41 l4l-. .mir- J . .... I.IT ... ,WT -tiiiiiiiifititrt in II ronr- o; in in n mi ir m dnniiif tn iir mo . m . ..i... ib. ! I B.L ii ,. """IM",""IMM''',',''l"nIM"jS L-i- Li " : ; . --.': ! ' . The whole art op (tovernMent consists in the art of being honest. Jenerson. i - jOL. 10, STRO UDSBURG, MONROE COUNTY, PA., THURSDAY, AUGUST 1, L850. Na:- 4' sr t Published by Theodore Schocli. TERMS Two dollars per annum in advance Two dollars aud a quarter, half yearly and if not paid before the en of the4year, Two dollars and a half. Those who receive their papers by a carrier or stage drivers employed by the proprie tor, wm oe cnargea i-a cents, per year, extra. . ixo papers aisconiinuea UnlU ail at the option of tHe Editor. i arrearages arePaai except ' ICAdvertiseraents not exceeding one square (sixteen lines) will be inserted three weeks for one dolifft.and twenty-five cents for every subsequent insertion. Th charge for one and three insertions xhe same. A liberal dcount made to yearly advertisers. IHrAll letters addressed to the Btormnst be post-paid. job pjpxiivo. Having a general assortmer' of large, elegant, plain and orna ' menial Type. Ave 'e Prepared to execute every ' description of Cards, circulars, Bill Heads, Notes Blank Receipts, I JUSTICES, LEGAL AND OTHER ; pamphlets, &c. r Printed xvith neatness and despatch, on reasonable terms , i'" AT THE OFFICE OF THE . t.f;v Jeffersonian Republican. Beautiful Lines. " The following beautiful lines, written by Benja jnih F. Niles, of Philadelphia, were -sung by two interesting daughters of Mr. Eberbach, during the removal of the pall and placing the lid permanent ly'on the coffin of General Taylor: v Hie triumphs are over, he is gone to his rest, To the throne of his Maker the home of the blest;1 How peaceful and calm he now rests on the bier, i FJach heart droops in sadness, each eye sheds a tear; ! JFhe, Hero the Statesman the journey is done, All. his cares are now o'ei; his last battle won ; . How sweetly he rests from his sorrows and fears, And leaves a proud nation in sadness and tears. Oh ! bear him full gently disturb not his rest ; j&id let the turf lightly be heaped on his breast, ,F;oroh! he was noble, and gentle, and kind; vAnd was deep in the hearts of his people enshrined, Lei the flag which he loved envelop his form, Which often streamed oer him in the battle's fierce storm ! Oh, calm let him rest with his deeds and his fame, Andjialos of glory encircle his name. , - From the Newark Daily Advertiser. Geolcsy-r-Tlie Interior Heat of Hie . Globe. In speaking of some Geological lours a few months since, we were led to make mention of the .unstratified rocks, and of their origin by cooling and solidifying from a previously healed and mel ted condition. This sounds wonderful to all and hence we now offer a concise view of the many glasses of facts which illustrate the interior heal of our planet. I. The volcanoes. These are three hundred in number, and they are situated on every side of the globe. If we take a round ball, and with a pencil mark on its outside 300 dot3, we will perceive that the bail is very thickly dotted over. So with our earth, on every side it is pierced with some of these three hundred openings, and the Jiery interior shines out most brilliantly ; often its .molten contents are expelled to the terror of thou sands of our fellowmen. This large, number of volcanoes, their huge streams of lava, and the lofty mountains they have thrown up all the interior ; heat. of our globe announce that the amount of that heat is most intense, widely diffused and ! great beyond conception. . II. Earthquakes .The cause of these are the same as the cause of volcanoes. This we know, for all their phenomena are the same. First, there are strange, alarming noises from beneath then a j quacking of the ground often risings and fallings ofithe surface, like long waves of the sea then vi- oleht rents in the solid earth then emissions of flames, vapors, smoke and melted rocks. If after few weeks all ceas.-s, and the natural calm fol- lows, ihen we say there has been ah earthquake ; but if the emission lasts a while-longer, then we call it a volcano often men are in doubt whether fo name it a short-hand -volcano or a prolonged j these other rocks have been of a burning nature earthquake. There are every conceivable grada- turning chalk into marble, sandstone into quartz, tion and intermixture among these phenomena, bituminous coal into anthracite, and slate into mi and the interior heat of our planet in some-wayjea. Their texture is crystalline such as a mol- produces bolh these classes of terrific wonders, Permanent volcanoes are indeed thickly set around the globe, but not in every district ; earthquakes, however, occur In every region, and nence tney reveal the great fact that the internal' heat of our globe is glowing beneath every spof of ground wherever we may tread. 