 | Edward Hitchcock, Charles Henry Hitchcock - 1860 - 442 Seiten
...one of the most common constituents of spring water." Hunt, of the Canada Survey, maintains that " dolomites, magnesites, and magnesian marls, have had...origin in sediments of magnesian carbonate, formed by tho evaporation of solutions of bicarbonate of magnesia :" which solutions have resulted from the decomposition... | |
 | Vermont. State Geologist, Edward Hitchcock, Albert David Hager, Charles Henry Hitchcock, Leo Lesquereux, Elkanah Billings - 1861 - 570 Seiten
...of spring water." Hunt, of the Canada Survey, maintains that " dolomites, magnesites, and magnesia marls, have had their origin in sediments of magnesian...evaporation of solutions of bicarbonate of magnesia ;" which solutions have resulted from the decomposition of sulphate or chloride of magnesia by bicarbonate... | |
 | Edward Hitchcock, Charles Henry Hitchcock - 1862 - 434 Seiten
...constituents of spring water." Hunt, of the Canada Survey, maintains that " dolomites, rnagnesites, and magnesian marls, have had their origin in sediments of magnesian carbonate,' formed by tho evaporation of solutions of bicarbonate of magnesia :" which, solutions have? resulted from the... | |
 | Edward Hitchcock, Charles Henry Hitchcock - 1866 - 448 Seiten
...one of the most common constituents of spring water." Hunt, of the Canada Survey, maintains that " dolomites, magnesites, and magnesian marls, have had...evaporation of solutions of bicarbonate of magnesia :" which solutions have resulted from the decomposition of sulphate or chloride of magnesinm by bicarbonate... | |
 | Thomas Sterry Hunt - 1875 - 520 Seiten
...double salt is formed, which is dolomite. 4. Solutions of bicarbonate of magnesia decompose chloride of calcium, and, when deprived of their excess of...bicarbonate of magnesia. These solutions have been produced either by the action of bicarbonate of lime upon solutions of sulphate of magnesia, in which case gypsum... | |
 | Thomas Sterry Hunt - 1875 - 530 Seiten
...double salt is formed, which is dolomite. 4. Solutions of bicarbonate of magnesia decompose chloride of calcium, and, when deprived of their excess of...bicarbonate of magnesia. These solutions have been produced either by the action of bicarbonate of lime upon solutions of sulphate of magnesia, in which case gypsum... | |
 | Arkansas Geological Survey - 1893 - 532 Seiten
...sediment.* In another place (Essays, p. 90) he says that dolomites, magnesites, and magnesian marls have their origin in sediments of magnesian carbonate formed...evaporation of solutions of bicarbonate of magnesia. Ramsay ,f Cordier, and LeymerieJ express similar views. Dr. Irving|| says that calcium being more strongly... | |
 | 1877 - 1224 Seiten
..."Conclusions" of his p»Fr on the Chemistry of Dolomites and Gypsums.*) " Dolomites, ntf?' nesites, and magnesian marls, have had their origin in sediments...bicarbonate of magnesia. These solutions have been produced cither by the action of bicarbonate of lime upon solutions of sulphate « magnesia, in which case gypsum... | |
 | Arkansas Geological Survey - 1893 - 530 Seiten
...sediment.* In another place (Essays, p. 90) he says that dolomites, magnesites, and magnesian marls have their origin in sediments of magnesian carbonate formed...evaporation of solutions of bicarbonate of magnesia. Ramsay, f Cordier, and LeymerieJ express similar views. Dr. IrvingH says that calcium being more strongly... | |
 | Geological Survey of Arkansas - 1898 - 530 Seiten
...sediment.* In another place (Essays, p. 90) he says that dolomites, magnesites, and magnesian marls have their origin in sediments of magnesian carbonate formed...evaporation of solutions of bicarbonate of magnesia. Ramsay, f Cordier, and Lej'merieJ express similar views. Dr. Irving', says that calcium being more... | |
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Dolomites, magnesites, and magnesian marls have had their origin in sediments of magnesian carbonate formed by the evaporation of solutions of bicarbonate of magnesia. These solutions have been produced either by the action of bicarbonate of lime upon... 
