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It has an origin thermal magma, that at temperatures of formation fluids below 100 ° C. Is formed near of volcanoes, it is in a quiescent state that next to extinction (that volcanoes virtually extinct or nearly so), principally of deep thermal water veins to less than 100 degrees Celsius rich in minerals and cold superficial magma veins
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Details
- Title: CINNABAR
- Date Created: 2015
- Location: Abbadia San Salvatore mine
- Publisher: Lucia franceschelli
- Rights: Associazione Minatori pre il museo
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