The American Presbyterian. (Philadelphia) 1856-1869, January 16, 1868, Image 7

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NEW AND REMARKABLE GEOLOGICAL
•
THEORY.
A Cambridge geologist, Mr. W. Robinson,
s lately propounded a theory of geology
hich seems to us well deservihg attention.
is statement of the theory is so concise
at we have to quote almost verbatim. He
mmences by stating, what is the fact,
at geologists have not yet helihritbrate
plain the recent submersion of , trie,..l4esert
Sahara, neither have they giVen. :any
big, approaching to a satisfact:oty.At'bount
the drift, and bon Id d ers vf,l4ch-itbound on
e earth's surface. He then peodeeds:—
Prof. Hansen'—o probably the most emi
,at authority among 'living astronomers
,on the lunar theory":----belleves that the
son's centres of gravity and magnitude do
t coincide; an therefore r the-herai-,
h ere we See hafges into a mountain too
h for water, atmosphere, or. life —the
),er hemisphere" being proportionately, de
,:ssed. If there be water on the moon, it
p st be alit on the depressed side, where
ere may be also abundance of life. More
`er, the moon rotates once only while re
r, lying round her- primary, the
light of this world never reaches her
ther side. Now, it is qUite conceivable
• t her divided centres should be made to
nei(lo, and thdt She': ghoul& be• miadi to ,
• ate iu fewer.houxs.than now she requires
• s for that PurpOsc. And if these changes
their shape :and --motion 'were effected,
:y would roll - a 'large' part of the lunar
or to the side we Alee,-and would. also,
airy the temperature ef the whole of the
on, and invert the temperature of the
is now most depressed,, Thempon -would
• n be a globe wrth water . on - troth tides;
all her newest aqueous formations would
limited to one-side, 'excepting 'that Some'
tion of detritus ,borne by. the shifting
tcrs would be sprinkled over the - surface
the hemisphere into which
,they rolled.
short, in these and variOlitibilier ways, if
II an alteration as has been supposed were
take place, there would be left evidence.
'that alteration for the investigation of
ure lunar geologists,. if, such, ; . geologists
• uld ever be.
, submit that geology has already furn
ed us with evidence that has.
era,
• backward to a time remote and at pre
, t undefined, but perhaps extending, to
'ugh not comprising; the time ofthe old
ertiaries, the earth was shaped as. the,
on is thought to be, and rotated-as-thee
on dues; that is to say, rotated -once only
ile revolving round herprimary; the sun.
bmit further, that we have evidence that
one of the last, mighty changes, this
ld's previously divided centres were
de to coincide, the northern hemisphere
ng, and the southern sinking, to the
,n level; and that at the same time the
h received its diurnal .. rotation. .N",o
- scion is' now raised concerning the4e.
d a.ry and primary strata,or the_v_et4ao4 , o-.
id it at Prole& start the interesting in
y whether the rolling of the waters,,oft
s from one hemisphere to the other, be.
' the normal mode of completing such.
es as the earth, the moon, and Mars.
following paragraphs are strictly limit
, o the state of this world from our era
kward to, or towards, the era of the old,-
tertiary formatiOns. My theory is, that
earth was formerly as the moon is now,
ing all her waters in the. northern hemi
ere ; an'dttiat bY the last' - great '-geologi
change, she received her present-shape
her diurnal rotation.
. It is commonly assumed that; from the
e of the commencement-of the priniary
tit, the water of the earth ha:S . lso6n -- dis
,uted in . both hemisphorcs as . now;and'
t in south and north alike, changes have
-,, effected by., the. subsidence ~and, elova
, of different -Portions .of :Obi lah.d. If
,e, assumption was; trucithe secrizgy ,•pf.
mirth and south would correspond -- ;`in
Lr words, the two heMispheres would
,be
logically twins:'- Writ aa-far 'as itivestiga
has been , carried, it shows thakwhile
hemisphere Was a great laboratory for
creation of ifibilliodene and pliocene de
ts in which northern latitudes abonnd,
xterisive aqueous deposits between the
, r tertiary and Omny recent geological
are to be found en the other ,side --of the
ator. , Sir R. I. Murchison atfirnfeid long
that . 14 such as South Africa is "now?..
