The New-York Tribune Newspaper, February 13, 1867, Page 5

F.ureryt 10 y Y 13, 1 nd eome dowr to | evidence, When I fo Brasil two years ago, on the first w‘éfiofl my ms! Rio de lln’:‘i.m, l‘gm- s e e Hay ot Bic mud hs g ckatle traces of the !on‘ur action of .lmum::fl co ‘. < MOVEMENTS OF GEN. HOWARD. BY THLRORAPN TO THE TRIBUNE. 81. Louts, Feb, 12.~Major-Gon. Howard arrived bere yesterday from the East. NEAV-YORK DAILY TRIBUNE, WEDNESDAY, FEBRUAR another curfous phenomenon in the glacier. Suppose e | hefe move very slow! 3ia h-voll;mulsllrgo fire, and I place wwmn the anl::d g‘y:n l;u‘m patt ofozhz we:h:t:edr [y M‘ long myself a larg —8 ne o : e same be th il gm oF gt and hee tho tirs and the dase with the howiers Aok fiag: 1 shall see thi ments of rocks which are upon the blaze, but I shall not foel the heat, because although | margin of the glaoier, the n‘l’:llo)‘nh::eu‘mde\-'nfll-fiw But it 18 transparent to the ght, it is opaque to the heat— ou see that 'fimt is bere margin, and woves liwb' heat does not readily pass through glass. Hence it isthat | Tindicating the inner margins of t! wo uniting glubn}' we maks 'P‘?W of glass, which foterferes with [ when the two branches of the glaciers meet, becomo the chahge of emaeh ure from within and without. | the conter.of the commpn glacter. Suppose two rive Take nstead of such a glass scrgen a plate of ice, an ico | which flow into one basin, and which uuite. The wite kr% , 6ud place it between m and tho firg and you | flowing in the two rivers by the two sides which mes i bocome the center of the nver. So it is with ers, a8 they weet Lere. The right side of this LEOTURE BY PROF. AG. ON THE ANCIENT 5 OLainis OF TRE TROPICS. P largo and sppreoiative audience asscmbled last avoning Lo Usten to the third lecture of Prof. Agassiz. oTné partioular subject selccted for the lecture was “The ABalpnt Glaciers under the Troples” On coming for” | will hiyve the same phgnomenon, as to viewing the light— “oward the speaker was recoived with applause. He then | the hlaze Will g séen—bul the heat will pass through. A | the glaciers, s vy pdiies i Dane of 106 i as transparant to hest a8 & pave of glassis | one, wnd the lett side of this one, unite; and we have now et : transparent to light. 5o that through a sheet of ice on e a mass of bowlders which are fn the center of the 'LADIES AND GENTLEMEN: Under the prossure of mate- | the irface of & 1ake, when tho sun shities upon the water, | glacier, atd which move at the a0 the RO 80 ths Fials crowding for presentation at the close of my lust | the stonos on the bottom Jooolve :en:.t‘;. .‘Ii? In that ma- all the foose waterials which accunulate here upoa the ner air bubbles are wade to ri 0] ntly. 3 0' are now moving rapidl, lownward at the rate ture, I omitted two statements which T weuldnow | j.0 0ot joe, o rock which is at some depth under | of nearly a foot a day during Tho Summer, or leaathan upply. Lu the first place, I would say to those who seck | the surfaco of thie fco may bo heated i such a manner | that during the Winter, at an average rafe of 23 fect relaxation and pleasure in travel, that the Valley of tnm in consequence nx( ‘u'me :;).c"%n bfiu:fi:fi: ;;;;} in w'»"'} P ¥ ém’llzml! o'o" ten yoars tm-yln-m hl:'“ rmv:g % . g will appear. Suppose that we ect, al ours_they wl Ve LDV e Amazon is st present accessible once a month | RC SRS LY ok boded) the Shrthos of e gli- K000 Tect. “*Sou' sce, Yherctore;, how fapidly these New-York in splendid steamers, and from | cier; that we have hege the inequalities of the bottom | bowlders will be trnn.rum,d to the lower end twice a monthfor the whole length of the Amazon, | over which the glaclor mgves; and thag bere | aLigh | of the glacier, and fall over its edge and terminate here s e e e a0 comortablo that our best river | rock over whioh it passés, tlie top of it belag only 20, 30 or | as a concentric wall of oose materiala, Those acoumuie; ‘have nothing better to offer. The other state- [ 5 feet below the surface. That rock will be 80 heated | tions of loose materials from a glaeier have receved names. They are called morains, We have here (1poi Brick.—Town and country rapidly are growing, DATIONAL, AVESI: ard the demand for Jumber cannot be supplied. Hence brick must take its place, but here isa difficulty, for la- ber I8 scarce and dear. The next resort is to make brick by machinery, but to do so with profit requires great strength and skiliful construction. Many brick machines have failed for these reasons, aud because they were too complicated to be managed by common laborers. But our inventors will not rest. Abram Requa claims he has & machine, called she Eureka, combining the objects de- airad, that is, one making brick rapidly and with compar- atively little help, while it 18 durable. By such inven- tions modern enterprise aloue can be met. Those in- dontn, Y pee paters from | the glaciers of LIS | 4 rested in this subject will find the machine fully de- 1am satisfied that the glacters themselves covered the | scribed in an advertisemont. land. Ome class of the Lllcim 18 wanting; nowhere are e —— evidence, I should only repeat have stated with Merel{ol o the 3:” within rthu vlllu{ of Switzerland i upon laius of this conpiry, [m{ghluy, however. that travel- ing northward from Rio to the neighborhood of Pernam- burn‘"l nowhere ceased to trace the same fact, and after visiting the valley of the Amazon, I buve become satis- fied that once the whole valloy of the Amuzon was 0Cou- ed hy‘n stupendons glacier coming down from the An- 8, a0 reaching to the Atlantic. 1 am convinced that all the l0ose materials which form now the bottom of the valley of the Armazon, are materials whioh hive been fronnd by that ice, and scattered evenly over the whole aud i the same manner as the valley of the Rhine is now occupied by mud and clay, which wers once und 0 the~ Alps, and have been brought AT THE BROOKLYN ACADEMY OF MUSIG TO-NKIGHT, 13re Tickels to be bad of B. Dyas & Co, No. 265 Fulloust., Breckiym Alo, for the sscommodation of New-Yorkers, s the Covwrera Roost of Tuw TinoNK. _Price 50 eonts. Anna E. Dickinson nt 1 want to make, 18 for the bonefit of those who are through the ice that the fce will melt away above it, and oom‘,.l. for private commergin) pyelations .m ‘Er‘\;u‘ and | any materials upou the surface of the glacier moving with | one side) a lateral morain ; we have here a r lateral | the surfaces of the rool r‘nlhhnd Dbeoauss everywhere AL the Cooper Tstitate, Ily with the \'W'or - Argazon, that the | jt—say a bowlder, for instance, or a large stone which has | morain ; and these two lateral morains form 4 the center | the rocks exposed to the action of the tropioal sun and The Standard of Excellence. TUESDAY B » loos of the East, o peppef, *I dove, the nutmeg, | fallen upou the surface of the glacler a d which | a medial morain; and that medial morain, falling over lhcuflrm rains are so discomposcd “they QUSIDLE: |y, pary boen in possession of oue of these iustrumeats for some time. VENING, Feb. 19, ?"v nin of fll‘u to a considerably extent. Yet the' character of | Frowm our own experience, and the experieace of others possessing the The Hoo. HORACE GREKLEY in tbe chatr. ¥or particulars see under bead * Leotares and Meetings.” A Inr Meeting of u T R Ve : : WEDNESDAY, 13th iust., at 74 o' L and Becoud v, e inequahty s that of this rounding motion, which wo have everywhere where glaciers have been at work. But Lly comes up (2 THE KTANDARD OF RXCR S CLAIMRD the morains exist. The nature of the valley had satisfied 4o ot know of any other machine # capable of doing il the work of me of the former presenco of the glacier, though I bad, | sfamily—jrom