'ill. Hot Springs. These also occur in every country on Ihe globe. They abound most among molmtains, because there the crust of the earth Kalfbeen broken and elevated, ana" a more ready escape for the internal heat has been formed. Hence in the United States they boil up most nu merously among the Alleghanles, the Ozark and Rocky Mountain. In Europe they mostly rise out of the Alps, the Pyrennees and the Appenines although there as well as here, they often spring up from level plains. It is the same in Asia, Af rica, Oceanica, and both the Americas. They are hottest when vplearioes are most active some times reaching the boiling point, though in all ca ses they must be greatly cooled by the waters and the rocks near tha surface. The great numbers : of these springs, and their universal diffusion, j orova a1n i hp. hnrvarsalitv of the internal heat of, - i ouriglobe. 'Artesian Wells. These have,been bored iaUlmoflt every country to 'the depth of many hun- drSsffcet'for obtaining Sbpious stream. They are'DUta few inches ;pide, tndja tube lei al) the way down to prevent jth Iateralescap .of tb wa ter. (This water which boifgjip).alway8 warm.) At Wurtenburg in Germany, they .ar'c u&e3 to warm the wattr which drives factories, an this prevents 1 1 tneir stopping by ice in winter. The same is the case in Alsace and Stutgardt. In China they are not Uncommon: And .every where the deeper ihey are sunk, the warmer is the water they bring up, and they furnish an additional proof of the u niversality of the interior heat of our palnet. V. Deep Mines. After descending about 40 feet the temperature of the earth remains the same both in summer and winter, below that depth it be comes warmer as we descend. This increase of heat downwardly advances with perfect regularity a little faster in some places, and a little slower In others, but in all, without any exception, there is an unvarying advance. On an average around the globe this increase is one, degree of Fahren heit for every 50 feet in depth. At the bottom of the mines in Cornwall, the thermometer stands 88 degrees this is 1200 feet below the surface and much warmer than summer weather there. We can conceive of nothing calculated to stop this ad vance of heat in the direction towards the centre of the earth, and if it continues to increase accord ing to the ascertained -average rate, then all known substances must be in a melted condition 20 miles below the surfaced At this rate we must cease wondering at the numerous earthquakes and volcanoes, for the crust of the earth must be a shell resting on a molten flood ! Earthly materi als are non-conductors, and therefore this internal heat cannot escape, or affect us at the surfaces. In the same manner streams and pools of lava become cooled and hardened on the surface, and thus their heat is confined, and their interiors after remain many years in a fluid stale. VI. Fossil Remains of Plants and Animals. These remains show that tropical plants and ani mals in former geological eras flurished in the! Polar regions. The ivory of the elephant is dug up, and furnishes an important branch of industry on the extteme Northern shores of Siberia, and delicate corals of the present warm and mild o ceaus, displayed their glories during former peri ods in what is now ice-bound regions of the Arc tic 'one. Thousands of facts like these from ev ery department of animated nature, proclaim a for mer high temperature in all high Northern latti tudes, and this uprated temperature can be ac counted for in no other way than from the influ ences of the internal heat of the earth. It has cooled gradually by radiation to its present slate, and further sensible cooling is prevented by the non-conducting crust in which it is enveloped. VIT. Extinct Volcanoes. These by far out number the present active ones. In North Amer ica along the whole line of the Rocky Mountains, and through the West Indies, they stand thickly ! as monuments of the past. Their craters are sym metrically formed, and they exhibit the same lava streams, though in a hardened slate, as those now burning. In Germany along the Rhine, travellers speak of "the castled crag of Drachenfels," the Eipel, and many others presenting the same phe nomena. The centre of France is studded with them, especially about Clermont. Tn Italy the town of Cumea founded a thousand years before the Christian era, is built in the centre of an ex- tinct volcano. There is a space of 60 miles in' , , . . lc"Bl" a"u "f. aijr auuu craters, one of which is two miles in diameter. All these with others in every quarter of the world, should be joined with the 300 that are now burn ing, if we wish to have the full proof of the fiery wonders in the interior of our globe. VIII. Igneous Bocks. By these are meant all rocks that are not stratified, such as the granite, sienite and trap. They exist . abundantly the granite as we have before remarked forming the gieat foundation rock around