) The Inactive Craters of Vesuvius. BY PROFESSOR D. T. ANPTED, F. R S. There exist aioiir.rl Naples eo many volcanic cones, sud luese aro In conditions so different in some respects, and so similar In others that . they are objects of very special internet to the gooloaloal traveller. But they are hardly less interpslin to thoo who have no special interest in gpolosry, for most of them may be brought into direct asHOclation with the historical events for which this part ot Italy is bo remarkable. The writteu hihtory of the eruptions with which they are connected hardly commences much belore the Christian era, but after this they mark, by some corresponding event, almost every ecu tury s it passed away. Some of them, no doubt, are very much older than any recorded historical events, for unrter other appearances perhaps these, as well as the old cones and craters of Vesuvius itself, have seen many human revolutions, even if they have not ante datod the human race. The whole country, however, U full ol interest. We turn from a modern lava current to look at the Heps of old lava on which St. Paul trod when landing at Tuteoli, on his way to Rome. After examining craters long since extinct, and serving as the foundation of many an early pagan legend, we nd clo?e by the grand subatructions of an am phitheatre, in whicii old paganism, still ram pant -though almost In its dying agonies, at tempted to Etamp out Ike flame of the new religion, by forcing its advocates to fight with each other, or with wild beans better taken care of than the human victims There are hundreds of such points, where the Interests oi science and history are so mixed together tha' It is difficult to separate them, or forget either one or the other. All the important craters near Naples not actually forming a part of Vesuvius itself, are on the western bine ot tne city, in the district of the Phlegrtean fields, and the islands beyond. The nearest to Naples, one ot the largest and one of the most remarkable, ii tnat in which is placed the celebrated monaitcry of the (Jamul cloni. Within this is the lake of Aenauo, a newer cone and crater, where is the well-known Grotto del cane, lteyond is the grand crater of the Aitroni, and next it the familiar Soli'atHra. These are succeeded by the smaller cones of the ilaranisl and the CiBliano. The Monte Barbaro, with its Campilione, a large and deep crater, next iollows, and near it is the Monte Wnovo. Beyond this again is the Lake Avernus, while the Monte Grillo and Monte Kosso, near Cumre, are immediately adjacent. The islands of Nisita, ProelJa, and Jschia also allbrd ample proof of the extension of the line of volcanic action in verv rvwnt times to a considerab e distance bevond its pre sent apparent limits, Nisita being indeed a verv perfect crater. Tne whole coast abounds witii all kinds of indications ot subdued volcanic activity. These cousist of eruptions of hot air and steam, numerous thermal springs, cele brated in ancieni aa well as modem times, gaseous emanations, and occasional sulphur t-prings. The ground has been and still is sub ject to elevation and depression to an extent sufficient to afl'ect seriously buildings near the f horc. The celebrated temple of Jupiter Serapis, at Pozzuoli, afloids ample proof ot these move ments, and the whole coast has evidently under gone a great change in comparatively recent times. It is doubtlesi still movinar. The lake ol Atrnnnn in a trnnrl inlrnflnt!ni. t the pheuomena usually presented by these silent volcanoes, and it is very accessible from Naples. It is surrounded by hills en tirely composed of tufuceoiM ash, greatly worn down by the weather, and tbese walls of ash form a large crater, depressed to about the level ot the sea; it. is doubtless old, though newer than other tutaceous lulls round Naples. In the Roman times its shores seem to have been already covered with vesetaiion, and its bed was not, as it is now, oiled with water. It wa. indeed, partly built upon ua louabitca. li--jnains of masonry and brickwork on a large scale are still to be seen at the bottom of the lull, near the edges ol the lake, and on the sides of the crater. There are also marks of tunnels, probably like that ot Posilipo, which have led into this crater to avoid the trouble of mount ing and descending the hill. These are now avoided by an open cutting, which exhibits the structure ot the cone to the level of the water. As far as this point the waole is tufa, and there seems to be no lava. The lake of Agnaiio is a delicious specimen of characteristic volcanic landscape. The volcanic ash has been very easily decomposed, and reaaily converted into a good soil, and thus the whole of the inclosing hills are richly clothed with vegetation. There are inuny small but picturesque villas and pretty garJens around it. The outer circumference ot tne inclosing hills is nearly three miles, showing a large crater, and the greater part of the bottom is now occupied by - water. The inclosing walls are less regular than most of the detached cones of any sue, an J are comparatively low and open towards the north. The flat, covered by wat?r, is very unhealthy, and measures are in progress to drain the lake. Jt may gain in salubrity what is lost in pictu resque beauty. Ou the southeast side of the lake is a building with the remains of old stuff, or chambers where not vapor issue at a very high temperature, and immediately be hind this are very extensive ruins, probably of Roman baths. The hot vapor issues at a temperature of 180 deg. Fahrenheit, and is sul- Jihurous, though not very stronply so. Close by s the well-known Orotio del Lane, where is an issue of carbonic acid gas and hot air with steam. The heavy carbonic acid gas, the choke damp of mines and wells, remains on the floor of the small cavern in quantity sufficient to asphyxiate dogs orothersmallanimals.forcedto remain near the ground in this atmosphere. The experiment might be tried with equal suc cess, and Rreater convenience, in a brewer's vat. These emanations of gis are, However, interest ing, as proving the existence of subdued and partial volcanic activity in this spot, which has apparently remained in the eanie place, and to the same extent, for the last two thousand years. If the visitor desires to sutisfy himself of the state of the case without stilling the dog, let huu dip his hat into the gas at the