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Show OGDEN. THE MORNING EXAMINER -r deposition on sea floor si l be point in question, uUd when the gi Mins re thinly bound and cetogether by presume, weldingn as mentation. the n k is kn iv (.uMise gisvei made ulu solid Cuuut less toi k is cm led conglomerate. shellfish live and die ou the H?a floor, slitre the watei is char and free from -- edinieui. Their haul shells ate made up largely of lime. Fa i tides of the broken shells ate easily dissolved in water and material is a i the resulting bare been brought f- (Ue THE GEOLOGY OF THE aud-ituu- e. RANGE IN COLORADO FRONT Hw the Mountains Were Made and How Nature Is Incessantly at Work to Change Their Forms. is Killings. The ground under our feet Is either lu the condition of the suil, broken up rock impregnated with decayed vegetable aud a .id gravel, or, matter, ilust, k nn the other hand, it ia the solid ihe Where to surface. the coming incoherent deposits cover up 1 lie bedrock ll is still invarinbly found in well borings at no great distance down.. The r is it I expow-dMilld rock, leJ-roc- s I! i J s . : i ? ' ' constantly wasting away and crumbling to dust. We get a measure of the time required for ibis in the decay of tombstoned. It is a very slow process, hut it is of prime importance in Ihe reduction of the mountain masses, and of the whole surface of the luud to it jura-eforms. The action of ihe weather it self is competent to csumi the decay masses. and disintegration of rock Kven the firmest building stone Is seen under the tnicrusrnpe to bn shot through and through liv cracks and crevices.' Water, therefore, readily stinks into the rocks, and if it freezes in their ini erst lcea it. must then expand and art a a multitude of liny naves to diive portions of the rock apart. Water running over the surface of the fund winks all the while from higher lo lower levels It never flows up hill. The motions of pure wider on the land could have scarcely any effect upon it. A siren m or a rivei, however, polishes its lied most effectively ami grinds on It bv means of the loose sand and pebbles which it matches up and pushes along in its course. The amount of wear ac compelled in this way by water running for countless yenrs In the same channel, and supplied all along with to pieces of broken rock with which crape its bed, is very great. carEvery gulch and every valley ries such a stream, active through out at least a part of the year. The rainfall as it runt off is conreut rated In the same valleys for many ends of years, so that the aceumulal ed cutting, thuugh so little lu cvcu a century, is enough in the end lo permit streams to sink themselves deeply in the hoitonwi of canons so lung as a slope down which they may flow remains. The valleys and canons were not filled In former than ages by streams much larger I tiros of the present day, Their width at the top Is nevsr tbs measflowed ure of the streams which through them In former times. The river cuts down like a saw, but to gradually that the decay and of the roci, actually rutting under the influence of the weather, together with the flow of water down the sides Into the main stream, and ibe Idling action of frost as water freezes lu tho innumerable crevices on the valley sides more than keeps pace .with the downslnklug. The saw rut of l Its river Is widened very inm-above so that a valley results aud 'the limbs of the letter slope far tou steeply to the point to represent the actual condition of the valley sides. The declivity In hsisened materials is never much over thirty degrees from the horfxonial. The agencies outlined shove are responsible fur nearly all the carving of the surface of the land. The mountains are nut piled ftp and laid uNin the plains. They stand out because they are mode tip of the more resistant rocks. The is like ricliing. Relatively proce-- a simple downrultlng forces are ceaselessly at worz. The parta of ilia land which resist most strongly are left in relief alter many thousands of feet of rock have been removed everywhere. The nature of the rock composing the crust of ihe earth may best lie understood by