Tonopah daily bonanza. [volume] (Tonopah, Nev.) 1906-1929, 1915-05-27
FINDINGS ARE SETTLED IN MINING CASE
CONTINUED from page u

erly side line thereof; that the point
where said southerly dipping limb Oh
} side OF said vein departs from saiC
mining claim through the northeast
! erly side line thereof is 11421s feet
westerly from the northeast corner oil
said claim measured along the north
erly side line thereof; that throughout
said distance OF 40 feet, where the con
tra-dipping limbs or sides OF said vein
are found in conjunction, as herein.
before stated, there is continuation
upward from the summit of the Juno
ture or union of said two limbs or
sides of said vet Of ore or vein
quartz to what was the surface before
the same was covered by the lava
flow; that the dip or downward course
of both the northerly and southerly
dipping sides or limbs OF the vein
where the two are found in conjune
ton, as aforesaid. and also in the
places where each, as aforesaid. has
its separate and independent top or
apex. is regular and practically Gree
from fluctuations; that the said south
erly dipping limb or side of the vein
in the easterly portion of the West
End claim that is to say, the easterly
$50 feet thereof, has been developed
from the top or summit OF said June.
ture OF said contra-dipping limbs to
and beyond the southerly side line OF
said claim, or for distance, meas.
ured on the slope or downward course
OF said southerly dipping limb or side,
of 500 feet or thereabouts, the average
dip there being IL degrees from the
horizontal; that the westerly portion,
that is to say. the westerly 300 feet
OF said southerly dipping limb or side
of said vein found in the West End
claim, has been developed from its
top to and beyond the southerly side
line of said claim, or for a distance.
measured on its slope or downward
ioci vi lVVV rect OF Whereabouts,
the average dip there being 30 de.
grees from the horizontal: that the
average dip of said northerly dipping
limb or side OF said vein, so far as
the same has been developed in its
downward course. is IL degrees from
the horizontal. that said vein is fis-
sure vein; that there is a difference in
the strikes or courses OF said north
erly and southerly dipping limbs OF
said vein Of about 40 degrees: that at
said places and throughout said dis
tances. where said contra-dipping
limbs OF said vein are found to inter
sect and form juncture, as aforesaid,
there has been a mingling Of the min
civilizations OF said two limbs OF said
vein within the angle beneath the
iuncture Of the said two limbs; that
at such places and throughout said
distances the footwall of said two
limbs of said vein, within the angle
beneath their said juncture. by the
process of replacement has been con-
verified into mineralized quartz for
considerable distances below said
iuncture. said replacement quartz ex.
tending from limb to limb.
That the shaft known as the Nc
Quillan shaft was the discovery shaft
of the West End mining claim; that
said discovery shaft encountered and
disclosed no vein or lode of mineral
bearing rock in place until, in its
downward course, II cut and disclosed
said northerly dipping limb or part of
said ven that said northerly dipping
limb OF said vein was cut and dis
closed In said discovery shaft on the
Bird day of April, 1903,
That all OF the ores mentioned in
the complaint and the amended COM
plant herein, as having been mined,
broken down, extracted and removed
by the defendant within the surface
boundaries extended downward verti-
cally of said Eureka and Curtis lode
mining claims, were mined. broken
down. extracted and removed by the
defendant from said vein and between
the extralateral planes described in
the next preceding Finding.