Bailey v. Mill Creek Coal Co.

20 Pa. Super. 186, 1902 Pa. Super. LEXIS 204
Superior Court of Pennsylvania·Decided April 21, 1902·No. Appeal, No. 238·Published·Cited by 1 cases

Opinion

Opinion by

Rice, P. J.,

The facts of this case are in many particulars the same as those which appeared in the case of Hoffman against the same defendant, 16 Pa. Superior Ct. 631. But in the particular about to be noticed the cases differ. There the plaintiff claimed title by adverse possession, and by his own testimony limited his claim and possession by the stone wall which separated his lot from the creek. The deposit in the bed of the creek was not upon his land. At least, the testimony did not show it to be. In this case the plaintiff’s deed calls for Canal street on the south. It appears from the map introduced evidence by the defendant that at that point Mill Creek flows longitudinally through Canal street. The general rule is, that where a public street, highway or alley is called for as a boundary in a deed, the grantee takes title in fee to the middle of the street, if the grantor had title thereto, and did not expressly, or by clear implication reserve it; and where there is no evidence as to the grantors’ title, it will be presumed to have extended to the middle of the road or street. If that rule is to be applied here, the plaintiff’s title, subject to the rights of the public, includes part of the bed of the stream, which it is alleged, has been raised by the deposits of coal dirt brought down from the defendant’s and other collieries. The proportionate responsibility of the defendant for the resultant injury has been established by the verdict of th.e jury upon sufficient evidence and is not now in question. The question is as to the measure of damages. The jury awarded for temporary damages $237.44 and for permanent damages $225. The lat-. ter were awarded upon the theory, that, even if no more coal dirt is deposited in the stream, the bed of the creek will not be freed by the washing of the waters from the deposit; in other words, that the condition of the bed of the stream at the time of the trial is reasonably certain to be permanent, and that in consequence of raising the bed of the stream the plaintiff’s cel-', lar has been made permanently damp and. musty and her- abil-. [190] ity to drain her premises destroyed. It would seem clear that, if there was sufficient evidence to warrant the jury in finding those facts, there was no error in the instructions complained of in the first assignment of error, or in the answers to the defendant’s points, which are the subjects of the third and fourth assignments, or in the admission of evidence as to the effect of these conditions upon the market value of the property, which is the subject of the second assignment.

Was there sufficient evidence to warrant the jury in finding those facts ?

Concerning the permanence of the condition of the bed of the creek, the learned judge who tried the case said: “ All of the witnesses in the case who testified on the subject, as we remember, fix the quantity of coal dirt and muck in the bed of the creek as being much less now than it was prior to the flood of 1894. Between the flood of 1893 and the flood of 1894, the deposit of coal dirt in the creek was fixed at from three to five feet; some of the witnesses fixed it as high as five feet; whilst after the flood of 1894 and down to the present time it was fixed at from one and one half to two feet.” Some of the plaintiff’s witnesses, including her husband, testified that the deposit has been gradually decreasing and the bed of the creek lowering, and one of them testified, that, while there is still some deposit in the channel of the creek, “ the material that has made all this trouble is washed down pretty well; the creek is pretty fair at the present time.” If this were all the testimony, then, judging the future by the past, the conjecture that the condition of the bed of the creek at the time of the trial will continue permanently would seem not to rest on a very solid foundation. But one of the other witnesses testified, when asked whether or not the coal dirt now in the stream has formed a new bed, “ Well, it has about formed a new bed of the stream ; it becomes solidified, becomes perfectly solidified, j-ou may say.” Again, when asked whether from his observation the filling is of a temporary or a permanent character, he said: “ I believe the bed of the creek as formed now is permanent, I believe that it is there permanently. I think that the floods and rains we have had have Reduced it about as much as they will, from the fact that it is solidified noW, that the water, it does not have the same effect on it since it has taken off two or three feet of the [191] coal dirt.” This testimony, while adding an element of pro'of not so clearly brought out in the testimony of the other witnesses, is not absolutely irreconcilable therewith. Nor can we say that it was so improbable as to be unworthy of credit. Viewing the testimony as a whole, we cannot say that the court erred in submitting to the jury the question, whether the bed of the stream had been permanently raised by the deposit.

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Bailey v. Mill Creek Coal Co., 20 Pa. Super. 186, 1902 Pa. Super. LEXIS 204 (Pa. Ct. App. 1902).

20 Pa. Super. 186 (Bailey v. Mill Creek Coal Co.) — published by Counsel Stack Legal Research, free access to 12M+ legal documents.

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27 Pa. Super. 55 (Superior Court of Pennsylvania, 1905)