Tonopah daily bonanza. [volume] (Tonopah, Nev.) 1906-1929, 1915-05-27


allel thereto through point on the
northerly side line Of said mining
claim ll421a feet westerly from the
northeast corner of said mining claim
measured along the northerly side
line thereof continued indefinitely in
its own direction southerly.
Special Finding
The said vein does not on its up
described as follows
Thesaid vein does not on its up.
ward course. or at its top or apex. OUT
crop or reach the present surface.
but is covered or buried to consid-
cradle depth by lava, locally known
as and called Midway" andesite.
which. after the formation OF the
vein, flowed over the then surface of
the territory in which the vein exists;
that at and for distance of $50 feet
westerly from where said vein or lode
crosses the easterly end line of said
West End claim. which crossing is at
distance of 1876 feet northerly from
the southeast corner OF said West End
claim. there is a juncture or union be-
tween two limbs or sides OF said
veins and from the summit of said
Jnnctnre or union the downward
course OF one limb or side thereof is
In a northerly direction, and the down.
ward course OF the other limb or side
thereof Is In a southerly direction;
that there Is continuation upward
from the summit OF said juncture or
union Of said northerly and southerly
dipping limbs or sides OF said vein of
ore and sllver-bearing quartz or rock
in place for distance from 20 or 30
to more than 100 feet, and to what
was the surface before the same was
buried beneath the said lava flow:
that such ore and silver-bearing
quartz were deposited where the
same are now found at the same time
and during the same period that the
main vein below was created, and
from mlneraLbearing solutions having
the same source: that the dip and
strike or course OF such upward con.
tinuation OF ore and silver-bearing
quartz are conformable - the dip
and strike or course of the said north
erly-dipping limb or side of sid vein
from the summit of said juncture
downward, and the court finds that
said upward continuation Is a part OF
said vein or lode: that thence wester
ly, and for a distance OF 800 feet, the
northerly and southerly dipping limbs,
sides. or slopes of said vein do not
unite or form a union or juncture in
their upward course, but for that dis
lance each OF said limbs or sides has
separate and independent top or
apex; that thence westerly. for
distance Of 40 feet, the northerly and
southerly-dipping limbs. sides. or
slopes Of said vein are again found in
conjunction, as in the said most east
erly 1850 feet; that thence westerly,
and until said northerly and southerly
dipping limbs, sides, or slopes of said
VEIN lntersect with and cross said
hortherly side line of said mining
claim, they do not unite or form
union or iuncture in their upward
course, but for that distance each of
SAID limbs or sides has separate and
independent top or apex; that be-
tween said distance Of 40 feet, where
SAID northerly and southerly dipping
hmbs, sides or slopes of said vein. as
aforesaid, unite or form union or
luncture in their course upward, and
SAID place on said northerly side line
OF said mining claim where, as afore-
said said contra-dipping limbs. sides
or slopes Of said vein respectively in
tersect said side line and cross the
same and so depart from said mining
claim, there are two points at which
appears that said contra-dipping
limbs, sides or slopes of said vein on
their upward course approach closely
10 juncture or union, but as to said
contra-dipping limbs. sides, or slopes
OF said vein at said two points actu.
ally forming a juncture or union on
their upward course. the evidence is
meager and unsatisfactory; that the
point where the said northerly dipping
hmo or side Of said vein departs from
inc said mining claim through the
norteerly side line thereof is 1870 feet
westerly from the northeast corner OF
SAID claim measured along the north.