Weekly Messenger, Volume 5, Number 225, Vevay, Switzerland County, 23 April 1836 — Page 1
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J." ftffif ti3 "if MJiiJiP Lfiai aaisSbJ W Eafeg 6s?g PIASTER'S RETREAT, I3DIAXA, SATURDAY, APRIL, 23, 1S36. VOL,. V. JXO. 5125.
f
TLIR.MVor
l'.niV:D VM) PL rLIS!ir:D ;cur in the upper country of Georgia aid Alak W&Siljf A 55 V. lifiilSX. jb;i!T!-., in Tourainc ii France and other plucks.
fif'v-two imrnbeis, TiuiKv:M" osfsi siti i.s vt all kmc arc found in alirvt
to..i who. if not paid until the expiration of the ! every country and every part ol the earth
f - if i Vo
xvit.ttii tne vear ana t.vo dollviis. i:
i - . i 1 1 .i r i .
anoo. m li,e vaiievs on the sunace ana nr. im- . . . . . . - o ....:".. l .. 4 : I l: ... f l.
.iv.' notion ft ceivea lor lass than six ."atst; epui- u mc iumu i ui ouum
POM.vur, ami Firry ckxts, if "ttitl ;tley are found m the seacoast, and on (lit vear and t .vo doll as, paid i.i jhijrhrsl mountains of the inforiour, on the hill
in at i.:iiti. S ll'.sriib.!
n tie pe-
al.l in advance
who receive
.-
the
papt
topav coats postage.
Africa, and in the cold of Siberia they some
rs hv j limes form a whole coast sometimes a mountain. On the tivunlaino near Capsian sea,
No pi;r JiscoiitmaeJ until all arrearages j'"-v are found above the region of the clouds: are paid,' a t.l notice to stop it scat to thc'of j -hey cover the Andes of South America, at a foe in wriiinir. height cf iC,2dO feet. In t!ie United States, .!,.ri;.,v,-.n!j ;i.iri..1 nt t'.- tisnnl iliaiJitone. cun'ainiiiirxhell. extends with some
r;i
Kvc.nt
advertising eloped ini'cirup
i . . f t x
lions, lroin the primitive rocus oi acw
companion-, w hen S'3 will bo demanded for a J Lnglani and the eastern border ot the Allef em lie. m l s"J for a rmde. paries, to the Bocky mountain.
i he remains of ether sea animals are less
v- - I
fice. or
nrovoJ nroiluce. tleiiereu a
t
a oi'ir-r idace as nmv oe
on. tikvr; iu payment.
I this of-:
reed up- abundant; next to the terlaceous kinds, Ushcs
hire the most frequent. They are found in al- . j most every part of the world, occurring in con-
-;'i?ed masses ot hones and shells, sometimes
iniJedded in a solid rock, and sometimes pet
Or-anirk iWds may be distributed into ji itiou. Amphibious animals are rarely found, . ' I 15.. I :....!. a tij-fl4Ki !i.l nnt tiritl in irrc it
,- crisc: i -!.'i 1:115 wiiic.'i nave prescrveu 'a:iu 11 is nvnnuu m-i ti.n . . - 1 - . : . . r. : " : !.:.!. C 1
lii
i,ir iir.laral slate, at least in part; petrified ;numht i s, titJ aftervhc age in which fishes were ,wa- ii-s. aivl impressions. produced, l'o.il tortoises and lizards have
Tii-.? first class consi-t principally of bones, joecn fo iml in vari-m parts of Europe, and the ...,.l whole skeletons, whica ?fitr having Hatter csncciallv in Ohio. The marine fossil
h -c: dopriw'd of the skin and ileh that cov"-i animals are in a great measure foreign to the ercd thtan, K-maia baiied in the earth, or 'coasts of those countries where they are tound ' concealed in deep caverns. Sometimes they j buried, ;md generally arc of species that are!
are calciael totaily or ia part, wilhojt having! now unknown. It is a singular lact r.owcver,
tastiheir configuration, and sometimes tliey re- ahat r.urope in and American shells, known as
such, have Irequcntly been lounU mingled to-
. i. .. ...
tain noi oiiiv i'"-" iiAiiiiijimi chu iv.iit.im portion of t.V: nd fioli. Pilrifccliv'is ordinarily, rompreliend all the -tonv subs-aces which have the figure o! an or ga nick bo.iv. There have been instances where a liquid impregnated with stony particles has ilj-vo 1 into a cavity formed by an on-mick ba lv which had disappeared. In S " i I i
that case, ihe stonv nnv has now cti into the
CIIKV V C
aether on the coasts of Arrica.
