100 N.Y. 424 | NY | 1885
[EDITORS' NOTE: THIS PAGE CONTAINS HEADNOTES. HEADNOTES ARE NOT AN OFFICIAL PRODUCT OF THE COURT, THEREFORE THEY ARE NOT DISPLAYED.] *426
[EDITORS' NOTE: THIS PAGE CONTAINS HEADNOTES. HEADNOTES ARE NOT AN OFFICIAL PRODUCT OF THE COURT, THEREFORE THEY ARE NOT DISPLAYED.] *427 This action involves the title to certain beach lands on the ocean shore at Far Rockaway. No dispute arises over the boundaries of the plot, or the location of the beach, as being included within the description of the deeds under which plaintiff's grantors formerly occupied the premises, but it is claimed that the earth or sand composing the beach has been *430 so affected by the storms and tides of the ocean that its ownership was lost by the plaintiff's grantors, and subsequent deposits, made within the same boundaries, were acquired by the owners of Long Beach, an island belonging to the town of Hempstead. This result is attempted to be supported under the rule governing the acquisition of real property by alluvion or accretion. The evidence tends to establish the following facts: That the beach in question is within the same boundaries, and, with the exception of a narrow lagoon running crosswise through it, is of the same form and shape now as it existed from the year 1685, when it was conveyed to the plaintiff's remote grantors by its Indian owners, to about the year 1835. Between 1835 and 1869 the changes in the surface of the ground took place which it is claimed worked the transfer of the ownership. At the commencement of the process of change, Long Beach consisted of a small island lying southward of Hempstead bay, separated on the west from the beach in dispute by a navigable inlet called indifferently Hog Island, or East Rockaway Inlet, or Brockle Face Gut, and a succession of beaches, islands, shoals and channels, extending some four miles. This inlet was about half a mile broad and communicated directly with the westerly end of Hempstead bay. To the west of the inlet a bar or beach known as Coot's bar extended from the mainland south to a point opposite to Long Beach, forming the westerly shore of Hempstead bay, and from thence west a distance of about three miles until it reached the westerly line of the town of Hempstead. The beach to the westward of the inlet, during the period from 1835 to 1869, underwent a succession of changes which it is quite unimportant if not impossible, to follow in detail, but usually consisted of a line or group of bars, shoals, islands and channels extending from the inlet to the shore of the mainland beyond the premises in dispute, but which were constantly undergoing physical changes by the influence of the laws to which they were naturally subject. These bars, shoals and islands were from the operation of the tides and wind in filling the channels, separating them, occasionally joined together, and at one time by the removal *431 of the inlet in question to the westward formed a continuous bar from Long Beach to a point west of the premises in dispute, and remained in that position for about three years. The removal of the inlet to the west was not uniformly effected by gradual progression, but frequently advanced in "jumps" of a quarter to a half a mile in distance, and frequently added or took away from the lands to which they were joined sections of beach covering half a mile or less in extent as the result of a single storm. During the period of time in question various inlets at different points upon this bar, were broken through from time to time, and were used by vessels trading in Hempstead bay until they were closed up by the action of the tide and wind, when other channels, by the operation of natural causes, would be opened in new places, and these openings would in turn become the channels through which vessels bound to and from Hempstead bay would pass.
About the year 1869 the inlets to the westward became closed up, and the original inlet adjoining Long Beach was reopened and has since become the sole channel of navigation for vessels entering the bay from the east. The process described finally resulted in attaching the beach in litigation to the mainland on the west, and forming a continuous beach about one thousand feet broad from such mainland to the inlet at Long Beach, being a distance of about four miles. This process also left a shallow and narrow lagoon or cove running inside of the beach in question from Hempstead bay to a point a little to the westward of the premises in dispute and separating the ocean beach proper from the mainland lying directly behind it.
