291 P. 825 | Cal. | 1930
[EDITORS' NOTE: THIS PAGE CONTAINS HEADNOTES. HEADNOTES ARE NOT AN OFFICIAL PRODUCT OF THE COURT, THEREFORE THEY ARE NOT DISPLAYED.] *310 THE COURT.
This court granted a hearing herein after the decision of the District Court of Appeal in and for the Second Appellate District, Division Two, Burnell, Justice pro tem., writing the opinion, affirming the judgment of the trial court, in order to permit a careful re-examination of the record herein. Upon such examination we are satisfied that said decision is correct as to the law and facts set forth therein, and we therefore hereby adopt the same as the decision of this court, reading as follows:
"There is no dispute as to the facts of this case, which may be summarized as follows:
"The plaintiffs, respondents here, are the owners of a parcel of land located at the south end of Vancouver avenue, on the westerly side of the street. Vancouver avenue extends in a southerly direction from Whittier boulevard, the latter running easterly and westerly. Both streets and all of the territory referred to in the evidence and findings are in Los Angeles county, outside of the boundaries of any incorporated city. Defendant-appellant owns a tract of land east of Vancouver avenue and south of the termination of that street, his property abutting that of the plaintiffs to the east and south and lying at a lower level. The general slope of the land south of Whittier boulevard, and also to the north of that thoroughfare, is from north to south. Prior to the making of certain improvements presently to be described the storm and surface waters falling upon the lands north of Whittier boulevard, to quote the language of the court's findings, `flowed in two natural and well defined channels, which channels were of the character of depressions or swales and diverged from a common point several thousand feet northerly of Whittier boulevard, and ran, one in a southeasterly, and one in a southwesterly direction, and entered Whittier boulevard at a point several thousand feet easterly and at a point several hundred feet westerly of plaintiffs' property and drained in a southerly direction therefrom without flowing over or upon the property of the plaintiffs or of the defendant.' In May, 1922, prior to the laying out of Vancouver avenue, and also prior to the improvements referred to, the defendant constructed an irrigating ditch with each embankment and a wire fence along the northerly side of his land and within a *312 few feet of the south line of the plaintiffs' property. In 1924 the county of Los Angeles graded and paved Whittier boulevard, and since this improvement its elevation at a point about fifteen hundred feet westerly of Vancouver avenue is approximately one and one-fourth feet higher than at Vancouver avenue, while its elevation at a point about eighteen hundred feet easterly of Vancouver avenue is over a foot higher than at Vancouver avenue. The lowest point, however, on Whittier boulevard between these points is at Victoria, formerly known as Clela avenue, the street immediately west of Vancouver, and like the latter, running south a short distance from Whittier. At about the same time that Whittier boulevard was being improved a large area of land lying north of it and extending for several thousand feet both easterly and westerly of Vancouver avenue, and which had in former years been used for grazing and later on for agricultural purposes, was subdivided and platted and a large number of streets laid out thereon and graded and paved, the northerly ends of the north and south running streets being over thirty feet higher than the elevation of Whittier boulevard at its several points of intersection with the southerly termini of said streets. The court found `that the grading and paving of said streets north of Whittier boulevard, resulted in the filling up and closing of said natural drainage channels north of Whittier boulevard and the storm and surface waters which formerly flowed across Whittier boulevard easterly of plaintiffs' property were diverted into Whittier boulevard at a point several hundred feet westerly of its natural channel and water that formerly crossed Whittier boulevard westerly of plaintiffs' property was diverted into Whittier boulevard at a point several hundred feet easterly of its natural channel and to a point several hundred feet easterly from where it usually flowed and crossed Whittier boulevard; that due to the graded and paved condition of said last mentioned streets, the natural flow of storm and surface water falling on those lands and the lands northerly thereof has been greatly accelerated with the result that during the rainy seasons of the year storm and surface waters flow in a southerly direction over and along said last mentioned streets to Whittier boulevard.' The result of the change in the grade of Whittier boulevard, together with the improvement *313 of that thoroughfare and of the land north of it as above described has been to cause this accelerated flow of storm and surface water thus brought onto Whittier boulevard to escape therefrom at the low points and thus to flow down Vancouver and Victoria avenues, to some extent onto the land of plaintiffs, and if not diverted, across the land of the defendant.
