6 Or. 198 | Or. | 1876
The rules of law applicable to this case seem to be well settled. Every proprietor of land through which flows a stream of water, has a right to the use of the water flowing in its natural channel without diminution or obstruction. (Wash, on Ease. 215.) The same rule applies to water which flows in a well defined and constant stream in a subterranean channel. (Angel on W. C., sec. 112; Wash, on Ease. 364); but it does not apply to water percolating through the soil or even flowing through an unknown and undefined channel. (Wash, on Ease. 210; Id. 364.) These rules, together with the maxim that every person may use his own property as he pleases, provided such use is not an injury to another, are, we think, all the principles of law necessary to a decision of the case. The only question to be decided by us is one of fact. Doe$ the evidence before us prove the existence af a constant and well defined. stream of water flowing in a subterranean channel, swale, spring or basin on the land of defendants described in the pleadings and evidence to the spring described as Taylor & White’s spring, in the evidence and upon the maps used in the argument before us, prior to the digging of the ditch complained of? It appears from the evidence, that the distance from the basin to Taylor & White’s spring is about three hundred and thirty feet; that the spring is about seventy feet lower than the basin, and that between them is a ridge rising from eleven to fifteen feet above the basin, composed of trap rock and earth. It is the theory Of respondent that the waters of the basin, prior to July 28, 1874, the date of the construction of the ditch complained of, flowed in a well defined channel through this ridge to the spring known as Taylor & White’s spring. No witness testifies that he ever saw such a channel, or that he knows of its existence. Several witnesses for plaintiff
One witness for plaintiff, it is true, testifies that there was formerly, at a point about thirty feet above Taylor & White’s spring a hole six or eight inches in diameter through which water could be seen flowing in a full strong channel in the direction of the spring. When we consider that this point was three hundred feet from the basin and only thirty feet from the spring, and that a wet, boggy place intervened, we cannot attach much importance to the evidence. This fact is entirely consistent with the waters being derived from percolation through the hill from the' basin, or with the water being derived from’ some other source. A number of other theories, more or less probable, have been suggested, but as in our opinion the evidence fails to establish that of plaintiff with sufficient