Wells v. Town of Remington

95 N.W. 1094, 118 Wis. 573, 1904 Wisc. LEXIS 1
CourtWisconsin Supreme Court
DecidedJuly 3, 1904
StatusPublished
Cited by6 cases

This text of 95 N.W. 1094 (Wells v. Town of Remington) is published on Counsel Stack Legal Research, covering Wisconsin Supreme Court primary law. Counsel Stack provides free access to over 12 million legal documents including statutes, case law, regulations, and constitutions.

Bluebook
Wells v. Town of Remington, 95 N.W. 1094, 118 Wis. 573, 1904 Wisc. LEXIS 1 (Wis. 1904).

Opinion

Cassoday, C. J.

The trial court directed a verdict in favor of the defendant on the sole ground that there was no evidence tending to prove that the alleged defect was within the public highway. To determine the correctness of this ruling, it is important to know the character of the defect and its location in respect to what was then the traveled portion of the highway, or the portion of the highway which was in a condition to invite travel, under the circumstances. It is undisputed that at the place in question the highway ran in a northerly and southerly direction, and was four or five rods wide, and fenced on both sides. It was crossed by Two-Mile creek, which was from two to four feet wide, and entered the highway from the east, flowing thence southerly, thence westerly, thence northwesterly, and thence in a westerly direction, in the form of a curve, to and through an embankment or dike leading across the valley. The creek valley was sandy, with much surface, flat, and from six to ten rods wide from north to south, and from five to six feet lower than the general level outside of it. Tor many years immediately before the time in question, the highway across the valley ran on the embankment or dike mentioned, the top of which was some five or six feet higher than the bottom of the valley. This dike was from fourteen to twenty feet wide at the top, and from twenty to twenty-four feet wide at the bottom, and as it came from the south, curved to the west until it reached the limit of the highway, and at that point there was a bridge sixteen feet wide and from sixteen to eighteen feet long, cross[576]*576ing the creejk, and from thence the dike ran directly north.. As stated by the trial court, the dike “was reasonably safe for travel prior to the 28th or 29th of June, 1897, when an unusual flood carried off the bridge and covered the entire lowlands between the extreme banks described — some six to ten or twelve rods in width — with water to a depth of some three feet in most or all of that part of the highway.” As early as, or eaxdier than, July 1, 1897, the flood carried away the bridge, leaving a break in the embankment of about forty-feet, and so made or created a hole in the ground over which, the bridge had been — extending eastward of the embankment some twenty feet, and being from ten to twelve feet or more-in depth, and nine feet deep at its most easterly edge, on July 7, 1897. There was no more rain after June 30, 1897,. and the water subsided rapidly. On the evening of the day on which the bridge went out, a fence was placed clear across-the highway, on both sides of the creek, to prevent travel. The next day such fences were removed, except across the-embankment, and the highway was thus open to travel, and from that time on teams passed north and south in large numbers, especially on the 4th day of July.

There is evidence tending to prove that the road commissioner for the previous year was at the locus in quo a day or two after- the bridge went out, and after the water had gone down a depth of three feet on the general level, and with a pole sixteen to twenty feet in length probed the hole from the south end of the dike, at the break therein, and found it to be from thirteen to fourteen feet in depth; that teams were crossing at the time, and he reported these conditions to the town board; that he was there again on the morning of' July 7, 1897, the day of the accident, and probed the hole-again, hut at no time sought to find how far the hole extended toward the east; that the valley had water over its surface until July 5, 1897, when there appeared a tongue or narrow strip of land, extending from the north bank of the valley to> [577]*577the creek at tbe south, and right up to the large'hole; that July 6, 1897, this dry strip was continuous from the north, except a little dead water near the north side of the valley; that on that same day some poles were placed across the creek, at a point where their north ends were about twelve feet southeast of the big hole; that on that day teams were crossing on such dry strip of land, going on the west side of'the poles mentioned; that the dry strip had been covered with grass, but was mostly washed over with sand by the flood; that July 7, 1897, this dry strip of land, opposite the big hole, was about nine feet wide, and came right up close to the big hole (this did not include the dip in the overhanging sod,' which had been undermined and had been covered by water, the body of the hole really extending under the edge of the dry strip) ; that directly east from the big hole, and nine or ten feet from it, was a mire hole, where several travelers had trouble; that there were wheel tracks- — wagon tracks — along the dry strip of land for some time before the accident. It appears and is undisputed that previous to the flood, and while the bridge was in place across the creek, there had been for a long time a passageway or fording place, called the “main ford,” which was used regularly by a large portion of the traveling public. That ford left the embankment several feet south of the south bend of the creek, and then went first in a northeasterly direction, and then curved toward the north, and crossed the creek at its southern bend, and then went in a northerly direction, and finally curved toward the west and entered the regular highway over the embankment. After the bridge went out and the fences which prevented travel were removed, the public resumed travel on the main ford, which, on the day of the accident, was covered with water for about three rods immediately north of the creek.

The plaintiff’s intestate was a little more than seventeen years- of age at the time of his death. He resided with his parents, eight and one-half miles northerly from the place of [578]*578the accident. On the morning of July 7, 1897, be left bis borne in good health, with a two-wheeled cart drawn by a borse or pony, destined to Mr. Winter’s place, about one mile south of the place in question. There is evidence tending to prove that, in going south, he drove on the dry strip of land described, and that on bis way home be started to drive over that same dry strip of land, between the poles mentioned and the deep hole. There is evidence tending to prove that a short time after one o’clock in the afternoon of July 7, 1897, a little boy discovered a boy’s bat floating on the surface of the water in the big bole, and a horse’s foot sticking up out of the water; that be gave the alarm, and the peojile in the vicinity came and found the borse or pony right on his back in the deep bole, and the cart bottom side up in the water, and tire boy right under the cart, and the umbrella, under the boy and farthest down; that the borse was still connected with the cart — the tugs bitched, and the pony checked up; that there was a short mark over the boy’s left eye and temple, and a black spot on the left side of bis neck, bis pants were torn in two or three places, two lifts were off the left shoe heel, two slats of the floor of the cart and one thill were cracked or broken, and bis bat was floating on the east edge of the bole— sis or seven feet from the foot of the borse and about the same distance from the shore.

Such is a general outline of the evidence upon which the court directed a verdict in favor of the defendant.

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Cite This Page — Counsel Stack

Bluebook (online)
95 N.W. 1094, 118 Wis. 573, 1904 Wisc. LEXIS 1, Counsel Stack Legal Research, https://law.counselstack.com/opinion/wells-v-town-of-remington-wis-1904.