Intelligencer & Journal. E. W. EDITOR. FOB PRESIDENT, , JAMES toCHANAN OF PENNSYLVANIA. [Sutytct to thi decitton of a National Convtntton,) Lancßitcr, February 33,1N4N. Canal Commlaaloner. Our columns of to4ay contain several commu nications, recommending prominent Democrats to the 4th of March Convention for the offico of Canal Commissioner. Whilst we do not ourselves avow any preference, we wish our friends to understand, that our columns are open to the discussion of the merits of all the aspirants. To*Dat is the anniversary of the birth of the "Father of our Country—the immortal WASH INGTON—of whom a renowned Orator of a for eign land beautifully and truthfully said: “No clime can claim, no country can appropriate him, the boon of Providence to the human race, whose fame is eternity, whose residence creation—in whose production it does really appear as if nature was endeavoring to improve upon herself. Cjesar was merciful—Scipio was continentr Hannibal was patient—but it..was reserved for Washington to blend them all -in one, and like the lovely chief oeuvre of the Grecian artist to exhibit in one glow of associated beauty the pride of every model, the perfection of every master.” Eulogy of such a man, however, can only result in_betraying the feebleness of language, and noth ing is left us but to study his example, and endea vor to Impress on the minds of the American people, in yet -more indelible characters, the glo rious precepts, which he has bequeathed to them -as an invaluable inheritance. It is the custom of many of our Legislative bodies, on each recurring anniversary of this day, to print the “ Farewell • Address ” of President Washington, and circulate it among their constituencies. We trust that th'cse .same lawgivers will have the time and patience to read the address themselves, and lay its wise and patriotic counsels to heart. Most especially do we commend this course to the taction that daily flies in the face of its most solemn precepts. Wash ington charged us-always to speak of the Union of the'States with reverence. He most pointedly directed us to “frown indignantly upon the first . • dawning of defy attempt to alienate one portion of ■the Union from thd rest, or to enfeeble the sacred ties ' that ngtc link together its various.parts .” He directed •us to suppose a dissolution of the American Union the direst calamity that could possibly befal us. Little did that great man believe, that in so short a period after his death men would not lose without destruction. If the periodical press, with its rich treasures of intelligence and science, were struck from existence, we should then know how much we had possessed, by feeling how much we had lost.*’ Invaluable Remedies. We have no faith in quack remedies, but think it always the safest plan to apply to a regular physi cian, in all cases of indisposition. Here are some remedies, however, for very prevalent disorders, that we have no hesitation in recommending as quite infallible. Try them : For Sea Sickness — stay at home. For Drunlcenncss—drink. cold water. For Health— rise early. For Accident —keep out of danger. To Keep out of Jail— pay your debtß. To Please All — mind your business. To Mdke Money— advertise. Death of Judge Daniel.— On the 10th inst., in the city of Raleigh, the Hon. Joseph Daniel, one of the Judges of the Supreme Court of the State of North Carolina, departed this life, whilst in the midst of his judicial labors. He had been in feeble health for some time past, but was confined to his room but a week or two before his death. Judge Daniel was about seventy years old, and for more than thirty years past-has been constantly in the service of the State, either as one of the Superior Court or Supreme Court Judges. ID* A Washington correspondent of the Journal of Commerce says that John P. Hale, of New Hamp shire, sitsjupon the whig side of the' Senate. He talks on that side too, the writer might have added. Democratic meeting at Leamon Place* A meeting of Democratic citizens, favorable to the nomination of Jaxis Buchanan for the Presi dency, will be held at the public house of Mrs. Miller, (Leamon Place,) Paradise townahip, Lan caster county, on Saturday, February 26, 1848, at 1 o’clock, P. M. A general attendance of -the Democracy is requested 9 James H. Houston, John R. Miller, Joel L. Llghtnor, Jamoi H. Meaulcr, Jacob'Ayres, , William F. Baker, Gaot D. Mcllviine, Georae-Slaymaker, John F. Leiovbr, David Andorion, A. L. Henderson, L ias Beam, 1 Thai. T. MMlvalno, Wm. ( VlcCtskoy, Harman Albright, Joel L. Lefovor, James Paul, John Rodgers, «. F. Houston, Martin Shuits, Wm. Hondorson, Adam Trout, John Llndocamp, Jacob D.aHoho, > Thomas 8. Henderson, Christian Earb, Samuol Black, John Shult*, John Griffith, John B. Trout, John D. Wilson, ™ c .