ax THE CORVALLIS GAZETTE, FRIDAY, OCTOBBER 27, 1893. The GAZETTE. Israed Every Friday Horning by : SUBSCRIPTION RATES: ' Per Tear,. T. . .' . . Six Months, Three Month, Single Copiee, Per Year, (when not paid in advance),.. . $2 00 1 00 75 05 . 2 50 Entered at the Port Office at CorralUs, Oiegon. as second ahus matter. RIGHT OR WRONG. Complaint is made by visiting sportsmen concerning the strin gency of the game tresspass laws of Oregon and the question pre sents itself: Which is the best? Shall every Tom, Dick and Harry, no matter from whence they come, be permitted to ride at will and without restriction over the pos sessions of our farmers and ranch ers and the birds and other wild game thereon be watonly slaugh tered, etc., or shall those whose interests are dependent upon the resources of their various farms be protected as the language of the law prescribes? We are not sitting in judgment, but ask that if the law is right should it not be sustained? . If wrong, repeal it. THB LAW. Section 1. It shall be unlawful for any person, other than an officer on lawful business, being armed with a gun, pistol or other firearm, to go or tresspass upon any inclosed premises or lands without the con sent' of the owner or possessor thereof. , Section 2. It shall be unlawful for any person to shoot upon or from the public highways.. Section 3. It shall be unlawful far any person, being armed with a gun or other firearm, to cause, permit or suffer any dog, accompanying such person, to go or enter nnon anv enclosed premises without the consent of the owner or possessor thereof; provided that this section shall not apply to dogs in pursuit of deer or varmints. Section 4. Any persons violating the provisions of this act shall be deemed guilty of a misdemeanor, and upon ' conviction thereof shall be punished by a fine not less than 15 nor more than $50, and in default of the payment of the fine imposed shall be committed to tbe county jail ot tne county in which the offense is committed, one day for every S2 of the said fine. Section 5. Justices of the peace for the proper county shall have jurisdiction of the trial of offenses herein denned., , We furnish our readers the re port of W. T. i Branch, the bank expert, who completed his labors in connetion with the examina tion of ; records in the. Hamilton, Job fc Co. banking institution of this city. The report was given to an advisory committe composed wholly t of interested depositors, by. whom it was unanimously adopted, ' The report shows that there were no- evidences of fraud td be found within the archives of the bank, and the only cause for criticism was the loose manner in which the Job brothers conducted their affairs'. From this report we glean . the ? opi nion . that there was no - intention of wrong do ing on the part or the brothers and that their failure was due wholly ; to. the stringency of the money market and to mismanage ment. , i . Ex-Speaker Thps. B, Reed spoke to"a large audience in Cleveland, Ohio, for ' nearly an 'hour, Monday of last wefc ' . He declared that the democratic .. party succeeded . in bringing about the closing of fac tories and mills,, something . they could hot do WHKifhe senate. The senate, lie Baid, is elected to gov ern the people, yet' it could only give the' people a test of. physical endurance, the . greatest - thing it has done ' being to remain ' in ses sion for thirty-nine, hours. ; I,,. .', '.,' .. ,i i m i i i i ; Here is the approach toward a two-minute gait ; daring twenty years) 1874,' Goldsmith Maid l:15j 1883, Jay-Eye-See, 2:10; Maud S., 2:08$ 1891, Sunol,' '2:08; 1892, Nancy Hanks, ' 204..;, This latter time has not r. been equaled thus fary-but there is no doubt but that, a twb-minute gai(will ,be' realized before many seasons have elapsed. Under the tree trade party's idea of newi'tariff ithal price of sugar will be increased 25 or SO per cent., also their tea and coffee. This ;! stddition, to the', household expenses, ' coming - at. the same time as a reduction in wages of 10 of 5 perj- cenitj will be sorely feltvj; li : ( i 0:V I'! !. 'i The -Choctaw' Indians should now be .ponsidered th,6rouglily civ ilized, k their j treasurer i having "skipped," ' leaving a1'. Shortage of something like $100,000.. ; Consid ering the amount he had to handle no Chifeago New Xork or Seattle man could ' baye1,; made a " heavier haul.' -. ' .