The Anaconda standard. [volume] (Anaconda, Mont.) 1889-1970, 1899-09-15
e width of the vertical vein is so

the width of the vertical vein is 80
feet.
The witness said that there are some
segments of veins, having an easterly
and westerly strike and southerly dlp,
between the vertical and fiat veins he
gave their relative distances from one
another, and from the fiat and vertical
veins, north and SOUTH on the 600 level
The witness said that he thought
there is only one large ore body dis
closed in the 900 level workings between
the faults.
rs it true that when the mineraliza-
ton of the east and west veins occur
red the mineral solutions spread out on
either side of the veins so that all
the ground became mineralized?' asked
Mr.. Hughes.
Yes, l think that is the case to a
large extent" answered the witness.
The witness did not know whether
the slopes between the faults on some
levels of the mine had been left out
of the model. As to the other levels,
he testified that some slopes had been
omitted. He described the slopes that
had been omitted and gave their d.
mansions.
He said that the reason that some
of the slopes had been omitted from
the model was because he had been ex-
cluded from the mine for a period and
did not have the notes necessary to con-
struct the Slopes.
The witness testified that there is one
place on the defendants model where
the color identifying a vein should have
been colored differently. in his judg--
ment. With this exception he approved
of the identifying colors. On the model
the veins are differently colored, and
each vein bears one color throughout
its entire extent.
Now Mr.. Hayes, are these two
an1n ln he q
vein?"
mo; they are different VEINS" an
swered the witness.
Then why did you color them the
same?"
The witness explained that the colors
had to be repeated upon different veins
in some instances, but that the coloring
in this respect had been arranged In
way to prevent confusion.
The witness said that the Windlass
vein, in the east part of the ground,
and the north connecting vein, in the
west part of the ground, were one vein
before the faulting of the ground, in his
opinion.
He stated, in answer to the ques-
ton whether some of the veins on the
model had not been differently colored
originally, that a vein east of the faults
now colored red, was first colored light
green. On the west of the faults there
is a vein colored green, and Mr.. Hughes
asked him if he had not first colored
both veins alike because he thought
they were identical. He answered in
the negative.
IF that is so, why did you color them
alike at f1rst?" said Mr.. Hughes.
Because the number of colors is linn
tied, and some had to be repeated"
was the answer.
The witness had said that there had
been a conference about the coloring
of the model.
He testified to several other changes
made In the coloring of the veins.
Asked If he approved Of one change,
he said no. Asked why not, he said
that he now approved of the arrange
ment of the colors.
He stated that originally the various
levels had separate and distinct colors
also. The change here was in the
entire system of coloring. A raise near
the surface of the ground had also
been the subject of change in its col
oring. The last change had been made
after a conference of the experts.
The witness said, in answer to a lead
ing question, that one coloring original
ly made would have necessitated a
crossing of the apex lines on the de-