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continuously in the form of a spiral as in the Bordenave system. To those wishing to pursue the subject further, the following books among others may be suggested:--Sabin, _Cement and Concrete_ (New York); Taylor and Thompson, _Concrete, Plain and Reinforced_ (London); Sutcliffe, _Concrete, Nature and Uses_ (London); Marsh and Dunn, _Reinforced Concrete_ (London); Twelvetrees, _Concrete Steel_ (London); Paul Christophe, _Le Beton arme_ (Paris); Buel and Hill, _Reinforced Concrete Construction_ (London). (F. E. W.-S.) CONCRETION, in petrology, a name applied to nodular or irregularly shaped masses of various size occurring in a great variety of sedimentary rocks, differing in composition from the main mass of the rock, and in most cases obviously formed by some chemical process which ensued after the rock was deposited. As these bodies present so many variations in composition and in structure, it will conduce to clearness if some of the commonest be briefly adverted to. In sandstones there are often hard rounded lumps, which separate out when the rock is broken or weathered. They are mostly siliceous, but sometimes calcareous, and may differ very little in general appearance from the bulk of the sandstone. Through them the bedding passes uninterrupted, thus showing that they are not pebbles; often in their centres shells or fragments of plants are found. Argillaceous sandstones and flagstones very frequently contain "clay galls" or concretionary lumps richer in clay than the remainder of the rock. Nodules of pyrites and of marcasite are common in many clays, sandstones and marls. Their outer surfaces are tuberculate; internally they commonly have a radiate fibrous structure. Usually they are covered with a dark brown crust of limonite produced by weathering; occasionally imperfect crystalline faces may bound them. Not infrequently (e.g. in the Gault) these pyritous nodules contain altered fossils. In clays also siliceous and calcareous concretions are often found. They present an extraordinary variety of shapes, often grotesquely resembling figures of men or animals, fruits, &c, and have in many countries excited popular wonder, being regarded as of supernatural origin ("fairy-stones," &c.), and used as charms. Another type of concretion, very abundant in many clays and shales, is the "septarian nodule." These are usually flattened disk-shaped or ovoid, often lobulate externally like the sur
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