HORNBLENDE
Miscellaneous
- Family: None
- Region: None
- Mined At: Unspecified
- Raw Mineral: Yes
- Generic: No
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
- Richard Willis (Owner)
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)<FONT SIZE=2><SUB>2</SUB></FONT><SUP>-<FONT SIZE=2>3</FONT></SUP><FONT SIZE=2></FONT>(Mg, Fe<FONT SIZE=2><SUP>2+</SUP></FONT>, Fe<FONT SIZE=2><SUP>3+</SUP></FONT>, Al)<FONT SIZE=2><SUB>5</SUB></FONT>[OH(AlSi<FONT SIZE=2><SUB>3</SUB></FONT>)O<FONT SIZE=2><SUB>11</SUB></FONT>]<FONT SIZE=2><SUB>2</SUB></FONT><SUB><BR>
</SUB>Hardness: 5-6 Density: 2.9-3.4 Insoluble in acids<BR>
Common to virtually all granites and feldspathic rocks, thus is most likely a part of most any clay used as found naturally &#151; complex and variable, as it is a group of the amphiboles. The variation with high Fe<FONT SIZE=2><SUB>2</SUB></FONT>O<FONT SIZE=2><SUB>3</SUB></FONT><SUB> </SUB>content is called &#147;basaltic&#148;<BR>
</note>
</notes>
</material>
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