Schull v. Lower Neches Valley Authority

416 S.W.2d 505, 1967 Tex. App. LEXIS 2375
CourtCourt of Appeals of Texas
DecidedJune 1, 1967
Docket6908
StatusPublished
Cited by8 cases

This text of 416 S.W.2d 505 (Schull v. Lower Neches Valley Authority) is published on Counsel Stack Legal Research, covering Court of Appeals of Texas primary law. Counsel Stack provides free access to over 12 million legal documents including statutes, case law, regulations, and constitutions.

Bluebook
Schull v. Lower Neches Valley Authority, 416 S.W.2d 505, 1967 Tex. App. LEXIS 2375 (Tex. Ct. App. 1967).

Opinion

PARKER, Associate Justice.

Summary judgment was entered that plaintiff Schull take nothing against defendant Lower Neches Valley Authority. Schull sued Lower Neches Valley Authority for |20,250.00 damages for the destruc *507 tion of barges and logs owned by plaintiff destroyed as a direct result of the Authority’s having constructed a salt water barrier dam across Pine Island Bayou, a navigable stream, causing waters to flood and destroy said personal property belonging to Schull. Schull has appealed. The parties will be designated as in the trial court.

Plaintiff contends it was error to grant defendant’s motion for summary judgment because his damage was the direct result of the intentional act of a governmental body engaged in the performance of a public work and, thus, comes directly under Art. 1, Sec. 17 of the Texas Constitution, Vernon’s Ann.St. Plaintiff next contends it was error to grant defendant’s motion for summary judgment because plaintiff’s loss was not the result of an unprecedented rainfall as that term has been defined by the courts of this state.

Lower Neches Valley Authority is a governmental agency as set out in Art. 8280, Sec. 103, Subdivision 13(c). Lower Neches Valley Authority was organized for the purposes of constructing, maintaining and operating in the valleys of the Neches River and its tributaries any and all works deemed essential to the operation of the district in the control, storing, preservation and distribution to all useful purposes of the waters of the Neches River and its tributary streams. It preserves fresh water and sells it to surrounding municipalities, industries and local farmers.

The undisputed facts of the case relating to these two arguments are stated below.

Pine Island Bayou is a tributary of the Neches River. The Bayou is 600 feet wide where it flows into the Neches. Since the deepening of the ship channel to 36 feet from Beaumont to the Gulf of Mexico over 30 years ago, salt water from the Gulf goes up the Neches and up Pine Island Bayou as far as Voth. The Bayou is subject to tide. On Pine Island Bayou some two or three miles due west of the Neches but five or six miles from the Neches following the Bayou meanders Lower Neches Valley Authority has a pumping plant. The bank there is 3½ feet above mean low tide. Downstream from, but near this pumping plant, Lower Neches Valley Authority in the early summer of 1963 constructed a salt water barrier of steel piling before Hurricane Cindy occurred. The top of this barrier was 3½ feet above mean low tide. The Bayou at that point is 160-180 feet wide. Above and below such point the Bayou is crooked and winding. Its width as places below the barrier is as little as 60 feet. Lower Neches Valley Authority constructed the salt water barrier dam of steel piling to an elevation of 31/2 feet above mean low tide of the Gulf of Mexico to prevent salt water from the Gulf flowing upstream from the dam. In August of 1963 salt water was at this point. Ordinarily, a like barrier was installed in the Bayou each year in May or June. The general area to the north and east of such barrier and plant was very low. The area to the north to Village Creek was known as the “Big Swamp”.

About five miles westward from the barrier, Highway 69 crosses Pine Island Bayou. Downstream from Highway 69 about Yz mile the Santa Fe has a bridge across the Bayou. Plaintiff’s home was located upstream from the dam about five miles, near Voth, on a knoll ISO to 175 feet from the Bayou. Near his house plaintiff had some homemade float barges built of timber and gasoline drums. The barges in the vicinity of his house were tied with ⅝" rope around a tree, with a five foot leaway on the rope. Also upstream from the dam were other barges tied with %" rope to a tree or trees, the ropes being four to five feet in length. On the bank upstream plaintiff had logs he had unloaded, pulled up against his land and secured to a tree by a chain. For several years prior to 1963 plaintiff had been engaged in the business of salvaging sunken logs out of Pine Island Bayou.

*508 Pine Island Bayou drains an area north of Liberty back towards Hull and Daisetta and over into the Sour Lake area. Its tributaries drain north and east of Sour Lake, taking in a large part of Hardin and Liberty counties. The Bayou also drains a large area of Jefferson County and the Willow Creek area out of Liberty County.

On September 17, 1963, Hurricane Cindy hit this Pine Island Bayou area. Heavy flooding ensued from torrential rains which averaged IS to 20" throughout the Sabine-Neches area with locally higher amounts in northern Orange and extreme southern Newton counties. Area streams were unable to accommodate the excessive rainfall. The area flood damages were estimated very nearly 12 million dollars. The above data in this paragraph is from the U.S. Department of Weather Bureau “Local Climatogical Data”.

Plaintiff had been in this area over 20 years. From the very beginning of this hurricane, water rose 2/ and 3" an hour. At Voth the water rose to 14.6' above mean low tide and was almost to the top of Highway 69 bridge. He testified:

“Q. And you didn’t know Cindy was going to produce that much water, did you?
A. Well, I don’t think you people did either, I will just answer that.”
“A. Well we have had several rises on the bayou since the time I have been out there and I have never seen one come and go like that storm Cindy did in there, and I have seen them come and rise and get awful high, but I have never seen them come up that quick and take everything with it.”

During the storm there was not any difference in the level of the water below the barricade as compared to above the barricade. The water at an elevation of over 3½ feet went over and around the barricade, flooding the surrounding low area.

During the storm the water was spread in all directions over the countryside.

As to the flooding, plaintiff did not know the exact hour it started but when the storm and rain hit there was a tremendous head of water coming from upstream from his home. The water rose fast all day and by late evening it reached its peak around 14 feet. Plaintiff made no attempt to retie or loosen the lines on his barges. It was too dangerous. When the water reached its height during the storm the ropes securing the barges either had to break or the barges had to sink. Plaintiff testified that the ropes were either broken or gone after the storm. He didn’t know whether they broke loose after the water reached an elevation of 12 or 14 feet or before. The logs chained to a tree were gone after the storm. Plaintiff didn’t know whether the chain broke or what happened, as he never did find the chain. He testified:

“You can put it the chain come loose if you want to. The chain might have come loose, I don’t know, but the wall of water coming down the bayou at the rate it come will move anything.”
“Q. Do you know when this timber broke loose?
A. No, sir, I don’t. It broke loose during the storm. After the water receded it wasn’t there.
Q.

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Bluebook (online)
416 S.W.2d 505, 1967 Tex. App. LEXIS 2375, Counsel Stack Legal Research, https://law.counselstack.com/opinion/schull-v-lower-neches-valley-authority-texapp-1967.