-. .. ': ; SatS the' New : York : Recorder 'The democratic party has. been in full control of the government for' nearly - eignt months. ;' What has it ' done? - Nothing. . What, is it going to do? - Nobody knows. It doesn't know itself. ' What does it propose to do? '- "Nothing. The federal election laws never put a dishonest Vote' n a ballot box, arid never kepi an honest one out --Is that why the south and Tammany 'want them repealed? ' Free soup houses .will run on fall time when we get free trade, says an exchange. THE OLDER COAST RANGES. With More Recent Geological Formations in Benton County. BY JOHN RAY. . Continued from Last Week. REVIBW. We have tried in the above to give a faithful description of the rocks as we have seen them. A few further points may j be suggested. Taking the Vine yard-Kings Valley ranges, they stand quite apart from more recent formations. An excellent example is found in the Osburn hill, where, standing alone, its base runs sweeping out as the oak, where it sinks under the base of a low Eocene hill. It is, too, at this junction of the older and more recent formations where so much igneous action has taken place. Where it runs entirely around the oldest system, up the flanks considerably, and also where recent formations are some what contiguous, they.have met the same fate. How near the Miocene comes to the older formation we do not know exactly, but from Summit to Yaquina there is comparatively little igneous action visible. There is a dike going up to Rock Creek, thereiisjanother at Pio neer, a little horizontal intrusion in the shales about Porter's, but as compared with the older formations it is as nothing. Then, again, its schistose trap taken from those places bear no resemblance to simi lar material east It is like its hills, very common. .. There is, too, every reason to believe that the metamorphism, such as it is, in the Kings Valley field.took place prior to the igneous operations subsequent to the rise of the Eocene deposits. Where this action has taken place it has been violent, but the quiet and easy change in the flags and shales of the older rocks does not exhibit this violence. Then again, with the exception of the little strata remaining upon the flanks of the older hills, they seem to be a solid body of metamorphic rock, and further, that the material with which this strata at the base is composed, is from the debris of the older strata above, breccia, flag and shale show this in a new arrangement of older material, andin the coarseness of grain not found in more recent or distant deposits. Another feature in the Kings Valley field is when the sediment composing the strata at the base of the hill was deposited it must have been in fresh water, for there is no sign of marine life. There is a leaf or two and creeping things have left portions of their bodies, birds and small animals their footprints upon the soft shale. The more curious too, it is, when we remember the west face . stands overlooking the . Pacific Ocean. But when we look at the deposits of the Eocene as well as Miocene which have been laid down, and largely, from this older land, we may try to imagine if we can the former greatness of this formation and the great change which must have taken place, but all we can now find or see is the skeleton of what was. . At the - Vineyard field, things seem more natural and with the opening .in the range previously mentioned the sea could sweep in,' up and down the valley, the bed of marl depositedand molus- cari life in highest enjoyment in the shelter there existing. ' " ' In a bulletin published by the Geolog ical survey, Washington, 1886, "Notes on the Geology of Northern California," by L S. Diller, who says, "The distribution of the rocks of the Chico group clearly indicates that during, the Chico epoch the northwestern portion of California, with the adjacent part ' of Oregon, ' em bracing the Trinity, Salmon, Scott, Sis kiyou and other mountain ranges; of the Coast Range, was a large island, sepa rated from the still larger continental land mass of the ' same "strata in the Great Basin and Sierra region by a wide strait now bridged over by the Lassen's Peak , volcanic ridge;" and ' again, "South of the Rogue, river ; valley the cretacean island lay completely west . of the position now occupied by the Cas cade Range. To the northward its ex tension