Blohowak v. Grochoski

96 N.W. 551, 119 Wis. 189, 1903 Wisc. LEXIS 100
Wisconsin Supreme Court·Decided September 29, 1903·Published·Cited by 2 cases

Opinion

Cassodat, C. J.

This is an action at law triable by jury as a matter of right. This being so, the order of the trial court changing the answer of the jury to the first question from the affirmative to the negative can-only be sustained [191] on the ground that the finding of the jury was contrary to the undisputed credible evidence. In granting the motion of the defendant to so change the verdict the trial court filed a carefully written opinion, reviewing the evidence, and reached the conclusion that the water complained of was mere surface water and did not have the essentials of a watercourse, as defined by the authorities. That court,. having heard the witnesses, was undoubtedly in a better position to determine the preponderance of the testimony and the weight of the evidence than this court. Had this been an equitable action and the verdict merely advisory, this court would undoubtedly have felt bound by the action of the trial court. The same is true if this case had been tried by the court without a jury. So, even in jury cases, the trial court has a broad discretion in setting aside verdicts as against the preponderance of the evidence, and granting a new trial. Schillinger v. Verona, 85 Wis. 595, 55 N. W. 1040, and cases there cited; Farley v. C., M. & St. P. R. Co. 89 Wis. 206, 61 N. W. 769. But to justify a court in directing a verdict or changing the answer of the jury from the affirmative to the negative, as here, the finding of the jury must be contrary to the undisputed credible evidence. ' In determining whether such verdict was contrary to the undisputed evidence, the trial court, as well as this court, was bound to consider the evidence in support of the verdict in the most favorable light it would legitimately bear. Renne v. U. S. L. Co. 107 Wis. 320, 83 N. W. 473, and cases there cited. So cofisidered, can we say that the evidence in behalf of the plaintiff is insufficient to sustain the finding of the jury?

To appreciate the evidence, the general situation should be considered. The plaintiff and defendant each own eighty acres of land, together constituting the W. half of the E. half of section 13, the plaintiff owning the south eighty and the defendant the north eighty. One Jensen owns the eighty immediately east of the plaintiff’s land, and on the southeast [192] corner of that eighty, and about forty rods from the plaintiff’s land, there is a large willow swamp, extending south, onto section 24. That swamp is from thirty to forty rods wide from east to west, and about one hundred rods long from, north to south. There is also a small swamp on Rasmussen’s land immediately west of the south half of the plaintiff’s land. About forty rods north of the plaintiff’s land, and a little west of the east line of the defendant’s land, is a small, pond, and about fifty rods northwesterly from that there is a still larger’ pond on the defendant’s land. It is conceded that' the water from the large swamp drains off westerly and northerly onto the plaintiff’s land, and thence onto the defendant’s, land, and also in a.southeasterly direction from the portion of that swamp on section 24. Such is the general situation. It is stated by the trial judge, in effect, that some twenty-five- or thirty years ago that large willow swamp extended northwesterly across the land now owned by the plaintiff, and nearly half way across the defendant’s south forty, and to the' small pond, and that the water in part from the large willow swamp drained off north into that small pond, and from, thence northwesterly into the large pond, mentioned, and: from thence north to a creek, and at times it ran off in such quantities and with such rapidity during several months off the year as to form quite a stream between the large pond and the creek; that while the timber was standing and the-soil uncultivated the water would stand in the large willow swamp during the greater part of each season, and in very wet seasons the water would drain into and run out of the-pond during the whole season; that after the timber was cut from most of the land in the two sections mentioned, and the-larid became cultivated except in a few spots where the timber had not been cut, the water was much more absorbed and less water was drained onto the low ground, and the same more-quickly disappeared by being drawn off, absorbed, and evaporated ; that the result was that, with the exception of one or-[193] two acres, tbe land in section 13, west of tbe plaintiff’s land,, became and was fit for cultivation; that tbe natural drainage of about 900 acres was into tbe basin constituting tbe original bed of tbe big willow swamp; that there never was-, however, any channel from tbe big willow swamp to tbe small pond, but that tbe water drained across tbe plaintiff’s land into tbe swamp and thence into tbe small pond through furrows and ditches constructed by tbe plaintiff; that there are places south and west of tbe swamp where in times of melting snow and heavy rains tbe water runs towards and into tbe swamp in such quantities as to form streams; that furrows or depressions are left through tbe field for such flow, which are bridged when crossed by tbe highway; that none of tbe water flowing into tbe swamp comes from living springs, but is surface water; that the defendant dammed up tbe northern end or outlet of tbe small pond, and thus retarded tbe natural flow of tbe water, and damaged the plaintiff’s land.

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Blohowak v. Grochoski, 96 N.W. 551, 119 Wis. 189, 1903 Wisc. LEXIS 100 (Wis. 1903).

96 N.W. 551 (Blohowak v. Grochoski) — published by Counsel Stack Legal Research, free access to 12M+ legal documents.

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