Revis v. I. S. Chapman & Co.

19 P.2d 511, 130 Cal. App. 109, 1933 Cal. App. LEXIS 955
CourtCalifornia Court of Appeal
DecidedFebruary 27, 1933
DocketDocket No. 597.
StatusPublished
Cited by1 cases

This text of 19 P.2d 511 (Revis v. I. S. Chapman & Co.) is published on Counsel Stack Legal Research, covering California Court of Appeal primary law. Counsel Stack provides free access to over 12 million legal documents including statutes, case law, regulations, and constitutions.

Bluebook
Revis v. I. S. Chapman & Co., 19 P.2d 511, 130 Cal. App. 109, 1933 Cal. App. LEXIS 955 (Cal. Ct. App. 1933).

Opinion

AMES, J., pro tem.

This action was brought for the purpose of recovering damages caused by the alleged draining of plaintiff’s land by the defendant. A trial by jury was had, in which plaintiff was awarded damages in the sum of $2,500, and from the judgment entered thereon defendant prosecutes this appeal.

Since May, 1909, respondent had been the owner of approximately ten acres of land located in that portion of San Bernardino County known as the artesian belt, and which is aptly described in the opinion of the Supreme Court in the case of Katz v. Walkinshaw, 141 Cal. 116 [70 Pac. 663, 667, 74 Pac. 766, 99 Am. St. Rep. 35, 64 L. R. A. 236]. The westerly half of this land is not involved here. The easterly half is described as low, damp, swamp-land which, under normal climatic conditions, was saturated with water. The respondent testified that upon the surface of his land there was a deposit of red soil varying from eighteen inches to two feet in depth, beneath which was a stratum of peat from twelve to fourteen inches in depth, and beneath that two other strata of peat varying in depth from six to sixteen inches, between which there existed stratifications of silt and sand varying in depth from eight to twelve inches. The general slope of the land is from a northeasterly to a southwesterly direction. The water in the soil is not a part of any stream or subterranean course, but was naturally percolating through the soil. Prior to the operations of appellant, which are hereafter described, water stood freely upon the surface of the ground and within ditches constructed thereon. The presence of the deposits of peat within this soil renders crops planted therein unusually prolific.

The land south of and adjacent to the respondent’s property, consisting of about ten acres, together with about thirty acres lying east of and adjacent to respondent's property, is owned by appellant. Upon this property appellant has been engaged for several years in removing the peat deposits from its soil for the purpose of manufacturing fertilizer for commercial purposes, and which is, after its *111 manufacture, removed from the premises of appellant and used for fertilization of the soil in other communities.

Respondent testified that along the south side of his land there was a bluff or elevation from ten to twelve feet in height. In the fall of 1927 appellant removed this elevation, and along the north line of its property constructed a ditch approximately five feet in depth. This ditch throughout the transcript is referred to as ditch “A”, and throughout this opinion will be so identified. In the winter of 192-7 appellant constructed a ditch along the south line of its property, parallel to and about two hundred feet south of ditch “A”, which, in the transcript, is referred to as ditch “B”, and which will be so identified in this opinion.

In 1924 respondent owned, in addition to the land here involved, the property south of and adjacent to it, which he subsequently conveyed to his wife, and of which appellant is now the owner. He testified that the character of the soil in that parcel of land was similar to the land still owned by him and which is involved in this action. In 1924 he first farmed that portion of his property which is now owned by appellant. During that year he planted crops of melons, peanuts, popcorn and other agricultural products. The crops planted that year proved to be unprofitable, with the exception of his crop of peanuts, which, he testified, yielded profitable returns, and that the land upon which his crops were planted, together with the land now owned by him, continued to yield profitable crops until the drainage of his land was accomplished by appellant as hereinafter described.

Respondent further testified that he continued to raise profitable crops until the construction of ditch “A” and ditch “B”; that after the construction of appellant’s ditches the water which had formerly saturated the strata of peat in his lands sunk to a level of five feet below the surface of the ground, as a result of which the peat became dry and the land unproductive; that it was impossible to raise crops upon his land without artificial irrigation. An expert witness, who had been a resident of the artesian area for many years, testified that after water is withdrawn from peat it gets very hard, cracks form in it and “that it seems impossible to get it wet”. That before crops could be grown a saturation of the peat would be necessary and that *112 this could not be accomplished with surface irrigation. Respondent further testified that a portion of the surface of his land sunk by reason of the removal of water from the substrata of the soil; that an artesian well, which formerly flowed on his premises, dried up. Other evidence was introduced tending to prove that the drying of respondent’s land was due to the operations of appellant which, however, it will be unnecessary to summarize here.

Appellant, on the contrary, contends that the. drainage of respondent’s land was not due to its operations but to a series of dry years and the lowering of the water-plane in the artesian area due to heavy draughts upon the supply therein contained. The evidence in this respect is in sharp conflict and presents a question of fact for the jury, but appellant further contends that the operations conducted upon its land was a reasonable use of the land and that, conceding that such operations resulted in the drainage of respondent’s land, he has no cause of action against appellant.

. The doctrine of reasonable use was established in this state in the case of Katz v. Walkinshaw, supra, and has been cited and reaffirmed in many decisions since that time. In that case Mr. Justice Angellotti, in quoting from the case of Pixley v. Clark, 35 N. Y. 520 [91 Am. Dec. 72], says: “ ‘An owner of the soil may divert percolating water, consume or cut it off with impunity. It is the same as land, and cannot be distinguished in law from land. ’ He says this proposition must be admitted, but nevertheless a case cannot be found in this country ‘ where the right has been upheld in the owner of land to destroy a stream, a spring or a well upon his neighbor’s land, by cutting off the source of its supply, except it was done in the exercise of a legal right to improve the land, or make some use of it in connection with the enjoyment of the land itself’.”

In Hudson v. Dailey, 156 Cal. 617 [105 Pac. 748, 752], the court says, with respect to percolating waters: “The general rule, as now established by the decisions of this court, undoubtedly is that where two or more persons own different tracts of land, underlaid by porous material extending to and communicating with them all, which is.saturated with water moving with more or less freedom therein, each has a common and correlative right to the use of this Water upon *113 his land, to the full extent of his needs if the common supply is sufficient, and to the extent of a reasonable share thereof if the supply is so scant that the use by one will affect the supply of the others.”

The same principle has been reaffirmed in many decisions in this state. Among them may be cited Cohen v.

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Bluebook (online)
19 P.2d 511, 130 Cal. App. 109, 1933 Cal. App. LEXIS 955, Counsel Stack Legal Research, https://law.counselstack.com/opinion/revis-v-i-s-chapman-co-calctapp-1933.