Agricola, Georgius
,
De re metallica
,
1912/1950
Text
Text Image
Image
XML
Thumbnail overview
Document information
None
Concordance
Figures
Thumbnails
List of thumbnails
<
1 - 10
11 - 20
21 - 30
31 - 40
41 - 50
51 - 60
61 - 70
71 - 80
81 - 90
91 - 100
101 - 110
111 - 120
121 - 130
131 - 140
141 - 150
151 - 160
161 - 170
171 - 180
181 - 190
191 - 200
201 - 210
211 - 220
221 - 230
231 - 240
241 - 250
251 - 260
261 - 270
271 - 280
281 - 290
291 - 300
301 - 310
311 - 320
321 - 330
331 - 340
341 - 350
351 - 360
361 - 370
371 - 380
381 - 390
391 - 400
401 - 410
411 - 420
421 - 430
431 - 440
441 - 450
451 - 460
461 - 470
471 - 480
481 - 490
491 - 500
501 - 510
511 - 520
521 - 530
531 - 540
541 - 550
551 - 560
561 - 570
571 - 580
581 - 590
591 - 600
601 - 610
611 - 620
621 - 630
631 - 640
641 - 650
651 - 660
661 - 670
671 - 679
>
161
162
163
164
165
166
167
168
169
170
<
1 - 10
11 - 20
21 - 30
31 - 40
41 - 50
51 - 60
61 - 70
71 - 80
81 - 90
91 - 100
101 - 110
111 - 120
121 - 130
131 - 140
141 - 150
151 - 160
161 - 170
171 - 180
181 - 190
191 - 200
201 - 210
211 - 220
221 - 230
231 - 240
241 - 250
251 - 260
261 - 270
271 - 280
281 - 290
291 - 300
301 - 310
311 - 320
321 - 330
331 - 340
341 - 350
351 - 360
361 - 370
371 - 380
381 - 390
391 - 400
401 - 410
411 - 420
421 - 430
431 - 440
441 - 450
451 - 460
461 - 470
471 - 480
481 - 490
491 - 500
501 - 510
511 - 520
521 - 530
531 - 540
541 - 550
551 - 560
561 - 570
571 - 580
581 - 590
591 - 600
601 - 610
611 - 620
621 - 630
631 - 640
641 - 650
651 - 660
661 - 670
671 - 679
>
page
|<
<
of 679
>
>|
<
archimedes
>
<
text
>
<
body
>
<
chap
>
<
p
type
="
main
">
<
s
>
<
pb
pagenum
="
126
"/>
for a distance of several fathoms, then from the upper part of tunnels or even
<
lb
/>
drifts that have already been driven, other drifts are driven again
<
lb
/>
and again until that part of the vein is reached which does not yield metal.
<
lb
/>
</
s
>
<
s
>The timbering of these openings is done as follows: stulls are set at
<
lb
/>
intervals into hitches in the hanging and footwall, and upon them
<
lb
/>
smooth poles are laid continuously; and that they may be able to
<
lb
/>
bear the weight, the stulls are generally a foot and a half thick. </
s
>
<
s
>After the
<
lb
/>
ore has been taken out and the mining of the vein is being done elsewhere,
<
lb
/>
the rock then broken, especially if it cannot be taken away without great
<
lb
/>
difficulty, is thrown into these openings among the timber, and the carriers
<
lb
/>
of the ore are saved toil, and the owners save half the expense. </
s
>
<
s
>This then,
<
lb
/>
generally speaking, is the method by which everything relating to the
<
lb
/>
timbering of shafts, tunnels, and drifts is carried out.</
s
>
</
p
>
<
p
type
="
main
">
<
s
>All that I have hitherto written is in part peculiar to
<
emph
type
="
italics
"/>
venae profundae,
<
emph.end
type
="
italics
"/>
<
lb
/>
and in part common to all kinds of veins; of what follows, part is specially
<
lb
/>
applicable to
<
emph
type
="
italics
"/>
venae dilatatae,
<
emph.end
type
="
italics
"/>
part to
<
emph
type
="
italics
"/>
venae cumulatae.
<
emph.end
type
="
italics
"/>
</
s
>
<
s
> But first I will
<
lb
/>
describe how
<
emph
type
="
italics
"/>
venae dilatatae
<
emph.end
type
="
italics
"/>
should be mined. </
s
>
<
s
>Where torrents, rivers, or
<
lb
/>
streams have by inundations washed away part of the slope of a mountain or
<
lb
/>
a hill, and have disclosed a
<
emph
type
="
italics
"/>
vena dilatata,
<
emph.end
type
="
italics
"/>
a tunnel should be driven first straight
<
lb
/>
and narrow, and then wider, for nearly all the vein should be hewn away; and
<
lb
/>
when this tunnel has been driven further, a shaft which supplies air should be
<
lb
/>
sunk in the mountain or hill, and through it from time to time the ore, earth,
<
lb
/>
and rock can be drawn up at less expense than if they be drawn out through the
<
lb
/>
very great length of the tunnel; and even in those places to which the tunnel
<
lb
/>
does not yet reach, miners dig shafts in order to open a
<
emph
type
="
italics
"/>
vena dilatata
<
emph.end
type
="
italics
"/>
which
<
lb
/>
they conjecture must lie beneath the soil. </
s
>
<
s
>In this way, when the upper
<
lb
/>
layers are removed, they dig through rock sometimes of one kind and colour,
<
lb
/>
sometimes of one kind but different colours, sometimes of different kinds but
<
lb
/>
of one colour, and, lastly, of different kinds and different colours. </
s
>
<
s
>The thickness
<
lb
/>
of rock, both of each single stratum and of all combined, is uncertain, for
<
lb
/>
the whole of the strata are in some places twenty fathoms deep, in others
<
lb
/>
more than fifty; individual strata are in some places half a foot thick; in others,
<
lb
/>
one, two, or more feet; in others, one, two, three, or more fathoms. </
s
>
<
s
>For
<
lb
/>
example, in those districts which lie at the foot of the Harz mountains,
<
lb
/>
there are many different coloured strata, covering a copper
<
emph
type
="
italics
"/>
vena dilatata.
<
emph.end
type
="
italics
"/>
<
lb
/>
When the soil has been stripped, first of all is disclosed a stratum which
<
lb
/>
is red, but of a dull shade and of a thickness of twenty, thirty, or five and
<
lb
/>
thirty fathoms. </
s
>
<
s
>Then there is another stratum, also red, but of a light
<
lb
/>
shade, which has usually a thickness of about two fathoms. </
s
>
<
s
>Beneath this is a
<
lb
/>
stratum of ash-coloured clay nearly a fathom thick, which, although it is
<
lb
/>
not metalliferous, is reckoned a vein. </
s
>
<
s
>Then follows a third stratum,
<
lb
/>
which is ashy, and about three fathoms thick. </
s
>
<
s
>Beneath this lies a vein
<
lb
/>
of ashes to the thickness of five fathoms, and these ashes are mixed with
<
lb
/>
rock of the same colour. </
s
>
<
s
>Joined to the last, and underneath, comes a
<
lb
/>
stratum, the fourth in number, dark in colour and a foot thick. </
s
>
<
s
>Under this
<
lb
/>
comes the fifth stratum, of a pale or yellowish colour, two feet thick; under-</
s
>
</
p
>
</
chap
>
</
body
>
</
text
>
</
archimedes
>