°l John Gallaher, Elijah H. Fraim, Robert Chamberlin, John A. Shultz, Isaac Rutter, Hiram Draucker, J. B. Baker, Andrew White, Lafayette Bak*, Elias B. Lindecamp, Joshua Chamberlin, Henry Eckert, Oliver B. Wilson, Jesse Rank, Charles Gay, . Anthony Lechler, David Russejl, Wm. McCanna, Caleb Atkins, John Johnston, John Barckley, Jno. H. Edwards, Wm. Galaher, Jacob Fiorow, Samuel Jackson, Ehrhart gchneider, [Feb’y 22, 1848. EDITORIAL BREVITIES, Appointment by the Governor.—Samuel A. Gilmoiie, of Butler, (Pa.) to be President Judge for the district composed of Fayette, Washington, and Greene counties. • 07* We are indebted to Senator Dir, of New York, for a pamphlet copy of his able speech on the war with Mexico, delivered in the Senate on the 2Gth ultimo. Washington, February IG. The President gave a dinner party to-day, which was attended by Mr. Clay and a large number of members of Congress, without distinction of party. Nearly every State in the Union was represented. That s a Fact. —A British journal, in comment ing on the recent acquisitions -of the United States on the side of Mexico, says— “ Looking to our first occupation of Eastern India, and our progress there afterwards, the less we say on the subject of the similar occupation by our American brethren of Western India the better.” U 7" The Londofi 7'imcs is displeased with Presi dent Polk's course in regard to the Mexican War. 07* Major Borland, one of the Encarnation prisoners who was captured with Maj. John P. Gaines, Capt. Cassius M. Clay and others, is talk ed of as a candidate for Congress in Arkansas. , 07* There are indications that the Democratic party of New York will unite upon Zadoc Pratt for Governor—the enterprising tanner and formerly member of Congress. He would be very likely to succeed. “A new way to pay old Debts." —One John Durgan was arrested in Boston for attempting to pay an old debt with a Harrison medal, which he alleged to an illiterate woman was a sovereign. A Vote op Thanks. —Among the toasts drank at a recent celebration in Yazoo city, (Mississippi.) was the following: By 11. C. Lewis—Christopher Columbus, the discoverer of America—very much obliged to him indeed/ Who, after this, will contend that republics' arc ungrateful ? - 07/A Kentucky-paper exultingly announces that land has lately been sold in Bourbon county for eight dollars the acre. Alas! for a ruined country! A new Presidential Candidate —John Van Buren, son of the ex-President, has been nominated by the Democrats of Erie county, .New York, as a candidate for the Presidency. i D“ There are now not less than three Johnsons in the Senate of the United States—from Maryland, Georgia, and Louisiana. Bible Agent in Mexico.— The American Bible Society have appointed the Rev. W. H. Norris, for many years resident in South America as a missionary of the Methodist Episcopal Church, to be their temporary agent in Mexico, for the purpose of ascertaining what can be done by the society for the circulation of the Spanish Bible in that country. , Mr, Norris sails in tw f o or three weeks. MATERNAL KINDNESS, i My heart grew softer as I gazed upon youthful mother, as she soothed to rest,- With a slow song, her lov’d and cherished one, The bud of promise on her gentle breast. ’Tis a sight that Angel ones above May stoop to gaze on, from the bowers of bliss, When Innocence upon the breast of Love, Is cradled in a sinful world like this. Boston Bots.-tA son was prosecuted by his father, in a Boston Court last week, for slander. The jury gave one dollar damages to the father. They ought to have given $5,000 in favor, of the public, against the father, for bringing up a son so Unnatural. - More Wit. —The following conundrum took a prize cup, at St Louis, the other day: Why was- the capture pf the city of Mexico like the novel “Ivanhoe?” Because it was Scott’s best work. Canada.: — A correspondent of the Montreal Courier deplores the condition of Canada, he asks: “ Shall we have a separation from the mother country, and become a republic? or shall ice join the United States * These are two questions upon which the country must now decide.” ID* Gen. TAYLon has written that he will not withdraw his name as a candidate for the presidency'; that the people have put him up, and they alone can put him