Duffy v. York Haven Water & Power Co.

81 A. 908, 233 Pa. 107, 1911 Pa. LEXIS 473
Supreme Court of Pennsylvania·Decided July 6, 1911·No. Appeal, No. 8·Published·Cited by 25 cases

Opinion

Opinion by

Mr. Justice Mestrezat,

The plaintiffs are the owners of an island in the Susquehanna river, known as “Three Mile Island” or “Duffy’s Island,” which is about 1,800 feet wide at its greatest width and about three miles in length. It is in Dauphin county, and its upper point is about two miles south of Middletown and its lowest point is about the beginning of the Conewago .falls. The line between Dauphin county and York county at this place is at low water mark on the western side of the river. At Middle-town the river bends sharply and flows thence almost due south to the falls. Between Middletown and the falls there are several islands, the largest of which is Duffy’s island. Shelly’s island lies to the west of Duffy’s island. At the head of Duffy’s island the current divides, part flowing straight between Duffy’s island and Shelly’s island, part flowing west of Shelly’s island and between it and the York county shore, and part flowing in a narrower and shallower channel, with two. curves, east of Duffy’s island and between it and the Dauphin county shore. The eastern channel varies in width from 700 to 1,000 feet. Duffy’s island is separated from the York county shore by a channel about 2,000 feet wide. The river narrows very much at the southern end of Duffy’s [109] island, and passes over Conewago falls at a descent of more than twenty feet in a mile.

At York Haven, just below the falls and about a mile below the foot of the island, the defendant erected, in 1902 and 1903, a power house and a dam. The dam in 1904 consisted of a wall about 300 feet long at right angles to the shore at York Haven, a similar, wall some 3,100 feet long, extending eastwardly and diagonally across the river at the falls, with its northern end about 500 feet from the west shore, and crib work of logs and stones extending beyond the end of the wall to a point about 1,000 feet west of Duffy’s island. The wall was of solid masonry, about twenty-five feet high, about six feet wide at the top, and about sixteen or eighteen feet wide at the bottom.

The winter of 1903-1904 was very severe in that vicinity, and the ice in the river was very heavy. It formed, broke and went out several times, but the river was never entirely clear at any one time. In March, 1904, the island was flooded with ice and water, destroying the plaintiffs’ buildings, farming implements, fences and other personal property, damaging the crops in the ground and removing the surface soil from the island. This action was brought to recover damages for the injuries thus resulting to the plaintiffs’ premises. The plaintiffs claim that the construction of the dam materially diverted the currents of the river and the ice and debris carried by these currents, and modified the quantity and character of the water surrounding the plaintiffs’ island, so that when the ice which formed in the river in 1904 broke, instead of moving off as it ordinarily had done through the unobstructed bed of the river, it was diverted and gorged to such an extent as to cause a rapid rise in the water, completely flooding the plaintiffs’ premises with water and large quantities of ice, and that when the gorge finally broke about March 8, 1904, the accumulated water and ice swept over the plaintiffs’ island and did the injury above stated. The defendant contends that the whole [110] river was gorged with ice, from a point four or five miles below the Conewago falls up to and including the falls; that there was no gorge at the dam; that when the breakup came the ice in the western channel gave way first; and that the injury to the island was due to the fact that the falls themselves and the eastern channel were gorged. The learned court submitted the case to the jury, and they returned a verdict for the plaintiffs. The defendant moved the court for judgment non obstante veredicto, under the Act of April 22, 1905, P. L. 286. The motion was granted, and judgment was entered for the defendant. The plaintiffs have taken this appeal. The single question is whether there was sufficient evidence to warrant the court in submitting the case to the jury.

The act of 1905 authorizes the court to enter judgment non obstante veredicto where a request for binding instruction has been declined on the trial. As we have time and again said, this act makes no radical change in the law or the relative functions of the court and jury, but broadens the power of the court and authorizes it, where binding instructions have been declined at the trial, to enter such judgment as should have been entered upon the evidence. If it appear that there is a conflict of evidence on a material fact, or any reason why there cannot be a binding direction, then there can be no judgment entered against the verdict: Dalmas v. Kemble, 215 Pa. 410. However indisputable may be the proof, when it depends upon oral .testimony it is nevertheless the province of the jury to decide : Reel v. Elder, 62 Pa. 308.

We think the learned court erred in entering judgment for the defendant. As said in the charge, the question for determination by the court and the jury was whether or not the acts done by the defendant in the construction of its wing dam and the crib wall extending therefrom resulted in or contributed to the injury to the plaintiffs’ property. The issue was a very narrow one. The plaintiffs contend that the dam obstructed the natural currents of the river and that the ice accumulated until it [111] extended up the river beyond the head of Duffy’s island, and when the thaw came and the ice broke it was thrown into the eastern channel and by reason of the size and character of that channel it was diverted westwardly across the plaintiffs’ premises. The defendant, on the other hand, contends that the river was filled with ice from shore to shore from a point below the falls up beyond the island, and that the dam was not the cause of the ice being diverted from the main channel into the eastern channel. It is further claimed that the Conewago falls and the eastern channel were, like the other parts of the river, entirely filled with ice.

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Duffy v. York Haven Water & Power Co., 81 A. 908, 233 Pa. 107, 1911 Pa. LEXIS 473 (Pa. 1911).

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