Deseret evening news. [volume] (Great Salt Lake City [Utah]) 1867-1920, 1892-04-01
Tag NEUTRALITY-SUSPICIOUS.


motjon for non-suit lac would
srs, no objection. In case they wished
,aIr.Is, on coupling w. s. Mccormick
lin the lossces, he would not insist ON
',,,t,ny that gontleman's name from
A.. case. but he did insist ON the non.
'n,, ssto MI the Others except Keith,
Kearn aud Judge.
obed l.. Palmer, the well known
mining engineer, was next called
M the defense, aud he stated
,bat he had been engaged In mining
IN Idaho, Montana, Nevada aud Utah.
since 1874 he had been this engineer
for the Ontario company, and he was
.l.o the engineer for the Eureka Hin,
centennial Eureka, and DAILY mining
companles. lie wA- thoroughly IA.
miliar with all tho properties shown
on the map, and had examined the
,,o,tinrs carefully. There was but
an, win there and that was brdded.
m. auaftzite was certainly the foot.
wnil' Of the vein, for the reason
that lNN WIN AANAN hhNh W hANN
niartzlte In very many places and
aver penetrated II, unless there was u
gath, and IN n number Of places the
orc rested on the quarizite lot several
hundred feet at a stretch. The true
walls Of the vein were the walls To
which the ore did extend, although moi
continuously perhaps, but beyond
which 1t did not pas. From the place
"A. - La. fIaa
Wiman discovery, the ore rested on
The quartzite clear across the Horse
incliue To station 80. In the lower
Maytlpwer dfiit tho ore also came
down 10 qutrtziIc, aud the same thing
wiz obsuI we'd for distance Of $50 feet
IN the Long Incline. The bulk Of the
lower end OF the Long incline was IN
0uaflzite, amt II was found again
further north. The stopo between the
Back incline and the Big incline came
to within short distance Of puartzile.
The witness went ON 10 multiply the
instances where the qusrtzito ws-
found, either with the orc resting upon
1t or but few lost away, and whvn he
got through with the subject he dii
not leave much Of tho theory that lime
formed the foot wall. II was sell.uvi-
uNnN AilNA AllNlN NNH u ANNNt W hNANhANf
In the foot-wall quarlyile, the evidences
Of IL being seen AT various places along
the vein, and the vein, a. n rule, cos
formed TO the Irregularities Of tue un'
deriving quarilite. Mt. Palmer here
referred 10 the sectional map anu point
ed ont places where the buchligg ul the
foot wsli was shown. This dip Of the
quariEite In the lower part Of the mine
was about 20 degree, hut u became
much flatlor Us II approached the sur
face.
what IL the manner OF mineral de.
petitions Ia limestonc!"
"rhcy are particularly noticeable
for the irresularity within limestones,
ia that the ore " not confined to one
leaf OF the limestone, but sometimes
takes tho place OF ted OF lime"
"Have. you reen any Instance.
whore the vein followed was COM
parstively thin seam, and then Gnd II
suddenly widen out Into large body
Of ore?"
''Ycs, such instances are seen all
through the mine"
"Afe you familiar with the Fair
view incllne?"
"Yes, | became acquainted with II
FNNlt NNklA VI wv y ttFs
been down to the bottom Of II. II was
then about 100 feet deep, anu II sunk
at an angle Of about 10 degrees"
els there a contact between quartz.
Ito aud lime In that inclint?"
Eyes, there IL, right at the top OF Il.
The open cut ut the head OF the incline
discloses the contact. Going down he.
yond that, IL h In quArtzite all the way.
-.
tracled from II, and also near the sur
face ut the contact"
"What " your opinion as 10 the
source Of the mineral found In the
contact n. the top OF the Fairview In
cline?"
81 think II il from the contact"
"Have you seen nh instance Of the
p0rlhyry dyke cutting a vein and the
vein continuing right along?"
eyes, many Of them. nave oh
served II In the Ontario and Daily. Ia
Bingham the Highland bedded vein
was cut by the Galena flssure aud the
vein was found on the other side, the
displacement being nifty feet In the
DAILY there are instances Of the vein
being cut by a porphyry dyke, and II
Il easily found on the other side, thb
displacement being slight"
ia there anything here to show, no
far "A development IL concerned,
whether the porphyry dyke was
formed after the vein was?"
"None, 80 far as the development
goes"
Mr., Williams then carefully exam.
ined the witness on every point upon
which he had testified, and for over
two hours bomharded Mr.. Palmer with
questions, which were all promptly
answered.
M. Dickson finally took tho witncss
IN hand again, aud the buckisug OF the
formation spoken OF by him was Illus
rated by sketches from Le Conps III.
ements Of Geology.
There was not as good vein, said
Mr.. Palmer, In the workings north Of
tile triangle as was found Ia either the
Court or Northlaud upraise.
Mr.. Willlams-Dld you direct any
OF the development work done by the
defensc2
Witness--I simply directed the work
OF making the Court upraise. The
vein was followed TO show that 1. pass
cd beyond both the Jennie Lind aud
Nevada.
When the examination was finally
concluded, Judge Zane said; "Gen-
tlemen VI the jury, the court viii now
adjourn over until Saturday morning
NJ ten, and am MT certain whether
we wi 20 on with the cure lhon or
not Ia the meantime, you mus, not
lAlk about the case or discuss Il among
yourselves"
Mr, Dickson said that both sides
would agree TO the rial being resumed
Gu saturday, ami the court then ad-
igufued