bottom ol the cavern, and approach it to his mouth to drink Pi' breathe the gas. Beyoud the lake of Agnano, to the west, is a valley intervening between the old cone of Agnano and tbat of the Sella! ara. In this val ley, and just uivler the walls ot the cone of the Afctroni, which rues immediately to the north, are the hot etufe, or vapor baths, ot the Piscia relll, prod uced by fumeroles In the rocks form ing the back ot'the crater of the Solfatara. The whole of the lava ot the hills on the east of the Boli'atara crater will be found converted Into china rlay. The ground is covered with aluminous eulovescence, while the soil of the alley is hot, and abounds in fumaroles. Ttoere are said to be hot springs issuing nearly at the tooijing point, and loaded with iron and lime, besides containing free sulphuric acid, a combi nation extremely rare. The sources of such uprmsrs must have intimate reUiion with the cavities under the crater of the Soliatara. The Msciarelli were called in classical time Fonlea Ltuuoqasi, from the white color of the grouutt, now removed to burn lor fine china, and tho waters are still used for medical purposes by the lower classes of Neapolitans, under the name oi "Aqua della Bolla." The 8olfatara itself is the crater of an old volcano, in which a certain amount of activity is still Vaceable. it Is an oval saucer, about six hundrod studs In its longer diameter, and is ourroi'nded, except on the southeast, Dy walls of tufa, beloniriuif to an old cone of eruption. The open side teems to have been broken throuvn by a current of old lava reaching to the Ufa. but much decorrmoaed- Thnrn is an emo tion recorded as hnviug occurred A. I). 1198, but ine accuuuis are oi mils Interest. It was kuowu to the ancients as the "Forum of Vul can.-' ana was oenevea to connect with Ischlu. TgEDAILY EVENING The principal erur tions from it are probnbly long antecedent to the historic period. The nppcaranre of the Hollatara on first, en teilng the ,1ncloBed area Is not very striking. The ground Is flat, with here and there pools of white ttntrnant ' mud drying on it sur lace. Klsewhere the ground is broken and partly covered by vegetation. The point ot chief interest appeals to be the vent, which Is at the farthest extremity, and ii always emitting steam at a high tciu- tierature. The whole ground reaounrts to the ipavy stamp of a foot, as If it were hollow. On approaching the principal vent, an almost con tinuous putl of steam is seen, accompanied by a strong rushing sound, and on going near, the temperature is lotind to be extremely hiirh too nigh, Indeed, to allow one to make an ob servation within the crevice or cavity from which the vapor Issues. If a lighted maich or piece of paper be placed near the point of erup tion, large clouds of dark smoke roll out. being rendered visible, it would seem, by the ap proach of ilame. There is a sensible smell of chlorine accompanying the vapor, aud both sulphur and arse ate are deposilcd by sublima tlon on the stones around. Sulphuretted hydro gen and sulphurous acid seem to be present in the issuing vapor, but In very small quantities. The presence of arsenic hat Den remarked 1n the uisiriot, and the quantify here is rather con siderable. The bottom of the crater ol the Solfatara is about two hundred and seventy-live feet above the sea, and its walls (the ancient cone) are now probably about two hundred feet higher than the bottom of the water. They are rather tuwp, and are composed chielly of volcanic tutf, the beds of which show mark of lilting in one part, near which are small caverns, from which lumaroles issue. They are, however, much weather-worn. The principal vent is within a fissure or crevice at least one hundrod yards In length, extending towards the south (vest j and on the line of this crevice are numerous smaller fumaroles, from which hot steau also proceeds. At one of these, near the principal vent, I was able to note the temperature, and found it to be 97 C, or within three degrees Centigrade of the boiling point of water, within eight inches of the surface. The rest were less hot, only because they were more cov ered and less accessible. To the north of this main fissure there are others. One of them is distinguishable in the caverns already alluded to, which are so hot that ono doe not willingly remain long in them. They are of no great size, and rnn in only about thirty or forty jnrds; but they are interesting from the exquisite and delicate crystals which line their wails. A rate mineral (Coquimbite) is espe cially abundant and beautitul, but the crystals are too iragile and delicate to be easily con veyed away. At many points where fumaroles show themselves, the peculiar phenomenon of smoke arising in abundance on the contact ot (lame, or even of smouldering red heat, such as the end of a cigar, may always be observed. The cone next in order, and far the largest of all, is tbat ot the Astronl, the crater of which is now the nursery for the King of Italy's wild boars, and Is only accessible by special permission. This, b'owevcr, is ob tained without difficulty. It is a very large and regular depression, the ton limns a mil aud a third acros in its larger diameter and a mile in its smaller. The crater is nearly a mile ncrofs at its widest part, aud three quar ters of a mile in its smaller. Tue outer circuit, or rim, ot the cone is more than four miles, ana is entirely unbroken, except at the entrance. Av;ewof (he Astronl, and the Lake of Aenano from the monastery of the Cnmaldoli is almost necessary to appreciate the very singular lea tiires of the district, and also clears up points that seem contused and obscure w ien only the lower ground is travelled over. Looking down from the terraces of the convent, at an elevation of about lourteen hundred leet above the sea, one i9 able to perceive the outline of a large cone, now much broken, but still fairly indi cated, partly by the ridge between Naples and Malta, connecting itselt with the hill of the Castle of iU. Elmo, and partly by the low hiils of Atenella and the higher elevation on which the convent is built. These have In closed a long oval space, about two miles across, and lour or five miles from northeast to southwest, but mostoi the rim of the crater is gone. A part of tne bottom of the crater belonjrina to this cone is seen from thei (Wtlvi.nl prrau out at one's leet, covered with small vil lages and well cultivated. Much of the cone was destroyed by the eruption ot the smaller cone ot Agnano, already described, and whose crater is now a lake. This destruction of one crater by another is common enough, and is ncn uiusiiuieu ui t cbuviiib linen, w nose present cone occupies the place of the more ancient cone of Monte Somma. The group ot coneB beyond, of which the A6troni is the best, may be re garded as belonging to the same series ot erup tions, all taking their oriain in the main fissure ol the Phlegra-an fields. 