Hoffman v. Mill Creek Coal Co.

16 Pa. Super. 631, 1901 Pa. Super. LEXIS 120
Superior Court of Pennsylvania·Decided April 16, 1901·No. Appeal, No. 203·Published·Cited by 14 cases

Opinion

Opinion by

Rice, P. J.,

On or near the banks of Mill creek are several collieries and washeries, and amongst them one operated by the defendant company. On the trial of this case evidence was given which tended to show, that in conducting- its business the defendant deposited culm and coal dirt upon its premises in such a way that naturally, and as was to be expected, it was carried into the stream and thence down the same, until it, in connection with similar deposits brought from other collieries, raised the bed of the stream at or near the plaintiff’s premises from two to four feet, according to the varying testimony of the witnesses.

[635] The plaintiff claims to be the owner of three contiguous lots, upon each of which there is a dwelling house. To part of this land he showed title by deed, and to the easternmost lot, the one nearest the creek, he claimed title by adverse possession. It is argued that his title by possession extended to the middle of the stream, but this contention is not sustained by his testimony. For a part of the distance the lot of H. E. Paul lies between his lot and the creek, and for the remainder of the distance a stone wall separates his lot from the creek. He testified unequivocally that his claim and possession eastwardly extended to the Paul lot and the stone wall, and there is no evidence that they extended further so as to embrace any part of the bed of the creek.

The plaintiff showed that in the freshets which occurred in January and February, 1893, the stream overflowed its banks and deposited in his cellars and on the surface of his lots considerable quantities of culm and coal dirt.

He also claims that since 1890, or thereabout, his cellars have been damp, and at times have had water in them, and he asked the jury to infer from other testimony given by him and his witnesses that these latter conditions were caused by the raising of the bed of the stream; in other words, that, as a result of the deposit of coal dirt, the stream is, in ordinary high water, above the level of his cellars, and that when it is raised by rains the water soaks through the soil into his cellars. The evidence adduced in support of this latter claim is not as clear and satisfactory as might have been furnished if the fact be as he claims. We cannot say, however, that it was not sufficient to carry the question to the jury, and in our consideration of the questions of law raised by the assignments of error we shall assume that their verdict has established the fact that the conditions last described were caused directly or indirectly by the raising of the bed of the stream, and that they will continue or recur as long as the bed of the stream remains at the same level.

We shall consider first and separately the plaintiff’s injury caused by the washing of culm and coal dirt upon his land in the freshets of 1893, because there is a distinction between a direct trespass and a consequential injury resulting from something done or maintained off the plaintiff’s land which may or [636] may not continue. The general doctrine is, that where injury is caused by trespass on the plaintiff’s land, since the defendant cannot remedy the wrong without another trespass, the injury is to be treated as inflicted once for all and full compensation is to be recovered in one action: 1 Sedg. on Damages, sec. 92, p. 128. But it does not necessarily follow that the measure of damages for the injury caused in 1893 was the difference between the market value of the lots before the coal dirt was deposited on them and their market value as affected by that deposit if allowed to remain. Prima facie the measure of damages would be the cost of removing the deposits and putting the premises in as good condition as they were before, if that could be done, and compensation for the total or partial loss of the use and enjoyment of the premises in the mean time. If, however, the cost of removing the deposits and restoring the land to its former condition would be greater than the injury from them, if allowed to remain, then the true measure of damages would be the difference in value merely. This is the doctrine of Seely v. Alden, 61 Pa. 302. But before invoking the application of the latter measure of damages we think it was incumbent on the plaintiff to give evidence from which a jury might conclude with some degree of certainty that the former measure would not fully compensate him for his injury, and in this particular there is a failure of proof. To show that the soil was unfit for cultivation, after he had plowed under the culm, was not sufficient to entitle him to recover the difference in value upon the theory that the injury was permanent, unless he also showed that the cost of removing it would have been greater than this difference, or unless, by reason of the quantity of the deposit, the jury would have been justified in inferring this latter fact without further proof.

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Hoffman v. Mill Creek Coal Co., 16 Pa. Super. 631, 1901 Pa. Super. LEXIS 120 (Pa. Ct. App. 1901).

16 Pa. Super. 631 (Hoffman v. Mill Creek Coal Co.) — published by Counsel Stack Legal Research, free access to 12M+ legal documents.

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