davidaulloa/AmericanStories huggingface dataset:
Cresco plain dealer. (Cresco, Howard County, Iowa) 1913-1945, 1916-10-13

Germans, thus showing that he Is en-
tirely in sympathy with him and his
like. None Of the republican press
doubts for moment that Hughes is
just as pro. ally as his spokesman,
Roosevelt. I wonder that the German
language press fails to take notice of
these facts which tell all German
Americans in plain language. as plain
as can be, that the republican party in
tend to use the German vote merely as
a catspaw in this campaign. The blind
'anything-to.beat Wilson sentiment of
theirs is q valuable ally in the fight of
thelenemies of peace against Wilson,
and the Republican campaign leaders
play very clever game in playing the
German vote out against the president.
If we fail to see that now, we shall
have to see our grievous mistake after
the election. when the mask will fall off
the faces of false friends if, unfortu-
nately, the president should be beaten.
l fear when the game is up, German
voters will regret to see that they have
been sold In the hands Of Hughes
and the republican party the issues the
German-American stood for will be
handled in rough-rider fashion, and,
what is more, Americas hitherto wise
and peaceful course will be put in the
gravest danger. Dubuque Telegraph
Herald.
Cresco plain dealer. (Cresco, Howard County, Iowa) 1913-1945, 1916-10-13
hi, !, the Year to Defeat G. N. Hausen

This is the Year to Defeat G. N. Haugen
If all the Republicans and 1ndepend'
ents who want congressman Haugen de-
feated would vote against him this fall,
he would be defeated. But doubt as to
whether their votes will be Thrown
away" restraints many of them; they
doubt that there is chance to defeat
him.
This fall he can be defeated, and he
will be defeated, if these Republicans
and Independents vote their wishes.
Carl Evans of West Union. man
with life as clean as hounds tooth,
and with hundreds of friends oil over
this district, is in the campaign with
the purpose and with the expectation OF
being Congressman Haugen's successor.
We ask the Republicans and lnde-
pendents if it would not be . relief to
have Congressman Haugen retired?
For Is wears he has been the fourth
Iowa districts representatives, Wash
ington. Is not that long enough-too
long-for = man of his incapacity?
It has been demonstrated that he
cannot be defeated for nomination. He
has certain political cunning and q
system Of distributing oleomargarine
speeches, free seeds, books, and other
government belongings that enable him
70 take the Republican nomination reg
ularly. If he is not to stay in Office the
rest of his life, he must be defeated in
the fall election. And his defeat can
not be accomplished unless Republicans
and Independents, who are tired OF Mr..
Haueen, vote for his opponent. In
Carl Evans they have man, in voting
for whom any voter may feel satisfac-
6on.
Let every Republican and Independ-
INT bear this in mind. The fourth Iowa
district will have to endure Congress
man Haugen, until you men BY your
votes in . fall election say that the
IsO. 600 people of this district have en-
lured him long enough-Decorah jour-
~.
Cresco plain dealer. (Cresco, Howard County, Iowa) 1913-1945, 1916-10-13
Issued on Friday of Each Week
Courage and Vision Mark wilson.

~O010Ss
81 people of the United States
who are on trial, not Woodrow Wilson.
No President in history has been call
ed upon to face such a succession OF
tremendous problems; no President IN
history has ever faced problems with
more courage, vision and statesman
ship.
His international policies have given
us peace with honor; his domestic poll
cies have given us prosperity and JUS
tice.
Not one of those who oppose him has
dared to file bill of particulars against
him: not one has had the manhood to
say boldly what he would not have done
that Woodrow Wilson has done, or
what he would have done that Wood
row Wilson has not done.
Only general attack, only blanket
criticism, only peevish fault-fnding,
only base alliance with every foreign
country that is in controversy with the
United States.
Never were issues so plain; on one
hand President who puts America
first. and on the other hand, those who
put party first.
Patriotism versus spoils; empty
promises versus splendid performance;
Democracy against Toryism, prog
ress against reaction, honorable peace
against Financial Imperialism, even
handed justice against Special Privl-
lege, prosperity against panics.
To reject Woodrow Wilson is to re-
iect the wise laws that have given
American industry and business such
amazing impetus.
To reject Woodrow Wilson is to re-
iect the foreign policies that have
given us peace and honor and highest
standing.
To reject Woodrow Wilson is to turn
the United States over to chaos be-
tween Nov. End, 1916, and March Bird,
1917, for his reputation involves the
surrender Of every American conten-
ton with foreign nations.
Do you want to drop pilot who has
steered US safely through the rocks and
storms?
You do not have to wait until elect
ion day to make the one answer that an
American can make.
An immediate contribution to the
Woodrow Wilson campaign fund puts
you in the fight at once on the right
side.
Against the millions of the oppo-
sition, Woodrow Wilson places entire
dependence upon the free offerings OF
the people.
Send your contribution today to this
newspaper. Your name will be print
ed on our roll of honor" and you will
receive handsome Autographed re-
ceipt from Wilbur w. Marsh, Treas
urer of the Democratic National Com
mittee.
Cresco plain dealer. (Cresco, Howard County, Iowa) 1913-1945, 1916-10-13

