V fUr Prosojf oua Business IVTrn A iw of Cottajre Grove Advertise in the Nuffffct. Bring; Your Job Work to the Nugget Job Office. Prices Reasonable Dcvotcd tothe Mining, Umbering and Farming Interests of this Community, to Good Government, and Hustling for a Grub Stake. VOL. II Cottage arove," Oregon, Friday, October 12, 1900. 3STO. 39 PROFESSIONAL. J. E. YOUNG Attomcy-al-Law . onico on Main trot, Wcit Hide CoTTACJtt GllOVK, OKU. ' J. P. JOHNSON and F. (J, liliy Attorneys and Oounselors-at-Law p . mill Merrnntllo Unv. onlnslnOM I'.O.liullMmt.. COTTAGE GROVE, ORE J. S. MEDLEY Attomcy-at-Law o o o ;-()(llce on Main ilreot-: CoTTAOK GltOVIC, OUK. JEROME KNOX Attorney -at-Law I'rompt uttc iitlon lyl'l to Mining HuhIiicm. CoTTAOK GltOVK, OKU. L. L. STEVENS Attorney -at-Law o o o 8jll ittetillon kIvcii to Mining llimliicm uinl Cullcrtlom. EUGENE, OltB. What to Wear When women sec a stylish, handsome jacket, you often hear them say: Oh dear, I vviHh I had one ....w x , 3ure u cogis so much." 0 Now it's the surest thing in the world they're not familiar with the PALMER GARMENT. They're absolutely correct for style none made any more perfect as to that, and the price is within reach of any woman's pocket-book. My! if every one could see them, how easy it would be to settle the question of WHAT SHALL I WEAR?" Eakin & Bristow. oBaneaeaHBHHOHOBHB9BBHBBoicHeBCRH9HeBeioHeiieHeHnM8BOBioeida9BBaaono MUXUX VT. TIIOMfXlK CHAM. At HXUUY. THOMPSON & HARDY Attorneys a iid Counsclors-at- Law Kjdl mteiiUon nlvon to the Uw of llnc. KUliKNK, OKK. L. T. HARRIS Attorney and Connsclor-nt-law 6tfUl attention kIvc" I" the Mine. First National Hunk Building. KWJKXK, ORE. RELIABLE ASSAYS. tmiile by mull rcrulvo prompt attotittun. FRANK P. WHITE, COTTAOK (HtOVlJ. UU 0m3 Willi Jnnio Iloincny, Mulnnt. ota, r. i.uiru. T. W. KKVIU: Lloyd & Nevill JIIN'IXCi I'A-CIINKKItH V. H. lBt UTY MINKKAI. HUUVKYOBS Itunmii 3SI-.W Chamber of Commori-o 1'OltTLAW), OUK. Tleiihonoriii)'IM7 i'.O. llox 1014 MrvKathcrlne Schlccf, M. D. Diseases of Women and Children COTTAGK GUOVK, OUK. D. J. GOVER Prospector and Mine Locator. For Information on Bohemia Mining District write me. Special Attontlon Olvon to Corrciimlenco BOHEMIA, ORE. Gr.o. 0. Knowlks. Chamim Or.rrt. NOTARIES PUBLIC Bohumia, Oku. Ollk-e at Muslck Mine and Elephant Mountain. BUSINESS. 00 'XO MRS. PET SANFORD'S For Fashionable Dressmaking. MAIN 8TKKKT CoTTAOK GllOVU, 0R. EAKIN & BRISTOW BANKERS' 5 Transact ft Oonoral IlanklnR Iluslnoss In All It llranches, CoTTAGIt GUOVK, ORU. J. W. BENTLY, . The practical-Boot and Shoe maker, located In the Case building, two doors east of the l'ostodlce. Repairing neatly and quickly done and satisfaction guaranteed. Call FOR MEN. Wo handle Sarannc Glove Company's ewxlK. They iiro considered the bent glove In the market. Good Vf How Oil Stock with patented string fuutciicr &0and76e. Our Steam Troof line nro a soft, plia ble glove, ax well as durable; Hindu with indented hiring fast ener 85c, (1 ntid f 1 25. Untitled Kit, nott (lnixh, making a v;ry nice driving glove, .f 1 26. Saranac Buck, light weight, fine Htock,n band, open hack, Porter fiiHtencr, welled.wax linen thread eoft and pliablu; undoubtedly the Itcnt glove in the market. . . . n 00. Unlined Chopper Mits, nil grain calf ikiii 00c and 1. Lined KitCiloves, fine stwk. . . .$1. & Newli COTTAGE GROVE, ORE. FOR BOYS. Cotton Swottcrs, good quality, in maroon and assorted utriped colors 60c. All-Wool, light weight, assorted col ored striped $1 25. FOR MEN. Cotton, good quality, color ma roon 50c. Mixed Cotton anil Wool, medium heavy, maroon 80c. All-Wool, good quality, medium heavy, maroon 10. Same as above, only finer wool, as fiorted Holid colors $1 05. All-Wool, very fine quality, in as sorted colored stripes. . . .