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Book III about halite and nitrium, alum and acrid juices and related minerals, sulphur, bitumen, realgar, and orpiment; the fourth, chrysocolla, aerugo, caeruleum, ferrugo
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BOOK III
37
between there and Arabia, in Cyrenaica. While all this latter salt can be called sal ammoniac, the name is usually given only to that from Cyrenaica. So much regarding the occurrence of natural halite within the earth. Natural halite is found also in springs, rivers, lakes and oceans on the surface of the earth. Springs, such as the hot springs at Pegasius, may carry salt. It is often produced from rivers when they are dried up by the sun's heat. The salt plain of Narbonne, France, is of this origin. The plain near the marshy spring at Schonbach in Elboganum becomes white with salt during the summer. A river may carry small grains of salt as do the Oxus and Ochus rivers where they flow out of the mountains opposite Balkh, or rivers may have a crust of salt on the surface and the water will flow out from under this crust as freely as does the water from under a glacier. An example of the latter is the river which flows into the Caspian Sea between Armenia and Mardos. Pliny has written extensively about salt, apparently having taken it from Theophrastus. A lake may be saturated with salt and even turn into solid salt. It turns into salt in different ways. The entire lake may be so converted as at Taranto, Apulia, and at Tragasaeus, Aeolia, which is near Amaxitus not far from the temple of Apollo. One part of the lake may turn to salt as at Tuz Geul, Phrygia, from whence comes the Tattaeus salt; in Cappadocia; at Aspendus, Pam-phylia. Only the ends of some lakes are converted into salt as at Cocanicus and Gela, Sicily. The lake near Citium, Cyprus, and the Dead Sea of Palestine have become saturated with salt. The salt from the Dead Sea is called "Salt of Sodom." Other lakes that produce salt are two desolate lakes in Balkh, one near Scythia, the other near Arios; one near Memphis, Egypt; many in Africa. Salt forms in thin crusts on the shores of oceans. In summer when it is hot foam forms and this is driven onto the shore and rocks. This foam, cut off from the ocean, dries and is converted into salt. The material Dioscorides calls
a\os άχνης,
Pliny calls "foam" and we, usually, "dry sea foam" or more correctly "salt formed from sea foam." Younger writers call it
salts spuma
(foam of salt). Although they write in this poetic manner nevertheless they understood its origin as I shall explain elsewhere.
I have said enough about the origin of halite and shall now take up briefly the manufacture of salt since I can explain the differences in its natural properties and formation more accurately this way. Salt is produced from marine waters, saline springs, salt wells, and from alkaline solutions. I shall explain the methods of making salt in a book on mining. Halite varies in color. The natural mineral from Sarmatia is transparent and white. Similar material is found in the Carpathians and in Dacia while the mineral from the lakes near Taranto is the finest of all. Our salt works at Luneburg produce white salt. "Flowers of salt" whether it blossoms in mines or brine pits is usually white. Gray halite is often not transparent, as at Sarmatia and Dacia. In these various localities the halite may be white in one place and black or gray in another. Norwegian salt which is
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Agricola. Textbook of Mineralogy.
Front page, forword and index
To the illustrious duke of saxony and thuringia and misena prince of Maurice
Book I Minerals color, taste, odor , physical properties of gemstones and minerals such as emeralds, diamonds, rubies, sapphires
Book II About different applications of earths (painting, medical) and their occurrences
Book III about halite and nitrium, alum and acrid juices and related minerals, sulphur, bitumen, realgar, and orpiment; the fourth, chrysocolla, aerugo, caeruleum, ferrugo
Book IV Sulphur, amber, Pliny's gems, jet, bitumen, naphtha, camphor, maltha, Samothracian gem, thracius stone, obsidianus stone
Book V about lodestone, hematite, geodes, hematite, selenite, lapis secularum, asbestos, mica
Book VI gems: diamond, emeralds, sapphire, topaz, chrysoberyl, carbuncle, jaspis
Book VII marbles, gems in rings and other applications
Book VIII metals, precious such as gold, platinum, silver
Book IX artificially coloring of metals such as gold, silver, copper
Book X lapis sabinicus, lapis selentinus, lapis liparaeus and other mixtures of stone, metal and earth
Latin Mineral Index
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