The New Encyclopædia BritannicaEncyclopædia Britannica, 1983 - Encyclopedias and dictionaries |
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Page 517
... chloride , or common table salt ( compare with seawater , at 35,000 milligrams per litre ) . Many spring waters issuing from deep sedimentary rocks are mineralized : some are only slightly salty , whereas others are several times as ...
... chloride , or common table salt ( compare with seawater , at 35,000 milligrams per litre ) . Many spring waters issuing from deep sedimentary rocks are mineralized : some are only slightly salty , whereas others are several times as ...
Page 786
... chloride structure , in which each ion occupies a position within an octahedron composed of six oppositely charged neighbours . The most common sulfide mineral crystallizing in this manner is the ore mineral of lead , galena ( PbS ) . A ...
... chloride structure , in which each ion occupies a position within an octahedron composed of six oppositely charged neighbours . The most common sulfide mineral crystallizing in this manner is the ore mineral of lead , galena ( PbS ) . A ...
Page 787
... chloride structure and similar crystal morphologies but otherwise exhibit many different properties . Their lustres range from the bright metallic lustre of galena to the dull and vitreous lustre of alabandite . All except oldhamite ...
... chloride structure and similar crystal morphologies but otherwise exhibit many different properties . Their lustres range from the bright metallic lustre of galena to the dull and vitreous lustre of alabandite . All except oldhamite ...
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