, 1869-09-13

nnIy II rrhefttAnd The tr7tc atafe n! n'fafrs In
Eastern aita io n.aii thcfn.e!srv II opre mid
tnsycr ot tht Advantages Arising from euf1fus''F-
e!al InterronTr With tho nlrtad1 lara. end faHlh-
II Increasing population of tnas region. Willie
our pterlr Etrl that llai n!fect!uu fur san frsu-
tuur1e Htrdrffi rumru!aurt from coin 1lou ts'ls-
t!un,. they mr. untrr tn obligations, financial nj
t'thffwtsr, IN TIM rtuut trrru of thr ueei1ehf,
HHi ate hot lnsthrii1e 10 ttrir own tnterchtA.
virginia tn! snd t1off Hin, thc r1'rlnE towns
Of tht coE*oek. have ernt1tsufei millions 10 THE
Wealth If Fan Ffnnct.ru merchants within the
rast s!S frssr, thltHEe Ii nnw IN f't~tirn tn
,Htcn,stti ttt tsnas n the inf tt.hr, art tn.ttt
~Sttttsffs silver tunts tsFipn Of Eastern Ne.
satn. III I.+t mt 1tte ',.r Hight urt-r trs*,"t
TT ,,a r'nn's Al lit t,''hts II Thi'r r.nr Ina.
ftrt FtrthHs 10 a-}trtkl'ts 1rst N. tltatrf-! rs
nhtrawt' srtsi +" II f,,+ ttttie m N1tir Il n In.
'att'l. ~ II. tht't. rtn-s IN III" astft.s''s
n1r NJ ttfpir's, rtts El.trH t~ta fht rrttt'r:
thl* stthlri if"st I'm IN trtsh is,ilIn4s rth'-t
IN a"tttr, st",t tbs h'ss lhlLs te~'s 1t thetf
rrsthr 4h.t ahi f"t tilht - sanh tttt"is ~ t,ss
th.sh-t4h !"''s.l t .i"sI.s ". Hss1 s*-f II s-st.s
ttl.I1 &ih. htA 1+td+lE4 .IiAF kirs 1sIs II n HH
tthG ts.IathHE.t, tht1a hL5a ~ jlAstH ittttEt ~
lle ilsttl al NJ sha ttEAL1 I3i"a IttsFt &FG tt+t
NAL tsAity lid ntr Hkn, VIII pay, III t"tti Isrs.
is"in e%s III tl,p" teE Inn. tbs ta'Mst"hh ',Ics
til If ltnm t# IN tIfs Iba TON; Mh'ls !!ha hAs LII
Lesh milling trG that IN shTt u alIHI tf"F Iku
II A~nn lHat II wu,ll1 hat Jay ut tiE pscse1t lirTe
uf MlIi,htf aI suns Of II Auus ~ ltF'4 ~ aa!""
IT I tan. Ihu a,eIa4u ,ttLi Mpw"sGr. IL 3t"iat
sIa4 PER till, whlll ll,at VI lhr tot!si"rL IL
&f,n11s ia. 1hu mancJ spent for t'u'f'er1ns Il
taiHAlhck AllIo would nlaAu \ lAnts"iHo tHE'
time tl'r ,luten st1xthhle3cts: TN tlTa'a.Es
atu fr,tttlEth III nut tAIhss. hJ MILL rfntrka
the nrns ii ir t'atnsk }tlti fh aE cant 0f nAAaI
nun yield fun. ~ III W Thu Cunstork ore.
ts.r1t s,f amin FDf ufI
occasionally n1i,r, tnyt thrr with irnenc ani n
| r.,usIdcrAnls percentage u! HnId; ttoss ot
TIeuu.r It'll asr tingularly tfr' from oil rHc than
uAthu xrcr hutl its Rats. aIi tnassra Of rcsaFJ-
r,'r. 1f.asutc II Eisvn 9,sh feel alroyr tho cye!