'Most of them are later in date than that of whose cone the Camaldoli range now afiords the best lndicution, and the exact order ot sequence is not quite clear. After visiting the Camaldoli, the next visit should be to Astroni. It is beyond comparison one ol the most striking and p'ieturesque placeg near Naples. The road to it is past the Lake of Agnano, whose crater has been partly destroyed and intruded on by the formation of the Asuoni cone. This is as nearly perfect as if it had been lormed yesterday. The circumference of the bafe is that of the present cone of Vesuvius, and the crater is larger. But as the cone of Vesuvius rises from a pluteau nearly three thousand leet above the sea, and that of Astroui irom the level of the sea, the appearances are different. The actual elevation ol the Astroni cone is also much less considerable, and the outer slope much more gradual than in the case of Vesu vius, though still veiy steep. The lowest part of the Astroni cone is towards the east, and Is not more than two hundred and sixty feet above the sea. The higher part is perhaps another hundred feet. The Vesuvius cone rises fifteen hundred feet. But It must be remembered thnt after a few thousand years of weatheriuc. little more than the bard core of rock bel msiner to a volcanic cone can ever remaiu, and ih-re!'ore the original outer coat ot ashea ot Astroni may have been once lofty and imposing enough. It is not till we enter tne crater that any tuea can be had ol the sini'iilur annom-nrim tliern nrPKnntorl il.it. side it looks only a Kteep hill of no great eleva tion. The moment the lodgo is parted (a kind ot tow er constructed at the lowest point ot the rim of the crater), the full meaning of the hill is recognized, for not even in Vesuvius ,s the cup- uae appearance oett'.'r wen. The read enters the hill as if from a crack in the rim. and presents to view a complete cup, with a somewhat irregular rim, depressed about two hundred and fitly feet, or nearly to the level of the sea. The sides of this cup are partly naked rock, but lor the nioet part are richly clothed with vegetation. Where the steepness is not too great, forest trees riso from little ledges, or thrust tneir roots into the crevices of the rock. The bottom is nea-ly level, with the exception of a small hill (also conical, and provided with another little crater), which rises out of it to the rizht. Three lakes, one of tolerable size and considerable depth, are seen in tne ainereni parts, xne Dot'oui is also covered with vegetation, generally of well-gro .vn forest trees, A cauiage road winds down one cide ol the interior, and terminates in a fine avenue crossing the tloor ol the crater. The ciater features are all admirably retained; and inut-ea tuo penect cup-like character has been rather assisted than otherwise by art in conse quence oi iue ubu io wuicu tnis curious valley is put. It has long been kept as a pre.erve of wild boats, formerly for thu Kin of Naples, now lor the King of Italy. No placu can be oo:i ceived more admiiably adapted, lor iho purposo. There is a park ot nearly five hundred acres in closed within a natural rine-tence of hill, clothed with luxuriant vegetation, and for the most purt much too nearly vei ileal to be scaled. ThU natural fence is nearly circular, and its heiiut varies from about two huudred and dfty to more than three hundred feet. One would think tbat no animal that doe not fly could tntcr or escape except through the gates, but as additional securitw.a high attillcial wall is built on the ridge otTho ciater. Within this area, which was once the nntuial throat through which fire and flame, hot steam and gases, and red-hot atones were ejected, and troua which TELEGRAPH TI 1 1 VI At SUKKT. P1IILDELPIIIA, SATURDAY, OCTOBER 27, 186G. tlio whole district was once burled in ashes, there 1 now no indication ot volcanic, energy. Kverjlhing is calm and Mill, except when the hunter comea to disturb the wild boar in his lair. The Mor.te Ciffllnro is a tmillcr cone, with a deep ciater, between the Astronl and Monte Bnrr-aro. Monte Csmpann, further to the uoith, and detached, is of the same nature, but neither of theso dilTer essentially from the Mouto Nuovo, which Is much more recent, and atloids more perfect illuetrnlions of its volcanic cbaractei. Tbe Campiglione is more distiuctive and very niuca larger. It is the name given to the Hat bottom of au immense crater, and its soil has long beer, remarkable for extreme fertility. The b ill forming part of the cone once inclosing the plum is called the Monte llaibaro, and is qnito as remarkable and valuable as tuo plain, inas much as its vinos aro among tbe besi, in tho teighboihood. They are among those that In the palmy days of Koine yielded the real Fnler nian. Before the formation of the Monte Nuovo, tbe Monte Barbaro must have been a promi nent oblcct from the sea, but it is now con cealed. The wehering of scores ot centuries bns also no doubt helped to reduce the height of this cone, and raise the bottom of the crater. The Monte Nuovo, formed with extraordinary rapidity in toe year 1358, is in some r-spocts the most interest iiur, as it is thenewcaand most perfect, of all the inactive craters around VcbuvIus. Very minute accounts remain of this eieat eruption, which was apparency tonicwhut ditlcrent from what is usual IK the distuct. Shortly before the final outburst, numerous earthquakes, rapidly suc ceeding each other, convulsed the whole dis trict of the Phlegnvan fields, and produced permanent changes ot level overalsrgn tract of country. It Is even recorded that the sea line was removed about a third ol a mile back in many places, while in certain limited areas the ground sank, forming gulfs and wide and deep trenches, from which water issued. Tbe water was at first cold. It soon became hotter, Increasing