is but partially knbwn.y,-- The heavy body of black clay men tioned on the Foster place is just such material as is found in the marsh land by Toledo' The fossil wood and Terredos with Corbiculas just obove and the fossil ostreai in the higher sandy clay stone show the estuarine conditions. , Higher in the formation a Zirphaia was obtained with other fossils unlike those found near Corvallis. ' Wil h a condition such as we have here,, viz. brackish water .land must have been to the west of it to furnish fresh water sufficient to modify' the briny water from the .ocean. Giving us this barrier , to . the ocean, the older' Coast Ranges, this condition is met and cannot be met otherwise, for up to this time the Miocene uplift had nottaken place.- :l , , Another problem also seems - to be solved, namely; why or how it is that at a . distance . of ten miles ;or more from Corvallis, strata of a lower: horizon is found? The opening in, the old 'Coast Range at Philomath permitting the tidal waters of the ocean to come in, we find right east of this Scott's hill, in the path of the channel, heavy bedded sand stones over 200 feet deep below the level of the .. valley... Even i in grain though alternating in shade. ' This is not the condition in Estriary waters, but rather thin bedded strata with fragments of leaves and wood, ' the . stone' partaking more of clay than ,f sand, and ' that,' in our lease, the, thin , .bedded ' andclayey strata were laid down ' previous ' to the heavier bedded sandstones.' ' '" ' E The Red Deposits. ' Much curiosity has been - manifested from time to time as to these deposits, particularly so as they are found so near the surface and nothing resembling them in or about the same to give cause for their being there. Mention has been made of the residual clay at Vineyard's which is the decomposed metamorphic rock containing hornblende or pyrox ene. These minerals containing iron give or stain the clay red or chocolate brown, which is the color of the clay, on the upper portion of the hill. According to eminent authority this disintegration has taken long time to effect Then taking into consideration the Hematite pebbles in the conglomerate, besides which a large body of brick-red crystal line Siderite is found in this formation. It will not be difficult to imagine that in the course of time a body of such de composed material lay on the hill side and was swept off by heavy rains. Age of Older Formation. In naming tbe strata of a formation or period the science of geology exacts evi dence of animal or vegetable life exist ing during the formation of such strata, in the shape of fossils. These, un fortunately, we have not in a shape or condition suitable for use in this way; the reason for this will be seen when looking at a situation which existed and which almost obliterated everything of this kind. It is true we have a few frag ments, but many fragments may not make one fossil, no more than one com plete fossil would be sufficient to deter mine the age of a formation. In this emergency we turn to Mr. Becker, who, while not approving of age determination by the appearance of rocks, suggests "In California great use can be made of re semblance." This suggestion is forced through the difficulties'.encountered in the similarity in .the California forma tions and the lack of fossils such as we meet here. But he further maintains "So far as is known, therefore, no beds in the Coast ranges of California younger than the Knoxville group have experi enced the peculiar magnesian and sili cious metamorphosim so characteristic of these ranges. Besides the resemblance in metamor phic rock another similarity exists be tween the older Tertiary and Cretaceous formations in California and our own. In California the strata of these groups lay in and east of the older Coast Ranges. This is precisely as we find it here, and so, no doubt it runs in this manner wherever found, fromCalifornia to Can ada. - Therefore, with the exception of the Breccia at Vineyard's, the strata at Kings Valley showjtheyare composed of the older material above them. We have a piece of dolomite attached to the Resi dual clay.similar to what isin the grits and conglomerates at King's Valley, and that this strata has againjbeen broken up into small fragments which have made up the next loweststrata in the Valley, which, as found, is"of