III the hru, aui ia ikh1str mountain, noul I've
rlr% from 1nss> tn lssc nnrt Mil k,uth nni VII
nni hall niIcs east aud wrist, separated hy 4
deep rnEun sruns q 1'wrr range of mountain. u
ct,iznotc sUrant,n IN tho cast, with Cations lcat-
!nH v1 from Isa northern and southern t,asc
" the Crtscrn.tlap*d sn'lny, which pasnca to TIN
wrst untt uiakca \ t'ciuuf arounI White I1nr
MuuEtaIn, which In wpAruirh fFon 1Fchsu7r I'LL
ty = trt'r Canon. Tho foot hills sloptHg from
White 1'in1 Mountain twhIch II ro,9-a feet htGt}
awxth Ttrasuru 1!lll cunhItsIin what II known ~
| tlr Iasr Metal IsanEr, which holds labyrinth of
stlls curs.Iux vaIctA aud hIlsct. The orva ot ths
western hniA' Of this Innuntuln arc l,ui little mixed
with 1,aSe MtlaI, a,ld can 10 reduced ~ mill but
tnlt Thesa. mines have aitEartci l,4t Iitt III
ton ~ yet, owing to trlr r1om rfnxI'n.tY to shc
| richer md free orr4 Of Trr2yurc Hit: but FROM
| developments AtrraitJ nsa3c, anl tusfactl In the
prcActIan that tho Base Metal Raugc HiI aid
.nsi!uus to the ~eslth Of White Pine
Starting few !.uni,rrt1 iret !rum tho highes
| peak of Treasure IiilIt and doping Rradnalis Il
,h- wert, hre ihrre tat., known as 1,rotntttc
Chloride aud ro1onIn Tor "rahgoneup," III,
Shoshcnc for clouds, whtrh chasr cnch other nun3
| ita smooth. limestone surface all w1nter). The,,
| fats present The nost 1,u4F Scene IN nur mines
The Gre here lies In hoEizonta! Gesis, generasi,
c3pne. With limestone, but IN soulc Instance
rising to the suIiace. These beds or la5ers Of ore
yasy In thickness from IL 10 81 feet; below then
emooth limestone Il encountered. The Eenese,
Shaft Of the Consolidated Chloride Flat Compan
has penetrated ore to fhe depth Of lis feet, meet
ing with no Intervening sheet OF limestone; til
! Eclipse, oil bromide Flat, Funk through 26 feet Q
ORE, shcn through &c feet solid limestone
an,l struck tho Eecont bed o? oTc, ,
feet thick, nnd of high grade: the Soooda5, I'll
| Rame nat. yet with sltniIar results bs passtnI
| through twenty-five feet Of limestone beneath til
| rrfi led Of ore. These are Characteristic feature
Of the uii1c. nj Chsna1cillo, chi,t. while o7tsld
Of thesc mats the whole mountain, t'eara d chs
rekeMfta tancc lii cycrJ particular to tha. Of rotos
TN tue s!oTes Af the mountain veins Ot lrfHcs
Met xith dipping towAtd the centre 6f tile hill 9
various arge<. The Will. vi the Ebcrlarslt vel
ntc ntsIly vertical tD depth Uf 9s feet, aud Al
la.. lee. apart; the California lips a5 deg, nil Il
| stn In II feet wide. All tho ORE az we'll rs II
enurtty rnck, 1. extremely harf, aud ererJ fool
pingrcsa Il rnate ht busting. the thunder
which Is ince5sant. trcluttns the tnlue. lsra.t
IT, til" Fa-r Metal ltaner, there atr nrrard
e,Hn ftcufdril tn tfIc district
+ Treasure Cltf IA situated on tnr of t'c n1nH
tain, hIluiV ntrl AVER ttIc i1uea, A'Ll has thr.
tnlhR t'7n exrEtss n.fares. twu churches Il la
t~l,r. I1I'tiIr rcl""'. Sabbath srhnn'+ ltnIri
Trustees. pnth = inti" nHl n t'T t'frAplrrHnlta
n wrtntrnnI7,t Il hn,1 wrlt-vnsrsiIth tttE. r.
tn,ntnr rfr"Ifs MFr krrt here. hu III" MInhg II
| rtf, + nrt'nns '1"I,Ittsa tn al'rn1 in The WAL
nt trr f.tr1r NJ IN" tttrr Turns vi the tiFet1l
The uNft1 tnIta ntt frult ntniii1 II" Inns" Ut Il
t,ntnln,n At 1fnt.1tttnH, sntlshr. thrrfnantnw
Et.tfnrti tltt R'l nl"t't t''sslt thrrnh-atl MI
IN tnn (l' mi 1trs.te CUR.
tnHA t. t;IHs,
slnIrr t'fi'pr VILLA 1',Ne Uti't ,t'-
/ A. huthti l