97 N.Y.S. 425 | N.Y. App. Div. | 1906
Lead Opinion
It cannot seriously be questioned that the jury were justified by abundant evidence in finding that at the place where the plaintiff fell ■» ridges of ice from two to four inches thick had formed across the walk, not from natural causes alone, but from the freezing of water discharged upon the walk from a pipe in a supporting wall on the abutting premises, and that said ridges had negligently been allowed to remain in said condition during the winter preceding the accident; and the uncontradicted statement of the plaintiff that-she slipped on this ridge; of ice is corroborated by' the circumstance that the _ location of the ridge and the place of .the fall were coincident. But it is claimed that this 'ease is controlled by Taylor v. City of Yonkers (105 N. Y. 202) because of the circumstance that the ■ ridge had been augmented by a recent fall of snow for which the defendant was not responsible: It appears that for several days before the accident the' temperature had been below the freezing point, and we may assume that the light snow, which according to . the defendant’s, evidence had fallen the day before, when packed down by travel, augmented this ridge by some inconsiderable fraction of an inch, and it is urged that it is just as likely that the recent snowfall was the sole cause of the injury as that the ridge of • ice contributed to -caupe it. ■ In the Taylor case the plaintiff fell upon a smooth surface of ice recently formed by rain followed by sudden freezing, causing the walks throughout the city to become slippery and dangerous, and the plaintiff sought to establish-liability upon'the theory that the slope of the walk, innocent-enough in itself,, contributed with the ice to cause the injury. Judge Finch said that the ice by itself “ was a sufficient, certain and operating cause of the fall;” obviously the 'slope of the walk, for which alone the-defendant was sought to be made liable, was not,by'itself “a sufficient, certain and operating cause.” But can it be said that to affirm that the ridge of ice had anything to do with the accident in the case at bar is a “ pure guess and an absolute speculation,” as Judge Finch said of the slope of the walk in the case cited ? The. ridge of ice by itself was an adequate cause. ,The slope of ■ the
Only one other question urged by the appellant requires consideration. The defendant excepted to the charge of the court that “ the city is obliged to keep its streets in good, safe, passable condition.” As I understand the rule, it is the duty of the city to do this, and in the discharge of that duty to exercise reasonable care (See Turner v. City of Newburgh, 109 N. Y. 301 ; Pettengill v. City of Yonkers, 116 id. 558), and it is manifest from the entire charge that this is just what the jury must have understood. The court charged the jury that they were to determine whether the ridges of. ice had existed for a sufficient length of time so that the city officials ought to have known that they were there and to have removed them, that nothing unreasonable or impossible was required of the city, and that they were to. consider the difficulties attending sndden.changes of weather. While the language used might have.been more exact-, that criticism can. be passed upon practically every charge, as a trial judge cannot be expected to define rules of liability with the exactness and' precision of ' a text. Writer. The defendant contented itself with a general exception, without calling the attention of the court to any precise point which it desired elucidated. Moreover,- it ds apparent that the defendant was not prejudiced. This portion of the charge related to the question of the defendant’s negligence respecting the ridges of ice, and it is difficult to see how a jury could have arrived at any other conclusion on that question. A reading of this record leaves little room for doubt that the ridges were formed from the cause' assigned by the plaintiff, and the defendant’s witness, who must have known the most about it, admitted that, they were there throughout the
Hirsohberg, P. J., and Hooker, J., concurred; Bioh, J., read for reversal, with whom Jenks, J.,. concurred.
Dissenting Opinion
Hawthorne avenue is a public street in the city of Yonkers, descending northerly to Main street at a very steep grade —14.2 feet in 100. Along the sidewalk on this avenue, opposite premises owned by one Schleuter, is a high retaining wall through which a pipe leads, forming an overflow discharge for surface water accumulating on the premises and conducted into a deep basin underneath the sidewalk. On February 20, 1904, the plaintiff, while passing over a sidewalk on .this street, slipped and fell at a point nearly opposite the pipe referred to, sustaining the injury for which she has recovered in this action. The evidence tends to establish that at the place of the injury there was ice upon the walk, in ridges, which had accumulated some time before, and that the sidewalk had been in practically the same condition, so far as the accumulated ice was concerned, for at least three weeks prior to the injury. The temperature did not rise above thirty-two degrees from February fifteenth until three o’clock in the afternoon of the twentieth, when it was thirty-four degrees, dropping back to thirty-two at six o’clock and to twenty-one at midnight. During the night of February eighteenth it commenced to snow; the storm continued at intervals through the night of the eighteenth and all day the nineteenth, three inches of snow falling, which had not been removed from the walk in question at the time the plaintiff fell.
The evidence in this case establishes practically the same conditions that existed in Taylor v. City of Yonkers (105 N. Y. 202), and the principle of law established by that case, that where there are two concurring causes producing an injury, for one of which the municipality would be liable and for the other of which it would not, the plaintiff cannot recover unless it appears that but for' the
We. thus reach the inquiry whether the record discloses 'facts-which warrant that conclusion, or whether the verdict in this respect ■ was the result of surmise and speculation.
Prior .to the twentieth, while the same' condition as to the ridges of ice upon the walk are shown to have existed, the plaintiff passed over the walk five or six times-without slipping or falling. The evidence as to the manner-in which she slipped is very meager, and the case is,-barren of any proof establishing or warranting the inference
I am sure of that. The snow that lay on this ice,-of those ridges, on which I fell, was the snow that had fallen the day before. I am positive that that snow that fell the day before had not been cleaned off, and I am positive that that snow was the snow that covered those , ridges on Saturday, the day I fell. Q. In other words, that less than twenty-four hours had elapsed between the fall of this snow and your fall on those ridges of ice. You fell on those ridges within one day after the snow fell? A. Yes, sir. Q. And that snow was still there and had not been removed ? A. Yes, sir. I fell a quarter or ten minutes of seven. I left the house a quarter of seven. I say that this sidewalk was icy at this place where I fell. It was the snow that was worn smooth that had fallen the day before.” This evidence hardly admits of any inference other than that the existing ice ridges on the walk had been covered by a new surface of snow, falling on the day before, which had been trodden down to smooth ice by travel,, and upon this new icy surface the plaintiff slipped and fell. Ho one can say with any degree of certainty that if 'this sharply-slanting walk had been clean when-the storm of the day before commenced, and the three inches of snow falling had spread uniformly over its surface and had been trodden down until it formed smooth ice, the plaintiff would not have fallen the same as she did. Adopting the language used by the court in the Taylor (Jase (supra), the plaintiff slipped upon this new-formed icy surface. That by itself was a sufficient, certain and operating cause of’ the fall. Ho other explanation is' needed to account for what happened. It is possible that the ice ridges existing when the storm commenced had something to do with it. It is also possible that they did not. There is no proof that they did. To affirm it is a pure guess and absolute speculation. The fact that the plaintiff had passed' over the walk in its ice-ridged condition on several occasions immediately prior to the formation of the new surface
For the reasons stated I think the judgment and order should be reversed and a new trial ordered, costs to abide the event.
Jerks, J., concurred.
Judgment and order of the Oounty Court of Westchester county affirmed, with costs. .