Many singular circumstancesare connected with these monuments of the history of our
The petrified and perfectly preserv
ijioae.
-d sltell is ."('ten found close by llie side of several others, calcined, worm-eaten, and destroyed. Here the beds of the shells lie horizontally, with the concave part uppermost, and with-
iv. iv. and ass.pned the ecxterior form !at any lureiirn mixture; there these remains
of l hi oranick bodv which v as there before. "'- found in the midst of fragments of granT.'t stone beconvs th.c statue of the substance M'-c, of sand, and of clay, jumbled together in which it has replaced. While the process of the greatest confusion. Same fishes have been decomposition is jrraduaily goini: on in a veg- suddenly and forcibly enveloped in the subctabh.'or animifsahsiasuc, it is sometimes 'stance which contains their impression, or rkew-'.s - surrounded ua.l pressed on by a stony jthcir cast in petrifaction. Wc can still pcriuicc. As each org inick particle dissolves and jceive the violent and convulsive contortions "lil-.M-irs-a sfonvo article replaces it. Thusjitito which these animals had thrown thern-
i .- .-i..-,.. ...K.- !sc!vii! i I'spnw tfrrillt catat rnnho of
sriu l'" ai.Cl parui.-e, i.i. r-vu auiisi.iuce ' - -
beria, covered with llieir flesh and skin and long hair, preserved by the frost which prevails in those regions. The remains of this
species have been found in most countries of
Europe, and in North and South America. The mastodon, an animal nearly similar to the. elephant, and which is very frequently confounded with the mammoth, has been discovered in the states of New York, Virginia, Ohio and Kentucky, and in Louisiana. There are said to be five species of this animal, one oae of which also has been found in the high plains of Quito, and another in France. The fossil hones of the rhinoceros, the hippopotamus, and the tapir have aUo been found. They generally seem, however, to have belonged to species much larger than the present known species. We might enumerate a very great number of extinct genera of beasts, birds, and fishes,
varying in size irom the rhinoceros to the mouse, from a species of birds much larger than any at present exist to the humming-bird, and from the whale to the minim, whose remains have been found in dilTereut situations and in different forms. The elk of Iceland, and the great butfilo of Siberia, may be mentioned as holding the first rank. Some of the extinct genera were of a very singular charac
ter, and entirely unlike any that now exit. But In the midst of all these different collec
tions of remains, human bones have never
been found. They have never been found
in any regularly stratified formation ; nor even
iu the beds of diluvial earth and gravel, or a-
mong the diluvial fragments in caves and fi
su res. i ney arc an tiecuieuiy posiuuvian, as
far as they have been hitherto discovered. The same is true of the quadrumana, including the apes and makis, animals which approach nearest to the human furm. If, therelore, all these vast and vaiious collections of the remains of organick bodies, were the effect of some singular revolution of the globe, which involved hundreds of genera in entire
destruction, does it not irresistibly appear that
man did not exist, at any rate in very great numbers, anterior to the last revolution of (he "lobe? What could have involved every organick body in general destruction, but smie terrible revolution, as the deluge, or a sudden alteration in the temperature of the globe?
And what but a deluge coula have piled to-
than (i.jy cities of Europe, it lias nlrcady, in- ern and cenThl bank of EnlHnd,aud rdrsrs. credible as it may seem, and in less than half jAtwood f I ii nurgbam. A charier fas been a century, acquired a rank and importance obtained frm. the l rd lie ii!ei..-.iit of Ireh.ta;, that is only exceeded by six cities, throughout (and has been transmitted to Lcn Ion fcr Lis
the whole extent of the European continent, majesty's sign mai.ual, wi.i. h will be :-AZi d as
pa
. . . i n':'ir!i II'.-1- ill.1 ill i;i I lilt-ill,. -iiiinriniir'..