to the boiliug point, and then issued steam, at a high temperature, blackened by laige quanilt cs of volcanic dust, forming a dense mud, deluging Pozzuoli, and reaching as far as Naples, about ten miles distant. On the cessation of this eruption of wet ashes and mud, dry ashes and red-hot fragmeuts of scjriae suc ceeded, and were thrown out in pnormous quantities, reaching even ono hundred and fifty miles from the spot, la the course of loss than three dnys a considerable bill wa formed lound the place of eruption. This fill at first was a mile and a half in circumference, and rose to four hundred and iorty leet above the sea level, completely covering a village, and filling up more than haif ol a large lake at a little distance. A lew smaller eruptions of the same kind followed niter very short intervals, but since then ovcrr thiug has been pericctly quiet. No lava cur rent issued, and tbe mischief done was com paratively small. It is impossible to visit and examine the Monte Nuovo in its pretent state without recalling something ofi this history. It is, perhaps, the onlv cone and crater of eruption in thj ncih" borhood in which there has been no apparent change produced by the infiltration ol gases and stenm since the close of the original erup tion. There are no slufe or hot-air emanatlous in its immediate vicinity. It is the result of a tew days' subterranean activity commencing suddenly, and terminating completely altera a very short time. On the 28th Sootpmbar were felt the first serious indications of approachin" volcanic activity; aud on the 6th of Ocrober lol'owing the last were ob.erved. ' In this seven duys, however, much was done, and the ellccts still remain. There is stdl the conical hill rising abruptly out of the plain, and show ing at the top a circular ridue. The elopes of this bill 'are still composed of scoriaceous lava and black volcanic sand. The substauce of the hill is tula, with dykes of coarse scoriaceous lava. The summit, however, is now les than tonr hundred feet above the sea (three hundred and eighty feet according to ray measurement with a good aneroid, but under unfavorable conditions oi the atmosphere), and Ihu3, if the old estimate of four hundred and forty feet is correct, it must have been greatly lowered by the rains ot five centuries. On reaching the ridge, which is easy enoucrh. the sidus hninir covered with low nud'nvood and trees, we look down into the orator depressed about three bun dled feet below the highest part of the ridge, aud only about eighty loot above the sen. The walla ol this crater are still very steep, and the pi. down to the circular area at the bottom w inos round the inside. This area appears Hat but is hiehcr on the side towards the north east. It is cultivated, yielding pood crops of maize aud some varieties of vegetation; aud thus its soil, which is entirely volcanic, has decomposed favorably. The walls of tbe crater are tuiaceous, and incline at a considerable angle. They are cut by a few dykes of hard rock. The diameter of the circular plain I estimated to be abont on? hundred and ek'hty yards. In the lust century, according to Hir William Hamilton, it was considered tbat the depression of the cratir beloiy the burliest pointwas rdmost as great as the elevat on of the highest . part of the cons abjve the sea, the latter being four bunored and, lortv and the former lour hundred and ninctn, showing a dulerencc of twenty-one leet. At present the respective tiiruresare three hundred and eigh'y, thiee hundred, ai.d twenty feet. The chief alteration, as miehl have been supposed, has been in the height of the cone, which is easily acted on by w eather. Shells have been occasionally found in the tufaccous mass of which tbe walls or Monte Nuovo are composed, and 1 found fragments both of iron ore and of compact basalt, the latter in considerable quantity. These were, no doubt, poitions of the 6trata detached and thrown up into the air by the lorco of the explo sion. Itlj said by some ot tho observers that stones as large as an ox were thrown up into the air during thu erurtion, and no one who has walked over the slopes of Vesuvius and measured the bugH uneuiar blocks of prey lava thrown out within the last few years and still unaltered, can doubt that Ihis is perfectly possible, and even probable. Beyond the Monte Nuovo we come to the in teresting and classical Lake A vermis, also oecnpying au inactive crater. It is larare, the lake being a mile and a halt round, and onon towards the south in the direction of another well-known piece of water, the Lucriua lake. The elooiu that once attached to Avernus has now disappeared, and it, as is not unlikely laree quantities of carbonic acid gas were emitted irom crevices In the neighborhood in the riu sical times, the.-e also have been choked up. It seems probable that the crater was then in the state of the present Hollatura: and it is quite certain that 1he changes of level that have been alluded to in speaking of the Moute Nuovo eruption, greatly affected the condition of the whole nsMuhUoruooa. ine enects or the gases issuing Irom the earth in all this neighborhood were well known, and marie srood use of bv tnn priests of the pauam temples that abounded in i he diHinci) -anu it was. not un tne tune of Augustus, when the Avernus and Luerlne laues were connected by an open cut with the sea. und formed a port, that the terrors aud super stitions connected with tbem died away, and inev were renoereu neaituy ana habitable. This port was destroyed by the Monte Nuovo erup tion. In tho last century the lake of Avernus was sounded, and found to have a depth of five hundred feet in tbe middle. Beyond the coast ol the mainland of Italy are the islands of Procida and Ischia. They have been supposed to be parts of one great anciont tia.ter. There is not much to piovo this, but beyond a dovibt they ore parts of volcanic cones. They are interestina islands, especially the Hitter, in which numerous hot springs still prcve the intensity of the subterranean boat. Is?cliia was the chief seat ot volcanic activity m this pnit of Italy previous to the great erup tion ot Vesuvius in the first century of the Chmlian era. . Ttiu-s, then, It appear that Vesuvius, now the nlv active volcanic vent io the nelhborhooi of Naples, is but the most recent locality in which a long scries of eruptions, commencing at some unknown