attention to the comll-tionof two simple experiments. We speak of the great classes of rock as, first, the group of the igneous rocks, those which, like volcanic lava, have once been million: and, in the second place, the sedimentary rocks. By sedimentary we mean laid down under water. If a large glass vessel full of water lie taken, ly throwing into il first sand, lhin when that liss fallen to the bottom, coarser gravel, suit earth and, lastly, flni-lbroken shell fragment, we may imitate the process of scilitnenl.it mn. The water a Mining eicics u;i the material cast iiiin it. lor it allows the larger, heavier imriicli-- to scttlo to the lmltom tlrri. The finer fragments sin!; nu iiw hlmvlr, bin they come to real after a brief time. The material will. litt'i r the of the experiment, lift laid down in layers that are approximately horizontal, and I hero are differences In the physical characteristics of successive layers. Some arc relatively coarse, while others arc of fine materials, aa th.y wi-r- supplied. On l!:e fiisir. near the shores of the Co'iitiiMiMS. this process bn been ls years. The going on for count uliingxliore have been constantly bringing sainl and mud. gravel and limey shell fragments of different deRivers sin chief grees of fineness. ageuis in supply ins theoe wm n down ruck materials. Tney are Cimrlnitslly sawtng on their, hid and m ceiling the resulting tine particles out to sea. 1 Inlay ers at the bottom of the section sediment s arc the older, while the newer aceumulal ions are at the top. ! The total pile is many lliuusaiids feet in thickness. The bntroni layers are under a very t ptissure. due tn the weight of the stratified layers above them. This has ,lsris nturli to weld their particle together and them solid. The small amount of water between-thgrains of sand and mud has dissolved part of the suhatunces of the Inclosing rock grains. With the loss of this water Ihe dissolved mate-tial- e have been depnsited chemically as a cement In hind the grains together, la these two ways the l.xice materials on the hcu lluor become solid rin k. nt disln-tegrailu- n $11.(5 SPECIAL $11.45 for a handsomely decorated dinner set. Other acts for 14.00 and up. We have the line of Chine. Olasa end Silverware for Christmas presents. 100-pie- ce - i Wheelwright Bros., 2476 WASH. AVE. A PHONE 147 The Utah National Bank a OF OGDEN . United States Depository, Ji Ei DOOly oeeeseoossse PNlidtllt Vico President Horace E. Peery Rilph E. Hoag As V. McIntosh Cashier Assistant Cashier Interest Paid Os Savings Accmmt THE ITALIAN s SWISS COLONY on the Pacific coast raise the finest wines grapes on the Pacific are absolutely pure. If you wish to dispense good cheer fur the holidays order come of their wine from coa-t.Th- k-s-s FRIZZINI BROS. h Street 25: 200 ALBERT F. cur-I'cn- uf-su- RICHEY, fy-ca- UNDERTAKER r 'Phone 150. e 2372 Washington Ave. If you want Eastern go to Ballard j Corn-Fe- d Beef & Rinckers Ml 24th StroeL 'Phone No. ' ! VIA TIME CARD. TO :tsJ Omaha Chicago Effective Dec. 4th. St. Locis Kansas City AND ALL PRINCIPAL BARTffRN No. 2 Overland Limited for. Omaha. Council Bluffs, Denver, Kansas City and A. B. cou-iaiit- lj- e. s s The interpret a' ion cf Ihe geo!,',, Ill history of the Krsni range in Folm-sdexamination of the rocks Hennsiicit in the- light oi aurh facts ax we have under water shows that often hundreds oii lined above, i in this kind. At one of feet of the same material are laid time au island mass of granite existed down before the supply of sediment is in the ea Rt 1e pla-where the moiiu-tait- is Down-ri- d now (hanged at the point of deposition dug ini res. U.I give ti tin icm k wea het-inand 1tc.in r; uin:i red tire I Be.lsuj mud made v.hi,h wo tall sialc. S.ntd nun lie. it maa verv cotisidcrnli'y. Tne MOSELEY. Traveling Paaaengar AgsnL Ogden. Utah. . .... A. B. MOSELEY. Trav. Pasa, Agent. river-cuttin- , s - For Full Information Call on At Morrison the layers underground at an angle uf 4i degrees wit It the horizon. The etching forces of uaiuiv have seized uy.m all the weak portions of the rock layers and the stronger sedimentary beds, coarse or flue, usually hard band-tun- e, As