spotsjof two shades of green, yellow, brown, light drab and white, with brilliant green sand occasion ally. This material is'too large to have been long in the water, or had much sco urine before tbeine deposited. We have, then, with our fragments of fossils our more perfect fossils of recent Cre taceous Eocene ,t and Miocene forma tions, the metamorphic jwith dolomitS at tached with other material showing a close relationship to the latter. With these we have every reason, to believe that the geological formations in this county are not much .different to the Older Coast Ranges of California, as well as the Chico-Tejon in close proximity thereto, and that these older Ranges will doubtless be where Mr. Becker places them, between Jurassic and Cretaceous. It is not to be understood that the geo logical formations given in this paper are confined to Benton county, for, while the writer has not visited other counties in the Valley, fossils sent to him from Polk county (south of Independence) are un doubtedly more Cretaceous than any yet found in Benton. But our object was and has been to rescue, if possible, these grand Ranges from the pretentious but rickety elevations of Miocene time.. To restore the title belonging to them which has been ruthlessly given to their less deserv ing neighbors. .How he may have suc ceeded those learned in the science of geology will best be able to determine, but he is conscious of this, that the opin ions . : formed have not been : hastily adopted, but the result of extended ex aminations and study. If our object has been accomplished the knoweledge of which will be a sufficient reward. , . 9HB:OX,A.CXAXf DMM. , Another feature of geological in terest ' in this part of the Willamette Valley . is the many, large, blocks., or boulders- found scattered here and there in the valley, but more generally near the base of the hills west of the river. These rocks are of foreign origin,"and so far as known to the writer, but little attention has been given them publicly. " They are also mementoes of the glacial period monuments marking the stranding, or wreck of the -"vehicle ' ' which con veyed' them during the movement' of the. prift, Then, ' oo, with .other mate rial brought and deposited 'during this period,1 of the leveling and smoothing and .the changes' wrought, was , of the greatest utility to Agriculture, and to ward the fame this valley has obtained. It is' then of these tramp rocks and other deposits at the time, we give a brief de scription, aided by observations in other fields in days agbne. ' t ' . ' ' ' ...Drift Material. In the great fields- of drift material covering the larger portion of Northern United- States there will naturally, be some diverdty in 'the"material: of those fields, first, through distance from native bed to final depositand second, distance longitudinally" furnishing a change in the kind ofrockl bat, tH4 agency used in conveyance donbtlesswiir Dethesame. The material here so far as known is gravel, loam, and .boulders.-. The gravel contains a variety of rock such ast gran ite, Jasper and-othCT metamorphic rocks, together with a variety of ancient igneous rock. The gravet'?rnns intb". boulders, well rounded, fairiy-J smooth ; whether taken from the river bed or from beneath its somewhat heavy cover in the valley. The loam is a lightish yellow or buff, though a shade darker and heavier than similar material in Nebraska. Among the large blocks or boulders we have granite, porphyry, quartzite grey, light and dark red and purplish, with heavy deposits of slate rock. In some of these deposits more beautiful and valuable stone is found such as lumps of ribbed chalcedony and richly variegated green stones may be gathered. A Nebraska field. For the purpose of getting a more cor rect understanding of the drift deposits we gather from another field the po sition of the several varieties of material as they were deposited and which, in general character, will obtain through out the period. In eastern Nebraska upon the- cre taceous floor drift material is found rest ing thereon amounting to eighty or one hundred feet in depth as follows: At the base, a hard and tough variegated clay in which is slightly mingled gravel and boulders. Upon this clay is found a bed of fine quartz gravel about two feet deep, size of gravel a little less than one quarter inch cube, and each grain