City of San Bernardino v. City of Riverside

198 P. 784, 186 Cal. 7, 1921 Cal. LEXIS 409
CourtCalifornia Supreme Court
DecidedJune 3, 1921
DocketL. A. No. 5925.
StatusPublished
Cited by64 cases

This text of 198 P. 784 (City of San Bernardino v. City of Riverside) 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 San Bernardino v. City of Riverside, 198 P. 784, 186 Cal. 7, 1921 Cal. LEXIS 409 (Cal. 1921).

Opinion

SHAW, J.

Both parties have appealed from the judgment.

The city of San Bernardino is situated in what is known as the San Bernardino artesian basin, and the lands com *11 prising it overlie a part of the subterranean water of said basin. The dispute in the case arises from the fact that both parties are taking such subterranean waters, the plaintiff taking them for the use of its inhabitants for domestic and other purposes, and the defendants taking them to be transported to the city of Riverside and the vicinity thereof for irrigation and domestic use, said region being entirely outside of the said basin and of the watershed which supplies water thereto. The complaint asks that the claims and rights of each of the parties be determined and adjudicated and that the defendants be enjoined from diverting water from said basin for use upon lands not situated therein or in the watershed tributary thereto.

The answer sets up the several claims of the defendants to the water aforesaid and denies that plaintiff has any paramount rights thereto. The defendants also filed a cross-complaint asking that their rights to take water from said basin should be determined and adjusted.

The court made elaborate findings in the case, covering three hundred pages in the printed transcript. Judgment was thereupon rendered, declaring the respective rights of the several parties in the water of the said basin. It was stipulated between the parties that “whatever judgment may legally be entered as based on the findings of fact may be entered regardless of whether the findings, or any of them, are or are not embraced in the pleadings as filed.” The appeal is presented upon the judgment-roll alone, and, in view of the aforesaid stipulation, our consideration of the case may be limited to a review of the findings, conclusions of law and judgment. The facts hereinafter stated are set forth in the findings.

The San Bernardino artesian basin is a plain, sloping generally toward the southwest. It is about twenty-five miles long from northwest to southeast, and ten miles wide. It is bounded on the northwest, north, and east by high mountains, and on the west, south, and southeast by hills or higher lands. At the southwest, near the town of Colton, there is a gap in the hills and higher lands, through which the water falling on the watershed, of which the basin is the lower part, escapes, partly by streams on the surface and partly by seepage through the sands, gravels, and soil beneath. The gradient of the surface of the basin from the *12 foot of the mountains toward this outlet varies from twenty-five to fifty feet per mile. Near the center there are level spaces which, prior to any artificial drainage, were swamps or marshes. It is probable that the basin was originally a lake and that its present condition is the result of the gradual filling of the bed in the course of ages by detritus washed down from the adjacent mountains. The material of the basin is composed of boulders, gravel, sand, and soils of varying textures. As the lake-bed gradually filled, the torrents from the mountain canyons changed their courses from time to time, forming underground' strata or waterways of coarser material in which water percolates more freely than elsewhere. The material also lies in strata of varying permeability. In the adjacent mountains there are several canyons, in each of which a small stream generally flows in the dry season, and from each of which a large stream flows when there is a heavy rain upon its watershed. Of these the largest are Santa Ana River at the easterly end and Lytle Creek at the northwest. At the mouth of each canyon where it emerges from the mountains there is the usual debris cone of the coarser materials, such as boulders and gravel. In these cones a large portion of the water of the respective streams sinks and disappears. The Santa Ana River and Lytle Creek are the only streams that continue flowing on the surface as far as the outlet, and not infrequently in the dry season they also disappear before reaching it. The porous material filling the bed of the ancient lake is at least one thousand feet in depth in some places. The outlet, it is believed, was originally a narrow gorge, which has become filled to the surface with material sufficiently impervious to water to serve as a dam and prevent the escape of water below the surface to any great extent. The whole mass of underlying strata composing this basin is saturated with water. The upper stratum is soil of a closer texture than the strata beneath. This overlying cap confines the water to the porous strata below, and the gradient of these formations causes a hydrostatic pressure therein. This pressure forces to the surface a large part of the water, beginning near Harlem Springs, six miles from the outlet, and forms a stream known as Warm Creek. This stream gradually increases in volume in its course toward the outlet, at which point, before any artificial *13 depletion of the waters of the basin, there was ordinarily a flow amounting to three thousand five hundred inches of water. A smaller creek of similar origin, called Town Creek, is tributary to Warm Creek. Both pass through the city of San Bernardino. As early as 1869 a well was sunk in the basin, in which the water rose to the surface and flowed out as a stream. Prom that time until the present it has been a common custom for persons owning land over this basin and desiring water to obtain the same by means of such artesian wells. There are now between two thousand and three thousand of them, and by means thereof large quantities of water are taken from the underground supply. Owing to the large number of these wells the pressure in the strata has decreased so that many of them do not flow over the surface, and pumps are used to raise the water.

