Pioche daily record. [volume] (Pioche, Nev.) 1872-1876, 1873-04-05

examinations of it. IAttorney explains the map Mt
1 found large Groupings OF vast ledge Win m
mineral from Panaca shaft to incline M the m
vein matter is of dirty red and yelowish color; ~
GShown rock] 1t looks like that; and that; the g.
vein is little softer than the country rock; -
took assays from the cut between the Panaca D
shaft and the incline every seven feet. lResults a
read.l The samples were taken from rock in II
place; have been down the incline M; there Is !,
streak of rich ledge matter from the incline 70 Il
point l; from that point found rich ore; there n
is good regular wall along there's went up the
drift to the west and found ore; found ore in the
LIST level running west from the incline; fouhd
good streak of ore from point ITO point 90; 7
found good ore in the winze between the seconu q
and third levels; found ore west OF Panaca SMART I
between the second and third levels; found ore /,
in the stope between the second ana third Levels
found ore in the drift from the crossconrse TO !
the Panaca shaft; found there = strong Ledge
with rich ores; assayed eight samples from that !
drift IReads results to che jury.l Some OF my
samples from the cut were got near Panaea
shaft; took samples from the west END OF tne
third level near Panaca shaft. laeads results OF
assaysl The ledge matter in the surface cut Is
very like that below; have no doubt that the
edge in the Lightner shaft is the same as that
| in Panaca shaft. A. |
FIRST level west of the Lightner shaft to the sur
face by ledge matter and weliden1ea wan
| through incline M; there was mineral part Vi
| the way sometimes one wall and sometimes TWO
walls; found schist to indicate vein matter;
| have no doubt that it is vein; didn't make
| ASSAYS OF ore from the incline
| prof II c. Husch called for plaintiffs have
| been mining engineer thirty years; in Germa-
| ny Spain and on the Pacific Coast; was edu-
Gated in the Freiberg mining school; nave
been engaged on this coast since iSo2; nave
frequently examined mines at virginia Guy,
Humboldt Battle Mountain district, W hlte Plne,
Eureka and here; have examined the haymohu
| & Ely mine; it was thorough examlnat,on
Explains the map From the r ana si snsi
northeast for "a feet in the cut on both sides
| found boulders colored yellow by oxyde OF ieaa;
in the cut found lead ore; from 70 iouLo
carbonate of lead; from there to h iound DARK.
ish black lead ore; from H to found h8ht
green slate with galena and carbonate OF lead the
vein is enclosed in brown shale; from W .no
} | formation becomes more quar.Ale; ING pam
r | nature of rock continues to incline NJ, ~ poii'
4 | found wall pitching in southeriy drec-
: | tion which has been followed 20 feet down; IN
a it isvein matter composed OF quartz, slate ana
g ore; at point found two distinct walls ex-
tending to point 2; the walls are Nearly l.; ptho
q dicular: the same two walls are exposed III the
Ii drift from point to 2; from point to IL west
t. is well-defned vein with wall and ore az point
in the incline the vein is dehned east OF Tue IN
| cline: on east side of incline the lode mas oeen
he stoned OUT on the west side the lode 10 denneu
d. from point to the first level; from Poiut W
a the Lightner shaft the lode has generally peen
e., stopped; from the first lever west 70 eue e.os ;
IS. head the vein is we'll Defined at point the VEN
ia ia cut by the crosshead west OF the cross-heaa
m from point 8 to point 70 the DRIFT Is throuSM
ar shae: at point Il near the Panaca smart arii'
t. | through
nd | strong lode is in the winze between the hrs'
nj and second levels; west OF that wlnze ore Eaf
ut been stoped the foot.wall is plainly visible d
I'm feet below the first level there Is ledge NATE t
IRE in the winze down to the third level from th'
me third level to the Lghtner shaft the lode na'
Ids been stopped; point % on the third Level tn
np cross. head is struck and runs northwest; oii
Sc has been run along the cross-heau 10 pom. a
the from point "a on the cross-heau W p1n 'o,,
ace there is small vein of rich ore 1t IS cohtnuou
III and can be traced nearly TO the Panaca shai
ing the same vein can be traced to point 81 west
rhe the Panaca shaft; the vein runs east ana We
cad and bitches south; between points II and ~
NJ; perpendicular raise along the Panaca shai.,
the the raise is son vein natter the raise eA.eno
liar from the third level OF the Pahaca snait w
low drift A third of the way up to the second leve
of | there is a 9nch vein in that drift; from I!
