HORNBLENDE

Miscellaneous

Notes

(Richard Willis)

Mineral, of the ideal form (Ca, Na, K)2-3(Mg, Fe2+, Fe3+, Al)5[OH(AlSi3)O11]2
Hardness: 5-6 Density: 2.9-3.4 Insoluble in acids
Common to virtually all granites and feldspathic rocks, thus is most likely a part of most any clay used as found naturally — complex and variable, as it is a group of the amphiboles. The variation with high Fe2O3 content is called “basaltic”

Authors

XML

<?xml version="1.0" encoding="UTF-8"?>
<material name="HORNBLENDE" descrip="" generic="0" rawmineral="1" searchkey="" loi="0.00">
<notes>
<note>Mineral, of the ideal form (Ca, Na, K)&lt;FONT SIZE=2&gt;&lt;SUB&gt;2&lt;/SUB&gt;&lt;/FONT&gt;&lt;SUP&gt;-&lt;FONT SIZE=2&gt;3&lt;/FONT&gt;&lt;/SUP&gt;&lt;FONT SIZE=2&gt;&lt;/FONT&gt;(Mg, Fe&lt;FONT SIZE=2&gt;&lt;SUP&gt;2+&lt;/SUP&gt;&lt;/FONT&gt;, Fe&lt;FONT SIZE=2&gt;&lt;SUP&gt;3+&lt;/SUP&gt;&lt;/FONT&gt;, Al)&lt;FONT SIZE=2&gt;&lt;SUB&gt;5&lt;/SUB&gt;&lt;/FONT&gt;[OH(AlSi&lt;FONT SIZE=2&gt;&lt;SUB&gt;3&lt;/SUB&gt;&lt;/FONT&gt;)O&lt;FONT SIZE=2&gt;&lt;SUB&gt;11&lt;/SUB&gt;&lt;/FONT&gt;]&lt;FONT SIZE=2&gt;&lt;SUB&gt;2&lt;/SUB&gt;&lt;/FONT&gt;&lt;SUB&gt;&lt;BR&gt;
&lt;/SUB&gt;Hardness: 5-6 Density: 2.9-3.4 Insoluble in acids&lt;BR&gt;
Common to virtually all granites and feldspathic rocks, thus is most likely a part of most any clay used as found naturally &amp;#151; complex and variable, as it is a group of the amphiboles. The variation with high Fe&lt;FONT SIZE=2&gt;&lt;SUB&gt;2&lt;/SUB&gt;&lt;/FONT&gt;O&lt;FONT SIZE=2&gt;&lt;SUB&gt;3&lt;/SUB&gt;&lt;/FONT&gt;&lt;SUB&gt; &lt;/SUB&gt;content is called &amp;#147;basaltic&amp;#148;&lt;BR&gt;

</note>
</notes>
</material>



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