For Satisfaction bull Is months
old, well built, color dark rec.
MRS. JOSEPH BoUsKA.
Cresco plain dealer. (Cresco, Howard County, Iowa) 1913-1945, 1916-10-13
Choice Shert Hem Bells for Sale.

Twenty extra good young bulls, sired
by Prince Buchan s63849, and Kings
Prince 395S4O. age 3-l5 months. viii
also sell some very choice heifers.
Colors Of both sexes, red, roam and
white. Ph. BARTHELME & Sons,
DEBORAH, Il.
Cresco plain dealer. (Cresco, Howard County, Iowa) 1913-1945, 1916-10-13

nmidni tof
and like beautiful Of
the The SO
few olars in
yet done,ju unchanged
know
the the without notice.
Who buingma
oreaiz of the materials market
of 34OO
order"
orkorde" through
the completed and materials at their
will be possible increased
how diigent has been the
halmerse effort 8
would be Chalmers the
722
Lowerh
ITSELF And
Is compromised
would be like Iisso picture to fit price
Aslo theresa namce
Sales
by
And hereub rsaysth
ninuedn
might will be exactly like the would buy spring
earnedA so
odsuto Of
Ale Just aboutpa your sat the for
Or
that hisnt
L. e. BAUER, Dealer, Cresco
Arizona republican., 1916-12-15

It is very easily recognizable Tn all but few places 1t is of a dark wine red color and very coarse grained It lies almost everywhere directly on top of the schist and diorite almost flat excepting where it has been faulted
 Beginning at an altitude of 5950 feet, directly above the old smelter of the United Verde Copper Company it can be traced, with but one or two breaks right down the east side of the range past the Copper Chief mine. It is ab- sent in the upper part of Mescal Gulch and for a distance south of the Pitts burg X Jerome mine because in this locality the schists, during Cambran times were not under water A small island of schist existed here which was only submerged during the following Devonian period when it received a capping of limestone. The remains of the old Cambrian shore-line about this island of schist can be very plainly seen in Upper Mescal Gulch near the old Log Cabin. At this point thin white bed of sandstone changing into the thicker red stone marks the waters edge in those ancient times.
 At Walnut Springs the sandstone is buried out of sight by fault to which the writer has given the name of the oouln ftdyileS lduit- Akdln Just aDONt the Haynes shaft in the old sandstone quarry it's outcrops show two steps faults and further north it is faulted again by the North Haynes fault and disappears under the limestone. To the east of Jerome and the great schist belt only two exposures are known to the writer. These occur. one by the lower ore bins of the United Verde Extension company at an altitude of 1850 feet and another just below the Copper Chief mine at about the same altitude.
 This great difference in elevation be- tween it's position on the west side and that on the east side of Jerome gives with considerable accuracy the throw of the great fault that runs down northwest and southeast along the range and to which the name of the Main Fault has been given,
 By careful study of this sandstone the miner can usually foretell the depth of overlying lava and limestone
Arizona republican., 1916-12-15