the fnet fobric bo the heaviest cloth—ea the Willoox & I have o of these dizect evidences arising from | Gibvs—(Belford Times, C. K —ddvertisement. hor, and Yed in the neighy | 18 GArried along with the glacier a3 {t moves | thelower endof the glacier, derived from b »;VJ:" e e ivatod 10 such adv8l. | down, wiken it comes to this polut, whero the glacier is | ¢ Torains, forms what is called & taFmina. mo- b oare aud il be ot akilitul manogemedt, | hollowed by the operation of the Tock belaw, that stone | raiii, —— Bupposs th nclts, avay. We ; : B b this ot and will no longer be carried for. | should seo the materials strangely arranged on the Pl benefit of the comnierce Which 18 now cxCiue- ~ of Euro] tions. And now lef ward. A glacier has very different aspects in its differ- | bottom of the valle We should” have a large ac: In e Baade o Europeat, Meet ot . evoutag (A laclor s, Yoty T tontung hy o skotch] | cumulation of materiais on the sidesof the valley, and ine, with whom wo have coms iu coutact, we unbesitatingly say that NOLES O lau 0N, OTTIWELL, Presitent. your_attention to the subject of this eve ‘ga ent parts. r “ Jlaciers mountaiy inequahties; and that there is here a deep val- | not in the conter. We should have every where angular | the ch: of the rocl irface, but only the indirect first T ‘H‘&f -nuuy"n" #‘w‘“&'.:"J.":mfi'fif-fl"w::;« W otyn i This gy; and that upon these ie- | bowldors, aud we should have a wall serous the valley b fhe triturated ,nuu‘bn tmunz to my fainil- r—— B Koncuon, n lffipn large masses of suowghave | the lower ond of the glacier, and we should have in’'the facts, T infer that the glacier of the THE STATE OF TRADE. Joun Hwrup, ' § Secrelarios. ———— merican [ustituto—Annunl Election,—An ISTERS and COMMITTEES of this Institute will be oy b g 2RO o3 ok e 7k ""L.. open N7 - Secrotary. Ie!{ o e Ru‘\iu X . That snow Wj in e Jhowy condi- | contera wall of equal bowlders, distinet perhaps fron tl Cyml geography. They were mentioned as cu tod 1 &nu, in the titude Of 450 for instatee, above | others, Now supposeé this mountain was Rranite, ern boundary of 8onth Amerida on the rder to Lioh es to the study of the glaclers. Ttis not lops n% ly o] i cer- | 9 3 b Where above that Jovel there s | whole of this row of bowlders would he gramtic, t) henomenh, and that fl the rising | BT TRLAGRAPH TO THE TR{PUNR. ous aoeumul ‘ORA‘ anow formed on the summits of cer- | 9,000 feet; 80 tha yWhe) o ole of 0 ,xo f,‘h{. nomenh, wad that b tho rsing “"i:m e o 7« RN [Sho study of the glaciers was an accident i the stud ust habe extended bere ( "nfi o the north- y order of the Trastees. s ; mwg"‘r ?u produce 1 the heauty of the scenery; | perpetual snow resting upon the Krowhd: Yot that snow | pose we Lave here black slate, the whole of uld nfluw Ay Bon, i ik e e Mo Pork "'"“0“ e e enera Moreh, i9 e sniow of Cumberiand | Juuwn Buii, Roe. " HORACR GRERLEY, Prosdoat, glaciers then did Dot go beyor ae ot everywhere the same dogree of compactness ahd | contain black slate. Aud suppose that herly there sy et ot | v i ! I ‘ w6 bowldes * would | morains of that fmmense glucter. I located that terininal | §iiic, ua‘hh ! g n mountaing, The lower it is, the more is it ex] to the | wore red porphyry, then t S LG aniluence st which 13 dérived from the picturesque beauty of | solidity, A w ce. T onger a0 now. | slight chatges of temperature which affect the sides of | bo of ‘rod porphyry. Thus we shwuld dave | morain in Sierrs ip g lecture whioh I delivered ut PArg | gondersd at ‘::”yw“' '%IM :n;:’ n.'?,'.'fi.,'“ 'I ::':lvl”(!;h nnf mmumfi, "The snow will be affected less at the hight | three morains of - different rh:)mv‘r parallel foro 1 had JW ‘1. 1 gfid them that we-o’ dividiug on 200 Aty 'mrlll“ Mm‘mfi“mfi."mmmo. @hich they undergo: the o the. greater exten- | of 8,000 0r9,000 foet, and lessand less us we ;omgu-mm {0 one another, ong of black slate, one of gZanite, and one | that b 1 4 enm:n when several I 45 “'}’fi B e ayY ras of Bloschat ant Dowaiegats. TiA NS e and. range which they have oocupied iu for Righer, ‘On ascending some of to 100 peaks in Switzer- | of porphyry; and at thie lower sud, g trausvorse wall | wook' 1 visted ¢ Y found 4y such traces of it o e Univormalies Chureh, commer o ke aad D 3 the sig which have Dbeen Jand, the highest in the BernesofOberland, the Jungfrau, | across the valle ,oomIoarl of "“M(., arious materials | glaclers can with 0. 1 scarce ‘and nominal; ) ) Twoutysecond Annual Roport 8ir prosence T.f countri 1 have been able to trace all these ohanges of the atmos- | combined togethor. nxl ot fhiug takes place, as the | which are in the ate vieinity of the Alps, or w‘mm. steady, and closed &m.»ma for No. 1; sales glacier moves in_that mfiner oward. Fragueuts of | gur regions where the rmgl nt marks No.1at o aad Np 2 l.: e:{? Oste dall, o lower Cho or TR s, 22,000 phiore n the ice. At the lower end of the glacier, we find ) That " graduall e e e, “find con | ock slip between o foe and the Tock; and we bave & | distinctly observed, %fim‘.‘f that graduaily the ico dually e e framments i & snowilike | stmilar and not un fpcousiderable accimulation of sucl | far wers L8o prosent all ; i jargone changes of teviperatnre wh dt.hgamirndullly St tmowhat of the s | imteriais b et (b s on o bottom of {he valle und | o fuets fo e £ would’ alUO8 Fou must be s E Tl v i - BT -] et gone changes of et e And if | ncter of o Jooss and partially-oemented 'uow, | its sidei. “As "tho ~glacigy woves on It s et with with one fact If you look at the mouth of the Amazon— | Sr. Lovis, Fab. 14.—Tobaceo m . but prioes radfed withln NEW-YORK utions awere made. And 1t | AT, o B diy tho conaiiton of pure mmow—no 10nger | stunca o its ' wholo Wlder *sarface; and_thus it | thero s notdelta there, " The longeat river ou cartl cag: i iver which Amount mue 4D any othel 'y w il A v LIFE INSURANCE COMPANY, 3 "the estub- | in the condition of loose and feathery flwkes, but reduced | tasps or grates ipgn = the roc o oasg, gy hment of the state of things which prevails now npon | to a condition rese bling frozen sand. Sucli arethe dif: | it moves, so that a glicier coming down & valley delta Wl the Nile, the Mississippi, Kmn,ml_u¢ last great | ferences in the character of the jo d W) 0y Q186 | 1s Uke p fije set with diamonds, which gre cousfautly sraj- -fl! o, geeat siroams of our globe have | foie indstive, the lower grados easior; Mized logical convulsions, which have made our earth what also differances in the aspect of ice. How H&xw 1) hf)€n lie rocks, constantly M&y &y h ABIEAS 0] o %lq%?“, 10036 o477 m'? Wlu;&. o ufi:f.‘lm’.mmm‘m n.l'.;.‘ 1880w durtng which the whole surface of the globe | because of the large amoynt of .flgrhwf ajr ng Bmu«; ng the whole surfa y flwbu* t thigi EQiLy Wig thi\um fials frmeces &1 3 5@l 5 for good to Drime Fall, iy ot $129 covered by masses of ice as thick, as | containsin its or ale. Tf we pi 00t umlu%q trow | fact with the onwatd moying glacier. Thé effécts of this to 1] iciopt telodlty to catfy the oum{ Ky eadog st B2 25, Bty Soaos sad mets sciive 48 §58 as compact, as those it in that mauner the alr, we render it white; and i | mechanical agenay are sb peculiar that they afo easily for" 13 that owing tol nature of for ehoice. _Timothy brih At » 3 1mfglum. Provisiogs quiet aad un- limited to the Arciic . Bo | wedip snow in water and press it rorward, 8o that | distingulshed from any other kind of abrasion. 1 bave | coal feh 18 composed solely of the loose materlals | charged. Lond Ta»unlw ”!m: vy scarce At 63 Pig. 0 od of iutense cold would have followed thos¢ | Wpter may replace the air, it losea wore and more of fta | frequepl o under the glacier. 