arc left in relief a hogbacks. g elsewhere, weathering and have stripped them off the granite flour T'ic on which they were deposited. granite itself has beru cut Into deeply, Inti, being stronger than the sediment nties, what ia left of il stands up high ataive them in mountainous massco. Continent building lias been attended by nun- - or lesa Assuring of the earth's crust, and one large block hns often been slow Iv pushed up w bile its fellow on the oi iter side of tiro great crack has remained in place. Fike's peak is such a block, pushed, or as we often uf say, faulted up many thousands feel. Tho great fissure bounding it on tne north is a line of weaknhus aud the Ite pa depression follows it. Along its extension, rock weathering, decay and ! river-cu- lt ing have been more effective than ia places where the earth's crust lias not been fissured. A small volcano broke out through the granite in the Cripple Creek region in the midst of itch a topography, as we have today in comparatively recent geological times. Khowera of ashes snj streams uf lava were Mured out from its vcnU Long after it had become quiet, but wliilo underground reservoirs of molten1 rock, still rxihtrd beneath ils core, heated solutions nie up through such fissures sitil cracks as they found ready for them in the volcanic rocks and in the granite, bringing gold, with some silelements ver and tellurium. These were deposited along the fissures chemically hound together as the valuable mineials in the Cripple Creek mining lint riel. Karlier surface flows of lavs to the ninth have overrun the region near Goldfield. They now apiicar in North and South Table mountain. The two were once continuous. rut Clear creek had made a deep through them. All the elements of the Front range ate lieing ceaselessly broken down by wcatheringand erosion. At tho present time stream flowing out from the mountains carry great quantities of granitic gravel with them. Tliclr predecewaonl, Vorking at higher levels, spread out a great sheet of such materials along the (dope of the rang. This originally continuous mantle of surflulul gravel now seen capping lung Isolated mesas has been cut into ths present streams and they have worked loan to depths of fifty to 100 feet below its top. The nics gravels are the most t of all the deposits in the Front range region, and their destruction at the hands of the rivers rutting valleys t lirottgh them brings the geological history of the country down to the present day. ! 1 2:SJ p.m. No. 4 Atlantic Express for Denver, Uiusha, Council Bluffs, Kansas City and ill 7:20 p.m. points east, dally ARRIVE. No. S Pacific Express from Council Bluffs, Omaha, Denver, Kansas City sod east dally 3:15 a.m. Limited No. L Overland Council Urns ha. from Bluffs, Kansas City, Denver and all points east, .. 3:25 p.m. .. . daily 2:00 p.m. No. 9 Fast Mail C. A. HENRY, Ticket Agent. the UXIOX PACIFIC. g d r.i Be surf year Ticket Beads dim u. - POINT8 UOGHANQETOSK: usr The toothilhi of the Front range are chiefly made up nt sedimentary rorzs. hut in the Pikes peak region the niuuntalus themselves are of gran tie. This Is au igneous rock, representative of the second great group of rocks. Its method of formation may ha understood by the melting of roek masses in the experimental laboraa very tory In furnaces which give first be high beat. The granite may H'Uuced t0 powder and then fused, cools rapidly, under When the ntu surface pressure, it becomes line glass a uoiieryatalllne body. By lessening to i Vi heat very gradually so as of tiiirf cooling the lengthen greatly certain changes are indicated upon the rock as it takes the solid form, The substance of It is partly glassy, as belore. hui In other places it possesses a crystalline character. Under the microscuiie It may be seen that crystals of recognizable minerals have formed In It. These same minerals have are known in many lavas-whiceroded at tfie surface of the earth after Mowing from volcanic vents. The artificial product Is essentially the same aa are the igneous rucs which have cooled under like conditions in lava flows. The law has been made out exsrlmenially that the