Before proceeding to the specific questions presented we deem it advisable to state some general principles of law on the subject of the waters of streams and artesian basins, which must be kept in mind in the consideration of the case.

[1] 1. The original rights to the waters of the streams in this state are those which by the common law were vested in the owners of the land abutting upon the stream, under the doctrine of riparian rights, as it is commonly termed. (Lux v. Haggin, 69 Cal. 255, [4 Pac. 919, 10 Pac. 674]; Hudson v. Dailey, 156 Cal. 628, [105 Pac. 748]; Palmer v. Railroad Commission, 167 Cal. 165, [138 Pac. 997].) Such rights are attached to the land as parcel thereof, and, of course, are private property. It is not necessary here to state the doctrine more fully, since there are no serious differences between the parties concerning it. We do not speak in this case of the public rights of navigation and fishery in navigable waters.

[2] It follows in consequence of this fact that all other present existing rights in the waters of streams have been acquired in some manner from the owners of such abutting lands, either by prescription, by contract, or by condemnation. Appropriation under the Civil Code is but another form of prescription, and the original rights of the abutting land owners are not divested thereby until the period of prescription has run in favor of the appropriator.

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

Related

Wang v. Ehang Holdings Limited
N.D. California, 2020
Great Oaks Water Co. v. Santa Clara Valley Water Dist.
196 Cal. Rptr. 3d 171 (California Court of Appeals, 6th District, 2015)
Great Oaks v. Santa Clara Valley Water Dist.
California Court of Appeal, 2015
In re: Havy Nguyen
Ninth Circuit, 2012
El Dorado Irrigation District v. State Water Resources Control Board
48 Cal. Rptr. 3d 468 (California Court of Appeal, 2006)
State of California v. Superior Court
93 Cal. Rptr. 2d 276 (California Court of Appeal, 2000)
Pleasant Valley Canal Co. v. Borror
61 Cal. App. 4th 742 (California Court of Appeal, 1998)
People v. Shirokow
605 P.2d 859 (California Supreme Court, 1980)
City of Los Angeles v. City of San Fernando
537 P.2d 1251 (California Supreme Court, 1975)
Jarvis v. State Land Department
479 P.2d 169 (Arizona Supreme Court, 1970)
Finley v. Teeter Stone, Inc.
248 A.2d 106 (Court of Appeals of Maryland, 1968)
Orange County Water District v. City of Colton
226 Cal. App. 2d 642 (California Court of Appeal, 1964)
California Water Service Co. v. Edward Sidebotham & Son, Inc.
224 Cal. App. 2d 715 (California Court of Appeal, 1964)
Miller & Lux, Inc. v. Bank of America
212 Cal. App. 2d 719 (California Court of Appeal, 1963)
County of Tuolumne v. State Board of Equalization
206 Cal. App. 2d 352 (California Court of Appeal, 1962)

Cite This Page — Counsel Stack

Bluebook (online)
198 P. 784, 186 Cal. 7, 1921 Cal. LEXIS 409, Counsel Stack Legal Research, https://law.counselstack.com/opinion/city-of-san-bernardino-v-city-of-riverside-cal-1921.