Enderson v. Kelehan

• Decision Date: 30 April 1948
• Docket Number: No. 34571.,34571.
• Citation: 32 N.W.2d 286,226 Minn. 163
• Parties: ENDERSON v. KELEHAN.
• Court: Minnesota Supreme Court

32 N.W.2d 286

226 Minn. 163

ENDERSON v. KELEHAN.

No. 34571.

Supreme Court of Minnesota.

April 30, 1948.

Appeal from District Court, Otter Tail County; Anton Thompson, Judge.

Action by Iver Enderson against C. M. Kelehan to enjoin defendant from diverting certain surface waters onto plaintiff's land and to recover damages. From judgment dismissing action on the merits, plaintiff appeals.

Affirmed.

Dell, Rosengren & Rufer, of Fergus Falls, for appellant.

Field, Field & Arvesen, of Fergus Falls, for respondent.

MATSON, Justice.

In an action to enjoin defendant from diverting certain surface waters onto plaintiff's land and to recover damages, judgment was entered for defendant dismissing the action on the merits. Plaintiff appeals.

Plaintiff is the owner of a quarter section of farm land in Otter Tail county situated to the northeast of, and catercorner to, a quarter section owned by defendant. Adjoining the land of plaintiff on the south and that of defendant on the east is another quarter section owned by one Loomer. Adjoining the land of plaintiff on the west and that of defendant on the north is a quarter section owned by one Swenson. The four farms together form a square of land equivalent to a section.

We are primarily concerned with the disposal of surface waters pertaining to an area corresponding to slightly more than the north half of defendant's farm. In the northwest corner thereof are four small depressions of an average area of one-half acre each. A little to the east is another depression comprising about an acre. Slightly to the west of the center of the farm is a depression covering about four acres, and adjacent to it are three smaller depressions aggregating approximately four additional acres. The foregoing depressions constitute a total area of 11 acres. To the east, a short distance from the line between defendant's farm and that of Loomer is a three-acre depression, and to the south of it are two more for an additional four acres. We are little concerned with the three depressions last above mentioned, except for the purpose of better illustrating the drainage problem found on defendant's farm. All these depressions are shallow, and prior to the drainage work hereinafter described they did not interfere with the farming of the land except as they retained an accumulation of surface water from precipitation. The amount of water collected, and the time for which it was retained varied according to the amount of moisture per season. In a dry season or late in the summer, the hollows would generally be dry or have little water in them. In the spring of each year, water from melting snows and rains would accumulate and remain in them until evaporated or absorbed by the earth. During wet periods, the water standing in the depressions would render not only the submerged portions of the land untillable, but also a considerable part of the surrounding area, which would be so saturated with moisture as to make the use of farm machinery impractical. The net result was that for the important part of the growing season these depression areas were not only unfit for use but served as a series of barriers which made it difficult to farm the surrounding and higher terrain.

At this point we turn to a consideration of the natural slope or topography of defendant's farm to determine how the surface waters would naturally flow except as impounded by these depressions. The natural over-all slope was from west to east toward the Loomer farm. There is some evidence that years ago a small part of the northwest corner area drained northward to the Swenson farm, but whatever drainage in that direction ever existed gradually ceased over the years, because of the formation, as the result of dust storms, of a small ridge along the north fence line. At best, however, this northward drainage was insignificant in amount. As a general proposition, however, the slope was to the east and southeast. In the fall of 1942, defendant constructed his system of drainage by using a road grader to dig shallow watercourses from 10 to 12 feet wide with a depth of zero at the edges and sloping toward the center to a depth that varied, according to the lay of the land, from 0.6 to 1.8 feet. They were constructed with wide and sloping sides so as not to impede the passage of farm machinery. We are here concerned with only three of these so-called ditches. The first commenced with the most northwesterly depression in the northwest corner and extended in a southeasterly direction for a distance of about 600 feet. Depressions on either side were drained by branch ditches. At its beginning in the northwest corner, there was an elevation of 96.4 feet, and at its terminus an elevation of 95.4 feet, or a drop of 1 foot in 600 feet. The water, after following this ditch to its terminus, diffused itself over the land to follow the natural slope in a southeasterly direction until it reached the four-acre depression slightly west of the center of defendant's farm. The elevation at this central depression was 95.1 feet. In other words, there was a gentle slope of only 0.3 of a foot. Except for this gentle slope, the land was level. At the central depression, the second ditch commenced and ran north for a short distance, then turned to the east, and thence southeasterly, where it terminated at an elevation of 90.0, or for an over-all drop of 5.1 feet. The turn of the second ditch to the north for a short distance was made in the interest of developing a more workable field area. The water, after leaving the eastern terminus of the second ditch, diffused itself over the land to follow a slope to the east until it reached the three-acre depression (near the east line), where the elevation was only 85.3 feet. In other words, the second ditch had an over-all drop of 4.7 feet. The third ditch commenced at the three-acre depression, extended in a northeasterly direction, and terminated at a point just west of the east line, where the elevation is 82.7 feet. From the beginning of the first ditch to the termination of the third ditch, there was a total drop of 13.7 feet. After leaving the terminus of the third ditch, the water entered a natural ravine and flowed under the east fence in a northeasterly direction until it reached a large slough on the Loomer farm. When the Loomer slough overflowed, the water ran through an outlet to the north into another slough or depression in the pasture on plaintiff's farm. The depression on plaintiff's farm has an elevation of 64.6 feet and is 5.5 feet lower than the Loomer slough, and in turn the latter is 11.9 feet lower than defendant's east line. In other words, the depression on plaintiff's land is 31.8 feet lower than the starting point of the drainage project on defendant's farm.

Defendant's drainage system was completed in the fall of 1942. In the springs of 1943 and 1944, the waters from rain and snow, which in part had formerly remained entrapped in the depressions on defendant's land until they disappeared through percolation and evaporation, flowed in their entirety through the ditches into the Loomer slough and thence to the depression on plaintiff's land. In the spring of 1943, the slough or depression in plaintiff's pasture was filled with water over an area of 27 acres. Prior thereto, the normal springtime water deposit covered only about six or seven acres, although there was testimony to the effect that in 1937, a year of heavy rain and snow, an area of about 20 acres was submerged. It is with respect to this situation that plaintiff sues to recover damages and to enjoin defendant from maintaining his drainage system.

1. "Surface waters" consist of waters from rain, springs, or melting snow which lie or flow on the surface of the earth, but which do not form part of a well-defined body of water or natural watercourse.¹ They do not lose their character as surface waters merely because in a measure they are absorbed by or soak into the marshy or boggy ground where collected. Hartle v. Neighbauer, 142 Minn. 438, 172 N.W. 498.

2, 3. With respect to surface waters, Minnesota has evolved the rule of reasonable use and follows neither...