longer the period of cooling tho larger the cry stals In ilie glassy matrix, and ihe magreater the amount of crystalline resiterial In the rock at against the dual glassy portions. The granite of Fike's imaz is made up entirely of common, perfectly crystalline min erals, three or four of which form lbs Is no great hulk of the rock. There seema It whatever. in it base glassy certain, therefore, that the rock cooled only with extreme slowness. At tivas the surface of Ihe earth the which flow out from volcanoes rapid Iv become solid. Within the earth at a distance of a f- -D- -. Nirfece. moltfin rook fa volra may become onol and i the character of a solid, under pres- . atowne sure, only with extreme which j These are condithma under is Igneous granite formed. The rock volcanic in In its origin, but it is not the sense of having been pint, of the materials dealt in hy a volcano active at the surface. As the continental land natascs ave raised above the level aud worn down by the action oT the weather, together with the rutting of streams and rivers, rocs that have reservoirs are cooled In t last laid Imre. The rocks which mnke up the mountains of the Front range tn 1'ikn'e peak region are chiefly granite, formed originally deep underground. With lltcni are other rocks which hare liten under great pressure in the depths of tho earth, so that they have hem sheared slung certain panes and their enu- -i fluent mineral drawn out into band. The total uplift which Iln-- have tnistained. with reference to Fes level. In iho mass of the cnmii.ciit. amomils to aevernl of the rocks miles, and originally above tlieiii. with portion of their own removed by ihe ccnse-1c- k mas, have been of wear mid tear of the rlenn-nithe urn I her and by running water. It borne m mind that should be sudden not thir vnl cliaiigea were lint very gradual. ail.) eiiitliipiake-likThe results which wr see are the produria (f causes which l.nre been ivr on the earth's Fttrface fur vat ijic-.iof time. They are still active in the same manner nr-- with like work is done with iniensity. extreme slow nr. 8. During a mans life the changes are almost loo slight to be noted, hut the accumulated results of time are very after king ireu-iironidei-ahle- . The fam-- operative on the earth work so quietly that they leave the face of nature almost unchanged from day to day. but they never cease from their activity. Giv-- it tin wivild fasiilon necessary Unnx llu-aanin form as we see about us. OgJen, Utahfl TIME TABLE Our New Years Resolution This Is San Pedro. Los Angeles and Salt Lake R. K. Co. West and South Temple Sts. Salt Lake City. DEPART. i For Provo, Lelti, Fairfield . - ' and Mercur, connecting at Nephi for Manti and intermediate points on 8:00 a m Sanpete Valley Ry Fur' Garfield Beach, TooMamStockton, ele, moth. Eureka and Silver City (via Learning- - Depot, Third DURING 1905 THERE SHALL BE NO OTHER 8ER CHICAGO VICE BETWEEN SALT LAKE CITY AND AND ST. LOUI8 QUITE SO SATISFACTORY AS BURLINGTON SERVICE. Keep this In mind and whenever you are ready to E? East ask me to produce the evidence. ton. IL F. NESLEN. General Agent 79 W. SECOND SOUTH ST, Balt Lake City. Cut Rates East For the Holidays the arnte are thrust Into the water and a big flail is Hupping around on the Ice. In this way fits ten pounders were taken out of the pond a few days ago in as many minute. The largest flah yet obtained weighed twenty pounds. It is the amc out at Salt River. The fish are Jammed logo her and lu Some of the river is alplace Hie bretc-most hidden liy the swarms of fth. low water and' the cobl have not killed many of thftn And when hiongbt ou on Fie Ice they kick their death kicks in Ihe conventional fush inn. Just before U- t- water on Shanks lake froze a couple of men rowed down the lake with a long, strong trailcylindrical net. open at one ing behind their scow. They were tillable lo get the net fill of firfi out Of the waer without help. The catch weighed 1.500 pounds. Garfield and Tooele Bench 5:35 p m ALL TRAINS DAILY, Daily Pullman Buffet Bleeping Car Service between Balt Lake, Milford, Modena and Calientes. Direct stage connections for all mining districts ia southern Utah and Nevada. 