down. Yet a whig letter writer has the impertinence to write from Washington that if Mr. Clay be nominated by the whig convention, “J have the best reason for believing that General Taylor will not permit his name to enter into the canvass 1’ ID* It is said the reason why the magnetic tele, graph will not be allowed in Russia is, that the emperor fears the introduction of such a multitude of upright poles. ID* Harris Bell, convicted at Honesdale of the murder of Mrs. Williams, has been sentenced to be hung. ID" The Telegraphic line between Philadelphia and Charleston is now complete. ID~Five hundred thousandhogs have been packed in Cincinnati during the present season. What a bristling army! ID* The total number of-tons of produce received at New York in through the New York State Canals, was 387,506. In 1846 the number of tons thus receiyed at New Y'ork was 1,107,270. It is no wonder that New York is prospering and con stantly increasing in population. ID* The Philadelphia papers announce the death of John White, Esq., President cif the Delaware Coal Company, and one of the most respected resi dents of that city. ID* The Whigs of New York, favorable to the elevation of Mr. Clay to the Presidency, have called a great mass meeting at Castle Garden on Thurs day evening next A Cracked Bell.— The Pennsylvanian says, many honest people, having heard of Bell's predic tion that the war will be voted down if submitted to the country, have come to the conclusion, that he is certainly cracked. HONORABLE SATISFACTION. When slander some loose scoundrel brings Upon your honest fame, ' Vengeance nor heals your bleeding heart, Nor clears the branded shame. But if to shoot' you down beside, He does the best he can, You’ve all the “ satisfaction” then, That’s due a gentleman 2 For the Lancaster Inielllieocer. Final Report of the State Geologist. Itgives jis pleasure to hear that the Legislature are movutg in reference to the final report of Mr* Rooebj, taj accordance with hie desire to render hie geological survey of the State complete. The aetjof assembly creating this public trust was passed the-29th of Much, 1830,and provides "for aOeologicbl and Mineralogical survey of the State." The third | section directed the State Geologist to make an annual report to bo laid boforo the Legis lature. Tho fourth requires him ultimately to de lineate the difToront geological formations on tho State maj), " and on tho completion of the survey, to oomplle a memoir of tho geology and mineralogy of the State, comprising a complete account of the loading subjoots and dlsoovorlos which have been ombraced in the survey." Several other duties were required by this and subsequent acts, such as to forniih specimens of the rocks, minerals, &c M and.detailed chemical analyses thereof. The appointment foil upon Mr. Rogers, who commenced the work at once, and continued it la* boriously til| tho let February' 1842, which is the date of the sixth and last annual report. For va rious reasons unnecessary now to recapitulate, no further field work or paid progress has been made. The Geologist and his assistants went out of office for want of further appropriation; yet he seems, con amore , to have cpmpiied with great care, his ."memoir," or final by very voluminous maps and Srafts, to make his final "memoir of the geology-a!nd mineralogy of the State" as complete and v useful as possible. All these are placed in the hands of the Executive, and the late State Geologist is-.in attendance at Harris burg on the Government, to furnish the Legislature requisite explanation; and if an appropriation be made, to superintend the printing and publication of this laborious and useful work. It is presumed that the Legislature, upon due investigation, will have but little hesitation in directing him to ceed with his final report, and granting him the requisite means. It seems due, after So large an expenditure of time and money, that the results should, as origin ally contemplated, be put in a shape to be useful. That the final publication will be eminently so, cannot well be doubted. So extended a collection of scientific facts and details of the geology and mineralogy of the State, must, when condensed and generalised into form as a whole, be eminently useful. It cannot be expected to be perfect, for geology, as a science, is comparatively young and progres sive. No doubt some deductions, hastily drawn in the reports, have been modified or discarded as erroneous, in the generalizations of the final re port. One or two very marked mistakes