Montecito Valley Water Co. v. City of Santa Barbara

77 P. 1113, 144 Cal. 578, 1904 Cal. LEXIS 734
CourtCalifornia Supreme Court
DecidedSeptember 2, 1904
DocketL.A. No. 1123.
StatusPublished
Cited by54 cases

This text of 77 P. 1113 (Montecito Valley Water Co. v. City of Santa Barbara) 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
Montecito Valley Water Co. v. City of Santa Barbara, 77 P. 1113, 144 Cal. 578, 1904 Cal. LEXIS 734 (Cal. 1904).

Opinion

HENSHAW, J.

Plaintiff claims, and the court found it to be the owner of fifteen miner’s inches of the natural flow of the Cold Springs Branch of Montecito Creek, which waters it carried away to non-riparian lands and sold for beneficial purposes to the inhabitants of Montecito. At different times three separate and independent tunnels were driven by the defendants upon lands owned by them and contiguous to the creek. The portals of these tunnels were above the bed of the creek. They were driven through the native rock, in a northerly direction, following generally the line of the creek and the main branch thereof. While starting above the level of the creek, as the tunnels were driven with slighter incline than that of the natural flow of the creek, they soon were developed, and continued to be developed below the line of the creek-bed. The distances of the tunnels from the creek-bed varied with the sinuosities of the stream from a few hundred to a thousand or more feet. In brief, therefore, and with substantial accuracy, it may be said that the tunnels were driven to one side of the creek, parallel with it, and below its level.

The country through which the creek flows is rocky and mountainous. The mountains are composed chiefly of parallel strata of porous sandstone, some of which strata are fractured and fissured, permitting the ready seepage or percolation of water. These strata extend across the canon and across the line of the creek, which cuts them at a right angle. They are separated from each other by parallel seams of clay practically impervious to water, which serve to retain the waters which each stratum of sandstone has gathered. The stream is formed by meteoric waters falling upon its watershed of some three and a half square miles. Some of these waters flow from the surface into the stream; others reach it by percolation through the sandstone stratifications.

Plaintiff, contending that the direct effect of these tunnels was to lower the plane of saturation, and to withdraw into the tunnels water theretofore naturally flowing in the creek, thus permanently impairing and reducing the supply to which it was of right entitled, brought this action against the owners of these tunnels for injunction and for monetary compensa *584 tion for the value of the water of which it had already been deprived. The court made its findings and gave its judgment, from which cross-appeals are taken by all of the parties. We will first consider the cross-appeals of the plaintiff and of the defendant the city of Santa Barbara, since the determination of the principal questions presented upon these appeals will dispose generally of the main contentions of all the parties, and leave for further consideration only those peculiar to the case of each separate litigant.

First, it should be noted as applicable to all of these appeals that this case is radically different from that of Katz v. Walkinshaw, 141 Cal. 116. 1 Here no question arises as to the use or the right to use, or the apportionment of seepage or percolating waters by and between the owners of the overlying lands. Here the waters flow or are developed in a barren and mountainous country, are of no use upon the lands within the watershed where they are found, but are of great value to the neighboring towns, cities, and fertile valleys. Bach one of the parties to this action is carrying the water to alien soil, and no claimants—not even those who are riparian proprietors—pretend to use the water upon the lands from which it is obtained. In Katz v. Wallcinshaw the condition presented was that of a well-defined underground catchment basin, a subterranean lake, so to speak, loosely filled with gravels. The lands above this subterranean basin were valuable because of the waters beneath, and such of the water as was taken from this basin and used upon its superior lands found its way back to the source of supply as surely as does such water when used by a riparian proprietor of a flowing stream within its watershed. In Katz v. Walkinshaw the controversy arose between the owners of such superior lands upon the one hand and a defendant water company -upon the other, which, tapping the subterranean basin, was draining its waters for use upon lands without the limits of the basin, which use, if continued, threatened the impairment and destruction of all the overlying lands. The main question which this court was called upon to consider, and did consider and decide, was whether the common-law doctrine of absolute ownership in percolating water, the cujus solum doctrine, was or was not, under the peculiar conditions exist *585 ing in this state, subject to just limitation under the doctrine of sic utere two, and this court, recognizing the inevitable injury that must be worked to private interests whichever rule should be held to apply, after much deliberation decided that however differently the rule might be declared in states and countries well and regularly supplied by rainfalls, in this state, with its great arid stretches, its seasons of drought, and its irregular meteoric water supply, percolating waters, when circumstances of hardship or injury should be presented in some particular ease, must be held under the rule and doctrine of sic utere.

One more general observation pertinent to the whole case-should be made. The right is unquestioned, and plaintiff itself nowhere disputes the right, of these defendants to drive their tunnels, to develop, take, and use any and all new waters which they may thus find. Plaintiff’s contention, however, is, that the effect of these tunnels below the line of the surface of the flowing stream is iLst to draw into the tunnels the waters of the saturated sandstone strata above (which saturated strata under normal conditions form a support to the flowing waters of the stream), and thus create a direct draft upon the flow of the stream itself, so that it no longer follows its natural course and bed, but sinks into the lower tunnels, which themselves practically, efficiently, and absolutely form new channels in place of the original surface stream. This effect of the tunnels is denied by the defendants, and this issue and the court’s finding upon it present the principal question in the case.

CROSS-APPEALS OF PLAINTIFF AND CITY OF SANTA BARBARA.

The court, after finding that the plaintiff was entitled of first right to the natural flow of the creek to the extent of fifteen miner’s inches, and that it was devoting this water to a public use, declared (finding No. 9): “That the said tunnels have pierced the strata hereinbefore mentioned and have drawn off the water stored in said strata, and lowered the planes of saturation in said strata (which said planes of saturation had previously thereto supported the flow of water in said creek), and caused the voids and crevices in said strata to be in part emptied of the water contained therein, and caused the waters of said creek and said tribu *586 tary springs and ciénegas

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Bluebook (online)
77 P. 1113, 144 Cal. 578, 1904 Cal. LEXIS 734, Counsel Stack Legal Research, https://law.counselstack.com/opinion/montecito-valley-water-co-v-city-of-santa-barbara-cal-1904.