or gravel apparently of the same size and weight, showing that not only this bed but beds above were conveyed by water and that the determining cause of deposit at that place was the strength of the cur rent at the time and size or weight of pebble. Above the quartz gravel is a bed of coarse, rusty sand followed by a less coarse bed of clean grain, topped with a bed of sand of finest jparticles: Each of these beds is well defined by clear level lines'running across the face of de posit Upon this bed of fine sand rests the rich buff loam to a depth of seventy five feet or more. Whilehis loam varies in shade or color Ja little, there is small difference from top to bottom in quality as to fineness orjichness. Not a pebble the size of a pea is found in it and though we travel scores of miles, excepting in the bed of the deep ravines, which time has cut through and down to the boulder clay, not a stone is to be found. One ex ception to this rule was found in this field but it was the only one known to the writer as follows: In one of those ravines and near the top of the sloping bank a large slab of red quartzite lay with a few small pieces, corners straight and sharp as when rivenjrom its native bed. This slab as it lay was sloping with the bank and evidently when de posited Jhad been uponthe surface of the loam after it.had become hard enough to sustain its weight; subsequent erosion forming the ravine had permitted its sliding from its original position. From the above we gather the method of the various deposits of the drift First boulder clay, second, very -fine gravel, followed by beds each one finer than the preceding till wereach.thetop, when it is capped by large and small angular rock belonging to the earliest of days. Each one of those beds gave indication that there was time between each de posit, that is, each one had become set tled so that a subsequent deposit rested fairly upon the bed immediately beneath it, and without mixing with each other, Xn The Valley. While we have not the number or variety of drift deposits as mentioned above, what we have will be found to have been deposited in the same order. Here we have as yet seen no boulder clay but we have in its place a much heavier deposit of gravel resting upon Eocene strata. This gravel is found in the bed of the Willamette river: It is covered by loam and soil in the valley near Corvallis about twenty feet ' Fifteen miles south it comes to the surface and covers many acres of land.- The, same gravel is used for our streets and roads instead of broken rock.- Where the gravel is covered by a subsequent deposit of sufficient depth it will be found to be loam, topped with darker soiL !- ' ' But if we are short of the variety of de- posits, as in the Nebraska field,,our blocks or boulders make up for this largely; for here they are strewn along for miles near the base of the foot hills and frequently stretching out one or two miles into the valley; where the center of a wave-like undulation occurs, these boulders will be scattered, and where the road passes over them they form a hard grey pavement BABY RUNNING SORE Wont Sight Ever Seen. Legs, Hands, ' ! ''' Arms, Body One Solid, Deep, , -;: Banning; Sore, .'i Began Using Cutlcura. In Two Weeks ' Great Improvement Followed .1 . .. by Complete Cure. - ..I.-. :.. v,v ,-!. . .-:;, :'!-. ! My child began to be sore when two months old Eczema on bis face and head. It rapidly Sread over all hia body. Every one who aaw m said he was the wont sight they ever saw. linen cloth ever ao many time a day, and then he would stick fast to his clothes. I could not dresa him alone for months.' His little lege, hands, and arm were just one solid deep ronnine sore. He was sore all overbat the deepest ones were on his armsj legs, and face. . Hisfaceand ears bad great deep cracks In the flesh, ana were swollen so that he did not took like a child. His were the worst sores I have- ever seen- of the kind. We began using the Cdtiouba Remedies, and in two weeks we conld see a great improvement, and now he is completely cured. His skin is smooth and white, and he seems entirely well. (Portrait inclosed.) We are so thankful. I would like to tell everyone who has a suffering baby about CimouRA. . , ... MBS. TRED. BARRETT, 1 Wlnfleld, Ingham County, Mich. 1 ' ' CUTICURA WORKS . WONDERS CtrnoTaa. Remedies have effected the most wonderful cures of torturing and disfiguring skin and scalp diseases of infants and children ever recorded. They afford rastant relief, permit rest and sleep, and point to a speedy euro, when the best physicians fail. 