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Sentences for "clays "
" The purest clays are produced by the decomposition of felspar, but almost all the crystalline rocks may produce them by the removal of their alkalies, iron, lime, etc.
Its advantages have chiefly been observed on two sorts, heavy clays and peat soils, on both of which it has been practised to a great extent.
The action of heat on the heavy clays appears to be of a twofold character, depending partly on the change effected in its physical properties, and partly on a chemical decomposition produced by the heat.
In such clays heat operates by causing the lime to decompose the alkaline silicates, and liberate a quantity of the potash which was previously in an unavailable state.
Experience has shewn that its effects are most beneficial on light and deep sandy soils, but that on heavy retentive clays it is without effect, or even absolutely injurious.
Heavy clays are observed to become lighter and more open in their texture; and those which are too rich in organic matter have it rapidly reduced in quantity, and the excessive lightness which it occasions diminished.
Red and blue clays 120 ” 3.
txt Above the Red Deep-Water Clays To hear the poet read ""Above the Red Deep-Water Clays,"" click .
The term ""marl"" is very generally employed to designate the clays of the Lower and Upper Trias, but the term is inappropriate, as they may contain no lime, and are therefore not always genuine marls.
In Britain, the Keuper is 1000 feet or more in thickness, and consists of white and brown sandstones, with red marls, the whole topped by red clays with rock-salt and gypsum.
Its Upper portion, for a thickness of 150 to nearly 300 feet, is chiefly argillaceous, consisting of clays with sandy layers, and occasionally courses of limestone.
Above these, or forming the base of the formation where these are wanting, come mottled clays and sands with lignite (Woolwich and Reading series), which are estuarine or fluvio-marine in origin.
The Jackson series is represented by lignitic clays and marls which occur at Jackson, Mississippi.
The former consist of blue clays and lignites, with an abundance of plants.
-All clays are the result of the denudation and decomposition of felspathic and siliceous rocks, and consist of the fine insoluble particles which have been carried in suspension in water and deposited in geologic basins according to their specific gravity and degree of fineness (see Clay).
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