original primary ores are found still of very high tenor, and these primary ores show even to great depth num- erous zones of relative barrenness and enrichment.
 The oxidized zone above referred to has left, whenever the deposit has been exposed on the surface. very large croppings of quartz and iron oxides tgossans) and this holds true for the ore body of the United Verde EXten- sion company, which Is not exposed on the surface but Is capped by some 6OO feet of limestone and lava.
 Were these removed this ore body would show the same surface indication as the other large known deposits.
 The oxidized zone consists ot siliceous sands. containing certain val ues in gold and silver that in some of the mines are of considerable economic importance. Certain associated miner als have occasionally formed concen- trations in the oxidized zones so that occasionally punches of secondary lead ores. manganese, and other rarer met als are found. These are of no inn portance, however.
 Whether the ore bodies are of the same period as the diorite intrusions or later may never be known. Certain 1t is, however, that they were there be- fore the overlying deposits of sand stones or limestones.
 The ore seemse to be replacement of both diorite and schist perhaps brought about by the solutions that ac- companied the intrusion of the diorite and at or near it's contact with the schist
 Nothing positive is known "n this point. Perhaps study by the gov- ernment may throw some light on the origin and manner of deposition of the ore. Without further data speculation in this subject is idle.
 cambrian Or Tonto Sandstone This bed of sandstone, which reaches a maximum thickness of only 90 feet, is one of the most important rocks of the district from the miners point of view | By studying its relative position tho great post-mineral faults can be trace with great accuracy ard their throw carefully cumputed.
Arizona republican., 1916-12-15

that he will have to sink through to reach the underlying ore bearing Gchist.
 There are two systems of faulting in the district which occurred during widely separated periods. The first, during -Cambrian times, faulted the schists and diorites and also the ore bodies, but not the sandstones and limestones which were not in existence when this system of faults occurred. These old faults were, judging by the present underground knowledge we have of them. of relatively small dis placement, rarely reaching d throw of over 100 feet. They are more in the nature of contraction slipss Their course is usually east and west or north and south and they no doubt proved pathways for some of the acid dikes.
 These faults, while of great interest to the miner. must be studied and traced for each property individually. They have no place in a preliminary survey or on a map to as small a scale as that which accompanies this report.
 Modern FauIting
 (Post- Tertiary)
 This faulting caused tremendous dis placement. the throw at one place hav- ing been accurately determinedVto be 1900 feet.
 These faults occurred after all the present rocks were formed and cut them all.
 The principal one has been called the Main Fault and is locally known as the Lower Contact
 Two other large faults have been named by the writer, the South Haynes Fault and the North Haynes Fault.
 The Main Fault
 This fault extends beyond First View to the north and beyond the Cop per Chief mine to the south.
 It's strike varies sligE..y at various points in it's course but approximates north 40 degrees west for the whole course Its throw at Jerome is 1900 feet, all the country to the east of Jerome having dropped that distance. This can be accurately determined by the difference in elevation of the Cam
Arizona republican., 1916-12-15
IN THIS DISTRICT THE BAN HASBEENPUT LIN W|LDCATT|NC

and while he has not yet submitted his report it is understood that "pre-or- ganzation stock" will be mentioned in the document more than now and again. MT. Harben while not making public his findings, did not hesitate to say that his office was watching close ly all promoters. He insinuated that justice would not deal gently with of lenders His office is keeping tab on all agents who are disposing of pre- organization stock. and if the com pany is not incorporated and the shares issued the law will take it's course.
 The Jerome district does not hold out many promises to the wild cat pro- moter The companies that have sold stock have in practically every case put the money so derived right into the ground, and in their legitimate eff forts to make a mining camp are not holding out hand in friendly welcome to the man who has not the same idea.
Arizona republican., 1916-12-15

Every attempt has been made to check wildcatting in Jerome
 The camp, while not entirely free from the shoe string operators, is be- ing protected in large measure by the attorney general, who is making d close investigation of the copper zone.
 The activity of Jerome. far exceed ing that of any other district. has lured men from every section of the coun try, and with the thousands who have driftcd into the boom land have been d few undesirables. The number has been lessened by the prompt action of County Attorney F. w. OSullivan, who finding a trace of Illegal promoting at once resorted to the courts. Fines, have in a measure succeeded in halt ing the selling of stock in claims far out of the mining district. if there be claims at all
 Assistant Attorney General George Harben was on the spot not long since.
Arizona republican., 1916-12-15

