Difference between revisions of "Habit"

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[http://www.amazon.com/gp/product/B000WDQF18?ie=UTF8&tag=gemsandwhywelove&link_code=as3&camp=211189&creative=373489&creativeASIN=B000WDQF18 Gemmology 3rd edition (2005) - Peter Read ]
* ''Gemmology'' 3rd edition (2005) - Peter Read
 
 
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'''Next:[[Symmetry| Symmetry]]'''
 
'''Next:[[Symmetry| Symmetry]]'''
 
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'''[[Table_Of_Contents| Return to the Table of Contents]]'''
 
'''[[Table_Of_Contents| Return to the Table of Contents]]'''

Revision as of 14:37, 1 June 2009


Basic

Imaginary crystal, prismatic with pyramidal/pedial terminations


The habit of the mineral is defined by the shape in which it will usually occur in nature. Contrary to form, these are not always ideal shapes, although some might be.

When we name habits, we change the suffix of the forms that make up the habit. For example, when the mineral has the form of an octahedron (as many diamonds have), we name the habit "octahederal".

When a mineral is made up of different forms, we name the habit accordingly. In the image on the right, the mineral exhibits 3 different forms (a prism, two pyramids and a pedion). We name the habit "prismatic with pyramidal and pedial terminations".

There are many different types of habit that may have their own specific names:

Botryoidal formation of malachite
  • Acicular
  • Bipyramidal
  • Botroyidal (or globular)
  • Columnar (or fibrous)
  • Dentritic
  • Dodecahedral
  • Euhedral
  • Mamillary
  • Massive
  • Octahedral
  • Prismatic
  • Scalenohedral
  • Striations
  • Tabular

Related topics

Sources

Gemmology 3rd edition (2005) - Peter Read
Next: Symmetry

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