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<br />Endangered <br />Species <br /> <br />The Colorado Wildlife Commission has <br />listed the Rio Grande sucker as <br />endangered. The Division of Wildlife <br />is coordinating a recovery plan for <br />this species. <br /> <br />The silvery minnow is federally listed <br />as endangered. Historically, this <br />species occurred throughout the Rio <br />Grande Basin in New Mexico and <br />Texas. It now occurs only in the Rio <br />Grande downstream of Cochiti Dam to <br />the headwaters of Elephant Butte <br />Reservoir in New Mexico, about five <br />percent of its historic range. The <br />primary limitation to recovery is a lack <br />of perennial river flows in the middle <br />Rio Grande, diversion structures and <br />water quality. <br /> <br />Groundwater <br /> <br />The use of groundwater in the San Luis <br />Valley dates from the late 1800s, when <br />small-production wells were drilled into <br />the upper few hundred feet of the <br />confined aquifer. Since the 1970s <br />conjunctive use by controlled recharge <br />of surface water through ditch diver- <br />sions and well pumping from the <br />shallow ("unconfined") aquifer has <br /> <br />Compact Facts <br /> <br />United States - Mexican Water Treaty of 1906 <br />Guarantees the delivery of 60,000 acre-feet of water annually at the International <br />Dam at Ciudad Juarez, except during periods of extreme drought. Elephant Butte <br />Reservoir in New Mexico was constructed pardy to ensure the nation's ability to <br />meet this obligation. The Rio Grande Compact provides that the allocations of <br />water to the states shall not be increased or diminished by reason of changes in the <br />delivery or loss of water to Mexico. <br /> <br />Rio Grande Compact of 1938 <br />Establishes Colorado's obligation to ensure deliveries of water at the New Mexico <br />state line and New Mexico's obligation to assure deliveries of water at the Elephant <br />Butte Reservoir, with some allowance for credit and debit accounts. The obligations <br />are calculated based on a schedule of deliveries. The Compact establishes the Rio <br />Grande Compact Commission to administer the terms of the Compact. The <br />Commission consists of one representative from each state and a non-voting <br />federal representative. Several tributaries to the Rio Grande are not subject to the Rio <br />Grande Compact administraton. <br /> <br />Amended Costilla Creek Compact of 1963 <br />Establishes uses, allocations and administration of the waters of Costilla Creek in <br />Colorado and New Mexico. The Compact makes apportionments and allocations <br />among specific facilities. It is administered by the Costilla Creek Compact Commis- <br />sion, which is composed of the water officials from Colorado and New Mexico. <br /> <br />become the predominant method of <br />irrigation water management, particu- <br />larly north of the Rio Grande. <br /> <br />acre-feet annually, of which an estimated <br />800,000 acre-feet is from groundwater <br />sources. Approximately 3,500 of the <br />6,500 wells in the basin with greater than <br />50 gpm capacity are in use. <br /> <br />Source: Colorado Department of Natural <br />Resources and RGDSS <br /> <br />Irrigated agriculture is by far the <br />dominant water use in the basin, using <br />an estimated average of 2 million <br /> <br />Groundwater Source Unconfined Aquifer <br />in San Luis Valley <br /> <br />Confined Aquifer <br /> <br />Aquifer <br />Characteristics <br /> <br />40 to 100 feet thick <br />Unconsolidated alluvial sand and gravel. <br />Clay layers separate the aquifers. <br /> <br />Ditch and canal leakage. Percolation <br />of surface water from streams on alluvial <br />fans along the periphery of the valley where <br />the clay layers are not present. <br />Up to 1,500 gpm on the west side of the valley. <br />Typically 50 to 700 gpm in the central and <br />eastern parts of the valley. <br />Usually acceptable for potable use, although <br />in localized areas of the central valley, nitrate, <br />sodium, and total dissolved solids are <br />unacceptably high. <br /> <br />Recharge Source <br /> <br />Yield <br /> <br />Water Quality <br /> <br />500 to <4,000 feet thick and estimated to average <br />2,000 feet thick across most of the San Luis Valley. <br />Upper portions same as unconfined. Sandstones and <br />fractured volcanic rocks in deeper portions. <br />Deep percolation of surface water from streams on alluvial <br />fans along the periphery of the valley where the clay <br />layers are not present. <br /> <br />From 50 gpm to over 3,000 gpm in the southern and <br />western parts of the valley. <br /> <br />Typically acceptable for potable use. <br /> <br />Source: Colorado Department of Natural Resources <br /> <br />( Rio Grande Basin Facts - 4 ) <br />