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Mineral vs Aluminosilicate - What's the difference?

mineral | aluminosilicate |

As nouns the difference between mineral and aluminosilicate

is that mineral is (geology) any naturally occurring inorganic material that has a (more or less) definite chemical composition and characteristic physical properties while aluminosilicate is (inorganic chemistry) any of many silicate minerals, such as feldspar and zeolite, in which a proportion of the si4+ ions are replaced by al3+, the excess negative charge being balanced by extra sodium, potassium or calcium ions.

As a adjective mineral

is of, related to, or containing minerals.

mineral

Alternative forms

* minerall (obsolete)

Noun

(en noun)
  • (geology) Any naturally occurring inorganic material that has a (more or less) definite chemical composition and characteristic physical properties.
  • * {{quote-magazine, date=2012-03
  • , author=Lee A. Groat , title=Gemstones , volume=100, issue=2, page=128 , magazine=(American Scientist) citation , passage=Although there are dozens of different types of gems, among the best known and most important are diamond, ruby and sapphire, emerald and other gem forms of the mineral beryl, chrysoberyl, tanzanite, tsavorite, topaz and jade.}}
  • Any inorganic material (as distinguished from animal or vegetable).
  • Any inorganic element that is essential to nutrition; a dietary mineral.
  • (British) Mineral water.
  • (Ireland, South Africa, informal) A soft drink, particularly a single serve bottle or can.
  • (obsolete) A mine or mineral .
  • * 1599 , , IV. i. 26:
  • O'er whom his very madness, like some ore / Among a mineral of metals base, / Shows itself pure;

    Derived terms

    * rare earth mineral

    Adjective

    (head)
  • of, related to, or containing minerals
  • Derived terms

    * mineral acid * mineral oil * mineral processing * mineral tar * mineral water * mineral wax * mineral weathering * mineral wool

    Anagrams

    * * ----

    aluminosilicate

    English

    Noun

    (en noun)
  • (inorganic chemistry) Any of many silicate minerals, such as feldspar and zeolite, in which a proportion of the Si4+ ions are replaced by Al3+, the excess negative charge being balanced by extra sodium, potassium or calcium ions.