The Anaconda standard. [volume] (Anaconda, Mont.) 1889-1970, 1899-09-28

ken and crushed, and have no uni
| formity of course. / consider this the
result of the faulting."
What do you say as to the ground
| between the faults being vein?"
| Il consider it a vein."
| With what course?"
1T runs north and south and is
bounded by the walls of the faults"
The witness testified that there Is
no connection between the Berkeley
vein and any vein west of the faults.
At the opening of court, after the
noon hour, the court announced its rul'
| ing upon the objection made to the in.
PRODUCTION in evidence of the original
| location notice of the Pennsylvania
claim. The court had had the matter
under advisement for a week or so.
well, gentlemen, / have read over
| the authorities, and / sustain the OBJ.
| lection to the original location notice
Of the Pennsylvania claim" said Judge
Clancy.
You want an exception, 1 SUPPOSE?
he said to Mr.. Scallon.
Yes, SIR" said the latter.
Give the defendant an exception, u
said the court.
After few more questions by Mr..
Scallon, the witness was turned over
to the plaintiffs counsel, and the cross
examination was began under Mr..
Hughes.
when did you begin your examina-
ton of the ground in controversy
asked Mr.. Hughes.
"On the Goth of December, 1885," the
witness replied.
And from that time till now you
put in IS days?''
Yes"
The witness testified in answer to a
| question that a certain part of the
slopes in the ground had not been eX-
| amined by him. The Slopes were not
accessible to him.
Were there sufficient facilities Of
| fered you to make a thorough exam
| ination Of that ground?" asked Mr..
| Hughes.
Il did not see everything, but I saw
enough to know what the ground is,
| said the witness.
He gave the dimensions Of the area
| between the faults, upon the 450 level
| that he had not examined, and stated
that it has an extent of 25 or 80 feet
north and south and rs feet east and
| west, giving its color on the 450 level
| plan map.
Tell us if the ore at the east fault
on the $50 level, near the Windlass
! vein, at the point you examined, is
dragged ore?" said Mr.. Hughes.
I'm the fault it is dragged ore; out
side it is not" said the witness.
For what distance along the Slope
is it dragged ore?"
Il don't know"
The witness said that the walls of
assures are sometimes mineraliZed:
usually the naturalization is confined
to one side. There are two methods
by which granite is mineralzed that
he is familiar with. One method is by
the naturalization of small cracks and
interstices in the granite; the other is
by the replacement of the softer parts
of the granite by copper.
The witness testified that he had
not seen any stopping, at certain point
on the $50 level, upon mineralized gran
lite that was being broken for ore. He
had seen no altered granite that looked
like granite whose softer parts had
been replaced by ore.
The witness said that he had seen
a piece of what he thought was. orig
inally a part of the north vein at the
wall of the east faults. 1t had been
dislocated from the north vein and
dragged into the fissure a few feet, but
it's particles had not been rounded. The
witness had never seen any dragged
ore that had been rounded which he
could identify as coming from any
particular vein.
do you mean to say, Mr.. Word.