TaU'l li V nccUOies Ilia spaces m-u a;;.uu i ...
" . . t . . .ii -- - - i t . iT"i(h rr.f-.f 1 1 U-
' nro-wes-uve uecav oi i.;e vejiciauic or am- ii-M'iun i.i..i.i-.n.iiii- .,.. ......wnvrv
l - . . ... - .....!..,
1 n-wtc mt..i hv ut tr.n- m aa Miil in I ores, pi eseius s.niiuiai a M.eai .nice:, muieies
1 IF.I I I - - --- -- - -.- - -
t
mi
nvi.io-:: it conies, feature lor f. ature. the con- nave
texture of the organick bodv. This is the ! petrified shells, with adhering threads of gold
m.nor "m which ihe formation of oetritied : and silver, have been met witn.
v.
London, Paris, Conslantinople, St. Petersburg,; Naples, Vienna, New York, being has already outranked
l.uniin, later pool, Manchester, Birmingham, Edinburgh, Glasgow, Lyons, Bordeaux, Marseilles, Lisbon, Venice, Milan. Prague, Moscow, Berlin, Amsterdam, Copenhagen, PaloTmo, Barcelona, Madrid.
1.500,000 850,000 500,000 350,000 250,0510 300,000 270,000 250,000 200,000 172,0C0 130.000 150,000 150,000 110,000 110.000 120,000 250,000 150.000 130.000 1 10,000 210.000 250,000 200.000 120,000 l(k).0:;0 15-):) 120.000
soon as the Fi bfcriptioii shall have ttci ,lo.i
reasonable extent, tilled up. The most eligible port on the west const cf Ireland has b en se lected for a f'e..tr. racket station, viz: 1 ilmbuy Bay, in the ccujnly of Gal way. fit in wl.irh it is j.ropo.fd tocarrv a rail road in a direct line throus'i Athlonc to Dublin. The distance is only 110 miles and the line of country presents unuual facilities
forth.; formation of a tail read, the country being level and containing abundance of materials necessary for the construction of the work, 'lie a.eiage iiu linaiion throughout the w hole lino is I in 072, and is oblnined without great crnl anl.mei.ts or deep cuttings, and will be entirely live from tum.cls .i.d viaducts. The directors announce that (hry have an offer of as much land as will suffice for tw enty miles of the rail road, the ground rcquisiic. for wharves., docks and Mores, 100 acres of building ground on (lie margin of Biturbuy Bay for ever, at a pepper crrn rent, a:.d likewise the unanimous approval ol the ia;:d owners along the lir.e. Proprietors cf live shares will Le entitled
! to a free passa in the company's ves-Hs be
tween Liverpool and iHiLlin: pr
opnetors ot
lliirlv .!.:!.. o... C...... r. ...... 1. ... V
It must at the same time, not be forgotten,! ica nad Bitniduv. am! eron.ieinr, , f ,.. .1,..
will he entitled to a reduction of ten percent.
that most of the above cities of Europe have
existed nearly or quite a thousand years, and have only acquired their present rank and importance during the lapse of age. Si. Petersburg, if our memory serves us, is the onlv one among them that maybe considered at all cotemporary w ith our ow n cities, hav in" en
tirely grow n up within the last century and a
on the cm rent freights by
. I . I. ..
aiiu me i ii.ugc! n.u ine carnage ol goods
tl'.e steam vesf( is.
i
is
nv
the rail road.
Ten thnusiind shares have been reserved, by special agreement, fortius country. Subscribers will not be liable f..r tnorc than
a deposit of one pound per f-hare (w hit h must
Iw.ir ll.;i ..i..ii.;.. ... i. , .1. . " I. v.
