Jackson v. United States

230 U.S. 1, 33 S. Ct. 1011, 57 L. Ed. 1363, 1913 U.S. LEXIS 2674
Supreme Court of the United States·Decided June 16, 1913·No. 720·Published·Cited by 80 cases

Opinion

Mr. Chief Justice White

delivered the opinion of the court.

This suit was brought to recover from the United States the value of property asserted to have been totally destroyed or rendered completely valueless as the result of *3 certain public work "done in pursuance of the acts of Congress' authorizing it, for the public benefit,' under the. direction- of the Mississippi River Commission and the Secretary of War and the United.States engineers.” And it was charged that under the circumstances stated and the facts alleged, the property had' been taken by the. United- States for public'use “within the meaning of-the constitutional provision,” and it .was averred' that there was consequently imposed "on-the United States an implied obligation to make compensation for the property so taken and destroyed.”

It becomes necessary to give a brief description of the topography of the country in which the property in question is situáted, in order to make clear its relation to the public work which it is asserted constituted a taking within the meaning of the Constitution. -

The.Valley of the Mississippi River, may. in a broad sense be said to commence at Cape Girardeau, Missouri, and to extend from there to''the mouth of the river, at the Gulf of Mexico. The river, however, in its course to the ocean does not run through the center of the vast fertile and allüvial plains which in a comprehensive and generic sense constitute the delta of-the Alississippi. On the contrary the situation of the riyer in this respect varies, occasioned by the fact that at divers places the upland or Mil ■country approaches to or constitutes the bank of the river. The difference in this regard is marked between the west and the east banks. The west bank is divided into four great basins — the St. Frances Basin, which ^extends from Cape Girardeau to Helena; the White River Basin, winch extends from Helena to the mouth of the Arkansas; the Ténsas Basin, wMch extends from the mouth of the Arkansas to the mouth of the Red River; and the Atchafalaya Basin, extending from the mouth of the Red River, to the Gulf. Practically'in the long sweep from Helena, where St. Francis Basin ends and the WMte -River .Basin *4 begins, to the ending of the Atchafalaya Basin at the Gulf there is no real topographical distinction between the basins, the west bank of the river in that great distance consisting of alluvial country having generally a very wide. though varying’ expanse. The division into basins putting out of view the St. Francis Basin, is therefore merely the result of a consideration of the watershed of each basin, all the water-, however, from each ultimately finding its way to the -Gulf of Mexico, either through the Mississippi-River, or in the.lower basins in part at least by the means of streams flowing independently of the Mississippi River .to the Gulf of Mexico. On the east bank the situation is different. In the long stretch from Cairo, Illinois, to a point a short distance below Memphis, generally speaking, the hills and uplands border the river and constitute its bank. From the point below Memphis to which we have referred’ to Vicksburg, Mississippi, this is not the case, and there is a great basin known as the Yazoo Basin, which, aside from peculiarities of its own, may be said to possess the samé general characteristics as the basins on the west bank of the river. From Vicksburg’ where the uplands come to the river and constitute its bank, down to Baton Rouge,-Louisiana, where the hills or uplands permanently recede from the river a different condition from that which exists on the west bank obtains. As we are concerned only with the situation below Natchez we put out of -view any statement concerning the east bank between Vicksburg and Natchez, and refer only to the con-' ditions ’ existing on the east.bank between Natchez and Baton Rouge.

From Natchez where the hills or uplands constitute the bank of the river to Baton Rouge, the line of hill or upland does not follow the course of the river, but recedes therefrom for a certain distance and then ¿gain abuts, on the river, -this process being repeated from point to point until Baton Rouge is reached; Of necessity therefore be-.. *5 tween the point of each departure of the uplands from the river to the point of reapproach there is an area of alluvial country bounded on the west by the river and constituting its bank, on the east by the hills, which as it were like a festoon or semicircle inclose the alluvial area between the river, the base of the uplands or hills, and the points of departure from and approach to the river as above stated.

These various areas constitute in the nature of things, minor basins having their own watershed. And between Natchez and Baton Rouge there are five of these minor basins, one between Natchez and Ellis .Cliffs, sixteen miles below Natchez, another between Ellis Cliffs and Fort Adams, thirty-nine miles below Ellis Cliffs, a third between Fort Adams and Tunica, seventeen miles below Fort Adams, and two othérs between Tunica and Bayou Sara, twenty-three miles below Tunica, and from Bayou Sara to Baton Rouge, a distance of thirty-five miles. These subordinate basins are included in a, general local ievee district known as the Homoehitto district. A dull and accurate statement concerning these basins, of their relation to levee building, and overflow, will be found in Document No.-1010, House of Representatives, 63rd Congress, third session, being a'ietter of- the Secretary of War trans-. mitting to the House of Representatives a full report of a survey made'by direction of Congress, by the Mississippi River Commission, of these basins. Of the hasin between Ellis Cliffs, and Fort Adams, the report of the Commission makes the following statement:

“Between Ellis Cliffs and Fort Adams, a distance of 39 miles by river, lies a basin whose protection from floods is greatly complicated by the presence of lakes, streams, and swamps. .
/‘It has a .total ’area of 59,412 acres, including 9,781 ■acres of cleared and 49,631 acres of wooded land, the assessed value of which is $204,739.'
“The systematic protection- of the basin as a whole is *6 impracticable without including drainage work of large proportions.
“It will be observed that there is a large amount of cleared land- which is now beiñg cultivated although meag'erly protected from floods by small private levees.'
“Owing-to the extent of swamp lands the cultivated area could not be greatly extended by thé construction of a levee along the river front.
“The benefits to be derived from the construction of a levée are relatively small as compared with the cost, and the work cannot be recommended.”

In February, 1894, the appellants or their predecessors in title for whom they have been' substituted on the record, filed their petition in the Court of Claims against the United States, alleging themselves to be the owners of various tracts of land in Adams County, Mississippi, composing three plantations. It was alleged as follows:

“2.

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Jackson v. United States, 230 U.S. 1, 33 S. Ct. 1011, 57 L. Ed. 1363, 1913 U.S. LEXIS 2674 (1913).

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