1 have penetrated | once riturated Ly the glicter and aceumulated w260, Peb. 13, l'?l-('bflfl 5 il § asles of 1,000 Ubls. at §11 78 for No. 1 u-§ nd ot tnal a T it jonger to be found ; the furthel in nee very far from the regions where they ot, have satistied geologists that our fains h were not mass, Spring, $2 85 for OFFIOR, NOS. 112 AND 114 BROADWAY. s o ' JANUARY 1, 1857 1o the side, from the lower extremity, and | along the shore, The evidenco of these glacial deposits setiode I geological history which have | whity appeargute, and bscomes more transparent. Tn | under the . ; i lmmg of N uh.-nmfl. Aud if this })rupx 0N A Q10T Al xdrlf; n away, and a8 tho ice is | through Ui the thass, when it was somdtimes | 1o all the river-botioms of South America are unmistak- | B .fl’" '_':.",fi‘;_‘:",fl‘ ”I:-'rl:‘mdbk xtra. ‘-wr . 80, you see that the study of the glaciers may well de- | frecr frim Bl Particles inte :fi” with the trandparency | gaping sufficiently to enable guo to dcr‘md lito | able. T have seen them on the Rio Negro, on the Purus, | i 7, Backeleut Fomr el gout doont, £ 8% ot - ve ‘our attention, and were it only to test the | of the mass, the fore does it alsiime a greenish or bluish | them.” Aud I have seen, 6re v here was | on the Madeira, on the Tapajos, on the Xingus, on the To- | Choice Western at G5e. Barley, Rye and Peas nominal. ~ Corn Meal in . re dootrine whic Vou Thay perhaps | tinge: and finally when It is perfectly pure snd perfectly | such an opportunity, how estensively the lower | cautins and on othier rivers, 6very wharo bEATII the saIne | fuir demand a: 3 0083 5 per {00 . = Shorts afo selling at $20. | Amount of Asts, Savasey 1, 1986 chagagtor gud showing that one and the same agent has D@ per tun, aa 1o quaity. | Amount of promiuias reeeived daring Awount of iuterest received and secrued, eladiog premiums 00 god, k... ring this evening | compact, and wiien it has very few fissures through its | surfaco of the glacler 18 studded with fragients of roc (m:‘p d thmflh 2927 and M} . able 10 track the glaciers ., 1t Assumes a doep blue color, which {8 its natural | set in the fce in a manner which \rm\'_qy{q ;h!s yig. | been 3EWwork in forming these doposits. Tho same ma- | Rai Freighta—Flour to Boston, $1; to New-York, 9c.; o Albaay, n, and where they are | ¢ Water, in its gatural conditio on ‘fn large | Thus carried forward with the gysl Y, you o) rials are also found ly otber vallbys in Eumhmrira. ne acquaintod uufi the | musses, is blue, ag kol&kfimmg- silver waite; and 'n-lnn-lnlnu@mm‘hanhfl%flv’ it llT produce. ill these loose materials have hoou rémdesa the hc":g::":n"' "t%,!;;’fl’;u_: ;t;‘dr. -rug fair dmud.ulluol h"l!' s when '|llwy the lce o t‘u olof, T 18 et u?p LAY that p«rh?ll )down uwofiwfih d up the minor pat icl:-; A‘:n;zlulul'lm' ly on ncwfiuul <le k|!|(' rmnnm ‘fifia A Bomertoes Famly, at 411281350, Lol isindag. with the indications | blue a] 3 e result of 1 until they are to powder, when they consist of | sueh loo as the glacler will not pound do " b &% Y ey 18/1a not the resu ot N'uV 2 Lacd/ L het, they mmulne !lll the manner in which ::j“' 1 Syring st 63 WO §3 nd Ho, 1 Wighee ot 03 90 d to give me you Tn order to b p the come familiar prosence. And _{his _cau - 61 the color of the sky. but it Ix its uatufal color. | softeg Lacks ground ensily by pressure. Harder stones | aud 3 ot S A 1 (gt by oy 3, s A gtudy oY n.l.% ghnr‘{l.r-qrs A lul'h.'nibnl Deautiful bluish tinge, even when the sky | set 1.{%....5;}.&:&%« fee \\':lruuleu*nl'rhn‘nndthwx thy lodl accurguinted fn the Valley of the dnll and nominal at Ste. for No. 1. ¢, wnd T therefore ™ attention, first, . when it rains heavily; scratohes wij bo queper and longer in proportion as thy *“5 ¢ 10 On8 Aa¥. ave thus the evidence that the No. Lat $1292 %125, Cotbon prit 3 ho supnuits of the Alps, whe 1the best opportuni- er look more beautiful, harder fragments of rock are larger,and occupy more space | O¢ ""‘QY“’NHZQ’& x, 5t at such a pate that a band i a0, Whisky steady; E ‘and sirrendercd and of studying the g\ ers of onr days, and then gradu- exhibit more glowing c¢ cothat moving bodily they may make decper furrows. | of 30 f eA ®n remdveg) fro) maflhe Vall Py fin;l:) ces dl’ork' lyu 00 demand; small -.Pfl-uu-! ly invite you to travel over those regions over which that are in a state of decomposition at the | ALl this may be seen under the glnciers, aud sometimes | of the AmAzon. I was induoed oot !r_." , m’: L g :ry Ma:‘fl' CB-IR s and 3 glaciers themselves have; moved, and perbaps we Depn washed by beavy rains. Do not imagine, | under paculiar ciroumstances, after a more thay usual | for 1t was not an agcidsutal dlmwnryre.[z«i‘ t“ fl!““:fl' oq:f.f' . ,3 T oo :. s :fl!fix:.'hu;:‘un soe that even where the tropical sun of to-day | then, that you have witnessed the glaciers to advantage, | motion. Ihave found the quw er tgewting from the | amount “of conat lost by the encroachhith 484 Cleat Hides loose, and orax (legs i (S, S BEpeuses. «vevnsens hines, thore was at one time a field of ice extendingover | when you have walked to the foot of they and witne sed | grinding just in advance of the \-w?n mfimufluw-a the Atlantic upop the ‘wquth of the AmMAZOn | sales of Shoulders at thc., G Biea Sl t 12)o. Lard Valley of the Amazon, extending toward the Atlan Theanowy aplendor of thelr surface. In obder to lpve an | the motion wmawning there in front fu the Morning, | by facts which I havé observed In oitr own country. All v ominal 3t 12810, 1 Prime ity ; Piipe Steam heid rhips covering the seq to such an extent, that the | idea what the Ium,w.\x is, you must see it under all | aftor a heavy frost, so that I oan suy I have seen the g the [alands along the 'fmut of Malue, -lun& ths Bay c. Meata—Sales at b} @BFDU }' gver in demand at d of work which 1s o char usatts, and south of the of Cop- . Timothy frner at $3 40; Fla 225, Linseed Ofl, $1 28 es frm and unchanged. ASSETS. Cast on fand, in Bank, and deposited in Union Trust Compan # Tavested in Unite ; codt. (Market value, $2,523,753 25,) Taveated in New-York City Bank Stocks, cost.. 52,51 39 (Marked value $57,515.) Tavested in New-York State Stocks, cost...oeee 1,438 84 x al @ tiag #1490 Baitar and € ueation May be furly asked, ns 1t is now asked at the | possible conditfons of the atmey here: and just as the sk | el at work doriig this kin A d 1 oy tneluded, are covel "Im 00! E 13 :Iuy - | of Mpss Jar rogion, whether there swas open water under the | looks differeutly under differeut conditions of illumini- | teristic. Suppose this whole mass wmelted awar, and nectieut, Long Ia ) far, do I believe, does the evidenco go. So | tion by the suv, just 8s the occan looks differently under | What shopid wi il g aco of he rock polished tn | materials of o glaclal character which are of the same I am satisfied, nges of the | different conditfons of agitotion, fust 8o does one and the | & way WOt Rt AN RN produce: tuat polished | Kind as those reating ou the continent, and of the re upon the surface of the globe been. | same glacier look differen When 1t hins been melting | surface would exhibit small scratclies resulting from the same hight, showing that the sos wust have washed ald exbibit deeper | that which'is wanting for the level on the contiuent, aud t " lling. Exchange ey market stesdy. i, Wieat docined, s of No. 1,1t No. | at ense cold | at the surface under u hot sin and a succession of thaws, | small particles of hard material; it s be 80, you aco at once how tiis i modified the smfaca of the globe to the it 1ooks like @ withered mass of snow—it looks like a de- | scratches produced by the action of larger pebbies, and the level on these *l“‘udfl could not have been main- r, 1, 5 Aing life from It surface—of interrupting | composed acenumulation of dirty street suow, after it has | would exuibit larger furrows resuling from the action of tained the same by the ouward movement of glaciers if | bush. Shipments: Flour, ; 20 bush (Market value, $725,59.) he noriual course of the vital phenomena, and preparing | been melting for some time. On the contrary, let a heavy | larger masses of rock. All this is easil e nd you | there had been breaks there. This furiishes us the evic | | Cuanurato, Feb. 12.