may be pointed out here, lest the eminent Geologist, wed ded to his original theory, inaynothave thoroughly .discovered and corrected them. One in particular, if an error, would displace " the order', succession, arrangement, and relative position of the several strata or geological formations within the State" very much. He says himself, in his first annual re port, page 4 : "The liability to commit serious errors-during the earlier steps of a geological investigation, de° voted to a country so little explored as Pennsylva nia, is obvious;" and therefore proposes " with holding the details annually collected, in order to embody them, at the termination of tho survey, in one comprehensive description of the State." Now is the time, therefore, if there be errors in the annual reports, to correct them. In his hrst report, pages 7 and 8, he calls all cast of the Cumberland valley the Southeasteni re gion, and all between the Southeastern region and the principal ridge of the Allegheny mountains, the Appalachian region of Pennsylvania. And on page 12 he savs': : "The Appalachian region, so far as it ha/been hitherto explored, is found to comprise twelve dis tinct strata or sets of rocks Dipping&somc times to the southeast and sometimes to the north west, the.se strata present numerous great undula tions, inconsequence of which some of them, more especially the lower ones, reappear often in the space between the Cumberland valley and the coal measures north-east of the Allegheny Mountains." " The lowest in position is a very thick blue lime stone,” &c. In his second annual report, paircs 1-i, 19 and 20, he adds a “sandstone formation at the base of the ■whole series,” and speaks of “the great limestone of the Kittatiny (Cumberland) valley ” as “ the next stratum in the ascending order.” And on page 15 he speaks of “ the whole thirteen formations which constitute the Appalachian region of Penn' J a/t By his second report, therefore, he makes the strata,- by adding a sandstone one as the bottom, to amount to thirteen in number. If it were so, it would af ford a curious coincidence , almost amounting to a miracle, of Nature having, a good many years pre cedent, laid down in middle Pennsylvania thirteen strata —a number just equal to the good old Thirteen United' States ! The Geologist arrived at this con clusion in his second year, and announced the dis covery and addition of one more stratum in his an nual report. • Now unfortunately for this coincidence, there is no doubt that the blue limestone spoken of in the first report, which is the same layer or stratum with the Lancaster county limestone bed, is really the lowest and consequently the oldest stratum not on ly of these valleys, but of the whole of Pennsyl vania. This is the bottom bed, and it is nowhere in Pennsylvania worn through so as to disclose its real thickness, or what lies under it. The sand stone, he calls the bottom rock, is the extension of his layer number four, which he found, in the north side of the South Mountain, placed, by the close foldings, or plications (as he calls them) of these various strata, on its edge perpendicularly; and, therefore, hastily concluded that it had protruded or forced itself through the limestone and slates on its top, from below. Whereas in fact that layer is the sandstone rock of Peters’ and other mountains, there enormously thick, extending down this way and papping all the hills around us till it thins or fines out in the north hill of Chester valley. It is now beginning to be known and recognized among Geologists that the ridges and hollows, the anticlinal and synclinal axes, the ranges of the mountainous regions and most of the inequalities of the surface, are the products of the gradual condensation or lessening of the interior or pulp of the earth, and the consequent wrinkling, folding, or crumpling of its crust, to conlorm this outer coat to the contracting size of the interior igneous liquid mass. This layer of sandstone is of course like the rest, distorted and folded by the contraction of the crust of the earth into various inclinations from a horizontal to a perpendicular position. The modus operandi of Nature in modeling the crust, seems to have been, and still probably to be, in condensing, to crumple or contract by breaking the.crust of the earth into strips, by long parallel fissures, alternately up and down, along the line of least resistance ; of course in the bottom of the ocean, where from the tendency of the interior heat to an equilibrian the crust would be