Albuquerque daily citizen. [volume] (Albuquerque, N.M.) 1895-1903, 1901-07-26

II WHE suspected that the owe OF
these, containing a considerable mum
her of limo strata i~ntcrbcdded with
marty shalc n sandstone u cap
ped by gypsifcrous shalc which at
times supports enormous beds OF gyp-
sum. might be equivalent To the miss
ing Pcrmian. Fun confirmation OF
this suspicion was secured when we
found near Tularosa. IN Otero county,
a magnificent series or charactorlstic
Perminn fossils. Another locality
cast Of Albuquerque mas also yielded
conilrmatory evidence. AS yet no
palContoloPlcal method has been
found for discrimination between the
Jurassic ana Triassic. thongh u
seems probable that the missing ovi-
dcncc will o q he forthcoming. Prac-
tically the rcd beds are among the
most important formations In the ter
ritory as they yield copper. gypsum,
alt and petroleum.
COPPER
II har"IS S''nls .uo nnu." W nuy
'hut me ''u p'un ~ u ,ua'
.ouICc vi ",nt'S az w '"ppvi " "
'~er'N'u,E' 'nS s."''nnon' "aS go,
7oIle"hat tWoepIhE anu u nnuH' w
'~onI'sh'u 'hnt " 'V9'S uIon u ~
lutlcal oasls' flrst, rs " uI''.t soul'r.
rue primitive conui,lun vi wv .olpol
w w tue io'm W su'Ph'ocs """ oN'u.S
'piacIns Vcsv,aplc ma.,e' ~ ~
Ia''s anu SunuH''m W - A.
ana .t'laaslc' inns oohu''lon 10
pe"u'l'u'y u'sp,aSc" Nv "oIa 'ouu.',
lor 'NarhP.', VIII VI nan' a
the neus OF f'rih'an WI" la1a,.
are 'i'cu 10 a Pcrpcnuivui" ~. a.
Wosu vi 'n, mola a"'v, Nv 80
itSelI chleny iorhieu vi cr,,n'coua
,trata' III 'he c~arpona.cous sn"'ee "
lnS 't"e' pc"a '" pu"''"'., ~
Stohes ouu,es '" oPpo ~
louhn III Sucn ap"nuanoc as " mnNo
,ohE scrNru 20 q ooul.. ,"pp,'
IN many taScS Wv oIs"niD W., w
ne or'siha' mass 10 py,i1
lztu an" PARTY ,"p,in' "" ,o
cuIrcncc :" 10 'nnpo'' q" ~
uahs 'anou ~
oN.r Il .n,so p"i, ~ H. ~
lo~ituna,elS III .n.s wa".iS %. n",
atcu s,n'c 'nc ooip,' 10 w. 80" :.
Hclchtly S~esr'E"'eu W W. p'oh'aoix
"u,hou .Nocpt ln.m"pa WI nan
Ssalc' ,no s'Ju"uy .'h uono
" coppeI ulc W loal'S ma.n ~,
lihpor'aN' u" ~ Sceiis ''''"i" tn"'
'n' E,va.'' pol''on ", ~ JoPP1 A."
u W'tnlh 'h' 'v'lIuoiy - ",I''cu
rom 'hc ma.''," picD'p'.atuu Wy ",
amt mu'''ul W 'noou asuiln'''"iy
7tIhta' me pIlnhal sou.o' ~ n'''u'
remains III any caSe uhvNplaiheu, ~
very interesting opJrct lesson as W
tue so'o,'aIS uVV"uiu'u.loh VI 'op'
per may ne seen III 'h' Hah NhhIcus'
Naballn OF san 'rlstoDai mountains
or Tor that matter lh'ahg oi inc
mountain ranges wherc the contact
OF the Superimposed stratlned rocks
upon the granite rs wen seen IN the
san AndreaS' Tor the eh'lre
thickness OF the carbohlterous ana
part oi the fefmlan rs iouhl lying
conformaDly on the granite anu warp
ing assures extend roush the IN
tire thickness 10 the granite contact
these assures nave Deeh hlieu from
above and rarely extend TO any as
lance into the granite. Al the srahlte
contact ~ n zone Where IRON ieech'
lngs from above nave FORMED n Ter
ruginous bed u Wherever the rs
sures eNtend To thls peit Oh Hoh-iih'
prognated congiomerate OF quartzl'e
there Is copper precipitation oiteh
hne masses OF copper slahce OF oNlue
occur mere put the eN,eh, OF tne ue'
post Is usuaIiy sirlctis ilihi'e" anu
not extensive u Is not nara 10 reau
the chemistry OF the depositloh Oh cop
per III the presence OF iron anu sur
phurlc hcld' "ner thc srahlto pou
rock forms n nasih the same principe
appiles 10 "a hlu'h more important nc
culnulation' nv may DC seen III the
San'h i','a o's'rl't, =,
icy ,h' prdctlc"' suo'"sIs' assn
munster "na' Woulu occur III case
.uprlle,pus SANDSTONE u shhlS o'
the leu p'ua were 'aush' up anu ~
oo~llo'a,'u ,hpic vi 'eaa NY III 'nc
nuHa u, a"uo''.a Nv S's1,lte ssnn.'o
Mnl.n alo 'n' S"'u anu S'lN', po"llnS
,n''uhlncs VI tho ioslpn "nu ne VII
20 ~P'Vp"lou w appIo,la,o 'no .uhuI
','us W Su'n nrh'ns lamps 40 'nosc
VI .nru,'uc :. 1"h oulo' ,n'uilu.
p"''nul",ly 70 ,oss " S'c .nut pot"
,n' t'u p'uS anu ,hc unuo''Slhs '"l
numerous nhes'ohes nav p'eh Hot
slhPly Pouctra,'u ahu uls'uipeu ny
~anu'sl'' "oMa uut III many pl"''S wv
o~rlElha' ,eulihch,a'Ios haNo peon
pIoh'h Ih,o iintihShtS iIohh 'hu slN,
VI p'a W 'nat vi slty DUN anu
nave Deen most intimately WlNou
WIN lhe Intrusive Quarlzlte anu
spar dlNes anu cohtact
uhder these circumstances nave Sc
oroe ovpp iohnnS IN r, ,bn -
| Violence of the proceeding has mill.
tated against the uniformity and the
consistency of the result. In one place