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<br /> <br />co <br />00 <br />("'J <br />-.j <br />("..;.) <br />c. <br />-, <br /> <br />~ <br /> <br />r- <br /> <br />,..... <br /> <br />-21 <br /> <br /> <br />j <br />.{ <br />'-'1 <br /> <br />.(d) <br /> <br />the Conejos by a suocession of years of low <br />runoff or by increased heavy withdrawals <br />from the artesian aquifers, or both. <br />Increased depletions north of the Con~dos <br />area by the reuse on new lands of return flow <br />whioh formerly may have reaohed the Conejos <br />above its mouths. <br /> <br />c j <br />','j <br />) <br /> <br />~~ <br /> <br />2. There is some evidenoe, although not conclusive, that <br /> <br />when the flow of the Rio Grande at Del Norte is below <br /> <br />r-. <br /> <br />600,000 acre-feet in a year, negative departures can be <br /> <br />