period, has come Into activity. Other places, espeolal I v in the no eh borhood of the Solfatara, exhibit a partial activity that seems to have eue ou with little change from time immemorial. Others again; as the Island of Ik-Mji, preceded Vesuvius in a long coerse ot activity, but censed when the newer vent was opened. Olhers pre ccried lochia ns many aaes as that island antedated Veiuvius, and ure now fertile plains and valleys. The whole district extending for about thirty five miles Irom east to west, and nbjut twelve miles from north to south, is also intimately conreclcd with tho older volcnnic vents to the f orth and east, and thoe ol newer date to the south. The Vesuvlan disirict, the Koman dis tiict (near Albano), nnd the Ema district, are ail connected underground. At various points there is activity and energy, for there Vulcan's thunder fliill giowls, and his stamp shakes the earth. Elsewhere there is present repose and inactivity. - But everywhere in this part of the world the dangerous tires are smouldering ani not extinguished. Theyburt forth from time to time, and no one can foresee or foretell where the next point of dinner may be. Thus the ex tinct and inactive volcanoes are hirdly less in teresiing than the cones of a few years ago. still smoking and always threatening. 2?rn;'e Lar for Oitobcr. . 1 LUMBER. 1 L OO K 1 M O I P L O O R I N V, IOUU. JTLOOIUMM FLOoKMOl! 8-4 CAhOl.lMA n.uOlllMi. 4-4 CAKOLINA i LOOKING. -4 VIHU1MA F..UOhINU. 4-4 VIKGIMA KLUOKINU 0-4 JiKLAWAKK t LOOKING. HIltLAWAHK KLOOUING am: m walmji r.ooin.sG. ASH AM) WALNUT FI.OOltlKG. MM' HOAIIDM. WAIL 1'LANK. 1 P( C lJ J A S T K R 1 N 0 LATHS 1 IOUU. l'LASTERlMl LATHS, AT KKM if h THICKS. AT REDUCtU PRICES. 1866 -CEIAU ANI) PINK MIIXfJLfcS . ttUAK AM) riK SHINtiLlid. PO. liUMI tMIAK PHIMILKS. JiO. 1 SHOUT OEDAK l-HINGLEH. WHIT. I I SK MUNULKg. . CYI KfrKS BHIM.LK8. FINE ASSORTMENT tOU BAlC LOW 1 Q(il LUMBER FOR UNDERTAKERS! .LOUU. Ll ilBEK FOR TMiEBT AKEK8 1 1 Hi T) CEDAR, WALNTT, AND FINE. HEP CEDAB WALNUT, AND PINE. 1866 ALBANY J. UMbEROFALLKINDh , ALIIANY LCMBEK OF ALL KlilDH SEASONED WALNUT. Iltt JOITAB. ( UfKlU, ANIj A8H. OAK I LK. AND BD3. MAHOGANY. HOPE WOOD AM) WALNUT VENEERS. 1866 -CIliAR-BOX MAN UK ACTCR 6 Rg ClGAli-hOX HI AMlFAnnnEIM. bl'AJMMII UMIAK 1HIX HOAKDCi. AT KEDUCED I'KlCES. i QCUZ SPRUCE JOlSTl SPRUCE J'HT J-OUO. fPHUCE: JOKSl I 81'BUCK JOlsTI E KOM 14 IO 82 FEET LONG. ' FHOM 14 TO Vi FEET LOivG. M'RUCK KILLS. HEMLOCK l'LAv AND JOIST. fcAOjLLrt." ' m A1AULE HROTRFR CO, ftZfmrp .o, Sato BOLTH STREET. rP W. SMALTJi'S LUMBKR YARD, N. E. COlv L . Ft F'l HCN'I H ami oTILKS Btioeis, t. , , CDF.AP FOR CASH, w liiie Fiue, seasoned. i.1!,1,r!tiMC!""1'1"l,")' Yellow (4 4, 8-4) aud White Miio (4-4) F.onrlDK Hoards. ia'jnl socoud yua.ity one and two-sides Fence i helf Ing Bonrd, Buss, sh, TManks and Boards. White Flue Bills all sues Btop Board, 4 4 6-4 ' "wWtha11 J-St d ocaulllu' ft"0 to 28 leet long, Bnruce Joists Bills, and Scantling from 12 to 28 feet. 1' no all wlot'ig. I'lasterliig La'h (Engllsb and 'alalu) Pickets. Bhlngies, (Jnesnut I'oat. etc. , - iMuliosany, Wa nut Flank and Board. All kinds oi Building Lumber cut and furnt-hoi nt the shortest notice, at the lowet price. H JJ lm UK 1 T EDS?A T E 8 i BUILDER'S MILL,'3 Ncs. 24, 26, and 28 S. FIFTEENTH St FIllLADELrTUA. k , j ESLER & BROTHER, WOOD MOULDINGS, BRACKETS. BTAlB BALUS TERS, ' KEWEL POSTS, QXltAL TCiNlNO, SCKOIL WORK, ETC. BUEI.VI.NG J-LAN ED TO ORDER. Tlio lurfeCKt a-eortn. tnt ol ood MouIdlng In thl-: city com-lauilv on band. 7193iu J C. JERKIN 8, LUMBER MERCHANT- Succoi-or to K. Clark, Jr., No. 324 CHRISTIAN STREET. Ccnetantij on hand a lro ail Taxied aasortmet of Building Lumber. 6 U4 WHISKY, BRANDY, WINE, ETC. N'o. 2'.' is'ortli THTKD Brreeu II HOvthlrK R aa wanted to p.ovc the absolute pprlti ot t Ins niilt.fe.r, ti e lolloping certlflcaten should do It 1 here Is uoa coliolic tiituulam kuownoouiinaudluiraucl li U-U.ii.mULU i urn such liliJi ouic(h . t i'LiLAPELi HiA, MeptembcrO, 18j. GLOW. H HllsKl wuichjou aend ua, and rluu tliat It conu iiisxoMui'Tiix roieoxoua amsTAKCB known ai i ami. ml whkb Is tLc characteristic and Injurious In KOOTii, OAUitKTT C A SI AO, i Analytical Chouitoti . 1,e" iouk Heptttraben, less I have analysed a sample ol CHfc.r-.NUT fiilma IMilbKY retched rem Air ibarlea Wbarton.Ji i 1 liiii.i e.phlu; r.nd tiavlng carulully teaied it, l " an p ei.xiU lo mate tl.at It Is entirely vukefuom poisonou k .t i. vuidia HuLHuiaen It la au uuuuuullf pur auu flm-ii; v'.red uua.llr ol wlilnky. JAMLS B. CHILTON, M. I., Analytical tliouns ', . Bostox, Waroh7,I85l. t ravened a rtifmltnl ana yslf ot commercial saa, vi.tso: C liI.WMT A.KOV1-; WBl.-tKK, wblcli ptoveaw I f tree li in the heavy Fusi! OJig, and peneoily pure an ui.tCulTiAU'd '"! tine Hanoi ol tbls wulaky 1 derive 'turn tte tmln mod In manulaaturluglt. iieptctiuliy, A. A. HaYM, M. D . Mate Assayn, No. i l!oy:tou stieet Kcr tut t i.HiTPi.doni! otin, cr bottle at&'o.2iJNortk I H1L3J blreei f nllude.i.lila. ; 7 i KATUAKS & SONS, I M J'ORTE II a OF - ; UUANDIES, WINES, GINS, ! Eto. Etc. - Ko. 19 North FRONT Street, riilLADELl'UIA, J M08KU KATBABB, ' HOTIACE A. HATBAKK, - 1'KLAKllb P, MATHAIB, 10 2 JpllED. BALTZ & CO., 15IF011TE11S OF WINES, GINS, Etc SOLE AGENTS FOB Riviere, Cardat & Co.'s , COG A AC Ko. 110 WALNUT STKKET, lliiLACELriUA. LO 3 3sa CUTLERY. C U T Jj li It Y. A fine assortment of POCKET and TA1ILK CL'TLKKY, KAZOUH, KA lilt KTROI'H. LtlllKn' H01SMOK4 lAlflt AM TA1LOUH' UUKAKh, 1TC. at L V. HKLMOLO'S Cutlery Store, Ko. ISB touth 1 K.N I H street, SliSi Three doom above Walnut ITODCJLKS A WOSTKNIIOLM'S POUK ET J V Knives. Hodiiers Wade's aud llu'chor'i Kazorx, 'lub'e l utlerv, Ladlea' BclHSora In C'abes. liaxorj bciraors anil an Kinds oil utlerv ground aua poiuneu tL. MALttlHA'8, No. 115 b.'TLKiil Bueet, oelow litunut 16 JO 01 "VT EUBALGIA CURED RED BY A SINdLE ApPLI M't MAUMKTie OIL" Bold H. K1UHTU Bireet, lalahotile WlluifV X eatlon ofUmAM at ITl'l.AM H Mil 9H m LruKKim. S(i ocuti aud II ixUin RAILROAD LINES. 