Harper, Hollingsworth & Darby Co. v. Mountain Water Co.

56 A. 297, 65 N.J. Eq. 479, 20 Dickinson 479, 1903 N.J. Ch. LEXIS 13
CourtNew Jersey Court of Chancery
DecidedNovember 27, 1903
StatusPublished
Cited by3 cases

This text of 56 A. 297 (Harper, Hollingsworth & Darby Co. v. Mountain Water Co.) is published on Counsel Stack Legal Research, covering New Jersey Court of Chancery primary law. Counsel Stack provides free access to over 12 million legal documents including statutes, case law, regulations, and constitutions.

Bluebook
Harper, Hollingsworth & Darby Co. v. Mountain Water Co., 56 A. 297, 65 N.J. Eq. 479, 20 Dickinson 479, 1903 N.J. Ch. LEXIS 13 (N.J. Ct. App. 1903).

Opinion

Embry, V. C.

Complainant’s bill is for an injunction to restrain defendants’ interference with its rights in the waters of a stream or natural water-course byr the diversion or abstraction of the waters of the stream and of the springs and rivulets which in part supply it. These rights and the defendants’ interference with them have, as complainant claims, been already established by a suit at law, brought by its predecessors in title, against two of the defendants, under whom the third defendant claims by title or right acquired after the suit at law. In its general aspect, therefore, the bill is filed in aid of a legal right, claimed to be sufficiently established, and to restrain by injunction the continued interference with the rights. Defendants deny any interference with complainant’s rights, set up alterations in the operation of their works since the judgment at law and dispute the conclusiveness of that judgment on the question of interference. The substantial facts relating to the water rights claimed, the alleged interference with them and the issues in the suit at law are as follows: Complainant is the owner of a mill-property to which is attached or appurtenant a right to a supply of water from a stream called Green brook, flowing through a valley, sometimes called the .Eeltville vallejq lying west of Summit, between the First and Second mountains. Complainant’s mill is not located on the stream, but water is supplied to it by means of a raceway, beginning at a dam in the brook called the Upper Feltville dam, and running about twenty-four hundred feet to the mill. Complainant’s right, or that of its grantors, to the water of the stream for use at its mill by means of this raceway was established by the suit at law referred to and has not been contested in this suit. About a- mile and a half above the dam the defendants have constructed a water plant which is now used to supply the city of Summit with water. The water supplied is derived altogether by pumping from wells [481]*481which have been-slink in the neighborhood of the stream, and in the suit at law it was claimed by plaintiffs, as it is now claimed here by complainant, that by the operation óf their pumping-plant the defendants abstracted the water from the stream and from the rivulets and springs which supplied it, thus reducing the flow of water in the stream to 'which complainant’s mill was entitled. As the defence in this 'suit is, based mainly on the contention that the verdict and judgment, which were obtained in the suit at law, are not conclusive in this suitj because 'of the alterations or changes in the operation of their plant since the verdict, it is necessary to make a statement in some detail of the location and character of the different parts of the plant in connection with the stream and its operation at the time of the trial at law as well as at the present time. The works of the water company consist of an artesian well, two open wells, called the upper and lower well, and an infiltration gallery, from which water is supplied to the upper well. About twenty feet from the upper well the pumping plant is located, and from this pumping plant pipes, fifteen to eighteen inches in diameter, connect with three shafts, sometimes called wells in the evidence, located at the two ends and the centre of the infiltration gallery. The upper and lower well are connected by a pipe about sixteen hundred feet long, and at the time of the trial at law water was supplied from the lower to the upper well, a syphon being constructed in the pipe, as the wells were at different levels. The lower well is farther down the stream than any of the other structures and is about a mile and a quarter above the dam, measuring along the bed of the stream. It is thirty feet in diameter, about twenty-five feet deep, and is located about fifty feet south of the stream, whose general direction is from northeast to southwest, through the centre of the valley. On the north side of the stream, about sixteen hundred feet above tbe lower well and about three hundred and fifty feet from the stream,'the upper open well is located. This is thirty feet in diameter and thirty feet deep. Between the upper well and the bed of the stream the infiltration gallery, about five hundred feet long, is constructed of pipes from fifteen to eighteen inches in diameter, laid with open joints to admit passage of the water [482]*482into it, and laid about twenty feet below the surface of the ground. Three shafts, one from each end and one at the centre, run from the surface of the ground to the gallery. This infiltration gallery runs in tire same general direction as the banks of the. stream, but, as it is laid on an angle and not straight, the end shafts are about two hundred feet and the centre shaft about three hundred feet from the north bank of the 'stream. The upper well is located nearly opposite the centre of the infiltration gallery and about twenty feet from it. The north end of the infiltration gallery is the portion of the plant which is located furthest up the stream. The upper and lower wells are open at the bottom but constructed with, cement walls .which are intended to be water tight. The artesian well- sunk near the upper well is a- water-tight tubing, extending two hundred feet down into the rock, and its operation is not claimed to affect the water-supply of the stream. The entire works are constructed near the head of the Eeltville valley and the sources of Green brook and the ponds, rivulets and springs about the works are thus described or located in the evidence. About two hundred yards up the stream, above the pumping well, there is a pond, called the Erog pond, one of the sources of the stream, into the upper end of which a small rivulet, apparently the source of the stream, flows, and at the lower end of which is an outlet into the stream. The first supply below the Frog pond is a rivulet or stream, running into Green brook from the south and called the Faitoute spring run, which takes its rise from a. spring on the rise of ground toward the south; another run or rivulet, about three hundred and fifty feet further south, also runs in upon the same side. These runs are opposite the infiltration gallery. The next stream is one south of the pumping-station and about three hundred yards further down the brook, but running into it from the north and from what is called the Ballantine spring,, located about four hundred yards north of the stream. Into the Ballantine spring run, before it reaches Green brook, another small stream, originating apparently in a small pond between the Ballantine spring and the pumping-station, runs into the Ballantine spring run. The lower well is located nearly six hundred feet down the stream from the Ballantine spring run [483]*483and, as I have stated, is the structure farthest down the stream. In the suit at law it was claimed by the plaintiffs that this lower well was located over a spring known as the “Boüing Spring,” and evidence tending to prove the existence of a spring at this place at the time of the location of the well was produced by the plaintiffs and submitted to the jury. Defendants in the suit at law denied its existence at that time and produced evidence tending to prove this claim. The question of the existence of the spring was left to the jury. After judgment in the suit at law the defendants ceased pumping water from the lower well through the pipe, and the present contention of the defendants is that this change in, the operation of their plant has so materially changed the condition which existed at the time of the trial, upon which the verdict was based, that , the judgment cannot be taken as conclusive upon the question of the interference at the present time.

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Cite This Page — Counsel Stack

Bluebook (online)
56 A. 297, 65 N.J. Eq. 479, 20 Dickinson 479, 1903 N.J. Ch. LEXIS 13, Counsel Stack Legal Research, https://law.counselstack.com/opinion/harper-hollingsworth-darby-co-v-mountain-water-co-njch-1903.