City of Los Angeles v. Hunter

105 P. 755, 156 Cal. 603, 1909 Cal. LEXIS 367
CourtCalifornia Supreme Court
DecidedDecember 1, 1909
DocketL.A. No. 2140.
StatusPublished
Cited by22 cases

This text of 105 P. 755 (City of Los Angeles v. Hunter) is published on Counsel Stack Legal Research, covering California Supreme Court primary law. Counsel Stack provides free access to over 12 million legal documents including statutes, case law, regulations, and constitutions.

Bluebook
City of Los Angeles v. Hunter, 105 P. 755, 156 Cal. 603, 1909 Cal. LEXIS 367 (Cal. 1909).

Opinion

HENSHAW, J.

The suit of the City of Los Angeles v. Hunter et al. is an action against forty-seven owners of land in the San Fernando Valley, to quiet title in the plaintiff to its asserted paramount right to the use of the waters of the Los Angeles River. The case of the City of Los Angeles v. Buffington et al. is an action against one hundred and sixty owners or tenants of land in the same valley, brought for the same purpose, and also to obtain an injunction restraining the defendants from making any diversion of water from the river when it is required by the city for supplying its municipal and domestic needs. The actions were tried together, and from the judgments which followed in favor of the city the defendants appeal. The legal propositions presented upon all appeals are substantially identical.

Saving certain minor objections going to the introduction or rejection of evidence, the principal contentions of appellants *605 are: 1. That the waters which they were taking by means of wells were not waters of the Los Angeles River; and, 2. If they were waters of the Los Angeles River, the city of Los Angeles had no superior right to the use of them.

The lands of these defendants, embracing in all about five thousand acres, are situated in the southeastern portion of the San Fernando Valley, where the surrounding mountains draw together and form what is called the “Narrows.” A description of the San Fernando Valley, adequate for all the purposes of this consideration, will be found in City of Los Angeles v. Pomeroy, 124 Cal. 597, [57 Pac. 585]. The cases of Katz v. Walkinshaw, 141 Cal. 116, [99 Am. St. Rep. 35, 70 Pac. 663, 74 Pac. 766], and McClintock v. Hudson, 141 Cal. 275, [74 Pac. 849, together with the Pomeroy case above cited, give so full and satisfactory an account of the water conditions existing, not alone generally in the arid portions of this state, but particularly of the conditions existing and controlling the considerations of the questions here presented that a reference to them renders unnecessary any detailed description.

The defendants were using water pumped from wells of various depth, which wells were situated at an average distance of about one thousand feet from the surface border of the Los Angeles River, though in instances the distances of certain wells were two or three miles. The contention of the city is that these wells abstracted water belonging to the Los Angeles River, to the use of all of which water it has a paramount right. The court so found. The defendants’ contention is twofold: 1. That the waters are strictly percolating waters, not belonging to the subterranean flow of the stream, but if concededly on the way to join and swell such flow, still percolating waters, to the use of which, as owners of the land, they have an absolute indefeasible right; 2. That over all the San Fernando Valley extends a clay blanket, impervious to water, underlying which blanket are water-bearing gravels; that the waters above this blanket feed the Los Angeles River, while the waters below this blanket do not; that they draw their well waters from the gravels below the blanket, and, therefore, conceding that the city of Los Angeles has a paramount right to the use of the waters of the river, they are not trespassing upon this right.

*606 The court rejected both of these contentions in the following findings:—

“That the waters of said river, in its course through said valley, penetrate into and completely fill the voids of said permeable material, down to bedrock, under the surface channel of said river, and on both sides of said channel, throughout the whole width of said valley, from a point at or above the level of the surface stream of said river down to bedrock.
“It is not true, as alleged in the answers herein, that none of the underground waters in any of the lands of the defendants, described in the amended complaint herein, are part of the Los Angeles River, mentioned in the said amended complaint, or of the waters thereof, but are waters percolating in said lands, and forming a part of the soil thereof, so as not to constitute a stream or watercourse; but, on the contrary, the court finds that all of the underground waters in all of said lands, from the surface of the ground down to bedrock, are flowing waters, and are part of the subterranean stream of said Los Angeles River.”

By these findings the court adopts the theory which is supported by the evidence of certain of the experts, that the waters of the Los Angeles River proper entering the valley sink to bedrock and spread out laterally, filling all the voids of the soil, and so move slowly down to the Narrows, where the Los Angeles River, owing to the declension in that direction of the land surface, appears as a visible stream. It is earnestly contended, against this finding that it takes no account of proved conditions; that it treats this great valley as being all a part of the Los Angeles River, and that in so doing it stultifies physical and geological facts; that it eliminates from consideration the rainfall upon the surface of the valley,—the water from all the surrounding mountains which not following well-defined channels, still by gravity is carried down and sinks into the valley lands; that the water flowing into the valley by numerous channels and sinking into the lands of the valley miles distant from the thread of the river, is by this finding treated as part of the stream long before, in the course of nature, it can have reached the true subterranean flow thereof. So it is insisted by appellants that these waters are strictly percolating waters, and that of them *607 they have the common-law right of absolute ownership, as modified in this state only by the doctrine of Katz v. Walkinshaw,— namely, that the quantum of water which they use shall be in reasonable proportion to the whole thereof, and that the water so taken shall be used upon the surface soil of the basin, or, at least, not carried away for exterior use, to the injury of any owners of the land within the basin.

But in the view which we take, it is immaterial whether the San Fernando Valley be considered a great basin, saturated by water from the inflow of the Los Angeles River and its tributaries, or saturated as a result of all the causes which appellants assign. In passing, it will suffice to say that the court was justified, upon a conflict in the evidence, in rejecting the theory of the clay blanket covering the valley at a varying depth. Unquestionably the San Fernando Valley is the great natural reservoir and supply of the Los Angeles River. Unquestionably the cutting off of this supply would as completely destroy the Los Angeles River as would the cutting off of the Great Lakes destroy the St. Lawrence. San Fernando Valley may indeed be regarded as a great lake filled with loose detritus, into which the drainage from the neighboring mountains flows, and the outlet of which is the Los Angeles River. Impeded by the soils, these waters of course move more slowly than they would in an open lake. But unquestionably the general movement of practically all is southeasterly to the Narrows, through and out of which flows the Los Angeles River proper.

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Bluebook (online)
105 P. 755, 156 Cal. 603, 1909 Cal. LEXIS 367, Counsel Stack Legal Research, https://law.counselstack.com/opinion/city-of-los-angeles-v-hunter-cal-1909.