Eureka daily sentinel. [volume] (Eureka, Nev.) 1871-1887, 1877-02-10
line at the 9th level, linestone; at 9Th level, |
uuArtzite. and in tho level of tha Wirdsaii

line at the 9th level, limestone; at 9th level,
quartzite, and in tho level of the Windsail
,ha,.t. quartzite and ore; all tho balance o!
the leveis,throrgh quartzite and limestone; on
sre:. the winze at the 7th and sth levels has
ore in the top Of it; crosses tho 10th level in
ore. and workings Of the Windsaii shaft;
there is ore NE. of the winze on the 10th
level; th'y have driven a level from the bot
tom Of tho winze; the day that l made the
IT,; those are all the levels at the date of sur
vey; l found the quartzite wall in the Rich
mond on the 9TH and 9Th levels; it runs in a
direction of s. 54h dg. f., magnetic, and the
Der seeing ore on walls; walls were not
smooth on 8th level; on the 7th level [ think
it was smooth; its dip | did not take; ] found
what / took to be hanging wall Of ledge; it
in the Eureka; found it on the 9th, 18th and
9Th levels; l think l found clay on three
l~ovels; there was a BODY of shale on the 7th
level; on the 9Th and Sth levels it was merely
a clay seam: its direction varied; on the 9Th
level S. 81 Dc. f.; sth level "i 5. 81 ;ds. f.: 'd dia
not take the dip; found no othrr walls in the
Richmond; | think | would have seen than
if they were well defined; lid not know how
the ore lay; was in ore chan On Tho ith
and 9Th levels: was in no other ore chamber,
except a small one on the 18th level; ON the
10th level O. Eureka Consolidated, about
9 #, of hanging wall is exposed: in tho
Bell shaft tunnel, the width Of the tun-
did not take the dip in the 10th level: tt dip
in the bell shaft tunnel is 90 dg.; on the line
of the dip from the Bell shaft tunnel to the
10th level, the depth is $40 IT.; actual psrpen-
dicular depth is 742 It.; l think it is the hang
ing wall OF the vein, because no other levels
run out and strike the large clay seam; at the
Bell shaft tunnel the seam is 2 or 3 fl. across;
! am not sure. for l did not measure it; the
direction of the seam at Tho Bell shalt tun-
mol, wo,ld carry it NE. of the Lawton shaft
80 IT,; the ground rises up, going up the hill
from the Bell shaft tunnel to the Lawton
shaft, 50 #. that dip would carry the clay
seam to tho SW at tie Lawton shaft, 40 #.
In 80 II. elevation; if carried to surface. it
map and Lawton shaft; it would have to
cross q ridge 10 get to Lawton shaft from the
Bell shaft tunnel; it would not have to go
over any ridge hirh her than the Lawton shaft;
tho clay sean, does not appear on the surface
between the Lawton shaft and the Bell shaft
tunnel; l have never examined the ground;
the ore marked on the map at the line is
called the Richmond mine;. it has always
been called the Richmond nine; l surveyed
your patents as the Utah, Artic, Ant-Artlc
and Atla1tic.
Kedirect-The line on map, from G to W.
represents the compromise line and The COM
promise extended line; ! have seen groupings
on the surface Of the Richmond mine; the
groupings | consider the same vein us the ore
bodies to the NV. of the line; l think it all
the same vein; On map Y, at point b, at the
widest place, at right angles to the wall, the
only place | ever took tn, width, it is 40 tt.
wide; OTIS Cham DER has its groupings on
the Sc. side of compromise line; none OF the
late locations extend across the line except
the Utah; l never saw quRrtzite on the west
side of the Hamburg; never examined it; l
can't say that the Hamburg is on the same
vein as the Eureka Consolidated; i tn nix it
is: l don't know how far the Hamburg is
from the Eureka Consolidated.
Eureka Consolidated rest their case.