Deseret evening news. [volume] (Great Salt Lake City [Utah]) 1867-1920, 1901-12-21
PARK VALLEY.


operating on the quartz taken from the
workings of this property
PARK VALLEY
At Park Valley the formation Is an
ideal one for gold, the veins occur ~
quartzite and also IN the older rocks
they are strong and now are proven
to have great depth. The localty Is
gold region that today Is merely Duu,
ding into life, 1t has made lts ihltlal
victory as a producer from the output
Of the Century mine, that despite tue
continued TO hold its own around tnlee
dollars per share, and there Is Httle
doubt but that Park valley VIII WIN
in the next few years turn out from
$1,000 to 100000 Of gold bullion lnto
the lap Of Utah. The above volume
may seem large to any one who mas NOT
seen the promising properties that eN-
list there, Few places In the inter-
mountain country show up better imam
II has, ne
Although gold is thus far the CHIEF
metal Of yalHe taken from lts VEINS
there Is. however very good Values III
lead and silver found In many VEINS
but these metals are found IN u form
that requires concentrating AZ Grouse
Creek, Il short distance from PARK var
lev. there are number OF very me
looking prospects, running very wen n
lead and silver. Although no snip
ments OF ore have as yet been mace
| from Grouse Creek, the work zone
proves the existence Of silver iead ore
in paying quantities, ana WITHIN the
next three years this camp VIII most
| certainly become n producer oil golu
silver and lead ores in paying quallty'
SIERRA MADRE MOUNTAINS.
The most promising spot, however
in the entire area Of Boxelder county,
is Sierra Madre mountain, 50 calieu
on account of it's rough saw-like ridges
and rugged cliffs This mountain
forms mart Of the main Wasntch range.
LYING Immediately east OF utah hot
SnrIngs. II extends from North ogden
canyon ON the south to Willard can
Won ON the north, and it's summit rises
about 10000 feet above sea lever, a
largo part OF It's area Is inaccessible on
account OF the rugged nature OF It's sur
face. The formations are OF the older
rocks including carb0nferons brim-
stone. slate, shale and the latter quartz
| ties. -. 90.
Midway in this mountain there ex-
us n series Of assure veins having par
allel dykes Of diorite and horn olende
and t,ll other cross dykes cutting the
assures and welded veins at right an
giles on the right side OF sierra
| Madre mountain. There are five very
distinct assures that rise at the contact
of the martzlte with the sexemite and
emf I'm northwesterly direction
! through the seyecute and O sixth vein
| or assure as the Solomon and bldora-
| DO assure breaks into quart2ite ana
continues onward into the slate and
birthstone In which exists the main Eli
dorado workings The width OF these
assures vary from TO 10 feet. They
mn very regular and are each cut by
n cross vein or dyke which dyke or
cross vein Is copper ??77?2? This cross
Is known as the Eulalia and haa been
but slightly worked up. The solomon
vein shows fairly good values In gold
hut has. as vet only been partly opened
Save I'm the Eldorado, no work has been
done upon Il.
THE ELDORADO,
In the Eldorado on the surface this
vein presents an ore body about feet
IN width. IN which lead ore carrying
about eight ounces OF silver runs very
regularly beyond the nrst level OF 100