Smith v. Musgrove

32 Mo. App. 241
CourtMissouri Court of Appeals
DecidedOctober 15, 1888
StatusPublished
Cited by1 cases

This text of 32 Mo. App. 241 (Smith v. Musgrove) is published on Counsel Stack Legal Research, covering Missouri Court of Appeals primary law. Counsel Stack provides free access to over 12 million legal documents including statutes, case law, regulations, and constitutions.

Bluebook
Smith v. Musgrove, 32 Mo. App. 241 (Mo. Ct. App. 1888).

Opinion

Rombauer, P. J.,

delivered the opinion of the court.

The plaintiff, on behalf of himself and other landowners in the valley of Honey creek, filed his petition praying for a mandatory injunction compelling the defendant to remove a dam which the plaintiff avers the defendant had erected across the channel of Honey creek. The petition states that such dam is a nuisance to plaintiff and other land-owners, and unless removed the waters of Honey creek would flood tlfeir lands and render them comparatively worthless.

The defendant, by answer, admitted the erection of the dam, but denied that it was across the channel of Honey creek. The answer states that the channel of Honey creek is as it always was, in a southeasterly direction and across the lands of plaintiff, and that the dam was erected by defendant on his own lands for the purpose of protecting them from overflow. The plaintiff, by reply, denies that the channel of Honey creek runs through his, the plaintiff’s, lands. He admits that prior to 1874, the channel of Honey creek was in a southeasterly direction from defendant’s lands, and did run through the lands of plaintiff, but avers that, in 1874, said channel changed and took a northerly course from the defendant’s lands, and that ever since said date the waters of Honey creek did run in a northerly direction and into Sugar creek, the creek forming a new channel, which it kept for a period of more than ten years, whereby said new channel became an ancient water-course, and that the dam erected by the defendant wholly obstructs this water-course.

[248]*248Upon a full hearing of the issues thus framed the court granted the mandatory injunction prayed for and the present appeal is prosecuted from this decree.

The evidence offered by both parties is voluminous and conflicting as to some of the data. The change in the channel of Honey creek is conceded by all the witnesses. The defendant, however, contends that the evidence shows that such change did not begin prior to 1876 or 1877, and was very slight until 1880, at which time the new channel was increased by the waters of a freshet, and thereby became the main channel of Honey creek. On the other hand, the plaintiff contends that the change began in 1874, and had assumed such shape in 1876, and in that year and ever thereafter the ordinary flow of the waters of Honey creek passed exclusively .through this new channel.

The decree of the trial court embodies no finding of facts as to the date when this change took place. As the case is in equity and the .finding reviewable upon the evidence on appeal, we have made a finding of fact based upon a careful analysis of the evidence and will proceed to state such finding and then apply the law thereto.

The lands of the plaintiff, as well as of the defendant, affected by the decree, lie in the Mississippi river bottom between the bluffs on its right bank and the river. Both tracts are along the old channel of Honey creek, which is a permanent water-course, having its origin in the hilly country beyond the bluffs and emptying its waters into the Mississippi river, formerly at a distance of about five miles below plaintiff ’ s lands. The defendant’s children are the owners of the dominant estate on the creek, their lands being about two miles above those of the plaintiff, following the meanderings of the stream. While the lands are those of defendant’s children, we will speak of them, for brevity’s sake, as those of defendant, he representing his children in this litigation.

The uniform course of streams coming from the' [249]*249west and emptying into the Mississippi river in that section of the state is from northwest to southeast, and such was the course of Honey creek prior to 1875. The stream carries considerable water in the wet season of the year, and deposits the brush and driftwood along its course when the waters subside. This process and the alluvial sediment similarly carried and deposited along the channel and on the banks of the creek, have the tendency of scouring the channel in some places, and raising it and the immediate banks in others, so that the channel becomes very irregular as to the general level, and in some places even higher than the adjacent lands beyond its immediate banks.

The next water-course to the north of Honey creek is Sugar creek, the general course of which is through the bottom lands from northwest to southeast, and then from southwest to northeast. This stream empties into the Fox slough of the Mississippi river at a poinf many miles north of the ancient mouth of Honey creek. As the course of the Mississippi river between these two points is from north to south, the elevation of the mouth of Sugar creek is necessarily much higher than that of Honey creek. We state these facts thus fully for the purpose of making it clear that we are impressed with the fact that the natural course of Honey creek, as determined by the surrounding circumstances existing prior to 1875, was to the southeast and along what is admitted to be its ancient channel.

Opposite to a point in defendant’s land, at which, according to plaintiff’s claim, the new channel formed, Sugar creek comes within a mile and a half of Honey creek. Nearly midway between the two creeks one Johnson had constructed a ditch twenty-three feet wide and three and one-half feet deep, presumably for the drainage of his own lands into Sugar creek. The ditch connects with Sugar creek and has a slight fall towards that creek. There is, and was at the times hereinafter stated, a slight depression of the land northwardly from [250]*250the point where this new channel took off towards Johnson’s ditch, so as to enable the waters of Honey creek, if tapped at the point where the new channel took off, io flow into Johnson’s ditch and thence into Sugar creek.

It is proper to state in this connection that while there is necessarily a depression sontheastwardly likewise from the point where the new channel took off, along the course of the old channel of Honey creek, this depression for the first mile or mile and a half, is very slight, and about the same in extent as the depression of the land towards Sugar creek. The main fall of the land towards the Mississippi river along the ancient channel of Honey creek, began- only after the stream left appoint formerly known as Walnut lake, so that taking the topographical features of the country as they existed, the chances of the creek to flow northwardly, or southeastwardly from the point where the new channel formed, assuming that the stream was left wholly to its own action, were nearly equal.

The map hereto annexed is constructed from the various maps offered in evidence by the parties respectively, and is deemed sufficient to show the geographical features of the country as to water-courses, the location of the plaintiff’s and defendant’s lands on Honey creek, the course of the new channel and the location of the dam erected by the defendant and sought to be removed by the mandatory injunction.

We find that prior to and in the year 1874 cattle going to water had worn a trail or path, cutting the bank of Honey creek at the point designated by the letter A. on the annexed map ; that parts of the water of said creek in said year passed through such cut • northwardly, and began, to cut a defined channel towards Sugar creek.

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Bluebook (online)
32 Mo. App. 241, Counsel Stack Legal Research, https://law.counselstack.com/opinion/smith-v-musgrove-moctapp-1888.