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