About
Vivianite is notorious for darkening upon exposure to light. This is caused by a chemical transformation of the iron which is responsible for its color deepening and decrease of transparency. Continued exposure may eventually turn a specimen black and make it completely opaque. Certain specimens may also be unstable and form cracks along cleavage surfaces when exposed to light. Due to its instability, it is recommended to keep all Vivianite specimens covered and out of any light except for the short periods of time when it is being looked at.
Vivianite is named in honor of John Henry Vivian (1785 - 1855), an English mineralogist and mine owner who first discovered this mineral in Cornwall.
Crystal Forms & Aggregates
Other ID Marks
Striking Features
Environment
Varieties
✓ common · ✗ uncommon
Uses
Noteworthy Localities
The Kerch peninsula, Crimea, Ukraine, is well known for exceptional Vivianite crystal sprays in fossilized shells. Sharp dark coxcomb balls came Berstadt, Wetterau, Hesse, Germany. Dark transparent green Vivianite crystal clusters come from several pegmatites in Minas Gerais, Brazil, especially Cigana, Conselheiro Pena, in the Doce valley. In Mexico, sharp crystals came from Santa Eulalia, Chihuahua.
In the U.S., large Vivianite crystals, including a rare violet and multicolored variety, came from the Blackbird District, Lemhi Co., Idaho. An old classic locality is Leadville, Lake Co., Colorado; as well as a built-over area in downtown Richmond, Henrico Co., Virginia. Vivianite associated with organic material comes from Mullica Hill, Gloucester Co., New Jersey; and light blue microcrystals come from the Palermo No. 1 Mine, Groton, Grafton Co., New Hampshire.
Common Mineral Associations
Distinguishing Similar Minerals
Photos
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