front this chamber has a narrow mouth, through which the
wood can be put into the hearth, which is on the ground. At the top and
in the middle of its vault, there is a large round hole which opens to
the upper chamber, so that the flames can penetrate into it. Between the
arches in the walls of the upper chamber are eight windows, so large
that the big-bellied pots may be placed through them on to the floor of
the chamber, around the large hole. The thickness of these pots is about
two digits, their height the same number of feet, and the diameter of
the belly one and a half feet, and of the mouth and bottom one foot. In
the back part of the furnace is a rectangular hole, measuring in height
and width a palm, through which the heat penetrates into a third furnace
which adjoins it.
This third furnace is rectangular, eight feet long and six feet wide; it
also consists of two chambers, of which the lower has a mouth in front,
so that firewood may be placed on the hearth which is on the ground. On
each side of this opening in the wall of the lower chamber is a recess
for oblong earthenware receptacles, which are about four feet long, two
feet high, and one and a half feet wide. The upper chamber has two
holes, one on the right side, the other on the left, of such height and
width that earthenware receptacles may be conveniently placed in them.
These latter receptacles are three feet long, one and a half feet high,
the lower part one foot wide, and the upper part rounded. In these
receptacles the glass articles, which have been blown, are placed so
that they may cool in a milder temperature; if they were not cooled
slowly they would burst asunder. When the vessels are taken from the
upper chamber, they are immediately placed in the receptacles to cool.
[Illustration 589 (Glass-making Furnaces): A--Lower chamber of the
other second furnace. B--Middle one. C--Upper one. D--Its opening.
E--Round opening. F--Rectangular opening.]
Some who use two furnaces partly melt the mixture in the first, and not
only re-melt it in the second, but also replace the glass articles
there. Others partly melt and re-melt the material in different chambers
of the second furnace. Thus the former lack the third furnace, and the
latter, the first. But this kind of second furnace differs from the
other second furnace, for it is, indeed, round, but the interior is
eight feet in diameter and twelve feet high, and it consists of three
chambers, of which the lowest is not unlike the lowest of the other
second furnace. In the middle chamber wall there are six arched
openings, in which are placed the pots to be heated, and the remainder
of the small windows are blocked up with lute. In the middle top of the
middle chamber is a square opening a palm in length and width. Through
this the heat penetrates into the upper chamber, of which the rear part
has an opening to receive the oblong earthenware receptacles, in which
are placed the glass articles to be slowly cooled. On this side, the
ground of the workshop is higher, or else a bench is placed there, so
that the glass-makers may stand upon it to stow away their products more
conveniently.
Those who lack the first furnace in the evening, when they have
accomplished their day's work, place the material in the pots, so that
the heat during the night may melt it and turn it into glass. Two boys
alternately, during night and day, keep up the fire by throwing dry wood
on to the hearth. Those who have but one furnace use the second sort,
made with three chambers. Then in the evening they pour the material
into the pots, and in the morning, having extracted the fused material,
they make the glass objects, which they place in the upper chamber, as
do the others.
The second furnace consists either of two or three chambers, the first
of which is made of unburnt bricks dried in the sun. These bricks are
made of a kind of clay that cannot be easily melted by fire nor resolved
into powder; this clay is cleaned of small stones and beaten with rods.
The bricks are laid with the same kind of clay instead of lime. From the
same clay the potters also make their vessels and pots, which they dry
in the shade. These two parts having been completed, there remains the
third.
[Illustration 591 (Glass Making): A--Blow-pipe. B--Little window.
C--Marble. D--Forceps. E--Moulds by means of which the shapes are
produced.]
The vitreous mass having been made in the first furnace in the manner I
described, is broken up, and the assistant heats the second furnace, in
order that the fragments may be re-melted. In the meantime, while they
are doing this, the pots are first warmed by a slow fire in the first
furnace, so that the vapours may evaporate, and then by a fiercer fire,
so that they become red in drying. Afterward the glass-makers open the
mouth of the furnace, and, seizing the pots with tongs, if they have not
cracked and fallen to pieces, quickly place them in the second furnace,
and they fill them up with the fragments of the heated vitreous mass or
with glass. Afterward they close up all the windows with lute and
bricks, with the exception that in each there are two little windows
left free; through one of these they inspect the glass contained in the
pot, and take it up by means of a blow-pipe; in the other they rest
another blow-pipe, so that it may get warm. Whether it is made of brass,
bronze, or iron, the blow-pipe must be three feet long. In front of
the window is inserted a lip of marble, on which rests the heaped-up
clay and the iron shield. The clay holds the blow-pipe when it is put
into the furnace, whereas the shield preserves the eyes of the
glass-maker from the fire. All this having been carried out in order,
the glass-makers bring the work to completion. The broken pieces they
re-melt with dry wood, which emits no smoke, but only a flame. The
longer they re-melt it, the purer and more transparent it becomes, the
fewer spots and blisters there are, and therefore the glass-makers can
carry out their work more easily. For this reason those who only melt
the material from which glass is made for one night, and then
immediately make it up into glass articles, make them less pure and
transparent than those who first produce a vitreous mass and then
re-melt the broken pieces again for a day and a night. And, again, these
make a less pure and transparent glass than do those who melt it again
for two days and two nights, for the excellence of the glass does not
consist solely in the material from which it is made, but also in the
melting. The glass-makers often test the glass by drawing it up with the
blowpipes; as soon as they observe that the fragments have been
re-melted and purified satisfactorily, each of them with another
blow-pipe which is in the pot, slowly stirs and takes up the glass which
sticks to it in the shape of a ball like a glutinous, coagulated gum. He
takes up just as much as he needs to complete the article he wishes to
make; then he presses it against the lip of marble and kneads it round
and round until it consolidates. When he blows through the pipe he blows
as he would if inflating a bubble; he blows into the blow-pipe as often
as it is necessary, removing it from his mouth to re-fill his cheeks, so
that his breath does not draw the flames into his mouth. Then, twisting
the lifted blow-pipe round his head in a circle, he makes a long glass,
or moulds the same in a hollow copper mould, turning it round and round,
then warming it again, blowing it and pressing it, he widens it into the
shape of a cup or vessel, or of any other object he has in mind. Then he
again presses this against the marble to flatten the bottom, which he
moulds in the interior with his other blow-pipe. Afterward he cuts out
the lip with shears, and, if necessary, adds feet and handles. If it so
please him, he gilds it and paints it with various colours. Finally, he
lays it in the oblong earthenware receptacle, which is placed in the
third furnace, or in the upper chamber of the second furnace, that it
may cool. When this receptacle is full of other slowly-cooled articles,
he passes a wide iron bar under it, and, carrying it on the left arm,
places it in another recess.
The glass-makers make divers things, such as goblets, cups, ewers,
flasks, dishes, plates, panes of glass, animals, trees, and ships, all
of which excellent and wonderful works I have seen when I spent two
whole years in Venice some time ago. Especially at the time of the Feast
of the Ascension they were on sale at Morano, where are located the most
celebrated glass-works. These I saw on other occasions, and when, for a
certain reason, I visited Andrea Naugerio in his house which he had
there, and conversed with him and Francisco Asulano.
END OF BOOK XII.
FOOTNOTES:
[1] The history of salt-making in salt-pans, from sea-water or salt
springs, goes further back than human records. From an historical point
of view the real interest attached to salt lies in the bearing which
localities rich in either natural salt or salt springs, have had upon
the movements of the human race. Many ancient trade routes have been due
to them, and innumerable battles have been fought for their possession.
