Simpson v. Cotton Creek Circles, LLC

181 P.3d 252, 2008 Colo. LEXIS 283, 2008 WL 756752
CourtSupreme Court of Colorado
DecidedMarch 24, 2008
DocketNo. 07SA42
StatusPublished
Cited by13 cases

This text of 181 P.3d 252 (Simpson v. Cotton Creek Circles, LLC) 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
Simpson v. Cotton Creek Circles, LLC, 181 P.3d 252, 2008 Colo. LEXIS 283, 2008 WL 756752 (Colo. 2008).

Opinion

Justice RICE

delivered the Opinion of the Court.

I. Introduction

This is an appeal from a water court's Findings of Fact, Conclusions of Law, Judgment and Decree ("judgment") upholding rules related to certain new withdrawals from the confined aquifer in Water Division Three ("the rules")1. Appellant Cotton Creek Circles, LLC ("Opponent") asserts that the rules are invalid because they are contrary to statute and violate the Colorado Constitution. We disagree, and we affirm the water court's judgment upholding the rules.

II. Background

In order to adequately examine Opponent's challenges to the rules, it is necessary to understand certain background information. We first discuss the sources of water at issue and the historical treatment of that water. Next, we look to the statutory authority for the rules at issue in this case, the substance of the rules themselves, and highlights from the water court's judgment upholding the rules. Last, we review key sources of law underlying many of Opponent's challenges.

A. Overview of Sources of Water Implicated

The rules at issue apply only to the confined aquifer in Water Division Three, which is generally coterminous with the San Luis Valley ("the Valley")2 See Alamosa-La [255]*255Jara v. Gould, 674 P.2d 914, 919 (Colo.1984). This court described the Valley previously in Alamosa-La Jara v. Gould, noting that it is located in south-central Colorado and extends about ninety miles from north to south. Id. at 917. We stated:

The major mountain boundaries are the San Juan mountains to the west and the Sangre de Cristo mountains to the east. The Rio Grandé 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 northeasterly 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.

Id.

The Valley contains underground water in the form of a confined aquifer and an unconfined aquifer. Id. The unconfined aquifer lies above the confined aquifer, and it is directly connected with surface streams in some places. Id. at 917-18. Below the unconfined aquifer lie "relatively impermeable beds of clay and basalt," which separate the unconfined aquifer from the confined aquifer. Id. at 917. The layers of clay and basalt do not exist around the perimeter of the Valley, and so surface water recharges the confined aquifer system at those edges. Id. In addition, we found:

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 layers into the unconfined aquifer.

Id. at 917-18. As a result, the unconfined aquifer, the confined aquifer, and the surface streams are hydraulically connected to varying degrees. Id. at 918.

Opponent argues that there is another source of water that should be taken into account in the rules. That water comes from the unconfined aquifer of an area known as the Closed Basin. A federal reclamation project called the Closed Basin Project has for decades "salvaged" shallow groundwater from the sump area of the Closed Basin that would have otherwise largely been lost to evaporation and evapotranspiration. See Closed Basin Landowners Ass'n v. Rio Grande Water Conservation Dist., 734 P.2d 627, 629 (Colo.1987). Wells completed in the unconfined aquifer in that area provide the means to divert the salvaged water to the Rio Grande, which aids Colorado in meeting its obligations under the Rio Grande Compact, which we discuss below. Id.

B. Historical Treatment of Water at Issue

According to the water court's judgment, there were already 7500 flowing wells in the Valley by 1958. Construction of wells in both the confined and unconfined aquifers continued until 1972 when the state engineer imposed a moratorium on new well permits, with the exception of permits for the unconfined aquifer in the Closed Basin. In 1981, the moratorium was extended to include the Closed Basin as well.

Administration of the water at issue is complicated by the existence of the Rio Grande Compact.3 The compact was a resolution of competing claims on water from the Rio Grande by Colorado, New Mexico, and Texas. Alamosa-La Jara, 674 P.2d at 918. In 1939, the legislature of each state ratified the compact, and the United States Congress approved it. Id.; see also § 87-66-101, C.R.S. (2007). The compact requires Colora[256]*256do to deliver water in the Rio Grande at the New Mexico border, though the precise amount varies according to schedules related to the natural supply of water at that time. Alamosa-La Jara, 674 P.2d at 918-19. The compact allows for accumulated debits of up to 100,000 acre-feet. Id. at 919.

However, beginning in 1952, Colorado accumulated debits beyond its allowed 100,000 acre-feet. Id. In 1966, Texas and New Mexico brought an original proceeding before the United States Supreme Court in an attempt to force Colorado to repay its debit. Id. However, that court never issued an opinion on the matter because the three states together signed a stipulation that the litigation would be stayed if Colorado met its delivery obligation on an annual basis going forward, and used all available administrative and legal powers to assure compliance. Id. The United States Supreme Court granted the motion. Id.; see Texas v. Colorado, 391 U.S. 901, 901, 88 S.Ct. 1649, 20 L.Ed.2d 416 (1968).

As a result, since 1968, the Colorado state engineer has been administering the Rio Grande mainstem and Conejos River on the basis of projected annual runoff, and water users have had their diversions substantially curtailed. Alamosa La Jara, 674 P24 at 919. In 1975, the state engineer promulgated proposed rules that applied to Water Division Three. Id. Among those rules were some pertaining to the use of underground water. For instance, the rules provided for phasing out underground water diversions unless the water user submitted proof that the well was operating under a decreed plan of augmentation, or had a decree as an alternate point of diversion, or that the use could occur without impairing the right of a senior appropriator. Id. The rules went up to this court in Kuiper v. Hogenson, 196 Colo. 197, 583 P.2d 910 (1978), and were remanded back to a water court. That water court disapproved of the rules, holding that section 37-92-502, C.R.S.

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Cite This Page — Counsel Stack

Bluebook (online)
181 P.3d 252, 2008 Colo. LEXIS 283, 2008 WL 756752, Counsel Stack Legal Research, https://law.counselstack.com/opinion/simpson-v-cotton-creek-circles-llc-colo-2008.