'Parent save your children years of needless suffering.' Cures -made in childhood are permanent, t i A ? f Sold throughout the world. rYles,-Cvncrnu, Oe.; BoAf,Uc; Bbsolvbbt, Pottsb Dau axd Chzk. Ookf., Bole Proprietors, Boston. j. How to Cure Skin Diseases.?! saailsdfree. D I DVC SMn 1 Bcsrp purified and beautified DAD I 0 by CCTictraa Soap. Absolutely pure. WCEN FUU OF PAI5S8 rind in Cnttennr. AntJ-Vafn Vimm. tar instant and grateful relief. It y IS Uie JUW9 HU1 VUIJ JMlir-IIIM"fr, m In other plaecs farmers have either sunk them beneath the soil or carted them away. A question here forces itself upon us; it is, from whence and how was this ma terial brought here? One may readily answer, ice and water, as given us by our text books, but do these materials not suggest themselves their mode of convey ance? It is scarcely possible for us to imagine the vast field of loam in Ne braska to have been carried in any other way than by water. So, too, the quartz, gravel and the different beds of sand, so carefully assorted as to size and weight, could scarcely be so delicately arranged by other than water. But when we come to the gravel and boulders, and blocks or boulders, many of them of great weight we cannot rest with water, but some other carrying machine resting in or upon the water is necessary. Nature has given us ice fields and bergs, floating upon the waters as ships upou the sea. These were the vessels, our gravel and boulders and larger material the cargo. The gravel and small boulders were picked up in the ' bays or on the seashore, where they have been rolled about forages by the dashing waters. The slabs of rock which we have called blocks or boulders have been torn from their bed in some cases, for in one case near here some years ago, there was found a line of granite in blocks stretching over ioo feet in length. By its side was a string of blocks of slate of equal length, close together, with quartz-' ite scattered here and there alongside.. These lay in the ground as pavement and apparently deposited as they were taken from their place of deposit , As to where this material came from we do not know exactly, but the course of the continental drift has been from the north, southward.It must be so in this case, for to the south and to the east and west we have high elevations, whichjfrom the low locationof .this material in the valley would forbid other direction than from the north. As well, so far as known, no rock of such antiquity is found in western Oregon. In Nebraska the near est location of such rock is several hun dred miles away, but the conditions here suggest a nearer place,' probablyiwestem Washington. The position in which these large rocks are found suggests a slow and quiet de posit. They also suggestjthat this was the latest and last effort of the glacial epoch. It is to be hoped that some of the finer and larger blocksj will be preserved, for as time wings its way and papulation be comes larger, with few of Jthese monu ments remaining, those preserved will be of no Httlevalue.to the studentjof the fu ture. . . The Willamette valley presents to the professional or amateur geologist a rare field for examination and study. The Minneapolis' Tribune asks, "Is sugar to be taxedT' ' ! The dem ocratic New York Sun answers as follows: "Of course it is, unless the democratic" platform ia tram pled under toot by its authors and advocates. : Se0THERS aTV I CLEAR , lit , t LUNU L""& & US EMS m I Mtm MENTAL ENERGY AVERTS Sarsaparilla ' S. P. Sanrav of Towanda, Pa., whose constitution was completely, broken down, Is cured. t7 Ayer's Sarsaparilla. ; He writes: : "For eight yean, I was, most of the time, a great sufferer from constipa tion, kidney trouble, and Indiges tion, so that my constitution seemed . ;to be completely broken down. I wa,' induced to try Ayers Sarsaparilla, and ; took nearly seven, bottles, with uch excellent results that my stomach, bowels, and kidneys are In perfect con- . dltion, and, in all. their functions, as ' regular as clock-work.' At the time fL : I began taking Ayert Sarsaparilla, my ; weight was only 129 pounds; I now can ' brag of. 159 pounds, and was never in