Womar v. City of Long Beach

114 P.2d 704, 45 Cal. App. 2d 643, 1941 Cal. App. LEXIS 1523
CourtCalifornia Court of Appeal
DecidedJune 30, 1941
DocketCiv. 12500
StatusPublished
Cited by4 cases

This text of 114 P.2d 704 (Womar v. City of Long Beach) is published on Counsel Stack Legal Research, covering California Court of Appeal primary law. Counsel Stack provides free access to over 12 million legal documents including statutes, case law, regulations, and constitutions.

Bluebook
Womar v. City of Long Beach, 114 P.2d 704, 45 Cal. App. 2d 643, 1941 Cal. App. LEXIS 1523 (Cal. Ct. App. 1941).

Opinion

*645 DORAN, J.

The appellant city appeals from a judgment herein whereby appellant, as defendant, “is perpetually enjoined from causing or permitting the surface waters on Atlantic Avenue or Hill Street, or the intersection of said streets, in the City of .Long Beach, State o£ California, resulting from rainfall, usual in nature and not extraordinary or unprecedented, to flow upon plaintiff's real property at the southwest corner of said intersection of said streets, or to flow, collect or concentrate upon said streets, or said intersection, in such quantities as to interfere with the ready ingress to and egress from plaintiff’s said real property”, and whereby certain damages were assessed against appellant for injury to property caused by the flooding of the said real property. Plaintiff has also appealed from that portion of the judgment which limits relief only from the effects of usual rainfall, contending that the decree should have provided for relief from all rainfall of whatever nature. The plaintiff died prior to the hearing on the appeals herein and his executrix, Myrtle D. Womar, has been substituted as party plaintiff in the place and stead of J. S. LePage. However, to avoid confusion, and for convenience, the terms “plaintiff”, “respondent” or “appellant” will be applied as though such a substitution had not been made, and will be understood hereinafter to refer to the original plaintiff in this action, as appellant or respondent, as the case may be.

At the time of the commencement of this action respondent plaintiff was the owner of a lot located at the southwest corner of the intersection of Atlantic Avenue and Hill Street in the city of Long Beach, the lot' being improved with a one-story brick building containing two store rooms, one occupied as a drug store and the other as a restaurant. Respondent brought the instant action against the appellant city, alleging that the appellant, by the grading of Hill Street and Atlantic Avenue at and near their intersection, and by the grading of other streets in the general locality, caused surface run-off water to be diverted to and accumulate upon Atlantic Avenue and Hill Street and to overflow into the respondent’s building, thus causing damage to respondent's building and to the personal property of respondent’s tenants (who assigned their claims herein to respondent). The prayer was for the abatement of the nuisance thus allegedly created and for damages.

*646 The trial court found that the appellant city had created a nuisance at and near the said intersection and gave judgment for the plaintiff as above stated.

. For the purposes of consideration upon this appeal by the city, the intersection of the streets in question lies somewhere near the center of an area in the City of Long Beach bounded by State Street on the south, the right of way of the Pacific Electric Railway on the north, California Avenue on the east and American Avenue on the west. Atlantic Avenue runs north and south, Hill Street east and west. Elevation charts, contour map and relief map introduced in evidence reveal the area to be generally low land.

Running from State Street on the south to Burnett Street on the north, two blocks north of Hill Street, the elevation along Atlantic Avenue drops approximately seven feet. The general drop in elevation along Atlantic Avenue from State Street north to Hill Street is about five feet. Along Hill Street, running west into Atlantic Avenue, covering a distance of several blocks, the elevation drops roughly about one foot; and running east along Hill Street to its intersection with Atlantic Avenue, covering about the same distance, the elevation drops about three feet. The elevations mentioned, according to the maps in evidence, are “derived from property line grades based on Old Long Beach Datum Plane”. Within the area bounded as above the land slopes generally to the northwest, with the exception of the extreme lower southeast section, where the slope is to the southeast. Atlantic Avenue, from State to Hill Street, appears to mark a low point on streets crossing it from east to west. In other words, the land directly east and west of Atlantic Avenue, over the territory mentioned, slopes toward Atlantic Avenue. At the intersection of Atlantic Avenue and Hill Street the general elevation is about 20 feet, and this general elevation prevails to 23rd Street, one block north of the said intersection, where there is a drop to 19 feet. The elevation at the southwest corner of Hill Street and Atlantic Avenue, the location of plaintiff’s property, is given as being from 20.2 to 20.6.

In January 1907 the grades on Atlantic Avenue north of Anaheim Street were established by a resolution of the Board of Trustees of the City of Long Beach, which resolution established the grade at the southwest corner of Atlantic Avenue and Hill Street at 19.2 feet. In July 1913 the *647 grades on Hill Street in the area above described were established by ordinance of the city, whereby the grade of Hill Street at the west line of Atlantic Avenue was established at 19.1 and at the east line thereof at 19.2 feet. It is not disputed that both streets were graded to the grade so established.

The maps in evidence indicate a fairly large natural depression existing in the block at the southeast corner of Hill and Atlantic in a state of nature. The elevation in this depression is shown as 19 feet. The existence of such a depression was borne out by the testimony of witnesses for both sides. It appears that water collected there when it rained and that upon occasions there was a considerable body of water at that point. At the time the property was subdivided there was a “pond” there, and the depression was thereafter filled in. Witnesses for both sides gave evidence that the intersection in question had been flooded during rains before as well as after the grading of the streets; and it appears from the testimony that the entire area had always been more or less subject to flooding during heavy rains. At least one witness, an old inhabitant, testified to having seen the southwest corner of Hill and Atlantic “under mud and water” prior to the time the streets were graded. His testimony, together with that of the other witnesses for both sides clearly established the existence of a serious drainage problem in the area, a problem created by the natural topography of the land coupled with conditions of rainfall peculiar to a semi-arid region like that of Southern California.

The trial court found that the surface of the lands embraced within the general area under consideration, south of Hill Street, “had a gradual slope and fall to the east into a large natural sump or basin east of said block of territory”; and that the lands north of Hill Street largely sloped and drained to the northwest. Appellant city attacks this finding as not supported by the evidence, and the attack thereon is plainly justified. As already pointed out, the maps in evidence established a general slope of the land to the north or northwest in all but the portion of territory lying to the southeast. The accuracy of the maps is not disputed, nor is there any competent evidence to the contrary. In fact the disputed finding is contrary to the allegations of the complaint in this respect. This finding established a natural *648

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Bluebook (online)
114 P.2d 704, 45 Cal. App. 2d 643, 1941 Cal. App. LEXIS 1523, Counsel Stack Legal Research, https://law.counselstack.com/opinion/womar-v-city-of-long-beach-calctapp-1941.