false coloured by Eric
Condliffe
The sample above is from a profile taken over
the active geothermal system in the Eastern Geothermal Field in the Uzon
Caldera, Kamchatka Penninsula, Russia. The sample was collected at~
35cm depth, and it was in contact with a fluids at ~ 65oC, pH
~ 5.4.
Similar structures are expected to exist in
many active arsenic sulphide forming environments (e.g., New Zealand, Japan)