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pg b098a: First annual report of the Geological Survey of Texas Publication 5235917-1.

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98

than that in which it naturally occurs. This does away with the inconvenience of having it crumble. Such bricks are considerably used in France and Belgium for railroad and other purposes.
  • 3. Lignite of a black color, in a finely powdered state, has been used in England, under the name of "Cologne Earth," as the basis of a black paint.
  • 4. Lignite has been successfully used in place of bone-black in clarifying sugar.
  • ANALYSES OF TEXAS LIGNITES AND COAL. Volatile Fixed Sul- W . Matter. Carbon. Ash. phur. Lignite-Rockdale, Milam County......... 19.925 52.425 22.000 5.650 1.235 Atascosa County................ 13.285 59.865 18.525 8.325 2.360 Athens, Henderson County....... 9.100 42.200 7.375 41.325 0.625 Rusk County...1.............. 16.825 46.325 31.475 5.375 1.090 Calvert Bluff, Robertson County... 16.475 58.400 18.675 6.450 1.330 Shelby County .................. 18.260 43.510 29.530 8.700 2.460 Leon County ................... 14.670 37.320 41.070 6.690 0.250 Rockdale, Milam County ........ 13.800 43.550 36.830 5.320 1.350 ANALYSES OF LAREDO AND EAGLE PASS COAL. Volatile Fixed SA , ul- ter Matter. Carbon. As phur. Laredo Coal ........................... 2.5 51.05 39.1 7.35 1.5 Eagle Pass Coal....................... 3.675 39.42 41.7 15.205 0.81

    MINERAL SPRINGS.

    Springs are of very frequent occurrence throughout East Texas. Somethey are very pure, and almost entirely free from any mineral matter, while at other times they are highly charged with iron, sulphuric acid, and salts of lime, magnesia, alumina, and alkalies. Iron springs, however, are by far the most plentiful of all the mineral waters, and it is an exceedingly common occurrence to see chalybeate waters arising from Tertiary strata. The interstratification of sand and clay beds, representing as they do alternate permeable and impermeable layers, is peculiarly favorable to the existence of local springs. Water falls on the sandy surface of a hill and runs down between the loose materials until it meets a clay bed. This proves impassable on account of its impervious nature, and the water, thus deflected from its downward course, runs over the surface of the clay until it reaches the outcrop of the bed in a hillside or river bluff, and here gushes out as a spring. The ferruginous springs derive their iron from the beds through which they pass. The sandy soils are often bleached on the surface, while "


    Compare First Report of Progress Geological and Mineralogical Survey of Texas, 1888, p. 20.

     

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