Rural Hygiene. Henry N. Ogden
because of their presence, and the worst thing which may be charged against a thick growth is that it keeps out the sun. Practically two points may, however, be urged against trees growing too close to a house. If near enough for leaves to drop on the roof, rain troughs and leaders become stopped up and cause trouble. A thick growth directly over a shingle roof allows organic matter to accumulate on the shingles, so that vegetation develops and the roof decays more rapidly than if exposed to sun and wind. Again, and it is no trivial matter, a house whose roof is easily accessible from trees is apt to become infested with squirrels, who get into the attic, run through the walls, and become a great nuisance. For these reasons, then, trees should be far enough away from the house to allow the sun to enter the windows freely and to keep away from the roof objectionable animals, large and small.
Space between houses.
It is a law or custom as ancient as the Romans that requires a proprietor to build his house so that the eaves should not overhang on the land of his neighbor. Our grandfathers, with the same idea, used to say that a man should be able to drive his team around his house on his own land. In our day it is highly desirable that a house should be built so as to leave as much land under control between the buildings and the lot line as possible. This, of course, does not apply to houses built on a farm of a hundred acres or more, but rather to the house in a small village where a few hundred people live closely together, under rural conditions. In such a village the water-supply usually comes from wells, and the wastes of the household are discharged into privies and cesspools. There is no law, unfortunately, which restricts the location of either of these two essential structures, and it is quite possible for a well, built within a few feet of a property line, to be ruined in quality by a cesspool, built later, on the other side of the line. It seems very unjust that, after the trouble and expense of building a well, a neighbor may render it worthless by the location of his cesspool, and yet, unless one can prove a direct underground connection between well and cesspool, no law is applicable to prevent the construction of the latter.
Besides such a menace to health, there are other objections to the immediate vicinity of neighbors which can be avoided by a judicious interposition of space. For example, the writer listened through a long evening, recently, to a hearing before a City Commissioner of Health, where one householder and a crowd of witnesses complained of the noise made by a kicking horse in an adjacent stable. The one witness who was not disturbed by the noise, and who lived in the vicinity, was unexpectedly found to be deaf.
It is wisdom also to have a reasonable space between a house and the highway, chiefly because the dust of the road is thereby kept from the house. There are people who find much enjoyment in watching passers-by on the road, and with them front windows would be as close to the road as possible, but it is wiser to have a front yard of at least fifty feet depth when possible.
Finally, the location on a sidehill, even when otherwise advantageous, is to be regarded with suspicion if the subsoil strata are horizontal and neighbors up the slope have cesspools in use. The writer knows of several cesspools, built in rock, which, so far as their owners were concerned, have worked successfully for many years, but the water leeching away through the rock was finally discovered to be the cause of continual dampness in neighboring cellars, on lower ground, to the manifest discomfort of those occupying the houses.
Composition of soils.
Having thus discussed the location of the house with reference to its surroundings, let us now more carefully examine the character of the soil or earth foundation on which the house shall be built. All soil is made up of varying proportions of mineral and vegetable matter in the interstices of which there are usually to be found more or less air, water, and watery vapor. The mineral substances of soil include almost all of the known minerals, although many of them are found in exceedingly small quantities. The most common and the most important mineral elements of the soil of New York State are carbon, silicon, aluminum, and calcium, which combine in various ways to make either sand, sandstone, clay, shale, limestone, or other rock. The particular form which these mineral elements assume is of interest in choosing a location for a house, for two reasons:—
In the first place, it has been asserted that the mineral constituents of a soil directly affect the health of persons living on that material. For instance, the earlier writers on hygiene gravely pointed out that very hard granite rocks, when weathered and disintegrated, became permeated by a fungus and caused malaria. We are, however, now so sure of the cause of malaria that we only laugh at a theory upheld by scientists of only twenty years ago.
Some constitutional diseases, including goiter and cancer, have been supposed to flourish in localities where an excess of calcium exists in the soil, and it is true that these diseases do have an unusual prevalence in certain limited districts; but no modern scientist ventures to say whether the boundaries of those districts are determined by the character of the soil constituents or by some other predisposing factor. The truth is that, in matters not absolutely determined by science, many theories usually have to be evolved and proved worthless before the real cause is found.
In the matter of appendicitis, for instance, it was formerly asserted that the seed of grapes was responsible for the local inflammation, and that one could never have appendicitis if such seeds were not swallowed. This theory is to-day almost forgotten, and one eminent surgeon has asserted that the prevalence of this disease in a district depends on the calcium in the soil, since it is to that mineral that hard water is due, although this has not been substantiated. No information is to-day available by which the fitness of a soil for securing sanitary conditions of building can be determined.
Cancer and soil conditions.
In the case of cancer, however, while no final conclusions can be drawn, there is some definite indication that the soil conditions have connection with the occurrence and continued appearance of cancer. It is known that this dread disease is abnormally prevalent in certain districts of the world where topography and climate are fairly alike. For example, the entire region between the Danube and the Alps from Vienna westward and between the Jura and Alps to Geneva furnishes the highest mortality from cancer in all Europe. The subsoil is clay with a thin covering of surface soil, the hillsides draining on to level valleys with meandering watercourses that frequently inundate and supersaturate the already moist soil.
This condition seems to prevail wherever cancer is abnormally prevalent. In England, in northwestern France, and in Spain the topography described in every case accompanies a high death-rate from cancer. It is of great interest to find that in New York State the two districts that are conspicuously affected by this disease have the same topography. The Unadilla Valley and some parts of the Allegheny Valley are noted for their cancer houses, and in both localities we find the same kinds of hillsides and water-soaked valleys as in Germany and France. It has also been noted that the older geological formations are free from the disease and that an occasional inundation does not seem to be a factor. Altogether there seems to be some ground for assuming a connection between cancer and soil conditions, at any rate until scientists have determined the real cause of the disease in those localities where it is now so markedly prevalent.
Topography.
The soil, however, with its mineral characteristics, does indirectly affect the health of the householder because different kinds of rock form themselves naturally into different surface formations, some healthy and some unhealthy. For example, localities where granite rock abounds and comes near the surface are usually healthy because the surface slope is great enough to carry off all drainage water rapidly. The air therefore is dry and not influenced by the immediate vicinity of swamps. The drinking water is soft, and malarial breeding places are usually absent.
Limestone rock, on the other hand, is commonly laid down in horizontal strata, and while a succession of strata may frequently give rapid slopes, marshes are very common, existing even on the tops of the hills. The drinking water is always to be suspected as to quality because, in the first place, it is hard from absorption of lime, and in the next place, cavities and seams in the rock allow polluting material to travel for long distances.
Sandstone, being porous, may be considered a healthy foundation, and sands and gravels of all sorts are usually free from marshy land.
Gravel has always