201 City Ticket Office, TICKET OFFICE HEALY HOUSE, Opp. Depot PHONE BELL 1S1Z. MEMBER AMERICAN TICKET BROKERS' ASSOCIATION. iMiuisville. Jan. 2. They are fishing with hatchets aud axes out on the ha, American For Provo, Fork, Lehi, Juab, Mil-foFrisco, Callentea and intermediate points 6:05 p m ARRIVE. . j From Provo, American Fork, Lehi, Juab, MilFrisco, Calientes ford, and intermediate poiuts9:45 a IH From Provo, Lehi, Fair-fielMcrcur and Sanpete Valley Ry. poiuU..5:35 p m From Silver City. Mammoth, Eureka, Stockton, d, IN KENTUCKY THEYRE F13IKNO WITH AXES. The drottgM mrnle rhponT. till there wa not more than a foot of two of water in many of (hem. A In, aud jpw (jUyg aK,, a old simp (ii0 jIOIja wnP rnvercd with ice five or jnt..s Jwip Tlie lHt"cr Uh had trouble keeping ahve even before freezing began. When the I re funned they were forced lower and lower in the" water. The ten. iitteen and I wen i y pounders were either jammed together in the big spring holes ur bad to swim around ou their siilcs. Out al Shank' lake iherc me thousands and llioiiaauds of fish. carp, and dogfish, inipriscued in llte iie. TliPy range nil the way from minnows' fo twenty pounder. If a man wanisany of them, all lie hns to do is to gor pet mission from the owner uf the pond to take them out. A hole is chopped around ths outlines of ihe lish as seen through I lie ii e, t he cake of ice is removed, 7:45 a m cut-off- ) rJ, tei-eii- Cane Run road. They are making bigger hauls in ten minutes than they could make wit It hooks aud lines in ten days. Ten and fifteen pound carp have been seen for and lui as big a long time and other kinds of fish in abundance end uf good weight are being obtained with the nxe and the baichet. The protracted drought which began last July and is not. yet fairly ended ia largely dw?ndle 1904. DEFkitT: and Express... 8:20 a. ia. cast-dall- condition of the layer or rock in the Garden of the Gods. The lines which mark the change from coarse to finegrained sandstone, ot from material of one kind to that of another, a from sand to tine sand an. these are the aud original lines marking the lower limits of the single rheets of sediment), now stand straight up and itn-nt- Mail Nov 6 r con-siuiitl-v e Threa Trains Daily s Ann-rii-a- four-fifth- 1 Kiinilatly-beii- UNION PACIFIC of sea shell were changed into compact limestone. The uuraietng of a the North cuuiiuent hat Kv ea to beds of ruck which were (tint) on the mean floor aa altitude, in FAxtern Coluralol of over B.ow feel aove ih Originally ihe laveis of BeJiucntary rocks were horiziiiiiaL 7 ue uplift was applied unequally lo them, however, nu that now in place the fcmgle bed are lilted tip at varisheet ous angles. Compreeaive forces in the earth crust have folded them greatly. Some Hand nearly veilical. This is th re-u- deep-seate- (nglomerates. Dne-giatu- down-sinkin- . CIS. ta costs ing broken up rock materia i and fine, were arrie.) ma to ia by W I raiiMpoitroi along and laid Linn in approxoreau o imately horizontal luiei. a bed aud and mu-,- and gravel. Afterward by were tney preBbine and made into firm aandaimi'-s- . bl.ale and nl wli'-ievc- ro-sul-ta I: natural tumiir all through ibe hanks of sheds, or a lime cement. The are usually tety firmly bound rock is ogi! her, and the reetiliing hmenoiif. Any t tares ot me oi gaiiinms which gave their skeo-ta- l pails lo make Whole shells are ofil up are fos-il- s. ten beauiiiully prrscrv eil. In successive formations we have a fairly complete rtiord f the. life Of the lime during were deposited. The taiiut whim iln-which needs tics ring up in the mind ui the ulisr.rvcr is how the transfer made so that sand, which va3 unit dciiofciteil under water on the sea floor ud made into firm link, flints a place now in the solid land. This has been exdone veiy gradually, and only with our treme slowness. ObseiVtiiiou along bind Iho that shows cnaKtliim is rising, with lefemtce lo the sea level, at Ike rate of about ue foul a rfiiMiri. 