thinest. The contraction would gradually fold these strips up ; which, with the effusion of mel.tcd matter by spirt ing through tfie cracks or fissures, together with the rapid accretion of sedimentary matter washed from the continents, would gradually fill up the ocean and let down the land in vast continental sheets too thick’and strong to break ; till the ocean changes place, overflowing the continents, and leaving bare the irregular crumpled bottom of the oceans, as new continents of dry land, with their ranges of mountains, and hills, formed by the fis sured strips, folded by the contracting power. In process of time this action alternates, and the ocean again and again changes place, and resumes its for mer bed, leaving behind the series of discoyered geological marks of repeated submergence, and retreat of the waters of the ocean. But to return. A conclusive proof that his sand stone is above and not below the limestone, arises from the mistake made in the third annual report, page 15,16 and 17, in which he says the sandstone in places covers the top and flanks of the'Welch Mountains in this county, and the limestone cir cling round its western end crops out, lying over and upon this sandstone. Now every body in this neighborhood knows that the Welch Mountain is not, as he says, an. anticlinal, but a synclinal axes, lying in a depression or trough of the limestone, which thus disappears all round, running under, and not cropping out upon the edge of this' ridge. In fact the slightest inspection of the borders of this Lancaster limestone valley shows the limestone bed disappearing under its hills all around, as he admits it does oa tip, nortft kide under the South Mountain or Conewago hills;'the same limestone re appearing from underthese hills into Lebanotvand Cumberland valley, V So that there can be no doubt, he has mistaken tho sandstone lying above the limestone, with its loose disintegrated portions covering. and protecting the hills and mountain., lidos, for a sandstoho protruded through (Vom be* low. All tho hills and mountains of the serioi near to the limestone aro synclinal axes or trough lying in long hollows of tho limestone bod bonoath. Tho loose sandstones brokon or crumbled iYom tho rock In place on top havo fiillon down, and cover ing tho sides of tho hilt* down to tho limestone, which dips under, are very well calculated to de ceive. As this great llmoitona bod Is found to be con tinuous in the Cumberland valley, extending (Vom beyond* Nowburg in Now York through by Easton, Reading, and Winchester in Vo., along south-west ward some fiOQ miles, it is reasonable to suppose, and geology proves tho fact, that it is equally per sistent north and south j and extends, dipping and rising away., northward under all the hills and mountains of Penna.,till it finally crops out almost in a horizontal position in Western New York. This layer is found to be the same by tracing its edge eastward from Niagara to Lockport and Ro chester, and so on east till it turns round by the Berkshire hills and ultimately meets the Newburg limestone. zi , But in giving a description of the number and layers of strata from the Blue Mountain north, a still greater error has been committed ; and one which, if not corrected in the general report and maps, will be destructive of much of their useful ness. The error is this; the Geologist found a limestone just north of the Blue Mountain on Sher man’s creek in Perry county, also south of Pine Grove, and at Schuylkill Haven, and again above Port Clinton, on the Little Schuylkill. All these places are in a range just at the foot of the north side of the Blue Mountain. Now he admits that the limestone'No. 2, of Cumberland, or Kittatiny •valley, as he calls it, dips northward under this mountain. The north side of this mountain not being so precipitous as the south side, does not dis j close its layers of rocks in place, but is covered with the earth and broken stone of the disintegra ted strata or rock formation of the mountain.' At the north foot of the mountain, thus sloping down and covered with earth, he found a limestone as J before said, appearing in many places. He hastily and erroneously concluded that the strata of the mountain did not turn up again on its northern side forming a trough or synclinal axes; but continued dipping from its south side northward, and of course that the limestone he found on its north side also i dipped to the north, and was a.layer or stratum 1 cropping out southward upon the north side of the j mountain; and therefore was a new stratum of • limestone lying geologically on top of the strata of j the North or Blue Mountain. If this were sb he | would be right, and it would be No". 