Palmer v. Waddell

22 Kan. 352
CourtSupreme Court of Kansas
DecidedJanuary 15, 1879
StatusPublished
Cited by39 cases

This text of 22 Kan. 352 (Palmer v. Waddell) 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
Palmer v. Waddell, 22 Kan. 352 (kan 1879).

Opinions

[353]*353The opinion of the court was delivered by

Horton, C. J.:

On July 10th, 1876, plaintiffs in error •filed their petition in the district court of Atchison county, •claiming damages of the defendant in error for unlawfully •digging ditches and erecting and maintaining certain dams and obstructions in a certain channel and natural watercourse, whereby the water was turned off the land of the defendant, and over the lands of the plaintiffs. The plaintiffs asked judgment in the sum of $2,000 for damages caused by acts of defendant, and further prayed an abatement of the nuisance, and an injunction to prevent further damages. The defendant’s answer was a general denial. At the November term of court, 1877, the cause came on for hearing before a jury. After the plaintiffs had introduced their evidence, the •defendant interposed his demurrer thereto. This was sustained, and the jury discharged. The plaintiffs now bring the case here on error for review.

Counsel for defendant claim the demurrer was rightfully ■sustained, for two reasons: First, They allege the evidence wholly failed to establish any natural water-course where the obstructions were erected, and only showed the defendant protected his premises by ditches and dams from surface-water, which they insist he had the right to keep off his own lands. Second, That plaintiffs were not entitled to recover, because they allege the proof established that the plaintiffs ■had no joint interests in the tracts of land named in the petition, or the possession or occupancy thereof, or the emblements thereon.

The testimony upon the question concerning whether there was a natural water-course upon the premises of defendant, was as follows — one witness testifying:

I knew of a stream of water flowing from the bluff into "Waddell’s land, and out of the western boundary. The ■source is a mile above the fence. Water don’t flow all seasons through it. At its source it flows all the year, but lower down it does not. It runs all the year, except during August. The course of the water could always be traced. Previous to [354]*354the dam, the water went down through Waddell’s farm into the old creek-bed; this bed flowed into Palmer’s and back into Waddell’s. There was a regular channel to the old creek when I first knew it, in 1859.”

Another said:

“Have known Waddell’s land sincé 1854. I moved near Oak mills in the fall of 1854. I knew the stream spoken of; it is the natural outlet of the water that flows on about a section of land. It is a little over a mile from its source to where it was dammed up by Mr. Waddell, near Oak mills. There was a ditch running square across Waddell’s field before the dam was made. Before the ditch was made the water ran down to the bottom, and when it got to the bottom it spread, and as it flowed, it went out to the creek-bed and flowed across Waddell’s place. It rah from the creek-bed down the bottom, and then into the Missouri river. I have known it was accustomed to run in this way since 1855 and 1856.”

On cross-examination this witness said:

“Whenever it rained, more water flowed down over Wad-dell’s lands than any other time. The flowing of the water generally occurred in the spring of the year. The water that flows from the upper country and runs down there, is the water that flows during the heavy falls of rain. The ravine drains the upper country. There are some springs up the hollow — three, I believe. The water flows about 100 to 200 yards from these springs — that is, in an ordinary dry time it runs from 100 to 200 yards from the springs; in rainy seasons the water runs three months down to Waddell’s farm.”

Another testified that—

“The obstruction was placed over what is called a branch. I have known it twelve or fifteen years. It is a mile or a mile and a quarter long, and drains 300 or 400 acres. The branch is fed by the rains that fall.”

On cross-examination, this witness said:

“The water flows from above, and the falling of rain. There are some springs. The water only flowed on the Wad-dell land after the falling of rain; it was only surface-water.”

One of the plaintiffs testified as follows:

“The stream runs in an easterly direction. From the dam to the head of it, it was a mile or over. Water had been running there since 1859. The water came down out of the [355]*355hollow above Oak mills. The stream had banks from a foot up to five feet high; it was five or six feet wide in some places — some places, ten to twelve feet wide. Part of the stream runs the year round, part does not. The stream is fed by springs. Before the erection of the dams, the water ran right across Waddell’s land to the creek-bed, and went round down the creek-bed towards Kickapoo. In 1875, the water came all the way down in the months of March, April and May. In 1876, the water flowed from the first of March until sometime in July. That season was wetter than 1875.”

Other witnesses gave similar testimony.

1-watercourse, instanced. Upon this evidence the case should have been submitted to the jury. Within the rule adopted in Earl v. De Hort, 1 Beas. (N. J.) 280, the channel to the old creek-bed, from whence the waters flowing therein i t ¶ ..... . . , reached the Missouri river, is a natural watercourse — at least, such an accustomed channel through which the water has flowed from time immemorial may fairly be said to possess the attributes of a natural water-course so far as to forbid the diversion, repulsion, or altered transmission of the water, to the injury and damage of adjacent fields and lands.

In the case, supra, it was held that the question whether an outlet for water is a water-course, does not depend upon the quantity of water it discharges. If the face of the country is such as necessarily collects in one body so large a quantity of water, after heavy rains or melting snows, as to require an outlet to some common reservoir, and if such water is regularly discharged through a well-defined channel which the force of the water has made for itself, and which is the accustomed channel through which it flows and has flowed from time immemorial, such channel is a natural water-course. The evidence in this case clearly tended to show that in times of heavy rains and in the spring seasons of every year, as far as the memory of man runs, the surface of the ground, back a mile and over from the Missouri river, is such as to collect the water falling on a large section of country to such an extent as requires an outlet to the river through the bottom or low lands at the foot of the bluffs, and [356]*356that the flow of the water had produced a definite or natural channel through the land of defendant and of other persons where such accumulated surplus water had been always accustomed to run. With this view, this water-course could not be obstructed rightfully to the injury of other lands, or the waters running thereon turned upon them to their damage; and the action of Waddell, if it had this effect, was wrongful. The adoption of this rule seems most reasonable, and to be dictated by sound public policy. When Waddell purchased his land, he had knowledge of this channel, and the condition of the surface of the surrounding country which caused the collection of the surface-water to seek an outlet through it.

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Bluebook (online)
22 Kan. 352, Counsel Stack Legal Research, https://law.counselstack.com/opinion/palmer-v-waddell-kan-1879.