Anderson v. Connecticut Fire Insurance Co.

231 Minn. 469
CourtSupreme Court of Minnesota
DecidedJuly 7, 1950
Docket35,094, 35,095, 35,096, 35,097
StatusPublished
Cited by36 cases

This text of 231 Minn. 469 (Anderson v. Connecticut Fire Insurance Co.) is published on Counsel Stack Legal Research, covering Supreme Court of Minnesota primary law. Counsel Stack provides free access to over 12 million legal documents including statutes, case law, regulations, and constitutions.

Bluebook
Anderson v. Connecticut Fire Insurance Co., 231 Minn. 469 (Mich. 1950).

Opinion

Matson, Justice.

Appeal from orders denying defendants’ alternative motions for judgment notwithstanding the verdict or a new trial.

Defendant insurers, four in number, each issued to plaintiff an insurance policy for $12,000 insuring him against all loss or damage to his building from “windstorms, cyclones, and/or tornadoes,” subject, however, to the proviso that the insurer “shall not be liable for any loss or damage caused by snowstorm, blizzard, frost or cold weather; * * The insured building, known as the Bar Harbor dance hall and tavern, is a one-story structure located in Cass county on Gull Lake. It is built in the shape of a T with the main part of the structure corresponding to the top of the T located on land, and with the leg of the T supported by 160 pilings, extending in a northerly direction from the lake shore out over the waters of a channel. The top of the T is 90 feet long and 50 feet wide and extends east and west, whereas the leg of the T is 90 feet long and 50 feet wide with a full-length porch 10 feet wide on each side. A gable roof covered the leg structure with one side sloping to the east and the other to the west. This roof was joined at right angles to a similar roof on the top part of the T which sloped respectively *472 north and south. Braced and timbered heavily as an integral part of the framework and roof of the leg structure, at its extreme northerly end, was a cupola or tower about 8 or 10 feet higher than the ridge of the roof, and from this tower a flagpole, anchored to an inside beam, projected upward another 8 feet. To the north the building was sheltered by a high bank on the opposite side of the channel, but to the east it was exposed to an expanse of open water for a distance of about four miles.

The primary issue is whether the building was damaged by a windstorm within the coverage of the policy or by a blizzard within the meaning of the exclusionary clause. The facts, as the jury could reasonably find them from the confiieting evidence, are that on Friday forenoon, February 27, 1948, a storm of considerable intensity commenced and did not abate until the following Sunday. A strong wind blew from the east and was variously estimated by witnesses as a “terrible gale,” as the strongest east wind in “11 years,” as “blowing terribly strong, because it almost took me off my feet,” as “so terrific you could hardly stay on the highway,” and that it was a “40 or 45 mile wind.” Snow from 21 to 24.5 inches fell on Friday and Saturday. The visibility was poor. A tree broke off at its base and fell across a telephone line. As early as Friday, between 4 and 5 p. m., the flagpole and tower on plaintiff’s building were observed leaning to the west. Shortly after noon on Saturday, the tower and the end of the building were plainly seen to lean as much as four or five feet to the west. Sunday noon, on the east half of the leg roof, “there was very little snow, only a few little spots where there would be a few inches, and you could see the shingles mostly all over.” On Tuesday it was first discovered that the leg of the T-shaped building had collapsed by tipping from the east toward the west so that the west wall was lying beneath the roof and the peak or ridgepole of the roof was 8 or 10 feet to the west of the true center line of the building. In other words, both side walls tipped to the west or in the same direction as the wind was blowing. Anchoring nails and bolts were also pulled or bent toward the west. In its collapsed condition, *473 the east half of the roof was found to he covered with very little snow, but the west half had a layer of 10 or 12 inches. The main part of the building, or the top of the T, was found to have twice as much snow on its roof, but it did not collapse, although, as a weight-supporting structure, it was weaker than the leg of the T.

Was the damage to the building caused by a windstorm, as plaintiff contends — and as the jury must have found — or was it caused by a blizzard or snowstorm, as alleged by defendants? The question was submitted to the jury with instructions which did little more than define windstorm, snowstorm, and blizzard in terms of causation. Windstorm was defined as a storm wherein the wind, and not snow or rain, is the efficient and proximate cause of the damage. A snowstorm was defined as a storm wherein snow is the efficient and predominant cause, and a blizzard as a storm whebein the efficient and proximate cause of damage is not wind, but snow, rain, frost, or cold weather or a combination thereof.

Was all question of fact precluded by the plain language of the policies? Is a high wind a windstorm only so long as it is unaccompanied by snow? When does it become a blizzard? Weather disturbances are frequently and popularly described by more than one term. Although the language of the parties to an insurance policy must be given its natural and ordinary meaning, and the words used are to be taken in their popular sense, such language and words as expressive of intent cannot be wholly disassociated from the purpose for and subject to which they are applied. The idea content of a word is frequently conditioned and modified by the subject to which it is applied (Maze v. Equitable L. Ins. Co. 188 Minn. 139, 246 N. W. 737), as well as by the geographical area or environment in which the word is used. In the present case, the parties were contracting for insurance against the hazard of windstorm in a northern area, where, with rare exceptions, it would be difficult during half of the calendar year to have a windstorm without an accompaniment of flying snow. Naturally, where seasonal snows fall, questions of fact will arise as to whether a winter storm is primarily a windstorm or a blizzard, and the answer is not to be *474 found in any arbitrary rule of law. Under such circumstances, are we to overlook the obvious purpose of the contracting parties by adopting a strict interpretation and thereby ascribe to them the absurd intent of contracting for the payment of a year-round premium to cover a risk that is practically inoperative half the year? To hold that the parties did not contract with reference to the falling of snow in midwinter is to ignore realities. See, Mork v. Eureka-Security F. & M. Ins. Co. 230 Minn. 382, 42 N. W. (2d) 33. No doubt the parties could so agree, but where the words as related to the subject matter do not compel so narrow an interpretation, it should be avoided. See, Maze v. Equitable L. Ins. Co. supra. Where, as here, the language is not so explicit as to be free from ambiguity, insurance policy provisions are to be liberally construed in favor of the insured. Cavallero v. Travelers Ins. Co. 197 Minn. 417, 267 N. W. 370.

The Texas court, in Fireman’s Ins. Co. v. Weatherman (Tex. Civ. App.) 193 S. W. (2d) 247, 248, recognized that a windstorm varies in its characteristics from one area to another when it said:

“* * * An East Texas windstorm would probably be accompanied by heavy precipitation, while a West Texas windstorm would probably be dry, but might be accompanied by so much dust as to limit visibility.”

In the instant case, the windstorm, which is not unusual for Minnesota, was accompanied by heavy precipitation in the form of snow and the visibility was limited.

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Bluebook (online)
231 Minn. 469, Counsel Stack Legal Research, https://law.counselstack.com/opinion/anderson-v-connecticut-fire-insurance-co-minn-1950.