6 of his thir ; teen strata. . s -Now the ascertained truth is, that this limestone bed is his No. 2 limestone, its top reappearing on the north side of the Blue Mountain, having disap peared under on the south side; just as the same bedj he admits, disappears from Lancaster county under the Conewago hills or South Mountain, and comes up again or reappears on its north side in Lebanon and Cumberland valleys, as his No. 2. This limestone bed beyond tfie North Mountain turns down quickly, dipping north and reappearing occasionally, zigzaging up and down with the strata, and forming the limestone of the valleys up to the main Allegheny Ridge. If this be the case, he has mistaken the frequent reappearance of No. 2 for a new layer a mile above, which, if it were so, would be No. 6of his series. And counting the layers clearly on top of it to the north, up to the Anthra cite coal.strata, which is at the top of all, he makes 13 layers, the Anthracite being No. 13. But it will be seen that by mistaking No. 2 on the north side for he has counted the five first over twice. To which adding his erroneous No. 1, and the conglomerate-immediately under the coal as No. 12, he arrives at the top or coal strata as No. 13. Any one can see that, this error, if persisted in through the final report and maps, will destroy much ot their genuine usefulness, ant} confuse all scientific arrangement and knowledge of the layers of rock or strata of middle Penn’a. i That this error has been made, will appear from some facts and deductions of the annual re ports themselves. For instance, the limestone of Buffalo valley near Lewisburg he calls; rightly, the old limestone layer or No. 2. When, directly across the river, running east along the north and south sides of Montour’s Ridge, are two valleys, with the limestone occasionally appearing therein, east to Bloomsburg. This limestone, although he says it crops out against the Ridge, and would, if not worn away, extend clear over, covering it up; yet it manifestly runs under Montour’s, almost ap- N pearing above ground in the anteclinal axes in its middle; showing itself at intervals all along on both sides. Now this limestone-.he calls No. 6,although the valleys run westward across the river, and come directly in contact with the limestone of Buf falo above and below Lewisburg, which limestone he calls No. 2. Again, the limestone stratum in Perry county may be traced up the valley of Sherman’s creek west to its head waters; and down Path valley, it occasionally appearing, t& Loudon ; and down round the ends of Jordan’s and Parnel’s Knobs, which are the end of the Blue Mountain, into Mcrcersburg and Chambersburg neighborhoods in Cumberland valley, the limestone of which is his Ko. 2. And yet, it will be observed, it has been traced as the same bed from Sherman’screek lime stone, his No.'6, continuously round ending in No. 2. They must, therefore, Be the same bed, the blue limestone of Cumberland valley and his No. 2. But further, the limestone in Kishacoquillas val ley he admits is the old stratum next to the bottom or Nt>. 2. Yet the limestone ridge along on the north side of Tuscarora Mountain, coming down, from Georgetown on the river, through by Pfouts’ valley, and running southwest from Lewistown, he calls No. 6. And tracing it and the layers of fossi- Hferous slate, and sandstone on Us top southwest up Aughwick’s creek, till he comes to Sydney Knob, and passes on to the west, side of Scrubb Ridge, lying west of Connellstown limestone valley, r he finds his stratification there risen to No. 9, as he supposes, and fitting directly against No. 4. For which, in page 60 of the 3d annual report, he gives the following reasons: “On the western side of that ridge” (Sydney Knob) “the formation disap pears in consequence of an enormous dislocation of 1 the strata, which commencing in this vicinity runs southward along the western part of Scrubb Ridge ” (some 20 miles long) “ tilting its strata and those of the subjacent side of the Connelstown cove, (com posing formations 3 and 2) .which it borders, into an adverted (inverted) position, and burying the rocks of our formation 5, and also the overlying formations 6, 7 and 8, so that the strata of forma .tion 4 actually lean in some places upon those of formation 9.” This is strong proof; for here again his Nos. 6 and 2 would have come together