1DIIILADELPIIIA, WILMINGTON AND HAL- X llilOKE HAII IIOAI) TIK TAHI.E. airomrtichiK MONDAY, .lulv 2, WA Trslnt will Itave Depot, corner of LKOAD Bttcct and WASUINOTON Avenue, tin iollows: .rea Train at 4 15 A. V. (Mondays exrepied). lor 1'nltinior and Watnlnglon, atoppiim at Cheater, limlnii le ii, Newark, Klkton, Nertheant, I'trrv villa, Ilvre-de-t Fare, Aherdeeu, l'erryiuan s, Alagniilla, Chases and hu nimer s Kim. V.v Moll Ttain at 8-lftA. M. (Cnndaya excepted, for raliimoie, topiiiiuratallreK"lar stations between I'hlla d It lila ai.d Hxitlinore. Deiiiwaic Kntlroad Tinln at ! A. M. f Sundays eeepted), f r rrln-en An: e, Mllford, and Intarnieillnto stations. I .xprc ii. Tialn at 114" A. M. (Sundays exceptod), for Kalimiore and Wafhlnvtcn Kxpress Train at 3 1. M. (.Sundays excepted), for Till llmoro and WHhliigtoii, atnnplng at t.'liester, Claviuont, Wilinintton, NewBik, Blkton, Northeost, Per'rv villa, Ilavrc-de-Crace, Abirdeen. I'enyiuan a, KdKewood,' Maii lii'lla, ( hnse s and Hleniuier's Run. Mulit K.xpres at 11 1'. M., forllaltimore and Wanhlnpton. Tajfeniiers liy Boat troin Hal (more for Knnrpxa Mon roe, Norfolk, City l'oinl, and Klcbuiond, w ill take the 114 A. M. train. Wll.MINT.TON ACCOM MOD ATION TRAINS, Pli P,lnK at all (Stations between i'liiiadi'lplila and WO. Ulllinlcll. Leave Phlladplpliia at ft A.M , lS-HO, 4 30, 0, and 11 'W P U. The 41.0 1'. M. train connects w-iili Deluwaie Kallroad lor llnrilPKlon and intermediate stations. - l.eae Wilmington at ;ni, 7 li, and 9-RO A. M., 4 and :.!'. M. The i-lftA. M. trnlnwlll not stop at staUous tr;wicn Chester tnd Phliadolphin, Trains for New Casilo lcae l'lilladc phia at 9 A.M. 1-uOand P M. T1IIiK;H TRAIN'S FROM BALTIMOUK. Leave Vl!mlnttii it 11 A. M , 4 :! and 10 P.M. Cllhtj'I Kit FDR rilll.ADhLPni.V. - JV.".. C,ICs,",r ' " I''. 10 14 aud 1H0 A.M., 4 13, 5-10, 7-II, and in : u P. M. FROM IiALTIfcORB TO rillLAtlKLPHIA. Leave llaltlm ie i i, A. M , Way. mull, 9-iW A. M., Ixpie.s. MOP. M .Express. 6 36 P. M., Express. 8 P. it , Express. 1 'J RAIN8 FOR BALTIMORE. I eave Cesler at 4 -in ami 8 .vj A. M , and : ,"8 p. m Leave W ilinliiKton at A V-l an.l H A. M., and 4 1:, P. M. l niKlit Iraliu v illi I'asscimcr Cais attached will leave ns follows : V llD'ltiBlon, for Perryvi le and In emieulate nations n! (I Oi P. M. llalllinore, lor Havrivde-Grace and Inuiiiieulale slations at 4 4.'i p. M, Perry villa liir Wll mli Ktrn ant Imo medtntp Hn:li.ln at 4 Vl A. M., connoct-li-K at Wi inlngton with 7 l"i A M train lor 1'liiiauclphla. Bl.'NUAY 1RAINS. ' FxrreMTra'nat4-l.'iA. M., lor Pnlttmore and Wash Irgton, lop Ir.jj nt Chester, wrminirton, Newark, Kiklon, .ortui sxt; Peiry llle llavre-de-l.raee. Aln tdeeu, Perry uian's, MaKPoiin, Cliase a and Riejnmer's Rnn Nlht Kxprtss, 11 P. M . lor Baltimore and Washington. Acconmoilatlon Train ut HMOP. M. for Wilmington and InttrtncdlHie stations. BALTIMORE FOR PHILADELPHIA. Leave lialiiuoie at r. M , stopping- at Ilnvre-de-Cracc.Perrjvllie.ntiQ WilmliiKlon. Alio stopi at Klkton nnd Newaik do take passenKevs tor Philadelphia and loavo pai seiiftera from W ashfnulon er Balt'moi e), and Chester to leave pussi liners from Unit I more or Washington. Acei liinioilallon Train from Wilmington lor Philadelphia and Intciniedlate stations at6'2C P. M 4 I'l 11. F. KEN'NEY, Stiperlnten lent. FOR NEW YOEK.-T1IE CAMDEN AND Amboy ai d rhlUdcijilila acd Trenton Railroad Com 1'iiiiT Lii.es. FROM PHILADELPHIA TO NEW YORK and Way Placet, from Wulnut Street Wliarf.wlil leave as ii Now s, vlr. : rABB. At 6 A. M , vln Cimden nr.d Amlioy, Accommoja- tion At 8 A M., via Cauidcn and Jersey City Express 8i0 At i P.M., viaCumueo and Amboy Express 8-OU A! !!... via I sm.li n mid Ambov Accomuodittlou anil V iiiinnnt 1st class 2'3o At ii P. M , via Camden and Auiboy Accommodutlou, and Fml.rant,irelasi ly Al 8 A. M.,!l and ft P. M., for Mount Holly, Ewnnsvllle, , 1'en.herlon. and Yincentowu. At l A. M. and !1 P. M for 1 ri-ehuld. t j ardlO A. M ,12 M., 4, f, (!, and 11-30 P.M. fbr Fish liotise, Palmyra, Hivcrton, I'rorrei.s, Oolanco, Beverly, " liwuter, liiiiliiiKlon, Flirence, llordentown, etc. The 0..' M. mid 4 P. M. lines run direct throiiRh to Trenton. LINES FROM KLN8INI1 0i DEPOT WILL LEAVE At 11 A. ft.'-tW, V.M., andli P. M (Night), via Kenslntilon and. Jersey City Express Lines, lure $a-00. 1 he G 4! P. JI. Llie will run duily. All othera Sundays At 7'iMi'and'll A. M , 8, 80. 6, and 6 45 V. M.and Mid Dlljnt. for llilMoi, 1 renlo'- 'c. At 7 aud 10-15 a. M..1J M.,3, f-f'. hd 6 P. M.. for Corn weli'a, Torrcidaio, HolmesburaV Tnoony, Wlsslnoinlng, UriCi .-! niK, and h r.nkloid, and a.' lu l j A. 51., lurllns tol, Behenck's. EdainKtoti, and 8 P. I. lor jUoliucsburg and Intel mediate stations. At 7 b0 A. M. ui:d 8-yo . M , for Niagara f!?H. BiifTalo, l nni irk, Caiif.ndulijua. Elinlia, Lliuca,Owen, 'toches. ter, Biuyhsinton, Oswego. Byracuse, Ureal Uend, Montrose, V ilkesbarre, Berantou, Mrotidxtnira-, WvJer ' (lap, Belvldere, Easton, Lauibertville, Fiemington, effl. - Tlie8-J0P.M Line connects direct with ti e train loav- . Itig Easton for Munch Chunk, Allentown,lSethlehem,oio. At t P- AI. for Lauibertville and Intermediate stations. Jyne.l,8tti. WILLIAM 11. U AT.M EltAKaiit. ; TjENNSyLVANIA CENTRAL RAlLRryAD. L i FALL. ARItAMih.MKNT. ika Tratna of the Pennsvivanla Central Ilatlroad h ave the Depot at Thlrts -llrst and Market streeia, which muv be reachel by the cars of the Murk cthtreet Pat tengcrRiUl- ay, as weil a by iliose of the Chcsnut and WalnutStrects l. unw iiy. Hundavs The Mnrkot Stroet oars leave Eleventh and .i.iivaiDir.i" uiuiiiivs vuioiu ixio oepjiriuro oi each J rain Munn's llai fiane Exjircss will call lor and deliver Bait-' Kneat the Dcpi.t. Orders left at the Oltlce, No. twl Cbes lint street, w ill receive ailentlon. i 'UtAiKs xkavs ii:i'oT, viz. : liny Expres at D-OOA.M. J noil Aeccnimodatfon, No. I A a, at 10 A. M. .t 11 201. M lust Line und Erie Express ailiisi xr Ph, kesburg Trai, .....V.V.M 1 !w p"m. llarnsliuig AccuamooaiioD ....at S:U) " 1 aneasler Accoinnioilatiou at 4 00 " I nbtirg and Fine Malt at Ono " I I iludeijii ia Express at ll-0il " Pittsburg and f.rie Mail leaves daily, except Buturday. Hiilitoelphlu Expiess lujiwt Oiiiiy. All other trains Oa'.ly, except Sunday. Passengers by Uay Express f o to M'illliinnpirt without cniingc ot inis.aml arrive ut l.oi k Haven at 8 10 P. m. l"BsfCiiv,cr.s by Day Fixprcss go to Carlisle and Ulmmbors LniR v ithoiit clianije ot curs. Mcepli g Car 'iieteis ean be-had on application at the 1 icket Ollice. No GUI Cliesmit street. ' TIIAIXM AllltUB at li:i-oT, viz. : f 'rclm.atl Exptess at 13-10 A. M. Pliilaileliihia Express Ht 710 puoli AccoiniiH.ilatlon.No. 1 a,at8-'.'0A.M A 7-10P M Farkesbtirg 'Irani at MA m Ln iist r '1 rain ,...at 12 IO p. M. last Line ....at 1-10 '"T F-xpiesj ., , 6.50 .. IJurrMiirKAccoiuuioUail.nl Ht 9.10 " I liihideli hiii I xincss urnves daily, except Monday. ClncniDnii Expiots arrives ally. All other trains daily, exccptBtitiuay. Pusmmera leaving Lock Haven at 7 00 A.M., and Wil l!nnnport at 8-40 A. SI., reach Philadelphia without change ol oars, Irom Wllliamsiiort, by Hay Express, at b-M t. M .JJ'li S"i,S5l.vn'" ''""road Coiapniiy-will not a sume nf.jt ,iorJi'fe'"';?,,,fxu,,pt ,,,r Wearing Apparel, and V. f in r'8t,'"''b"'iy , Ore Ilunured .Dollars In va ne. All BagtaKe exceeding that amount in value w ill be lit the rl.kol the owner, unleas takei, by sp "oiul contract. 