Yankton County, South Dakota v. United States

CourtUnited States Court of Federal Claims
DecidedDecember 21, 2017
Docket17-488
StatusPublished

This text of Yankton County, South Dakota v. United States (Yankton County, South Dakota v. United States) is published on Counsel Stack Legal Research, covering United States Court of Federal Claims primary law. Counsel Stack provides free access to over 12 million legal documents including statutes, case law, regulations, and constitutions.

Bluebook
Yankton County, South Dakota v. United States, (uscfc 2017).

Opinion

In the United States Court of Federal Claims No. 17-488L (Filed: December 21, 2017)

************************************* YANKTON COUNTY, SOUTH * DAKOTA, a County of the State of South * Dakota, * * RCFC 12(b)(1); Takings Clause of the Plaintiff, * Fifth Amendment; 28 U.S.C. § 2501; * Statute of Limitations; Claim Accrual; v. * Stabilization Doctrine; Justifiable * Uncertainty THE UNITED STATES, * * Defendant. * *************************************

Mark V. Meierhenry, Sioux Falls, SD, for plaintiff.

Carter F. Thurman, United States Department of Justice, Washington, DC, for defendant.

OPINION AND ORDER

SWEENEY, Judge

In this case, plaintiff Yankton County, South Dakota (“Yankton County”) alleges that certain dam construction and operation activities undertaken by the United States Army Corps of Engineers (“Corps”) along the Missouri River have led to an unnatural alteration of the river’s stream bed, effecting a taking of plaintiff’s property and damages to two bridges owned by plaintiff without just compensation in violation of the Takings Clause of the Fifth Amendment to the United States Constitution. Plaintiff seeks $11.5 million in damages plus attorney’s fees, costs, and expenses. As explained below, because plaintiff’s claim accrued more than six years before plaintiff filed suit, this court lacks jurisdiction over the instant case.

I. BACKGROUND

The Missouri River is the “longest river in North America,” extending approximately 2,341 miles from western Montana to just north of St. Louis, Missouri, where it joins with the Mississippi River. 1 Compl. ¶ 5. Gavins Point Dam, which is located west of the city of Yankton

1 The facts in this section—which are undisputed for the purpose of resolving defendant’s motion to dismiss—derive from the complaint, the parties’ submissions (including attached exhibits), and matters of which the court may take judicial notice pursuant to Rule 201 of the Federal Rules of Evidence. in Yankton County, South Dakota, is the furthest downstream dam along the Missouri River. 2 Id. ¶¶ 6-7. The first major tributary entering the Missouri River downstream from Gavins Point Dam is the James River. Id. ¶ 21. The James-Missouri confluence is east of the city of Yankton in Yankton County, South Dakota. Id. ¶ 20. Plaintiff owns two bridges that cross the James River: Fleeg’s Bridge, which is approximately four miles upstream from the James-Missouri confluence at County Road 366, and Johnson Bridge, which is further upstream at 303rd Street. Id. ¶¶ 31-33.

Healy Aff. Ex. 3 at 8.

Construction of Gavins Point Dam was completed in 1955. Compl. ¶ 11. Operated by the Corps, its purpose is to “provide flood control[;] assure an adequate supply of water for navigation, irrigation, stream sanitation[,] and municipal use[;] and generate and sell electrical power.” Id. ¶ 10. Directly above the dam is the Lewis and Clark Lake reservoir. Id. ¶ 13.

2 Yankton County is located in the southeast portion of South Dakota. See, e.g., South Dakota Counties, United States Census Bureau, https://www2.census.gov/geo/maps/general_ref/stco_outline/cen2k_pgsz/stco_SD.pdf (last visited Dec. 19, 2017).

-2- A. Impact of Dam Construction

A river current washes away sediment from banks and riverbeds. See Healy Aff. Ex. 3 at 13. The river itself maintains equilibrium by replacing the sediment that is washed away with sediment deposited from upstream. Id. When a dam is constructed, a reservoir forms as a result of water being held back, and the flow of water slows at it enters the reservoir. Compl. ¶¶ 13-14. The slowing water causes sediment to settle to the bottom of the reservoir, and water released from the dam is typically clear water. Id. ¶¶ 14-15.

Following construction of the Gavins Point Dam, the riverbed of the Missouri River below the dam degraded due to the lack of available sediment to “reestablish the sediment load lost above.” Id. ¶ 15. Degradation—i.e., the lowering of the riverbed—causes erosion of a river’s banks as the river seeks to maintain a natural grade. Healy Aff. Ex. 3 at 14. At the James-Missouri confluence, degradation has caused an over nine-foot drop in the elevation of the Missouri River riverbed between 1955 and 2010. Id. at 28-29. The degradation of the Missouri River due to “sediment trapping by the [Lewis and Clark Lake] reservoir formed by Gavins Point Dam” has been “well documented” since the 1980s and was “known to the [Corps] in the 1950s when the dam was being constructed.” Healy Aff. Ex. 3 at 4-5; see, e.g., Def.’s Mot. Ex. A at 9 (chart showing the decline of water surface elevation of the Missouri River at the James River confluence and other locations from 1956 to 2001). More generally, “[t]he effect of sediment trapping on downstream channels has been studied by numerous geomorphologists” over the past half-century. Healy Aff. Ex. 3 at 5; accord id. at 59-61 (containing a sample of published studies regarding riverbed degradation from as early as 1943).

The James River pushes sediment into the Missouri River to mitigate the latter’s sediment deficiency. Id. at 9-14, 18. This process is known as head cutting or channel incision. 3 Compl. ¶ 23. Head cutting takes place “when a stream or river erodes its bed and ‘incises’ vertically into the bed of the river or stream channel” as a result of “an imbalance between incoming and outgoing sediments.” Healy Aff. Ex. 3 at 4. In the instant case, the “artificially lower surface water elevation on the Missouri [River] results in a steeper gradient on the Lower James River[, which] increases flow velocities and sediment transport,” resulting in head cutting. Compl. ¶ 28.

For tributaries, their local base level can be raised or lowered by the trunk river. As the Missouri River degraded its bed, it lowered (or dropped) the local base-level for its tributaries. The drop in local base level caused an increase in the channel slope for the lower James River and this led to erosion of the James River channel in a process called headward erosion. Headward erosion starts at the mouth of a tributary and progresses upstream in the form of a knickpoint (or headcut). As the knickpoint progresses

3 Channel incision typically refers to the erosion of “smaller rivers and stream channels,” while degradation refers to the “erosion of larger rivers.” Healy Aff. Ex. 3 at 4 n.1.

-3- upstream, it lowers the bed and increases the bank heights. Steep, tall and unstable banks are characteristic of incised channels and they have been found to follow a predictable sequence of channel changes including down-cutting and bank widening. . . . [H]eadward erosion can progress many 10s or 100s of miles upstream of the initial cause of base-level drop. . . . Missouri River degradation propagated into tributary streams and rivers in the form of knickpoints (headcuts) and the degradation migrated many tens-of-miles upstream into the tributary’s drainage network.

Healy Aff. Ex. 3 at 6 (emphasis added) (citations omitted) (relying on published studies from 1983, 1986, 1989, 2007, and 2009). For example, in 1989, the Corps published a report containing a conclusion that “Missouri River degradation caused the lower James River to erode its channel.” Id. at 20.

In turn, channel incision causes channel widening:

Channel widening occurs in incised channels because the banks become overstepped and fail by mass wasting (landslides and rotational slumps). . . .

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Yankton County, South Dakota v. United States, Counsel Stack Legal Research, https://law.counselstack.com/opinion/yankton-county-south-dakota-v-united-states-uscfc-2017.