$2 25. White, medium heavv $2 50. FOR CHILDREN. Lawn Hoods, made of lace open work; very pretty designs 35 to 65c. Embroidered and Tucked Muslin and Swiss, different designs 75c to $1 35. Ladies' Sun Tlonnets, made of cham bray, full back crown, stitched and lined, assorted colors, ,50c. Our lino of Loopo Embroideries, Rib bons and Drygoods Notions is lurge. Ladies' Summer Skirts, large vari ety ; in price from . . . ,50c to $3. Shirt Waists, different colors and kinds 50c to $G 75. Ladies' Neck Wear in latest styles. . 15c to 00c. ... GARMAN & NEWLAND ... 9aeBSBQBOHOBnCHOB0B0BOBOOnOBeBBOBOnGSBOBOBBefleB0HOBOBeB0BOHOBei9OflO9nOtlOHSR6aone H. C. MADSEN, Watciimakkr. IlepnlrlnE at rciMonable chargea. All work guaranteed flrat-cla.ii. Watchcn, Clocki ami Jewelry at Lowest Trlcea COTfAGE GROVE, ORE. ELITE o Shaving o Parlor Cottagk Gkovr, Oke. GEO. E. GRIFFITH, Prop. William Renshaw THE EXCHANGE" ALF WALKE1. Manager. DKAU5II IN KINK WINES, LIQUORS, CIGARS. Malnitreet, OottBo Orove, Ore. Hotel Eugene HOJjLENBECK BROS, k BRISTOW. Headquarters for MINING MEN. KVEHV WANT ATTENDED TO. EUGBNK, " " ORKGON. NOTICE FOR PUBLICATION. CALL ON B. L. PICKARD & SON For HOL'SK TAINTINO, TAPER HANOIKO, B1QN WOltK.CAnUIAOE I'AINTINO. Work guaranteed COTTAOK GROVE, ORE. TUB JEWKLER. I AM IT! "Cop" First-class Watch, Clock and Jowelry Repairing . Hurd and Soft Soldoring. Wo will soli you nnything In our lino at lowest living prices. W. L. COPPERNOLL, Mgr. Land Office at Roseburg, Oregon, September 27. 1000. VAlInnla ImrflltK rt! I'd II tllllt thfrllmVa inn-named settler has filed notice of his intention to make tinal prool in sup port of his claim, and that said proof will be made before Joel Ware, U. 8. Commissioner, at Eugene, Oregon, on November 23, 1000, viz: Samuel E. Phillips on 11. E. Wo. 7407 for tho Lot 8, NW1-4 8W 1-4, Sec. 28, T. 10 S., R.8 W. ... He names the following witnesses to provo his continuous residence upon and cultivation of said land, vi : Charles Colcord, G. W. Smith, A -bertFcrncll, James Law, of Crcswell, Ore. , J.T. Bbidoes, Register. FOR SALE. I have 75 to 8o goats for sale. VilS Vbatch. Parties "desiring to build barns, cimHc or nther outbuildings would do well to take advantage of the low figure at which The Booth Kelly Lumber Co. are offering some cull lumber in i incn ana 2 urcu tliirkness. Call on them or write them for particulars. Take the Bohemia Nw?ge When you cannot sleep for coughing, It is hardly necessary that any otie hniild tell vou that you need a few- doses of Chamberlain's Cough Remedy to allay tho Irritation of tho throat, and mako sleep possible. It Is good. Try It. For salo by Benson Dnoo Co. , Cottago Grovo. Lyons & Api'leoatk, Drain Druggists. JOB COULDN'T HAVE STOOD IT If he'd had Itching Piles. Thoy're terribly annoying; but Bucklen's Arnica Salve will euro the worst case of Piles on earth. It has cured thousands. For Injuries, Pains or Bodily Eruptions it's tho best alve in the world. Price 25c n Itox. Cure guaranteed . Sold by Benson Dittm Co., .druggist. "For three days and nights I suffered agony untold from an atfaek of cholera morbus brought on by eating cucum bers," says M. E. Lowther, clerk of the district court, Centerville, Iowa. "I thought I should surely die, and tried a dozen different medicines but to no pur pose. I sent for a bottle of Chamber. Iain's Colic, Cholera and Diarrhoea Remedy and three doses relieved mo en tirely." This remedy is for salo by Benson Druo Co., Cottago Grove. Lyons & Ajtlkqate, Drain Druggists. Mr. Altgeld as the attorney gen eral of a Bryan administration would be every bit as appropriate as a Bryan administration. For BprainB, swellings and lameness there is nothing so good as Chamber lain's Pain Balm. Try it. For salo