Majority
Headnote
1. Adjoining Landowners—Lateral Support.The plaintiff was the owner of land south of Jefferson street, in the village of Haverstraw, and the defendant owned a considerable tract of land north of that street. The soil in this vicinity, north and south for several miles and back from the Hudson river several hundred feet, is peculiarly adapted to the making of brick, and for upwards of 25 years the plaintiff and his predecessors in title have been engaged in digging away the surface of his land to procure materials therefor. The defendant has also been engaged in the same enterprise, and in the year 1895, owing to more extensive operations, had dug deeper into his premises than the plaintiff. This action was brought to recover damages resulting from the defendant’s extensive excavations, by reason of which in each of the years 1895 and 1899 large quantities of clay and sand subsided or slid from plaintiff’s land upon those of the defendant. The excavations and operations still continued, and an injunction was asked to restrain the defendant from further similar use of his lands. Defendant had dug up to the center of the 50-foot strip known as “Jefferson Street,” which appears to have been long since abandoned as a public highway. The complaint was dismissed upon the merits, and plaintiffs appeal.
The court made this finding of fact:
“The subsiding and falling and slipping away aforesaid of soil On the lands of the plaintiffs, and the subsiding, falling, and slipping away of the soil mentioned in the complaint, were caused by or contributed to by the acts and excavations by the plaintiffs and of their predecessors in title on the lands ■owned as aforesaid by the plaintiffs,, and by the acts and excavations of the .plaintiffs on said strip of land called ‘Jefferson Street.’ ”
The finding as to the contributing cause is supported by the evi■dence. The excavations of the plaintiff had not been such as to result •in a mere depression of the whole surface of his lands. Their result was to leave the new exposure irregular in shape. Contiguous with the ■center of Jefferson street, to which point the defendants had brought their excavations, the plaintiff had left the surface of his ground_ so that its formation was wedge-like in shape, the evidence warranting the conclusion that the pyramid or wedge was some 200 feet in width and about 250 feet from apex to base. The physical condition, which resulted in the leaving of this pyramid, was that the plaintiff deprived that part of his land adjacent to his northern boundary at Jefferson street of the full measure of support by cohesion which it would have possessed had the lands been left in their original.natural state, or had the excavation resulted in a practically level surface.
It seems to be settled that, so far as lateral support of the soil is concerned, in its natural state, without the burden of buildings upon it
The views w6 have expressed render it unnecessary to discuss the legal questions said to be involved by reason of.the 50-foot strip, known as “Jefferson Street,” intervening between the lands of the parties, and the questions of ownership therein presented by the record.
The judgment should be affirmed, with costs. All concur,
Cases cited
- Panton v. Holland 17 Johns. 92 p. 611
- Dorrity v. Rapp 72 N. Y. 307 p. 611
- Hay v. Cohoes Co. 2 N. Y. 159 p. 611
- Farrand v. Marshall 21 Barb. 409 p. 611