davidaulloa/AmericanStories huggingface dataset:
The Winslow mail., 1925-10-02
SOCIETY
Mrs. Driver Entertains

Mrs. Driver EntertalnS
Mrs. V. H. Driver entertained
last week with a series of two
bridge parties, one on Saturday af-
ternoon and one on Wednesday.
Mrs Bert Kleindienst and Mrs. G.
A. Hansen held high score and Mrs.
R. L. Champion held second. The
following ladies enjoyed Mrs. Driv-
er's hospitality: Mesdames E. H.
Black, G. j. Brooks, Bert Klein
dienst, w. S. Chase, R.. L. Cham
pion,, D. L. Bundy, V. H. Wilson,
Chas. Daze, Durham, S. Folsom, ].
A. Green, J. Hickey, M. Janeway, J.
r. Janeway, J. w. Kleindienst, B.
Evans, J. w. Bazell, F. Farnsworth,
c. H. Payne, r. Walcott, Chas.
Shew, V. c. Proctor, Neil. r. E.
Matthews, Chris. Sorenson, Moore,
G. A. Hansen, r. J. Woods, c. B.
hindleson, Robillard, J. A. Peter
son, ]. R. Anderson, w. G. Quebe-
deaux and Miss Nan Brown.
Ladies' Aid Elect Officers
At a regular business of the
Methodist Ladies Aid held at the
church Wednesday, the following
officers were elected for the ensu-
ing year. Mrs. E. H. French, presi-
dent; Mrs. w. w. Ward, first vice
president; Mrs w. w. Wade, sec
ond vice-president; Miss Mary
Zeimer, secretary; Mrs. Dean Bur-
ney, treasurer The next meeting
will be held at the church October
14th, to arrange for the bazaar to
be held October Goth and 31st.
Circle Meeting
The ladies of the Christian
church circle held their first meet
ing of the fall season Thursday af
ternoon Plans for the Christmas
bazaar were made at this meeting.
The bazaar will be held December
and z. The next meeting of the
circle will be held in the afternoon,
Thursday, October 8, at which time
election of officers will be held.
Mrs. Saunders Entertains
Mrs. H. B. Saunders entertained
two tables of bridge Tuesday even
ing. The guests were Mrs. L. H.
Ball, J. F. Powell, w. D. Chase, R.
J. Wood, W. w. Perkins, Miss Mar
tha Hunt and Mrs. Reck, sister of
Mrs. Saunders. Mrs. w. D. Chase
held high score for the evening.
Bridge Party Tuesday
Mrs. L. H. Ball and Mrs. R. ].
Wood were joint hostess at de-
lightful bridge party on Tuesday
afternoon. Eight tables were en-
tertained and served dainty lunch
at the close of the afternoon. Mrs.
Bruce Matthie held high score and
Mrs. Orbra Gray second.
Embroidery Club
Mrs. c. Seigmund entertained the
Embroidery club at her home We'd
nesday afternoon. This was the
first meeting of the club following
the summer vacation Refresh
ments were served and a social
time enjoyed by those present.
Social Tonight
The ladies of the Winslow w. G.
T. U. will hold a social this even
ing at the home of Mrs. A. l.. Dunk
lin, 514 Kinsley avenue.
Entertained at Dinner
Mrs. J. F. Powell, Mrs. r. ]. Wood
and Miss Martha Hunt were din
ner guests of Mr.. and Mrs. L. H.
Ball, on Tuesday evening.
Rassvet = Dawn., 1925-08-19

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International., 1925-09-07
THE RED MOUNTAIN OF
THE KINO COPPER COMPANY

it continuing downward : without
dlmInut-0n.
NOW consider this from the
same above named source: "That
metoric waters have played an
important part at least in the con-
centration of the veinlike portions
of the deposits contained in the
fissures and fractures, there is
little doubt, but the evidence of
metasomatic replacement afforded
for instance, by bands or lenses OF
ore several inches in width and a
number of feet in length, wholly
or in part replacing the hard wall
rock, seems to indicate hydrother-
NAL solutions were probably a fac
tor in the origin of some of the
deposits. These solutions may
have been associated with the in
trusive quartz monzonite magma,
or with later intrusions Of granite
porphyry or ryolite. Rhyolite
intrudes the quartz monzonite at
point half a mile north of the
mine"
Though the foregoing excerpts
are taken from United States Geo
logical survey Bulletin 582, pub
lished in 1915, they form part
of the report made by government
geologist Frank C. Schrader of
his examination of the aforesaid
Red Mountain in 1909. Since
which time but little practical
development work has been done,
owing to internal friction among
the various owners, and also on
account of the Great War. How
ever, the recent consolidation Of
/ the above mentioned and other
properties, by "The Kino Copper
Company" effectively disposes OF
those obstacles. Besides the re-
lated routine difficulties, the
directors of the Kino Company
had also several other hard nuts
to crack-and they have cracked
them successfully. With founda
tons laid for far-sighted corpor
ate enterprise, with properties i'm
med,ately adjacent to the City Of
Nogales, and with headquarters
located in that city permanently
with permit from the Arizont
Corporation Commission to sci
Treasury Stock; and compre
hensive prospectus in the hand.
Of the printer, the directors O.
"The Kino Copper Company pro
pose to proceed to enlist thC
capital to develop the propertie
of the company in the same
thorough manner that have prac
ticed from the initiation of thei
ambitious undertaking = d
moreover, they have no fear.
International., 1925-09-07