" 1. have been her main features during
• • tless ages anterior to,the-,l,teatiOn of
n.:.. human race."' Mr. Darwin inTorms us
'-. '..t " no extensive fossiliferous deposits of
, ! e recent period, nor of any period tater
ittediate between it and the ancient tertiary
~,..
:.,ch have been preserved on either side of
tfte continent" of South America. From
M. Woods we learn that the - part of A.us
t` lia of which he treats " is similar to what
rope was immediately after the .
second
period." "Thus," says Prof. Sedgwick,
t erring to facts of this description, "we
I '
tT seem to be almost shutting out from
southern hemisphere the noble monu
, 'tants of past time which decorate'the TOW-.
- . period of the earth's history." To seine
itparent exceptions reference will be made.
the sequel. At present, let it be observed
tt the geological difference between the
hemispheres is confessedly vast. No
lognized scientific hypothesis accounts for
. t difference. All current theories clash
b. it. Assume that the.water , wag form
' and for a considerable geological age,
in the north, and the problem is-solved.
n any other theory be conceived of, that
.
- I solve it ?
t
, .
. .Northern Africa is 'remarkable -for a
.sert of sand 800 miles, in breadth,eand
~..,, • ble that extent in dength. It. stretches
• 4 tward into Arabia. It was recently cov
,i:' 'd by the sea. It perhaps re-appears . in
THE AMERICAN PRESBYTERIAN, THURSDAY, JANUARY 16 1868.
the same latitude in the great sand-bank of
the Bahamas. Geologists have failed to find
a cause for these phenomena. Now, if the
waters were before the existing era all in the
north, they found their coast-line at or near
the latitude 'where the land rose above the
mean level. Clouds would pass from them
southward to a greater or leas distance, ac
cording to the Bteepneas or slownessof the
rise ofthe ground; and the region of perpetual
snow and glaciers would then 'be not near
the North Pole;' hut toward the equator,
leaving ,an extensive .district between .the
sea-shore and the icy heights to be covered
with vegetable and animal life. Thus may
we, by the theory now propounded, account
those evident tykes- bf 'coast of
ancient ocean which have hitherto baffled
all reseireb.
3. Among the most puzzling of all the dis
coveries of modern times axe those chn
nected with the former state of the North
ern Arctic regions. The remains of buried
life, detected' therc 'show thgt ; at- a period s
comparatively recent; the climate must have
been as warm as is the climate of . England
now. The difficulty oil ahcointineor
admitted fact has seen fpult.
:Professor Haugbton calls it, the opprobrium'
Vow ''ttinperiture depends
chiefly ori revel.. The housewife knows thit
when
,t l ll9 water-jugs ace ,splittingwA ff 4opt,
in the mpiertstory, the•wine ainfpotato63tiri•
the cellar are Baby' and t the traveller, find-
ing the heat of northern Italy unendurable,
after,a few honrs'i•ellinib"ng is;SurrOtniled" by
snow and . riyere.of ice. 4,our
: hemisphere
Were formerly sunk helo . w the mean level,
its northern parts being covered by the sea,
save where the mountains rose above it,
those „ n etts would.,haye a, wArin, Apt„,,t,o_ say
a steaniingi 91,1,1 - nat4.`: 4114, iS it be thopglit
that, jn removing one diifieuley, I pan great
i n g..an atlier Gy bappoSin g lasenee tine"'
direct light of the sun,:it obvious to re-
ply that the broad belt of, the earth beyond
the coast, in_i'vhich the gyeatest abundance,
of terrene life would, find its , home, would
receive light by refraction :'that the chenii-
cal constitution of tbe,atmosphere is admit
ted to-have been changed';. -that. , what, we
now call the -Northern. Lights might play
more vigorously and `widely than now • that
the greater part' of-the Fauna then fiving
required probably but little light; and that
a large proportion- Of the existing inhabi
tants of the Arold enyughi u the
night. , • • - -
4 In Milton and Cheadle's narrative of
their journey over the Rocky Mountains,
they describe, both " verbally and pictori&ly-,
a bill rising:from the left bank of the ricler
Thompson. 40 or 50 'feet above the bank
is a very broad terrace; 60 or 70: feet higher
a second, and 400 or 500 feet above the river
a third. They are not masses of sand- like
the Sahara; but are eoinpoSed: of shale;sand
and gravel, the. detritus:, oK. the..monntait2.
