Alamosa-La Jara Water Users Protection Ass'n v. Gould

674 P.2d 914
CourtSupreme Court of Colorado
DecidedDecember 5, 1983
DocketNo. 80SA288
StatusPublished
Cited by29 cases

This text of 674 P.2d 914 (Alamosa-La Jara Water Users Protection Ass'n v. Gould) is published on Counsel Stack Legal Research, covering Supreme Court of Colorado primary law. Counsel Stack provides free access to over 12 million legal documents including statutes, case law, regulations, and constitutions.

Bluebook
Alamosa-La Jara Water Users Protection Ass'n v. Gould, 674 P.2d 914 (Colo. 1983).

Opinion

DUBOFSKY, Justice.

This is an appeal from a judgment of the district court for Water Division 3 (water court) regarding rules promulgated by the Colorado State Engineer1 (proposed rules) [917]*917limiting the use of surface and underground water in the San Luis Valley. Curtailment of water use in the valley is required by the terms of an interstate stipulation under which Colorado must meet its Rio Grande Compact (compact) obligation to deliver scheduled amounts of Rio Grande water at the Colorado-New Mexico border on an annual basis. The dispute over the proposed rules concerns the distribution of that curtailment: between Rio Grande and Conejos River water users, between Rio Grande mainstem and tributary users, and between well owners and surface diverters. The water court approved rules for administering separate obligations for deliveries from the Conejos River and the Rio Grande mainstem, and disapproved rules which phased out all wells in the San Luis Valley unless each well owner could demonstrate a lack of material injury to senior surface water users or provide a plan of augmentation to replace the water taken by a well. The water court also held that the compact applies to all tributaries of the Rio Grande. We reverse the water court’s tributary ruling and affirm its separate delivery and underground water rulings.

I.

The San Luis Valley in south-central Colorado extends approximately ninety miles from north to south and fifty miles from east to west at an elevation varying between 7,500 feet and 8,000 feet above sea level. The major mountain boundaries are the San Juan mountains to the west and the Sangre de Cristo mountains to the east.2 The Rio Grande mainstem rises in the San Juan mountains, flows south-easterly through the valley to Alamosa, and then runs south through a break in the San Luis hills, which border the valley on the south, into the state of New Mexico, then along the border between Texas and Mexico, emptying into the Gulf of Mexico. The Conejos River rises in the Conejos Mountains to the south-west and flows north-easterly along the southern edge of the valley, joining the Rio Grande mainstem at Los Sauces. Despite its high altitude, short growing season, and average annual precipitation of only about 7.5 inches, the valley sustains a productive agricultural economy dependent upon irrigation water.

The upper 6000 feet of fill below the valley surface consists of unconsolidated clay, silt, sand, and gravel, and interbedded lava flows, containing an estimated two billion acre-feet of underground water. Some of the underground water is in an unconfined aquifer system at shallow depths. Beneath the unconfined aquifer are relatively impermeable beds of clay and basalt and beneath these confining layers are substantial quantities of water which comprise the confined aquifer. The confining clay layer generally does not exist around the valley’s perimeter, and the confined aquifer system is recharged from surface flow to the underground water system at the edges of the valley. Because the recharge areas are higher in elevation than the floor of the valley, the confined aquifer is under artesian pressure, resulting in the free flow of water from some artesian wells and springs at natural breaks in the confining layer. In some places, where the confining layer is less thick and more transmissive, water from the confined aquifer will leak upward through the confining clay lay[918]*918ers into the unconfined aquifer. The unconfined aquifer is directly connected with the surface streams in some places. To varying degrees, the surface streams, the unconfined aquifer, and the confined aquifer are hydraulically connected.3

The first appropriations from streams in the valley began in the 1850s on the Conejos River. The first appropriation on the Rio Grande mainstem was in 1866, and the most extensive development for irrigation purposes on both rivers was between 1880 and 1890. By 1900, the natural flow of all surface streams in the valley was over-appropriated. High spring runoff and low summer flows in valley streams, coupled with years of severe drought, resulted in undependable water supplies for irrigation; thus, farmers turned to wells and reservoirs to supplement and regulate their water supply.4

Well construction in the valley began as early as 1850. Between 1880 and 1891, about 2,000 artesian wells were drilled. Withdrawals from the confined aquifer by wells remained relatively constant until the early 1950s when a number of large capacity wells were constructed. In 1972, the state engineer ceased issuing permits for wells to be drilled into the confined aquifer after determining that both aquifers were tributary to the surface streams in the valley, based on studies by the United States Geologic Survey and state water agencies. There are more wells on land irrigated by surface water from the Rio Grande main-stem than on land in the Conejos River Basin because many of the Conejos farms are too small to use sprinklers connected to wells and wells in the Conejos River Basin west of Antonito must be drilled to such depths that pumping them is uneconomical.

Since before the turn of the century, valley water users have had to contend with out-of-state demands for Rio Grande water. In 1896, complaints and claims for damages from the Republic of Mexico led the United States Department of Interior to deny permission for the utilization of federal land in the construction of most reservoirs planned for the valley. The dispute with Mexico was resolved by treaty in 1906, 34 Stat. 2953 (1906), but the next year, the United States Supreme Court, in Kansas v. Colorado, 206 U.S. 46, 27 S.Ct. 655, 51 L.Ed. 956 (1907), articulated the doctrine of equitable apportionment, opening the door for the assertion of justiciable rights to Rio Grande water by the states of New Mexico and Texas.

To avoid litigation, Colorado, New Mexico, and Texas began in 1923 to make efforts towards a negotiated apportionment of Rio Grande water. Negotiators from the three states signed a permanent compact in 1938. The compact subsequently was ratified by the legislature of each state and approved by the United States Congress in 1939. 53 Stat. 785 (1939). Codified at section 37-66-101, C.R.S., the compact obligates Colorado to deliver water in the Rio Grande at the New Mexico border based upon two schedules tying delivery obligations to levels of inflow, as measured at upstream gauges on the Rio Grande mainstem and the Conejos River, to which is added the flow of the Los Pinos and San Antonio rivers (tributaries of the Conejos) measured near Ortiz, New [919]*919Mexico. The amount of required discharge varies according to natural supply. In low water years, small deliveries are required; in high water years, large deliveries are required. The compact fixes Colorado’s overall obligation in the equitable interstate apportionment of the Rio Grande at a level intended to protect water use as it existed from 1928-1937 (the compact study period). In recognition that variations from predicted performance for each river would occur in the future because of the sequencing of wet and dry years, variable runoff patterns,5 and new depletions, the compact allows accumulated debits up to 100,000 acre-feet. See Article VI of the compact.6

Beginning in 1952, Colorado accumulated debits in excess of 100,000 acre-feet.

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Bluebook (online)
674 P.2d 914, Counsel Stack Legal Research, https://law.counselstack.com/opinion/alamosa-la-jara-water-users-protection-assn-v-gould-colo-1983.