ore Panaca shaft northeast to point 20 II vel
ne in ouartzite from one to four feet wlde petWee
al points rs and 20 the vein is also well ae q
baf frnn noint 05 nm 70 point Sc, west of cross-hea
ore; there is well defined veln there Is Boou ~
the all along the third level till crossheaa 10 %.
hid countered; west of the crosshead bae looc ie
e in pears, assuming It's regular my w., m
yels the cross head fifth level has shifted the Ve
haft but somewhat differently; below the line Oh u
ore turbance the vein is regular; in passing oo
,yel; Wine from fourth to fifth level (3o ieet cas-.
it is Hermes shaft FOUND tne ,9uS ,unna,ion
the points to in the incline nj the f"rmauon
some slate and quartzlte' the seih t' ,~,iar
the third levels is in quartzite; II Is leSu ..
White quartzite except at the cross neau ~ 10 TO-
,k in slate Int we'll Defined from nth to fourth lev
; the the pitch of the vein is about 49, at point n
the the Panaca shaft the VEN UPS ho it o.,
rally point 80 the tn I'd level 1t assumes iss lesu
shaft pitch the vein has nortneriy Pi'en - I'm
ltner naca shaft to in the surface cut from poii
To the surface near incline M, the vein Is pea
, and | PERPENDICULAR; the ledge is well defined IN
out cut from the Panaca snai' W ~ - - 4.
visits IL shows both sides of The vein shown rock
ak of pronounces it similar to that iound III sur
must cut; found such ROCK iloii p pm 80 IN
rren; along first and second levels iounh iocS I'm
| in vi
" the the ledge is so well defined i'll the cut that
le in one ought to be aple 10 'laoe a., ~ s,o,,
Ray. that is found in country fock away ron l,
break | ledge; there Is no pottiou VI ING w. ~
in is panaca shaft ana incline NJ that essays cahho
neral; obtained; the lead ores carry silver; III MAJ
,y the the incline M, which was uolle iH.d h
in the vision one party of worknen followed the
iden- down from the SURFACE a'iu alo."o - -
orally from point L. their excavations met WIN
If the varying hal1 an inci' lounu W. W, .tna or,
varies; Panaca shaft 80 feet down we VEN h
down the shaft; undoubtedly wy ieuSo - So,
mooth | shaft is the same that in the cut; from
IL and general dip OF the ledge below would expe
fit, the find Groupings above "nele 'neS "''' ~
q deep in the cut is nearly vertical - ,
~ M Crosseyam;ned-I have been since The 1
q we'll January examining the Raymond ELY mn
g were have been engaged almost continually
IRE was then; have made assays my i;n ,ar n
, Tn gat | completed; two men are now WORKING iof u
:. san, feet down in the Panaca shaft; they are 10
Iennes ing an ore vein; am not the company se
re. he | surperintendent; did not come hsre 10 pei
line Nj; in San frahciscoi eaino ~ ~, ,eina ana
alf the Mr.. Raymond 70 eHaii.o . ~ inaa T. tha
st level could, estapnsh the iaS' 'n ~; tn p.naca
con- have been engaged aseApo.sin M Ar;ynna M
between Eoernardt, Aurora neAa ~ ciifrn;a ut M
ny rock in Nevaaa, anu Que case ~ IN mi,;no
md diff umne Hill; was nrst ehsaSv naa .nnner mi
in mat expert III 1868 OF "a, 'nat We n 1870
marked Mokelumne Hill cai'ie ~. w M Ea,ther riy,
the par engaged II 4uarIA nil. s, ,aso to ia w
samples an En9nsh coHpany, I'm ~; California. m,
s rather gagged III copper niinti5 A Ei,arhorlt min
WY "a' that it was vein; the question was whetl
omitted was vein or aeposi. .u i ,vaS one n
Isl would case was as 70 Whe.te sn. tn., there we
y point veios; estaollsneu sns %at NV nresent g
J, on the veins; became satisnea pa"mnnd Ey
ca shaft sions IN regaru W VIC Il a week
ng pres days. lfoln.s ous W ,hi S bowed that
hat they der MS SUPERVISION, Will aun,Sh and comnl
nd con- ploratlons nau oee. .noA ~ na ssnse N
lullr IL