In 1725 the formation of Coot's bar was of so permanent a character that it became the subject of a grant from its owner, the town of Hempstead, to one Hicks, and from that time to the present the said Hicks and his heirs and grantees have occupied and enjoyed the beach lying between the original Hog Island inlet and the west line of the town of Hempstead and reaching within about eighteen hundred feet of the premises in dispute. Portions of this beach have at times been submerged or washed away, and it has at times been cut into *432 by the formation of new inlets to Hempstead bay, but at all times there has been some beach lying above the ocean tides, but outside the line of high-water mark capable of occupation and enjoyment by its owners.
Under these circumstances the trial court refused to find that the extension of Long Beach to the westward was made by the process of accretion, and held as a question of law that the defendant's lessors, the town of Hempstead, did not acquire title to the land in dispute by that process, and we concur in the conclusion reached by it.
There seems to be but little conflict in the authorities or even between counsel in this case as to what constitutes alluvion or accretion. It was held in Rex v. Lord Yarborough (3 B.
C. 91) "that accretion is an increase by imperceptible degrees." "The lord of the manor claims when there is a gradual accession to land adjacent." (Wash. on Real Prop. 58.) "The test of what is gradual as distinguished from what is sudden seems to be that, though witnesses are able to perceive from time to time that the land has encroached on the sea line, it is enough if it was done so that they could not perceive the progress at the time it was made." (Angell on Tide Waters [1st ed.], 71.) It was said inEmans v. Turnbull (2 Johns. 314) "that, if the marine increase be by small and almost imperceptible degrees, it goes to the owner of the land; but if it be sudden and considerable it belongs to the sovereign." (Citing 2 Blackst. Com. 261; Harg. Law Tracts, 28.) "To acquire title to land by alluvion, it is necessary that its increase should be imperceptible." (Halsey
v. McCormick,
It would seem from these definitions that two insuperable objections exist to the claim of the appellant; one being that a large part of the formations, of which the beach in question now consists, was created anterior to the junction thereof with Long Beach and constituted property subject to acquisition and ownership by others prior to plaintiff's claim; and secondly, that the mode of progress of Long Beach to the westward was frequently by sudden removals of the inlet, and the consequent junction of large and perceptible sections of beach to the easterly *433 lands — as the result of a sudden and violent operation of the tides. We, therefore, think the court below correctly held that the defendant did not acquire a legal right to the possession of the lands in question by his lease from the town of Hempstead.
It is also claimed by the appellant that even if he has failed to establish title in himself to the premises, that the plaintiff still is not entitled to maintain this action because of defects in his own title. It is argued that the beach in question having been once cut off from the mainland and surrounded by navigable water, thereby became an island, which, like other formations of land in tide water, was the property of the State.
The evidence establishes a continuous chain of title to the premises in dispute from its native Indian owners down to the plaintiff, covering a period of two hundred years, and each conveyance bounding its grantee upon the Atlantic ocean. Under the law of this State such a description makes the line of high-water mark the boundary of the granted premises, but it also carries with it the liability of such a line to fluctuate by the action of the water. These lines of description for a period of one hundred and fifty years included the locus in dispute, and the same, with the uplands, was occupied and enjoyed by the plaintiff's grantors and now remain the property of the plaintiff, unless the title thereto has been lost to his grantors through the causes referred to.
