Hornblende
Hornblende is a complex series of silicate minerals.[1]
Hornblende is not a recognized mineral in its own right, but the name is used as a general or field term, to refer to a dark amphibole.
It is an isomorphous mixture of three molecules; a calcium-iron-magnesium silicate, an aluminium-iron-magnesium silicate, and an iron-magnesium silicate.
Hornblende has a hardness of 5–6, a specific gravity of 2.9–3.4 and is typically an opaque green, greenish-brown, brown or black color. It is most often confused with the minerals augite and biotite mica, both of which are black and can be found in granite.
Occurrence
Hornblende is a common constituent of many igneous and metamorphic rocks such as granite, diorite, gabbro, basalt, andesite, gneiss, and schist. It is the principal mineral of amphibolites.
Very dark brown to black hornblendes that contain titanium may be called basaltic hornblende, from the fact that they are usually a constituent of basalt and related rocks.
Etymology
The word hornblende is derived from the German horn and blenden, to 'blind' or 'dazzle'. The term blende is often used to refer to a brilliant non-metallic luster, for example, zincblende and pitchblende, the ore of uranium.
Hornblende Media
Hornblende diorite from the Henry Mountains, Utah, US
Related pages
References
- Hurlbut, Cornelius S.; Klein, Cornelis, 1985, Manual of Mineralogy, 20th ed., John Wiley and Sons, New York, p 416-7, ISBN 0-471-80580-7
- Mindat retrieved 06/21/05
- Scandinavian mineral gallery Archived 2010-05-02 at the Wayback Machine retrieved 06/21/05
- Table Info retrieved 2/27/07