as the same stratum. But as this would confuse, perhaps bverturn, his previous theory of two limestone beds, one many thousand feet above the other, he resorts to the monstrous conclusion, that Nature to ac commodate his theory, had actually turned upside down an enormous quantity of the country, more than 20 miles long, so as to bury the upper layers and bring the under ones of the inverted mass in contact with his No. 9'. When, if he would call his No. 6 No. 2, they, the No. 2’s, would, as they do, come together exactly. This and the other instances cited are conclusive and prove beyond doubt, that there is no other great limestone stratum but No. 2, the bottom layer; that No. 2 as you advance north has been occasionally taken for No. 6, thus erroneously introducing it as a second great limestone stratum; and that he has thereby doubled the number of layers by counting them over twice. It will be seen, therefore, that there are but six strata in the anthracite region where he admits they are -the most numerous.— First, the great limestone bed at the bottom; Sec ond, the slates and shales, green, yellow and. red, from the limestone up to' the conglomerate and sandstone rock called the old carboniferous range; Third, that rock; Fourth, the redshale rock lying on its top, forming the redshale valleys round each of the three anthracite coal basins; Fifth, the hea vy conglomerate rock immediately under the coal; and Sixth), the cdti strMxr itxelf which 1. at the top of tho layers, y ; It is not intended to derogate from the great faithlhlneaa, industry, and ability, of the State Ge- Ologiat. But only, in all ftankncii, to exhibit tho nocoaaary result of a due examination of the Ikoti t and thereby endeavor to have the correction made, in the forthconSlng Final Report, without whioh, it la greatly to bo (bared, the wholo expenditure would bo worao th.iFuselcas, REFORM, PoiUerlptl Highly I|nport tint ftoin Mexico! Oh' PIiACVt Confirmed by Mexican ok, thonha ond accejileit by General Scott, HE ARK 11 OF DESPATCHES TO GOVERNMENT. Terms of the Treaty. The Baltimore Sun of yesterday morning con tains the following important intelligence from Mexico, brought by its Bony Expresses from New Orleans, in a Picayune extra of the 13th: T ired at Vera Cru * °» Sunday; last, the 6th inst., bearing despatches from General! Scott for the government at Washington. He was on ly four days from the city of Mexico. The des patches brought by Mr. Freaner 'are of the utmost importance. Hie nature of them - was not gener ally known at Vera Cruz, hut from a source in which we have abiding confidence we learn that the Mexican Congress has sent in terms of peace, which Gen. Scott has taken the responsibility of accepting. One of the articles of this arrangement is that twelve thousand United States troops shall Mei,co , until certain obligations are ful filled , the remainder of the troops to be withdrawn. We learn further that the preliminaries of the treaty of peace were signed on the first day of February by the Mexican Government, and that no doubt was entertained that the Mexican Congress, which was to meet in a few days, would ratify the same by a large majority. By the terms of this treaty we understand that the United States obtain the boundary of the Rio Grande,* New Mexico and Upper California. The pecuniary consideration for these concessions is a mere trifle compared with that proposed in the conference at.Tacubaya. Our dates by this arrival are to-'the evening of the 2d inst., from the city. 6f Mexico, and the in formation given above comes to us through so ma ny channels and in such authentieform that we see no reason to question the fact." The Washington correspondent'of the Sun states, also, that, the Treaty- has been received in Wash- For the Lancaster Intellijeneer. Canal Commissioner. THis question is beginning to occupy, very gen erally, the public'mind. The President of the Canal Board has but one more year to serve: it is therefore, important that the people should as todhe Democrat to succeed toi this important trust. Col. HENRY C. EYER, formerly a highly popular member of the. State Senate, from the 15th district—in my opinion is the proper man. Few men in Pennsylvania enjoy a more enviable reputation than Col. Eyer. His business qualifica tions are eminently great. One of the largest far mers in the interior of the State, CoioneiEyer is therefore among the. largest tax-payers in Pennsyl vania. It is proper to remark, that the farming interest of our noble State is at this time