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<br />result~ng from high intensity rainstorms. The Purgatoire <br /> <br />River is the largest tributary of the Arkansas River in <br />Colorado. Records of the flow of the Purgatoire River <br /> <br />reflect the nature of tributary inflows as described above. <br /> <br />The only long term records of tributary inflows below Canon <br /> <br />City are those on the Purgatoire River. Even here the <br />records of the Purgatoire River at Las Animas are not <br /> <br />continuous during the 1908-1984 study period, and corre- <br /> <br />lations with other gage records were necessary to estimate <br /> <br />the inflow to the Arkansas River. A comparison of the <br /> <br />Purgatoire River flows with other tributary inflow for <br /> <br />concurrent periods of time revealed that the,Purgatoire <br /> <br />contributes more water than any other tributary. <br /> <br />Streamflow records for Big Sandy Creek, a major north- <br /> <br />side tributary of the Arkansas River below John Martin, are <br /> <br />available for the years 1969 to 1982. As indicated in the <br /> <br />U.S.G.S. remarks related to these streamflow records, the <br /> <br />Big Sandy Creek flows at the gage "are affected by diver- <br /> <br />sions above the station and return flow from irrigated <br />areas." Inspection of the daily discharge records iJ,lus- <br />trates these upstream effects. The records show that in <br /> <br />- <br />most years there is an unnaturally high increase of flows in <br /> <br />about mid-November and a sudden decrease in flows in about <br /> <br />April. Upon further investigation, it was determined that <br /> <br />these unnatural changes in flow are due to the operations of <br />the Amity Canal Company. In previous years, the Amity Canal <br />has discharged water into the Big Sandy Creek at a point <br />approximately six miles above the gage. This discharge is <br /> <br />-27- <br /> <br />OJ. ,,/'. <br />