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Show , and .' 1 6.000 aet'e:s ot land. Alimoulh 1 d!f'$iruge \la_tin (8J .$ .u$s) is 7' l_ger" Oom C!'flU i$ much small$r tor mogt ot tb$ eattmen:b' Qr$8 is lo'Wf;tl' and the a_. fio. i$ ,&ppnJd$at· 60% of 'h'ke aw .t efta-lt OHek .1" 21,OCO ,2 Com Cr$k is 'llsd to imga.t$ vW$_ 4'()O and 4,,00 aer$. , Qre ft$t. . tla$ M,a<blf .k daiM. bUia "$ ap_ot-el,. tea sqe miles, 'but it includes s$Wu high peaks. Meu:remen'bs Qr the now IJit MeadG'W Gl-$.t taken 19Uh sa. l'b; ,.hpw the di..ebarge to 11>. {)" .. 25!C of \bat or iMlk Ceek or 8,000 &er$ t'eet per 1e.' The flow of Me ONe-it, CO'tiblae.4, t tb«t of WalJt. $k. tipt-ee 1,aOO at in nQ year$. ,he sma.U6 st$ ant$4.' the velley are dry f' th,$ tb$ t,)t , --yon$' \0 ttUlt iftt.iOlr ut Ut ''W111y d'U pet ",r the year bu1i ther mAf, 110_ftr be eo_ now higtl 1)) tM )t()n$ yeqt.3; ding the ent11'fiJ '-uba.r:e, y'e PQund _ Qt tbfJ 'V&llelf 0'01#$ u$Ween the indi1ddual .... gTain$ of graitel. sandie silt _d clay Sedl"J;t,1 which ha1ffl oo(tl'l accumu. uting there i,hr9\1gh 'M ages:; \be dtb Qt the llOistwebean.n8 st"ata ranglng from 9. tew t.et on the alluvial slopes :n:ertr Rol4en4 to Soo teet :i.n the l pQ1"tions of 'he V'flUe1. lb••n4 ad grt".l bet\$ in th, valley s,ed.imen$ aet a$ ooxaduit4 tor the passage of _%> ires *0re 1t . ted t!"hi'l 1We ?$Ihl '9 lfet'a?Bl Srl 2 Offiae, WeshiBgton" Df a ., • iS" !;,Ieil.lZer f # UI'l:i;i;ad states hinting p. 2£ t13:"'" p. U. 2£. Qit;.,1 p. 91. _. p.,. 2.3. |