the whole globe ! The evidence that they have all had their origin from a liquid fire, are complete. Their position is beneath, or rising from beneath, the very region of intense heat. Their shape shows a former liquid condition having been ejected in veins, cracks and crevices of other rocks. Their effects on ten liquid naturally assumes in solidifying, Their composition is identified with that which now streams from volcanoes such as felspar, horn- blend ana silica, me transition is graauai ana perfect from modern lavas into all the varieties of igneous rocks. And artificial experiments have shown that these igneous rocks when melted by great heat in furnaces, assumes on cooling in the open air the same characteristics as lava, and it is known that cooling under great pressure as in a volcanic cone, and afterwards rent by earthquale forcesand exposed to view presents the exact form of trap. This latter fact is eshibitod on a grand scale at Mount JEtna in the Val del Boye. Here then we have a grand, and magnificent evi dence of the interior heat of the globe the igne ous rocks, entirely belting around pur planet, form ing the foundation pf the earth, rising into lofty mountain peaks and mountain chains, and yet all having their birth from a former melted condition. In this truth all geologists areagreed and confirmed. The southern shores of that peninsular presents . t ;t r I -f Mi: similar appearances uotn oi, rising arm oi lamng. Ancient temples standing on the shore have been so far let down that the tops of lofty columns now rise only a few feet above the water. This has happened in the Bay of Baice, both to the temple Lof Neptune, and the temple of the Nymphs. The temple of Jupiter Serapis; on the coast of JN aples was gradually lowri down Vneath the waves, sd shell &sk attached Mky 9Sh gorgeoi rfelt ijjlaranyagam .that sa temple Wh W adjoining coast has sep so fen tly raistd up that marble pillars 'are still standing and the remains of the shell fish still attached, are now elevated thirty feet above the level ol the sea. In South America the coast of Chili for distances of a hundred miles, has been seen to spring up suddenly with tremendous commotion both of the land and of the ocean. Harbors have been destroy ed, the soundings rendred shallower, and a3 a proof that the interior of the country rose still higher, the streams and brooks showed an in creased descent, and more violent rapids. The most noted of the upheavals occurred so lately as in the years 1833, '35 and 37. Another class of proof of these risings and de pressions, occurs in mines. The strata are bro ken by a smooth crack, and on one side of this cleft they are sometimes raised up or settled down many feet, so that the beds of ore or coal come to a sudden stop, and the miners with much difficul ty are obliged to reach upward and downward to find their continuations. A still more stupendous class of evidences are presented by both continents and all large islands ; for without exception they have all-been repeat edly submerged beneath the ocean. And as the ocean cannot rise up above its universal level, the continents must bodily have been lowered down. And these astonishing undulations, both of rising and falling, bespeak a fluid interior a heavy flu id of molten rock on which the hardened surface may float, and admit of being elevated and de pressed. This external hardened shell would be too large from time, as the interior cooled and contracted, and hence like anaich, it would press latterally against itself, rise up into mountains, sink down into valleys and ocean beds, and be come fractured : for with' so flat and thin an arch it would not bear its weight. X. The Specific Gravity of the Earth. By as tronomy the earth can be weighed, and its density ascertained. And its known density is not so great as the presure of its materials resting one upon another would naturally produce if these materials were at the ordinary surface temperature. This deficiency, of natural density is so enormous that it bespeaks the continued operation of a great and general cause a cause co-extensive with the whole interior of the globe; and the only adequate cause of which we have the best knowledge is this interior heat. Heat expands all bodies and makes them lighter in proportion to their bulk. XI. The Shape of the Globe. This is nearly round : it is some what depressed at the poles, and raised up about the equator precisely in the form which a fluid receives when whirled around. It is the shape the present ocean takes having its polic diameter 26 miles shorter than its equation al diameter. And this peculiar form of the pre sent solid parts of our globe, indicates a former state of fluidity a fluid caused by natural interior heat. XII. The Nebular Theory of the Solar Sys tem. This theory rests for its foundation not up on nebular appearances properly so called, for these by glasses may be resolved