Grounds v. Louisiana Highway Commission

157 So. 385, 180 La. 670, 1934 La. LEXIS 1557
CourtSupreme Court of Louisiana
DecidedOctober 29, 1934
DocketNo. 32775.
StatusPublished
Cited by4 cases

This text of 157 So. 385 (Grounds v. Louisiana Highway Commission) is published on Counsel Stack Legal Research, covering Supreme Court of Louisiana primary law. Counsel Stack provides free access to over 12 million legal documents including statutes, case law, regulations, and constitutions.

Bluebook
Grounds v. Louisiana Highway Commission, 157 So. 385, 180 La. 670, 1934 La. LEXIS 1557 (La. 1934).

Opinion

LAND, Justice.

Plaintiff, as the owner of a plantation in Dossier parish lying just north of the ShreveportrMinden highway, known as route No. SO, has brought the present suit for damages fox-loss of his crops of alfalfa and cotton, caused by an overflow in 1930.

Plaintiff alleges that there are a number ■of bayous along this highway between Shreveport and Red Chute, across which the highway passes, and that the Louisiana highway commission, in remodeling and paving this highway in 1929 and 1930, instead 'of providing sufficient bridges across these bayous, tore out the bi-idges'which had been built by the police jury of Bossier parish, and filled in these bayous with dirt, leaving inadequate culverts to take off the water that naturally passed thi-ough these bayous, thereby causing the waters to back up and overflow his lands.

Judgment was rendered in favor of plaintiff in the sum of $3,470, and plaintiff has answei-ed the appeal and prays for an increase of the judgment to $12,000.

1. In Connolly v. Louisiana Highway Commission, 177 La. 78, 147 So. 505, it was held by this coui-t, as stated in the syllabus of that case, that the “state highway commission is liable for damages from destruction of crops on land overflowed because of inadequate culverts installed in constructing highway.”

There are then only two facts to be established in oi-der to recover:

First. Did the defendant, Louisiana highway commission, in remodeling and paving this highway along this route, fill in the natural bayous over which it passed to such an extent as to cause the water that would pass off through these bayous unimpeded to back up and overflow the lands of plaintiff ?

Second. If so, then, to what extent were plaintiff’s crops damaged? ,,

Plaintiff has filed in evidence a map showing the location of the Shreveport-Minden highway and the bayous over which it passes.

*674 The estimate of the natural water passage of these bayous and the flow left by the highway commission is as follows:

The natural water passage of Cross Bayou .............'....................... 576 sq. ft.
The natural water passage of Alligator Bayou .................................... 410 sq. ft.
The natural water passage of Little Mus-sell Shell ................................. 750 sq. ft.
The natural water passage of Bayou at “E” ...................................... 350 sq. ft.
Making a total natural overflow, leaving out the canal which was not changed, of ......................................... 2,086 sq. ft.

The openings left by the highway commission are as follows:

At Cross Bayou.............................. 50 sq. ft.
At Alligator Bayou.......................... 3 sq. ft.
At Little Mussell Shell...................... 512 sq. ft.
At Bayou "B”............................... 000 sq. ft.
Making total opening left by the Highway Commission ................................ 565 sq. ft.

The total opening of 565 square feet, deducted from the original opening of 2,086 square feet, leaves 1,521 square feet, showing a congestion ,of practically 73% of the natural outlet. In other words, the highway commission left 565 square feet of opening to take care of 2,086 square feet of natural water passage.

Eunning down through sections 12, 13, and 24, as per map filed in evidence by plaintiff, there is a heavy, line drawn by the engineer, Mr. Dutton, dividing the drainage district lying east of this line to Eed Chute and the draináge district lying west of this line to Eed river. The drainage district on the east carries off practically all the overflow water east of this line or elevation, and the drainage district on the west drains only the local lands through this territory, and requires nothing like as much drainage as it does on the east side of the separation line. There is an elevation of the territory just west of the separation line near Eobinson’s store over which the water has never been able to flow.

It is apparent, therefore, that plaintiff’s lands which are west of the separation line could not be affected by the high waters in the drainage district east of the line, unless through the back water coming out of and through Little Mussell bayou across a low place, some distance north and entering into Cross bayou at point on the map marked “F” and “6,” which would come on down through the territory just west of this elevated land.

There had never been an overflow west of Eobinson’s store for the last thirty or forty years, as far back as witnesses could testify, until 1922, when Kirby dammed up Cross bayou.

When that was blown out, there were no more overflows until the highway commission stopped up Cross bayou, Alligator bayou, and Mussell Shell in 1929 and 1930, eight years later.

Since these bayous have been stopped up, plaintiff has had three overflows in four years, 1930, Í931, and 1933.

The statements of various witnesses for defendant about the high water on both sides of the highway in 1919, 1922, 1927, and 1930 apply to the territory east of the high ground or Eobinson’s store, which was an elevated section of the country running north and south across the highway at that-.-.point.

*676 This state of facts eleárly shows that the stopping up of these bayous caused these overflows. The lower court arrived at the same conclusion, after seeing and hearing the witnesses.

2. The main defense is that the overflow was not from the waters from bayous in the east drainage district, hut was caused by overflow waters from Red river backing up and covering plaintiff's land.

The report of Mr. Crank, the local weather man, shows that on May 18, 1930, the stage of the river was 26.7 and that there were 13 feet of bank at Shreveport, when the water was at its highest stage on plaintiff’s land.

.There is a levee all the way down to Gatlin’s place, 30 miles below Shreveport. It was impossible for the water to back out of Red river ¡until it reached the end of the levee at Gatlin’s .place, which was 81 miles below plaiptiff’s .property, with a fall from plaintiff’s place .to .Gatlin’s of seven-tenths foot to the mile. Hence it would have required a perpendicular rise of 22 feet for the water to back up and overflow plaintiff’s land from Loggy bayou below Gatlin’s, and such a rise would have covered every housetop from Shreveport to Loggy bayou. We are not impressed, therefore, with the main defense urged in this case.

3. The last matter .to be considered is as to the quantum of damages to be allowed.

Plaintiff had 500 acres planted in cotton. His lands were overflowed May 23, 1930, and the water receded, about June 10th.

Plaintiff admits in-his testimony that his crop was not a total loss.

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Bluebook (online)
157 So. 385, 180 La. 670, 1934 La. LEXIS 1557, Counsel Stack Legal Research, https://law.counselstack.com/opinion/grounds-v-louisiana-highway-commission-la-1934.