Gibson v. Sharp

277 S.W.2d 672, 1955 Mo. App. LEXIS 79
Missouri Court of Appeals·Decided April 8, 1955·No. 7393·Published·Cited by 23 cases

Opinion

*674 RUARK, Judge.

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The case' is here by transfer from the Supreme Court. 270 S.W.2d 721.

Plaintiff’s petition (filed June 1, 1951), after stating ownership and privity in title, alleged that the owners of adjoining lands-agreed to the digging of a drainage ditch having for its purpose the benefit of both parties, about 1912, the digging and maintenance of the ditch thereafter and the use of such by both parties until the year 1951, when defendants barred plaintiff therefrom by construction of an earthen dam at the boundary line between the parties. Prayer is for mandatory injunction. The trial court denied the relief prayed for.

The substantive question is whether plaintiff-appellant has a right- of drainage along and through a ditch which crosses the land of defendants-respondents.

Pláintiff is the owner of the North Half' of the Northwest Quarter, " Section 23, Township 17, Range 11, Pemiscot County. The east forty acres of this eighty was formerly owned by A. H. Wright, who died in 1942. Plaintiff purchased from.his heirs in 1944. This east forty will be referred to as the Wright land-. Lying along the north boundary of. plaintiff’s land is another eighty-acre farm owned by the defendants, which is described as the South Half of the Northwest Quarter, Section 14, Township 17, Range 11. Defendants are the heirs or devisees of W. M. (Preacher) Duncan, who died in 1941. It is the east forty of this land, directly north of the Wright forty, which is said to be burdened by a drainage ditch easement. We will refer to this forty as the Duncan land. Lying immediately north of the Duncan land is a tract which we will call the Coleman land. Running through the Coleman land in a general east-west direction is Pemiscot bayou. At the point with which we are here concerned this bayou runs close to. the north line of the Duncan land, leaving an intervening strip of Coleman land not exceeding seventy-five yards in width. All of the land involved is low and, in general, level, although it, particularly the northeast portion of the Duncan land, contains what are referred to by the witnesses as ridges. These appear to be low swells of the character formed by sediment-bearing water and are not to be confused with the high, rocky, “hog back” ridges found in some other portions of our state. - The drainage slope in the immediate vicinity is slight, but such as there is is to the northward toward Pemiscot bayou. Thus, standing on the Wright forty and facing north and slightly “downslope” .with the drainage, one looks from it across the Duncan forty to the Coleman tract, where Pemiscot bayou runs its crooked way.

At some time between 1912 and 1914 plaintiff’s east forty was occupied and farmed by plaintiff’s predecessor in title, Wright. All of it was in cultivation except a small tract near the north boundary which was lowland, in thicket and used as a pasture. At that time the east forty of the Duncan land to the north was in woods except some nine to fifteen acres on the east side cleared and in cotton. Duncan did not live on the tract and cultivation of this portion was by tenant. Extending through the approximate center of the Duncan tract was a swale or a swag, not in any sense a ravine or gully but a depression or series of depressions which were lower - than the land on the east and west and where, at least in wet weather, water collected and stood in the woods. This series of depressions, sometimes referred to as sloughs, extended some distance into the Wright forty which adjoined on the south. As water accumulated in rainy seasons on the Wright land and the higher portions of the Duncan land it gradually worked its way - to the north down the swale.toward Pemiscot bayou; so also in extremely wet weather and when the water in the bayou was high did it creep back up through the sloughs and spread over the lower lands. The Wright land, even at this time, had some laterals or ditches which drained into the swale on-its south side of the boundary line. While the evidence is not entirely clear as to this point, it would appear that there were also some lateral ditches on the Duncan land.

According to plaintiff’s evidence, about the year 1912 Wright and his sons, by agreement with Duncan, cut what is called *675 the spade ditch. This ditch commenced on the boundary line between the Duncan and Wright forties at about the center and and thence meandered northward with the swale through the woods following the depressions, skirting where possible the ends of minor swells, to the north line of the Duncan land. From there the water drained off into the bayou through a “dip” on the Coleman land. This spade ditch was not continuous but was only a connecting of low spots in the swale and a cutting through of the “ridges” where necessary. It was to some extent experimental, to find where the water “wanted to go.” Most of the work was done by Wright and his sons, but Duncan was present from time to time during the progress of the work and helped occasionally. Within two years afterward the Wright family, this time with the assistance of some extra help, went in with teams and scrapers and, following approximately the meanderings of the drainage which had been established by the spade ditch, made a continuous ditch approximately six feet wide at the top and four feet at the bottom. The depth varied as necessity required according to topography. This is called the scraper ditch. The construction was by agreement with Duncan, who, prior to commencement, walked over the land with Wright and was present and occasionally assisted by taking an ax and chopping roots out of the way. The principal labor and expense were furnished by Mr. Wright and the time spent in this construction was approximately two weeks.

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Gibson v. Sharp, 277 S.W.2d 672, 1955 Mo. App. LEXIS 79 (Mo. Ct. App. 1955).

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