by Benson Drug Co., Cottage Grove. Lyons fc Aitleqatu, Drain Druggist. The increase in the price of cotton is doubtless encouraging to Chairman Jones' round bale trust. Bohemia Nuggetand Weokly Oregonlan $2.00 per year. Cbe Chicago ZypewviUv Price $35.00 The CHICAGO Cannot Be Excelled for Compactness and Clearness of Writing. It is easy to learn to operate, aud there is a small number of parts to get out of order. E. L. King, Gen'l Agent for Ore. Albany, Oregon. C. J. Howard, Local Agent, Cottage Grove, Ore. mesao dMimoa . (vn fin A fin RoK NrTV TvrvA Items of enered'"irt"er:'e.5r fb Mining Men The Third of a Series of Articles on Structural Geology. CONTRIBUTKD. From the distribution of tho more imporant elements in the earth's crust and the mineral foinis which they assume, we have now to advance a stage farther and Inquire how tho minerals are combined and distributed so as to build up the crust . As a rule simple minerals do not occur alone in large masses, more usually they are combined in various proportions to form what are known as rocks. A rock may be dellned as amass f inorganic matter, composed of ono or more minerals irnving for the most part a variable chemical composition, with no necessary symmetrical external form, and ranging in cohesion from loose debris up to tho most solid stone. Blown sand, peat, coal, sandstone, limestone, lava, granite, though so unlike each other, are all included undet the general name of rocks . Following are some of tho important terms applied to rocks : Sedimentary Composed of sediment which may bo either a mechanically suspended detritus such as mud, sand, shells or gravel, or a chemical precipitate, us roqk-ttalt or calcareous tufa. ,The various deposits which are accumulated on the floors of lakes, in river courses, and on the bed of the sea are examples of sedimentary rocks. Fragmental Clastic is composed of fragments derived from somo previous rock. All ordinary detritus is of this nature. Concretionary is composed of mineral matter which has been aggregated round some center so as to form rounded or irregularly shaped lumps. Some ndnerals, particularly Pyrite, Marcasite, Siderite and Calcite are frequently found in Concretionary forms, especially round some organic relic such as n shell or plant. In alluvial clay Calcareous concretions often take curious imitative shapes and are sometimes called fairy stones. Oalitic is made up of spherical grains, each of which has been formed by tho deposition of successive coatings of mineral matter round some grain of sand or shell or other foreign paiticle. A rock with this structure looks.Iike Ash-roe. Stratified Bedded is arranged in layers, strata or beds lying generally parallel to eacii other as in ordinary sedimentary deposits. Aqueous is l.iid down in water, c mprising nearly the whole of tho sedi mentary and stratified rocks. Uustratitled Massive having no arrangement in definite layers or strata. Lavas and the other eruptive rocks are examples. Eruptive Igneous is forced upwards in a molten or plastic condition into or through tho carth'b crust. All lavas are eruptive rocks; also called volcanic be cause erupted to the surface by volcanoes. Crystaline consisting wholly or chiefly of crystals or crystalino grains'. Rocks of this nature may bo either Igneous or aqueous or caused by sublimation, when the materials have crystalized out of hot vapors, as in the vents and clefts of. volcanoes. Glassy Vitreous having a structure and aspect like that of artificial glass, such us absidian. Porphyritic is composed of a compact or crystalline base or matrix through which are scattered crystals much larger than those of the base. . Many eruptive rocks have this structure and aro often epoken of as Porphyries. Schistoe