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Phosphorescent Calcite on Dolomite
Description:
Phosphorescence of Calcite. A calcite crystal on dolomite from Penfield Quarry, Monroe County, New York. Dolomite, calcium magnesium carbonate, is a common mineral that occurs throughout the world. Thick beds of dolomite were produced by the alteration of limestones (made of calcite, calcium carbonate) by magnesium-rich hot solutions, a process called 'dolomitization'. Dolomite forms good crystals in veins in ore deposits. Crystals also occur in open spaces within massive dolomite beds. Dolomite and calcite typically form crystals with a characteristic rhomb shape. Here the sample is illuminated by visible light. Image #1 of 2 in a sequence.
Credit:
Ted Kinsman/Science Source
Unique identifier:
SS2708826
Legacy Identifier:
JC5940
Type:
Image
Size:
5760px × 3840px (~63 MB)
Fine Art America
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Tags
calcite
carbonates
crystal
crystals
dolomite
dolomitization
geology
limestone
mineral
mineralogy
minerals
phosphorescence
phosphorescent
photo
sequence
specimen
specimens