—~Cotton active; sales of 800 bales Middlings o8 | Lavested in otber Stocks, cout. e MR o e B ooy exs | Fuin fall upon It, and then ail its surface bocotnes fine : the | see fliave therefore two signaby which the preserice of the | deiroe that all these wolated parts of land which stand | e (Market value, $30,000.) upon it. Tattach great imports philosophical | dirt s washed away and its glowing colors are brought | glacier niay be traced even it the fce abould disappesr; | Out 1o the ooean were once portions of the continent con. | F-;t Ont nmm‘ |ri._muuflm-,-4nn(hxn(~‘ aalend 800 bales; | Loavs ou dewand, secured by U, 8. and other nt of view, to the study of th Hecmuba1Ft | ont: and under thees circumstanoas you ahould attempt to | ove, the peculiar acoumulation of loose mutoriale, of rocks | iected witl It ouly by L loose materialy pisbed e SRy e e A B W T TR K Bhoek ¥ " 34,00 0 al be demonstrated that'such we conditiou of | aee them, if you want to see thewm to the best advantage. | thai have coue down from the mountaing and have ac- | by the glaciers, Andif T be permitted to confec ture . agalusy r correspoudivg period Wb week exports, Shasad ur earth, it will follow that th There are some phenomens connected with the trans | eumulatod ou the edges of the ice aud npou the surface, T will suy that the line which I asoribe to theso P a_and_un- 8 ugation of the spectes, and of the descent of the ani Jon of suow into fee, 8o that a glacier may be | and the pecullar kind of grinding which tle surface of limit of soundings, I8 along a i 2e15 Corn 2,49 00 that live now, from those of past days, is cut at the which > and the results of which | the rock exhibits from ite contact with the ice. Histor g Mt B #5c. Hay frm; bearing t by this Winter which put an e all Living 136 such ehanuges upon the gronnd npon which the | ically we have the evidence that the glaciers have not from twenty to thirty miles, the . B les of 3 AT the surface of the e platse.] | glacier rests that the presence of the er may he ree- | alwiys been Lmited within the boundarios thay now o ne time extondod in (he form of | Shouldersat Lic. ot Sides at 112 Lard bigher; sales at 132134e. | Quarterly xad sem!-aanual Premiams dus sub- hat do we have? The accumnl of $now 2 T will represent t spy. The travelers .on the AIps in tue 15k, 14th, and A tho bay of rundf the coast ,‘}lfi;-:{—-";r"_.*?“'n"";f- 1364 Bank Sterling, 66} New-York mn-inlh D |,':us goesedreccireiots fig: | 5 conturics, and more. partienlarly the myestigators huy of Massachusotts, the Sound, aud | BUee L, TRatuoes, fii.’-:::‘w".‘.m.'.'.“.h,".zfi‘...; e 4 rdually passing fre rivers emptying iuto the At Premiusma o Policies i t tready begun to ex und vominal. White of the 16th eentury, who ha led with Joose materials ‘course of transwission. al lantic, nto a miore foy condition, scending fro here enow falls futo th ere Ui Alps with a view to study the phduomonn of the moun W o 99,145 3 ey Summer. iers; a tiins, have left us records of the extenslon of glaclers nrv this Imwense soa of ; ..‘nm.( g toward —ifivwr.s o y eauty. | within the Alps, and their statcments whow the ocean, and it was when t ceean | The Trustees have declared tarn P follows: A SCRIPE o on the retrenting glacior that these 10ose mo ¢ £6 507 #4 he Trustees hare declared o retarn an as : v L 4 active: sales 65 bhds. at $225 Dl‘vlh ND of FIFTY PER CENT participating premiams | that where we b wero issued tweive wmosths prior to Jauasey which oce bave now glaclers, there wer 1 e miade room above ! noved out, nud the melting of ¢ he sen, or on the pl retics, molts onl: oh rise upon the side larger glaclers formerly to thelr | we here the average t ar is al . t that valley is 5,000 fi N can’ tr ternsinal | for the secumulation of fresh wiler the suifice, and t; sales of Prime at ption of the Dirideads doclarsd In 1855, Where t # at the sirfree of t beyoud the prese r. To | the have hollowod a1 uih Mkl slon of pocki ot 6. Botom rodeemed m cash on sud afler the drst Mooday b8 , tho snow may accum ; large 0 tom of th D etory ahort, 1 would say that thews pheaom Bess Pork; sgln st 821, Daih Sussiders, sles of poovec ot o} D459 | March neat 0w pemssmiston st i omio Oios Puisios sxblped o @eoumuiate, the snow, if 1t moves from the place where it 500 or 000 will supp v across the Valley of Switzerland to | carved to its present ¢ As the tempersture |y L T aclas o It et iavons w153, | Notes wil o eredited with tbe Bedemption o8 the setticmeat o woul falls, uiy be preser ven where the tem- # feet of peaks rising above Jurn, and that we have the evidence | Kradually rose, the massos w away untll | Whisky; sslesof Raw st $2 25 New-Orieans Sugar; sales st | PFe®'Eo raturo s above & This 15 what take T a8 seen in b fuen ‘becupied the whle of this extended | they wero circumscribed within tho Arctic region, sud | 1= Rie Coel slesst 24j@2c. Cotion, 8230, . By webon'ef e Bosel, WILLIAM H. BRERS, Acteary. lnce In the Alps. e have unfortunately wh from the mountain into. the valley, this being | plaln wcross ihe Valley of Switserland and abutted againat | the plain of Brazil was free Wit R0 Pob. 12 —Cotton dal: Middling 2023 Spirita i . 5 0 glacier region on the eastern side of this coutinent. ottom of the valley, slanting from the suminit of the | the Jura, Professor Gaylot, who s studied the trausport — Turpentine dull| ssles st O0e. Rosins quiet; sales at $32$5. Tar fir; Durimg the year 7,206 new Policica were issucd, insuring $23,74,308 'here are glaclers only in the Rocky Mountains, and on | mountain toward the lowlaud. I will represout here the ders aeross the plains more minutely thun 2 i ot @ — ha'h.au rnl'm: o('mx'h suninits, which extead from the surface as covered Aually covered with onstratod that each valloey from the PUGILISM. Savaxxan. Peb. 18—Cotton frn ; Liverpool Middling 3le. BALANCE SHEET OF THE COMPANY, JAN. 1, 1857 Mountains to southern ¢ ! 8 h do v ol \ (v o e - s nthl o southern extremity of South & down in thisway | Alpa has ou ench side rows of bowlders, which extend — cwm, OATTLE MARKET. At daabore s oot oo $6,727,8) ¢ HOERATIO | Feb 13 —Recsl tilg, 769 Bheep and Lambe, 4,459, Prices for esquent to January r (continuing his ilius- | across the platn of Switzerl tthe | so that the factsa whic Alps, aud thoss which Guylot ascertalned while Alps 1o the Jura, ithin ‘the | FIGHT AT XAUGATUCK JUNCTION BETWEE! orica, varying 1o bight according fo the av. tem- ture of the differeut levels. Within the Arctic re- 0 | Beef, Batra, o1urln SLI@$15. Secoud qual- lflfinal.lm hn,oq N FOR $500 A SIDE | ity 41004 LR 1597, Redorved Twill also represe ) WAKBURTC Fist g quaitty, $3%60 prooks, ons the lovel ot which the snow remains perpetunlls o o thot we sh s, & ground is at the lavel of tie sea. Aud tuis co lagier. il at | in® ihe plain of Switzerlamd, colneids o show g : ‘Shoep and Lurmbe from 3 to 7 centa wd, s §to §oent Dt tlings prevails on this coutinent, especially in rosent hero the triu é.mmmr..m. t this wholo surface of TV wa onge 00 IDED IN FAVOR OF BOLST e e e o LI T e s e | B N kit s 4 fi’mfim.hmnnr 10 the sonth than 4n Europe and chain, here another mou n, and here a the Wlowed by t New-York train arriving in Ne when frozen Mition sold &b & serifen Market closes dul. A--’:Iu::n: for 7o lasmraace o8 8il, eniste este) The séudper of § from the Northern States was unalier than last | T4, b oiicies (valuations at 4 per ceat interest, n Monday might, just as the lamps of the old re ia A ¥ nutain ohaji. bt preminm) ... 