Salt has at times served for currency, and during many centuries in
nearly every country has served as a basis of taxation. These subjects
do not, however, come within the scope of this text. For the quotation
from Pliny referred to, see Note 14 below, on bitumen.
[2] The first edition gives _graviorem_, the latter editions
_gratiorem_, which latter would have quite the reverse meaning from the
above.
[3] The following are approximately the English equivalents:--
Pints. Quarts. Gallons.
1 _Cyathus_ .08
3 _Cyathi_ = 1 _Quartarius_ .24
4 _Quartarii_ = 1 _Sextarius_ .99
6 _Sextarii_ = 1 _Congius_ 5.94 2.97
16 _Sextarii_ = 1 _Modius_ 15.85 7.93 1.98
8 _Congii_ = 1 _Amphora_ 47.57 23.78 5.94
The dipper mentioned would thus hold about one and one quarter gallons,
and the cask ten gallons.
[4] The salt industry, founded upon salt springs, is still of importance
to this city. It was a salt centre of importance to the Germanic tribes
before Charles, the son of Charlemagne, erected a fortress here in 806.
Mention of the salt works is made in the charter by Otto I., conveying
the place to the Diocese of Magdeburg, in 968.
[5] Pliny XXXI., 39-40. "In the Gallic provinces in Germany they pour
salt water upon burning wood. The Spaniards in a certain place draw the
brine from wells, which they call _Muria_. They indeed think that the
wood turns to salt, and that the oak is the best, being the kind which
is itself salty. Elsewhere the hazel is praised. Thus the charcoal even
is turned into salt when it is steeped in brine. Whenever salt is made
with wood it is black."
[6] We have elsewhere in this book used the word "soda" for the Latin
term _nitrum_, because we believe as used by Agricola it was always
soda, and because some confusion of this term with its modern adaptation
for saltpetre (nitre) might arise in the mind of the reader.
Fortunately, Agricola usually carefully mentions other alkalis, such as
the product from lixiviation of ashes, separately from his _nitrum_. In
these paragraphs, however, he has soda and potash hopelessly mixed,
wherefore we have here introduced the Latin term. The actual difference
between potash and soda--the _nitrum_ of the Ancients, and the _alkali_
of Geber (and the glossary of Agricola), was not understood for two
hundred years after Agricola, when Duhamel made his well-known
determinations; and the isolation of sodium and potassium was, of
course, still later by fifty years. If the reeds and rushes described in
this paragraph grew near the sea, the salt from lixiviation would be
soda, and likewise the Egyptian product was soda, but the lixiviation of
wood-ash produces only potash; as seen above, all are termed _nitrum_
except the first.
HISTORICAL NOTES.--The word _nitrum_, _nitron_, _nitri_, _neter_,
_nether_, or similar forms, occurs in innumerable ancient writings.
Among such references are Jeremiah (II., 22) Proverbs (XXV., 20),
Herodotus (II., 86, 87), Aristotle (_Prob._ I., 39, _De Mirab._ 54),
Theophrastus (_De Igne_ 435 ed. Heinsii, Hist. Plants III., 9),
Dioscorides (V., 89), Pliny (XIV., 26, and XXXI., 46). A review of
disputations on what salts this term comprised among the Ancients would
itself fill a volume, but from the properties named it was no doubt
mostly soda, more rarely potash, and sometimes both mixed with common
salt. There is every reason to believe from the properties and uses
mentioned, that it did not generally comprise nitre (saltpetre)--into
which superficial error the nomenclature has led many translators. The
preparation by way of burning, and the use of _nitrum_ for purposes for
which we now use soap, for making glass, for medicines, cosmetics,
salves, painting, in baking powder, for preserving food, embalming,
etc., and the descriptions of its taste in "nitrous" waters,--all answer
for soda and potash, but not for saltpetre. It is possible that the
common occurrence of saltpetre as an efflorescence on walls might
naturally lead to its use, but in any event its distinguishing
characteristics are nowhere mentioned. As sal-ammoniac occurred in the
volcanoes in Italy, it also may have been included in the _nitrum_
mentioned. _Nitrum_ was in the main exported from Egypt, but
Theophrastus mentions its production from wood-ash, and Pliny very
rightly states that burned lees of wine (argol) had the nature of
_nitrum_. Many of the ancient writers understood that it was rendered
more caustic by burning, and still more so by treatment with lime.
According to Beckmann (Hist. of Inventions II., p. 488), the form of the
word _natron_ was first introduced into Europe by two travellers in
Egypt, Peter Ballon and Prosper Alpinus, about 1550. The word was
introduced into mineralogy by Linnaeus in 1736. In the first instance
_natron_ was applied to soda and potash in distinction to _nitre_ for
saltpetre, and later _natron_ was applied solely to soda.
It is desirable to mention here two other forms of soda and potash which
are frequently mentioned by Agricola. "Ashes which wool dyers use"
(_cineres quo infectores lanarum utuntur_).--There is no indication in
any of Agricola's works as to whether this was some special wood-ash or
whether it was the calcined residues from wool washing. The "yolk" or
"suint" of wool, originating from the perspiration of the animal, has
long been a source of crude potash. The water, after washing the wool,
is evaporated, and the residue calcined. It contains about 85%
K_{2}CO_{3}, the remainder being sodium and potassium sulphates. Another
reason for assuming that it was not a wood-ash product, is that these
products are separately mentioned. In either event, whether obtained
from wool residues or from lixiviation of wood-ash, it would be an
impure potash. In some methods of wool dyeing, a wash of soda was first
given, so that it is barely possible that this substance was sodium
carbonate.
"Salt made from the ashes of musk ivy" (_sal ex anthyllidis cinere
factus_,--Glossary, _salalkali_). This would be largely potash.
[7] This wondrous illustration of soda-making from Nile water is no
doubt founded upon Pliny (XXXI., 46). "It is made in almost the same
manner as salt, except that sea-water is put into salt pans, whereas in
the nitrous pans it is water of the Nile; these, with the subsidence of
the Nile during the forty days, are impregnated with _nitrum_."
[8] This paragraph displays hopeless ignorance. Borax was known to
Agricola and greatly used in his time; it certainly was not made from
these compounds, but was imported from Central Asia. Sal-ammoniac was
also known in his time, and was used like borax as a soldering agent.
The reaction given by Agricola would yield free ammonia. The following
historical notes on borax and sal-ammoniac may be of service.
BORAX.--The uncertainties of the ancient distinctions in salts involve
borax deeply. The word _Baurach_ occurs in Geber and the other early
Alchemistic writings, but there is nothing to prove that it was modern
borax. There cannot be the slightest doubt, however, that the material
referred to by Agricola as _borax_ was our borax, because of the
characteristic qualities incidentally mentioned in Book VII. That he
believed it was an artificial product from _nitrum_ is evident enough
from his usual expression "_chrysocolla_ made from _nitrum_, which the
Moors call _borax_." Agricola, in _De Natura Fossilium_ (p. 206-7),
makes the following statements, which could leave no doubt on the
subject:--"Native _nitrum_ is found in the earth or on the surface....
