McDonald v. New York Central Mutual Fire Insurance Co.

380 S.W.2d 545
CourtTexas Supreme Court
DecidedJune 10, 1964
DocketA-10025
StatusPublished
Cited by63 cases

This text of 380 S.W.2d 545 (McDonald v. New York Central Mutual Fire Insurance Co.) is published on Counsel Stack Legal Research, covering Texas Supreme Court primary law. Counsel Stack provides free access to over 12 million legal documents including statutes, case law, regulations, and constitutions.

Bluebook
McDonald v. New York Central Mutual Fire Insurance Co., 380 S.W.2d 545 (Tex. 1964).

Opinion

CULVER, Justice.

Petitioner, McDonald, brought this action against New York Central Mutual Fire Insurance Company to recover for the destruction of his house located in Matagorda County under the terms of a policy of insurance issued by that company. The policy covered loss caused by wind and hurricane but excluded loss caused by tidal wave, high water or overflow, whether driven by wind or not.

*546 The jury found that the winds of the •hurricane directly and proximately caused the loss and damage; that the loss was not caused by tidal wave, high water or overflow whether driven by wind or not and that the loss did not result from the combined action of the wind, tidal wave, high water or overflow. Based on this verdict the trial court entered a judgment in favor of McDonald and against the Insurance Company. The Court of Civil Appeals reversed and rendered judgment that McDonald take nothing, holding that the jury’s findings failed to be supported by the evidence. 374 S.W.2d 767. From a review of the record we reach a conclusion to the contrary.

Admittedly the house was totally destroyed at some time during the passage of Hurricane Carla through this area in September of 1961. It was one of the most destructive storms that has visited the Texas Coast so far as property loss is concerned. Mr. McDonald left his house on Saturday morning, • September 9th, and when he returned on Wednesday, the 13th, the house was gone. The evidence bearing on the loss is circumstantial. The only testimony was given by Mr. and Mrs. Jensen who lived nearby and rode out the storm in a concrete building. The remainder of the evidence consisted of maps and official records and reports.

McDonald’s house was located on Turtle Bay about 6 feet above water level at mean low tide and was supported on pilings approximately 4 feet above the ground. Turtle Bay, so-called, is a rather long, narrow inlet generally about a mile in width extending in a northeasterly direction from Tres Palacios Bay, a much larger body of water. Palacios Bay in turn forms a small and the upper part of Matagorda Bay, which is some IS miles in width. Between Turtle Bay and Tres Palacios Bay there extends- a long narrow peninsula almost the entire length of Turtle Bay. Mr. Jensen lived and grazed cattle on the land formerly the site of Camp Hulon west of the town of Palacios. McDonald’s house was located on the west side of Turtle Bay directly across from Camp Hulon.

On Sunday, September 10th, Jensen and his wife made several trips down this peninsula to move his cattle back from the water’s edge where they had drifted or were blown by the wind. On the morning of that day he went to the end of the long peninsula and found that the water level was 18 inches to two feet over mean low tide. At that time he could not see across the bay on account of the rain. In the afternoon he made two similar trips for the same purpose and found the conditions the same as they existed at the time of the first trip. In his opinion the wind was blowing from the northeast at the rate of 100 miles per hour. On the morning of the following day, Monday, September 11th, he drove his car out on the peninsula but could get no further than the narrowest part of the peninsula which was about a mile from the tip end. The elevation at that point is about the same as that across Turtle Bay where the insured property was located. At that time Jensen still could not see across the bay. According to him the wind velocity had increased to about ISO miles per hour. Between 3:00 and 4:00 o’clock that same afternoon he made another trip out on the peninsula. At that time the lull came and lasted for about 15 minutes. The rain ceased and he could see across Turtle Bay. McDonald’s house was gone and all he saw were the high line poles along where the house had stood. After the lull the water began to rise rapidly and he and his wife hurried back to the safety of the concrete refrigeration building. Mrs. Jensen accompanied her husband on his last trip on Monday and also looked across the bay approximately a half mile to the location of the house and saw nothing standing but the poles.

Introduced in evidence were various official reports, charts and maps from the United States Weather Bureau and the United States Corps of Engineers. It seems to be undisputed that at all times before the eye or center of the storm reached *547 the Palacios area the wind was blowing from a northeasterly direction. After the eye passed inland, due to the counterclockwise motion of these hurricanes, the wind was reversed and in the Palacios area blew in the opposite direction. The data introduced in evidence showed that the leading edge of the eye reached Port Lavaca, some 20 miles southwest of the Palacios area between 3 and 4 p. m. Monday, the 11th. In advance of the eye many stations along the Coast that morning reported the highest recorded wind velocity. A peak gust of 170 miles per hour was estimated at Port Lavaca. Gusts of ISO miles per hour were estimated at other nearby points. Sustained winds were reported at more than 115 miles per hour at Matagorda, which is about IS miles east of Palacios.

The Insurance Company counters with a report from the Palacios Federal Aeronautics Authority station, which recorded that the wind was from the north and northeast on the 10th and that the highest wind observed on that day was up to 48 miles per hour. But the last observation was made at S :58 p. m. on that day and the station was abandoned shortly thereafter. The report did show that from the beginning of that day the wind was more or less steadily increasing in velocity.

So far as the high tides and wind-driven water are concerned the Weather Bureau at Galveston gives a report on the peak flooding at various points along the Texas Coast. The information was collected from all available sources but mostly was obtained from the Army Corps of Engineers. According to this report the peak tide at Port Lavaca was 16.6 feet above mean sea level. Of course to determine the depth of the water above ground at any point the ground elevation must be subtracted. At Port O’Connor the peak was 14}4 and at Palacios 15.4. However, at these points the height of the tide was ascertained from an observation of the high-water mark. The report does not profess to determine when the peak was reached. Unquestionably, all of this area was flooded by hurricane-driven water, but we may reasonably infer from the evidence before us that the flooding of this area took place in the second phase of the hurricane after the center had reached the area and after the ensuing lull. Up until that time the wind was blowing from the northeast and was calculated to blow water from Turtle Bay toward the southwest and away from McDonald’s house. There were no bodies of water northeast. The Insurance Company lays much stress on the statement made by Jensen that on the occasion of his last visit down the peninsula to round up his cattle early in the afternoon on Monday and before the lull, he watched big waves in the bay “easily IS to 20 feet high”. Certainly he was not talking about any waves in the narrow Turtle Bay, but out into Tres Palacios and Matagorda Bays, Had those waves been sweeping toward the peninsula and toward the property in question, it would seem that Jensen and his wife and automobile would have been swept away.

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Bluebook (online)
380 S.W.2d 545, Counsel Stack Legal Research, https://law.counselstack.com/opinion/mcdonald-v-new-york-central-mutual-fire-insurance-co-tex-1964.