Faught v. Dawson County Irrigation Co.

19 N.W.2d 358, 146 Neb. 274, 1945 Neb. LEXIS 84
CourtNebraska Supreme Court
DecidedJune 29, 1945
DocketNo. 31937
StatusPublished
Cited by13 cases

This text of 19 N.W.2d 358 (Faught v. Dawson County Irrigation Co.) 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
Faught v. Dawson County Irrigation Co., 19 N.W.2d 358, 146 Neb. 274, 1945 Neb. LEXIS 84 (Neb. 1945).

Opinion

Simmons, C. J.

In this action plaintiff seeks to recover damages for loss of crops as a result of flooding. Trial to a jury was waived and had to the court. The trial court found for the plain[275]*275tiff. Defendant appeals. We affirm the judgment of the trial court.

We state the evidence in conformity with the rule that in a law action findings of fact made by the court have the same force and effect as the verdict of a jury, and if there is competent evidence to support them, such findings will not be disturbed on appeal. Linch v. Thorpe, 140 Neb. 478, 300 N. W. 383.

Plaintiff is the owner of a piece of irrigated land of about 70 acres, generally rectangular in shape, and contiguous lengthwise to and above the main canal of defendant.

Defendant is the owner of an irrigation canal and works, its main canal running generally east and west in Dawson county.

Plaintiff’s petition here states two causes of action.

The first cause is based upon the destruction of .7 acres of beets as .the result of two floodings occurring in May of 1940. These were caused by the overflow of defendant’s canal. The trial court found that plaintiff was damaged in the sum of $10.31.

The second cause of action is based upon damage to and destruction of beets and the killing of a perennial crop of alfalfa on another part of the same farm by flooding which occurred beginning on June 7, 1940. The trial court found for plaintiff and awarded damages in the sum of $101.65 for the beets and $500 for the alfalfa.

Plaintiff’s land is bisected by a draw or creek running generally north and south through about the center of his land. This in the lower area is referred to as Spring creek. This creek forms the outlet of a drainage basin several miles to the north and extending generally north and south, and empties into the Platte river. The creek is described as a swale or dry creek, except in times of heavy rainfall. Its meanderings are defined but without distinct banks until it reaches within a short distance of plaintiff’s land. There it has distinct banks. At a point about 100 feet north of defendant’s canal the west bank is lower than above that point.

[276]*276In 1925 defendant constructed a concrete box underdrain two feet by six feet, and a 24-inch diameter pipe underdrain at the point where the bed of the creek intersects its canal. At a higher elevation they had provided two structures, six feet wide, in the upper bank of their canal, capable of being opened to allow excess flood waters to enter their canal.

To the east of Spring creek, there originally appears to have been a swale called Stump' ditch or creek, which in part at least drained naturally to the east of Spring creek. About 1891 or 1892 an irrigation ditch Was built along the east side of this swale, so that waters no longer passed down it, but were diverted onto the lands to the west and excess waters reached Spring creek. Thereafter, the lands below that ditch were tilled and leveled, and the ditch no longer existed in fact. About 1935 Stump creek was tapped with a drain ditch about two miles north of plaintiff’s land and carried into Spring creek a half a mile or so north of plaintiff’s land. This prevented flood damage to the intermediate lands.

The Cozad Irrigation Ditch runs generally east and west across this drainage area a few miles to' the north of defendant’s canal. Still a few miles further to the north the Gothenburg Irrigation Ditch runs generally east and west across this drainage area.

During the night of June 6, 1940, over two inches of rain fell at Cozad and apparently a heavier fall occurred in the drainage area to the north.

At that time the defendant’s canal was carrying a considerable quantity of water diverted from the river. The next morning its wasteway to the east of the point in question was opened, and during the early forenoon its intake gates were closed. At that time the water had backed up and flooded plaintiff’s land west of the creek, although the underdrains were functioning. The canal being filled with water, the spillway gates into it were not then opened. At about noon the water was coming down from the north,' and, so far as plaintiff’s land is concerned, within the banks of the creek until it reached a point about 100 feet from de[277]*277fendant’s canal. There it overflowed the bank and had flooded plaintiff’s land to a depth up to three feet, or more. The underdrains were clogged with weeds and other debris'. The defendant’s canal was- then empty. The gates of the spillway were opened as much as possible, permitting the accumulated water to enter the canal. The obstructions in the underdrains were removed, and after some time the height of the water receded. Plaintiff’s land remained under water for two or three days. The evidence is that the rainfall on plaintiff’s land would not have caused the flooding and would have drained off without damage to his crops. The evidence also is that had defendant’s structure not been placed across this creek, the flood waters would have passed on without damage to plaintiff. .

Also, during the day of June 7, the drain ditch was emptying water into Spring creek above plaintiff’s land. On the morning of that day, the Gothenburg canal was carrying a small head of diverted water sufficient to prime the ditch and keep down the growth of weeds. Its intake gates were closed early that morning. Floodwaters from the north came down to the Gothenburg canal and overflowed its banks, and ran into the canal. Shortly after noon of that day, the south bank of this canal gave way and the waters were released to flow south and eventually into Spring creek. At the same time, floodwaters overflowed the banks of the Cozad canal and came on down into Spring creek. All these waters, however, remained within the banks of Spring creek until they reached a point about 100 feet from defendant’s canal, where they banked up against the canal and flowed out upon defendant’s land.

The above statement of facts is consistent with the evidence and the findings of the trial court.

Plaintiff alleges that defendant was negligent in the construction of its outlet or underdrain in that it was inadequate to permit floodwaters to pass through in sufficient quantity and to prevent the accumulation of waters that flooded plaintiff’s land; and that it was negligent in permitting the underdrains to become clogged. The trial court [278]*278found generally and specifically for the plaintiff on these allegations of negligence.

Defendant argues that for' 20 years prior to the time in question these structures had proved adequate, and that negligent construction and operation were not proved.

We have repeatedly held that it is the duty of those who build structures across natural drainways to provide for the natural passage through such obstruction of all waters which may be reasonably anticipated to drain there. This is a continuing duty. Crummel v. Nemaha County, 118 Neb. 355, 224 N. W. 864; Leaders v. Sarpy County, 134 Neb. 817, 279 N. W. 809; Webb v. Platte Valley Public Power and Irrigation District ante p. 61, 18 N. W. 2d 563.

It appears quite obvious that the underdrains were not adequate to permit the passage of all waters which the defendant should have anticipated might drain there.

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Cite This Page — Counsel Stack

Bluebook (online)
19 N.W.2d 358, 146 Neb. 274, 1945 Neb. LEXIS 84, Counsel Stack Legal Research, https://law.counselstack.com/opinion/faught-v-dawson-county-irrigation-co-neb-1945.