Hinton v. Little

296 P. 582, 50 Idaho 371, 1931 Ida. LEXIS 24
CourtIdaho Supreme Court
DecidedFebruary 21, 1931
DocketNo. 5482.
StatusPublished
Cited by11 cases

This text of 296 P. 582 (Hinton v. Little) is published on Counsel Stack Legal Research, covering Idaho Supreme Court primary law. Counsel Stack provides free access to over 12 million legal documents including statutes, case law, regulations, and constitutions.

Bluebook
Hinton v. Little, 296 P. 582, 50 Idaho 371, 1931 Ida. LEXIS 24 (Idaho 1931).

Opinions

*373 GIVENS, J.

The complaint alleges and the affidavits in support of the temporary injunction are of similar effect, and the testimony of the witness for the plaintiffs on the hearing in regard to the temporary injunction, shows unde-nied and undisputed except by defendants’ answer, which merely generally denies the allegations of the complaint, that the territory in question is underlaid at a depth of from two to three hundred feet, and beneath an impervious stratum, by subterranean waters confined horizontally between this upper impervious stratum and lower stratum, of such a nature as to force this subterranean water when artificial openings are made in the upper stratum to, and in some instances above, the surface of the ground. Laterally the subterranean waters are evidently continuous and permeate throughout the basin, inasmuch as the allegations and evidence show that the flow of all the wells are more or less interdependent and are affected by the increased or diminished flow of each well. The engineer for the plaintiffs further testified that the water entered this subterranean basin from high mountains lying to the south of the basin. *374 Evidently there is thus some movement of this water at least into the basin from the south and laterally beneath the ground and between the different wells.

Respondents contend that the same rule is to be applied to the appropriation of these subterranean waters as is applied to surface waters, namely, first in time is first in right. Appellants contend on the other hand for either what is known as the English or common-law doctrine, that the owner of the surface of the ground owns all the water within his land, or the so-called American doctrine. It is evident that the English doctrine cannot be applicable because when any one of the land owners in question, so far as the evidence now shows, takes water from his well, it diminishes the flow in the other wells; hence it would seem apparent that he is taking not alone that which belongs to him, as underlying his land, but is in some measure at least, taking either directly or indirectly that which comes from underneath the land of other owners. Appellants contend for what is sometimes called the American, or the .correlative use doctrine, in effect this, that under circumstances as disclosed above, each surface owner is entitled to take his proportionate share of the entire body of underground water, in the particular basin underlying the lands in question and affected by the different wells. There are numerous authorities which sustain the English doctrine and there are authorities which define and sustain the American doctrine of correlative use, the first case probably clearly announcing the American doctrine being Katz v. Walkinshaw, 141 Cal. 116, 99 Am. St. 35, 70 Pac. 663, 74 Pac. 766, 64 L. R. A. 236. Without attempting to enumerate, cite, examine or distinguish all of the decisions from the different jurisdictions, which have had occasion to touch upon this question, there are in this state four decisions which bear upon the question.

Appellants contend that King v. Chamberlin, 20 Ida. 504, 118 Pac. 1099, 1100, and Public Utilities Com. v. *375 Natatorium Co., 36 Ida. 287, 211 Pac. 533, sustain their doctrine, and respondents contend that Le Quime v. Chambers, 15 Ida. 405, 98 Pac. 415, 417, 21 L. R. A., N. S., 76, and Bower v. Moorman, 27 Ida. 162, Ann. Cas. 1917C, 99, 147 Pac. 496, 500, sustain their position. From an analysis of these four cases and a consideration of the legislative enactments therein cited, with regard to subterranean waters, we have a fairly well-defined announcement both by this court and the legislature as to what rule is to be applied in this state in connection with the appropriation of underground waters. It appears to be now fairly well settled that all underground subterranean waters are percolating waters, that is, that there is more or less movement, both perpendicular and horizontal, through the earth and rocks. Therefore, whether underground waters move in a well-defined channel, either in a generally confined direction as to the points of the compass or spread out laterally, is merely a question of difference or degree.

It would seem, therefore, that it is impossible to attempt to lay down one rule with regard to subterranean waters, existing more or less as a relatively stationary body of water under the ground, and subterranean waters in which there, is a decided movement. In any event, the facts in the case at bar show that there is movement of the underground waters involved in this litigation and we need pass herein op no other situation.

In Le Quime v. Chambers, supra, a spring upon certain land at no time prior to its diversion flowing a sufficient quantity or volume to form a surface stream or carry any water beyond the limits of the subdivision on which it arose, was appropriated. The land on which the spring arose was filed upon by one Irwin. Upon a contest Chambers was given a preference right to file on the land and tore up Le Quime’s pipe, which he had theretofore used to convey the water in question to other lands. Chambers contended, as the appellants do herein, that the ownership of the land *376 gave him the exclusive right to this water. Le Quime contended that the water was subject to appropriation, and he being prior in point of time was entitled to it, though the ease really involved water coming naturally to the surface, not by way of an artificial well; the court said in this connection :

“It is next contended by respondent that since the waters going to make up this spring are purely seepage and percolating waters and do not come from any well-defined subterranean stream, they are not subject to location under the laws of this state, and that their appropriation is, therefore, not protected under the act of Congress. In line with this contention it is argued that percolating and seepage waters are as much a part of the land itself as the soil, the rock, and stone found therein, and that such waters are not the subject of appropriation or diversion. The principal ease relied on by respondent in support of this contention is Southern Pac. R. R. Co. v. Dufour, 95 Cal. 615, 30 Pac. 783, 19 L. R. A. 92. In that case it was held that “The law controlling the rights to subterranean waters not running through a channel or defined course is very different from that affecting the rights of surface streams. In the former ease the water belongs to the soil, is a part of it, is owned and possessed as the earth is, — -it may be used, removed and controlled to the same extent by the owner; and no action will lie for injuries caused by cutting it off.’ This case, however, has been distinguished and greatly modified, if not entirely overruled, on this particular point in the more recent cases of Katz v. Walkinshaw, 141 Cal. 116, 99 Am. St. 35, 70 Pac. 663, 64 L. R. A. 236, and opinion on rehearing, 74 Pac. 766, and the case of Cohen v. La Canada L. & W. Co., 142 Cal. 437, 76 Pac. 47.

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Bluebook (online)
296 P. 582, 50 Idaho 371, 1931 Ida. LEXIS 24, Counsel Stack Legal Research, https://law.counselstack.com/opinion/hinton-v-little-idaho-1931.