The Anaconda standard. [volume] (Anaconda, Mont.) 1889-1970, 1899-09-27

the part inside the Pennsylvania claim
| is west of the Pennsylvania east end
| line. The tops of sulphide ore bodies.
| on the 30 level, outside the Pennsyl-
vania north side line, are east of the
| Pennsylvania east end lines. The sui
| phide tops of the Windlass and north
veins are inside the defendants ground,
| the witness said. He did not know
whether the sulphide top of the No,
vein is inside or outside the decided
ground
The No. 8 vein, from it's easterly ter
minaton on the defendants apex map
| to the south side line of the JohnStown
| claim, was the subject of investigation
| next. The distance of the vein from
| the Johnstown south side line on the
| lower levels and it's downward dip were
| given. On the 400 level the west drift
| on the No. vein, at the west fault, is
about 105 feet away from the south side
line From the angle in the south side
line of the decided ground to the west
fault it is 1856 feet, the witness said.
The vein is farther south at the fault
than west of there. This is the vein
that is close to the line dividing the
defendants ground from that of the
plaintiffs.
The witness explained what he meant
by saying that the clay seam in the
faults was mineralized in a mechanical
way. He said that the edges of the
veins were cut off by the faulting. and
pebbles of rolled ore from them intruded
into the clay seams.
WAS that by the faulting itself?"
asked Mr.. Scallon.
Yes: the seams were not MINERAL
lied by mineral solutions" said the
witness.
He said that the mineral mass in the
faults was from two to twelve feet
wide and was what was created by the
faulting. Witness BullSly's sketch of
the fault crevice represented his notion
of the fault formations.
He testified that while there are no
Slopes on the defendants model at one
| point on the 800 level where they exist,
| neither were there any there on the
| plaintiffs model.
The witness said that the assumption
| of the horizontal and vertical displace-
| ments We're made upon the basis of
| measurement furnished by the situa-
| tions of the porphyry bodies He ex-
| planned that the reason he had told Mr.
| Hughes he could not make a certain
| computation was because Mr.. Hughes
| had not given him the quantities neces-
| sary to be known in order to find the
| unknown one.
| The witness projected the lire Of the
| dip of the No. s vein in the most west
| erly raise from the 500 to the 400 level.
| The distance of this line from the
| Johnstown south line is 40 feet, the
witness said The correlation maps
| were placed in evidence, and the wit
ness was excused.
| The fourth expert witness for the de-
| Tense, William F. Word, was called
| Mr.. Word said he is a mining engi-
neer and has followed his profession
many years. He is part owner and SUI
| perintendent of the Gold Belt mines,
| in Marysville, Mont, and was super
| intendent and general manager of
mines elsewhere. He was prospector
| and a miner also.
Did you say you are superintend-
| ent, Mr.. Word?" asked Mr.. Scallon.
Yes, sir; and also an assayer." said
the witness.
He said that he was educated at the
| University of Michigan and graduated
from that institution, taking the de-
| gree of A. b. He was educated with
the special object in view of following
mining, and took the best course fox
that purpose that the college afforded
He was taken off the stand for a few
moments. while Frank o. Smolt All
assayer and chemist for the Boston Il
Montana company, testified to lists OF
assays of samples of rock which he
| made for him.