The popular opinion is diet Ale highest ter
race was once down about the present sea=
level, and was gradually elevated by press
ure,- from -beneath ; till -the second terrace
was level.with.- the sea when there was a
.
pause in the upward moVement, followed in
process of time by similaryobeayalsi. till Abe
Trt-rd - Crie - ragb — , it is very In ill - V 61 - 0118 tuat tne
terraces escaped ".the enormous fractures
and foldings by which the whole crust of
the world has been disturbed;" and doubts
harden into incredulity when it is found
that, on the oppl e sRe oQ-t t lae .. river an
other bill rises, Alt l
ttik) kimile# o 4Fraces,
4 ,
"of exactrXtAo e li - e'igHt:Pilhw:•argu- ,
ment •'%till, ettinulatiye ; for thesettravelbus
tell such terpacescare:foundtrot 60
,
3,1 46"
all 'nn n the banks of the riye c. unto ita,
junction with the Fraser, but - alsO In vari t is
parts of the continent, and as far south as
Mexico, and that " in' nearly , every case
where they aro'found they occur' in." three
successive tiers.;- -, Assume.that the:waters
have been".,lncTed and, not, the that
formerly the water. stood at -the of
the loftiest terrace; and .was. 7 hr ao great
change in the relativelevelefthe tic; hemi
spheres lowered 300 to 400 feet, and by sub
sequent and , slighter changes - dtainid down
'to its present place and_ heory and fact are
harmonious.
s,Arnong the most perplexing problem&
that await solution is that arising from the
drift and boulders- of, the ,w v
orldirtieular
ly the letter. 'They are found of every size
and form, haying , generally , moved in a
southerly direetion. To account for them,
mart34 - MigttatitOFt the glacial hypothe
sis,-by-which it, is assumed-that-same time
between thertertinvianrthearrentepochs the
norkherp lokiipilhe.rs=WA, -. 5 caP1194,44 ,1 1 ic„P,,
frouutlie.inki to thelfcirty-Second .Or Sozlieth;
degree r of, latitude.-N9 cause_i,s assignectifor
immense imenSe and temporary Mantle Of ice,
or for its disappi3arancel , Nor is there the
slightest ,grouElth for-imagining• that ;it over
existed, except the. : fragments.of ,rock that
have been described and Certain scratchings
here and there apparent on the hill side. If
science admit of such theorizing, it need not
shrink 'from the - seheine of interpretation
given in this letter. ,C,enceiye that, the wa
ter was formerly all in the north, 'Ana that
by far the greater part, of it was rolled to the
south by that movement which' altised 'one
hemisphere and depressed the other till both
found Weir present level, :and `the two'fOld
cause accounts.for the existence of boulders,
for their motiOn, and the direction in which
they have travelled.
