Beetison v. Ballou

44 N.W.2d 721, 153 Neb. 360, 1950 Neb. LEXIS 42
CourtNebraska Supreme Court
DecidedNovember 22, 1950
Docket32807
StatusPublished
Cited by4 cases

This text of 44 N.W.2d 721 (Beetison v. Ballou) 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
Beetison v. Ballou, 44 N.W.2d 721, 153 Neb. 360, 1950 Neb. LEXIS 42 (Neb. 1950).

Opinion

Simmons, C. J.

So far as concerned in this appeal, plaintiff brought this action for a mandatory injunction ordering the defendant to remove a dike constructed on his land, and that the defendant be permanently enjoined from con *362 structing or maintaining any embankment upon his land interfering with the natural flow of floodwaters from Wahoo and Salt Creeks, and for equitable relief. Defendant joined issue and prayed for a dismissal of the action. After trial the court found generally for the defendant and dismissed the plaintiff’s petition. Plaintiff appeals. We reverse the judgment of the trial court and remand the cause with directions.

For brevity of description and better understanding of the factual situation, and without being accurate in detail, we have prepared and use a chart for the purpose of showing the relative position of the lands, the physical conditions, and the structures involved.

*363 The land involved in this action is bottom land and generally in the flood plane of Wahoo and Salt Creeks. Wahoo Creek drains an area of about 500 square miles. Salt Creek at the point where Wahoo Creek joins it drains an area of over 1,000. square miles. The Sioux City line of the railroad forms a dam across the valley with the outlets as indicated under the bridges across the streams. Below the land involved, the Omaha line of the railroad and the highway form similar dams with similar outlets.

Plaintiff owns the land described on the chart as plaintiff and plaintiff-1, the latter tract apparently having been pürchased about the time or after this action was initiated.

Defendant owns the land described as defendant and defendant-1, the latter tract having been purchased about the time or after, this action was initiated.

In November' 1945, defendant built a drain ditch and dike along the line indicated on the chart as A to B— a distance of 1,750 feet. The work began at the railroad track at A, followed the north bank of Wahoo Creek for some 400 feet, and then straight east — all on defendant’s land. It is about this dike that plaintiff complains.

Plaintiff’s evidence shows that by natural course, floodwaters from Wahoo Creek flow out and across the lands marked defendant-1, and then, in part at least, across defendant’s land, then onto the Stanley land, and finally into Salt Creek. Plaintiff offered evidence that such was the course of the waters at flood periods in 1908 and on occasion thereafter, prior to the building of the dike.

Plaintiff’s evidence further is that after the dike was constructed severe floods occurred in 1947 and thereafter; that in those floods the floodwaters from Wahoo Creek flowed across defendant-1, came against the dike, were turned and formed a channel along the south side of the dike, and flowed down upon his lands; that on several occasions flowing water was two or more feet *364 deep south of the dike; and that at the same time there was little, if any, water oh the north side. He testified that those waters destroyed crops, washed his land, and left silt and debris upon it. Whenever we use the word “debris” here, we mean logs and material of that character that are carried by swiftly moving waters.

Defendant’s evidence is in accord with that of the plaintiff. Defendant’s witnesses testified that the- natural course of the floodwaters from- Wahoo Creek was across defendant’s lands and onto the Stanley lands and plaintiff’s lands.

Defendant testified that he dug the ditch in 1945; that he put the dirt removed on the south side of the ditch forming the dike because he had to put it somewhere, although one of his witnesses testified that he saw evidence of dirt having been removed from south of the dike at its lower end. Defendant testified that he built the ditch to drain surface waters, and that he put the dirt on the south side so as to protect his property and to prevent the' floodwaters from Wahoo Creek filling his drain ditch with silt and rendering it useless. It seems obvious that if floodwaters from Wahoo Creek would come upon his land with sufficient volume and velocity to deposit damaging silt in his drain ditch, those waters would also flow upon and across defendant’s lands, as plaintiff’s evidence shows they did before the dike was built.

The evidence is that from about 500 feet east of point A, defendant’s land slopes to the west. Defendant in constructing the dike put a tube and floodgate through it at point A. The floodgate was so constructed that it opened so that waters from defendant’s lands would flow south into Wahoo Creek, but in the event of waters coming against it from Wahoo Creek, it would close and prevent the flow onto defendant’s land at that, point.Defendant testified that the floodgate was so constructed to prevent the tube filling with silt from floodwaters of Wahoo Creek. This part of the dike was washed out. *365 in part in June 1947, and later restored by defendant.

That the dike had served its purpose of preventing the drain ditch from filling with silt is established by defendant for he testified that the land south of the dike from point A halfway to point B had been built up with silt deposited there by floodwaters. Again it appears obvious that floodwaters were materially retarded in their flow by the dike so as to cause the deposit of the silt. One of defendant’s witnesses testified that he had seen floodwaters go across defendant-1, come against the dike at its lower end, form a channel, and then flow east upon plaintiff’s land past point B. Defendant’s engineer witness testified that south of point B “for some hundred feet” he saw where the “heavy flow” had gone across from defendant-1 onto plaintiff’s land.

The evidence also is that, depending on the contour of the land, floodwaters from Wahoo Creek would have to rise between 14 inches and 3% feet above the land south of the dike before they would flow across onto defendant’s land. It also appears from the evidence that when all the land is flooded above the top of the dike, as it was once in 1947, after the waters had receded to the line of the dike, all the flow of the flood-waters south of the dike is across plaintiff’s land and that the flow of waters on defendant’s land north of the dike is the run-off from defendant’s land.

There is evidence that following severe floods, debris is left on plaintiff’s land. There is no evidence of debris being left on defendant’s land. In one instance after one flood the defendant’s evidence is that there was no debris left on his land.

Defendant’s theory is that plaintiff has. no cause for complaint for several reasons. One is that his land is open to the east and that water flowing past point B will seek its own level and flow backward and flood his lands. Obviously that would depend upon the volume and duration of the flood. This contention ignores the issue. Plaintiff is not complaining about waters being on de *366 fendant’s land but is complaining of the change of the course of the waters at floodtime. This contention seems to admit the merit of plaintiff’s' complaint.

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Cite This Page — Counsel Stack

Bluebook (online)
44 N.W.2d 721, 153 Neb. 360, 1950 Neb. LEXIS 42, Counsel Stack Legal Research, https://law.counselstack.com/opinion/beetison-v-ballou-neb-1950.