Topping v. Great Northern Railway Co.

142 P. 425, 81 Wash. 166, 1914 Wash. LEXIS 1364
Washington Supreme Court·Decided August 11, 1914·No. No. 11949·Published·Cited by 14 cases

Opinion

Mount, J.

This action was brought by the plaintiif through his guardian ad litem to recover damages on account of the death of his father. The father, Edward W. Topping, was a young man thirty years of age. He was killed while a passenger on one of the trains of the Great Northern Railway Company which was wrecked by an avalanche at Wellington, in this state, on March 1, 1910.

The cause of action was based upon the following paragraph of the amended complaint:

“That on to wit the 1st day of March 1910, Edward W. Topping was a passenger for hire on one of defendant’s trains, between the cities of Spokane, Washington, and Seattle, Washington, and en route to the latter and while such passenger, said train was, on said last named date, through the negligence and carelessness of defendant, derailed and wrecked at or near the station called Wellington, on said road, the exact nature and extent of said acts of negligence on the part of defendant not being fully known to plaintiif, but well known and understood by defendant, and the said' Edward W. Topping was then and there killed in and by said wreck and derailment of said train.”

The answer of the defendant was a general denial and an affirmative defense of vis major, or act of God. The [168] cause was tried to the court with a jury. At the close of the plaintiff’s evidence, a motion for nonsuit was denied. At the close of all the evidence, a motion for a directed verdict was also denied. After the cause was submitted to the jury, a verdict was returned in favor of the plaintiff for $20,000. This appeal followed.

Numerous errors are assigned. But we are satisfied that the motion for nonsuit and motion for a directed verdict should have been sustained by the trial court, and for that reason we shall notice only these assignments.

The following facts are practically undisputed: Edward W. Topping took passage from Spokane on the defendant’s train bound for Seattle, on the evening of February 22, 1910. This train was a regular passenger train running from Spokane to Seattle across the Cascade mountains. The distance between Seattle and Spokane is about 375 miles. The running time was about 12 hours. This train did not carry a dining car, but carried sleeping cars. It is conceded that Mr. Topping was a passenger for hire on this train. At the time the train left Spokane, there was known to be a storm in the Cascade mountains which had been raging for a period of one or two days. But at that time trains were running regularly on about schedule time. This train was No. 25, and will hereafter be referred to by that number.

In the Cascade mountains, is a tunnel about three miles long through the summit. The station'at the east portal is known as the “Cascade tunnel.” The station at the western end of this tunnel is known as Wellington, at which place there is a hotel and a few other buildings located on the mountain-side near the railway. Train, No. 25 reached Cascade tunnel at the eastern end of the tunnel at about 5:30 in the morning of February 23d. At that time the storm had not abated in the mountains and the line at points between Wellington and Seattle was blocked with snow. Train No. 25 remained at Cascade tunnel until the evening of Feb[169] ruary 24th, when it was taken through the tunnel and placed on a passing track at Wellington, where it remained until February 28th, or the morning of March 1st at about 1:30 o’clock, when an avalanche of snow swept down the mountainside and carried this train with it a distance of about 100 feet below the track, where the train was destroyed. Edward W. Topping and other passengers were killed. Others were injured.

When train No. 25 arrived at Cascade tunnel on the morning of February 23d, there was a heavy snowstorm. Snow had been falling about 24 hours. It had been falling at the rate of about three feet per day. Some of the witnesses testified that, when the train went through the tunnel to Wellington, the snow there was between eight and nine feet deep. It was not shown or claimed that this was all fresh snow. A part thereof had accumulated during the winter.

The railroad track at Wellington was built upon the mountainside. The railway tracks at this place consisted of a main line, two or three switches, and what is known as a “passing track.” The passing track connected with the main line at each end. During the time train No. 25 stood upon this passing track, the railroad between Wellington and Seattle was blocked with snow and slides, so that trains could not run through. The track was also blocked with snow and slides from the Cascade tunnel east toward Spokane. From the time train No. 25 was placed on the passing track at Wellington on the 24th of February until the 1st of March, every effort was being made by the railroad company to open the track so that trains could be run through. On the night of the 28th, or the morning of March 1st, an avalanche of snow broke upon the hillside to the north of the train, and slid down, carrying the train with it. This avalanche broke off four or five hundred feet above the track, and extended from 1,500 feet to 2,000 feet along the track. At that time, there was an unusual storm raging: wind, thunder, lightning, and excessive snow. It was an unprecedented storm. The [170] avalanche came without warning and swept the train down the hillside.

Part of the time while the train was at Wellington it stood in the mouth of the tunnel, which is hut a short distance awáy. It was then moved down a little west of the town of Wellington, where it was when finally swept away. To the west of Wellington, there were snowsheds. A little further on was what was testified to hy some of the witnesses as a flat place. The hillside above the train extended up at an angle of about 30 degrees. The snow upon the hillside at the time of the disaster was from nine to twelve feet deep. The railroad had been operated in this place for a period of seventeen years. The storm was an unprecedented one, both in length of duration and in its violence. Snow slides had been known to occur along the mountain-sides during the winter seasons during heavy storms. These slides usually occurred in gulleys. A slide had never been known to occur at the place where the train was standing on the siding. A little west of this, some five or six hundred feet, a slide had occurred some years previous, but at a point where there was a gully.

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Topping v. Great Northern Railway Co., 142 P. 425, 81 Wash. 166, 1914 Wash. LEXIS 1364 (Wash. 1914).

142 P. 425 (Topping v. Great Northern Railway Co.) — published by Counsel Stack Legal Research, free access to 12M+ legal documents.

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