into1 stars, but upon a multilude of facts in the constitution of the solar system. The solar system is a single piece of mechanism. Any one of its parts is incomplete alone. It must be regarded as a unit. A single Intelligencer, with one most simple design, has called it into, being, and that by natural means. Its whole structure corresponds with the nebular theory of its origin. None other is conceivable. Pucn a ieoryjs enureiy conservam wim au wie known laws of matter: there is' not a single juc c i .1 11 .1 not a single difficulty. The facts in ils favor can- nol be given here they would occupy at least a column, and ihey, in order to be distinct, should stand alone. Moreover the natural condition of matter as we chiefly behold it is fiery condition The sun we must regard as a great ignited mass so also the fixed stars. Some of the fixed stars go oul they loose their brightness and shine no more, like our earth. The mighty changes going on among them should prepare us for our present argument, uur sun, too, nas occasional spots probably of solid material floating on its surface. Some of them are 30,000 miles in diameter, and occasionally they split and break into fragments like a piece of ice. borne pnilosophers supposed ( that they were openings, in a shining envelope through which the dark body of an obaque sun is seen. Such openings might close up from the sides, but could not present appearance of a split ting breaking solid. Thus while astronpmy teaches us that our earth is a planet, and shines with reflected light like Ju piter and Venus, geology by her doctrines of in terior heat, leads us to suppose that it once shone by its own native lustre, was a burning, glowing glittering star. t). Amusements iii Congress. The latest and. most fashionable amusement among the grave and revered members of the House "of Representatives is wafer snapping! The wafers used by Uncle Sam are white, and about the size of a quarter, and every desk is abundantly supplied with them. Held horizontally between the thumb and finger of the left' hand, and skilfully snapped by the right, they sail gracefully through the air, describing all, sorts of parabolic curves un til they come in contact with the eye, nose, cheek or forehead, for which fate had predestined them. To stand behind the bar of the House and look over the heads of members during a dull speech or a manoeuvre, the wafers flying in all directions look like ah inverted snow-storm, with the flakes going up instead of down. Several of the more dignified members, whose probosces are uncere moniously greeted by these wandering missiles, have loudlv arid angrily protested against this Un dignified and childish amusement; but the big boys only laugh and snap their wafers in their faces the more industriously. This new species of national amusement is ra ther costly not so much on account' of the ex pense of the wafers, though that is some; but prin cipally because of the high, price paid forthe time of Congressmen at Wasbingtpn. Hbweyer,"when the great men of' the nation are-engaged in snap ping wafers,1 they are likely doing no other mis chief.. () You may cure galls in- horses with perfect ease, by the use pf wh'itfe , There is at p$&jfi tree in Berks cpunty Pa., upVardV of one hujjo'.red years old. It still bears fruit. i : i .... . : : : . Wonderful Case. In ihe July number of the American Journal of Medical Sciences, we find a full accnunt of one of the marvellous surgical cases cases of tremendpus injury to the moat vital organ, fol lowed by unexpected recovery and restoration to perfect'heahh which every one feels' to be so incredible per se a. to require the most ab solute and overwhelming proof in every partic ular before yielding belief. "The times have been That, when the brains were out the man would die." By and by, we shall begin to believe it pos sible for a man to live, and be wise and witty too, without any brains at all ; a notion that seems to be somewhat of a growing one in Con gress and in some parts of the South, where it j is quite evident that the emptiest heads are get ting uppermost and carrying off all the honors of disunion and disloyalty. The case we allude to which occurred in New England nearly two years ago, and was then one of the nine day's wonders of the press was that of a man who, by a premature explo sion while blasting rocks, had a largo bar of iron driven through his head clear thr.ougb, traversing face and bram without being killed on the epot, or indeed, seeming to be very un usually harmed thereby. The Journal has a full, complete, and' authentic history of the case from the time when it occurred on the 13th of September, 1848, up to January of the present year, when the patient visited Boston, and was examined by various medical bodies and dis tinguished practiiiouers, including Dr. Henry J Bidgelow, Professor of Surgery in .Harvard University, by whom the description