It is from this variety that the Venetians make _chrysocolla_, which I
call _borax_.... The second variety of artificial _nitrum_ is made at
the present day from the native _nitrum_, called by the Arabs _tincar_,
but I call it usually by the Greek name _chrysocolla_; it is really the
Arabic _borax_.... This _nitrum_ does not decrepitate nor fly out of the
fire; however, the native variety swells up from within." The
application of the word _chrysocolla_ (_chrysos_, gold; _colla_, solder)
to soldering materials, and at the same time to the copper mineral, is
of Greek origin. If any further proof were needed as to the substance
meant by Agricola, it lies in the word _tincar_. For a long time the
borax of Europe was imported from Central Asia, through Constantinople
and Venice, under the name of _tincal_ or _tincar_. When this trade
began, we do not know; evidently before Agricola's time. The statement
here of making borax from alum and sal-ammoniac is identical with the
assertion of Biringuccio (II., 9).
SAL-AMMONIAC.--The early history of this--ammonium chloride--is also
under a cloud. Pliny (XXXI., 39) speaks of a _sal-hammoniacum_, and
Dioscorides (V., 85) uses much the same word. Pliny describes it as from
near the temple of Ammon in Egypt. None of the distinctive
characteristics of sal-ammoniac are mentioned, and there is every reason
to believe it was either common salt or soda. Herodotus, Strabo, and
others mention common salt sent from about the same locality. The first
authentic mention is in Geber, who calls it _sal-ammoniacum_, and
describes a method of making, and several characteristic reactions. It
was known in the Middle Ages under various names, among them
_sal-aremonicum_. Agricola (_De Nat. Fos._, III., p. 206) notes its
characteristic quality of volatilization. "Sal-ammoniac ... in the fire
neither crackles nor flies out, but is totally consumed." He also says
(p. 208): "Borax is used by goldsmiths to solder gold, likewise silver.
The artificers who make iron needles (tacks?) similarly use sal-ammoniac
when they cover the heads with tin." The statement from Pliny mentioned
in this paragraph is from XXXIII., 29, where he describes the
_chrysocolla_ used as gold solder as made from verdigris, _nitrum_, and
urine in the way quoted. It is quite possible that this solder was
sal-ammoniac, though not made in quite this manner. Pliny refers in
several places (XXXIII., 26, 27, 28, and 29, XXXV., 28, etc.) to
_chrysocolla_, about which he is greatly confused as between
gold-solder, the copper mineral, and a green pigment, the latter being
of either mineral origin.
[9] Saltpetre was secured in the Middle Ages in two ways, but mostly
from the treatment of calcium nitrate efflorescence on cellar and
similar walls, and from so-called saltpetre plantations. In this
description of the latter, one of the most essential factors is omitted
until the last sentence, _i.e._, that the nitrous earth was the result
of the decay of organic or animal matter over a long period. Such
decomposition, in the presence of potassium and calcium carbonates--the
lye and lime--form potassium and calcium nitrates, together with some
magnesium and sodium nitrates. After lixiviation, the addition of lye
converts the calcium and magnesium nitrates into saltpetre, _i.e._,
Ca(NO_{3})_{2} + K_{2}CO_{3} = CaCO_{3} + 2KNO_{3}. The carbonates
precipitate out, leaving the saltpetre in solution, from which it was
evaporated and crystallized out. The addition of alum as mentioned would
scarcely improve the situation.
The purification by repeated re-solution and addition of lye, and
filtration, would eliminate the remaining other salts. The purification
with sulphur, however, is more difficult to understand. In this case the
saltpetre is melted and the sulphur added and set alight. Such an
addition to saltpetre would no doubt burn brilliantly. The potassium
sulphate formed would possibly settle to the bottom, and if the "greasy
matter" were simply organic impurities, they might be burned off. This
method of refining appears to have been copied from Biringuccio (X., 1),
who states it in almost identical terms.
HISTORICAL NOTE.--As mentioned in Note 6 above, it is quite possible
that the Ancients did include efflorescence of walls under _nitrum_;
but, so far as we are aware, no specific mention of such an occurrence
of _nitrum_ is given, and, as stated before, there is every reason to
believe that all the substances under that term were soda and potash.
Especially the frequent mention of the preparation of _nitrum_ by way of
burning, argues strongly against saltpetre being included, as they would
hardly have failed to notice the decrepitation. Argument has been put
forward that Greek fire contained saltpetre, but it amounts to nothing
more than argument, for in those receipts preserved, no salt of any kind
is mentioned. It is most likely that the leprosy of house-walls of the
Mosaic code (Leviticus XIV., 34 to 53) was saltpetre efflorescence. The
drastic treatment by way of destruction of such "unclean" walls and
houses, however, is sufficient evidence that this salt was not used. The
first certain mention of saltpetre (_sal petrae_) is in Geber. As stated
before, the date of this work is uncertain; in any event it was probably
as early as the 13th Century. He describes the making of "solvative
water" with alum and saltpetre, so there can be no doubt as to the
substance (see Note on p. 460, on nitric acid). There is also a work by
a nebulous Marcus Graecus, where the word _sal petrosum_ is used. And it
appears that Roger Bacon (died 1294) and Albertus Magnus (died 1280)
both had access to that work. Bacon uses the term _sal petrae_
frequently enough, and was the first to describe gunpowder (_De Mirabili
Potestate Artis et Naturae_ 1242). He gives no mention of the method of
making his _sal petrae_. Agricola uses throughout the Latin text the
term _halinitrum_, a word he appears to have coined himself. However, he
gives its German equivalent in the _Interpretatio_ as _salpeter_. The
only previous description of the method of making saltpetre, of which we
are aware, is that of Biringuccio (1540), who mentions the boiling of
the excrescences from walls, and also says a good deal about boiling
solutions from "nitrous" earth, which may or may not be of "plantation"
origin. He also gives this same method of refining with sulphur. In any
event, this statement by Agricola is the first clear and complete
description of the saltpetre "plantations." Saltpetre was in great
demand in the Middle Ages for the manufacture of gunpowder, and the
first record of that substance and of explosive weapons necessarily
involves the knowledge of saltpetre. However, authentic mention of such
weapons only begins early in the 14th Century. Among the earliest is an
authority to the Council of Twelve at Florence to appoint persons to
make cannon, etc., (1326), references to cannon in the stores of the
Tower of London, 1388, &c.
[10] There are three methods of manufacturing alum described by
Agricola, the first and third apparently from shales, and the second
from alum rock or "alunite." The reasons for assuming that the first
process was from shales, are the reference to the "aluminous earth" as
ore (_venae_) coming from "veins," and also the mixture of vitriol. In
this process the free sulphuric acid formed by the oxidation of pyrites
reacts upon the argillaceous material to form aluminium sulphate. The
decomposed ore is then placed in tanks and lixiviated. The solution
would contain aluminium sulphate, vitriol, and other impurities. By the
addition of urine, the aluminium sulphate would be converted into
ammonia alum. Agricola is, of course, mistaken as to the effect of the
addition, being under the belief that it separated the vitriol from the
alum; in fact, this belief was general until the latter part of the 18th
Century, when Lavoisier determined that alum must have an alkali base.
Nor is it clear from this description exactly how they were separated.
In a condensed solution allowed to cool, the alum would precipitate out
as "alum meal," and the vitriol would "float on top"--in solution. The
reference to "meal" may represent this phenomenon, and the re-boiling
referred to would be the normal method of purification by
crystallization. The "asbestos" and gypsum deposited in the caldrons
were no doubt feathery and mealy calcium sulphate. The alum produced
would, in any event, be mostly ammonia alum.
