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A mineral lick (also known as a salt lick) is a place where animals can go to lick essential mineral nutrients from a deposit of salts and other minerals. Mineral licks can be naturally occurring or artificial (such as blocks of salt that farmers place in pastures for livestock to lick).
This is often done with corn or a mineral block, such as a salt-lick, and where the hunter sits perched in a higher elevation some distance away, awaiting the deer's visit. [10] If this were done at night, a miner's acetylene lamp, or an electric spotlight, was placed near the mineral block so as to see the animal when it approaches. Another ...
An Introduction to the Rock-Forming Minerals (known familiarly as DHZ, from the surnames of its authors [1]), is a reference book by William Alexander Deer, Robert Andrew Howie, and Jack Zussman often considered the "bible" of mineralogy.
Within a mineral species there may be variation in physical properties or minor amounts of impurities that are recognized by mineralogists or wider society as a mineral variety. The International Mineralogical Association (IMA) is the international scientific group that recognises new minerals and new mineral names.
Feldspar (/ ˈ f ɛ l (d) ˌ s p ɑːr / FEL(D)-spar; sometimes spelled felspar) is a group of rock-forming aluminium tectosilicate minerals, also containing other cations such as sodium, calcium, potassium, or barium. [3]
Hauyne or haüyne, also called hauynite or haüynite (/ ɑː ˈ w iː n aɪ t / ah-WEE-nyte), [7] old name Azure spar, [8]: 571 is a rare tectosilicate sulfate mineral with endmember formula Na 3 Ca(Si 3 Al 3)O 12 (SO 4). [1] As much as 5 wt % K 2 O may be present, and also H 2 O and Cl. It is a feldspathoid and a member of the sodalite group.
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Deer stones are generally located in the most productive, well-watered areas of the northern Mongolian steppe.[11] [12]Although Mongolia is globally quite arid, deer stones are generally located in the most productive, well-watered areas of the northern Mongolian steppe, particularly in the north and the west of the country, where most of Mongolia's cultural development has always taken place.
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