Simmons v. Winters

27 P. 7, 21 Or. 35, 1891 Ore. LEXIS 9
CourtOregon Supreme Court
DecidedJune 24, 1891
StatusPublished
Cited by66 cases

This text of 27 P. 7 (Simmons v. Winters) is published on Counsel Stack Legal Research, covering Oregon Supreme Court primary law. Counsel Stack provides free access to over 12 million legal documents including statutes, case law, regulations, and constitutions.

Bluebook
Simmons v. Winters, 27 P. 7, 21 Or. 35, 1891 Ore. LEXIS 9 (Or. 1891).

Opinion

Lord, J.

This is a suit in equity, brought by the plaintiff to enjoin the defendant from diverting the waters [39]*39of a certain stream commonly known as Sheep Creek ditch, and for damages. The waters of Sheep Creek ditch flow through the lands of the plaintiff and the defendant. The theory upon which the suit is predicated, is that Sheep Creek ditch is an ancient and natural watercourse, with well-defined banks and channels, to the uninterrupted flow of which the plaintiff is entitled as a riparian owner, and by the diversion of which he has already been damaged, and will be irreparably damaged unless the defendant be restrained and enjoined. The facts alleged being denied, the defense set up was prior appropriation of the waters of Little Sheep creek by means of a dam, ditches and dry ravines, or draws, into what is commonly known as Sheep Creek ditch for the purpose of irrigation, stock and domestic uses.

The legal aspect of the case involves an inquiry into (1) what constitutes a watercourse; (2) the quantity of water to which an appropriation is restricted; and (3) the nature of the water right which may pass as appurtenant to the premises conveyed.

Considering these in their order, the inquiry is, what is included within the term watercourse? When there is a living stream of water, within well-defined banks and channel, no matter how limited may be its flow of water, there is no difficulty in determining its character as a watercourse. But when the stream is of that class which periodically or occasionally flows through ravines, gullies, hollows or depressions in land, and by its flow assumes a definite channel, such as indicates the action of running water, there is often some difficulty of distinction.

A watercourse is defined by Bigelow, J., as “ a stream of water usually flowing in a definite channel, having a bed or sides or banks, and usually discharging itself into some other stream or body of water.” (Luther v. Winnisimmet Co. 9 Cush. 174.) It is “a living stream with defined banks and channels, not necessarily running all the time, but fed from other and more permanent sources than mere sur[40]*40face water.” (Jeffers v. Jeffers, 107 N. Y. 650.) The size of the stream is immaterial, but “it must be a stream in fact as distinguished from mere surface drainage occasioned by freshets or other extraordinary causes, but the flow of water water need not be constant.” (Pyle v. Richards, 17 Neb. 182.) It is defined in Eulrich v. Richter, 37 Wis. 226, to be “a stream of water usually flowing in a certain direction, in a regular channel, with bed and banks. But the water need not flow continually — the channel may be sometimes dry.” “ There must, however, always be substantial indication of the existence of a stream which is ordinarily and most frequently a moving body of water.” (Weis v. City of Madison, 75 Ind. 253; 39 Am. Rep. 135.)

“A watercourse,” says Mr. Angelí, “consists of bed, bank and water; yet the water need not flow continually, and there are many watercourses which are sometimes dry. There is, however, a distinction to be taken in law between a regular flowing stream of water, which at certain seasons is dried up, and those occasional bursts of water, which in times of freshets or melting of ice or snow, descend from the hills and inundate the.country.” (Angelí on Watercourses, § 4.) The distinction is, as Hawley, C. J., said, “that it is a flowing stream of water — a watercourse as distinguished from water flowing through hollows, gulches or ravines only in times of rain or melting snow.” (Barnes v. Sabron, 10 Nev. 237.) “ Such hollows or ravines,” said Dixon, C. J., “ are not in legal contemplation watercourses.” (Hoyt v. City of Hudson, 27 Wis. 656; 9 Am. Rep. 473.) But, “if the face of the country is such,” said Beasley, C. J., “as necessarily to collect in one body so large a quantity of water, after heavy rains and the melting of large bodies of snow as to require an outlet, 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 an ancient natural watercourse.” (Earl v. De Hart, 12 N. J. Eq. 280.) “In a broken and bluffy region of country,” said [41]*41Mitchell, J., “intersected by long, deep gullies or ravines, surrounded by high; steep bills or bluffs, down wbicb large quantities of water from rain or melting snow rusb with tbe rapidity of a torrent, often attaining tbe volume of a small river, and usually following a well-defined channel, * * * sucb streams partake more of tbe nature of natural streams tban of ordinary surface waters, and must at least to a certain extent be governed by tbe same rules.” (McClure v. City of Red Wing, 28 Minn. 186.)

