Burr v. MacLay Rancho Water Co.

116 P. 715, 160 Cal. 268, 1911 Cal. LEXIS 511
CourtCalifornia Supreme Court
DecidedJune 22, 1911
DocketL.A. No. 2284.
StatusPublished
Cited by25 cases

This text of 116 P. 715 (Burr v. MacLay Rancho Water Co.) 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
Burr v. MacLay Rancho Water Co., 116 P. 715, 160 Cal. 268, 1911 Cal. LEXIS 511 (Cal. 1911).

Opinion

THE COURT.

From the judgment in this action the plaintiff appealed on the judgment-roll alone and his appeal resulted in á modification of the judgment of the court below by this court. The report of the case is to be found in 154 Cal. 428, [98 Pac. 260].

The appeal now before us is that of the defendant and the interveners from the judgment and is presented on the judgment-roll, together with a bill of exceptions. The nature of the case and many of the facts appear in the opinion filed in the matter of the plaintiff’s appeal and we shall not, therefore, undertake to make a new statement of the same matters.

The appellants make the point that the court erred in overruling the demurrer to the complaint. The facts stated make out a case under the theory that the plaintiff and the defendant were the owners of land overlying a subterranean supply of percolating waters and that the doctrine of Katz v. Walkinshaw, 141 Cal. 116, [99 Am. St. Rep. 35, 64 L. R. A. 236, 70 Pac. 663, 74 Pac. 766], applies. They are not substantially different from those appearing in the complaint in the Katz case which was there held to state a case for unlawful interference with a supply of percolating waters common to both parties. There is an allegation that water-bearing strata extending, under the lands of plaintiff and defendant, “are in streams, or subterranean bodies or chambers, and are in a state of continuity from their sources to the said dike.” This, it is urged, makes it uncertain whether plaintiff is claiming as an owner of land overlying a common supply of percolating water, or as riparian owner of land upon an underground stream or lake. There is nothing in the complaint to indicate that the plaintiff was claiming as a riparian owner upon a lake or stream. A reading of the whole complaint shows plainly enough that the pleader, notwithstanding his somewhat vague use of the word “stream,” was not undertaking to set" forth the existence of a defined watercourse, but to allege that a body of percolating water was underlying the lands of the *271 plaintiff and a part of the land of defendant. Beyond all this, there can be no question but that the defendant was not misled by any uncertainty in this respect, since the record shows conclusively that the plaintiff did not claim that any underground stream could be shown to exist, and that the parties, throughout, were dealing with the case as one involving relative rights to percolating waters. Even though the demurrer might have been sustained on this ground, its overruling furnishes no ground for reversal. (Alexander v. Central etc. Co., 104 Cal. 532, [38 Pac. 410]; Jager v. Cal. Bridge Co., 104 Cal. 542, [38 Pac. 413]; Rooney v. Gray Bros., 145 Cal. 753, 79 Pac. 523].)

It is strongly urged by the appellants that the findings fail to show that the whole of plaintiff’s lot 191, or any part of lots 153 and 190, overlie the underground basin or water-bearing strata from which the defendant pumps water and that if such findings are to be construed as showing that the supply of water claimed by plaintiff as extending under said lots is the same as that from which the defendant is pumping, they are without support in the evidence.

The findings state that, underlying the entire tract of twenty thousand acres conveyed by Maclay to Widney and others as trustees in 1885, which includes all the lands in controversy, “including the lands of plaintiff and extending to the foot of the mountains on the north, about three or four miles northerly from the lands of the plaintiff, ... are water-bearing strata of varying depths of sand, boulders, and coarse material, and lying over each of these strata are impervious strata of clay or cement extending towards, but not entirely to, the said mountains. That at a distance of about-miles in a southerly direction from plaintiff’s lands, there extends across the said valley and across said 20,000 acre tract, a dike which is almost or entirely impervious to water.” Another finding states that the dike crosses the valley and passes through defendant’s lot 192 and that it “arrests the progress of the water underlying plaintiff’s land and the water underlying the northern part of lot 192.” Another states that the subterranean waters extending through said water-bearing strata are supplied by the rains which fall upon the mountains to the north and east of said valley and “find their way into said water-bearing strata and permeate the said strata” and *272 percolate through the same underneath the “overlying stratum of clay or cement down to the said dike, by means of which the movement of said water is arrested, and the waters impounded, forming a subterranean basin wherein the said subterranean waters are retained.” Also: “The waters in said water-bearing strata underlying the lands of plaintiff and other lands in the vicinity, including the lands in which defendant’s pump is situated, are, in their natural state, under pressure from the head of the waters near said mountains, and are by nature restrained and retained in said strata by the said dike and the overlying strata.” Findings are to be construed so as to support the judgment, rather than so as to overthrow it. It would require a very narrow and forced construction of these findings to hold that they do not show a common supply of percolating water, lying in continuous strata saturated with water and extending under the three lots of plaintiff and into and under the part of the defendant’s lot 192 in which the defendant’s wells and pumps are situated. We hold that they support the judgment in this particular.

With respect to the sufficiency of the evidence, we think that, when taken in connection with the admissions made by the pleadings, the evidence is sufficient. There is, it is true, but little evidence that the water-bearing strata supplying defendant’s pumps extends under lots 190 and 153, and that evidence is altogether circumstantial. But that exact point is covered by the admissions of the pleadings. Lot 190 adjoins lot 191 on its northwesterly side. Lot 153 corners with lot 190, lying almost due north of it. The slope of the land is from the north towards lot 192 through the three lots of plaintiff. The complaint avers that underlying the lands of the plaintiff and extending to the foot of the mountains on the north are water-bearing strata, that the waters therein are in streams or subterranean bodies or chambers and are in a state of continuity from their sources to and under lot 192, that the waters are supplied by winter rains falling upon the mountains, which waters find their way into said water-bearing strata, that under the plaintiff’s lands and defendant’s lot 192, where its pumps are located, said waters are, in their natural state, under pressure and are restrained and retained in said strata by said dike, and that the water pumped by defendant is taken from said water-bearing strata underlying said lands of plain *273 tiff and defendant.

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Bluebook (online)
116 P. 715, 160 Cal. 268, 1911 Cal. LEXIS 511, Counsel Stack Legal Research, https://law.counselstack.com/opinion/burr-v-maclay-rancho-water-co-cal-1911.