City of Los Angeles v. Pomeroy

57 P. 585, 124 Cal. 597, 1899 Cal. LEXIS 1041
CourtCalifornia Supreme Court
DecidedJune 3, 1899
DocketL. A. No. 419
StatusPublished
Cited by77 cases

This text of 57 P. 585 (City of Los Angeles v. Pomeroy) 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. Pomeroy, 57 P. 585, 124 Cal. 597, 1899 Cal. LEXIS 1041 (Cal. 1899).

Opinions

BEATTY, C. J.

This is a proceeding to condemn “all the estate, right, title, and interest” of the defendants in and to a tract of land embracing about three hundred and fifteen acres, for the purpose of enabling the plaintiff—a municipal corporation—to construct and maintain thereon the “headworks” of its projected system for supplying water to its inhabitants for private and municipal purposes." The defendants, appealing from a decree of condemnation and from an order overruling their motion for a new trial, not only allege numerous errors in the rulings of the superior court, but challenge the correctness of its findings of fact in many important particulars. With respect to these disputed facts it will be necessary to state the various contentions of the parties in discussing the particular legal questions to which they give rise, and, passing them over for the present, we,will, in this connection, only attempt to set forth the more general aspect of the case, as to which there is no substantial disagreement.

The city of Los Angeles, at the date of the commencement of this action, June 8, 1893, contained a population of about seventy thousand souls and covered an area of about twenty thousand acres. At the date of the trial, in March, 1896, the population was upward of seventy-five thousand, having increased to that number from less than twelve thousand in 1880. This rapid growth of the city promises to continue, and the only source of water supply for its inhabitants and for municipal purposes is the Los Angeles river, which flows through the city from north to south. The principal source of the river above the city [605]*605is the San Fernando valley. This valley, embracing a watershed of from four hundred and fifty to four hundred and ninety square miles, is almost completely inclosed by considerable ranges of mountains, rising in places to an elevation of over six thousand feet. The most important of these ranges is the San Fernando, which bounds the interior valley on the north. On the south and west it is bounded by the Cahuenga range, which at its northwestern extremity unites with the San Fernando. On the east the Verdugo hills are connected with the San Fernando range on the north, and, extending toward the south, leave a comparatively narrow outlet to the valley between their southern extremity and the eastern prolongation of the Cahuenga range. Through this outlet at the southeastern corner of the interior basin the Los Angeles river issues, flowing in an eastern direction parallel and close to the northern base of the Cahuenga range, until, having passed that obstruction, it turns to the south and flows through the city to the Pacific ocean. The interior of the San Fernando valley is a plain composed of detritus washed from the mountain sides, and having a moderate slope from the San Fernando range on the north toward the Cahuenga range in the south, and from the west toward the east. This portion of the valley—that is to say, the portion composed of material not in place, detritus washed from the mountain side—which, for convenience, may be called the valley proper, extends about twenty-four miles from east to west, and is about twelve miles wide at its widest part, embracing an area of about one hundred and eighty square miles. Its material is composed of bowlders, gravel, sand, and occasional masses of clay. The rainfall within the watershed of the valley is variable. When it is abundant, and the loose, porous material composing the valley proper is thoroughly saturated, the streams issuing from the rocky canyons of the mountains flow over the surface to the outlet of the valley and pass off as flood waters down the channel of the Los Angeles river. But this surface flow does not continue for any great length of time, and, under ordinary conditions, the mountain streams sink in the sand within a short distance of the mouths of the canyons, and no water appears upon the surface until it shows itself again in the Los Angeles river, where it takes its rise a short distance [606]*606north of the Cahnenga range on the southern side of the valley proper.

The land which the city seeks to condemn lies at the base of the Cahuenga range, in the narrow outlet of the valley. It is almost two miles in length from east to west, and averages a quarter of a mile in width. At its eastern end it is about a mile west of the point where the Verdugo hills make their closest approach to the Cahuenga range—the width of the valley proper at this point being about two miles. Where the land lies the width is from two and a half to three miles. The surface of the river where it flows out of the land in question at its eastern end has an elevation above the sea level of about four hundred and sixty feet, and is two hundred feet higher than the main portion of the city of Los Angeles. In ordinary seasons, after the flood waters have run off and the river has assumed its normal condition, the water rises to the surface at some distance west of the land sought to be condemned, and increases rapidly in volume as it flows toward the east. There is considerable difference between the estimates of different witnesses, but it may be said i-n general terms in this connection, where strict accuracy is not important, that the surface flow of the river, where it enters the tract in question, is about twelve hundred inches, miners7 measure, and that its volume is about doubled by the accessions it receives in passing through the tract. These accessions are of the character that would naturally be expected from the topography of the valley and the nature of the soil under and adjacent to the surface stream. The whole country on either side of the stream is found to be completely saturated with water—the plane of saturation near the open channel being slightly higher than the surface of the river, and gradually rising in proportion to the distance from the stream. From the sides and bottom of the visible stream the water percolates, or trickles, or gushes, according to the nature of the soil, whether fine and comparatively compact, or coarse and gravelly and more loose and porous.

The plan of the city for utilizing the land which it seeks to .condemn is to drive a tunnel through it from east to west, a few feet below the bed of the river, and to extend filtration galleries. north and south from the tunnel in such number and at [607]*607such places as may he iound best adapted to securing an ample supply of water. The plan also embraces a submerged dam and collecting chambers or reservoirs, but the main feature is the tunnel with its lateral galleries, from which0the water, draining and filtering out of the saturated soil, is to be delivered to the main supply pipe of the city, and thence to its dis-^ tributing system.

The principal points of controversy between the parties are: 1. As to the existence of a well-defined subterranean stream by which the waters, or a large portion of the waters, resulting from the rainfall within the watershed of the San Fernando valley, are carried off through the pass between the Cahuenga range and the Verdugo hills; and 2. As to the rights of the city of Los Angeles, as successor to the Mexican pueblo, in the waters of the Los Angeles river.

The claim of the plaintiff is, that the city has certain extensive rights in the stream over and above those of ordinary riparian owners, and that the stream itself consists not only of the visible surface flow of the river, but of the large subterranean flow slowly passing through the bowlders, gravel, and sand under and adjacent to the river.

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Bluebook (online)
57 P. 585, 124 Cal. 597, 1899 Cal. LEXIS 1041, Counsel Stack Legal Research, https://law.counselstack.com/opinion/city-of-los-angeles-v-pomeroy-cal-1899.