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<br />. <br /> <br />I <br /> <br />. <br /> <br />was, in the earli,)r report, estir:1'lted frcn the rel3tive procipi- <br /> <br />tation based on altitude. The runoff records for 1937 on East <br /> <br />and Middle Mancos Rivers, indicate a different distribution of <br /> <br />runoff, principally 3S between these forks. <br /> <br />In the following tabulation the percentage of runoff <br /> <br />from the severnl forks of Mancos River, r.s esti~ted in the <br /> <br />original study frOB the altitude-precipitation relation curve <br /> <br />GnU consumptive use, is contrasteJ with the percentage derived <br /> <br />frOB the 1937 recorcs corrected for diversions above the several <br /> <br />gages: <br /> <br />:Percentuge of runoff based on <br />:Oribin31 Study 1937 Records <br /> <br />Mouth of East Nsncos River <br />Mouth of Middle" " <br />Area between forks abOve [lnd <br />West ~lqncos River at mouth <br />Mouth of West Mancos River <br />by d ifferen ce <br />Mouth of West M3llcOS River <br />by altitude-precipitation <br /> <br />16.'30 <br />17.29 <br /> <br />21. 22 <br />12.97 <br /> <br />2.81* <br /> <br />.30# <br /> <br />65.51 <br /> <br />63.00 <br /> <br />Man c os e;.age <br /> <br />100.00 <br /> <br />100.00 <br /> <br />* By difference at Mancos ga~e. <br /># Calculated froD Gver~ge annual unit runoff <br />square mile, between Man cOS and Tov/'1oc, ,.. <br />of s~e average altitude. <br /> <br />of 30 acre-feet per <br />sinilar territory <br /> <br />Storable Flow at Weoer Reservoir <br /> <br />With distri~ution of runoff to the several forks at their <br /> <br />nouths, as c.eterDined frC!il 1937 records, the flow of these streams <br /> <br />'2.'3'2.6 <br /> <br />15 <br />