The Arizona sentinel., 1896-08-22

of eheEG Gia and Colorado rivers have for the most part deep sedimentary soil of brownish, gray sandy loam, resting, in most places, upon gray clay subsoil at depth of from ten to twenty feet below the surface, The clay subsoil forms hard pan which is impervious to water. These soils have been slowly formed by the decomposition of shades, sandstones, marls lmestones, etc., mixed with or ganic and vegetable matter, washed down by the mighty rivers and have been gradually deposited during the course of centuries. The fertilzing brownish mud held in the wat tlof the Colorado and Gils rivers resembles that from the Nile, and its quantity varies from 01 to o.5 per cent, though the water when even considerably discolor- ed by mud is good to drink, resembling in this res pect the Missouri river water chemical analysis of the sediments of the Colorado and of the Nile exhibits wonderful similarity in the constituent parts of each. That of the Colorado exhibiting a trife less potassa, most phosphoric acid and car bonade of limestone beds through which the Colo rado paSses In other respects the sediment of the Colorado is almost identical with that of the Nile. It will be noticed therefore, that when this water is used for irrigation it is superior to artesian waters since it is constantly supplying the land with the richestfertlizing elements The soil of the valleys IS extremely rich in dedomposed vegetable matter and uncombined carbon, readily absorbing the aerial gases, such especially oxygen, which en- tering the soil, decomposes the organic matters so that they can be taken up and nourish the plants which may be considered leading feature in its fertility. It also readily takes up aHd retains moisture, while the rmress of it's particles affords every facility for percelation and the activity of capillary action. In ts mechanical composition its particles are in a state of very fine division, which renders it more productive than coarser soils. It acquires heat readily in the daytime, and the loss of the heat at night is very gradual that it re- mains always warm and is not subject to sudden changes of heat and cold Besides it's essential stituents of water, organic or vegetable matter, sand and clay, chemical analysis shows that lime, soda, magnesa, iron, ammonia and available forms of nitrogen phesphoric acid and potash enter into composition in the proportions best adapted to add to it's fertility though of course, as is always the in soil analysis, its composition varies in different localities and is not aways constant.
 The soi the uplands, mesas, lighter and more gravelly and in some places of tree, loamy, calcareous character. The mesa lands are warm and generous. They seem especially adapted for the grape, olive and citrus fruits generally Their soil contains more magnesia, lime or chalk than the bottom lands. It cracks and retains moisture admirably in summer It is of that character which will produce wine that will keep good for fifty or hundred years, and improve annually, not being liable to sour on exposure to the air, after one year old to become turbid and change color in the bottle or glass.
 We can safely say that the soil of Yuma County nowhere be surpassed containing as it does all the essential clements of richness and fertility.