6. Shortly bofore the human era, or, as
some say, contemporaneously with man,
there existed in great abundance animals of
huge forrn.` The visite, who glides by rail
from London to the Crystal Palace can form
some conception of the state of conti
vents at the era ,referred to.. Those mon
sters of the pliecene age Aye' Only disap
peared
front the face of the,!.Orth; lint there ,
is strong - grdund for, belaying their 'arinibil.:-
ation was sudden. "It is / impossible," says
Mr. Darwin, "to r,eflent, t on the changed ;
state of-the'AMerec - iiii dontinent 'Niithdut the
deepest astonishment. * * The mind at
first.isArreeistibly hurried into thel•belief, of'
some great catastrophe; but thus to destroy
animals, both large and small, in Patagonia,
&c., up to Behring's Straits, we must, shake
the entire framework of the globe." And
what then ? Is it to be assumed, despite the
evidence, that the entire _framework of the
globe has not been shaken . because we do
not understand bow it, could be shaken ?
Orbigny, an aathority equal to Mr. Darwin
—and that is saying much—finds no way of
accounting for the state of the Ainerican
co ntifients--with out--assiuniag.,--th at the -re-.
pose of .the world was ,follciwed suddenly, ;
by-a ,vast , geologioal
Convtflsion
which destroyed all the animals of these
continents at -,A single stroke:: IcTies-writea
aceidentar and simultaneous anrilhilatiOn
the huge terrestrial animaleWhich inhabited
the American continents. - Both these very
eminent observers bring .before:na tht.ap-,
pearance of!,wide-spread• And sudden des
truction. Mr. Darwin leaves the, phenome
na unexplained: M. Orbigny conceives them
to have been produced by the upheaval of
the Cordilleras, , however, do not
stretch: over stitheient• degrees. df latitude.
Accept the supposition that the waters of
the south were all rolled thither from the
north r aud the ,traces.. of
,thedestrtiction of
life Between the two poleS,' to which Mr.
Darwin refers with
_the deepest astonish-
Men t, 49Iiigeir ro -," rA.I or
7. Ai 1 46 *-el OliglecVl4oll 3 Nl l o4o
by which - Sir C. .Liiirtias,Taid firtiitder
great and lasti,kg , p Aiga_tionsy ibepit may be
found abundant evid'enee—of great effects
produced b7yl,,iihidaelirriiih of wt . oitcrigyer a
smalil.Arca T ..such as ,ro&ds.%.toric lilipn_e the
depth of fifteeliElfeet, in some
aili plart.
otherstilid -aetr tks': . tO t t
depth ; „water3flowiin.gifor weeks*..4ensely
charged witb".olsictinae it coat- begritijout
be in g hatigethi nto mud-; honsesi lOW* y
filled with kiaitkpto:o2le second istolty, and
h uge stques;rollcd, 4,0„k and up 0.1 1 . 1 .Ai5- i -
B,aker describes the : state , of the,iiiVelAtba
ra tit,E,Om"o.sevAgns.4,(ollowe::7l4#*t..oB
are dense svith;•tbe: soil washe&frorti kkost,
fertile:laedscfar,lSrom its point,sk juketigin
with the..Ni,le.; . ipasses of bamboo and drift
wood T toget,lker„, W z ith,' large, ty.ee;;: t s,44' fre
qu e n tly the: 'dead' :bodies of 'Oils and
buffaides,are hurled along 4y_lira ors
in wild confusion." The similar effects pro
duced bylr eataely„sm which-i,moved by-the
far greattirl plirti:of, the waters of ithe ,glbbe
frork,,,,one hernieliere into . the other_ would
be indescribably greak. Aktritus Lo frotal .
the north would be strOvedpvrlth,eirrtitb-;
in 'Borne 'cages cOnsideribit deposits would
be left; and Wher6vetthe 'waters lound , ,An
outlet through, a .eonsiclerable ..valley into
the deep cavities to . . which they rolled,the
muddy traces of their exit would remain..
Therefore, that there should be found, in
many parts of the south' recent - aqueous, and
terrene
.deposits, quite in harmonY With
Alio theory now. ~o ffered for consideration.