The second process is certainly the manufacture from "alum rock" or
"alunite" (the hydrous sulphate of aluminium and potassium), such as
that mined at La Tolfa in the Papal States, where the process has been
for centuries identical with that here described. The alum there
produced is the double basic potassium alum, and crystallizes into cubes
instead of octahedra, _i.e._, the Roman alum of commerce. The presence
of much ferric oxide gives the rose colour referred to by Agricola. This
account is almost identical with that of Biringuccio (II., 4), and it
appears from similarity of details that Agricola, as stated in his
preface, must have "refreshed his mind" from this description; it would
also appear from the preface that he had himself visited the locality.
The third process is essentially the same as the first, except that the
decomposition of the pyrites was hastened by roasting. The following
obscure statement of some interest occurs in Agricola's _De Natura
Fossilium_, p. 209:--"... alum is made from vitriol, for when oil is
made from the latter, alum is distilled out (_expirat_). This absorbs
the clay which is used in cementing glass, and when the operation is
complete the clay is macerated with pure water, and the alum is soon
afterward deposited in the shape of small cubes." Assuming the oil of
vitriol to be sulphuric acid and the clay "used in cementing glass" to
be kaolin, we have here the first suggestion of a method for producing
alum which came into use long after.
"Burnt alum" (_alumen coctum_).--Agricola frequently uses this
expression, and on p. 568, describes the operation, and the substance is
apparently the same as modern dehydrated alum, often referred to as
"burnt alum."
HISTORICAL NOTES.--Whether the Ancients knew of alum in the modern sense
is a most vexed question. The Greeks refer to a certain substance as
_stypteria_, and the Romans refer to this same substance as _alumen_.
There can be no question as to their knowledge and common use of
vitriol, nor that substances which they believed were entirely different
from vitriol were comprised under the above names. Beckmann (Hist. of
Inventions, Vol. I., p. 181) seems to have been the founder of the
doctrine that the ancient _alumen_ was vitriol, and scores of
authorities seem to have adopted his arguments without inquiry, until
that belief is now general. One of the strongest reasons put forward was
that alum does not occur native in appreciable quantities. Apart from
the fact that the weight of this argument has been lost by the discovery
that alum does occur in nature to some extent as an aftermath of
volcanic action, and as an efflorescence from argillaceous rocks, we see
no reason why the Ancients may not have prepared it artificially. One of
the earliest mentions of such a substance is by Herodotus (II., 180) of
a thousand talents of _stypteria_, sent by Amasis from Egypt as a
contribution to the rebuilding of the temple of Delphi. Diodorus (V., 1)
mentions the abundance which was secured from the Lipari Islands
(Stromboli, etc.), and a small quantity from the Isle of Melos.
Dioscorides (V., 82) mentions Egypt, Lipari Islands, Melos, Sardinia,
Armenia, etc., "and generally in any other places where one finds red
ochre (_rubrica_)." Pliny (XXXV., 52) gives these same localities, and
is more explicit as to how it originates--"from an earthy water which
exudes from the earth." Of these localities, the Lipari Islands
(Stromboli, etc.), and Melos are volcanic enough, and both Lipari and
Melos are now known to produce natural alum (Dana. Syst. Min., p. 95;
and Tournefort, "_Relation d'un voyage du Levant_." London, 1717,
_Lettre_ IV., Vol. 1.). Further, the hair-like alum of Dioscorides,
repeated by Pliny below, was quite conceivably fibrous _kalinite_,
native potash alum, which occurs commonly as an efflorescence. Be the
question of native alum as it may--and vitriol is not much more
common--our own view that the ancient _alumen_ was alum, is equally
based upon the artificial product. Before entering upon the subject, we
consider it desirable to set out the properties of the ancient
substance, a complete review of which is given by Pliny (XXXV., 52), he
obviously quoting also from Dioscorides, which, therefore, we do not
need to reproduce. Pliny says:--
"Not less important, or indeed dissimilar, are the uses made of
_alumen_; by which name is understood a sort of salty earth. Of this,
there are several kinds. In Cyprus there is a white _alumen_, and a
darker kind. There is not a great difference in their colour, though the
uses made of them are very dissimilar,--the white _alumen_ being
employed in a liquid state for dyeing wool bright colours, and the
dark-coloured _alumen_, on the other hand, for giving wool a sombre
tint. Gold is purified with black _alumen_. Every kind of _alumen_ is
from a _limus_ water which exudes from the earth. The collection of it
commences in winter, and it is dried by the summer sun. That portion of
it which first matures is the whitest. It is obtained in Spain, Egypt,
Armenia, Macedonia, Pontus, Africa, and the islands of Sardinia, Melos,
Lipari, and Strongyle; the most esteemed, however, is that of Egypt, the
next best from Melos. Of this last there are two kinds, the liquid
_alumen_, and the solid. Liquid _alumen_, to be good, should be of a
limpid and milky appearance; when rubbed, it should be without
roughness, and should give a little heat. This is called _phorimon_. The
mode of detecting whether it has been adulterated is by pomegranate
juice, for, if genuine, the mixture turns black. The other, or solid, is
pale and rough and turns dark with nut-galls; for which reason it is
called _paraphoron_. Liquid _alumen_ is naturally astringent,
indurative, and corrosive; used in combination with honey, it heals
ulcerations.... There is one kind of solid _alumen_, called by the
Greeks _schistos_, which splits into filaments of a whitish colour; for
which reason some prefer calling it _trichitis_ (hair like). _Alumen_ is
produced from the stone _chalcitis_, from which copper is also made,
being a sort of coagulated scum from that stone. This kind of _alumen_
is less astringent than the others, and is less useful as a check upon
bad humours of the body.... The mode of preparing it is to cook it in a
pan until it has ceased being a liquid. There is another variety of
_alumen_ also, of a less active nature, called _strongyle_. It is of two
kinds. The fungous, which easily dissolves, is utterly condemned. The
better kind is the pumice-like kind, full of small holes like a sponge,
and is in round pieces, more nearly white in colour, somewhat greasy,
free from grit, friable, and does not stain black. This last kind is
cooked by itself upon charcoal until it is reduced to pure ashes. The
best kind of all is that called _melinum_, from the Isle of Melos, as I
have said, none being more effectual as an astringent, for staining
black, and for indurating, and none becomes more dry.... Above all other
properties of _alumen_ is its remarkable astringency, whence its Greek
name.... It is injected for dysentry and employed as a gargle." The
lines omitted refer entirely to medical matters which have no bearing
here. The following paragraph (often overlooked) from Pliny (XXXV., 42)
also has an important bearing upon the subject:--"In Egypt they employ a
wonderful method of dyeing. The white cloth, after it is pressed, is
stained in various places, not with dye stuffs, but with substances
which absorb colours. These applications are not apparent on the cloth,
but when it is immersed in a caldron of hot dye it is removed the next
moment brightly coloured. The remarkable circumstance is that although
there be only one dye in the caldron yet different colours appear in the
cloth."
