Berenholz v. United States

1 Cl. Ct. 620, 1982 U.S. Claims LEXIS 2297
CourtUnited States Court of Claims
DecidedNovember 23, 1982
DocketNo. 61-78
StatusPublished
Cited by32 cases

This text of 1 Cl. Ct. 620 (Berenholz v. United States) is published on Counsel Stack Legal Research, covering United States Court of Claims primary law. Counsel Stack provides free access to over 12 million legal documents including statutes, case law, regulations, and constitutions.

Bluebook
Berenholz v. United States, 1 Cl. Ct. 620, 1982 U.S. Claims LEXIS 2297 (cc 1982).

Opinion

OPINION

COLAIANNI, Judge:

Plaintiffs in this action are owners of a parcel of land situated adjacent to Lake Erie in Monroe County, Michigan, just north of the village of Estral Beach, Michigan. Plaintiffs seek to recover for the loss of their land due to erosion and flooding allegedly caused by defendant’s actions. Defendant, through the Army Corps of Engineers, removed a 35-ft. section of the dike protecting plaintiffs’ property from Lake Erie in order to transport equipment across plaintiffs’ land to effect emergency repairs on a dike protecting the north border of the village of Estral Beach. Plaintiffs contend that following the completion of these repairs, the removal of the equipment from plaintiffs’ farm, and the replacement of the 35-ft. section in the plaintiffs’ east dike fronting Lake Erie, the east dike gave way. As a result, plaintiffs’ farm was, and remains to this day, flooded.

Defendant maintains that plaintiffs’ claim sounds in tort and that they do not thus fall within the 28 U.S.C. § 1491 jurisdiction of this court. In addition, defendant suggests that any loss suffered by plaintiffs was caused by their failure to maintain their dike and the severe storms and flooding of 1972-73, and not the result of the impaired condition of the dike following the deliberate removal of a 35-ft. section by the Corps.

[622]*622For the reasons set out below, it is concluded that the defendant’s actions which resulted in a permanent flooding of plaintiffs’ land amounted to an invasion of the plaintiffs’ property rights and constituted a taking under the constitution, and plaintiffs are entitled to the fair market value of their property with interest.

Facts

Plaintiffs Gustav Berenholz, Antonina Miller, and Moshe Z. Miller are land contract purchasers of the 168-acre parcel of realty in question that is located in the Township of Berlin, County of Monroe, State of Michigan, hereinafter “the property.” The parcel in question, as well as the adjoining areas, including the Estral Beach area, a total of 640 acres in all, was owned by the Strong family for many years. The farm and the other acreage passed to Henry Strong upon the death of his father, John Strong. Henry kept the farm, but sold off the remaining property, including the Estral Beach acreage. Upon the death of Henry in 1946, his nephew, Fred Strong, inherited the farm.

Location of Plaintiffs' Property Relative to Village of Estral Beach.

As shown in the above sketch, the 168-acre farm lies directly north of the village of Estral Beach, Michigan, and is bounded on the north, south and east by earthen dikes, and on the west by Port Sunlight Road. The dike dividing plaintiffs’ property from the village of Estral Beach is plaintiffs’ south dike and the village’s north dike. It will hereinafter be referred to as the “south dike.” The eastern boundary of plaintiffs’ land is a north-south line proceeding due south from the east end of the north dike to a point due east of the south dike. A section of dike runs along the north one-half of this boundary and then takes a dogleg bend to the west to join the [623]*623south dike, leaving a portion of plaintiffs’ land outside the east dike. The “south dike” protected the northern portions of Estral Beach from flood water coming across plaintiffs’ land and also protected plaintiffs’ land if the flood waters were coming from the direction of the village. The “east dike” protected plaintiffs’ land from the waters of Lake Erie.

The property at issue was originally marshland. In 1913, dikes were built around the property by Fred’s grandfather, John. The dikes were made of clay which is abundantly found in the subsoil of the area. The north and south dikes were approximately one mile long and had a variable height, being highest at their eastern or Lake Erie ends and slowly descending as they approach the Port Sunlight Road boundary of the farm on the west. The east dike was about 1500 ft. long and about 6 ft. in height. Each of the dikes had a 30-to 40-ft. wide base and a 20- to 30-ft. wide flat upper surface. The top of the east dike was wide enough to accommodate a 14-ft. wide by 17-ft. long shanty which was in use for many years during Fred’s recreational visits to the property for skating and hunting.

The elevation of the farm dropped from about lake level at Port Sunlight Road to 5-6 ft. below lake level at the east dike. The farm was made up of a clay loam type soil west of the drainage ditch, as shown in the above sketch, and of a mucky topsoil east of that ditch. Because of the high water table, the farm did not drain well. Each spring over 100 acres of the farm would be covered with several feet of standing water due to the thawing of accumulated snow and the usual spring rains. This water would, because of the poor drainage of the soil, have to be pumped off the farm. The pumping operation would start in late April or May of each year depending upon weather conditions. It would sometimes take up to 10 days of 24-hour continuous pumping to remove all of the standing water. Following this, some additional time would be necessary for the ground to dry out so that crops could be planted. Because the pumping and drying out operations normally would not be completed before June, the type of crops which could be grown on this farm were limited. Over the years, soybeans, which could be planted in June and harvested as late as October or November, proved to be the most reliable crop.

The parcel had, beginning with John Strong in 1913 or 1914, continuously been used as a farm. Fred had successfully operated the farm from the time of his inheritance until he sold it. During the late 1940’s he personally farmed the land, but because of a change in circumstances, in the early 1950’s, Fred engaged Dale Reaume to farm the land for him. Mr. Reaume worked the farm and they shared the proceeds. This arrangement continued until the sale of the farm in September 1972.

For some 60 years the dike remained intact. In all of the years of its existence to the time of the action complained of, the dike had never leaked and had always effectively kept out the Lake Erie water. Several factors accounted for its durability. Expert testimony revealed that Lake Erie is the shallowest of the Great Lakes. It has a prevailing west-to-east wind which makes its eastern end deeper. The property is located at the western end of the lake, where the shallower depth diminishes wave action. The region is further protected from northeast winds by the topography of southern Ontario, which serves as a natural interruption of the fetch length (the distance of open water between the origin of the wind and the shore) to reduce the wave action at the shallow end. A large marsh area in front of plaintiffs’ land had over the years been greatly reduced in size, and, at the time of the April 1973 flooding, was largely submerged. It nonetheless still served to abate wave action against the east dike. Additionally, the dike was covered with brush and a line of deciduous poplar trees, spaced at approximately 6- to 10-ft. intervals, whose roots served to hold the clay of the dike together, and strengthen it against the elements. Some of the trees had grown so large that they could not be encircled by an adult’s out-stretched arms. [624]*624Smaller diameter trees and low growing brush grew between the larger poplar trees.

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Cite This Page — Counsel Stack

Bluebook (online)
1 Cl. Ct. 620, 1982 U.S. Claims LEXIS 2297, Counsel Stack Legal Research, https://law.counselstack.com/opinion/berenholz-v-united-states-cc-1982.