so good health. If yon could see me.be--fore and after using, you would ,vant me for a traveling advertisement. , I believe this preparation of Sarsaparilla , to be the best in the market to-day.? . ; Ayer's Sarsapariila .. ! ""- .. ... ir : i. v ; - prepared by Dr. J. O. Ayer & Oo Lowell, Uaaa, f Cures other8wHI cure you IV. L, DOUCLAG i 03 SHOE hoTWp. Do vm wear thera7 Whaa next In need try pair. . Bt In the world. ? '.mm mm ! V4.UU 42.00 nmiADKS 2.00 r-T roii soy ) If yos want t ffxe DRESS SHOE qife In the Watt ttybs, oWt pay $6 to $8, try Iny $3, $3 JO, $4.00 or $5 Shoe. They fit equal to cttttom madeand look and wear at wed. If yon wish to economize In your footwear, do (0 by parcRulot; W. L. Doagtas Show. ' Name and prlco stamped oa the bottom, look for it when yon buy. W.X.IXHT0ULAS, Biwefcton, Km. Sold by Z. H. Davis, Agt., Corvallis. IB. W f Li.'. .rTW- MYSTERIES! The Nervous System the Seat of Life and Mind. Recent Wonderful Discoveries. No mystery has ever compared witb that of human life. It has been the leading subject of professional research and study in all ages. But notwithstanding this fact it is not gener ally Known that the seat of life Is loca ted in the up per part of 1 he spinal cord, near tbe base of the brain, and so sensi tive is this portion of the nervous sys tem that even the prick of a needle will cause Instant death. Recent discoveries have demonstrated that all the organs of the body are under tbe con trol of the nerve centers located In or near the base of the brain, and that when these are deranged the organs which they supply with nerve fluid are also deranged. When it is re membered that a serious injury to the spinal cord will cause paralysis of the body below the Injured point, because the nerve force Is prevented by the injury from reaching the paralyzed portion, it will be understood how the derangement of the nerve centers will cause the derangement of the various organs which they supply with nerve force. Two-thirds of chronic diseases are due to the Imperfect action of the nerve centers at the base of tbe brain, not from a derange ment primarily originating in the organ- it self. The great mistake of physicians in treating these diseases is that they treat the organ rather than the nerve centers which are the cause of the trouble. Dr. Franklin Miles, the celebrated spe clallst.has profoundly studied this subject foi over 20 years, and has made many important discoveries in connection with it, chief among them being the facts contained in the above statement, and that the ordinary methods of treatment are wrong. All headache, dizzi ness, dullness, confusion, pressure, blues, mania, melancholy, insanity, epilepsy, Sr. Vitus dance, etc., are nervous diseases no matter how caused. The wonderful success of , Dr. Miles' Restorative Nervine is due to the fact that it is based on the foregoing principle. Dh. Mixes' Restorative Neuvink Is sold by all druggists on a positive guarantee, or ut direct by Dr. M?les Mbdical, Co., Elkhart, Ind.. on reoelpt of price, $1 dot bcttl. six bottlos top in. express prepaid. It contains neither opiates nor dangerous uru. OUR PERFECTION ADJUSTABLE S SHO E FOB MEN'S WEAR, Are the Best of the Lastest Improvements. r HEre unlike alLo'ther Ad jiis.taUle Slices, as (heyjiave the Appearance of the Regular Make. ... , They expafiti acioes the b;al and 1 joints as much as t he aclion of the foot requires, thereby giving per fect conilbrt to the Wearer'. " f The v cost no more and are war- :' ranted to wear as long as (he ordi nary shoe. j The adjustable feature enables this should keep' its shape better jthan any other. ,c.j ; They require" uoue.-.of s the so called breaking In.? J " j People wishing to wear ;a nar inower, shoe than usual and fit, the same time emoy solid comfort people having tender feet of auy description. "land! people looking for a shoe that they can Wear from morning until night without tiring the foot will give the Perfection . Adjustable ihe preference. Depot for'Benton County, Headquarters for Clothing.' i Cm Oontrh. Boauaencss. Sera Throat. . 