It is undoubtedly true that the proprietorship of lands may be lost by erosion or submergence. The one consisting of a gradual eating away of the soil by the operation of currents or tides, and the other of its disappearance under the water and the formation of a navigable body over it. The plaintiff's grantors have at all times since 1684 remained the owners and occupants of the mainland adjacent to the beach in dispute, and as such owners have been entitled to the rights which attend the title of littoral or riparian owners. "They would be entitled to whatever should be gained from the sea by alluvion or dereliction, and their title was liable to be lost by the advance of high-water mark, bringing their lands within the ebb and *434
flow of the tide." (East Hampton v. Kirk,
When portions of the mainland have been gradually encroached upon by the ocean so that navigable channels have been extended thereover, the people, by virtue of their sovereignty over public highways, undoubtedly succeed to the control of such channels and the ownership of the land under them in case of its permanent acquisition by the sea. It is equally true, however, that when the water disappears from the land, either by its gradual retirement therefrom or the elevation of the land by avulsion or accretion, or even the exclusion of the water by artificial means, its proprietorship returns to the original riparian owners. (Angell on Tide Waters, 76, 77; Houck on Rivers, § 258.) Neither does the lapse of time during which the submergence continues bar the right of such owner to enter upon the land reclaimed, and assert his proprietorship. (Angell on Tide Waters, 77-80, and cases cited.) It is said in Hargraves' Law Tracts (Sir Matthew Hale's De Jure Maris), 36, 37: "If a subject hath land adjoining the sea, and the violence of the sea swallow it up, but so that yet there be reasonable marks to continue the notice of it, or though the marks be defaced, yet if by situation and extent of quantity and bounding upon the firm land the same can be known, though the sea leave this land again, or it be by art or industry regained, the subject does not lose his property, and accordingly it was held by COOKE and FOSTER, M. (7 Jac. C.B.), though the inundation continue forty years." "But if it be freely *435 left again by the reflex and recess of the sea, the owner may have his land as before, if he can make it out where and what it was; for he cannot lose his propriety of the soil though it be for a time become part of the sea, and within the admiral jurisdiction while it so continues." And again: "As touching islands arising in the sea or in the arms of creeks or havens thereof, the same rule holds which is before observed touching acquests by the reliction or recess of the sea, or such arms or creeks thereof. Of common right, and prima facie it is true they belong to the crown, but where the interest of suchdistrictus maris, or arm of the sea or creek or haven, doth in point of property belong to a subject, either by charter or prescription, the islands that happen within the precincts of such private propriety of a subject will belong to the subject according to the limits and extents of such propriety." (See, also, Gould on Water, § 166.) A case quite in point is referred to by the respondent's counsel as arising in Delaware in 1815, decided by the Court of Common Pleas upon a learned opinion by Judge WILSON, a copy of which is attached to the plaintiff's brief. The case does not seem to be elsewhere reported. It arose over the ownership of an island called Wilson's Bar, which had been created by alluvion upon land formerly contained within the boundaries of an island called Little Tinnicum, but which at some time had been worn away by the ocean. The court say: "The right to the new island and also to land gained by alluvion or dereliction, all of which are governed by the same principle, follows the right to the soil which is covered by the water. Though the surface of the lower part of Little Tinnicum was destroyed by the force of the winds and the waves, and it was consequently overflowed by the water of the river, yet the owner did not lose the propriety of the remaining land covered by the water if it was regained either by natural or artificial means, it continued to belong to the original proprietor." "The earth deposited on it became his by the right of alluvion, and of course this island formed on it by such deposit became his. And though it probably has extended *436 beyond the limits of the old island, the addition is plainly alluvion."
It would seem also to follow as the necessary consequence of these rules that the existence of the lagoon between the plaintiff's hotel property and the beach constitutes no obstruction to his proprietorship of the beach formation, however created, if located within the original boundaries of his possession. (Deerfield v. Arms, 17 Pick. 43.) It was held in the case of Railroad Co. v. Schurmeir (7 Wall. 272) that a sand bar in the Mississippi river divided from the mainland by a slough twenty-eight feet wide, and which at high water was entirely submerged, belonged to the riparian owner, although the acts of Congress made the river a public highway at the place in question. It is also said that "rocks and shoals lying along the margin of navigable fresh rivers belong to the riparian owners." (Gould on Water, § 77.)
The evidence in the case and the findings of the trial court concur in establishing the fact that during the period of change hereinbefore mentioned portions of the beach in front of plaintiff's premises became submerged, but at all times there existed upon or near such premises, shoals bars or islands, which afterward became the nucleus around which gathered the deposits now composing the land subject to litigation. It seems to us clear that the owners of this property did not lose their title thereto by reason of the changes described, and that the State has not acquired any property therein. The sovereign succeeds to the ownership of such islands and formations only as are originally created and located in tide-ways outside of the boundaries of property subject to individual ownership.