It is obvious from Pliny's description above, and also from the making
of vitriol (see Note 11, p. 572), that this substance was obtained from
liquor resulting from natural or artificial lixiviation of rocks--in the
case of vitriols undoubtedly the result of decomposition of pyritiferous
rocks (such as _chalcitis_). Such liquors are bound to contain aluminum
sulphate if there is any earth or clay about, and whether they contained
alum would be a question of an alkali being present. If no alkali were
present in this liquor, vitriol would crystallize out first, and
subsequent condensation would yield aluminum sulphate. If alkali were
present, the alum would crystallize out either before or with the
vitriol. Pliny's remark, "that portion of it which first matures is
whitest", agrees well enough with this hypothesis. No one will doubt
that some of the properties mentioned above belong peculiarly to
vitriol, but equally convincing are properties and uses that belong to
alum alone. The strongly astringent taste, white colour, and injection
for dysentry, are more peculiar to alum than to vitriol. But above all
other properties is that displayed in dyeing, for certainly if we read
this last quotation from Pliny in conjunction with the statement that
white _alumen_ produces bright colours and the dark kind, sombre
colours, we have the exact reactions of alum and vitriol when used as
mordants. Therefore, our view is that the ancient salt of this character
was a more or less impure mixture ranging from alum to vitriol--"the
whiter the better." Further, considering the ancient knowledge of soda
(_nitrum_), and the habit of mixing it into almost everything, it does
not require much flight of imagination to conceive its admixture to the
"water," and the absolute production of alum.
Whatever may have been the confusion between alum and vitriol among the
Ancients, it appears that by the time of the works attributed to Geber
(12th or 13th Century), the difference was well known. His work
(_Investigationes perfectiones_, IV.) refers to _alumen glaciale_ and
_alumen jameni_ as distinguished from vitriol, and gives characteristic
reactions which can leave no doubt as to the distinction. We may remark
here that the repeated statement apparently arising from Meyer (History
of Chemistry, p. 51) that Geber used the term _alum de rocca_ is untrue,
this term not appearing in the early Latin translations. During the 15th
Century alum did come to be known in Europe as _alum de rocca_. Various
attempts have been made to explain the origin of this term, ranging from
the Italian root, a "rock," to the town of Rocca in Syria, where alum
was supposed to have been produced. In any event, the supply for a long
period prior to the middle of the 15th Century came from Turkey, and the
origin of the methods of manufacture described by Agricola, and used
down to the present day, must have come from the Orient.
In the early part of the 15th Century, a large trade in alum was done
between Italy and Asia Minor, and eventually various Italians
established themselves near Constantinople and Smyrna for its
manufacture (Dudae, _Historia Byzantina Venetia_, 1729, p. 71). The alum
was secured by burning the rock, and lixiviation. With the capture of
Constantinople by the Turks (1453), great feeling grew up in Italy over
the necessity of buying this requisite for their dyeing establishments
from the infidel, and considerable exertion was made to find other
sources of supply. Some minor works were attempted, but nothing much
eventuated until the appearance of one John de Castro. From the
Commentaries of Pope Pius II. (1614, p. 185), it appears that this
Italian had been engaged in dyeing cloth in Constantinople, and thus
became aware of the methods of making alum. Driven out of that city
through its capture by the Turks, he returned to Italy and obtained an
office under the Apostolic Chamber. While in this occupation he
discovered a rock at Tolfa which appeared to him identical with that
used at Constantinople in alum manufacture. After experimental work, he
sought the aid of the Pope, which he obtained after much vicissitude.
Experts were sent, who after examination "shed tears of joy, they
kneeling down three times, worshipped God and praised His kindness in
conferring such a gift on their age." Castro was rewarded, and the great
papal monopoly was gradually built upon this discovery. The industry
firmly established at Tolfa exists to the present day, and is the source
of the Roman alum of commerce. The Pope maintained this monopoly
strenuously, by fair means and by excommunication, gradually advancing
the price until the consumers had greater complaint than against the
Turks. The history of the disputes arising over the papal alum monopoly
would alone fill a volume.
By the middle of the 15th Century alum was being made in Spain, Holland,
and Germany, and later in England. In her efforts to encourage home
industries and escape the tribute to the Pope, Elizabeth (see Note on p.
283) invited over "certain foreign chymistes and mineral masters" and
gave them special grants to induce them to "settle in these realmes."
Among them was Cornelius Devoz, to whom was granted the privilege of
"mining and digging in our Realm of England for allom and copperas."
What Devoz accomplished is not recorded, but the first alum manufacture
on a considerable scale seems to have been in Yorkshire, by one Thomas
Chaloner (about 1608), who was supposed to have seduced workmen from the
Pope's alum works at Tolfa, for which he was duly cursed with all the
weight of the Pope and Church. (Pennant, Tour of Scotland, 1786).
[11] The term for vitriol used by the Roman authors, followed by
Agricola, is _atramentum sutorium_, literally shoemaker's blacking, the
term no doubt arising from its ancient (and modern) use for blackening
leather. The Greek term was _chalcanthon_. The term "vitriol" seems
first to appear in Albertus Magnus (_De Mineralibus_, _Liber_ V.), who
died in 1280, where he uses the expression "_atramentum viride a
quibusdam vitreolum vocatur_." Agricola (_De Nat. Foss._, p. 213)
states, "In recent years the name _vitriolum_ has been given to it." The
first adequate description of vitriol is by Dioscorides (V., 76), as
follows:--"Vitriol (_chalcanthon_) is of one genus, and is a solidified
liquid, but it has three different species. One is formed from the
liquids which trickle down drop by drop and congeal in certain mines;
therefore those who work in the Cyprian mines call it _stalactis_.
Petesius calls this kind _pinarion_. The second kind is that which
collects in certain caverns; afterward it is poured into trenches, where
it congeals, whence it derives its name _pectos_. The third kind is
called _hephthon_ and is mostly made in Spain; it has a beautiful colour
but is weak. The manner of preparing it is as follows: dissolving it in
water, they boil it, and then they transfer it to cisterns and leave it
to settle. After a certain number of days it congeals and separates into
many small pieces, having the form of dice, which stick together like
grapes. The most valued is blue, heavy, dense, and translucent." Pliny
(XXXIV., 32) says:--"By the name which they have given to it, the Greeks
indicate the similar nature of copper and _atramentum sutorium_, for
they call it _chalcanthon_. There is no substance of an equally
miraculous nature. It is made in Spain from wells of this kind of water.
This water is boiled with an equal quantity of pure water, and is then
poured into wooden tanks (fish ponds). Across these tanks there are
fixed beams, to which hang cords stretched by little stones. Upon these
cords adheres the _limus_ (Agricola's 'juice') in drops of a vitreous
appearance, somewhat resembling a bunch of grapes. After removal, it is
dried for thirty days. It is of a blue colour, and of a brilliant
lustre, and is very like glass. Its solution is the blacking used for
colouring leather. _Chalcanthon_ is made in many other ways: its kind of
earth is sometimes dug from ditches, from the sides of which exude
drops, which solidify by the winter frosts into icicles, called
_stalagmia_, and there is none more pure. When its colour is nearly
white, with a slight tinge of violet, it is called _leukoion_. It is
also made in rock basins, the rain water collecting the _limus_ into
them, where it becomes hardened. It is also made in the same way as salt
by the intense heat of the sun. Hence it is that some distinguish two
kinds, the mineral and the artificial; the latter being paler than the
former and as much inferior to it in quality as it is in colour."
