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<br />". .' <br /> <br />Approximate Arcas of Ground"oater Reserves <br /> <br />The physical boundaries of the deltaic aquifer comprise <br />the Gila Mountains on the-eastern side; Sierra de las Cucapas, <br />massiff on the western side in Nexico; and the Cargo Muchacha, <br />Chocolate Mountains and Laguna Hountains form the northern <br />bloeks (Figure A-6). The apex of the delta lies north of Yuma <br />in United States and from this apex the materials thicken to the <br />west and south"ard. The southern boundary of the groundwater <br />reservoir is the saline-water interface which occurs south of <br />the 32-degree parallel. <br /> <br />In gross aspect, the ground.,ater reservoir extends over an <br />area of approximately 2,800 square miles; about one-third in <br />the United states and t,,,o-thirds in Mexico. Based on available <br />data, it has been estimated there are more than 300 million <br />acre-feet of recoverable usable groundl,'ater in the vast sub- <br />terranean systcm; approximately 100 million acre-feet in United <br />States and 200 million acre-feet in Mexico. <br /> <br />I <br /> <br />Usable Recoverable Groun<h,ctter <br /> <br />Area <br />(So. Hiles) <br /> <br />Reeoverable <br />lia'ter <br />(Hillion AF) <br /> <br />Economically* <br />Recoverable <br />lia'tcr <br />(Hillion AF) <br /> <br />Percent <br /> <br />United Statcs <br />Arizona 460, <br />California 1160 <br />Sub-Total 920 <br />Mexieo <br />Sonora 1,080 <br />Baja Califol11ia 790 <br />Sub-Total 1,670 <br />GIlAN]) TOTAL 2,790 <br /> <br />55 <br />55 <br /> <br />30 <br />30 <br /> <br />50 <br />50 <br /> <br />no <br /> <br />60 <br /> <br />100 <br /> <br />135 80 60 <br />90 55 40 <br />- - <br />225 135 100 <br />335 195 100 <br />*600 It pumping lift <br />