4,979,957 B abd here is another T week, bub the defciesey waa tad fron Switzerland. Now, up by Westor Catle.” Working loy, ¢ 18 oceupied by jogrocs northiern latitude n Gry 1670 or 71 | valley. This vall ¥ 2 e g gZro northern latitude in Europe, the suow- | yet trapsformed into cowpact b thus far when it occurred logliate city were beginning to throw a sickly glare on the | Oxes swid, per pair 80 to Retarn Premiun, declared prioe to 1364, paya- b remain on the bhighlands at higher and | having lost in » measure its anowy character. not have been alone so w sidewalks and the podestrians passing to and fro on bust e .24 % oy s you -approach mearer and | This valley is occupied b o o y itry ahare \ > e o el oo the i it nder the tropteas | Intlon of wagwy 1o, Which I gradagily passing into.tha orw b, prevaried i e ont of Tuak, | U888 OF pleasure, carried among 1ta passengors o small but PASSENGERS ARRIVED. ‘ he land of perpetual Snow rises to 14,000 feet; while in the | ¢ cter of ice, These two arms of the glacier hero meet | ing the ™ o | aelect party of York roughs, who were anxiously seck FROM SAVANKAT, ¥eb. 5—In steamalip San Salvador—Georze A. l Switzerla the | Ingthe w bouts of a prize-fight which it was expected | M "Y'1"l;"v:‘l':l:hn'n:.::l-m"”lkIJ“IM"X&IJ e to a th 1 | would take place on the succeeding day in the viclnity of 1. Evarett, Job C. Duten, W, H Sbepberd ‘Geo. Site, 3. 1o Brown, 1. McCall, J: W, Brows, sod 2in bark Queenslaad—dr. W. A. Darby TRUSTEES: MORRIS PRANKLIN, President of the New Yort Lift Insraace Caw of Frane beon enjoying the gor 0641 the nort emperats regions, upder latityle of ti! ¢es say, the | together, and fqrm ome great glacler cecupying this - Which tha #‘{‘&%a Petusdihily oh' (e | (thgd) vi Shion 13 bl vesult of the confraction of bty B100 Teki s the level of the sea. xgfie(w @lleys. What will tako pladé ¥l From ail | plains of | « 5 120t gt which the sow remains on the £y ? thse flnubl,&n-‘ufl“ thero are constantly folling blocks | not | ew Maven. Figally reachivg an English sporting-house in roughout the year in the s of Switzerland. A\i'f» of 100se mAL Vsl § te froln the ®all of the | prevaliag - | one of the narfowest and dirtiost strests of New-Haven, a mfi the principals is within, wait- POO CLOW, Feb. 12—} Doremas & Nixon, Dry Goods), No. 43 “Varrcash. JOHN M. NIX¢ If ybul:xnmln;,r be lvall(-y '!\lw. \, ‘u'»\ 101 it moun! llnd s l} be of ’l e nteg: ll;lbll of the | l!]u)‘rfll Ilnlllll'll: te. It was then |l|hn||v we g ed (hin) oue hore is no uniformity in th at which snow is per- | rock; and masscs of atenc of ¢ erabic dimensions | enough in all these fucts to wake 1t prob: 1ng 10 - when the fight is to take piace. The - - naut, ot 8¢ WhICH the glapiers come down intu the | nuay drop down, sometimes a8 ligh us u houss and | find tye traces of glactets in Englaud. As | iraincr of this man, & goodlooking and ell.formed n , DAVID DOWS (David Dows & Co., Float Merchaoks), No. 3 Sasbsh alleys, for the obvious reasons that the igqualities of | sometimel of sfucller dimensions. Al these masses | I sgartod on a hunting r'flfi&'%i‘ %r conng fellow, glves an fnvitation (o the reporter to Lake A LATEST SHIP NEWS. 18AAC . KENDALL, Usion Buildinge, corue: of Wiliiam aad Plus-sls. 0 surface so affeot the local tompergtur inmany | will be arrested us they reach the bottom of the | glaolerd fhrough the British [T afid i 'wrk at * hisman.” Drawing aside s curtalu o wu inuer e i DANIEL 8. MILLER, (late Dater, Miller & Co., Grocers.) cenmulatedl ice. Suppose I represent here Y renched The Blghlands of Westmoreland aud afterwards | roofs in the rear of the har, which is ornamented with cheap PORT OF NEW-YORK. WL . DUSSNBERRY, (Reet Sikils Bieler) \ , which are as 1gch nd foet above the ea, WArm winds fromh the Sou mannér 08 to mels away the Win HMENRY K. BOGERT (Bogrt & Kneelaad), No. 49 William st. JOHN L. ROGERS, (late Wyets, Rogers & Co., lmportocs), No. 86 W iidiaanat. JOHN MATRS (Merchant), No. 20 South st. b prints, we find onrseives iu the presence of the ble b nnu\\'llllmn Warbu on, who s o fight on ARRIVED. with the help of Providence,” as ¢ sympa- | gr.am Salr . SRR aly remarks, in answer to a question of | g, e .vf"u.v‘:: Salrmdec, AR s ¢ ulge | tlopeof thoa 1 of the | these masses of rocks, the results of the disiitegration | proceeded to those of Scotland aud Ireland, tuan 1 found everywhere the same signs of glaciers, the saue marks, ~ | the sume polished surfaces, the samo lateral morains, the | the | fime gonsenirie moraine st tho foot of the daciei—in | thisug rough ] in such a | which Is continnally going on, as all 1o 1y fu the | stantly falling to pieces. In conssquence «are rolling dow ., l\x ected from the soft- &r tion, immense ras bDIRg influcnce of A soaiharn wnde 1pd, on the find that thefmass of loose mat irt, al) tho evidgnces that the low fayd of England, | ours. Mr ‘Warburton has round, rosy, well fed e (1taL), Diliberto, Palermo, 100 days, with fruit, &e., 0 ¥, open to coid infiucioe of bortbern winds, | accumnlating fromn any glacier is very extraordingry, 11 wfmt it ANGW 1 alus ju Sungper, Wai oncg oc- | fegtures, small, i blue eyes, and an_aspect of fat es & Co. DUDLEY B, PULLER (Faller, Lord & C), No. 17 Greeawichek. he: Anosw mmay remaiu permanently even below the | represent here all kinds of rocks accumulated iy tho | cupied “by glaciers of sutfigent dithdostons to fave | coblen eit. W sk biw if e uever fought before, aud (of Bermuda), Thomss, Bingapore Oct. 24th, via 84 Hel ‘R WI b of the Mtz B fi»?m sc.] Now, we have | he answers k .- with wdwe to' Npring, Nott & Co. Pused Angier Nov. 6. JOHN B WILLIAMS, President of the Metropolitan Bank. WM. H. APPLETON (Appleton & Co., Publishers), Now 443 and UF the sea-shord. [A Hope Dec. 13, cromed the Equator Jaa. 1, la lon. 35 & now. And t owing to | edge of the glacier m consequonce this process of worage lovel of perpetusl enow. An & T he moving down 1n broad troughs of these vast accutnu- isiutegratio eve, in_ this profjle view, will | proved why other parts of the world must have been “Twiee" tious of snow {yto lowes valleys, and thougli they thare | o arreaseal Heres oy (@ pomt o con | bold, fof Europo alone ot coid, and | et thoan ring fihts Mr. Warburton 1 SESE Halown 4 600 xPIVon, L0 1o oo T | Breser. neot & higher chilate, there (s tuch ama-s of i oW that | talt veen the F« and the fock. I wust say | North Anlcrics enjoy a w ufe In 1846, [ " hexactly—Leaatways thero was ropes or stakes.” | 3. 1o Oelrichs & Co. Y i . - ROBERT B. COLGINS (Colllns & Brothers, Stationers), No. 106 Lesws. vealp iy dowgwarg desouyt (nfo We wareg vgliogs 1t | & word abont this before I procced. T have re reseptad | Elme to (s coptivent, o dthe gt seull ok in Now Vore the stakes heayy ' fark Queenalund (of Sydney, N. 8. W.), Wicks. FooChow, Sept. 1. | yrypt. ) s ptéservod, to a gréeat extent. Tn the Valley of the | the glacior as arched—higher w the middle than | oA, 4 Jo% NOTTS Aftef the fi}h al 0} tew Vell, van was for a threepun note and the other wos | with teas, ke, ip.