Washington County Water Co. v. Garver

46 A. 979, 91 Md. 398, 1900 Md. LEXIS 52
CourtCourt of Appeals of Maryland
DecidedJune 14, 1900
StatusPublished
Cited by6 cases

This text of 46 A. 979 (Washington County Water Co. v. Garver) is published on Counsel Stack Legal Research, covering Court of Appeals of Maryland primary law. Counsel Stack provides free access to over 12 million legal documents including statutes, case law, regulations, and constitutions.

Bluebook
Washington County Water Co. v. Garver, 46 A. 979, 91 Md. 398, 1900 Md. LEXIS 52 (Md. 1900).

Opinion

Fowler, J.,

delivered the opinion of the Court.

This is an action on the case brought by the plaintiff, Samuel B. Garver, against the Washington County Water Company to recover damages alleged to have resulted from the unlawful diversion by it of a water-course.

*405 The only question presented is as to the propriety of the rulings upon the prayers.

During the course of the trial the plaintiff offered testimony tending to prove that he was the owner of the land through which the water-course in question runs; that on said land there was erected a flouring and chopping mill, and that from time immemorial this stream of water, known as “ Raven Rock Stream,” flowed free from obstruction in a well-defined channel to and through the land of plaintiff and to his mill, except when the waters were low in the summer; that at a point not far from the bed of said stream, about a half-mile up stream from the mill, and several hundred feet from the plaintiff’s mill-dam, there is a spring known as “ Rohrer’s Spring,” from which the water also flows into said mill-dam during certain portions of the year; that there is a sink-hole in the bed of said stream about a thousand feet from the point where said stream leaves the defendant’s land; that the land between the sink-hole and the spring is limestone; that during all the time, whether there was sufficient water to carry the stream to the sink-hole or beyond it, a large amount of water goes into said sink-hole and under the surface of the ground at a point in said hole where limestone rocks project into the bed of the stream; that the defendant in 1896, near the head waters of said stream and about two miles from the lands and mill of the plaintiff, erected dams across the same for the purpose of retaining the water and distributing the same through pipes to its reservoir and from thence to Hagerstown; that at the time and immediately after the water of said stream was thus diverted by the defendant, the water in the spring sank 8 or 10 inches, and that this diversion has continued to have this effect. In order to show that the water of the stream flows to the spring through a subterranean passage, the plaintiff offered testimony tending to prove that when the water of the stream runs into the sink-hole the spring is 8 to xo inches higher than when it does not so run; that when muddy wate *406 •runs into the sink-hole the water in the spring soon thereafter becomes muddy also, and that this happens when it has not rained near the spring, but has rained near the .source of the stream ; that many years ago an experiment was made by throwing chaff into the sink-hole, and that a short time thereafter chaff appeared on the surface of the water of the spring, and was seen coming out from under the rocks where the spring emerged. It was further proved 'that by reason of the diversion of the stream and the sinking of the spring the plaintiff’s mill was deprived of sufficient water to operate it, and that prior to said diversion he had sufficient water for that purpose, except in the dry sea-son, when the water was low. There was also evidence tending to show that the loss to the plaintiff by reason of the diversion of water from the mill amounted to $100 per year, and that the loss arising from deprivation of water for his stock was from fifteen to twenty dollars per year, and that the loss he suffered from the time of taking the water -to the time of bringing this suit, was at the same rate for the respective items of loss for such proportion of the year.

The defendant offered evidence admitting the erection of the dam as alleged, but tending to prove a state of facts contradicting the case made out by the plaintiff in regard to the amount of water in the stream and its connection with •the spring through the underground passage.

There was a verdict and judgment for the plaintiff for $33-75) the Court having instructed the jury that the plaintiff could only recover for the loss which accrued between the time of diverting the water and the bringing of the suit, that is to say, between the 1st of July and 14th of November, 1896. The defendant has appealed.

As we have seen, the only exception in the record before us relates to the granting of certain -of the plaintiff’s, and the refusal to grant certain of the defendant’s prayers. The first, third and fourth prayers of the plaintiff were granted as offered, and his second as modified by the Court, and ■the first, fourth, fifth and seventh of the defendant rejected.

*407 Before proceeding to consider the action of the Court as above set forth, we will briefly state the general principles of law applicable to a case like this. However interesting it might be to examine the text-books and the decisions of other States to determine what these principles are and their limitations, we would hardly be justified in so doing when it has been so recently done in the opinion of this Court delivered by Judge Alvey in the case of Baltimore v. Warren Manufacturing Co., 59 Md. 103. While it is true that the case just cited was one in which the defendants were charged with having unlawfully polluted the stream, yet the general principles announced were-applied and are applicable as well to an unlawful diminution of quantity as to deterioration of quality. After stating that, before the time of Lord Coke, the general principles in relation to the pollution of streams had been settled in England, the learned Judge says : “ In more recent times all common law authorities agree that a riparian owner has the right to the natural stream of water flowing by or through his land, in its ordinary natural state, both as to its quantity and quality, as incident to the right to the land on or through which the water runs ; and that right continues, except so far as it may have been derogated from by user or by grant.” These general principles are not, and cannot be, controverted by the defendant in this case, but he contends that they have no application to the case at bar, first, because the evidence does not show that there was a flowing water-course which could have been diverted, and secondly, that if there was any such water-course it was in part underground and percolated, in contradistinction to flowing, in a channel to a point from whence it flowed into the plaintiff’s mill. But, whatever may bé the merits of these contentions, they both relate to questions of fact which are for the jury. The plaintiff offered evidence to show that the diverted stream flowed through his land and supplied his mill all the time except for a short period in summer, when the waters are low. Among the definitions of a water-course is the following by *408 Judge B-igelow in the case of Luther v. Winnisimmet Co. 9 Cush. 174, which Prof. Washburn characterizes as most accurate and compendious. “ A stream of water usually flowing in a definite channel, having a bed, sides or banks, and usually discharging itself into some other stream or body of water. To constitute a water-course, the size of the stream is not important; it might be very small and the flow of water need not be constant.

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Cite This Page — Counsel Stack

Bluebook (online)
46 A. 979, 91 Md. 398, 1900 Md. LEXIS 52, Counsel Stack Legal Research, https://law.counselstack.com/opinion/washington-county-water-co-v-garver-md-1900.