is contri buted to the Journal. The paper includes the official statements of Dr. Edward H. Willaims, of Northfield, Vermont, who first saw the pa tient, and Dr. J. M. Harlow, of Cavendish, who attended him throughout the whole case ; as well as certificates from Joseph Adams, a Justice of the Peace, and the Rev. Joseph Freeman, who were witnesses personally con versant with the facts. It is altogether so ama zing a case, so perfectly authenticated in all particulars, and of an interest so far above all mere technical or professional interest, that we thhink we cannot do beflHthan condense its leading features for the gratification of our rea ders. The sufferer in the case, Phineas P. Gage, a young man of twenty-five, "shrewd and in telligent," a contractor or head workman on the Rutland and Burlington Railroad, bad char ged with gunpowder a hole drilled in the rock, and directed his assistant to fill in the sand ; supposing which done, he dropped his tamping iron into the hole to drive the sand home. It happened, however through some inadvertence, that the sand had not been poured in ; and the iron striking fire upon the rock:, the powder was Inflamed and the accident produced by the iron being blown out like a ramrod shot from a gun. The tamping iron was a round rod three feel seven inches in length, and an inch and a quarter in diameter, tapering to a point at the top, and weighing thirteen and a quarter pounds. The whole of this immense weight and lenth this bar or bludgeon of iron was drivm, through Gage's face and brain, as "he stoopTd over the hole, in the act of tamping the sand. It struck him on the left cheek just be hind and below the mouth, ascended into the brain behind the left eye, passed from the skull, which it shattered and raised, "like an inverted funnel," for a distance of about two inches in every direction around the wound, flew through the air, and was picked up by the workmen, "covered with blood and brains, several rods behind where he stood. Gage, who was also more Or lessscorched, was prostrated, apparently less by the blow of the iron thane force of the explosion. He fell on bis back, gave a few con vulsive twitches of the extremities, but "spoke in a few minutes." His men placed him in an ox cart, in which he rode three quarters of a mile to his lodging, sitting erect ; got out of the cart himself, and with but little assistance ; walked to the piazza and afterwards up stairs, talking rationally to 'tne physicians and giving them a clearer account of ihe accident than his fiiends could ; occasionally vomiting up blood, the effort of which caused haemorrhage from the wound, with the actual loss of a considera ble portion the substance of the brain. The left eye was dull and glassy, but was sensible to the impression of light. Gage bore his suf ferings with heroic fortitude, telling Dr. Wil liams, "here is business enough for you," and expressing to Dr. Harlow the hope that " he was not much hurt." Of course, it forma no pari of our intention to giro a detailed account of the treatment and management of the case, which was not varied. by any circumstances of interest to persons not of the medical profession. We merely note, generally, that, for the first ten days, eve ry thing went on well, Gage being, with some inierrals of natural delirium from fever, pretty rational and hopeful; thai, at the close ofthu period, he lost tho sight of the left eye, and lay for a fortnight in a 8emicomatose"siaie, or par tial stupor ; that he then began to improve in body and mind ; was, within two months, walk ing about in the street, in defiance of instruc tions : suffered a relapse in conseqnence ; ana finally, being reentered from this, was, in the tenth week, free from pain and rapidly conva lescing. The leading feature of this case," says Prof. Biffttlnw, Hs its improbability A phy- siciap who holds in his hands a crowbar, three feet anxLa half long, and more than thirteen lbs. in wSBrt. will not readily believe it has bean djiven with a crash through the brain of a man who is still able to walk off, talking with com posure and equanimity of lha hola in his head." Prof. Bj, who justly describes tha case as one t perhaps unparalled in the annals of Kurgery,3' says that he was "at first Wholly skeptical," but that he was personally convinced Mr. Gage, as we said, visited Boston in January, and was for some lime under the Professor observation, who had hU head hhaved;antl a cast taken 4 which, with the tamping ironj is now deposited in the Museum of the Massachusetts Medical College. At that time, the wounds were perfectly healed, the only vestiges of the accident being blindness and an unnatural prominence of tho left eye, 'with paralysis of the lids a scar on the cheek, and another on the Skull showing the irregular elevation of a piece of bone "about the size of ihb palm of tho hand," and, behind it, an irregular and deep hollaw