Destito v. State

207 Misc. 493, 139 N.Y.S.2d 97, 1955 N.Y. Misc. LEXIS 3426
New York Court of Claims·Decided March 3, 1955·No. Claim No. 28030·Published·Cited by 1 cases

Opinion

Lotjnsbebry, P. J.

This claim is for damages to the claimants ’ premises, situate on Dominick Street in the city of Borne, adjacent to the Mohawk Biver, resulting from an overflow of that river which occurred October 2, 1945. The claimants contend that the flood resulted from negligence and mismanagement in the operation by the State of Delta Dam, which dams the Mohawk about five miles above Borne and forms a substantial reservoir known as Lake Delta.

This is the second appearance of this problem before this court. Iodice v. State of New York (Claim No. 28103), decided by this court June 10, 1949, arose from the same fact situation and involved other premises in the same vicinity. We concluded that improper and negligent operation of the dam during the year 1945 caused, or at least aggravated, the flood condition in [495]*495the city of Borne, and granted judgment in favor of the claimant. The Appellate Division disagreed, however, and dismissed the claim (277 App. Div. 647), on the grounds that the dam was erected to supply water for the Barge Canal and that the State was under no duty, either by statute or by common law, to operate it for flood control purposes; that it violated no right of the claimant so long as it discharged no greater volume of flood waters from the dam than flowed into the reservoir; and, that during the flood in question it in fact discharged from the dam a lesser volume of water than meanwhile entered the reservoir. The Court of Appeals affirmed the decision of the Appellate Division without opinion (303 N. Y. 740).

The decision of the Appellate Division in the Iodice case {supra), must therefore necessarily govern the disposition of the present claim unless the claimants establish either (a) that the very existence of the artificial structure known as Delta Dam and of the artificial lake formed by it in some manner caused the flood on the claimants’ premises to be worse than it would have been had the dam not existed; or (b) that the State in fact discharged more water from the dam than flowed into the reservoir during the flood period; or (c) that the dam was in fact erected in part for flood control purposes and was improperly regulated for such purposes; or (d) that, whatever the original purpose of the dam, the State had in fact assumed a duty to operate the dam with regard to flood prevention and had improperly discharged such duty.

The record is extremely voluminous, comprising 2,362 pages and some 140 exhibits, to which must be added 889 pages of testimony and some 80 exhibits in the Iodice case which were incorporated by reference into the present record. It is obviously impossible to detail this mass of material, but the court deems the following essential facts adequately established.

By chapter 147 of the Laws of 1903, known as the Barge Canal Act, the reconstruction of the existing canal system into what is now known as the Barge Canal system was authorized, subject to approval by the voters of a $101,000,000 bond issue for the purpose, which approval was given at the ensuing general election. The act provided, among other things: ‘£ The additional water supply required for the improved Erie Canal shall be provided by * * * and building storage reservoirs on the upper Mohawk near Delta and on West Canada Creek near Hinckley, with all necessary feeders for connecting these and existing reservoirs with the improved canal. The supply of water for the Erie Canal shall be sufficient for the uses of the [496]*496canal with at least ten million tons of freight carried on it per year.”

Pursuant to this authority the State began in 1908, and completed about 1911, the erection of a large dam across the Mohawk just below the former village of Delta and about five miles upstream from Rome. The completed structure was about 1,300 feet in overall length and about 100 feet high. At a level about eight feet below the top of the rest of the dam was a spillway 300 feet long, the elevation of which was 550.2. The resulting reservoir had an area of about 4% square miles, and a capacity, when filled to spillway level, of approximately 2,750,000,000 cubic feet of water. At the base were located four discharge pipes, controlled by valves, having a total discharge capacity of about 3,000 cubic feet per second when the reservoir was full, and somewhat less when the water elevation was lower. The construction involved the razing of 295 structures comprising the entire village of Delta, the removal of all trees located in the reservoir area, and the relocation of roads and of a portion of the Black River Canal. The area which drained into the reservoir comprised about 150 square miles. Provision was made for securing additional water by diversion from the Black River by way of an artificial channel known as the Forestport Feeder, which empties into the Mohawk above the Delta Dam.

The waters discharged from the dam flow south along the Mohawk River channel, which was left in its original condition, and into the summit level of the Barge Canal at Rome. The summit level is about 18 miles in length, extending from Lock 21 about a mile west of New London, easterly through Rome to a point about five miles west of Utica. Its chief source of water supply is Lake Delta, but provision exists for securing additional water from Hinckley Reservoir by means of a channel known as the Nine-Mile Feeder, which discharges into the summit level east of Rome. Hinckley Reservoir, also constructed pursuant to the Barge Canal Act, was formed by draining the West Canada Creek, the waters of which normally reach the canal east of the summit level. Excess water is discharged back into the Mohawk River by means of four spillways, located east of Rome, the principal one of .which is the Nine-Mile Creek spillway. Stand- - ard practice is to maintain the water in the summit level at elevation 420. Above elevation 422.5 navigation ceases because of loss of necessary clearances.

Until the year 1945, it had been the practice of the State to maintain the water level in Delta Reservoir several feet below [497]*497the spillway height from late spring through the rest of the navigation season, which lasts until about December 1st. Thus, in the period 1930 through 1944, the average distances between the water level and the top of the spillway were: May 20th, 2.02 feet; June 30th, 4.114 feet; July 30th, 6.354 feet; August 30th, 8.767 feet; September 30th, 9.76 feet; October 30th, 9.527 feet; November 30th, 7.814 feet.

In 1945, the practice was entirely different. The water level remained continuously above the spillway until August 14th. Thereafter it gradually lowered to about two feet below on September 11th. It again rose above the spillway, remained mostly above for several days, and then fell to a point 2.4 feet below on September 25th. It again rose, and on October 1st stood at elevation 550.4, or 0.2 above spillway. On October 1st, 0.37 inches of rain fell, followed by 3.81 inches on October 2d, a two-day total of 4.18 inches. The reservoir level raised to 554.3, or 4.1 feet above spillway. The Mohawk overflowed its banks at Borne, flooding claimants’ and other premises. Lifelong residents and official records agree that there had never before been a flood in this section of Borne, aside from some temporary flooding resulting from ice jams, the cause of which had been eliminated many years ago. The canal reached elevation 424.3 and all navigation ceased.

1945 was a year of heavy rainfall.

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Destito v. State, 207 Misc. 493, 139 N.Y.S.2d 97, 1955 N.Y. Misc. LEXIS 3426 (N.Y. Super. Ct. 1955).

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Destito v. State
1 A.D.2d 753 (Appellate Division of the Supreme Court of New York, 1955)