Hull v. Harker
Cases that cite this one
24 later published cases cite this decision.
- Board of Supervisors v. Board of Supervisors (Iowa 1932)
- Town of Paden City v. Felton (W. Va. 1951)
- Town of Paden City v. Felton (W. Va. 1951)
- Grimes v. County of Polk (Iowa 1948)
- Hunt v. Smith (Iowa 1947)
- Besler v. Greenwood (Iowa 1927)
- Cresap v. Livingston (Iowa 1921)
- Miller v. Hester (Iowa 1914)
- Parizek v. Hinek (Iowa 1909)
- Heinse v. Thorborg (Iowa 1930)
- Schwartz v. Wapello County (Iowa 1929)
- Tennigkeit v. Ferguson (Iowa 1921)
- Lessenger v. City of Harlan (Iowa 1918)
- Kaufman v. Lenker (Iowa 1914)
- Martin v. Schwertley (Iowa 1912)
- Lyon v. Board of Supervisors (Iowa 1912)
- Jontz v. Northup (Iowa 1912)
- Hatton v. Cale (Iowa 1911)
- Cech v. City of Cedar Rapids (Iowa 1910)
- Chicago, B. & Q. R. v. Board of Sup'rs (8th Cir. 1910)
- Baker v. Incorporated Town of Akron (Iowa 1909)
- Steber v. Chicago, Great Western Railway Co. (Iowa 1908)
- Brown v. Honeyfield (Iowa 1908)
- Neuhring v. Schmidt (Iowa 1906)
This list shows which later cases cite this one. It does not say how they treated it, and no review of that has been done. Not a substitute for Shepard’s or KeyCite — verify before relying.
Opinion of the Court
Plaintiff’s land is situated adjoining to and south of the lands of defendants, and a natural swale runs in a southeasterly direction, crossing the lands of defendants and the land of plaintiff. This swale is the principal waterway through which surface water from a considerable distance to the north is carried southward into what is called “ Preston’s Branch.” In two or three places north of plaintiff’s land this swale is crossed by «highways, and in each instance an opening has been'provided below the surface of the highway by means of large tiles, eighteen to twenty-four inches in diameter, through which any surface water which may flow down the swale after heavy rains may pass. It is shown beyond question that this swale is the natural channel through which the surface water from defendant’s lands and other lands more remote from
The natural swale referred to in the case before us seems to serve substantially the same purpose as the swale described in Wharton v. Stevens, 84 Iowa, 107. It is the natural water course for the drainage through plaintiff’s land of the surface water from the lands of defendants and others, and defendants have the right to have the water from their lands flow over plaintiff’s land along this swale or natural water course, so long as they do not cause it to be discharged, upon plaintiff’s land in a greater quantity or in a substantially different manner than before the construction of their tile drains. We are satisfied from the evidence that no water is drawn by these drains down to plaintiff’s boundary that'would not naturally find its outlet along this swale if no drains had been constructed. Possibly defendants’ lands are more quickly freed from surface water by means of these drains, but an examination of the whole record fails to show that any substantial injury accrues to plaintiff from an increased flow of water. In case of a heavy rainfall the surface water flows at once over plaintiff’s land, but after the surface has been relieved of the immediate accumulation of water there seems to be no such flow through
Defendants “ are not diverting the water from the waterway provided by nature. They are not seeking to conduct the water contrary to the course of nature, or in a way it did not run before the soil became the property of man.” Vannest v. Fleming, 79 Iowa, 638. To entitle plaintiff to relief, it must appear “ that the quantity of water drawn upon plaintiff’s land was materially and unduly increased, to plaintiff’s damage,” by the construction of defendants’ tile drains. Dorr v. Simmerson, 127 Iowa, 551.
We are satisfied on the whole case that plaintiff has no ground of complaint, and that the decree dismissing his petition was proper, and such decree is therefore affirmed.
Case-law data current through December 31, 2025. Source: CourtListener bulk data.