The Anaconda standard. [volume] (Anaconda, Mont.) 1889-1970, 1899-09-12

north branch has been stopped up to the
west fault, and there the stopping ends.
There is none OF the vein beyond the
fault.
What shape are the slopes at the
eastern end of the north connecting
vein?' asked Mr.. Scaloln.
THE east side of the slopes has a
slope of about As degrees" said the wit
ness.
The next vein south of the north con-
nectng vein, corresponding with what
the PLAINTIFFS witnesses called the
Rarus vein, was called the south vein
by Mr.. Hayes, who described it, as II is
below the surface, also.
The vein known as No. 8 vein, shown
on the apex map by red mark at the
west end of the Rarus claim, just south
of the Rarus south side line, was next
described.
Then vein known as the Powder
vein came in for attention. This vein,
the witness said. passes from the south
vein to or near the north connecting
vein. and it cut off at the east by the
faults. 1t has been worked by means
of slopes from the 700 level upwards.
" ends at the faults.
THE vein goes farther east on the
upper levels than it does uron the lower
levels" said the witness. THE faults
cut 1t on IN that Snape
What is the shape Of the slopes at
the faults-straight or diagonal?" asked
Mr.. Scallon.
Diagonal. They follow the west
stope of the west fault" said the wit
ness.
He discussed the Pennsylvania next
and said it was cut off by this fault
also.
At this point Mr.. Scallon suspended
n IN asly ha IN no l.
lowed to use the plaintiffs maps in
connection with the examination of the
defendants witnesses, in order to COM
pare their testimony with that OF the
plaintiffs as to particular workings. He
said he thought that the maps ought
to be in court.
Mr.. Hughes, for the plaintiff said
that the defendant had tracing of the
plaintiffs general map. He added that
he should like copy of the defendants
map and would take advantage of the
opportunity to ask for an order for the
same.
A discussion of this matter was had
between Mr.. Scallon and Mr.. Hughes,
and it was finally agreed to between the
respective counsel that each should
have copies of the others maps Stipu-
lations and an order embodying the
terms of the agreement were signed
by the court later in the day.
The examination of the witness was
resumed, and he stated in answer to
question that the north connecting vein
and the south vein both cross both end
lines of the Johnstown claim. The
Pennsylvania vein was traced under
ground, and the witness stated that it
is also cut off by the faults.
Where does the vein east of the
faults known as the north vein apex"
asked Mr.. Scallon.
I'm the Michael Dewitt ground" said
the witness.
The witness said that the veins are
quite regular till they reach the faults,
where they are cut off.
The witness said that the veins east
of the west fault extend further to the
west as depth is attained, following
the westward dip of the faults.
The Windlass vein, which is also east
of the faults. apeXes in Michael Dewitt
and Pennsylvania ground according to
the witness. The fault lines are dis
tinctly outlined, said Mr.. Hayes. He
gave the strikes and dips and the vary
ing distances apart, on the various
levels and at different points of their
strikes, of the two faults.
He said the faults are filled with
broken rock and crushed parts of the