Foliated consists of minerals that have crystalized in approxi mately parallel wavy and irregular lamine, layers or folio. Such rocks are called generally schists. They have in large measure been formed by the alteration or metamorphism cf other rocks of various kinds by vast terrestrial movements. VariousschenieHof classification of rocks aro in uso among geologists, somo based on mode of origin, others on mineral composition or structure. Accordingly in the following account of the more important rocks which enter into tho Htructureof tho earth's crust a three-fold sub-division will be adopted, viz: Sedi mentary rocks, eruptive rocks and Schistose rocks. Veins and dykes are a part of the evidence of volcanic action. "Wo have only to consider how they occur in connection with the protrusion of erupted material within the crust of tho earth. When the material so erupted has solidified inn vortical or nearly vertical fissure, so as to form ft wall-like mass, it is called u Dyke. Otherwise tho position of erupted rock that have consolidated in irregular rents aro known as Veins. Dykes vary from less than a foot to 70 feet or more tn width and run in nearly a straight course sometimes for many miles. They con sist most usually of diabase, and andesite, basalt or allied rocks. Like intrusive sheets, but in a less degree dykes harden or otherwise alter the rocks on cither side of them. Sometimes their sides are coated with 11 thin crust of black glass as if they had been painted with tar. This glass represents the effect of rapid coating. No doubt the whole rock of the Dyke at the time when it rose from be low mid filled tlio space between the two walls of its opened fissure was a molten-gla-jg. But inside this layer the molten rock had more time to cool. In cooling its various minerals crystalized and the present Crystalline structure was de veloped. Into tho fissures opened in the earth's crust there have been introduced various simple minerals and ores which, solidifying there, have taken the form of Mineral Veins. Theso materials arc to be distinguished from the eruptivo veins and dykes above described. A true mineral vein consists of one or moro minerals filling up a fissure which may bo vertical, but is usually moro or lesi Inclined and may vary in width from less than an inch up to several hundred feet. The commonest minerals found in these veins are quartz, calcito, barytes and floor spar. Tho metalliferous portions of ores nro sometimes native metals, but aro more usually metulic oxides, silicates, carbonates, sulphides, chlorides or other combinations. There appears toben.wno reason to doubt that tho substance deposited in mineral veins were mainly introduced dissolved in water. Not im probably heated waters rose in tho Assures and as they cooled in their ascent thov coated the walU with the minerals which thov held in solution. These minoral's may have been abstracted from the surrounding rocks by tho permeating water, or they may have been carried up from Borne deeper source within the crust. Now and then n fissuro has been reopened, as land shells and pebbles are found far down in mineral veins, showing that during the titno when tho layers of mineral matter wero being deposited tho fissures sometimes communicated with the surface. I IT IS HERE! I Hi Tlie Largest Stock iij Solitlj Isabel -CONSISTING OF- y Shelf and Heavy Hardware; Stoves and Tinware; Pumps, 35 fc: Pipes and AGRICULTURAL IMPLEMENTS! 3 t: Guns and Ammunition, Stttdebaker Wagons, r SZ Canton Clipper Plows, Harrows, Etc. 3 S For Miners' Sunnlies. the only house South of Portland. 3 5 v Give us a call. .31 ffiJ GRIFFIN & VEATCH, ' , g COTTAGE GROVE, OREGON. !!' ?T7Z . 1 . ... . 1 hi it iti tit m. jg til hi 111 111 111 ( nt 111 m