
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 class | Carbonates : Calcite group. |
| Chemical formula | CaCO3 |
| Crystal system | Trigonal. |
| Habitus
|
Calcite is the mineral that shows the most types of crystals (600). Most common forms are tabular, sharp and stubby rhomboedric, prismatic an scalenoedric (dogtooth spar). Calcite also occur as fibric aggregates and coarse to fine grained aggregates or stalactitic. |
| Cleavage | Perfect rhomboedric in three planes, subconchoidal fracture. |
| Hardness | 3 |
| Density | 2.7 |
| Color
| usually colorless, but nuances in blue, yellow, green, red, violet, even black and opaque. |
| Streak | White to grayish. |
| Luster | Vitreous to pearly or dull. |
| Occurance
| Calcite is the main ingredient of limestone and is found in stalagmites and stalagtites in caves. Calcite is common in hytdrothermal veins and can also occur in eruptive rocks (at depth, it isn't stable at athmospheric pressure - as a melt). |
| Notes
|
Reacts violently with hydrochloric acid. Double refractive. Clear calcite is called Iceland spar. Often flourescent when contaminated by manganeese. |
Uses
| The
limestone form of calcite has been extensively used since ancient times. It is
burned to quicklime (CaO), slaked to hydrated lime [Ca(OH)2] and mixed with sand
to make mortar. Limestone is one of the primary ingredients in the manufacture
of portland cement. It is employed in metallurgical processes and as aggregate
for both concrete and asphalt mixes. Marble has long been used for statuary and carvings, and as polished slabs for facing stone. Travertine is also a favorite interior facing stone, usually for interior use. Iceland Spar, a transparent form, has been used for optical and crystallography research for two centuries. |
| Locations
|
Crystals of calcite is also common, for example at
|