'ihe positions of of the cimiiueut the nuclear mtis-i- s standing in the ocean appear to have herd fixed throughout all the time of which we have any geological record, hut the cuntiuciiis as a whole have been aud greatly uplifted, though slowly, wiiu many temporary when the "sea auvaunll over their borders. 1 he sum total of thine oscillations ha, hern au tiplilt. of inaiiv ihousands ia that the land is ll of feet. The of s itnw nuide up of risks hIiIi'Ii were laid down originally in beds of sand, mud, gravel or almll fragments in comparatively aln.llow waler off Ihe shelving shores of the continents. The process of laud making Is going on. Flotilla is a prone lin. poriimi uf l uc I'liiicU Slates limo. ing upraised at the pivsout the uplifts which the contents sustain aie differential. Kui races that were once nearly piano at sea level are now u thousand or more feet above the ocean, and unequally upraised or warped. Occasionally the accontpantotl movement hits been within the conllimuial noisscs by the fiiritiailuii of great (insures with tho on gradual upraising of the solid rook one side of tin vertical break or cracw, while lhar on tlw other side h in place. This Is kuuwi m favfanning. Ktu-- great cracks are orable channels for uprising solutions Vnlu-fil- o containing the precious metals. ore hoilies result when these are liag-men- Vudor the same restore it to tor (lie lunitsitoiM it is quite pus-ibgeologist to state simply and clcxrly i.lii! nature of the liners which have proilucsj a country such as lies immeof Deliver or Coio-r.td-o diately to iho tti-- (By Or. Geoiye I. Finley, ProfcsadiI I of Geology in Colorado College. The observer who altogether unacs quainted with sera a confusing array of facta before hint aa he hi anils looking across the plains at the Front range in Colorado. He Is apt nieuially to vail into action severe forces, lie looks to earthquakes and vague npneavels as having been chiefly agents in producing the more fantastic nn-.-- i ahaix-- which he seen. Ilia attention will nut wander from the phenomena which appears inoat strange to his mini. 11j docs nut consider the commonplace. Ho never connects the forces which are ceaselessly though quietly at work today with the aspects of (he earths surface about him. The geological which have come to him through general rending have left him in thu condition of the man to whom n little learning is n dangerous thing. The geologist who would give him briefly the clewa necessary for the interpretation of tho great results in the laadscaite is handicapped in several ways. He cannot use the technical terms which have liecome second nature to him. He must start at the very liegiunlng, fur he is not aafe in presupposing that hie hearer is surely grounded, with no confusion of ideas in the facte on which ho in to bnihl. Specialist though be be, and however painstaking he has worthed to grasp the truth of geological processes, ho must expect that hia hearer will, he startled at those of hie explanations which come to him quit newly. The man will say in n word, i cant believe that, Again the explanation will be so slni pie ns to seem to his hearer totally Inadequate to produce the which he sees. His friend will not listen to him cordially if he adopt the spirit of the man who said, I'm . not arguing with you: I'm telling On the other hand, the task of marshaling the proofs step by step is a very lengthy one. Only by long continued observation and much thinking can one become competent in dealing with the facts of any science. But when all is said and done, every thoughtful man, as he goes about through the foothills and in the mountains finds himself puzxling over questions regarding their structure. Fie would gladly know why aurh great inequalities at the surface exist, bow the harj rocks all about him have originated, and the true meaning of the fantastic forms which they often take. He is, perhaps, interested In uisierstanding the nature of ore deposition, the manner in which minerals of economic importance have been brought together in one place. Now, a physician can put aside all the terms lie usee in his prescriptions for the time being, can explain intelligently to him the condition of a special organ of ths body, and 1 lie nature of the means which lie is to use to prix-oabe- II I LTAU. TUESDAY MORNING. JANUARY, 3, 1905. For particulars, call oa or address agent a Salt Lake Route, or J. M. MOORE, District Passenger Agent W. E. G1LLETT, Gen. Pass. Agt. Cheap Rates to St. Louis other Eastern point Fast through trains daily to Chicago via the CHICAGO & NORTH-WESTER- No. N the No. 12, Salt Lake local No. 2, Chicago, St. Louis .. .. line between the Missouri River apd Chicago. Direct connection with all lines to the East. Two trains daily Omaha to St. Panl and Minneapolis; excellent service to Duluth and Superior. k 7:45 a. m. 9:30 a. m. Urn-lie- .............. d 2. 