One 'example must be given. The rushing
flood, turned eastward. by -the . .. Cordilleras,
would roll down' the valley which 'now finds
,the outlet, of, it's 'streams at the.: 4 l - nouthl
the La:Plata, covering the - ;valleyivith
in which would be entombed the'remains of
'•': • • '" _ • • • c;.‘ - i •• .:
or thrice a 3 large, 7 —and which is described
by Ali. t Dar 4 aa' vased'eposit Cr in •
in which are entombcd,mammiferous re
mains in ,w r enderfal abund• - ince." ; No cur .
rent geological theory accounts, for'
Pampas; for the sudden -,upheaval of th•
Cordilleras, it is presumed, none will accep
as an established ,readei en
tertain asmorthyngeonsideration the . noye
hypothesis now., presented, which. offers ••
solution of the problem?
a f ti
a,3 ' ' (... 21.'7 C". 7 c .„ ..., . ...
' VOW slllMtg - + '' '
lii. i
• -
•
?sac's Ormuz SAil7. O . for Barns, Scalds, Scrofula, Salt Rheum,
Sores, Broken Breasts, Fred Bites, Chilblains, Stings, Bruises, Cuts,
Swellings, kc., whether upon man orheast, is the,most wonderful
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lEEE
Moffat's Life Pills an& Phenix Bitters
were first used in private practice in 1825. They Were introduced
to the public in 1835, shiceifrhfch time their reputation haTextended.
until they have a sale in excess of all other Cathartfc and Purifying
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Bilious and Stomachic dieekiei t 'svitether of long or l sitiiit 11fit - ratirtn.
They are entirely vegetable in their composition, sad harmless to
the gentlest infant. One ingredient - Opens the' po l rkk of the skin;
another is diuretic"; and stimulates proper action o I ! the kidneys;
third is emollient, loosening phlegm and humor rOm the' lungs;
other properties are warming and cathartic, and cleanse the etomach
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byterian Church, Gananague, Cal., of Fever and Ague ' 1
Rev. Ed. 11,
May, Twenty-flat NeeYore Rliertumallsnr 'and. Piles of 25 years
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Moffat's Life Pills are 25 cents per box.. Moffat's Phoenix Bitters,
$1 per bottle. They are sold by all respectable dealers thrmight
h the continents and the I.eands„of tho Ocean.
*MITE k 'HOWLAND, PrOprietors,
Succesenrs 20 Dr..TUHSMOPFAT; and Dr. Wm: B. MOPPAT,
litiettirStiee4 New York '
•• -• • t • •
CLIMAX
iIWLIND'S GERMAN BITTERS,
HOOFLAND'S GERMAN TONIC.
The Great Remedies for all Diseases of the
LIVER, STOMACH, OR IHOESTIVE GROANS.
HOOPLAND I S COMM BkrrERS
L,
Is oomposed of the pure jatoei (or, as they are medicinally
I, termed, Extracts) of Roote, Herbs and Barks,
I mak.iilg , a preparation . , .
Nit
entirely ,frce frail ako,
iloofland's German Bitters.
Those, whohavelso objection to the,lorabinalion ,of the
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. .
ROOVIAND'S GERMAN TONIC.
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• .
ponstipation,', t Flatilfintoso -Inward! Piles, Fulness' ,of .
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8 .
I t i z tl in coih i gitkirit i feat i le t rV i nt or
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i
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,
1 - Itiollaied l lPGiirzFlatt 33!tiers,
HOOFLAND'iIL'OERNIAN TONIC,
PREPARED BY 4facicson, , '
Twilint3rAw‘o: years sine they we re first introduced
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pi
..T a ii n d i OS,' DYSnenliiiiiiroiiiii di-Nervous D e
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C -
' '• - -' ll . - DElgtl_Arriir,
Resulting.frons any Cause whiteverl PROSTRA-
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health); `b'ein'g. ' • ' • '
•
PERSONS.`: A DVANCED' N LIFE, - -
And feeling the hand of time weighing heavily Upon th'em,
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-3L4
Male portion of our popu litioh are - seldom in the.
enjoymunt of good . , , - health; I or, to use their
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guid, devoid of all energy , e xtremely _ nervous, and have no
...
