Agricola, Georgius, De re metallica, 1912/1950

Table of figures

< >
[Figure 161]
[Figure 162]
[Figure 163]
[Figure 164]
[Figure 165]
[Figure 166]
[Figure 167]
[Figure 168]
[Figure 169]
[Figure 170]
[Figure 171]
[Figure 172]
[Figure 173]
[Figure 174]
[Figure 175]
[Figure 176]
[Figure 177]
[Figure 178]
[Figure 179]
[Figure 180]
[Figure 181]
[Figure 182]
[Figure 183]
[Figure 184]
[Figure 185]
[Figure 186]
[Figure 187]
[Figure 188]
[Figure 189]
[Figure 190]
< >
page |< < of 679 > >|
1
Lastly, the seams, which are the very finest stringers (fibrae), divide
the rock, and occur sometimes frequently, sometimes rarely.
From
whatever direction the vein comes, its seams always turn their heads
toward the light in the same direction.
But, while the seams usually run
from one point of the compass to another immediately opposite it, as
for instance, from east to west, if hard stringers divert them, it may
happen that these very seams, which before were running from east to
west, then contrariwise proceed from west to east, and the direction of
the rocks is thus inverted.
In such a case, the direction of the veins is
judged, not by the direction of the seams which occur rarely, but by those
which constantly recur.
40[Figure 40]
A—SEAMS WHICH PROCEED FROM THE EAST. B—THE INVERSE.
Both veins or stringers may be solid or drusy, or barren of minerals,
or pervious to water.
Solid veins contain no water and very little air. The
drusy veins rarely contain water; they often contain air.
Those which
are barren of minerals often carry water.
Solid veins and stringers con­
sist sometimes of hard materials, sometimes of soft, and sometimes of a
kind of medium between the two.

Text layer

  • Dictionary
  • Places

Text normalization

  • Original

Search


  • Exact
  • All forms
  • Fulltext index
  • Morphological index