Singleton v. Atchison, Topeka & Santa Fe Railway Co.

72 P. 786, 67 Kan. 284, 1903 Kan. LEXIS 248
CourtSupreme Court of Kansas
DecidedJune 6, 1903
DocketNo. 13,195
StatusPublished
Cited by8 cases

This text of 72 P. 786 (Singleton v. Atchison, Topeka & Santa Fe Railway Co.) is published on Counsel Stack Legal Research, covering Supreme Court of Kansas primary law. Counsel Stack provides free access to over 12 million legal documents including statutes, case law, regulations, and constitutions.

Bluebook
Singleton v. Atchison, Topeka & Santa Fe Railway Co., 72 P. 786, 67 Kan. 284, 1903 Kan. LEXIS 248 (kan 1903).

Opinion

The opinion of the court was delivered by

Pollock, J. :

This action was brought by T. C. and S. M. Singleton against the railway company to recover damages caused by the obstruction of an alleged watercourse which produced an overflow of plaintiffs’ [285]*285lands, destroying crops growing thereon. The jury returned a general verdict for plaintiffs, with answers to special questions as follows :

”1. When was the railroad embankment across plaintiffs’ lands which they allege caused their damages constructed?' A. In 1886.
”2. What company constructed said embankment? A. Chicago, Kansas & Western Railroad Company.
”3. What company owned the line of railroad running across plaintiffs’ lands in May, 1898, and which.they allege caused the damages complained of in their petition? A. Chicago, Kansas & Western.
”4. What company was operating said line of railroad in May, 1898? A. Atchison, Topeka & Santa Fe Railway Company.
”5. Is the land of plaintiffs mentioned in their petition bottom land? A. It is. ■
”6. Are there any hills or bluffs on or around the land described in plaintiff’s petition? A. Higher ground east of railroad, but no defined bluffs.
”7. Did any water of any consequence flow into the depression alleged to be a natural watercourse ex-* cept such as in times of very high water in the Verdigris river overflowed its banks, flowed over such depression across a portion of plaintiffs’ lands, and again flowed into said river south of plaintiffs’ lands? A. Very little water flows into depression except what flows from river at times of reasonably high water.
”8. Does the depression claimed by plaintiffs to be a natural watercourse extend to any high bluffs ? A. No.
”9. Did any of the water that flowed into or through said depression come from high bluffs or gorges between bluffs ? A. No.”
”11. For what distance does said depression extend over lands of the plaintiffs ? A. From the river to railroad.
”12. Did any water except surface-water falling upon a portion of plaintiffs’ lands flow through said depression across plaintiffs’ lands except when the [286]*286Verdigris river overflowed its banks ? A: Yes, when river was three-fourths full.
“13. If you answer the last preceding question in the affirmative, then state what portion of the year, if any, water flowed through said depression, and from what source. A. During the time of freshets ; from the Verdigris river. . ■ ,
“14. Is it not a fact that, prior to the construction of the railroad embankment complained of in plaintiffs’ petition, persons owning land east and southeast of said line of railroad dug a ditch or drain in the direction of a watercourse which flowed from the high land where the town of Benedict is situated, which said named watercourse flowed through ‘Reed’s branch’ into the Verdigris river? A. Yes, for the purpose of draining some swampy land east of the natural watercourse in question.
“15. Did not the water flowing through said depression, during the time of an overflow of the Verdigris river, again flow into said river through said ‘Reed’s branch’? A. Yes.
“16. Is not the land south and southeast of the point where said depression intersects the line of said railroad now in cultivation ? A. Yes.
“17. How much of plaintiffs’ land lying south and east of the Verdigris river was in cultivation in May, 1898? A. About eighty acres.
“18. What kind of crops, if any, were growing on plaintiffs’ land lying south and east of the Verdigris river in May, 1898? A. Corn.
“19. In the event that you find for the plaintiffs, then state how much you award them for injury to crops on the south and east side of the Verdigris river, and also for injury to crops on the north and west side of river, to wit. A. South and east side of river, $80 ; north and west side of river, $1020.”

On motion judgment for costs was entered for defendant on the special findings, notwithstanding the general verdict. Plaintiffs bring error.

The findings of the jury sufficiently disclose the na[287]*287ture of the case and render a statement of the facts unnecessary. The propositions relied on in support of the judgment rendered are that no natural watercourse was obstructed; and consequently defendant is not liable. The property overflowed was situate in a bend of the Verdigris river. The findings disclose that in times of high water, when the banks of the river were three-fourths filled with water, at the place in question a portion of the water would leave the regular channel, flow across the bend, and again intercept-the regular flow lower down the river. The question is, Does the obstruction of the flow of water under such conditions constitute the obstruction of a natural watercourse and render the obstructor liable for ensuing damages ? The solution of the problem depends on the legal definition of the term “watercourse” or “natural watercourse”; for if water so flowing be surface-water, as contradistinguished from water flowing in a natural watercourse, it is conceded tp be a common enemy against which all may lawfully impose obstruction at will.

This court has considered questions akin to' that here presented. It is contended by counsel for plaintiffs that the findings of the jury bring this case within the definition of a natural watercourse as stated in Palmer v. Waddell, 22 Kan. 352, and as limited in the of case Gibbs v. Williams, 25 Kan. 214, 37 Am. Rep. 241. In Palmer v. Waddell, it was held:

“Where surface-water having no definite source is supplied from falling rains and the melting snow from a hilly region or high bluffs, and owing to the natural formation of the surface of the ground is forced to seek an outlet through a gorge or ravine, and by its flow assumes a definite or natural channel, and escapes through such channel regularly during the spring months of every year, and in seasons of heavy [288]*288rains, and such has always been the case so far as memory of man runs, held, that such accustomed channels through which the waters flow may fairly be said to possess the attributes of a natural watercourse.”

In Gibbs v. Williams, 25 Kan. 214, it was held :

“In order to create the exception noticed in Palmer v. Waddell, 22 Kan. 352, it is not sufficient that the conformation of the surface be such that the water falling on a large tract of land naturally flows upon and over a depression at one end of that tract; there must be a necessity for the outflow over this depression in order to prevent the flooding of a considerable body of land, and there must be a distinct channel, with well-defined banks, cut through the turf and into - the soil by the flowing of the water ; the bed of a stream, or something which will present on casual glance to every eye the unmistakable evidences of the frequent action of running water.”

The case of Palmer v. Waddell

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Bluebook (online)
72 P. 786, 67 Kan. 284, 1903 Kan. LEXIS 248, Counsel Stack Legal Research, https://law.counselstack.com/opinion/singleton-v-atchison-topeka-santa-fe-railway-co-kan-1903.