,appetite.
To this. clase . ofilersons tho BITTERS, or the
especially recommended:
, • -
WEAK AND . DELICATE . CHILDREN
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Thoirsaadc of certificates have aticimulated in the hands
of the propritori'buttspace.will - allow of the publication of
' but a few. Those, it will be observed, are.men of note and
of suck standing that they must be believed.
T N
Hon: 'GO°. W. WoOdwira,
. .
Oliief joatice of the Sdpreme court - of PeOnitylvithia, - Miites:
_., . - PhiliidOlphio,'Mnfoli 16, 180.
fit
", I- " find - - gloolland'o ,- - ' Gentian 'Bitterst'- is; a .
good torrid ; useful in die , .' exiles or the digtiotivO'or
gniiond,Of ,grent bone, ! U. in= cakes of 'dob.ilityi
and.ifinit- of .noyons actioniyi Ole system. .. -
itiip.re tyuly . , (}.EO. W. WOODWiELD."•
-Hon. janiels Tliompsoa,; •
Jodge of the Supreme Court of-lAnneylpartia.
April' 26, 1866
ei I considerllo °timid's German BiEtert&a, uaiudbte meth
nine in case of attacks of Indigestion or Dysipsii.."L'.T: can
certify this from my experience of it., •,. !,"rt.
irours,..w4th respect, . -.JAMBS THOMPSONI"-
From Rev Joseph H. Kennard D.D
•
Pastor of the •• Tenth Bdptist .Chitreh;. Philadelphia.
Dr: Jackson—Dear Sir: I have been frequently requested
to connent. my name. with recommendations , of. different.,
kinds of medibines, but reg4lll4 the practice as out of my
aPproprhite sphere ;' I ^ ' have in all cases.declin-'
Da
ed ; hat with'' 'a' f Chit- - proof in various instan
ces And particularly in .- my mkt''. family, •of the
usefulness,-of Dry Hoofland's German Ditteri,:l depart for
once:D.01,1110 8 4 1 course, to..oxpress..my full conviction
that, for general debility of tAe; system, :and, eepeciaity fon
Tiber Complaint, -itii a safe and ,nahatble preparation. In
itioin,e cases it may fail; but usually; I doubt Vet', it will be'
Very Venifteial to thoie Who stiffer from ;the above causes.
-Yours, very respectfully,
. ''.' . ..1....H. 'KENNARD, Eighth,- beloW.Coates;St: a
From Rev. E.D. Pendell.
.
.Assistant - Editor Christian Chronicle Philadelphia.
x have derived decided henefit from the use of Iloofland's
German Bitters, and feel it my privilege to recommend them
as it most valuable tonic, to all who are suffering from gene
ral debility; or from diseases arising from' derangement of
theiliier. • Yours truly,
E. D. FENDALL.
CAL - 0"TICIN.
Hoofland's Germ an r r• --- Remedies . are
gir that the sig nature of C. counter
feited. . M. JACK
-0
SON is on the rapper .of each bottle. All
others are counterfeit.
• Principal Office and' Manufactory at the German Medi
cine Store, No. 6.31 ARCH Street, Philadelphia, Pa.
CHARLES it. EVANS, Proprietor,
Formerly C. IL JACKSON & Co.
PRICES.
Hoofland's German Bitters, per bott.e, . . $1 00
" " half dozen,. . . 500
Hooflantl's German tonic; put Up in' quart bottles, $1 50
per: bottle; or a-half:dozin for $.7 50.
Do not forget•to examine well the article you buy.
in order:to get the genuine. - - - -
For onto` y Drininigto and Dealord everywhere.
' ,
Nettie send; with despath, twelve dozen Alleock's Porous
Plasters. Our daily experience Confirms their very superior
. excellence. • At this moment• of writing a man applies for
one who, by entanglement in the shaft of machinery, had
both his, legs broken, spine severely injured, and was for
nearly a year entirely helpless. Thisman found relief very
soon by tke application of a Plaster to his spine. Ile was
soon "enabled to work, and now he labors as well as ever.
