Bryson
Burke Diamond Corporation
© 2001 - 2003

BRYSON BURKE
Home
Mission
Board
History
Business Plan
Latest Information
Building Our Drill
Innovation
Photo Album
Satellite Weather
Free News - Sign Guestbook
INVESTING
Investment
Stock
Quotes
COMMUNICATION
Press Releases
Newsletter
Current Information
Contact
SITE GEOLOGY
Geology Reports
Site
Geologic History
Magnetic
Maps Index
Heavy
Minerals Index
Grenville Province Index
DIAMOND POLITICS
Blood Diamonds
Kimberley Process
DIAMOND GEOLOGY
Indicator
Minerals
Kimberlites
Decay
of Kimberlites
Kimberlites
& Magnetics
Placer Deposits
Magnetic Reversal
Crustal Thickness
How Diamonds are
Made
Glaciation Issues
Mineral Transport Index
Doing the Map Work
Gathering Samples
World Mining Index
Excavation
and Recovery
Mining Corporations
Mining News Magazines
Environmental Issues
Diamonds in Space
World's
Only MineCam
Live Volcano
Geo-Cams
EXPLORATION
Site Exploration
History
Topography
Map Index
Location
Map
Claim Maps
Index
DIAMONDS
Diamonds and Graphite
Diamond Formation
Grading Diamonds
Price of Diamonds
Industrial
Diamonds
Drilling
Equipment
Medical Use of Diamonds
Gemstones
Birthstones
Hall of Fame
DIAMONDS
IN CULTURE
Good Books
on Diamonds
Cremains to Diamonds
Diamonds in Lawsuits
Irish Diamonds
Unusual
Diamond News
Diamonds in the
Media
Famous Jewelers
In Advertisements
Top
Twenty Cut Diamonds
Top
Diamonds
Diamond Lore
Theft/Hoaxes/and Fraud
Religion Index
Diamond/
Culture Index
Television
Movies
Games
- Play Now
Music
Weddings
Royals
Our Darlings
Diamond
Animal Index
INTERACTIVE
Reflection/Refraction Index
Crossword
Puzzle Index
Which Is A Diamond
I
Which is a Diamond II
Become a Gemologist





| Mineral | Formula |
| acmite | NaFeSi2O6 |
| aegirine-augite | (Na2,Ca)(MgFe+2Fe+3)Si2O6 |
| diopside | CaMgSi2O6 |
| enstatite | MgSiO3 |
| fassaite | Ca(MgAl)(AlSi)O6 |
| jadeite | NaAlSi2O6 |
| spodumene | LiAlSi2O6 |
| Tschermak's pyroxene | CaAl(AlSi)O6 |
| ureyite | NaCrSi2O6 |
Pyroxene Library at Amethyst Gallery
The pyroxenes are an important group among the single chained inosilicates. They are common rock forming minerals and are represented in most igneous and many metamorphic rocks.
Their presence in a rock indicate a high temperature of crystallization with a lack of water. If water were present, a double chained amphibole would most likely have formed instead.
The name pyroxene comes from the Greek words for fire and stranger in a false allusion to their surprising presence in volcanic lavas.
Pyroxenes are sometimes seen as crystals embedded in volcanic glass and the assumption was that they are impurities in the glass, hence the term "fire strangers". However the pyroxenes are simply early forming minerals that crystallized before the lava erupted.