15 p. m No. 4, Atlantic Express, all 7:00 P- - m. points East ARRIVE DAILY. No. 5, Pacific Mail. Salt Lake and all points East ....11:45 A No. 1. Chicago and St. Loula 2:40 p. Jn. Wa can save you money. Write me. limited C. F. WARREN, No. Jl, Local from Park City and Sin Pete Valley.... 7:00 p. m General Agent, No. 411 Dooley MUiek, Salt Lake (Sty. No. 3, Pacific Express from 12:55 a. m. all points East Through Bleeping care to Omaha, Chicago and St. Izuuis, Now York aad Ronton. Free reclining chair curs. A perfect dining car service on all through trains. C. A. HENRY. Ticket Agent. Ogden. I. A. BENTON. Gen. Aget.Fsgr.Dcpt. 3'Trains Cft Bast of Everything. roll mas drawing-roodeeping can, ballot smoking end library can, Booklorera library, dining cars, la carte aervke, free reclining chair rare and standard coaches. tor fvrtfew lalcnMiloa apply Is C. . WALK El. Glut At. C. A HW. Ry. Scuta St 38 and 40 Wast m Sac-Mi- d SALT via Atlantic Mail all points East RAILWAY double-trac- G Mala Street. TeL 250. LAKE CiTY, UTAH. Salt louo City. O. B. GILSON, Agent Ogden. R. G. W. TIME CARD IN EFFECT. JUNE 8T11, 1904. DEPART DAILY. mr$rs Always on Tim At the Dances At the Theaters, or Catcha Train in a Hurry WILL YOU Invest In a place of enlmpreved lantft In Weber County t THE OREGON SHORT LINE TIME Adjoining Improved farms f CARD. Dec. 4. 1904. Half mile from R. IL Station? DEPART: Right rext to Irrigation Canal f No. 7 Butte and Portland 12:05 p.m. Providing you can buy cn monthly No. 9 Pocatello, Montpelier 1:25 mm. payments? und Butte 7:15 p.m. No. 11 Cache Valley Say $10 or $15 or $20 par menthf and Tinlic 10:50 a.m. No. 12 Sail Or quarterly? No. 8 Salt Lake and interOr annual payments?. 7:35a.m. mediate points And no Interest? Provo, No. 2 Salt Lake. And no taxea? and all points Milford The owner ll pay taxes and cot 3:40 p.m. tinue to itaa the land until It la aoii'b Aiiiy No. 10 Salt take and interJar? 5:30 p.m. paid mediate points 8:15a.m. No 4 ARRIVE: 2:15 p.m. No. rli take No. 9 Suite ard Pocatello Bald place ot land will coat yon 12:50 a.m. Express No. 11 Suit Lake and Tintic 6:55 p.m. par aero. $400 for 20 aerem Nck 7 Sait take and Mil$800 for 40 vcreai 11:25 a.m. ford $1,209 for (I acre No. 3 Salt take and inter8:05 Am. mediate points Address or Call on No. S Portland and Butte.. 7:00 a.m. No. lo Butte and Pocatello 6:tH) p.m. ' If l-- Chinch T had to walk the floor all niaiit with the l.ahy. ('an von think of an.vM'injg woreo than that? Got haul Yc : you niifihl have married out in ('tc'iij.'ind, where the. No. 1.' Obi Valii-10:35 ,m. Pitihis are six niijinho hmu unkcr I r.iir.B eoulh of Juab do not run StaU'.-uu.iu- . Sundays. C. A. HENRY, Ticket Agent. ' She carries her age w. ti. doesn't A. B. MnSELEY, she"" Trav. Pars. Agent. Nt very mi. hn dropped several Dsden, Utah. m in n y pcrsoiul i iwlcdge. D. i:. DURLEY, G. P. A T. A.. -years IWicl.nid Lid lor. Salt take City. - So Daily 3 Remember Always 'Phone 22. f Transfer Company. Allen OGDEN 412 25UiSL Owl Saloon The ONeill Broa.. Props. No. 232 25th St Dealers In first class liquors of ail kinds, wines and brandy. All goods delivered to any part of city every Saturday. Whisky 75 eta to $1.75 quart. Wine 35 cts per quart; 8 quarts, $1 quart Whiskey pr. gaL to $2.25 $5. O'NEILL BROS, PROPS. Phone 135Z. . HUNTER & KENNEDY Room 6, First National' 3ank Utah Ogden, Budding CarpeatLlng, Building, Repairing Remodallng of Houses Promptly attended ta-- All work Guaranteed Enquire at Scan the Want Ads Telephone i. Ola Nolaoiv 045 825-- y. ttta street |