Non-Hidden Crystal Gems Gemsonas/Copiapite

Copiapite was a Crystal Gem, who participated in the Great War, until she was destroyed by Magenta Agate, and is an original character created by White diamond 777 and Kosmochlor jade 13325. BlueWhiteLight has made a fusion involving her.

Appearance
She had dark orange skin, orange khaki hair, vermilion red shirt with a star in the middle, had a dark orange miniskirt almost black, and sienna-colored toenail gloves, and red crimson boots.

Personality
Copiapite is described as very shy and not socialising much with the other gems, but had tries to help the rebellion.

Abilities
Copiapite possesses standard Gem abilities including bubbling, shapeshifting, fusion, regeneration, agelessness and superhuman strength/durability.

Fusions with Fanon Gems

 * When fused with Turquoise, they form Amesite.

Trivia

 * BlueWhiteLight felt sorry for Copiapite that she got shattered.
 * This prompted him to make a fusion involving her.

Gemology

 * Copiapite is a hydrated iron sulfate mineral with formula: Fe2+(Fe3+)4(SO4)6(OH)2·20H2O Copiapite can also refer to a mineral group, the copiapite group.
 * Copiapite is strictly a secondary mineral forming from the weathering or oxidation of iron sulfide minerals or sulfide-rich coal. Its most common occurrence is as the end member mineral from the rapid oxidation of pyrite. It also occurs rarely with fumaroles. It occurswith melanterite, alunogen, fibroferrite, halotrichite, botryogen, butlerite and amarantite.It is by far the most common mineral in the copiapite group.


 * It rarely occurs as single crystals, is in the triclinic crystal system, and is pale to bright yellow. It is soluble in water, changing the water color to deep orange or orangish-red. In solution copiapite is very acidic. In high concentrations a negative pH can occur, as reported in waters draining from Richmond Mine at Iron Mountain, California.Copiapite can easily be distinguished from native sulfur because it does not give off an odor when dissolved in water. It can be distinguished from similar appearing uranium minerals, such as carnotite, by its lack of radioactivity. The only way to differentiate between the minerals in the copiapite group is by X-ray diffraction.
 * Copiapite was first described in 1833 for an occurrence near Copiapó, Atacama, Chile.It is sometimes known as yellow copperas. Other occurrences are in California, Nevada, and in the filled paleo sinkholes and caves of Missouri.