In Gibbs v. Williams, 25 Kan. 214; 37 Am. Rep. 241, it is held where surface water from rains and snow in a hilly country seeks its outlet through a gorge or ravines, and by its flow assumes a definite channel with well-defined banks, such as will present to the casual’ glance tbe unmistakable evidence of tbe frequent action of running water, and through wbicb at regular seasons tbe water flows, and has done so immemorially, sucb stream is a natural watercouse. In West v. Taylor, 16 Or. 172, Strahan, J., said that “water wbicb has accumulated from spring rains and melting snows, and wbicb has flowed several miles between regular banks of a well-defined watercourse * * * must be deemed a watercourse.”

Tbe conclusion to be deduced from these decisions is, that a watercourse is a stream of water usually flowing in a particular direction, with well-defined banks and channels, but that tbe water need not flow continuously — tbe channel may sometimes be dry; that tbe term watercourse does not include water descending from tbe hills, down tbe hollows and ravines, without any definite channel, only in times of rain and melting snow, but that where water, owing to tbe billy or mountainous configuration of tbe country accumulates in large quantities from rain and melting snow, and at regular seasons descends through long, deep gullies or ravines upon tbe lands below, and in its onward flow carves out a distinct and well-defined channel, which even to the casual glance bears tbe unmistakable impress of tbe frequent action of running water, and through wbicb it has flowed [42]*42from time immemorial — such a stream is to be considered a watercourse and to be governed by the same rules.

In this state, the doctrine of the right to water by prior appropriation for mining or irrigating lands has not been adopted or applied, except as the parties have acquired their rights under the act of congress of 1866. Nor has there been any legislation by the state upon the subject. By the act of congress, the right to water by prior appropriation from the streams upon the public domain was recognized and established. But the appropriation, said Mr. Justice Field, “is limited in every case in quantity and quality by the uses for which the appropriation is made.” (Atchison v. Peterson, 20 Wall. 514.) The measure of the right of the first appropriation of the water, as to extent, follows the nature of the appropriation, or the uses for which it is taken. (Ortman v. Dixon, 13 Cal.

Free access — add to your briefcase to read the full text and ask questions with AI

Related

WaterWatch of Oregon v. Water Resources Dept.
501 P.3d 507 (Oregon Supreme Court, 2021)
Klamath Irrigation District v. United States
227 P.3d 1145 (Oregon Supreme Court, 2010)
Fleck v. Neal
514 P.2d 1101 (Oregon Supreme Court, 1973)
Wellman v. Kelley & Harrison
252 P.2d 816 (Oregon Supreme Court, 1953)
Oliver v. Skinner and Lodge
226 P.2d 507 (Oregon Supreme Court, 1951)
Tudor v. Jaca
165 P.2d 770 (Oregon Supreme Court, 1946)
United States v. Florea
68 F. Supp. 367 (D. Oregon, 1945)
Dill v. Killip
147 P.2d 896 (Oregon Supreme Court, 1944)
Coxl v. Campbell
143 S.W.2d 361 (Texas Supreme Court, 1940)
Mogle v. Moore
104 P.2d 785 (California Supreme Court, 1940)
State v. Hiber
44 P.2d 1005 (Wyoming Supreme Court, 1935)
Broughton v. Stricklin
30 P.2d 332 (Oregon Supreme Court, 1934)
Bothwell v. Keefer
27 P.2d 65 (Idaho Supreme Court, 1933)
Turner v. Big Lake Oil Co.
62 S.W.2d 491 (Court of Appeals of Texas, 1933)
Rio Bravo Oil Co. v. Weed
50 S.W.2d 1080 (Texas Supreme Court, 1932)
East Bay Sporting Club v. Miller
161 N.E. 12 (Ohio Supreme Court, 1928)
Lakeside Irrigation Co. v. Markham Irrigation Co.
285 S.W. 593 (Texas Supreme Court, 1926)
Hildebrandt v. Montgomery
234 P. 267 (Oregon Supreme Court, 1925)
J.W. Turvey v. J.C. Kincaid
226 P. 219 (Oregon Supreme Court, 1924)
Murphy v. Kerr
296 F. 536 (D. New Mexico, 1923)

Cite This Page — Counsel Stack

Bluebook (online)
27 P. 7, 21 Or. 35, 1891 Ore. LEXIS 9, Counsel Stack Legal Research, https://law.counselstack.com/opinion/simmons-v-winters-or-1891.