300 to 400 feet below the country to the south. This fault also has a small fork extending down the Haynes Gulch. The gulch was formed in this fault. eroding it's way along the break and leaving on the south side of the gulch an isolated piece of the Cambrian sandstone perched up on the hillside just below the railroad station.
 Outcrop of Ore Bodies
 A study of the three large known ore bodies of the district namely. the United Verde mine, the United Verde Extension mine and the Copper Chief mine. all show that the crest of the ore body, whether on the surface or as in the case of the United Verde Exten- sion, covered by the limestones. was composed of large quartz and gossan outcrop. In each case the original mineral through oxidization has left on the surface very large and unmistak- able indications of the big bodies found below. In the case of the United Verde Extension mine these silicous croppings happened to be covered up by the Cambrian sandstone and limestones. below which they oxidiZed. Were these sandstones and limestones re- moved however. similar croppings to those at the Copper Chief mine and the United Verde would be exposed. Summary of Notes for Practical Ap-
 pIication
 The ore-bearing formation is the pre-Cambrian complex of schist with diorite intrusions and acid dikes. The ore is found in both the diorite and schist as pipes occurring where the schistosity is marked.
 The ore bearing complex underlies the limestones and sandstones and therefore the ground under these lime- stones is good prospecting country and perhaps better than where the schist has no capping, for the limestones may hide croppings that would otherwise show. Seeking for cropping of an ore body under hundreds of feet of lime stone is. of course, rather blind pros- pecting but the history of the United Verde Extension find under such cir cumstances will no doubt stimulate
 Continued on Page Eight)
Arizona republican., 1916-12-15

brian sandstone. Above the town it is at an elevation of 5950 feet while near the Slaughter House it's elevation is 1850 feet above sea level.
 The dip of the fault is to the east and seems to vary considerably. At Jerome it is probably nearly 65 degrees below the horizontal and it seems to get sleeper in depth.
 On the surface it can easily be traced by following the line of contact be- tween the lavas and limestones with the schist belt. This contact is the fault Under ground it shows as a badly shattered zone from so to 200 fee, wide. This shattering. however. seems to have been caused by a slow shearine rather than a sudden break and it cer- tainly followed the planes of weakness along the schistosity of the old pre- Cambrian schists and diorites
 The South Haynes Fault
 This fault extends from the Summit between Mingus and Woodshute noun tains northerly to and just beyond the Haynes shaft where it is cut by the | North Haynes Fault
 It crosses Mescal and Walnut Clutches passes by the Verde Grande shaft on the west, cuts through the hill above the United Verde smelter and can be clearly seen coming down this hill to the Sandstone Quarry on the railroad.
 A fork of this fault extends from the Verde Grande shaft through the United Verde power house and past the Haynes shaft on the east.
 All the country to the west of the fault has been dropped about $50 feet in two steps. These show very inter- estingly just above and between the Powder House and the Quarry. By di- recting the gaze to this slope the red Cambrian sandstone can be distinctly seen broken in two steps leading down to the quarry.
 The North Haynes Fault This fault runs almost east and west through the Haynes Gulch. starting al the main fault south of the Glory Hole then passing just below the railroad station and continuing on up the first gulch just north of the Haynes shaft. The country north of it has dropped
Arizona republican., 1916-12-15

Continued on Page Eight
Arizona republican., 1916-12-15

The following are extracts from the
New Mexico state record. (Santa Fe, N.M.) 1914-19??, 1916-12-01

value OF the arrangement of this part
OF the house will be appreciated by
every housewife. At the rear Of the
kitchen are the pantry and the rear
porch. Both Of these may be used to
very good advantage In connection
with the kitchen. The pantry Is at.
ted with shelves and q work table. A
large window furnishes an abundance
of light. The refrigerator may be
placed On the ear porch, and. since
this porch Is open on one side only. q
great many uses may be found for the
porch during the season when the TEN.
perature will permit Its s -
There are two bedrooms. each hav.
ing a large closet, one at the front Of
the house and the other at the rear.
A hall connects all rooms with the ex-
ception Of the dining room. There Is
a closet In the hall which furnishes o
handy place In which to keep extra
b~edclOthes. The bath Is roomy and
we'll equipped. A special feature In
this part of the house is the clothes
New Mexico state record. (Santa Fe, N.M.) 1914-19??, 1916-12-01
ATTENTION TO CARE OF MILK
Average Farmer Can Apply Principles
Of Sanitation as Well as
Small Dairyman.