: .......!-.,.. ..mio.ign omraiiKeu nc pa -it on the allocation of the shares ) nr'il m some-degree by the superior growth of New jthc ac t of Parliament for constructing the i
.niveii a p.ouusianu aiong i ro;:l is ohtamed: nor will tl.ev afterward bo
ide, or ahead of tht oldest cities iu Eurone.
while Baltimore and Boston are fast treading upon the heels of eomr that only a few yeais since were out of sight ahead of them. New Orleans is also pushing on with rapid Mi ides, and in the "far West" innumerable to'wns and cities are springing into existence
..,U l- I U, -. C : ... . i-iif4 ucttlir.il.fr :iri imnrtmrp (!. !l C "l IM 1 .
f;eiuci rjueu .irri oecips u, nii me a n i ma is on ; ----... j.... .....v-v. ...... M u.jiu i iece. Liverpool, Dv whom also anpfi.1. . r.i. i .i . . , ' , I; 1 1 !. : i .1 i .. r . . , .... ' . '
i iic iops oi ine iiigiicM moun;ams anu covered 7' "' " " oo ; canon? n r snares y. ii he receive! I, under sen
responsible for more than the amount of their respective shares, which will ho called for hv instalments, not exceeding live pounds per share at any one time, ami at intervals of not less than two months between each roll. Prospectuses ofthe plans of the undertaking ....... l... ! c i i. . i .-. i.
.11... u'li.iiu.iuii j( nil uavis. o. z I.urii-
r.l, bv
them over with e;irth?
Having thus generally surveyed the series
j Some of them already numbered 10, 2.), 30, i,nd endorsed '-iiritisii and Ann-iica! ics of i 'y ueariy .V.000 inhabilan;?. and in the 'course company. . .. . C'..i. .i .-.
inter-
becn found in a mine of loadstone, and solid substances, which form th cru of our-rourSft f a few years, w ill outsliip many in i
They also
filled
O! lie
globe, we shall next proceed to the theory of
the water whica cover its surface.
i 11 I .... . 1 ;l-,-. tr i 1-1-.1.-1 in ..inii.h'ir ..r ,.l ( I , 1
j iil IS usual i v e xpi.t men. .i.nv- v..ij n. -., w.-.j
M-sld'.iz d bodies, an 1 those winch have ; w ith that metal, hoen c!ia!iged into bitumen or into coal, may ! Thus, before our stratified mountains, and be rek rred to the same system of formation, ihe metals which they contain, were formed, Manv petrifactions are, doubtless, formed by ; before the fragments of these mountains, united tn1 crvslaiilz ition i.a the earth, of the siliceous ' together produced rocks and earths of accuse .tier so a'oun.lunl in im;.v organick bodies, 'ovulation, the globe must have been covered
I.nnre-sions are found between the lamina? m a great measure, and at different periods,
certain argil'.. icius schist..; they are the re-'sometimes with the waters ofthe ocean, somevees or moulds representing skeletons of an- times w ith a body of fresh wa er, and lastly,
imils, porticularly ii.'i .-s, leaves, reeds, and with several lluids of an unknown nature, im entire plaits. In Some ofthe western states. ! pregnaled with substances which have envoi
i nprcssions of human feet, have been distinct- joned the madrepores, the shells of marine, !v observed. More recently, it is alleged, tur- and of fresh water animals, and the fishes,
kev tracks hive been discovered in some of the whose petrifactions or impressions we find
schists b-.rderingon Connecticut river in Mas- heaped up one above another. In the immense
sachuseti. succcssun of ages which these tranquil forma
We sh.-.'l now consider the difTercnt classes !tions required, interrupted from time to time of fossil remains. The petrifaction of veget- by violent revolutions, it appears cither that
