New-York tribune., 1875-07-09

. CENTRAL Diffusion or SMALL q, tNIIritS OF
GnID .ViR \ LAE.F APEt-ONE-fUihp OF + T't
IIIIs CotFRlp WITH HEAVY 1lNBER-lHN SOIL
HICa AND DE' =. go 90
nm. Er,rdtti.a. .fnns ~
West Of the 10lth meridian and south oI me
~. parallel - latitude thH "'i,.i r'a rE'," m M
brGin- succeeded ly lni,,"n's ara siuc~ "i l,.',ic
az. , ,+ Is -.. r. ever ne older strata from
Wv E.st of the lO.ti meridian. m d. ia. - q
c-r.at development 81 hleiim'ipmc -la''' InlrA"'
and Granite. c0rttinIu- Numerous veins AMI hf'>,
OF ouarz and It is here thlf tAe mineral w'aih q" thr
Iii- il 10 be- sought for and found II u 'A' ~
p..k country is e. aracter.td ~ Ih1-rr 'l grant
~ .- and qliar'litr. tr.e.ug Il trom uJuh ~ soufh
, l,,rrtin., ~. N l.,e of solter sat- which have
Nm ,t,c..t b, dcuudaf.n .nd produced brufd. love
,. n alas, land hcf cen the I'nccoy red hills and
Si -. ... l.r.l'r ,a..- Numerous veins and gre
1i strata III m, direction ~ tlc "st.nr;' nlten iAe
m 80 - of i pranlfd lo-ccoiOI, and almost invariably
ol f,-c,- of IMMORAL uaticr. H. the taco~' siiis-
,.in. ~ llnone ifun of llor' or loss ncrmiNed VIA
't and ntr.,tz are or.. .ioaay faund bui i- they
,,'i .,, .oM / nave ho,n unable. - the
present time 20 detect At ia tuc m-s at nay d'lo-'''
hlonr ftrcu u.acr Lave lactci claims on tAe cree
hrle nn dln- lnd small .uice.. bat they nave n' cold
H. oN the result OF heir Li,o - 'i me refIt- ,n9
-ratci Tlcy port fr.ii 10 - cents To th' 'i hi
washed out uu buckets 81 ;hc average sra'c ' u"i 30
l. pan- with q roc.er anl oD,alnrd - scit- W".I
nf gold. or about six ., i'- "y' 10" ".rt
be- M the rae OF Ia cri.. u me PAU PAU
,holc hIi Niil Do much less than tLl'' 'h0-h IN cone
pla.es "a IT,. pu,il of catiN 'n Ne ~ fei ' 't' DE-
- t.f VII rc'd higher le,.dt-- Ac gold - 80 ''lli
,a aT.ff- with I.fc fiif dl@i accompany .h-
II and ..luW- nv ia, appearance tiat li i-- n'" lr'
nv b, te action 0i Na.r Nuf h most ri"np '''ii
l,rd rom quart veins n tue -lats 11oni iAr urad-
bnr ,n.rif -ion ~ small iiauiitlr- = E'! "trr
re-. ,r.I ,,nle tire action oi th" sto ans iia- lo' y
rn,,.rtls..,,l if 300 li.ll,cd ,uan.I h. and hAi7.
T,er,4 Is rDai srnoNerut age iiti saw it'lh-
t. Cetenuc beds of cirtaeeour -i its Nhrn "" i"i-
.r ,,.tiulf.ou. mal prove vlluanlr. There tr' 80
ts nf caylnn ere Cooi quality III tue lDri->ic -fH
I'm ii a. V..f.ln l4-. ol the hills. Prof Hayden mas
estimated fhlt nearly ono-thrd me "A"l' "'i ''",
.rrd " IN a heavy growth nf pine lumber aud should
ir,l.c his estimate have been carefully nl'r b. D. iN
minus ,oHderosd. known generally a. N"f"aN pine ana
T.,1 nine straight, Tree from iiii@ l"i
nu..ba'f their HIGHT aud viii furnish ioS' a''laflhg
,r,n ~ IA 20 iuchc. ~ diameter. aId % rf uolr h "a
i-Dsfu have tlces Along Tie .ic'" i~i'h-
ff rre 100 f.ci in hi-h and two or three tcci through
.ii. l-rnnud The wood - soft rfrdght. huI rather
,,I-,. Ia i. easily snt lat has uui 80 -f4t Trans
and oak lou ihe hauhr Of the eastern sittihs -nd h
tl. elevated northern portions 10. pnc la i.lr g.
,f.,el hV a tall slender nll, tDe', Used i5 tlr ~
,ii,n- dr Ind, pole. The hofs. of o." Ills - ni fl-
diaf. iu ~ character between tlnt m the VI ,si@-
mi Valley and the Elray Mountains, dtd piihir
~ .u. f,f each rc-pu hr~r 20 b" f0nud -rON .ir
ilc hv side The soil g.. rich aud deep and III the bot
TOMS alo.- tho small s tLtk AMI i'ti', olich
several erf n depth. Qrpdueiut urdFf growth or h"i
t,,,e. suitable Tor hay Along the hIlsidcs through
thc for-sts .ld even 1n tic m".uitih oY- "Hcic !h
rreks .re covered soil eo"i 1roWih ~ cAttl nt
rs s every where t0 be- found li tic shelter aU"rGcd
lt fhf Wofis anil dfep valleys makes THIS country a..
nj rnlly adapied for ,.och hgs g pnrposss Water oT
rxctllrnf dnIAB IL abundant, hne nptlng- are I" De
i,,tuo ai through tie hills aud since have beau ia thls
rt.eion we have experienced neIaent shOweis oi AIN