While Pliny gives prominence to blue vitriol, his solution for colouring
leather must have been the iron sulphate. There can be no doubt from the
above, however, that both iron and copper sulphates were known to the
Ancients. From the methods for making vitriol given here in _De Re
Metallica_, it is evident that only the iron sulphate would be produced,
for the introduction of iron strips into the vats would effectually
precipitate any copper. It is our belief that generally throughout this
work, the iron sulphate is meant by the term _atramentum sutorium_. In
_De Natura Fossilium_ (p. 213-15) Agricola gives three varieties of
_atramentum sutorium_,--_viride_, _caeruleum_, and _candidum_, _i.e._,
green, blue, and white. Thus the first mention of white vitriol (zinc
sulphate) appears to be due to him, and he states further (p. 213): "A
white sort is found, especially at Goslar, in the shape of icicles,
transparent like crystals." And on p. 215: "Since I have explained the
nature of vitriol and its relatives, which are obtained from cupriferous
pyrites, I will next speak of an acrid solidified juice which commonly
comes from _cadmia_. It is found at Annaberg in the tunnel driven to the
Saint Otto mine; it is hard and white, and so acrid that it kills mice,
crickets, and every kind of animal. However, that feathery substance
which oozes out from the mountain rocks and the thick substance found
hanging in tunnels and caves from which saltpetre is made, while
frequently acrid, does not come from _cadmia_." Dana (Syst. of Min., p.
939) identifies this as _Goslarite_--native zinc sulphate. It does not
appear, however, that artificial zinc vitriol was made in Agricola's
time. Schlueter (_Huette-Werken_, Braunschweig 1738, p. 597) states it to
have been made for the first time at Rammelsberg about 1570.
It is desirable here to enquire into the nature of the substances given
by all of the old mineralogists under the Latinized Greek terms
_chalcitis_, _misy_, _sory_, and _melanteria_. The first mention of
these minerals is in Dioscorides, who (V., 75-77) says: "The best
_chalcitis_ is like copper. It is friable, not stony, and is intersected
by long brilliant veins.... _Misy_ is obtained from Cyprus; it should
have the appearance of gold, be hard, and when pulverised it should have
the colour of gold and sparkle like stars. It has the same properties as
_chalcitis_.... The best is from Egypt.... One kind of _melanteria_
congeals like salt in the entries to copper mines. The other kind is
earthy and appears on the surface of the aforesaid mines. It is found in
the mines of Cilicia and other regions. The best has the colour of
sulphur, is smooth, pure, homogenous, and upon contact with water
immediately becomes black.... Those who consider _sory_ to be the same
as _melanteria_, err greatly. _Sory_ is a species of its own, though it
is not dissimilar. The smell of _sory_ is oppressive and provokes
nausea. It is found in Egypt and in other regions, as Libya, Spain, and
Cyprus. The best is from Egypt, and when broken is black, porous,
greasy, and astringent." Pliny (XXXIV., 29-31) says:--"That is called
_chalcitis_ from which, as well as itself copper (?) is extracted by
heat. It differs from _cadmia_ in that this is obtained from rocks near
the surface, while that is taken from rocks below the surface. Also
_chalcitis_ is immediately friable, being naturally so soft as to appear
like compressed wool. There is also this other distinction; _chalcitis_
contains three other substances, copper, _misy_, and _sory_. Of each of
these we shall speak in their appropriate places. It contains elongated
copper veins. The most approved kind is of the colour of honey; it is
streaked with fine sinuous veins and is friable and not stony. It is
considered most valuable when fresh.... The _sory_ of Egypt is the most
esteemed, being much superior to that of Cyprus, Spain, and Africa;
although some prefer the _sory_ from Cyprus for affections of the eyes.
But from whatever nation it comes, the best is that which has the
strongest odour, and which, when ground up, becomes greasy, black, and
spongy. It is a substance so unpleasant to the stomach that some persons
are nauseated by its smell. Some say that _misy_ is made by the burning
of stones in trenches, its fine yellow powder being mixed with the ashes
of pine-wood. The truth is, as I said above, that though obtained from
the stone, it is already made and in solid masses, which require force
to detach them. The best comes from the works of Cyprus, its
characteristics being that when broken it sparkles like gold, and when
ground it presents a sandy appearance, but on the contrary, if heated,
it is similar to _chalcitis_. _Misy_ is used in refining gold...."
Agricola's views on the subject appear in _De Natura Fossilium_. He says
(p. 212):--"The cupriferous pyrites (_pyrites aerosus_) called
_chalcitis_ is the mother and cause of _sory_--which is likewise known
as mine _vitriol_ (_atramentum metallicum_)--and _melanteria_. These in
turn yield vitriol and such related things. This may be seen especially
at Goslar, where the nodular lumps of dark grey colour are called
vitriol stone (_lapis atramenti_). In the centre of them is found
greyish pyrites, almost dissolved, the size of a walnut. It is enclosed
on all sides, sometimes by _sory_, sometimes by _melanteria_. From them
start little veinlets of greenish vitriol which spread all over it,
presenting somewhat the appearance of hairs extending in all directions
and cohering together.... There are five species of this solidified
juice, _melanteria_, _sory_, _chalcitis_, _misy_, and vitriol. Sometimes
many are found in one place, sometimes all of them, for one originates
from the other. From pyrites, which is, as one might say, the root of
all these juices, originates the above-mentioned _sory_ and
_melanteria_. From _sory_, _chalcitis_, and _melanteria_ originate the
various kinds of vitriol.... _Sory_, _melanteria_, _chalcitis_, and
_misy_ are always native; vitriol alone is either native or artificial.
From them vitriol effloresces white, and sometimes green or blue. _Misy_
effloresces not only from _sory_, _melanteria_, and _chalcitis_, but
also from all the vitriols, artificial as well as natural.... _Sory_ and
_melanteria_ differ somewhat from the others, but they are of the same
colours, grey and black; but _chalcitis_ is red and copper-coloured;
_misy_ is yellow or gold-coloured. All these native varieties have the
odour of lightning (brimstone), but _sory_ is the most powerful. The
feathery vitriol is soft and fine and hair-like, and _melanteria_ has
the appearance of wool and it has a similarity to salt; all these are
rare and light; _sory_, _chalcitis_, and _misy_ have the following
relations. _Sory_ because of its density has the hardness of stone,
although its texture is very coarse. _Misy_ has a very fine texture.
_Chalcitis_ is between the two; because of its roughness and strong
odour it differs from _melanteria_, although they do not differ in
colour. The vitriols, whether natural or artificial, are hard and dense
... as regarding shape, _sory_, _chalcitis_, _misy_, and _melanteria_
are nodular, but _sory_ is occasionally porous, which is peculiar to it.
_Misy_ when it effloresces in no great quantity from the others is like
a kind of pollen, otherwise it is nodular. _Melanteria_ sometimes
resembles wool, sometimes salt."
The sum and substance, therefore, appears to be that _misy_ is a
yellowish material, possibly ochre, and _sory_ a blackish stone, both
impregnated with vitriol. _Chalcitis_ is a partially decomposed pyrites;
and _melanteria_ is no doubt native vitriol. From this last term comes
the modern _melanterite_, native hydrous ferrous sulphate. Dana (System
of Mineralogy, p. 964) considers _misy_ to be in part _copiapite_--basic
ferric sulphate--but any such part would not come under Agricola's
objection to it as a source of vitriol. The disabilities of this and
_chalcitis_ may, however, be due to their copper content.
[12] Agricola (_De Nat. Fos._, 221) says:--"There is a species of
artificial sulphur made from sulphur and iron hammer-scales, melted
together and poured into moulds. This, because it heals scabs of horses,
is generally called _caballinum_." It is difficult to believe such a
combination was other than iron sulphide, but it is equally difficult to
understand how it was serviceable for this purpose.