n.bles seeni to belong to the quartzeous, alum- the mammilerous animals, the birds, and the inous, and magnesia:, schists, rather than to great cetaceous animals did not yet exist, or calcareous ro' Us. Tht; petrifying substance ' that they e xisted in a situation which secured i most frequently of epi u i.-agate, onyx, or ' them against the elfects of those catastrophes jasper, bu petrifactions are sometimes formed : w hich buried the countless generations of the bv pvrites-' Some have been found w ith py-' lesser set animals in the bowels of the earth, rites on one side, and ag ;Les on the other. : There have not, at least, been found any Fossil cars of corn, impregnated with silver, remains of the mimmiferous, nor of the cetawith copper and oilier m-i;ilick substances ccous race, decidedly covered over with a have been found. IV triiicd fruits are very : regular stony bed. A petrified buffalo lias rcrarc. Tine i.avo bccii f'Ui.u oil heights, vhcre ci-ntly been ton ml in the north of Mexico, j.;ow they do nut grow. jnearthc United States, hut it is doubtless of The impression- of vege table are found nl- recent formation and ncarthe surface. Petrimost exclusively in the m.iily and argiilacc- factions and impressions of birds and insects, tins schists. Tnose of leaves and branciies are ;ire rare, and seldom very distinctly marked, comnvn. .-,;; present the most delicate We. have seen petrified insects from Lake traces of the structure of flowers. Many fos- George, N. Y. which w ere very distinct. 4-il plants whi' h are found in one country, are iThe a counts of honey-combs, petrified with now entirely the production t.f a foreign conn-bees, larva; and eggs, found in a cavern of LFptrv. El.islick fossil gum, said to be cahouteh-! per l'gvpt, are very doubtful, out k. wliich grow s only in Peru, has bee.i The remains of quadrupeds, are found acfound, it is said, in England. Piece -s of indi-cumulated in regions where similar animals genotis wood have been found, of which one end do not now exist. The mcgalonyx, an unwas in a natural state, and the oilier bitumin-i known animal of the tribe of sloths, of the size ated. iof an ox, has been dugup in Virginia and some Among the remains ofthe animal kingdom. 'of the Western states, the megatherium is disshells and zoophytes are the most abundant: -covered near Buenos Ayres, and joins to a thov occunv immense spaces, but arc prinei-"character resembling that of the sloth, the
pativ founu m calcareous rocks, .wore than ; mute or nimoeeios. lossu unicorn anu a ti0 genera have been found in the env irons of fossil btar it is said have been found in the Paris. They are of en confusedly mingled caverns of the north of Europe, without any with impressions of leaves, petrified w ood, 'covering. The fossil elephant, which is of a hones and teeth of tfshes. In the Paris basin,! kirn as different from that of India ami Africa, it is a curions fact, that there are two alterna-ias the hoisc is from the ass, has left proofs of
tior.s of marine and fresh water form iliors, in'its ancient existence in all Europe, in I orl lithe following order, viz. lower marine, lower -em Asia and the New World. The islands
th old world whose namce have been f-
to us and our 11 hers before us, fornn hundred years.
Such in fact i the wonderful
impulse be
stowed upon a free people by a free govcrn-
:id such the characteristic vtror with
The Surplus revenue goes on increasing at an alarmim? rate. Thirtv-lhree milhons.se-!