several inches in length, beneath which the pulsations of the brain were perceptible. "Taking all the circumstances into considera tion," says Ifrof. Bigelow, "it may be doubled whether the present is not the most remarkable history of injury to the brain which has ever been recorded." This is unquestionably true ; but considering the little real injury caused by the passage of a tamping iron through Mr. Gage's head, the wonder is that a pistol bullet a buck-shot; or even a little needle can do so much executfon on the heads of oiherpeo ple. North American. Human Equality. Rothschild with all his wealth is forced to content himself with the same sky as trie poor newspaper writer, and the greater banker can not order a ptivate sunset or add one ray to the magnificence of the night. The same air swells all lungs. The same kind of blood fills all veins. Each one possesses, really, only his own thoughts and -his own senses. Soul and body these are the only property which a man owns. All that is valuable in this world is to be had for nothing. Genius, beauty, and love are not bought and sold. You may buy a rich bracelet, but not a well-turned arm on which to wear it a pearl necklace, but not a pearly throat with which it shall vie. The rich est banker on earth would vainly offer a for tune to be able to write a verse like Byron. One comes into the world naked and goes out naked. The diffence in the fineness of a bhofj, linen lor a shroud is not much. Tlie Bird and the Snake. The Mobile Herald relates the following : Two gentlemen of our acquaintance, of .unim peachable veracity, witnessed a scene, the oth er day, worth recording. They observed, at a distance of some thirty feet from them, very strange and unaccountable conduct on the' pari of a bird, commonly called the "cow bird," re sembling in color and shape the mocking bird of this region, though somewhat smaller. On watching it narrowly, they discovered that it was engaged in a conflict with a snake soma 18 or 20 inches in length. In a few moments the bird was victorious. It suddenly caught the snake by the head, and, flying with it to an old pine tree, succeeded, after a hard stuggle, in fastening it to a pointed splinter, Thus pin ioned, the snake was entirely helpless. The bird watched it for a moment with apparently the utmost complacency, and then continued its repast, devouring within ten or fifteen minutes three-fourths of the snake. Assessment of School Tax. The annexed letter from the Chief Clerk of the State Department of Common Schools in regard to the propper mode of assessing School taxes, may be of service to the School Direc tors in the different School districts. It was written in reply to one asking for the official construction of the law on this subject. We And it in the Reading Journal. Secretary's Office, Dep't of Common Schools, Harrisburg, May 27, 1S50. John S. Richards, Esq. Sir: Your let ter of the 25th instant, enquiring what i the proper construction of the 24th section of tho act relating to Common Schools, passed 7th of April, 1839,80 far as the assessment of School taxes is concerned is now before mo. Although there is some ambiguity in the section alluded to, yet a careful examination of its language and the terms used, will lead to the result in tended by the legislature. In levying the tax, it is the duly of the board of directors in the first place, to assess upon all offices and posts of profit, professions, trades, and occupations, upon all single freeman above the age of twenty-one years, who do not follow any occupation.AXY sum which they might deem proper and sufficient not exceeding tho amount as sessed on the same for State and county pur poses ; except, that the sum assessed on each, (office or post of profit, profession, trade, occu pation, and stngie freeman) shall in no case be less than fifty cents. Hating done this, they should in the seconS place ascertain the balance of tax to be raised, and apportitfn.it upon the property of thorfis trict made taxable for State and county purpo ses. Farming is not deemed an occupation, as contemplated in the'School Law. .yf Under the foregoing provisions, persons hold ding office, &c, may be assessed more ihH fifty cents, but never less. The properly is liable to be assesed with the other property of the district, for the balance pf tax to be raised, after the first assessment shall have been com pleted. In the foregoing, I have emphasised those terms considered most aigificant in the section, for the purpose pf leading the mind to a more clear appreciation of their importance. . Ve'ry Respectfully Yours, &c., for the Su perintendent! 4 FRED. J- FNN, Chief Clerk! '5 A Western editor announces that his better half, had the previous day presented him with u a twelfth little fa.sponsibilityVl and immediately low makes the fgiiowinf appeal, whichtve hope, was duly responded lo : " More subscriber want ed at this office."