Swett v. Cutts

50 N.H. 439
Supreme Court of New Hampshire·Decided December 15, 1870·Published·Cited by 14 cases

Opinion

Bellows, C. J.

In respect to water not gathered into a stream, but circulating through the pores of the earth, beneath its surface, it is now settled that a land owner, who, in the reasonable use of his own land, obstructs or diverts the flow of such water, even to the injury of his neighbor’s land, is not liable to respond in damages.

This is not upon the principle that has been in some cases adopted, that the land owner has the absolute and unqualified property in all such water as may be found in his soil, and may therefore do what he pleases with it, as with the sand and rock that form part of that soil, but upon the same general principle that governs the use of water flowing on the surface in well defined streams or channels; that is, to make a reasonable use of it for domestic, agricultural, and manufacturing purposes — not trenching, however, upon the similar right of others.

So in respect to water percolating through the soil, the land owner may ordinarily drain his land, may obstruct the usual course of the flow of such water by walls for cellars and other purposes, and may dig wells and use the water for domestic and agricultural purposes.

The test is, the reasonableness of the use or disposition of such water ; and ordinarily that is a question of fact for the jury under the instructions of the court.

In favor of the unqualified and absolute right of the land owner to-dispose of all such water as he finds in his soil, or that he may draw there by wells dug in his own land, it is urged, that he cannot know the condition of the water beneath the surface, the changes that take-place, or the Sources of supply of the springs and wells in the adjoining-lands, or what portion is drawn from his own soil and what was originally found in his neighbor’s, and therefore that there is no ground for presuming a mutual agreement between the land owners in ages past in respect to such underground water, or for holding- a right to have been acquired by use or acquiescence. So is the leading case of Acton v. Blundell, 12 M. & W. 336.

In the first place, we do not understand that the right of the riparian owner to the use of streams of water running upon the surface is to be deduced from the presumed mutual agreement or acquiescence of [444] land owners, but rather as a natural right, incident to the land, to partake in the enjoyment of the common bounty of Providence, as in the cases of light and air. Dickinson v. Canal Co., 7 Excheq. 299; Shury v. Piggot, 3 Bulst. 339; Chasemore v. Richards, 2 H. & N. 168; Tyler v. Wilkinson, 4 Mason 397.

And in the second place, although it may be true that in the majority of cases the condition of the water-flow beneath the surface is not accurately known, yet in a great many instances its general course,— from the slope of the surface, the appearance of springs, and other indications of water, — is quite obvious.

Indeed, this doctrine appears to embrace that large class of cases where the water flows in sight upon the surface in wet seasons of the year, but not to such an extent as to mark a regular channel with banks and sides, and also where the water moves slowly, but obviously, through boggy or swampy lands constituting the sources of streams and rivers.

The doctrine, in fact, would justify a land owner in intercepting and diverting the water, so working its way through spongy or swampy land, at any point before it was gathered into a regular channel, although it might be obvious that such water was the source of a stream which furnished valuable mill sites, even although such diversion was in no way necessary to the enjoyment of his land.

The contrary doctrine in respect to water percolating beneath the surface is established in this State in the well considered case of Bassett v. Salisbury Manufacturing Company, 43 N. H. 569;* and the question is, whether the doctrine of that case applies to water which appears on the surface in the season of melting snow and heavy rains, but is not gathered into any regular channel or water-course, or whether such water stands upon the footing of permanent streams [445] running upon the surface in regular channels. If upon .the latter footing, then the instructions were sufficiently favorable to the defendant.

Upon the examination of the cases which maintain the doctrine that the land owner may dispose of the water percolating beneath his soil as he pleases, they will be found to include the case of mere surface water not gathered into streams.

In Rawstron v. Taylor, 11 Excheq. 380, it is laid down by Parke, Baron, in the opinion of the court, that in the case of common surface water rising out of springy or boggy ground and flowing in no' definite channel, although contributing to the supply of the plaintiff’s mill, the supply being merely casual and the water having no defined course, the defendant is entitled to get rid of it as he pleases.

The same doctrine is announced in Broadbent v. Ramsbotham, 11 Excheq. 602, which was an action for diverting water on defendant’s land which naturally flowed over the surface of a hill into a brook which supplied plaintiff’s mill. The court, per Alderson, Baron, says the right of the plaintiff cannot ■ extend further than the right to the flow in the brook itself, and to the water flowing in some defined natural channel, either subterranean or on the surface, communicating directly with the brook itself. No doubt, he says, all the water falling from heaven and shed upon the surface of the hill, at the foot of which a brook runs, must, by the natural force of gravity, find its way to the bottom, and so into the brook; but this does not prevent the owner of the land on which this water falls from dealing with it as he may please, and appropriating it. He cannot, it is true, do so if the water has arrived at, and is flowing in, some natural channel already formed. But he has a perfect right to appropriate it before it arrives at such a channel.

It is quite clear that such surface water is put upon the same footing as water percolating beneath the surface; and the cases are quite numerous that show it, and we think it should be so upon principle.

The great objection to applying the doctrine, which forbids the diversion of running streams, to water circulating in the pores of the earth, is, that if applied without qualification it would, to a great extent, prevent the beneficial enjoyment and improvement of one’s own land. A similar effect, though less extensive, would be produced by applying that doctrine to mere surface water not gathered into any regular and defined channel. In many cases of springy and swampy lands the water moves from a higher to a lower level over a wide space, which, under such a doctrine, could not be drained or reclaimed. So in case of rain falling upon the side of a hill, and which would naturally find its way upon the surface into a brook at the bottom, — such a doctrine might effectually prevent the improvement of very extensive tracts of lands.

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Swett v. Cutts, 50 N.H. 439 (N.H. 1870).

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