He would'• cheerfully pay $5 for a single: Plaster, if they
could not be.had•at a loWer rate. lam surprised that sur
geons do not make use .of -these perforated Plasters, to the
exclusion of all others; as their flexibility and adhesiveness
are greatly
_ln advance. of all other plasters with which I
arifaccitiainted, while the perforations peculiar to them ren
dered them gre.itly . superior to all others for ordinary sur
. gical uses; ' Knowing the Plasters to be so useful, I have no
scruples that my sentiments should be known.
J. W.-JOHNSON, M.D.
PHILADELPHIA, PA.
over ten years, so es to be entirely helpless and unable to
do any itind of hard work. In June last I procured one of
ALLCOCK'S POROUS PLASTERS and wore it three weeks,
when . I found-my back entirely cured , and was able to mow
and cradle as well-as ever. I could in my best days.
•• • . STEPHEN PUGSLEY.
. .
40 Tj JEL 30 i,
AR4 OFTEN EFFECTED
BY SIMPLE MEANS.
LET THE INTERESTED READ.
Pain of the Back, Cheat, and Side.
When there is pain, upon pressure or without, especially
of the ribs, of the sacrum or breast bone—in aching from
sprains or bruises—in stitches or cricks of the side, kidneys
&c,—in local affections, where strength or support are neededs
ALLCOCK'S POROUS PLASTER
AFFORDS PERMANENT RELIEF.
Being flexible, they - give no trouble, are wonderfully pre
ventive.of
Colds, Coughs, and Sore Throats,
and no application sooner relieves those troublesome maladies
HISTORY OF, &c., .Ic.
ALLCOCH'S POROUS PLASTERS are the result of stu
dies and experiments of Dr- Sehecut, of S. C., of Dr. Wni.
Wagstaff, now Baron Wagstaff, of Horace 11. Day, the dis
tinguished manufseturer, of rubber goods, and of Thomas
Allcook, Chemist and Member of the College of Pharmacy
of New York, now Col. Alloock, &e., Ac.
Medical. men of all are unanimous in their favor.
- . HAATFORD, Corm., Nov. 11, L 864
MESiis. T. ALLCOOK & Co:.
ALLENTOWN . , PA., April 4,1865
MESSRS. T. ALLOOOl‘...t- CO., •
DEAR SIRE: , My daughter used one of your Porous Plas
ters. She had a very bad pain in her side, and it cured her
in one•week..
Yours truly,,
An Important Utter.
SHRUB OAR; Yonirowx,..N. Jan- 19, 1860
T. ALI-COCK Co
GENTLEMEN:-I have been troubled with a lame back
The Really Great Plaster.
ALLCOCR'S POROUS
has the compactness of kid, and the flexibility of a silk
glove.
Dr. I. T. Renderson's Letter
PARNVILLE, LA., March 8, 1550
DR. T. Ar.Lcocw—Sir: I have been suffering under a se
vere attack of neuralgic disease of my bowels for years, with
hypertrophy of the 'heart, and bade tried everything known
to the practice of medicine from the very best !CD's., but
truth prompts me to say that your plasters have given me
more permanent relief than anything else I have used, and
I believe will produce aperfect cure.
The counter-irritant effect of your plasters is produced in
such : a mild and graflual way, , they so invigorate the circu
lation around the partsto which they are applied, and ex
ert upon'all.nerirous diseases such a great sedative influence,
that I place them confidently at the head of every plaster
now in use. • , - .
Yours, Tory truly,
_I. T.. RDNDERSON, M. D
--- galSt7-3.11 n, .y 111.61, .1. as - vistrinriny.cousin in orning,
who got me one of your Portous PIASTERS for my.chest.
