Albuquerque weekly citizen. (Albuquerque, N.M.) 1891-19??, 1895-05-04
COCHITI COUNTRY!
Veins That Go Deep Into Earth
and Are True tiSSureS.
With OultrOpS That Stand Out Boldly
iOr Two Or Three Miles.
AMI IN Places Afr from Ihlrb 10 rorN
test Wiig.
I'M SAY " AN OLD MtNIE

| ''N""'' )'""F'AG' l'''uly prepare,
several ARTICLES un the C,shtI country
And Am"ug them wAr tlr" -nhJmnr-i ~,
ucl" which IL clipped ir.m the lA.uyrr
C"lu., Mmug Record.
Bland tdy, y VI, AriI - rhr ore.
bearing I"iIy ritC Iu,kr 1T various y I,-,
rhua ~ her" miles ~ rLtrnt. tiimIul
/ llEh mountain I"AkH Aui rIIgrH, eat
lrrI IA NArt"ur dirretIuur ~ rAuuus aud
gurgrr, i"rin~I hy the recent rrurIuu ui
thr roi 81 pAitr 81 these r,Skr bS h,sSI
waters And streams Priur iut'.c -r,,riuu
That termed these Cautur IA some places
~ VOLCANIC s'ti"u, great brrAkr u,yut,
opening deep crrNIcrs Iutu the Interior 81
1h" earth thr"ugu th-s" upper one. bear.
iug rNkr. Through these cr-NIrrr NAHl
inAHf''r "i m"!t"u volcanic rrk matter ID
ru"h~d al, Aui, ia places, uvrItpwr aud
covers the I~rrhy rite r'ck WItnA CAP.
| l'lug, where 1t IN suIbIIhr,I aud now All
lrAiS ~ the iurin 81 u"n nrr. brArIu. rnC l
II a volcanic. hasRltlc character |, vac
probably during the second urhrnvAl 81
these Nulrauir r,rkr that the r-ntr ami
great crrNIo-r we're iurmci. caused by
earthquake nuiiuns; tnry nov aII-Ar ~
ia" oidrr p"rphyritIc rNkr which were
ere hearing
The crrNIcrp broke thrrugh the lsrr.
! rhyrItlc rugk ia n u"Tth"rly dlrrcliuu and
uuw appears ar tue hrpurr urr bearing
INNING VEINS. The VEIN hllIus 81 thrrr
usrurrH. or earthquake. formed cracks,
must have been d-rIv-i from the sur.
rounding rocks through the action IT
very hot waters which dissolve very
large percentage Of silica together WIN
| tue urrn II gold, rllv-r and other rock
material which, while IA solution, were,
carried hy the water into these veins or
rreNic-- aud there lett H. harden and
cry stAliIE" Intu the form IT VEN matter
n"w 1" hr seen after tue water ,vspur.
nted.
II these h,ctH. briefly prevented, are
true, then II In sale t. conclude that the
Ncinr, whether barren ~ rich ~ ores, ~
lerp into the earth. AMI are true NsHurrp
"i great extent instead at surface runtrar
tIuu cracks or shattered cracks IA the
ruckH ui slight extent AMI depth
Now. let ~ r''r what the tActr pr-s-ut,
| 80 LAT 49, development hAH guus IA uu
some at the principal VEINS aud pros
l-ctr, and th'-- also, that can l,r deter.
mined by nHturr'r dIgging Through Tia.
erosion 10y water hundr-iu at feet d,..l
down scru-- some uf thrr vans g. the
bottom "t the dr-J-rt rauonc.
som" ~ VI" principal VEINS show their
VEN or"'h"Af'hs lnn''rr cropping h"lii!
IA plaza, Que, twu and three mice ia
i"hf.h' hfth anu south, ia" vrin mat
ter hring largely hAri, whitirh. chiya-
lAiihr quartz, ~ ~hich tue valuabl" Gree
ARE d'sS-nihs,'~i Tins wA- uu, rn
easily attacked by tue elements Nui
"rUied away As Mas the Euii-r country
iock on either rId-. 80 ia ron- pAc-r Il
stands nut III ridges ten ar hil--u feet
above the enclosing wallis aud FROM ten
!" tlt--n ~ more feet IN Thickness
Tins VEIN matter, n-,m-tiu-a, IN plnc.r
reaches u width h-tw-.u tr walls. Of
ron thirty To- forty feet
The I'Ay ore ~ far M ,i-yrlui.,I sh,,.
un the suriAcr, sud IN ia. Crrun p,,,,,
! cue Star, Washington. AlL,tu.,l,. Nh,
other prominent pr'p,+,.t-. Il. ,rr.,.,,I.,
distributed Throughout IA. uu,rL mai
other gAnyur matter uf ,L. v.,,a f.,
rlAcr. II IA fnuud we'll r,u,.u,r.,..J -
~ uth-rn thin ar lean
Ennnyh work h.. L..., ..,.,.,...
lh,u ,h. ,,,h ,r,.. 80, .,,,,,.'..
rirL and aIund.n, ,n,,,,h -, ,,,.,, Isl!
IA th,. "a hrI,. ~ ,L.. ,,,i, ." WV
I.. moved In,,,,, ,h., .,'I''.,,' ""' h".'
warrant r,rh r,,n,n 49, W
ryr dryrIn,,n,.n, '' 'A"''
An,l,,., r,,,,,,',
II ~ Ia "a n., ,..,, I'll 49,, ,rI."N
,ll,rr ,,u.,',,n.n -, -.
AssF las 4.