3pMpprMDpUyjrelevWsi)osiiis;Cons;U vMid sVsThnaai -For CeaMtunyi Uon it has no failed: will orRa tou If token in tirae.) Bold by Drugg-isis on a ruarante. Tor Louie Back XArja'i 8PLAIIT2. SSetO. ATARRH. BELfOOY. lts tou Oatarrh t Tnta wmalT fa mmnn. remedy ia gm sta. Iclector teedtoonrejrou. FlioeoOota. Isieotor trea, For sale by.T.Gfaham. ' ' " CANVASSERS. Canvassers wanted to sell Nursery Stock. : C0BVAI.U3 MUB8KBT CO. H ES t : I. . i sijaaj-w- - i . . . r or voeas, use bj -,i - - - Ha Rheumatlsrriy Lumbago, Sclatlcay Kidney Complaints, DR. SAKDEN'S ELECTRIC BELT With Electro-Magnetlo SUSPENSORY i-uieHi.i uch improvement. I Win cure without medicine all Weakm. resulting from over-taxation of brain nerve forcen: excesses or India. cretion, as nervous debility, sleeplessness, laniruor rheumatism, kidney, liver and bladder complaints! lame back, lumbago, sciatica, all female complaints general III health, etc. This electric Belt contain. Woadrral Improvements over all others. Current la ineUuaUy felt by wearer or we forfeit ts.0oa.00, and will cure all ot the above diseases or no pay. Thou, sands nave been cured by this marvelonsTirvention after all other remedies failed, and we (rive hundreds of testimonials In this and every other state. Our Powerful Improved ELECTRIC BESPF.K90RT, the frreatest boon ever offered weak men, fuse with .11 . Utth and VIsorou Strawth GUAKAHTKED In SOU 80Uv Send for illus'd Pamphlet, mailed, staled, (rea t . SAHOEN ELSCTRIO CO., Wa. ITS first Street. tORXJLA.lVa OKU EAST and SOUTH VIA THE SHASTA ROUTE. OF THE Southern Paeific Company Express Trains l.eays Portland Dally. SOUTH. NORTU. Lt Portland 8:1ft p.m. I Ly Sau Frisco 7:00 pre Lv Albany.... 10:23 p. m. Lv Albany 4:2S am Ar Sai Frisco 10:lfia.m. Ar Portland 8 :20 am Above trains stop at sdl stations trom Portland to. Albany inclusive. Tangent, Shedds, Halsey, Harris burg', Junction City. Irving, Eugene, and all stations from Roseburir to Ashland inclusive. Koseburg Mail Daily. Lv Portland 8:30 a. m. I Lv Roseburg. . .7.00 a. m Lv Albany 12:45 p. m. I Lv Albany 12:30 p. m Ar ltoscburg; 6:60 p m Ar Portland 4:80 p. Lebanon Branch. 8:10 a m. ..Lv. . .Albany Ar. ..3:25 p m 9:00 a m. . Ar. . ,Lebann...Lv. . .2:39 p m 1:20 p m..I.v. . . Albany ;...Ar.. 10.21 a n 2:09 a m. .Ar. . .Lebanon. ..Lv . ..9:30 a n DINING CARS ON OGDEN EOUTE. Pullman Buffet Sleepers: AND SECOND-CLASS SLEEPING CARS, Attached to all through trains. Tut Si DMjIob. BETWEEN PORTLAND AND CORVALLIS. stall Trait. j Except SEnli7. LKAVS. Portland 7:30 a. m. CorvalUs 1:00 p. ro. SKBITK Corvallis 12:15 p. m Portland 6:35 p. m At Albany and Corvallis connect with trains of the Oregon Pacific Railroad. Sxpreu Train. Daily IxeaptSusday. LEA VI. Portland. 4:40 p. m. UcMinnville 5:45a.m. ARRIVE. UcMinnville... 7:25 p. nr Portland 8:26a. m THROUGH TICKETS To all poiuts in the Eastern States, Canada and Europe can be obtained at lowest ratea from A. K. Milner, agent, Corvallis. -- " E: P ROGERS, Asst. O. K. &P Agrant R KOEQLEKMaoarer. Portland, Oregon. A. F, PETERSON, ARCHITECT AND BUILDER. Special aUeiiti-m ttven to Job ivorU, ptivr btiUinjr. store a?;d oOice, tHiiug. Ke&pmg on lmnd n choice litre of room and p'l-tare mouldings. 1 am prepared to 1111 rders for ail sixes of fiiuture frames with neatness an' ''iipatcr fealfofactimi Ukiant-d, Give nie a cal "dies UBu shop two blocks southwest of public FOR A CASE IT WILL-HOT CURE, ti An acrreeable Laxative and NERVE loma v Sold by Druggrists or sent by mall. 2Sc., 6m, and $1.00 per paokaaje. Samples free. TTf TTO The Favorite TOOTH POVSU 11. U ULU for the Teeth and Breath, 860. iU- Fdraale'by T. Graham. U '" Irf it JOHNSON, ATTOBtlEY '.'AT LAW, ' ' " xoiiVAMVis. oii. SECOND-HAND STORE. Stoves, FumitTire, . Household of All. Kinds .,, BOUGHT AND SOLD. Bamins !s All Lines of Goods. ' nVtm CAMPBEIL, A r, ,' .OOEVALLIS, OREGON. If sin stiset, X doors jprth of nodes' Qun Store. ' BO WEN LESTEK, DEITTEST. Office upstairs over First National Bank. STBICTLT F1BST3LAS8 WOHK OUABAHTEED. OorvalJis - Oregon " CAS KEY & OTTERSTEDT, And?-Wagon-Making, r ,- I KHIOHT's OLD STAJTDi., V. CORVALLIS, ; - - OREGON. All woik in the line done promntly and satisfaction guaranteed. , A 1 - S Physicians, Surgeons an4 Ac- ic tH2AO coucheurs.Yie3 ' aa-dffiice nn-stairs In Farra and Allen's ' Krick. uthice nonrs from scov a. M-.ana from 1 to 2 and 7 to 8 r. u. Calls promptly . . . .11 -ii j -7 l t atteiuled to at ail noars; eitner aay or niiib ii Jas. A. CAUTHORN, i j ; j I iOorvallis, Oregon, f, j j ; j Real Estate and Insurance1 !Apl Vann 1. anil a and CKtv Pronfirtv for sale. Bents Collected. Taxes Paid. 1 :tar ti fififiCL J.txkj miA.in . f- -t