you only had on your side Of the
PatagOnlas lime in combination
with other alkalis, acids and SOL
vents, which with the percolating
waters Of past geologic ages
would have leached and picked
up the copper from your huge but
low grade mass, and in their
gravity journeyings through cons
of ages would have dropped or
deposited their supersaturated
concentrated copper content at
greater depth, in some friendly
nook with some affinity and pre-
cIptant, IN such case the Kino
company should have marvellous
deposits of copper in it's Red
Mountain, Prudential (King-Hud-
gin) Mcdowell, Buena Vista, and
other groups. In that case, with
your large area, the secondary
enrichment at depth, in all human
probability would have been such
an imminent prize to seek, that
it would more than justify sinking
to record depths, and l would
take flyer myself"
Such "doubting Thomas" can
be answered briefly and incontro-
vertibly in this wise: "While it is
true that little or no lime exists
NOW on the Kino or West slope
of the Patagonia Mountains. in
former geological epochs that en-
tire section on both sides of those
mountains was covered by huge
blanket of lime. Sizeable strata
of lime still exist on the east side
International., 1925-09-07

The United States Geological
Survey, in It's Bulletin 582, says
Of the Red Mountain group OF tne
old -Four Metals claims, the heart
and body Of which have been ac-
qulred by THE Kino Copper Com
pany":
1T is intruded in the south fault
zone Of the GuaJ aJolote block, where
it, together with some of the ad-
joining older quartz monzonite
has since been profoundly sheeted
shattered, crushed and minerlized.
AS shown in Plate AAIII, it is
sliced by a dominant east-west
vertical sheeting about parallel
with the fault scarp. Under
gound it is shattered and travers-
ed By fissures, seams and frac-
lures tending in almost every
direction, and these are filled
largely with pyite and chalcopy-
rite to such an extent that the
rock mass as a whole forms a sort
of Jrecc.a cemented by the iron
conotent. 1t is stained a brilliant
red on the Weathered surface"
Again We quote from the same
source:
"The deposits are copper bear
ing ores occurring in the miner
lied intrusive quartz monzonite
The ore minerals are principally
chalcoryrite, with some second
ary chalcocite and considerable
pyrite, most Of which is probably
cupriferous. The deposits occur
in the form of subordinate veins,
lenses, stringers, and seams in the
fissures, joints, sheeting planes
and other fractures in the rock
and also to a large extent as me-
tasomattic replacement deposits in
the body Of the rock itself
notably in the walls Of the fissures
and fractures, where solid bodies
as pockets of relatively pure
metallic minerals are Of common
occurrence. The principal gangue
mineral besides the altered rock
and pyrite is quartz, which, how
ever, is only sparingly present
The entire hill, 1900 feet or more
n width and 1000 feet in length
Isl more or less mineralized anC
contains a large amount of low
grade ore, as shown by the cross
cut tunnels. in figure Al. The
minerlization extends through {
known vertical range Of nearly
400 feet from the croppings a
the top Of the hill shown in fig
ure Al and Plate XIII, to anC
below the deepest workings o.
wines sunk rom the lower tunnel
where the geologic conditions show
International., 1925-09-07
Page Seven

LESS than two miles distant.
Biologists say that on that side
while the earth movements
through the ages were marked and
numerous, some remnants Of the
lime still exist. However the same
authorities say that the major
earth movements have occurred on
the west side of che Patagonias.
and that igneous intrusions. frac-
turing, fissuring, sheeting, slicing,
pressuring and crushing were there
on more stupendouos scale than
on the east side. Quite naturally
those seismic convulsions rended
the old lime mantle in all direc-
t1ons, presenting n1yriads more
cleavage planes for percolating
waters to erode, in the lapse Of
millions Of years eliminating the
lime on the west side, while that
on the east side, more solid. with
fewer fractures, was better able
to resist "the remorseless tooth of
tlme," and still stands intact in
places. In fact the lime once
existing on the Kino side of the
Patagonias has been eroded. Once
the lime was there and at time
when It's full elects in depositions
OF metals were far more active
than on the east side"
To elaborate: When those tre-
mendous earth movements of frac-
turing, fissuring, shearing, slicing,
cvrushing and grinding were oc-
Continued on Page 8.)