iron hii nil mA nnil fiitv 1 1 .. .ilttn in I iliifl-iis vvrn!''1'
... i- ir, ,iw i . f t i Iwhich a vankee nerves his arm and puslies in the public collers on the lust of Aiareh. ' . . . r... 1 . . , i i i ,t , I, his fortunes in w hatcver direction he sees hi Ihe amount is now probaniv tiiirtv-nve mill-i ... , , . , ,. ,IM i - . 1 , - f ito turn his steps, mr whatever subiect he dilons. 1 he administration is in danger of re-1 , , , -
reis iiir auemiou; ami sucu iiKewise, are uie unparalleled extent and resources of our country, tht without th.c occurrence of some unlooked for calamity or the intervention of a
MAJ. NO AILS LATEST ANECDOTE. Chapi. i.5. One of onr midshipmen at Li.bon, being a little top-heavy, going off to his ship, encountered the Chaplain "of the English flag ship, whom he tumbled into (be river, and he was rescued after a dangerous t ffort. The midshipman o.iert-d to Vive him satisfaction; but when he learnt it was a clergyman he redoubled Ihe offence, bv statin"that there were two Chaplains .aboard 'his shi and the reverend gentleman ' might take his choice for a meeting. We do not know how it is with naval Chaplains at the present time, but formerly there was r.ot much fanaticism about them. Be ing once a prisoner of war onboard an English 7 in the Downs, we were particularly plras?d wiili (lie agrvcahh. nv tmers. and general intelligence of the Chaplain. 'How is it,' said wc,' 'that your nan are always so orderly at prayers?'' Discipline, sir, and system. When they fiist
i i . i .iiciii i iinu iiiii vrin'iv, rinii, fiivti. i eiiiinioti - ' . i -. . . . lo place this matter however in a . , ., , . - . .- . port, a more unruly, disrespectful set t f fi 1-
. . r I I HI, lilt . ..CIH.IIl .IUH-. UI 111- IIIIIIIUIU1I U.IU! I ,.,,. I, , II I -1 . , ,,. stronger point of view, we have prepared a r . , low f never hasnlietl sails w hen musterctl for
va ...v.. V I . .. . I I I
i'l.nur imi oumu.sv, iicai unci clean enough to be m:.-o, but I never could fix (heir attention;
they na:l an abominable trick, t'ui in-' fin
alizing, to its fullest extent, the truth of the maxim of other days. 'Crcscentimscquiturcura pecunniam majorumpue fames."
POPULATION.
foreign war, which mav heaven forfend, we
can sec no limit to our growth, or no rank in
, ... , , . ,!the scale of nation-; to which wc may not asOur principal cities have not only increased . ol ... .. . ., . r , . . . . ' -nire. S hull i . iiib pvit. it lt 1 he tt-islorttl IP
. , . . .... . -. . . . pire. ...uuiiu, ntiTiever, u nr. inc misioriunr with unexampled rapidity in population, but 'r.i- . , - 1 i: ....;ii , , ' . ,l .. 1 .. of this country to become involved in war with they have acquired a standing for wealth, t, . r. -1 J , , . , i i - i i I ranee, or with any foreign nation, after havknowledgc and physical power, winch places . . ,, r i i i i . . o . I. . t ' , ine: nootited all (air and honorable means to theni in an imposing attitude, even w lien con-' , ., , . , . ., , , . , ,-i ,- - v. avoid it, let us enter ifito it with our whole trasted with the most poT crlul nation in Lu- . . , , ., . 1 ,. . .heart and our wholi soul, always remcmner-
rope
fresh water: upper marine, upper fresh water.
The circumstance prove a difference in their -e and origin. Enormous beds of shells are
found in various parts of the globe, many of
them several square leagues in extent, and
in the north of Siberia, it is said, are only
heaps of sand, ice, and bones of elephants and rhinoceroses, mixed with those of great cetaceous animals, and even with the remains of gigantick birds. Whole carcases of (he
. . a 111. . v m f 1 tv
a? fret tr.KK. I !'ct nnmmre nods oc- elephant (mammoth) hare been touna tn ot-
few statistical items, and invite the attention
of onr readers to the follow ing table: At the present moment, the commencement of IS3G, the population ofthe city of New York is 2G0.873 Philadelphia 200,000 Baltimore 1)2,000 Boston 7r,i03 New Orleans (iO.MO!) Charleston 3l,-VK) And this table will shw the gradual increase : New Y. Phil. Bait. 1790 33,131 42,720 13,503 1800 00,180 70,287 20,011 1810 56,303 90,50 1 -10.555 1820 123,700 119,325 02,738 1825 107,059 110,000 70.000 1S30 2'.)3,007 107,811 80,025 1835 209,b73 200,000 92,000 Boston New O. Char. 1790 18,033 0,500 10,359 1S00 21.937 9,500 18,719 1810 33.r,50 17,312 21,711
1820 13,298 27,170 21,780 1825 58,277 35.900 27.5! H) 1830 151,381 57,381 80,280 1835 78,003 00,000 31,500 One hundred years ago, the entire population of the above six principal cities in the U. Slates, scarcely amounting lo 35,000. Fifty ) cars after, in" 1790, when the first national enumeration was taken, it had increased to 129,781, and at the peesent time amounts to 735,000. Such indeed has been the wonderful increase ofthe city of New York within the last 10 or 50 years, that from a population ol about 30.000, when it was outranked by more
''Biiwarp, c . .....