I was so sore through me at the time I could hardly speak
or breathe. It was not more than three hours after I put it
on before I felt comfortable. I bad suffered very much
from soreness of the chest,. with cough and hoarseness, for
months; • but your
. plaster has cured me, and my health
better than it has been tor years.
YoUrs, Respectfully,
PIIEBE PATCIIER,
BrLivzn DAM, Schuyler Co„ : .!T.Y., Sept. 14, 1566.
Cure of Crick in the liable and Lumbago.
LYONS; N. Y., July 4, 1562
.
MOSIts. Ati.COCH & Co.—Please send !lie a dollar's worth
of youv plasters. They have eured,,xne of a crick in the
back which' has 'troubl'ed me for some time, and now my
father is going to try:them for difficulty about the heart.
L. H. SH.ERWOO D.
Where One was Odd a., few Years ago, a Thousand
Are Sold Now
They strengthen, warm, and invigorate the part upon
which they are. applied, and relieve nervous affections of
the bowels, lumbago, pain of The side, and usually all local
pains. In affections of the kidneys they are of great ser-
Lime Back.
NEW Yomr, Nov. 230359
T. Auccoor Zi•Oo
GENTLEMEN:—I lately snffered severely from a weakness
in my back. „Having heard : your ;plasters much r-com
mendedfor cases of this kind, I procured one, and, the re
sult was ' ull I could desire.- A single plaster eared me in a
week.
Yours, Respectfully,
• • J. G. BRIGGS,
Proprietor of the Brandreth House
Agency, Braudreth Rouse, New York.
Sold in` Philadelphia by
Johnston, Holloway & Co.,
nd all Druggists.
WISTAR'S BALSAM OF WILD CHERRY
Fot the ettee'of Coughs, Chidt, Hoarseness, Asthma, Influenza, Croup,
_Bronchitis, Predisposition to Consumption, &e:,
This great remedy is too well known and is performing too mneh
good to mak2 it necessary to go into an elaborate discussion of it.
merits: Suffiee it to say that it still maintains its supremacy in
curing diseases of the most obstinate character, and that all who
starer from the above complaints, after having tested this remedy,
seldom have occasion to resort to other appliances to Insure a per-
feat restoration to health
Testimony of Mr. PETER SHAW.
WEST T. w
INFIELD, N. Y, Dec. 10, 1660
Messrs. S. W. Fowls k SON, Boston:
Gentlemen—During the winter of 1858 I was very much out u s e
health, afflicted with a severe Cough, Pain in the side and Litngs,
and a general depression of health to such an extent as greatly to
alarm myself and friends as to the result. During this time I trb
several highly recommended remedies, with little or no good re
sult, and bad concluded to try the erect of a Southern climate
upon my health; 'but, before carrying this resolution into effect, I
was induced by the urgent solicitation of your agent, Mr. Mundy,
to give Dr. WISTAILN B&LSAM or WILD CHICORY a trial. I did so, and
to my great joy found immediate and permanent relief by th I
be
e vse
of only one bottle, and lam now in as good health as ever.
tiers your. Balsam one of the best remedies, for Coughs, Colds, nod
all Lunyi Diseases, now in use, and cohscienthinsly recommend it
ss
such
,Yours truIy,PETER SHAW.
•
Prepared by SETT( W. FOWLE k SON, IS Tremont St., Boston,
nd for sale by druggists generally._______
A POSITIVE CURE FOR SCROFULA
In all its manifold forms
T. W. Ilossou, Eaq , of Parkersburg, West Va., writes to Dr. An
ders, July 3,1366, as follows:
bed 37 Running Ulcers when I commenced taking your lo
dine Water, and am now entirely cured of Scrofula."
Dr. Anders , lodine Water
is a pure solution of lodine, toithout a solver* Me most 'powerful ri
&dieing Agent. and . Restorative knaton. Circulars free.
J. It. DINSIIQRS, Proprietor, 36 Dey Street, New York. Sul
by all Druggl sts: •
. .
JOHN V. N. HUNTER.