Northport Irrigation District v. Jess

337 N.W.2d 733, 215 Neb. 152, 1983 Neb. LEXIS 1233
CourtNebraska Supreme Court
DecidedAugust 12, 1983
Docket82-378
StatusPublished
Cited by10 cases

This text of 337 N.W.2d 733 (Northport Irrigation District v. Jess) is published on Counsel Stack Legal Research, covering Nebraska Supreme Court primary law. Counsel Stack provides free access to over 12 million legal documents including statutes, case law, regulations, and constitutions.

Bluebook
Northport Irrigation District v. Jess, 337 N.W.2d 733, 215 Neb. 152, 1983 Neb. LEXIS 1233 (Neb. 1983).

Opinion

*153 White, J.

This is an appeal of a permanent injunction against the director and division engineer of the Nebraska Department of Water Resources (State) from requiring the plaintiff, Northport Irrigation District (Northport), to obtain an appropriation permit to pump water from the Upper Dugout Creek into its canals for irrigation. In granting the injunction the trial court found that (1) the United States of America was granted the right under its appropriation No. 768 from the State of Nebraska to recapture seepage and return flow from its project lands; (2) the decision in United States v. Tilley, 124 F.2d 850 (8th Cir. 1941), recognized that this appropriation entitled the United States to recapture seepage and return flow before it reaches the North Platte River and that this decision is res judicata as to the issues in this case; and (3) pursuant to contract, Northport is entitled to the rights of the United States under appropriation No. 768.

Northport installed a pump in the Upper Dugout Creek near Bridgeport, Nebraska, and began pumping water from Upper Dugout Creek into canal laterals to serve its district on July 21, 1981. No right of appropriation had been granted to Northport to the waters flowing in the Upper Dugout by the State. The State issued an order to Northport to stop pumping without an appropriation permit on July 22, 1981. Northport complied and filed this action seeking an injunction against the State.

The primary issue in this case is whether seepage waters from lands under an irrigation project or canal, which drain into a natural watercourse, may be collected by the appropriator from the natural watercourse and be applied to further beneficial use by the project or canal, or whether once the waters have returned to a natural watercourse they become public waters and are subject to administration by the State. We will first discuss whether Upper Dugout is a natural watercourse, and then whether all *154 waters contained in Upper Dugout are public waters.

This action is an action in equity which is reviewed de novo without reference to the findings of fact made by the trial court. Barry v. Wittmersehouse, 212 Neb. 909, 327 N.W.2d 33 (1982).

The Northport Canal crosses the top one-third of Upper Dugout Creek in an east-west direction. Upper Dugout Creek itself flows in a north-south direction and empties into the North Platte River to the south. The stream is approximately 11 miles long, and is fed by a spring in the north that directs the flow to the south but is only large enough to supply the . top 4 miles of Upper Dugout Creek with a constant flow of water. Prior to the start of construction on the Northport Canal in 1920, the remaining southern portion of Upper Dugout Creek contained water only after a rainfall, although there was testimony that another small spring from Bratten or Braddon Creek formerly flowed into the center of Upper Dugout before it was artificially dammed. Since the canal began flowing in 1926, the lower portion of Upper Dugout Creek has never had a dry measurement and flows year round. The evidence was quite clear that the only reason for the increased flow was due to seepage waters from lands irrigated by the canal which, through percolation or drainage, had found their way into Upper Dugout Creek.

Northport concedes that “there’s no question here about whether there’s a reasonably definite channel.” Upper Dugout Creek flows in a well-defined channel cut in the soil by the action of the water. The creek has 2- to 3-foot-high natural banks and a 2-to 3-foot-wide bed consisting largely of gravel and sand. On all the maps and plats introduced into evidence, which varied from those originally surveyed and platted in 1877 until the present, Upper Dugout Creek is clearly shown as a creek in a well-defined channel. The photographs offered further serve to *155 illustrate the well-defined and substantial existence of the watercourse.

A watercourse is defined by statute as “Any depression or draw two feet below the surrounding lands and having a continuous outlet to a stream of water, or river or brook shall be deemed a watercourse.” Neb. Rev. Stat. § 31-202 (Reissue 1978).

“ ‘ “To constitute a water course, it must appear that the water usually flows in a particular direction; and by a regular channel, having a bed with banks and sides; and (usually) discharging itself into some other body or stream of water. It may sometimes be dry. It need not flow continuously; but it must have a well defined and substantial existence. * * * there is a broad distinction between a stream and brook, constituting a water course, and occasional and temporary outbursts of water occasioned by unusual rains or the melting of snows, flowing over the entire face of a tract of land, and filling up low and marshy places, and running over adjoining lands, and into hollows and ravines which are in ordinary seasons destitute of water and dry.” ’ ” Barry v. Wittmersehouse, supra at 912-13, 327 N.W.2d at 35, quoting from Mader v. Mettenbrink, 159 Neb. 118, 65 N.W.2d 334 (1954).

The de novo review reveals that Upper Dugout Creek had permanent source headwaters in the north and possibly another in Bratten Creek before its flow to Upper Dugout Creek was dammed. The Upper Dugout Creek headwaters flowed in a southerly direction, with a final discharge into the North Platte River. While the lower portion of Upper Dugout Creek was often dry except for rainfall before the building of the canal, we do not believe that this fact alone negates the existence of a natural watercourse. “ ‘Those who are acquainted with the streams and water courses of the arid Rocky Mountain region of this country, draining as they do to steep, mountainous areas, with their swift currents running over gravelly and rocky bottoms, know that *156 often in the dry summer months many of them are entirely dry, at least upon the surface. All of them, nevertheless, have well-defined beds, channels, banks, and currents of water, at least the greater portion of the year, and are in every respect water courses to which water rights may attach. But it would be plainly impracticable in this western part of the country to require that, in order to constitute a water course upon which rights may attach, there must be a continuous, uninterrupted, and perennial flow of water during the entire year, and from year to year. Hence the requirement of the law is that in order to constitute a water course the stream need not flow all of the time.’

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Bluebook (online)
337 N.W.2d 733, 215 Neb. 152, 1983 Neb. LEXIS 1233, Counsel Stack Legal Research, https://law.counselstack.com/opinion/northport-irrigation-district-v-jess-neb-1983.