Applied Geology a Treatise On the Industrial Relations of Geological Structure
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Sea-water contains 2. 6 per cent of salt, and nearly i per cent more of other saline ingredi- ents ; the brines of Syracuse hold from 14 to about 18 per cent of salt ; those of Michigan, from 15 to nearly 20 per cent ; those of Goderich, Ontario, from 20 to 24 per cent ; and the weaker brines of West Virginia and Ohio, about 10 per cent.
Beds or deposits of rock-salt occur associated with beds of gypsum, marls, and clays, and sometimes, as at Goderich, of porous dolomites. They have in all prob...a- bility originated from the desiccation of salt lakes, or of sea-borders cut off from the main body of water by bar- riers which were occasionally overleaped by the outside waters, thus adding new supplies to be concentrated by evaporation. In the process of concentration such waters would naturally first deposit their least soluble ingredient, gypsum or anhydrite, which is always present in sea-water, and afterward, with increasing concentration, their salt ; while earthy substances, washed from the adjacent lands, 3 o6 APPLIED GEOLOGY.
What to read after Applied Geology a Treatise On the Industrial Relations of Geological Structure?
You can find similar books in the "Read Also" column, or choose other free books by Samuel Gardner Williams to read onlineMoreLess
To quickly assess the difficulty of the text, read a short excerpt:
Sea-water contains 2. 6 per cent of salt, and nearly i per cent more of other saline ingredi- ents ; the brines of Syracuse hold from 14 to about 18 per cent of salt ; those of Michigan, from 15 to nearly 20 per cent ; those of Goderich, Ontario, from 20 to 24 per cent ; and the weaker brines of West Virginia and Ohio, about 10 per cent.
Beds or deposits of rock-salt occur associated with beds of gypsum, marls, and clays, and sometimes, as at Goderich, of porous dolomites. They have in all prob...a- bility originated from the desiccation of salt lakes, or of sea-borders cut off from the main body of water by bar- riers which were occasionally overleaped by the outside waters, thus adding new supplies to be concentrated by evaporation. In the process of concentration such waters would naturally first deposit their least soluble ingredient, gypsum or anhydrite, which is always present in sea-water, and afterward, with increasing concentration, their salt ; while earthy substances, washed from the adjacent lands, 3 o6 APPLIED GEOLOGY.
What to read after Applied Geology a Treatise On the Industrial Relations of Geological Structure?
You can find similar books in the "Read Also" column, or choose other free books by Samuel Gardner Williams to read onlineMoreLess
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