Deseret evening news. [volume] (Great Salt Lake City [Utah]) 1867-1920, 1892-03-31
xopTuLAYp.aAYFLowER SUIT.



Tho defense. lie lie Mt present eh'
"a in the manufacturing business,
has followed mining for many
.s.,. In various parts pi this Territory
Iii Yin Nevada, bel1T quite familiar
-nh silver lead mines. He said he
had made several examinations OF the
,,opettles shown on the map and had
i.,natutsd himself with all the work
,a1. ma well ~ the surface. Going up
hsrulch from Park CITY the road ran
a,onq the gulch, AMI the hill to the
nor,h rose rapidly. Going over the
I'm 10 the south was another gulch.
The gulches were duo mostly to erosion,
vbleh had cut the strata. There was
ayein there, and II cropped out nj
the Wilman discovery, where there
Wa ore. Going down the die.
coyery contact vein was found. Tho
t,stwall was certainly quartziie, ~
ras demonstrated by the fact that the
we rested upon II near the Wllmap
discovery, In the Horse incline, IN the
m. entire workings. In the lower
Ain. for exampls. The ore rested upon
me uuartzite Tor two hundred feet AZ "A
grelch, amt there was also stretch Of
Il In MATHS din. OF course, thore
were places where tho ore did not
come down to the quartzite. In tho
,topes la the Horse incline the slopes
reached from the qunrtziie below, 10
twenty-five feet above. He had not
leen able 10 trace the ore beyond the
ouartzlts below, or the blue sparry
limestone above.
Mr.. Marshall--Is there any con.
tuuous strata Of lime that continues ~
underle the orc In the vein?
The Wituess--rhorc is not. In ono
portion the ore may occupy one layer
efbeds, AMI la another Iart IL may aud
docs occupy ether beds.
ais there ANY zone Of mineral
ihere?p
stWell, the mineral IA limited by the
quauzl,e below and 'bluo sparry lime
hb0vt."
'ls that the lode2"
.Thr miner would call II bis lodo,v
''Is there anything between the two
walls YOU have described that would
tAuHf you ~ NUM- Wv N'AAt
"Nn sif.n
At this poipt n large plaster model Of
the ground, giving q very good general
idea oftho hills amt guich, with the
various workings aud uoints rcfcrred 10
marked upon It, was Introduced, aud
by ID the witness easily illustrated the
course OF the contact clear around TO
the other side OF the hill. Various cuts
had been riade hv the defense IN the
hill beyond the William disc very, and
the quartsite found In the latter was
proved, by IT, position, etc, TO be OF
tho same bot as found in the former.
The ore fOund Ia the doiCn lnnps cuts
assayed.
Judge Royle--Wc ask that they show
where the apex is no..
MIR. Brown--We will show that we
own the Fairview, and license from
the Ontario 10 the Ape, tie NJ G. anu
the BlrJ. Il IL competent for " TO show
the course Of the voiu, no matter where
1t comes out.
Judge Royle--Wc claim that the
vein, n Il IL cut OIL by our poFpbyry
dyke, leaves the apCx IN either the
Jennie Lind or Central Hill, both Of
which we own.
Judge Mashall--I will now ask the
witness where the apex OF the vein
~
Without the slightest hesitancy he
traced the lines OF contact and AIex
around to the Fairvicw, whore lie lo-
Gated tho apcx. This conclusion was
reached through cuts having been made
In the hll, disclosing the contact ami
formation, by mathematical calcutta
ton, and by the application OF simple
geological principles. with the aid Of
the Typographical and sectional maps
aud the clay model, tho witness clearly
illustrated all Of his conclusions and
demonstrated the correctness Of them.
This testimony was all 0f vital import
Auce, but IA IL all had reference 10 the
maps, 1t IA impossible TO accurately re-
produce II.
"Did you nnd porphyD2" asked
judge Marshall.
"Yes, there is porphyry near the
Jennie Lind dIscovery?j
"What Ia tho formation Of the Wood
side tunnel?r
at Ia quarlgito from the mouth.
There are places where Il Ia much
cracked, and thore II n great deal OF
seepage, causing lime to deposit on
Would doubtless give lime reaction.
This tunnel, In places, is lined with
Ice. This would certainly cause the
quertziie to give lime reaction"
"What In the width OF the quartzito
IN the crosscut from tho WOOdside
shani"
"About thirty feet"
"lsit your Judgment that a strata Of
lima a M la.Hliaa nj
"NO, sir. Ia the instrnco where this
has been found the quartzito has been
forced up, or buckltu, and reef Of Il
has been projected above the lime"
"ls the quari2ie you Hnu under
the slopes IN MATHS incline the same
quartIite you encounter elsewhere IN
tue mine?0
III is iientically the same.p
Something has been said about
Tue porphyry dyke cutting oil the
Vein?D
III the porphyry dyke exists"
doubtful smile, "End Il did cut n vein,
should expect to hud the vein ON the
other side, because u p0rphyry dyke II
Ike any other nsSure. II there II u
dyke there, II must hHve been formed
subsequent 10 the formation OF tho
vein, because wu have the vein ON
either side Of It,"
The witness produced number Of
samples Of quarlzlte aud blue sparry
inns, taken from various points In the
mine, which were passed over TO the
jury.
The court then adjourned uutil this
morning, WHOM the cross.examinatlou
OI MI Van Dusen commenced.
Union Glee Club.