[13] Inasmuch as pyrites is discussed in the next paragraph, the
material of the first distillation appears to be native sulphur. Until
the receiving pots became heated above the melting point of the sulphur,
the product would be "flowers of sulphur," and not the wax-like product.
The equipment described for pyrites in the next paragraph would be
obviously useful only for coarse material.
But little can be said on the history of sulphur; it is mentioned often
enough in the Bible and also by Homer (Od. XXII., 481). The Greeks
apparently knew how to refine it, although neither Dioscorides nor Pliny
specifically describes such an operation. Agricola says (_De Nat. Fos._,
220): "Sulphur is of two kinds; the mineral, which the Latins call
_vivum_, and the Greeks _apyron_, which means 'not exposed to the fire'
(_ignem non expertum_) as rightly interpreted by Celsius; and the
artificial, called by the Greeks _pepyromenon_, that is, 'exposed to the
fire.'" In Book X., the expression _sulfur ignem non expertum_
frequently appears, no doubt in Agricola's mind for native sulphur,
although it is quite possible that the Greek distinction was between
"flowers" of sulphur and the "wax-like" variety.
[14] The substances referred to under the names _bitumen_, _asphalt_,
_maltha_, _naphtha_, _petroleum_, _rock-oil_, etc., have been known and
used from most ancient times, and much of our modern nomenclature is of
actual Greek and Roman ancestry. These peoples distinguished three
related substances,--the Greek _asphaltos_ and Roman _bitumen_ for the
hard material,--Greek _pissasphaltos_ and Roman _maltha_ for the
viscous, pitchy variety--and occasionally the Greek _naphtha_ and Roman
_naphtha_ for petroleum proper, although it is often enough referred to
as liquid _bitumen_ or liquid _asphaltos_. The term _petroleum_
apparently first appears in Agricola's _De Natura Fossilium_ (p. 222),
where he says the "oil of bitumen ... now called _petroleum_." Bitumen
was used by the Egyptians for embalming from pre-historic times, _i.e._,
prior to 5000 B.C., the term "mummy" arising from the Persian word for
bitumen, _mumiai_. It is mentioned in the tribute from Babylonia to
Thotmes III., who lived about 1500 B.C. (Wilkinson, Ancient Egyptians
I., p. 397). The Egyptians, however, did not need to go further afield
than the Sinai Peninsula for abundant supplies. Bitumen is often cited
as the real meaning of the "slime" mentioned in Genesis (XI., 3; XIV.,
10), and used in building the Tower of Babel. There is no particular
reason for this assumption, except the general association of Babel,
Babylon, and Bitumen. However, the Hebrew word _sift_ for pitch or
bitumen does occur as the cement used for Moses's bulrush cradle (Exodus
II., 3), and Moses is generally accounted about 1300 B.C. Other attempts
to connect Biblical reference to petroleum and bitumen revolve around
Job XXIX., 6, Deut. XXXII., 13, Maccabees II., I, 18, Matthew V., 13,
but all require an unnecessary strain on the imagination.
The plentiful occurrence of bitumen throughout Asia Minor, and
particularly in the Valley of the Euphrates and in Persia, is the
subject of innumerable references by writers from Herodotus (484-424
B.C.) down to the author of the company prospectus of recent months.
Herodotus (I., 179) and Diodorus Siculus (I) state that the walls of
Babylon were mortared with bitumen--a fact partially corroborated by
modern investigation. The following statement by Herodotus (VI., 119) is
probably the source from which Pliny drew the information which Agricola
quotes above. In referring to a well at Ardericca, a place about 40
miles from ancient Susa, in Persia, Herodotus says:--"For from the well
they get bitumen, salt, and oil, procuring it in the way that I will now
describe: they draw with a swipe, and instead of a bucket they make use
of the half of a wine-skin; with this the man dips and, after drawing,
pours the liquid into a reservoir, wherefrom it passes into another, and
there takes three different shapes. The salt and bitumen forthwith
collect and harden, while the oil is drawn off into casks. It is called
by the Persians _rhadinace_, is black, and has an unpleasant smell."
(Rawlinson's Trans. III., p. 409). The statement from Pliny (XXXI., 39)
here referred to by Agricola, reads:--"It (salt) is made from water of
wells poured into salt-pans. At Babylon the first condensed is a
bituminous liquid like oil which is burned in lamps. When this is taken
off, salt is found beneath. In Cappadocia also the water from both wells
and springs is poured into salt-pans." When petroleum began to be used
as an illuminant it is impossible to say. A passage in Aristotle's _De
Mirabilibus_ (127) is often quoted, but in reality it refers only to a
burning spring, a phenomenon noted by many writers, but from which to
its practical use is not a great step. The first really definite
statement as to the use of petroleum as an illuminant is Strabo's
quotation (XVI., 1, 15) from Posidonius: "Asphaltus is found in great
abundance in Babylonia. Eratosthenes describes it as follows:--The
liquid _asphaltus_, which is called _naphtha_, is found in Susa; the dry
kind, which can be made solid, in Babylonia. There is a spring of it
near the Euphrates.... Others say that the liquid kind is also found in
Babylonia.... The liquid kind, called _naphtha_, is of a singular
nature. When it is brought near the fire, the fire catches it....
Posidonius says that there are springs of _naphtha_ in Babylonia, some
of which produce white, others black _naphtha_; the first of these, I
mean white _naphtha_, which attracts flame, is liquid sulphur; the
second or black _naphtha_ is liquid _asphaltus_, and is burnt in lamps
instead of oil." (Hamilton's Translation, Vol. III., p. 151).
Eratosthenes lived about 200 B.C., and Posidonius about 100 years later.
Dioscorides (I., 83), after discussing the usual sources of bitumen
says: "It is found in a liquid state in Agrigentum in Sicily, flowing on
streams; they use it for lights in lanterns in place of oil. Those who
call the Sicilian kind oil are under a delusion, for it is agreed that
it is a kind of liquid bitumen." Pliny adds nothing much new to the
above quotations, except in regard to these same springs (XXXV., 51)
that "The inhabitants collect it on the panicles of reeds, to which it
quickly adheres and they use it for burning in lamps instead of oil."
Agricola (_De Natura Fossilium_, Book IV.) classifies petroleum, coal,
jet, and obsidian, camphor, and amber as varieties of bitumen, and
devotes much space to the refutation of the claims that the last two are
of vegetable origin.
[15] Agricola (_De Natura Fossilium_, p. 215) in discussing substances
which originate from copper, gives among them green _chrysocolla_ (as
distinguished from borax, etc., see Note 8 above), and says: "Native
_chrysocolla_ originates in veins and veinlets, and is found mostly by
itself like sand, or adhering to metallic substances, and when scraped
off from this appears similar to its own sand. Occasionally it is so
thin that very little can be scraped off. Or else it occurs in waters
which, as I have said, wash these minerals, and afterward it settles as
a powder. At Neusohl in the Carpathians, green water flowing from an
ancient tunnel wears away this _chrysocolla_ with it. The water is
collected in thirty large reservoirs, where it deposits the
_chrysocolla_ as a sediment, which they collect every year and
sell,"--as a pigment. This description of its occurrence would apply
equally well to modern _chrysocolla_ or to malachite. The solution from
copper ores would deposit some sort of green incrustation, of carbonates
mostly.
