Switzer v. Yunt

41 P.2d 974, 5 Cal. App. 2d 71, 1935 Cal. App. LEXIS 1009
CourtCalifornia Court of Appeal
DecidedMarch 1, 1935
DocketCiv. 1378
StatusPublished
Cited by14 cases

This text of 41 P.2d 974 (Switzer v. Yunt) is published on Counsel Stack Legal Research, covering California Court of Appeal primary law. Counsel Stack provides free access to over 12 million legal documents including statutes, case law, regulations, and constitutions.

Bluebook
Switzer v. Yunt, 41 P.2d 974, 5 Cal. App. 2d 71, 1935 Cal. App. LEXIS 1009 (Cal. Ct. App. 1935).

Opinion

MARKS, J.

Plaintiffs and defendants are owners of tracts of land in Tulare County on opposite sides of a county road which runs north and south. Defendants own eighty acres which extend one-half mile along the east side of the road, and plaintiffs own twenty acres which extend one-eighth of a mile along its west side. The south boundaries of the two tracts form a straight line. The county road is graded above the level of the adjoining lands for the entire distance of one-half mile except in two places, one being just south of the north line of plaintiff’s property, and the other in a place that does not concern us. At the point we have mentioned, for about eighty feet, the road is a few inches below the grade of defendants’ property, but it is several inches above the grade of plaintiffs’ property. The road had gutters on both its sides below the surface grades of both properties. Thus the road formed an effective dam against the free flow of surface waters from east to west except at the two points mentioned.

All of the land in the neighborhood of the tracts in question was what is designated by a department of the federal government as “hog wallow land” which had to be leveled before it could be successfuly farmed. The evidence shows that in its natural state defendants’ land had upon it á depression of not more than one and one-half acres in area and of not more than two feet in depth. It was referred to by many witnesses as a “duck pond” and was situated near the west boundary and about halfway between the north and south boundary lines of defendants’ property. There were two other smaller depressions on defendants’ land and one on plaintiffs’. These depressions held surface water during the rainy season and several witnesses for plaintiffs testified that over a period of a number of years they had never seen water draining from the duck pond. It would seem that the purpose of this evidence was to lay the foundation for the conclusion that when the land was in its natural state the duck pond furnished a reservoir for all surface waters and prevented their draining away.

Plaintiffs graded and planted their land to grapevines about the year 1921. Shortly thereafter the defendants *74 graded and planted the north forty acres of their property, and later graded and planted the south forty acres. In these operations the hog wallows were leveled and the bottom of the duck pond was raised, though just how much is not apparent. It continued to be the low point on defendant’ property.

It is not questioned that in its original state, as well as after the grading operations were completed, the general slope of the country was from northeast to southwest. The north twenty acres of defendants’ property was irrigated from north to south, the next thirty acres from east to west, the next ten acres from south to north, and the south twenty acres from north to south. All lands adjoining the road on the west side of defendants’ property, including plaintiffs’ property, was irrigated from east to west.

The southwesterly slope of the country was gentle. There is in the record a profile map of the county road and the property immediately adjoining its sides. The profile line of the center of the road does not show a change of grade of more than three feet six inches and those of the properties immediately adjoining it a change of grade of not more than three feet two inches in the one-half mile depicted. Mr. Switzer was of the opinion that the westerly fall across his property and the twenty-acre tract adjoining it on the west was not more than five feet.

In 1930 or 1931 the use of defendants’ south forty acres was changed from growing alfalfa to growing citrus trees. The alfalfa land had been blocked into squares by ridges which held drainage waters upon the ground. This blocking was abandoned when the citrus trees were planted. During the rainy season of 1931-32 some trouble was experienced by defendants because of the backing up of rain water against the road which flooded portions of their orchard. By arrangement with the owner this water was drained under the road and into a drainage pit on the property adjoining plaintiffs’ property on the north. During the rainy season of 1932-33 defendants threatened to sue the county of Tulare for damages to their land and trees if drainage were not provided under the county road. Plaintiffs threatened to sue the county if such drainage were provided in front of or near the front of their property.

*75 On January 28, 1933, the county of Tulare installed an eight-inch drain pipe under the road at a point a short distance north of the northeast corner of plaintiffs’ property. Some time during that afternoon Mr. Switzer and his neighbor to the north built a dirt dam along the east side of their properties with its center about opposite the drain pipe. A hard rain started that same afternoon and lasted through the night and into the next day. During the night the dam broke near the northeast corner of plaintiffs’ property. The water washed top soil and fertilizer that had just been spread off the property. Mr. Switzer and another witness testified that before the storm they saw an employee of defendants digging ditches along the east side of the road and on the west side of defendants’ property. After the storm dug ditches were found, one leading from the duck pond on defendants’ property and emptying into the gutter of the road near the east end of the drain pipe, a second dug ditch in the east gutter of the road draining water from north to south, and a third dug ditch in the east gutter draining water from south to north in the direction of the drain pipe.

Neither party contends that the rain commencing on January 28th was a great and unusual storm or that the water that collected on defendants’ property was flood water or anything more than surface drainage water precipitated by the storm.

Plaintiffs instituted this action and prayed that they recover their damages caused by the erosion of their land and that defendants “be perpetually enjoined and restrained from allowing any surface or rain water or any water from their said land to empty upon, flood or run over the land of plaintiffs, and that said defendants be restrained from running any surface or rain water or any other water from their land onto the land of plaintiffs”. Defendants filed a cross-complaint whereby they sought to enjoin plaintiffs from obstructing the natural flow of surface water across their land.

It was evidently the theory of the plaintiffs at the trial, and is again asserted here, that the duck pond on defendants’ property, before it had been leveled, furnished a natural reservoir which restrained all surface and storm waters falling or draining upon defendants’ land; that defendants *76 partially filled it when they leveled their property; that they should not have been permitted to fill in low places or change the natural contour of the ground; that having done so, by leveling their land, they were responsible for the damages suffered by plaintiffs. This theory'was adopted by the trial court in its findings.

The judgment is drawn upon another theory. It gave plaintiffs damages in the sum of $200. It provided that defendants be “perpetually enjoined and restrained from causing by artificial means any surface water to flow from their land onto the land of plaintiffs T.

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Bluebook (online)
41 P.2d 974, 5 Cal. App. 2d 71, 1935 Cal. App. LEXIS 1009, Counsel Stack Legal Research, https://law.counselstack.com/opinion/switzer-v-yunt-calctapp-1935.