"It is apparent from the evidence (nor is there any contention to the contrary) that the construction of the ditch, embankment and fence by the defendant did not in any way detrimental to the plaintiffs affect the flow of the surface or storm waters under the conditions which obtained at the time of their construction or until the completion of the various improvements above referred to. But in 1925, and after conditions had been changed as described in the portion of the findings from which we have quoted, there was a heavy fall of rain and the water which poured into Whittier boulevard flowed south therefrom in Vancouver avenue `just like a river' as one witness expressed it. Defendant's ditch was utterly inadequate to the task of carrying off this torrent of water and his embankment and fence presented an obstacle to its further southerly progress and caused it to back up and to overflow plaintiffs' property, thereby causing considerable damage thereto. There was a recurrence of these conditions in 1926.
"The appellant denies liability for the damage caused to respondents' property and seeks a reversal of the judgment upon the theory that as a matter of law he was not required to receive surface waters in greater quantities or in a different manner than would occur under conditions such as existed prior to the improvements referred to and the consequent interference with the flow of such waters and the diversion and concentration thereof onto his property. Stated in different words, his contention is that he had a right to protect his property from the onslaught of waters which, under natural conditions, would not have been precipitated thereon.
[1] "It is thoroughly settled in California that the owner of the upper or dominant estate has a legal and natural easement or servitude in the lower or servient estate to discharge all surface waters naturally falling or accumulating on his land, upon or over the land of the servient *314
owner in the manner in which they would naturally flow from a higher to a lower level and that the owner of the lower estate is answerable in damages for any injury which may be caused to the upper estate by reason of obstructions which he has placed in the way of such natural flow, thus causing it to back up or remain on the land of the upper proprietor (Jaxon v. Clapp,
"In view of the different rules applicable in the respective cases of flood and surface waters it is important that the nature of the waters involved in the present case be ascertained. [3] Flood waters are those which escape from a stream or other body of water and overflow the adjacent territory (McDaniel v.Cummings, supra; Gray v. Reclamation Dist., supra; Horton v.Goodenough, supra). [4] Surface waters are those which are produced by rainfall, melting snow, or spring and which in the case of the two first-mentioned sources are precipitated, and in the case of the last-mentioned source, rise upon the land. (See cases cited supra.) Such waters are not divested of their character as surface waters by reason of their flowing from the land on which they first make their appearance onto lower land in obedience to the law of gravity. It is waters of this character that the lower or servient estate is bound to receive from the upper or dominant estate and the flow of which he may not obstruct to the detriment of the upper proprietor provided their flow is a natural one. [5] The upper proprietor may not divert by artificial means *316 the surface waters upon his own lands to the lands of the lower proprietor nor may he accelerate by means of ditches or increase the drainage of his own land to the injury of the lower owner. His right `is limited to the disposition of the water through the chosen channels of nature.' (Board of Trustees v. Rodley,supra.)
[6] "Tested by these definitions it is evident that the water which came into Vancouver avenue from Whittier boulevard and hence onto the land of the plaintiffs and the escape of which over the lands of defendant was prevented by the obstructions maintained by him was surface water, caused by the rainfall on the land north of Whittier boulevard.
"It is significant that all of the decisions which state and apply the rule as to the duty of the lower proprietor to receive the surface waters flowing from the land of the upper proprietor relates to the natural flow thereof. Thus Heier v. Krull,supra, states the rule as follows: `Every landowner . . . has a lawful right to complain of others who, by interfering withnatural conditions, caused such surface water to be discharged in greater quantity or in a different manner upon his land than would occur under natural conditions,' while in Jaxon v.Clapp, supra, it is enunciated: `The general rule is that where two adjacent parcels of land belong to different owners, one being lower than the other, and the surface water from the higher tract has been accustomed by a natural flow to pass over the lower tract, the owner of the higher land has an easement by virtue of which storm waters from such land may be permitted to flow on the lower tract, which latter is charged with a corresponding servitude,' and in Sanguinnetti v. Pock, supra,
the court said: `It is settled law in this state that plaintiff as the owner of the upper land has an easement over the lower adjacent land of defendant to discharge surface water as it isaccustomed naturally to flow, and defendant had no right to intercept such natural flow to plaintiff's injury.' (Italics ours.) See, also, Board of Trustees v. Rodley, supra, andRudel v. Los Angeles County,
"Appellant's second point is that the judgment in the sum of one thousand dollars which was awarded plaintiffs in the court below `is excessive, and contrary to the evidence and not supported by admissible testimony.' [10] As to the amount of damages suffered by the plaintiffs the case was apparently tried by both parties upon the theory that the proper measure of damages was the cost of repair, whereas the correct rule is that the measure of damages for injuries to real property is the difference, if any, in its market value before and immediately after the injury (Perkins v. Blaugh,
The judgment is affirmed.