We are also of the opinion that the principles applicable to the apportionment of lands formed by accretion among the owners of contiguous uplands is quite controlling as to the rights of the respective parties in this case. Such owners are entitled to lands made by accretion or reliction in front of their property and contiguous thereto in certain proportions according to the formation of their respective shore lines. (Houck on Rivers, § 162; 3 Wn. on Real Prop. 58; Angell on *437 Tide Waters, 171.) However such accretions may be commenced or continued, the right of one owner of uplands to follow and appropriate them ceases when the formation passes laterally the line of his coterminous neighbor. "A littoral proprietor, like a riparian proprietor, has a right to the water frontage belonging by nature to his land, although the only practical advantage of it may consist in the access thereby afforded him to the water for the purposes of using the right of navigation. This right is his only and exists by virtue and in respect of his riparian proprietorship." (Gould on Water, § 149; Buccleuch v.Metropolitan Bd. of Works, L.R., 5 H.L. 418.)
The principles upon which the rights of littoral proprietors to lands reclaimed from the sea are determined have been frequently discussed in cases arising in our sister States, but those discussions are not important here, and the cases are referred to only for the purpose of showing that such reclamations are apportionable among the littoral owners according to the lateral lines of upland possessed by them. (Gould on Waters, §§ 162, 163, 164 and 165; Deerfield v. Arms, 17 Pick. 43; Wonson v.Wonson, 14 Allen, 85; Thornton v. Grant,
It would seem to follow from the principles referred to that the owner of Long Beach could not, even if the process of its enlargement and extension was effected by accretion, claim beyond the point where such accessions began to be made adjacent to the property of adjoining owners, and as the line of each successive owner of uplands was reached in the process of extension a new obstacle to the appellant's claim would seem to arise. This result would occur undoubtedly after passing Hog Island inlet as some of the land westerly thereof was originally solid beach, and occupied by the grantees of Hempstead before the extension of Long Beach.
Aside from those discussed no material objection was made *438 to the judgment appealed from except that concerning the jurisdiction of a court of equity over actions of this character.
The circumstances of the case are peculiar, and we think within established principles entitle the plaintiff to the relief sought. He was the owner of a hotel upon the ocean beach greatly resorted to by visitors in the summer for the benefit of surf bathing and sea air, and which could be enjoyed by them advantageously only by the undisputed control of the beach in question by the owner of such hotel. The use and character of the property was such that intruders thereon could not be excluded by substantial barriers, and a remedy against them by an action of trespass would necessarily be of doubtful success, and probably afford an inadequate indemnity for the injuries inflicted. During a long period of time successive efforts have been made by the defendant and his lessors to obtain possession of the premises in dispute and occupy them to the exclusion of the plaintiff. Actions have been threatened against him and claims of title made, which constitute a serious annoyance to the owner and impairment of his ability to derive an adequate compensation for the use and rental of such property. The defendant Norton transferred an interest in his lease to the other defendant Levy in order to multiply the claimants to the beach, and the prospect of successive litigations in connection therewith. These annoyances had continued for a series of years and occasioned damage to the plaintiff's rights of property which could not be easily ascertained or adequately compensated for in an action at law. The evidence also tended to show that the defendant Levy was a person of little pecuniary responsibility and presumably unable to respond in damages for the injury his conduct was liable to inflict upon the plaintiff's rights. Under similar circumstances the jurisdiction of a court of equity to interfere by injunction to quiet the title and prevent an injury for which no adequate remedy exists at law has been frequently exercised and approved by the courts. (Hilliard on Inj., chap. 10, § 1; Watson v.Sutherland, 5 Wall. 74; Livingston v. Livingston, 6 Johns. *439
Ch. 497; Lacustrine Fertilizer Co. v. L.G. F. Co.,
We think this a case where the remedy by injunction was proper, and within the principles laid down in the cases cited.
The judgment should, therefore, be affirmed.
All concur.
Judgment affirmed.