-.nk W. Cameron. Has had ligut winds aod No. @ Wallst hamouni, 1,100 feat above Uae level of the sea,yousee | eentre. Yon s£8at once why thiy 1d bo 50, )_|€ 'K‘cfi was A passenger at aife, 1 a fpur-pounder.” s most of the passage. WILLIAM BARTON (Wi, Barton & Son), No. hose misses of foe come down from the wmonutafns. In | ehini aiinf Tlyg walls will Leht tho walis, aud 3l m the Nell-knotn tracks of glacters, warkd al ov6r fpur pOunCr fles of fair, open country I8 traversed | | Dark Fiim Barrs, Conjers, of and from Bermads, 14 daga, with bides, | WILLIAM &, BOOTH (Bootd & Edgar), No, 90 Frontat. 6 d | ke, to 1. N. Herv SANFORD COBE, Prasideat Eagle Fire fasaraace Co., No. 7l Wall o ud apot for the figh GEORGE A. 0SGOOD, Baaker (Van Schaick, Massett & Co.), No. I8 Willamst. HENRY BOWERS (Bowers, Beeckmau & Bradford, jr., Dry Goodel, No. 59 Leosard-st. CHARLES L. ANTHONY (Asthony & Hall, Dry Goods), No. 68 a # of the Bernese Oberland, the | points of contact With the ico there 18 a higlier teufpera- | bilis. (Applattse.] T hecame satisficd then thatthe clim to find a ¢ ble and socl cet above the level of the | ture than gt some distanee from it. The natnral conse- | of the earth had undergone a stupendous el af last the grouid is pitcbed on the banks of the noble v Jower extreme is as bigh | quence is that whare the glaclor abiits ngainst the rock, | waa uot a local phenomenon, or ihe higirer devation of | Housatonic River, in a clover fiold on_high ground, , the line of perpetual suow beiug a little | 1t 1s melted down and is rounded off, whils the center ré- | the Alps, as was at first supposed, which brd held the | with the siugons windings of the ice-bound river, spanned bove 6,000 feet. Now, this rccumulation of masses of | mains perimanent. Now, when masses of rock fall dosu of Switzerland, extending acioss the plain of 1ges, for a prospective n belt of oo in certain p ys is owiug to the form | the woy u slope, they are arrested in these trong land to the Jura; 4t we had hore the evidence of | eedar trees, for the ground the pretty little town of arth, showing | Milford, with smoke curling from tho tops of Ita cottag)s . Quis (uHul’ey) Vigos, Baaal, 51 days with sugar to Napier & ord. Swith, Norfalk. 6 days, for New-ITeven. Ci uco, Jan. i company with bark Hasard for New-York Wicks. er, P. R, 11 days, with fruit toJ. & T. I inet., had & beayy gale from the N W. with sagar R, the ground upon which the (kg 1ases of snow may | betyiech the ok ‘and’ the rocks: and we have gen: | a great revolution in the history of the Shoulnte during the Winfer, Just a8 yoll see inyonr | &ally here at the function, beiween the stone 3 Trom n yers warm elimate,Which geological phetioni | and mahufactures appearing cround, and 1 e 4,024 wie Liowe ol Lol tn port B s Dosen: s | Losmard et lhere, where anow fed, jce will be | walla forming. the sides of the valleys and he ice | e show us our earth had enjoyed before tho tempera- | busy betting and bustling crowds, who were making pr b L b N Xk | Al Vo oo MORRIS FRANKLIN, Presidoot. formed Ly alternate trans accumnulations of rock ; and they are son ture bad sunk far below what it is now, it tuse again to | grations for the approachin fight. ‘The ring hav.ug iladelphia 1u 2 day cher, loading. A » BELOW, ISAAC C. KENDALL, Vice Presideat. rmation—by alternate thaw- | itself, the and freezing of that snow. And this ice {g the snow may reman in these sheltered pl r thaw the snow in oth on of the glmu# yery our plalis, in cofis fort walls of 80 05100 £ or | its present condition. T will uot tire you with many | been pitched, secouds and bottle holders are ohosen Dines o O Therefore, all along the | more details concerning this subject,” but I will ssy | by the wmen—Kit Barug and Tommy Healoy for fl""v"h-"fl o e arts. In fact, the T g wt'n.tlnwr.flnd these acou- | that a few 5 ago our evideuees went [ Warburton, and “Butt” Riley and George Casoy Bris Porest State 3 ot to the formation of mulutions; aud as thcse bowiders ape fragments which | only to this that glaclers hud covered | gor Horatio or “Rice” Bolster, the oppouent of | <o Gharies Holt. of the fall of snow have broken away from the moh of temperate North Al ca A well as the (mnmrmn, Tim Conners I8 chosen referes, and in the SAILED, f Europe. I have trac marie of glaciers, | tossing for corvers Warburton gots the sun in LIS oYes. | 5o a1 1y 1 on. 60, 10, hark Fortuna from Livernool for Galveston. bip Daulel Kug bt from Bowbay 68 80 extensive that the WILLIAM H. BEERS, Ay, THEODORE M. BANTA, Castier. o s R BOGERT, M. D., } Mefical GEORGE WILKES, M. D. Exuniaers CLAKIKS WIIGHT, M. D, Assisient Modionl Kxaminer. 18, they are angular. | tho w materials | whol i which fhe suow undefgoes during the The whole of these ifications of the In order that snow | whigh fall oabaiar | and otber geologists who have followed in these fuvestt: [ The Yale students, the gamblors, thieves, pickpockets ‘ 4 i ¥ pepwe e stuc " a 3 " | Dec. 20, lat 2990 8., lou. 11 %0 E. o nd bail, which a; s in which fro bowHers. and moves at a i e with e dn my wterpretation of | tighters, and others on the field ‘orowd up to the ropes, | gr '{A:,,,':fl - = Ty e ve come to the conclision that the whole | aud men in v “loud” attire from Houstou nd.the Dac. 23, lat. 93 30 436 K. apoks Br. Sloopof War Pantaleon, The nu.'nwl’kn e 9 i 933 IV eTe 4 « ) nks bagin to offer bets in & noisy man- | fir P A via St Elelena and Ascenslos. been covered with fce down to | contigious faro hanks begin to Do S B B AW brig Hornet, from Cape Towa for to the latitude of | ner. At four miuntes past 9 o'clock ([ tclien bl fur cap i the Mg, Jumps in himself, and 1s sa- | Loudou. st with loud colatm froui the crowds of his friends The ship Unlon (B ) | At $180,000. The by ater falls from the skv, may be trausformed Wto | epeclal rate. s reasons. I the he glacier 1ce, fato ti*e ¢Gmpact . wis of ice, n’m place, but that is not, t is necossary that pressa d thawing should ta as we shall prese cauge. 1L moves 1ace, in_consequaiice of which the snow becomes filled | in conseque ice of the mass of snow ith water, and then that y { the snow which has | which fs g y Tt moyes in conse ¢ of the sbove valusble Hook, published and h;: No. 222 Broadwas, e3a be consulted at No 40 & cutaueous diseascs of the bead which are when in Columbia, | r g of glacial action. | MEMORANDA. Debilitatal Caticle, Suppressed Secretion, Th I Caroling, unmfstakable mar . . = Dandrud, Ptyrinsia (lncrated or saly dundea®), Muttarated i the bunks of the Obio. I have seen | present. lowing. poen Bylted froesing with that which has remaned 1n'a | queuce of i sulting from % Mr. Horati R rystaliized condition, form of loose, porous ice, a | and which, while f Vol Joiow thit erern States, and T couid not resist the | = At 57 minutes past 9 o'olock Mr. Horatio (or o, eaH nowy mass whieh grud: 14100 0f that pro- | frozen water oceup . It Kiittate on'Thin continent the | Bolster follows bt fuF cap Iuto_the Aok, uod 1s aiso the | W dietseder o), B2 S0, il (0 ancranen (ot yellon ond e S "'[“('F:ullu'f“":nydm-xu 3 i transform-d 1, compact mass of fce | you allow water to which i | the Mtaln glaciers na they | vocipient of mueh euthusiasm. The rougha ure uow in u | sel fun Gregs adrd g e asinding Al hlads of b1 heads, o oLher disoases it from any ice formed by Trost upou the | bottle will burst, because ice occupies more space than lare o great difficulty arose | perfoot fover of exellewent, wnd bets of Trifteen to tew PORTS, B Yoss of a1, and promature gravuess To Doctor Cares Acae f DOMESTIC g Sycosls (Pimples. Mattarated, o7 Tubercular Kruptions of the Skin), alee ‘omethous for Now York. bipe Lala aud Sea Gull, Baii- s, and it was mude one | are freely offored on Bolater. 