[16] The statement in Pliny (XXXVI., 66) to which Agricola refers is as
follows: "Then as ingenuity was not content with the mixing of _nitrum_,
they began the addition of _lapis magnes_, because of the belief that it
attracts liquefied glass as well as iron. In a similar manner many kinds
of brilliant stones began to be added to the melting, and then shells
and fossil sand. Authors tell us that the glass of India is made of
broken crystal, and in consequence nothing can compare with it. Light
and dry wood is used for fusing, _cyprium_ (copper?) and _nitrum_ being
added, particularly _nitrum_ from Ophir etc."
A great deal of discussion has arisen over this passage, in connection
with what this _lapis magnes_ really was. Pliny (XXXVI., 25) describes
the lodestone under this term, but also says: "There (in Ethiopia) also
is _haematites magnes_, a stone of blood colour, which shows a red
colour if crushed, or of saffron. The _haematites_ has not the same
property of attracting iron as _magnes_." Relying upon this sentence for
an exception to the ordinary sort of _magnes_, and upon the impossible
chemical reaction involved, most commentators have endeavoured to show
that lodestone was not the substance meant by Pliny, but manganese, and
thus they find here the first knowledge of this mineral. There can be
little doubt that Pliny assumed it to be the lodestone, and Agricola
also. Whether the latter had any independent knowledge on this point in
glass-making or was merely quoting Pliny--which seems probable--we do
not know. In any event, Biringuccio, whose work preceded _De Re
Metallica_ by fifteen years, does definitely mention manganese in this
connection. He dismisses this statement of Pliny with the remark (p.
37-38): "The Ancients wrote about lodestones, as Pliny states, and they
mixed it together with _nitrum_ in their first efforts to make glass."
The following passage from this author (p. 36-37), however, is not only
of interest in this connection, but also as possibly being the first
specific mention of manganese under its own name. Moreover, it has been
generally overlooked in the many discussions of the subject. "Of a
similar nature (to _zaffir_) is also another mineral called _manganese_,
which is found, besides in Germany, at the mountain of Viterbo in
Tuscany ... it is the colour of _ferrigno scuro_ (iron slag?). In
melting it one cannot obtain any metal ... but it gives a very fine
colour to glass, so that the glass workers use it in their pigments to
secure an azure colour.... It also has such a property that when put
into melted glass it cleanses it and makes it white, even if it were
green or yellow. In a hot fire it goes off in a vapour like lead, and
turns into ashes."
To enter competently into the discussion of the early history of
glass-making would employ more space than can be given, and would lead
but to a sterile end. It is certain that the art was pre-Grecian, and
that the Egyptians were possessed of some knowledge of making and
blowing it in the XI Dynasty (according to Petrie 3,500 B.C.), the wall
painting at Beni Hassen, which represents glass-blowing, being
attributed to that period. The remains of a glass factory at Tel el
Amarna are believed to be of the XVIII Dynasty. (Petrie, 1,500 B.C.).
The art reached a very high state of development among the Greeks and
Romans. No discussion of this subject omits Pliny's well-known story
(XXXVI, 65), which we also add: "The tradition is that a merchant ship
laden with _nitrum_ being moored at this place, the merchants were
preparing their meal on the beach, and not having stones to prop up
their pots, they used lumps of _nitrum_ from the ship, which fused and
mixed with the sands of the shore, and there flowed streams of a new
translucent liquid, and thus was the origin of glass."
APPENDIX A.
AGRICOLA'S WORKS.
Georgius Agricola was not only the author of works on Mining and allied
subjects, usually associated with his name, but he also interested
himself to some extent in political and religious subjects. For
convenience in discussion we may, therefore, divide his writings on the
broad lines of (1) works on mining, geology, mineralogy, and allied
subjects; (2) works on other subjects, medical, religious, critical,
political, and historical. In respect especially to the first division,
and partially with regard to the others, we find three principal cases:
(_a_) Works which can be authenticated in European libraries to-day;
(_b_) references to editions of these in bibliographies, catalogues,
etc., which we have been unable to authenticate; and (_c_) references to
works either unpublished or lost. The following are the short titles of
all of the published works which we have been able to find on the
subjects allied to mining, arranged according to their present
importance:--_De Re Metallica_, first edition, 1556; _De Natura
Fossilium_, first edition, 1546; _De Ortu et Causis Subterraneorum_,
first edition, 1546; _Bermannus_, first edition, 1530; _Rerum
Metallicarum Interpretatio_, first edition, 1546; _De Mensuris et
Ponderibus_, first edition, 1533; _De Precio Metallorum et Monetis_,
first edition, 1550; _De Veteribus et Novis Metallis_, first edition,
1546; _De Natura eorum quae Effluunt ex Terra_, first edition, 1546; _De
Animantibus Subterraneis_, first edition, 1549.
Of the "lost" or unpublished works, on which there is some evidence, the
following are the most important:--_De Metallicis et Machinis_, _De Ortu
Metallorum Defensio ad Jacobum Scheckium_, _De Jure et Legibus
Metallicis_, _De Varia Temperie sive Constitutione Aeris_, _De Terrae
Motu_, and _Commentariorum, Libri VI_.
The known published works upon other subjects are as follows:--Latin
Grammar, first edition, 1520; Two Religious Tracts, first edition, 1522;
_Galen_ (Joint Revision of Greek Text), first edition, 1525; _De Bello
adversus Turcam_, first edition, 1528; _De Peste_, first edition, 1554.
The lost or partially completed works on subjects unrelated to mining,
of which some trace has been found, are:--_De Medicatis Fontibus_, _De
Putredine solidas partes_, etc., _Castigationes in Hippocratem_,
_Typographia Mysnae et Toringiae_, _De Traditionibus Apostolicis_,
_Oratio de rebus gestis Ernesti et Alberti_, _Ducum Saxoniae_.
REVIEW OF PRINCIPAL WORKS.
Before proceeding with the bibliographical detail, we consider it
desirable to review briefly the most important of the author's works on
subjects related to mining.
_De Natura Fossilium._ This is the most important work of Agricola,
excepting _De Re Metallica_. It has always been printed in combination
with other works, and first appeared at Basel, 1546. This edition was
considerably revised by the author, the amended edition being that of
1558, which we have used in giving references. The work comprises ten
"books" of a total of 217 folio pages. It is the first attempt at
systematic mineralogy, the minerals[1] being classified into (1)
"earths" (clay, ochre, etc.), (2) "stones properly so-called" (gems,
semi-precious and unusual stones, as distinguished from rocks), (3)
"solidified juices" (salt, vitriol, alum, etc.), (4) metals, and (5)
"compounds" (homogeneous "mixtures" of simple substances, thus forming
such minerals as galena, pyrite, etc.). In this classification Agricola
endeavoured to find some fundamental basis, and therefore adopted
solubility, fusibility, odour, taste, etc., but any true classification
without the atomic theory was, of course, impossible. However, he makes
a very creditable performance out of their properties and obvious
characteristics. All of the external characteristics which we use to-day
in discrimination, such as colour, hardness, lustre, etc., are
enumerated, the origin of these being attributed to the proportions of
the Peripatetic elements and their binary properties. Dana, in his great
work[2], among some fourscore minerals which he identifies as having
been described by Agricola and his predecessors, accredits a score to
Agricola himself. It is our belief, however, that although in a few
cases Agricola has been wrongly credited, there are still more of which
priority in description might be assigned to him. While a greater number
than fourscore of so-called species are given by Agricola and his
predecessors, many of these are, in our modern system, but varieties;
for instance, some eight or ten of the ancient species consist of one
form or another of silica.
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