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 | | Chemically, clays are hydrous aluminum silicates, ordinarily containing impurities, e.g., potassium, sodium, calcium, magnesium, or iron, in small amounts. |
 | | Residual clays are most commonly formed by surface weathering, which gives rise to clay in three ways--by the chemical decomposition of rocks, such as granite, containing silica and alumina; by the solution of rocks, such as limestone, containing clayey impurities, which, being insoluble, are deposited as clay; and by disintegration and solution of shale. |
 | | Chemically the feldspars are silicates of aluminum, containing sodium, potassium, calcium, or varium or combinations of these elements. |
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