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<br />.~ <br /> <br />\ <br />,c <br /> <br />~ <br />r~ <br /> <br />, <br />~.. <br />, <br /> <br />, <br />~ <br /> <br />, <br /> <br />~' <br /> <br />~ <br />t".... <br />~\.t <br />('1 <br />l.,_~) <br />c. <br /> <br />supply and drainage system, is not less than 500,000 acres. As the <br /> <br />so-called trough of the valley is well over to'ViD.rd the base of the <br /> <br />Snngre de Cristo R.onge on tho <lastern side, the bulk of the land lies <br /> <br />to the west and northwest. <br /> <br />Irrigation has depended on the use of the ",ater of local <br /> <br />strea.ms of the basin and on large di versi ons from the Rio Grande <br /> <br />into the southwestern part of the irrigated territory. <br /> <br />The history of the dovelopment is interesting. Tho first <br /> <br />area irrigated was along tho Alamosa-Salida r~ilroad line, in the <br /> <br />lower part of the trough imrnediQtoly west of and parallel to the <br /> <br />natural seeped area. In this section of the basin a broad belt of <br /> <br />land was rapidly brought under irrigation. Drainage difi'iculties <br /> <br />soon developed that led to progressive abandonment of lands along <br /> <br />the eastern border of this ir6gated zone and to its progressive <br /> <br />extension westvmrd. As years went by, this progressive shifting of <br /> <br />the irrigated zone westvmrd continued lmtil its western margin had <br /> <br />reached the extreme west side of the valley and the broad stretch <br /> <br />of once- occupied lands to the eastward was left to revert to its <br /> <br />original state, badly damaged, ho.rever, by alkali. <br /> <br />Drainage of th e y'restern area then be~me necessB.:F\J I and. the <br /> <br />,'mters developed thereby aided in a progressive reoccupation of a <br /> <br />part of the neighboring lands to the eastvmrd that were once occupied <br /> <br />and then abandoned on account of becoming ,"mter-logged and affected <br /> <br />by alkali. <br /> <br />5 <br /> <br />L <br /> <br /> <br />