Thompson v. Andrews

165 N.W. 9, 39 S.D. 477, 1917 S.D. LEXIS 181
CourtSouth Dakota Supreme Court
DecidedNovember 22, 1917
DocketFile No. 4112
StatusPublished
Cited by51 cases

This text of 165 N.W. 9 (Thompson v. Andrews) is published on Counsel Stack Legal Research, covering South Dakota Supreme Court primary law. Counsel Stack provides free access to over 12 million legal documents including statutes, case law, regulations, and constitutions.

Bluebook
Thompson v. Andrews, 165 N.W. 9, 39 S.D. 477, 1917 S.D. LEXIS 181 (S.D. 1917).

Opinion

WPIITING, T.

Plaintiffs sought to enj-oin defendant from continuing to maintain a ditch whereby -he -drained wafers from his land, which wafers were eventually discharged upon and across the lands of plaintiffs. Findings and judgment were for' plaintiffs, and defendant appéaled. The general course of the-[482]*482■drainage in the watershed involved in this action is to- the south. That part of it which has within it the lands of the parties to this action is about 3 miles in length north and south, and contains something over 1,200 acres. The upper mile of such watershed is about a mile across at its widest part, and contains a tract of some 325 acres, the southeastern part of which is appellant’s land. Upon appellant’s land there is a low' flat tract of some 100 acres, on which there accummulates the surface water coming from all of said 323 acres, but no other waters of any kind. The next half mile of such watershed is less than a half mile in width. South of this the watershed gradually widens until, one-half mile farther ■ south, it reaches the land of one respondent. From here it gradually widens .and covens a tract somewhat regular in outline and which is a mile in extent north and south and somewhat more than a mile east and west at the widest place. Respond'ents’ lands all lie within this lower tract. As before noted, the upper mile of such watershed contains some 325 acres. The tract between this and respondents’ lands, being a tract one mile north and south, contains, about 300 acres. The lower tract contains about 650 acres. These lands are all devoted to agriculture. The slope of appellant’s 100-acre tract is to the southeast. It is surrounded 'by a bank. At the lower side of this tract or basin nature left a ditch through -the rim of the bank. This ditch was some 2 feet in depth. Even with this ditch unobstructed there would have to be some 2 feet of water over this basin before any water could overflow through such ditch. It appears undisputed that, when appellant’s land was first settled upon some time prior to 1880, this basin was perfectly dry and produced fine crops of hay. During the -winter of 1880 and 1881 there was an unprecedented fall of snow. When this melted in the spring this basin was' filled. It gradually dried up, but it was at least two or three years before it again became dry. Appellant then broke up this basin and raised crops thereon. About 1894 appellant laid a tile drain underneath the ditch above mentioned, and at a depth sufficient to entirely drain this basin. In. 1909, the title having become clogged, appellant dug an open ditch- along the patch of, the natural ditch and to a depth sufficient to drain such basin; this, ditch did not extend beyound his land, but its lower end opened into a natural swale or depression and the waters from the ditch [483]*483eventually flowed upon and across respondents’ lands. From the lower side of the basin down to where the water first reaches respondent®’ lands -there is a fall of about 25 feet.; and between the point where such water enters upon their lands to the. point where it leaves same, a distance of some three-fourths of a mile, the fall is 21 feet.

The' trial court found’ that the deeping oif the said natural ditch leading from this 'basin' increased1 the flow of water onto respondents’ lands, thus rendering a few acres belonging to each respondent unfit for husbandry. Appellant contends -that the damage complained of was not caused by the deeping of such outlet-, but was the result of unusual rainfall occurring during the years complained- of, and- that the same damage would have been suffered even if the said- basin had retained the water accumulating therein-; he afeo contends that he had a right, in the nature -of an easem-ent, under section 22, c. 134, Laws 1907, as amended by section 11, c. 102, Laws 1909, to -drain such basin through such artificial outlet, even -though by so -doing a greater volume of water was discharged upon the lands of respondents to their damage. Said section 22 reads in pa-rt as follows:

“Owners of land may drain- the same in-the general ■ course of natural drainage, by constructing open or covered drains, discharging the same into’ any natural water course, o-r into- any natural depression," whereby the water will be carried into some natural water -cours-e, or into -some drain on the public highway with the consent -of the board having supervision of such highway, and when such drainage -is wholly upon the owner’s land1 he shall not be liable in- -damages therefor to- any person or persons or corporation.”

[1] Among -those things which the statute -recognizes as essential to this right -of -drainage are: (1) The water must be discharged into a “natural water course,” or into a “natural depression whereby the water will be carried into some natural water course”; (2) The drainage -must be “in the general course of natural drainage.” T-he trial court found' that:

“The water is not discharged from' [appellant’s] said ditch into any natural water course; * * * there is no natural water course upon any of said- lands over and aeróse which said water runs.”

[484]*484The court did find that the water followed “the general course of drainage” the entire distance from appellant’s land down to and across respondents’ lands. The term “water course” has come to have two distinct meanings,; the one when referring to that water course in and to which riparian rights may attach, and the other when -referring to- that’ water course through which an upper land-owner may discharge water from his land. Quinn v. Railway Company, 23 S. D. 126, 120 N. W. 884, 22 L. R. A. (N. S.) 789. As pertaining to drainage this court in the Quinn case adopted, from Lambert v. Alcorn, 144 Ill. 313, 33 N. E 53, 21 L. R. A. 611, the following description or definition of a water course, to which definition- we adhere:

“If the conformation of the land is such as to give to the surface water flowing from one tract to- the other a fixed and -determinate course, so as’ to uniformly discharge it upon the servient -tract at a fixed and definite point, the course thus uniformly followed by the water in its flow is a water course within' the meaning of the rule applicable to that subject. Doubtless such water course can -exist only where there is a ravine, swale, or depression of greater or less depth, and extending from one tract onto -the other, and. so situated as to- gather up the surface water falling upon the dominant tract and to conduct it along a defined course to a definite point of discharge upon the servient tract. But it does not seem to be important that the force of the water flowing from' one tract to the other has not been sufficient to- wear out a channel or canal having definite and well-marked sides or banks. That depends upon the nature of the soil and the force and rapidity of the flow. If the surface water in fact uniformly or habitually flows off over a given course, having reasonable limits as to width, the line of its flow is, within the meaning of the law applicable to- the -discharge of surface water, a water course.”

The course which water took from appellant’s land down to and over respondents’ lands was a “natural water course” under the above decision and as contemplated by the above statute. It is also' clear that such “natural water course” was the “general course of natural 'drainage” for all water flowing from such basin.

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Bluebook (online)
165 N.W. 9, 39 S.D. 477, 1917 S.D. LEXIS 181, Counsel Stack Legal Research, https://law.counselstack.com/opinion/thompson-v-andrews-sd-1917.