The Anaconda standard. [volume] (Anaconda, Mont.) 1889-1970, 1899-09-07

to No. II cross-cut, which is inside the
west fault. The fault is at the inter
section of drifts No. Il and No. Is.
Now. having got this far with the
Rarus vein, where do you go next"
asked Mr.. Patterson.
"Easterly," answered the witness.
Then the foot wall of the Rarus
within the faults is at or near work
ings "A A, rs A and rs Az"
You have misstated your question
Those workings are east of the east
fault
Then, will you state where the foot
wall of the vein is within the faults?'
1T is colEcident with drift No. IS,
continuing eastward to drift No. H.
The witness was next asked where
the hanging wall of the vein is in this
neighborhood.
Judging from the developments
made, / should place it at the exte-
rior boundary of the ore developed,
said he.
Mr.. Robinson then indicated the
position of the hanging wall on the
map. Mr.. Patterson went over its
course carefully from point to point.
The 500 level was made the subject
of attention, and Mr.. Robinson said
that the hanging wall of the vein is
in drift No. 10 and the foot wall is in
drift No. 10.
DO you carry the hanging wall
through the faults?" asked Mr.. Pat
terson.
Through the west fault; not through
the east" answered the witness.
DO you designate the hanging wall
east of the faults on the 500 level?"
No: it is not developed. The 500
level is only partially developed level
it is regarded as only half level"
The witness traced the foot wall of
the vein on the 600 level from drifts
Nos. So and 80 at the west eastward
through drift No. IL to drift No. 2
at the eastern extremity. He then To-
Gated the position of the faults on the
600 level map, and said that they are
1875 feet apart on this level.
He placed the hanging wall of the
vein in drift No. II at the west, and
carried it eastward across cross-cuts
No. so through drift No. IL, across
cross-cut No. 9, through an undevel-
oped area into the large slopes. A
south branch of the vein here is in
drift No As.
rs the extreme southerly extension
of the hanging wall in drift 1872" ask
ed Mr.. Patterson.
LAS developed, yes said the wit
ness.
He placed the bottom of the Bat
terman raise in the hanging wall of the
vein.
HOW lar TO the SOuln Oh llle bdttcl =
man raise is the hanging wall?' asked
Mr.. Patterson.
Il put it at, not south, OF the Bat
terman raise at this point" said the
witness.
THE vein at this point is usually
called the Windlass vein, is 1t not?'
Yes"
The witness here stated that the
vein, at this point, can be traced up
ward to either the apex of the Johns
town discovery vein or the apex of
the Rarus vein.
This point is within the faults?"
asked Mr.. Patterson.
Yes" was the answer
The 700 level was gone over in like
manner with the levels above.
Mr.. Robinson marked the faults or
transverse assures on the 700 level map
and stated that they are approximate
ly 200 feet apart here. The drifts were
not marked; so they could not be nam
ed in tracing the foot wall on the map.
Mr.. Robinson stated that there is an
east and west area, 300 or 400 feet in
extent, undeveloped on the 700 level
This prevents the tracing of the foot
wall. The ground extends across both
faults.
The hanging wall was described by