broadly connected with the financial operations of the gov ernment. It is to this great and controlling, branch of industrial operation—it is to the producing class es that Pennsylvania must now look to-redeem her plighted faith—to vindicate her honor— maintain her integrity and honest fame in the estimatitfii of the world. It is the bone and the muscle, the toil and the sweat of the laboring man that is taxed, and must continue to be taxed, to pay off the pub-' lie debt of the State. ! Is it then surprising that the agricultural and producing interest of the Common wealth are being thoroughly aroused to a sense 01 their duty, and a full determination to sustain Gov ernor SHUNK in maintaining the., credit of the State at home and abroad. The people know that the money which they pay-from their earnings, in the shape of taxes, will be legitimately applied to the liquidation of= the public liabilities. s ln this aspect of the public affairs, it is. just to conclude; that the Democrats of Pennsylvania will select the* next Commissioner from among the producing classes.; and we congratulate ourselves that a Democrat so acceptable, in all respects, as Colonel Eyer is being so extensively adopted as a'candidate a ; farmer of enlarged and practical-views, a. sound Democrat, patriotic in-feeling, and last, though not'" least, an honest man. SUSQUEHANNA. For the Intelligencer. Canal Commissioner. Amongithe. Democratic candidates for Canal Commissioner, to be nominated by the coming 4th of March Convention, no one stands so deser vedly prominent as WILLIAM BEATTY of Butler county. The writer of this communication has known. Mr. Beatty for many years asa prominent, ketive, and unwavering Democrat. He was one of the first settlers of Butler, and has filled a num ber, of responsible and honorable offices, the duties of which he has discharged with great credit to himself and much to the public satisfaction. More than 20 years ago, he represented Allegheny and Butler counties in the Legislature, and some years since represented the 24th district in Congress. For more than .10 years past, he has been an active, fearless, and energetic member of the Democratic party—and no man in Western Pennsylvania wields a greater influence, or would carry a stron ger vote. He is “ honest and capable,” and would make a worthy colleague of Judge Longstreth. A WESTERN DEMOCRAT. For the Lancaster Intelligencer. Canal Commissioner. SAMUEL HOLMAN, of Dauphin county, is in every respect a most suitable person for the office of Canal Commissioner. He is an architect and engineer, and familiar with the details both of com struction and repair of the public works. He has distinguished himself as a man of great energy and skill, by the construction of many of the finest bridges on the waters of the Susquehanna. Since the Board of Canal Commissioners became elective, he had charge for several years as super intendent of the Canal from Columbia to the Mil leretown dam on the Juniata, arid faithfully and laboriously performed the duties of that appoint ment. He is just such a man as the Democratic party desire to entrust with public affaire. His superior qualifications for Canal Commissidner, strongly recommend him to the approaching con vention. As a Democrat he has been unwavering and uncompromising. He is both “honest and ca P able -'’ CERRO GORDO. For the Intelligencer* Canal Commissioner. As the time is approaching when another can didate is to be nominated for the office of Canal Commissioner, permit me to direct the attention of the Democracy to a gentleman, whose claims chal lenge the support of every Democrat. I refer to JOHN NILL, Esq., of Franklin county. Mr. N. is a gentleman of intelligence, and of un questionable integrity. Reared in the school of Democracy, he has ever been a steadfast and con sistent supporter of its men and measures. I know of no one in the interior of the State, who has rendered more efficient service to his party. Mr. N. has held the office of Collector on the public works for several years, but declined a reappoint ment this winter, thereby proving that he not only preaches rotation in office, hut is willing to reduce it to practice. He is a thorough friend of the National and State Administrations, and would, if elected, make an efficient and faithful Commissioner If the State Convention unites on Mr. N. as the Democratic candidate, iris success, by a triumphant majority, is undoubted. , A COLUMBIAN. E7-The total number of emigrants who sailed from Liverpool m 1847, was 134,524, whdTin