With the advent Of the bacterial
count that is run on milk in larger
cities Of the country, and the careful
inspection of diaries by state officials
more attention is being paid to the
care of milk In all phases Of its pro-
duction.
Although the bacterial count is not
practical for the product Of the aver
age farmer the principles of santa
ton can be applied by him, almost as
easily as by the small dairyman. Wash
ing the udder and teats Of the COW
and drying them each time with a
clean cloth before milking is one of
the simplest, and yet most important
steps.
Reliable dairymen have said it is
impossible for clean milk to be pro-
duced If the mixer works with wet
hands. Almost invariably B. coli "a
cause Of intestinal troubles) will be
found in the milk that is gotten I'M
der such circumstances.
New Mexico state record. (Santa Fe, N.M.) 1914-19??, 1916-12-01
SIMPLE RULES BEST
Authority Is Of Opinion That the
Country Has Too Much Au.
t0m0bile Law.
SAYS PUBLIC IS NEGLIGENT
Refusal Of Pedestrians to Observe the
Simplest Rules Of Personal Safety
Responsible for Immense Ma.
jority Of Accidents on
Highways.

I'VE now have too much automobile
law. The next trend must be toward
the elimination of all unnecessary re.
qulrements. and the enactment Of q
few simple rules and regulations that
may be easily understood, easily en-
forced. and, as nearly as possible. uni
versally observed. Such an elimlna.
ton would in many instances do away
with vbout three-fourths of our pres.
ent laws"
II. M. Rowe Of the American Auto.
mobile association, thus set forth the
present problem of the motor car own
er. Continuing, he says:
1T is needless to say that the motor
lists themselves deplore most keenly
the steadily-increasing number of ac-
cidents and fatalities O%ccasioned by
the use of the motor car, but the peo-
pie have not yet come to fully realize
that these accidents are the result of
negligence on the part of the public to
observe the simplest rules Of personal
safety, rather than neglect on the part
Of the motorist. The utter disregard
Of his personal safety shown by the
average individual when occupying the
public highways Is appalling.
1T is a matter of u%ndisputed record
that between 80 and 95 per cent of all
the accidents that occur result from
the neglect Of the individual pedestri-
an, and less than 5 per cent are caused
by the direct fault Of the motorist or
the reckless use of the motor car. Ly-
ing between these figures somewhere
are from 3 to s per cent of the acct
dents where both parties are respOn-
sible.
simple as 1t may seem, a set Of
traffic rules and regulations that will
work out in practice r not easy to
prepare. 1t follows that rules and reg
ulations which will work out are those
that will permit vehicles and individ-
uals to move with the largest degree
of freedom without coming in contact
with each other. Through cur legis-
lative board we have set about codi-
flying such a practical set of traffic
rules that may be easily understood
and enforced. We are hopeful that
they will be generally adopted. OF
course, there will be notifications in
different instances, and, of course,
they will be attended by varying de-
grees Of success in their enforcement
and in promoting the purpose of their
enactment; but we believe that a sub
stantnl uniformity can be established
throughout the country"
New Mexico state record. (Santa Fe, N.M.) 1914-19??, 1916-12-01

and sightseeing tours in their cars
will welcome this patent baggage car
rier. A rack is carried above the hood
so that the baggage holders are sus-
pended on each side of it and clear of
the hood cover. A bracket Is secured
to the dash portion of the car In this
invention Of a New Yorker. Forward
ly arranged supporting posts are piv-
otally connected to the rack. There
are means for d~etachably securing the
rack to the bracket, as well as means
for ~detachably securing the posts to
the chassis frame. With this device,
father may now allow mother and the
girls to take as many clothes as they
wish without having to dig his way in
and out of the car whenever a lengthy
trip is contemplated-Farming Bush
ness.
New Mexico state record. (Santa Fe, N.M.) 1914-19??, 1916-12-01
BEST Time TO CUT
SUDAN GRASS CROP
Best Hay Yield Secured When
Cut Just After Full Bloom
Holds Up Well.

(By j.. F. NICHOLSON. Agronomist, Elk
pertinent Station. University OF Ari-
zona.)
Sudan grass yields the best hay when
cut just after full bloom. There are
times when 1t is advisable to cut the
hay before it has reached full bloom,
on account Of removing the first cut.
ting, so as to get a more abundant Sec
ond crop. If the season is short it may
be impossible to get two full crops, and
in this case it would be better to cut
the first n prematurely. Sudan grass
will probably stand longer without de-
teriorating in its hay-producing quail
ties than any other of the forage crops.