vol enirancr to a quarrel, nut Ueun la
;an i isiev nan an anoauna
ii . . i . . i . .... . i . . - .
iear n unu ine tqpost r may bcvMre ol tin e. . mot s n.-mn part ot the prayers, til puifii'g j ,i r- i c i ,.i 1 tin ir finger in their cheeks, and ptippiii". lik-. And may the God of bat les so nerve our i.. .7: r i ' . i ,i , ! t'e draw ing ol a champaigne. I triet every arms and strengthen our hearts as to carry us : ,i i i " i i , , - , , 4 u !iuethtd, by nods, y inks, severe ooks. cv-c., tt triumphantly through the con est. .i;- .- i . i . 1 J - q this practice, but w ithout fleet. At Otic word more and w e hare done. jlast, one Sunday, a tail for-t.p man. near nui Lei us. above all things else, preserve invi-!amu?iMl himself as Usual; y,Ca, being very olate li-.e union of these confederated States: i VCXC(1' aiil' thrown off my guard, 1 closed the as we could cherish the very apple of our eve,' uo,,'m "ig, 4 Come, d n your eves, no let it be Ihe pearl beyond all pi ice, that w e i xnouJ f that This was a language they w ill part with only, w ilh cur lives. From for- 1U I 'etl'3' understood, .since w inch no crew n eign invasion we have but little to fear fnun'n"lc orderly.' union at home we have evi ry thing to hope.' V0" have an easy time, mv dear Sh !' Our glorious constitution has thus far been i 3 CS? "' nmch tt tlo: I take the head of (! e handed down tons, sacred unsullied ami mi i-' t;ible, prepare the punch, mix the s;ilad, a::d olate then Ictus in the name of heaven trans-1 peper the devils.'
mit the same as a blessed ami precious legacy lo our children pure as the virgin snow, unsullied as wc received it from our fathers.
hv i. the winter so long? is a ouestion of
ten asked, ami answered many ways. Ti. following is the most imrenious. ifnot (he most
Stem Navigation or the Atlantic. Wc 'philosophical reason, wc have vet heard null ive at length succeeded in obtaining particu- vanccd. lars of the project, so long entertained and sol . . , . . . ,, c, , ' .-. v i i r . i i !avs Jutly to Pa, " v ill you tell me n-.v t.c;,r. often adverted to in English papers, o cstab-' t " w u . , , . f . , ' . ,' , : by tiin winter - soI jo--. id ii e er cn.l at hshing a line of steam packets between the' a!M north"" amerioan continent and Great Britain. Lrj VailJv.- The re.sou is, this is Lc-.P vr-nr. I he company is formed by the appointment Allj ,ie Wmivr has lr:qvd oVr .-jum-, t-Vnmxr of patrons ami directors the number ofthe awl fall, first bci"g eleven and ofthe latter nineteen,' And j in-d the nexf winter, which ilms font s witli power of increase. The capital is two! ul tiK-retorc takes up tlonl.le tiua: to go ih,.n;'ii."' millions of pounds sterling, in shares of fifty I pounds each. The fust patron is Lord Mal- Dkvtii of tub uoiiikr of N'.U'ei.r.. grave, lonl lieutenant of Ireland, and the mar-! Madame Marie ! aUiiia Bonap.irte died :;t quis of Lamalnw no is another. The other! Rome on the 22l f I'ebru.trv. S'i.? w a nine are also noblemen. The bankers arej horn on the 2lth cf August, 1750, at Aptcin, the bank of Ireland, the provincial bank of. ofthe Ramallini family, ;md had lived a! Home Ireland, Ladbroke ek Co. of London, the north-! ever since 18 1 1.