3 I one. | “Bolatar in ovidently unfis to fight, his skin beivg [ Wiaprox, Feb. 13 —~Safled, steamsbly of un ugly A bo o sirips, W"’ besides, he welghs fi!ll 24 pount while arburton strips with a skin white a3 & now-born baby, at 150 glacier moved | pounds. Bolster's eyes are @iscolorered, and ho finda it Comedoms. (black worms or gruba), and Moles and Prockles v uid Warts ramoved w thout catting, on persousl application. e only Pbysicias i this couatry who makes & of water. Glaclerice has none of the properties | water. The amount of water which penotrates the i it is frozen water, for in it cicr, aud penetrates through it, s not only that which ¢ it 18 totally ditfevent. - When a sheet of ice is | rasults from~ the mslting of the ice; bui when- upon the surface by the accumulation of er, instead of snowlug, it rains upon the gla- MoUnLAln Fanges Upon crystals, eometigies plaing from the bot. | eler, the rain pevetraics into all - the . holes vo accnmulated and » sometimbs foriotd 4t {he very surface, and | and fissures in the ice, sinking until it 18 arrested by the | this low latitude. How yaa it that o g a0 even lsyer on the whole surfuce of the water, | snow; and then, of course, in the course of time It will | ou an even surfacel =~ No ono was prepured - for | almost tiapostble to” assuine an erect posture. Bolster DIED. Tually sroviing in thickucss by the successive ac- | freeze, and in freezing it will expand, wnd the natural | wich o questidn, which was very matural, but the | fought twice befien «d wus defcatsd, by Sam. Collyer e i peat Bupel A ol of Bolesih s umilation of sliollar laycrs, untii the lower temperature | consaquence of expanelon is motion, The motion, mist Dherioniena we 86 upon the rocks lcad me Lo thls eouclu- | wud Mike Carr. Ho formorly served tn the army, abf 1 H aseday, Peb. g f the scasol being exhausted, the water is covered by a | take place in the direction of the least resistance - that is, : that thou powhere in the Alps glaciers | of respoctable parent. u Waterbury, Conn. His hight k e Kt w hich the elmatie condition | cown the valley: aud the natural cousequence of all this Alpa Klaclers | 0FTaspsotale P Srarburtonis 5 Jeot # inalies. Thie | Tho biialest the ually ofs o5 o A tho countey tuiy when examined | i @ stationary mass of ice, but fs an of tho State of N Jg the lakes, | i is shining warmly and the sky is magnificent. The | 43 eloek p. m. fully, 1,0t presents | ever-moviug mass, the. rate of ita motion being | and everywhers in the West—) o identl. | gentle surface ofj the Housatonis at the foot of the hill S CKEWAN—Died on the 11th of Fob., Jokn Carflale, 00 of Joba . aod essive stuges of | Proportionate to the Dbulk of the fce. Tha | cal with klacial marks as to be sufficlent to suilsfy the fiokn 1ike un sndiess belt of pearls aud dlamonds aait | MYEEEARCII KL, bead s Tautin il 25 daa Rr | it part of the fce, therefore, which {s | souud mind of w careful observer thut though we have | glistens in the sunbesius. At1S minytes past 10 o'clock the | g Joerle TaThe e e Anlly are trited to attend tho fuserd, from thicker, moves faster t the sid which are | now no glaciars moving on a plai, we had thew then, | seconds and principals advance to thio canter of the ring. | “ihy rade oo of bis t9, No. 433 Weat Tweaty irst-at., on Wedoes- lizmer, and the middie pait, being the most porous, | snd that the glacker, by some pecuiur coudition auterior | looking at eac! sther's faces smilingly, shako hands in s the Ltb inat., 4 1 p. . Thaves faster than the Wpper Vars which is purous, but | to our time, wust have besn eapable of woving on plan | friendly manner, and afier a moment’s delay retreat N_On Tuewiy morsing ¥, 12.Dr. Jomn & Orton, after & loog ORT owe the water (o pass righi through, and faster, also, | surfuces. A Duidsh nuturalist lis sinee given us the evi- | backward to helr corners, Time I8 ealled by the Referoe. and painé | lllaews, iy the year of his han the lower part, which is more compact, while it | dence that in Greenland U e rm whnvimé | Hiol tat, who lika his back and cheat covered WIth BUge | Dhe frieods of e finly sre fviled so attand ble ugera ot b Lt e adwits a great quantity of water. T speak from | upon even ground. ‘The [ on utises, by what foree do | plastors, aud Warburton advauce toward each othe?, | “dence, No. 241 Court st., Brooklys, oa Thursday, Feb. 14, at 2 o'cl measuremeents which [ have repeated for ten years, and | these glaciors movet It Is well known that the tempera- With thefr breasts bared and their hand neh,on gnard, P W e o wocording fo the 1atitude; that it is colder | and the fight has benun, - After 8 great de of wilking RAY_0n Monday, Feb. 11, Ploreace Eatel, duaghter of F. A aud Sarsh Cuant S, Fob, 12 —Arrived, steams Liverpeol. and Carlotta for New-York. st constant objectious to thess I from which these glheir Wes aod Wart, Dr. PERRY s of the aboe All consuli H] “pervoually or by letter, are frae Strumatic Salt Baths. THE PENNSYLVANIA SALT MANUFACTURING COMPANY'S STRUMATIC BALTS AND WATERS are soverelzn for the care of ; DYSPEPSIA, RHEUMATISM, © SCROFULA, SWOLLEN GLANDS, OF THE SKIN, &c., & o D ul'nankll.!:.’m & Invited to attend ber funeral ve., 00 Thurnlay, the 1ith inst., v i8i 1a in Layexs wiich mi uring the alternation ht—dyring the alter above aud below 22° Falwenieit. hen tho tergpernture falls helow retained 1D large masses ve. And 8o, diring these L f the for on the Wit rnodlh' d iy ale bunbles and | ERUPTION For sale at all the ed 3 years | mosth and 23 day he whter, (hat when 4 ) facts Lhave bad an opportuity of obwerving with the A e es 4 ( 4 th e, A with & shoek, War oath, wud under diffe utmost accuracy, and which wero trolled by tegno | further north and warmer further sonth. It s equally well | and skipping about, both men ¢line 3 . v L A el ). i IS o it Kuown that the amount of molsture which nconmitlates | burton ~adidnistering = his r:plxllal rli\'l:l "}vflmfl::;lv nfl.fi"m-’.‘.ufi.?«?‘:.:' uml'l"v.g 'fi:‘-':‘v:.:n.:,‘::"w'::: « IS xnn-llnn"n TR e d made upou the glaciers of the theoretical | Tt surveys which So that there {3 10tbin, cting of the clers i Suppose this to represent ridges of | ure will full mo; the Beruese Oberland; this one representing Pour, Vive, Six, Bight, Tea, Fiftsea to: Oos Hendred Dollars & flob Forsale by KO, C. AL jhat the vow Layer differs nd whe: you exanine th brouglit upon your ial all ploces tiers are i u the atmosphere is un al wocordiog to the latitude. It soverel on the nostrils o, 88 i# equaily well known that in bigher lstitudes this molst- | who Halle, 1ok ng Up with u smile iuto Warbu v.‘.'i’..l'a‘f.'a':‘.‘.'u.'.wf- hoams eopy. ety e formof suow (han | FIve rounds were fought in this manner, Bolster goink | [t o (Sl I e o brif mes.Inthe TE veu of M “Thoso ure all the eonditions we want. | down after recelving n series of Likht biows on the faos T Bt F b iva of Huwiek, Seotiand, sed for wore than 34 yw belng trapsformed tnto fee, and under the tn- | and head, no blood being drawn by either of the n:?'umeg Alps. s 18 formed. g from the manuer in uIAn»Al. th , crue : o ow, glagier oo is total avd the | t rn, and this the Finste o, Wilizw i, 4t fact thast it differs in its strictur N, enables | here n glacier which 1 have surveyed fi osctiied bekln 16 move, and It will | in the sixth round Warburton, who would certafuly bav e redamt ol S ST il are papéctly oviad o atosd = : - I these Qifferences 10 ree o | succession, every hotlder 3 the surf: ward, becanse that would wtrary 10 | wou the fight without ai iy trouble in ten I‘ ‘h -nl- ‘Whe faneral from his lte residence, No. 224 West Thirty r.:mas‘ Bt WAYNE'S Omfilrr‘& Cares Iroi! Trcn Trout ' which we ace on - | prowinentiy being surveyed and its D emoe which produiced the movement ; b 1t will | utes, adminiatored three fonl blows succonsively while Ba | seventh sad Bighth-aven, on Frilag, JHIB a1 alck p. . ATy Oy sy oy | With referetice to the side of the valley wove southward naturally, and so there is no objection | ster lay on the g { with his han mx. the Yal Tacalns will be taken to Gresuwood for iaterues '} Cures 2! SAty Rasve. ut, with classical promptitida, Teres n; rtaln that they are not [rozen sea- “ - | 1, advanced into rluilmlv e on thut score to the conclusion that extensive glaviers “filfl:“ «ryll'nlr of Habet" | wrTMORE-At uaarj. Ottr, N. J., on 'rn—ohh, Feb. 12, Fanole M., ot the mAas With which they were nttdelied and | changes in other years, and so that changes mig) ave ouce existod upon these level surfuces, moving | = Habet," us the it ] ., m floated away. Forli aclor foe, wll these foating | compared wlhich “oceurred in different parts of the | southward, for xlfinru wust be coualdered as | foul fn favor of o dnr.qnd{l{flm)h‘wmh_}lzl thuhht.