Show LIP san c playgrounds 1 1 OF AMERICA by Q R 1111 MOURN chief uttam af BENJAMIN nR NJAMIN wet wee we e 1 8 sill fill alive and rould could bring his bij kite kilt und and ley and slid wet silk 11 thread to borne some comen of el fri thas hie file contrast nf of ages afi ftp ep edited ted would ain lindly gt a gimik share of the lie headlines hut but la in glacier mon lion tana tans there Is juil just tenil surf urt of a with 3 rather linn than men in ihli this dratwa of incon cel vable age at least eighty million years no ago ac conlIng to it e geologists a of mck etmus i lot allAg sometime sometimes feet la in lis formed in that region bj by sediment al lowly fettling settling to some now long van vanished 1 ailed bot bottom tonit all Allt title lile llan fw cross sailon ie Is nog known As al guu klan strata all on the very holtom of it 11 wits a ewt layer of aleso Il MoM r A y faint blue in color but W e it tile rl ng to a yellow 71 ese Alcon Algon kinn klan rod aleo also oc 00 cir in he lite grund road a and 1 new neier hae lime been revealed theo thee except for the IN clef that flint the file colorado hier peeled that partle ular spot not to dig the file world s biggest hole aut in file lie C anjer no fer park region there was a perhaps still till stronger circumstances a bulging bulgin 9 and crackling of the whole alkon klan section with as i a climax an overlapping cow called the th awls thrust this whatever ivha lever the reason or exact do de falls of tuch beh 1 I r pl e ed the ailyn allyn limestone the lowest widest and therefore pr estimably the oldest if of the whole e eighty million nill lion jear old Algion kiltin family fin on top of atch newer so jojn ger rock lint flint hail it just u lout loul breo been luc the surface of HIP 1 e larth arth atti ero eroslow slot by and tern pern ture fure ch chandis angis so i well ai as by water alfr ur or glacier Kl afler the front of lite lie oveil arping layer Is simala ao 10 but constantly until the tile aged allow bottom layer may now he st en high on tile cliffas along the tile eastern edge of the fit park purk ar or well ae as tin kerfoot at of nally glacier two pire elre and oilier other biln nearer the ite divide bu the erosion has been I 1 that hat which wore a gap in the yellow ler laver to the tile northen and left chief bounin in a lefoot foot silhouette there slone alonea a sullen unflinching of the ear it II 11 cor C or hereabout astride the he youn 7 feat plateau formed speck by by a 8 patient A 44 2 il 0 J of ft chief mountain 0 ocean cean through thousands of later centuries chief Is a tooth shaped preempt tous will yellow monster guare jIng the northeastern corner comer of the park it inny may be seen by every many glacier visitor from I 1 hyvl htway aay amar lower st mary lahe otril or ohN and those riding arc d babb to the canadian boun boundary dAr get many lews of it or it may even be i glimpsed b by Y westbound west boand passengers of the grairt NO northern Ncr thern railway a few roles miles beford the glacier part park station Is reath renard d another int rostin feature of tile lie glacier mountains is that many of tl ra 19 wear 0 unique black stripe this is s a diorite layer from 50 to feet if hick lick which tell tells a story of some fIn indent clent lava intrusion into the sedimentary rock sometimes the adjo adjacent ent alaers are whitened as if it burned to ash by the he laia laa vave and ripple marks of some prehistoric sea are also frequently encountered on be the glacier cinder park mountain sides M u 1130 11 N estern et News union |