1 or niilherinioriuatloii, apply to l'oiul tHKS ;A.l T':!kot Aft1,, No-Ohainut St. IA.MI EL H. WALLACE, 1 Icket At cm, at the Depot. An Emigrant Truln runs dailv (except Sundav). for lit 1 purtiuilari as to lure and aerouiiiiodtttlnna, apply tu ' 11IANCI8 iCNK,No.U7IiCCK Bluet. ,-I7UEI(;HT LINES EoR N KV ToRKAND X1 nil the B'litiors on the CAMDEN and AMKOY and ctiinecili g Railroads. 1NCKEA-EL DESPA I cll 1HE CAMDEN AND AM IK J If RAII.ROad' AND IRAN 8PORTA I ION t'l I.M PA N Y Fl.Eltlli r LINES hr New Yolk will leavo WaLSI'T btreet Wharf at U 0 clock P. M dnl!y (hundajs excepted). Freight must lie ihllvticu bctore 4a o'clcok, to be lor wiin.cn ihe tnme dav. ltetnriilrg.thD above lines w ill leave New York at 1 in on. and 4 and 6 P. M. Freight for'lrentop, Princeton, Kingston, New Rruns e lik, nnd all points on the Canteen and Amboy Railroad; a so, on the Jleh ldcic, HeJawaie, and Fluunngtou, the New Jorsey, the F.eehold and Jameiburg, and the lltir- ii'l-ti ii and Mount Holly Uallroa la, reculved and for- inded up to 1 P. ,M, '1 l,e Bclidtie lieUwarc Railroad connects at rhllllps buig with lite Lehigh Yal.ey KaMroad, and at Mmiiiu- 1 i.i hunk with all points on the L'Isv.ate. Lackawanna, ano Western Nallioid, forwaidlng to Syracuse, Uullalo, lid oilier points in W estfrn New York. '1 he New Jersej Rullrond connects at Ellznbsth with the f-iw Jersey Central Rtllrwad, and ut Newrk with the M-oirls i ml Essex Railroad. A a'ip meiuorantium, specifying the marks and nniuVrs, slill cr a (iidconslgnt cs, muil, In every iiisluiice, bo scut wllu ench load ol goods, or no receipt will be given. N. Ii Increased lacllltlea have been ruadu for the t'aiifi.orttttlon of live atoca. Drovers are Invited to try the rente. W hen stock ia furnished In quantities or two l urioads or more, It will be delivered at the loot of Fortieth mil. i.eur the Drove Yard, or at Piar Vn. 1. North Liver, aB ihe snippets may designate at the tluie of -liiptiiciit. For terms, or other Intel niatlnn, applv to WAIl ER FREEMAN, Freight Agent, Ko. 220 B. DELAWARE Avenue, PUlli.deipUla CrtQ ARCH KTTJEKT. GAS FIXTURES CH AN DEL1EH8, BRONZE STATUARY, Era -VANK1LK A- (,o. would renpicliuily direct Ule atteu tli.n cl their trlmcla, and tke Publin.er2.l'J .t,10U" oige and elevart Bssortuient ot 4B FIXllHkS HANDEIIEKS, and ORNAMENTAL - BROsZk WARFS. 'Jliose witbln ltaiidjoiiie and thoroughly iraile (lcod, at veiy reasonable prices will dud It to their advi-maie lolve us a call boioro pur.Lasujg else- V if rji. roiled or tarn'sl-ed flxtuies reflnfshed wlih scrcfcKars aud at rcasouabla prlcea. re4tui VAN KIRK b CO GORN E X CIIANa E B AO MANCKACTOltT. , J O H H T. BAILEY A CO., I BP.MOVKD TO I N. E. comer of market ana WATua Btre.u Pbliadalphla, DEALERS IN H AU8AND BAQOIKQ . oi every uesnilptlon, lor Gtaln, Flour, Ba t. Bupbr PIopbate ol Lime,, Bona Dual, Kio. Larve an small l UN NY BAU9 eaustautlr on baud. Also, WOOL SACK.H. Joun T. BaiLkt. Cascades. RAILROAD LINES. T? L A D I N (3 R A I L It O A 1. il.w ..... f;,,'AT inVt K IINE. -k . 'T"T-ATM'! PDIA -K, uik, INTERIOR Or i, :I!WLVAV,A- T,IK Bflll'VLKILL. BIIMIji'K i .AIA, Cl J1HHM.AND AND WVOMIN'l VAf- r'i ?21JB NORTHWEST, AND 111 II .a f. A DAS. WINIfcK ARRANCFMENT OK fASSESQER TRAINS. r.i oc oin-r s.iswi, C. 'l ii ,,,.r.Ccn,,,n a Depot, at THIRTEENTH an4 hour'sw? Btieets, Pidladelphia, at the following AI 7-10 A ti,'m.Strn "TOMMOnATION, Ro.urnini "C. tor Reaolng and il.ta. mediate 8talfona. Vlle' 6'ri'uVovt r Tamir- Lebanon,' liarrl.tiur,,. Pot'a- llagerstown, elo. eio, Z " 1 -'"'n. otl, CaiUsle. Chambersburir CeMrat Cumberland Yallev. and Hchi. vlkill and banra tmlus flir Nonhiiinherland, Wllllanuport, York. I fatimbersbtiif , Plnegrove. etc. v AF I EKNOOM EXPRESS Leavee rVlacclphla at 8 3C P. M., for Reading Potls ville, lla'rihbnrg, eto., tonnect'iig witn Keading aul Colunibia Railroad trains lor Columbia, r'C . KEADINU ACCOMMODATION Leaves Keacli.g at ll'.i A. M., stopping at all way sta- tlons, anlvligat PMIadelph a at 9 40 A M. Returning, leaves fhilaueiphla at 4 80 P.M. ; arrives In Iteaoingat7 IW P. M. Trsliia for Phlladnlphla leave llarrhhurg at fl irt A. M., yna Poitsville at 8-4o A. M , arriving in Ph.ladelpbla at ltiOP. M, Arieir.con trams leave Ilarrlsbnrg at J-10 I. 6ioPMV'"0 ' 5,45 i'' M"' rrlvln 111 I'huailelpiua at " ' IIARRISBUFO ACCOMMODATION Leaves Reading ai 7 io A. M., und ll.iriDliing at 4 10 P. M. Ccnnteting nt Resclng with Af.ernoon Acoommn dutlon south al ti ao P. M., rrivli,f In PhUadcIpHa at a 10 P. Al. Market train, with passenger ear attached, leaves Phila delphia nt PM6 noon lor Reading and all wav nation. I eaves Reading at 11-80 A.M .aud Dowiilngtowu at ItX P. M tor Philadelphia and all way stations All tbe aln ve trains lun da'ly, Bundaya exespted. Fui:daytrlnalaveP..tt.villats-OiiA. M.,nd Phlla. Ipli',!, 8 15 l'- M Lve PnilHdelpliU lor Roding at 8 00 A. M.,rtuinlng from heading at 4 llf, M. CllEalF.lt V AI LEY RAILROAD. rasjengera ir Duwnh gton and Intermediate notr ts tHethe7HOand8-.