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ITEM: 1041 MICROLINE, DIOPSIDE, SPHALERITE AND CALCITE



For Sale by owner

Description:        

We are using 9w short wave UV light Fluoresce

Color under Short wave UV light

SHORT WAVE UV COLOR

Fluorescent Mineal

GREEN

WILLEMITE

BRIGHT-ORANGE

CLINOHEDRITE

BLUE

HYDROZINCITE; DIOPSIDE

POWER BLUE

MICROCLINE

VIOLET OR PURPLE

HARDYSTONITE

PALE YELLOW TO BLUE

SHEELITE

ORANGE-YELLOW & BLUE

SPHALERITE (best under long wave)

RED/PINK/ORANGE-RED

CALCITE

Non Fluorescent Minerals

Non-fluorescent minerals like Zincite (Zinc Oxide), and Franklinite (Zinc Iron Manganese Oxide). Both minerals are rare and inconspicuous at all but one general site. That site is the famous zinc and manganese mines of the Sterling Hill and Franklin, New Jersey in USA. 

Why do minerals fluoresce?

Energy from the UV light disrupts the moving structure of the electrons in the minerals' atoms.

As the electrons try to reorient themselves, they release energy we can see as visible light.

The mineral emits it's own light and not merely reflect it. Some minerals continue emitting light for few seconds to minutes when the UV light is shut off, this is called phosphorescence. This occurs when the electrons take longer to stabilize in their orbits.




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