- Prlonds aud nl-urv;-um amwily are in’ ‘1&::‘»':’-!%;’: [ ShOw an u.r»'{m.l Stricture Wy different from | year, or even different parts of the | meteorvlogical phenomena ' skin to the motion ter's fricnds. ‘The fight was for §600 4 BiGE (e FoRe (o Toskiunes of SISO . 2 ‘Tronen water formed upon ponds. The difference | day. Thus I have mseertained aud determiued the | of oceanio ourrents, whish move in the direo Wiho wore not satiatied with such a amafl affuirin uribis | v tor » shoe lsee, lln P Wit from the teansformation of the layers of srow both | change which the glacier undergoos durlug its ouw; Yon in which the equulization of temperature | managed to get nnnruuxll-ufl'. '.'(l:m i lvml wuma::x—o:ll'-t ln::-'A ook d y prossure and by thawinz. Thess misses of glacier ico | wovewent, the resalt, briefly stated, ~being tis: | takes place, aud this s from the north southward. Bub the @ound, on_the Naugatuck FaRIon toe e e o} the family a8 reqacated 1o atiend thy fieral ranular, like a kind of pudding-stone, coipented to- | that {0 this region the movement s about be usked, to what extent Lave these .‘l‘uwuun k“;m:(‘e;‘mut:' T amed Arnold of Derby, Conn. o' the heure ‘of James PRI o1 West Thirty-uiutdat., on ber by water frozen o he {ntervals 250 feet in a year, in the center; and the movement down Dhsarvations whieh § made | Arn 0 the Bewee of Jormtt N S uiens. ily dscortain that difference of struety | hero may he 14 fect in the center; and the movement at that kit up and down tho fuclosed track in (o thost | I Brookin, 1. D, on Tussday, Feb. 11, of congestion of the - T the mamner i W 1t | the lower end of the glacier will be perhaps only 15 feet & of the eouritry must have boen | Alsgusting ans Deastly maune! the space of twenty t h oo dectdes the fight on @ claim of | " quBECER 6" nd Jub & Wolsors, in the of position durlug one year might be e Ouvrwnr” u.l‘o.fl!ul-m-.l.!.ufl‘fi [ N TEITRR— SWATNES DEMAS BARNES & e . MecKiltop, Sprague & Cou Mo 57 Parkrow, New-York, PUBLISH AENUALLY, THE COMMERCIAL AGENCY mmk Th olwme containany Loy of the Busiaege Mcliwal parie of oo Staten sod Brival, Lvadinca with & ming indouiing (oo RELAT $Tavpivg AND Comumnciai Oxmaar oF Aok It she STAND @D Womx %‘{'flfp‘v‘mu vaar L e OLUME FOR 1647 um'e X and eostoros 4 10 its uatural color. Tha Dest arlicle i and Rensws the Hair, use. Warranted -~ Depot No. ™ Nassant. " of all_kinds BEPAIRED by ey .}E?mmu e O Ay o -@ 2 gy T AT N Uidis o you wast & whiff of aweet Elsiom 1o u pretty Ntle garden fower, but It st approach 1o It in We beavealy odor of PHA £ ¢ 4 rlon 8. Wilion. D & matier of wouder (0 seafurers to find that | year iu the center: while the moveusent up here may b “thing [1ke 6,000 feet In the - and 1 aim sat- | miuntes, © chwwing,” bItng ARl n5ing each other with ully invited to attend Wae fureral D LS ierss e sudi iy Gikigipent, sanieh s e e T o i e, Ch i ety Y Dot | ey oo that wo have had. s e Tt motéatation o interterence from the dolighted crowd. | Tie,( R ™ Brookiye, K. ... bo-morrow wero in & few m whle @ miass of wti1] Digher wp viot moré that 30 or 3 feetin u year. - All | tinent eovering the 1=nd to the de “Brosuey” had his upper b ML B B o o oug | (Vuoreday) aliermoon, a3 on water, which wonld bave these dumensions, | this results fioim the e l:‘w’lmflu or porosity 6f the ice, | feet. This spow tran sfo med into fee, thy pressure of the off, and fils head nearly K ll S -mmn An:yllrl "m. Hme to melt, becnnso 1§ welts ot the surface | its capability for the admission of water,io be frozen | joe upon itself aid the unequal penstra of | reporter left the “W‘;' Ne Slanat™ siabite™ tetny Goeds. It i from glaciers, | thiere, 4nd by its expatision to_produce motion fu the xla- | water through the wnss, s i jtselt » wuff wpon tho platform of tho sudl e NS : Moursig FOROADWAY. hus constastir on onetitution, and to one rewarkable | cler. Another fact is, that the sides wove wore | cause to bave determided this onward movem wherly | unconsoious and wuliceded | at | anY | A ARD W IAEKSON K et wl oter Nwining Dres t{hu ok, Which, is i WA | slowly thau the conier. 1 have had stakes placed | from north to south. Whethier this explanation bo true | dog, hlanehll‘l‘ L ghe Sodnt dlstance of About 30 foet pawia Cloaks, Vils, Crapes, Haudkerehiels t ihe sun’s rays (o penetr | e raliel"itnos 'all Beross the’ gin | or not. ft 1y certain that over all his continent we have | of the country DoTico SRR L ol thor thay ahosld ahica waited on wilh goods AL heir residecce ultaneously the temperatire of all the little intervaly | cier, and st short ntervals. so that there were o unmistakable warks of giacial action. We have these calmly whittilng sticks, ane e wl‘-‘o oo xmn’( ‘short notion No. 351 Broadway, opposske Tiffan; & Co. ich . interveue between the frugn s comented | twenty stakes on each lue; and I haye had them meas- | polished surfaces from the Arotic region down to latituee or should uot arreat U Tepo » 3 “ S er, and p nln-u Aismte in - ma :l‘udultn"'p«u!wl‘l'lluer\uln‘;"xmd “‘I’l‘;.‘:‘dh“ after a year [ 32°. We have this xnm\‘lm‘(.m 4 north-sontherly direc- ial Notices. M lceborg hose stakes would presen! oury S hat] “that is, the | rection, and we bhave, more than 1 A NOINeUse s v -] b S o swall K center hind moved the fastest; and on the sides the mo- | of loose bowlders over the wholo e thent, | PFRSONAL—Among the arrivals at the hotels aro fi!f‘ ial Noh wizé of azal 1ob or An g, and then all the frag- | tion had been less; 8o thal npon the margin the annual | all of whieh can be traced to rocks resting in plaoes north | W, Bodisco, the Russian Minister, at the Clarendon Hotel; | mmammmmneanssm it v ts melt away very papidly: 50 that this will explaii | motion was b pore than ten feet, oven bers, whero | of the position they —occupy. Now all this | (Co00 T audrew of Massachuseits, at the Brevoort rapid disappearaie of large icebergs when they have | i the ceut Imation was 260 foet Now thio masas | ehows the hotion has becd from the north southward, and | €% (0¥: f Rhode Island, at the Fifth ave. into temperate seg 1 Whe the e TPl b the wluctors will TIove 8 the Thie oy | 18 refottncn (o the clanging ‘empernture on bur earth, | House: Gov. Burnalde SIS "L atie hnoYon. B. 1. y the temperature of tho which e e eambug - DA OF T ginciers | EhAY evidapon 1b enough w Juskiy the eonsladen thapiny | Hotol sehe EHopc THOWER KU U NETT U Bowon, 798 vl By our attention 10 thist Gact of the L g enmoplence” 6f UICHEC poculiar struc: | menss giaeiors bave extendcd over tig continent to the Loss and Win. 1 Sowar b S0 ey | Loas NGHT ELOOMING CBRLUY Vecause 1 suall Kave "to ‘rosort Wo shall find “eiat bowl il i | (U000 T v ol Gy Gk o Uy i | e CHAOORIMBUTAGER ook y explain