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<br />drouth of such stupend-ous charactor that both baoins will have <br /> <br /> <br />to suffer. You havo torockon with that. On the other hand if <br /> <br /> <br />you take the 20 year record of the river. we are dealing here <br /> <br /> <br />with a very extrema situation a hypothetical.extreme. <br /> <br /> <br />En..1I0RVIBL, Th9-t's true. <br /> <br />. <br /> <br /> <br />. <br /> <br />lIR 0 I,IcCLURiJ ~ r:L'ha t if; my CtnswOr IJr, Chairman 0 Tho <br /> <br />possibility is so remote that California is not fearing it. <br /> <br /> <br />1m. NonVIDL, I don't know but I am unable to antioiputo <br /> <br /> <br />what intermountain diversion may bo m2de in the upper states. <br /> <br /> <br />I don't know exactly what the upper GtateG have in mind, but <br /> <br /> <br />using .the .past as a criterion, I imagine th8..t tllGY v"ill under- <br /> <br /> <br />take to reach the limit in intermountain diversion, and it may <br /> <br /> <br />be to such .a' point as vlould create a desporate. candi tion in the <br /> <br /> <br />lower division, This in addition to thoir full development with- <br /> <br />in the basing <br /> <br />1.lR.UcCLUIill, I cannot concoive that s\.lch a condition may <br /> <br /> <br />or will arise within any reasonable period, and the compact, <br /> <br /> <br />if made, can .cortainly be revised if ,.my such extraordinary <br /> <br /> <br />oatastropho should occuro <br /> <br />. <br /> <br />. <br /> <br />I:IR. CARPljlTT;m: Hr. ;Jerviel, the tendency of the peo];lle <br />belOW is to regard the border of the basin as a sort of <br />outer rim~ as the rim of a dish.. Tho mountainous aroQ,s are <br /> <br />largely interior mountain masses and it io physically impossible <br /> <br /> <br />to penetrate to this interior source if they wculd, and all <br /> <br /> <br />they could penetrato vlould be the mere rim. <br /> <br /> <br />.lill. NORVIDL: Then, I assume you will be willing to limit <br /> <br />. <br />. <br /> <br />10 <br /> <br />15th-S.F.-lO <br />