-.A. M. and 4-30 p. M. trains from Phlla li'lphla. returning from Downuigtowa at 7 t.0 A. M. and l i'.Ai I, oon. ItEW YOtK E.rRE8S FOR riTTSBCKO AND TUB WF.hT Lraves New York at "and A. M a 8 00 P.M., passing Reading at 1 1. land 11 63 A.M and 148 P. M., and con iteetlng at Harrlsbur with Pennsylvania and N'lrtltera Ccnttal ltallroad cxpiess trains lor Pittsburg, Chicago, Wf lhainsptrt, Elnina. Baltimore, etc. Heturmng, express train leaves llunliburg on an-lval of the Penns lvania exptess from Pittsburg, at 3 and 'I 0r A. M.and 015 P. M,, passing Reading at 4 40 and 10'6'i A. 51., and 11 30 P M .and arriving In New York ai 10 A M. ard ii'43 P. M. e'lciplng cars accompany those trains through between Jersey City and Pittsburg, without change. A uiall trnln for New Yo:k leaves ITarrtsbnrg at210P. ' M. Mall train for Harrlsbnrg lraves New York at VI M. SuliC YLKILL VALLEY RAILROAD. Trains leave Potnville at 7 and 1180 A. M and 7T5 P. M . returning fiomTamaiiua at 7 86 A. al. and 140 auA ' 4 15 P.M. Bl'lll YLKILL AND 6CBQCEHANNA RAILROAD. Trains leave Auburn at 7 50 a. 51. for l'lneurove and Ilairltbtirg, and 1-WP W.fbr I"'' mve &nd Iremout, re turning from DamsO; ntS-2o"p; M.,aud from Tro-jnontatT-iOA.H.j-jjft.p M. TICKETS. Through flrst-cit;?" tlykota and mlernt tleXets to alt the principal points in ti e I'. i "est and Canada 1 he following tickets aie obtainable only at the ottloe of 8 BRADl OHD, treasurer, Ne. W7 B. FoUK'lH btreet. Philadelphia, or of ti. A. NICOLLS, Gcneial Uuuerlnteud uent, Reading : COMMUTATION TICKETS. At 23 per cent, discount, between auy point desired. for families and firms. MIT FACE TICKETS. Good for 20(0 mi es between a 1 points, $52 50 eaca.for famllios ano firms SK5ASON TICKETS. For three, six, ttina, or twelve months, for holder only, to all pulLla, at reauctd rates. CLEROYMEN Residing on the line of the toaa will be furnished card entitling themselves and wives to tickets at I alf fare. EXCLUSION TICKETS From Philadelphia to principal slatl .ns, good for Satur day, Buiir'ay,ahdMoiiday,atrduccd lato, to bu had only nt u o Tkkfct olllre, at TH 1 UTEEN Til and CALLOWUILL BlTbCtS. . , FREIGHT. Goods of all (Jpfcrlptiona fiiwaidrd (o alt the ahova l,i?Xi21ll t?:omVm'm 'ISM Depot, BROAD and WILLOW Bt-eel. FREIGHT TRAINS Xeave T-lilladelpl.la dally at 6 ;i A. M , 12-43 noon, and 0 p. M ,', for Iteaoing, Lebanon, Harrltburg. 1'otta villa Tort Cluitou, aud all points lot-ward. ' MA1LB Close at the Philadelphia pott Offlee for all places cn th read atd lis branchei at 5 A. M.,and for the nrluolual tationaonly at H I P. M. i"' TjHiLADELPHIA, liEKMAfJTOVVN, AND J- AOKRIS'IOWN hAILROAD. ' On and after AVEi-N'ESD AY, May 10. ISM. FuK OEUMANTOWN. LeavcPhlltdclphia t!,7.8,,io,ll,u A.M..1 2 a-in V.;, 4. 0, 53. , B, 7, 8, J, 1(1, 11, li P.M. ' ' ' 1 Leave Cermantowii 0, 7, 8, 8 -.'0,9, 10.11. 12 A M lhea-iJ'Uiwntralii.aiidS audi. tp trains will not stop on ILeGermnutown Branch 1 ON BUN DAYS. I.eavi I'hiladclnhia 910 A. M.,2,3, n.S.lO'l P.M. Leave Ueimantown 8 A. M., 1, 4, 'f . HV P. M CHEBM T HiLL HAILROAD ' and?l P. M. 1hift C 10' 13 14 " S 3' 5 Leavo Chcsnut Hill 710 minutes, 8,8 40. 1140 A W 1-40, 8 1( , b 40. 0 40, 8-40 and 10 40 minutes P.M. ' ' ON BCNiMYS. Leave Philadelphia 9 10 mitiutos A M, 2. It. and 8P v 0-.C,e.eri!I,U7-W,Ul,,u,M A- lOJt CONBH0II0CKFN AND NOERISTOWN Leave Philadelphia fl,8 8. mlnuies, llfj A.M.. Vi ill ,6l.e.e-li.-iiiimite.t.iidli,- P.M. '' andTlM?rll,,tOWnC;!l',7,7 60'8,UA' M,'I''' 6' 'J he f& P. M. train will stop at School Lane.Wiasa, lilcton, Manayunk, hprlng Mill, and Con. hohockeu only ON BCNDAYH. Lehverhlladelphia 9 A 51 ,-.'K,4,and7JP.M. Leave Noiristovvn 7 A, M.. 1, 5j, and 1 V M FORMaNAYI NK. Leave Uil'adclphia 6, 8a.) minutes, 11 05 A.M.. Vi 4J,5J4,3.8-U5,ardlli P. M. . ' 8HpVM?lMUm'k6,7i'8!'0,9i' U-JA-M-.2. ON SrNDAY8. ' Leave Philadelphia 9 A.M.,5,-,4,and"iP.M Leave Manayunk li A. M.,l,i, and t P. jr. . B. W 1LBON, (.lencral Biiperiutemlent. Deaot NINTH Anil U1IEBN Btreet I Streets, N OltTIl PFNNSY LVANIA RAlOfiilnt: Depot. THIRD Street, nhnvn II Eor UKTnLEHEM.llOYLUMTOWN. Al A IKirr ( EASlON.Wll.LJAilSl'OKr.aild WJLKlUMBAttKB ' At 7'tO A. Al (Exnressl. l.,r n.i),ui.... Uit!rn11p,ki.,Ia,i'iL',0,,'VViiUu,.9p,,rt' '"itariS At 8U0 P J'. (Express) iur Dutulehem, Eaaton.eto reaching Earn i i H 40 p. M. olo, At 6 ! i . i o Hetblehein, Ailentown. Mauch Chunk 1 er Doj leMcv. tt at K 35 A M , 2 30 aud 416 p. M vuunK For Fort Wa:blngton at 10 A. 51. and 11 P M For Lantdaie at ti 15 P. M. .. While cars ol the Second and ThlM Bik.i. ti Pashtnuex Cars run direct lo the do) ot. ikai8 nut PHILADELPHIA. IeaveBethlelumat6"J5A.M.andl2-!!.'. Knnn ..ii.k P.M. ' w Leave Doy entown at 0-40 A.M., 315 aud 5-30 P r LeaveLaoida eatbOOA. 51 r' w' Leave Fort Washiutloit at 10"f0 A. M.. and nip w ON BI NDAY3. r'"' Philadelphia for Tlethlehem at 9 A. M. l'hlladelilila for Doy lentown at 2-;to p. M llo leslow n lor Philadelphia nt 7 20 A. M Hothlehtm for Philadelphia at 4-10 P. M Through Tickets must bo procured at the tlcknt nftlx. 'HIjiD street orlitKKB Street. ' omcea, 6'n ELLIS CLARK, Agent. 1 -piLADELPHIAAND ERIE RAIL- J.OUU.KOAlJ.-'llili great line traverses the North ern and Northwest Cotnties of Pennsylvania totheCitv ol Erie on Lake Eiie It ltus been leased aud is oueratad by the FemiB lvania Lallroiid Company. liait. ur rASHH.At.i'.it inAiasAt PHILADFLPIIf A Arrive Enstw aid-Erie JIuli Train, 7 A.M.; Erie Exoreaa Train. 1P.M. . .ne r.xpreaa Leave Wsstward Erie Mall, 9 P. M. : Frli r.n... Tnln UM. ' Passenger cars run througaon tne Erie Mall andExnresa a us both ways between Philadelphia nsd Erlo. NEW YORK CON KCTlON. tra: Leave Now York at 9 A. M r.v KH..,iJ-:i,!,j;',.' " a. i u t" Bleeping Cars on all the ulght trains. 1-or lnrnt malum rejecting p.dscrg ir business i (orner 1UIRTIE111 a.,d MiU i-l t.V! 1 Li .... ri;,. , '"I'lnreiiixikw lolkl'lOP. 5f. apply at KiA!,'?.,'V,r ',tiK'it l",,lno8- 'h Company Agon'ti, S. It. i: n'". ,."'1,,,1IJr-1rni'r Tlur-ecnth and Market streets. ffiS!',cJ."iJK..,,&0W"' E"" W1"ittm Uruwn II. H HOl'STCN.tlenfral Trelght Agent, Phtla. II. W.GW NNEU.Geni rHl'l h ki-t Agent, Phlla. A. L.TYLElt. General Blip , W llllamport. TV ilig 1 J K8T JKRSKY RAILROAD LINES," FROM 1 i. A MARKET Street l pptrFerry),conimeno MONDA Y, Ke pieuiber V4, 1NW. vimmouo- I. KAVK. Villi. A 111 I I'll! A AS Vl.linTira. For Drldgoion, taleui, Mllville, and ail InLdrionlut. Atatlcrs.BlKA M.Mail, 8 3()P.M.,Pansener For Woodttiry.H A. M , 8 :10 and 6 P. M For tape Sisv. at 8 :0 p M. KtTliRMNO 1RAIN3 LEAVE Wotlbiiry at 7'l anil 8"40 A. M.. nad 4-54 p xr llrltlge-tn at 7 t" A.M. and 8vio p M 1 reh.'h. o PaUm at 6 f 0 A. M. and 8 (,. . m l .S,!.' 'A':? ?.'? kllllvll'., at II Mi A. M n.l o w ' 'll "rl r, M. 1 IiVui. r unAiit avenue. 5, sLLAtlt.SujitrjuteuJunt. i ins train connects at beaiiinii with Kmt rusni.i. alle train for Unrrlshurg. etc, at Pout C IN TON with Calawlssa Ilni roao trains for Wiulaiushum lock Ilach. F.lmira. eto t at HARRlHHI.'RO with 1 1 ape M.y at 11-45 a. M , Passenger ar d Pre U ht I
Significant historical Pennsylvania newspapers