Volcanic sublimate

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A volcanic sublimate or fumarolic sublimate is a mineral which forms directly from volcanic gases during an eruption or discharge from a volcanic vent or fumarole.[1] Native sulfur is a common sublimate mineral and various halides, sulfides and sulfates occur in this environment associated with fumaroles and eruptions.

References[edit]

  1. ^ Manahan, Stanley E. Environmental Chemistry, CRC Press, 2004, Eighth Edition, p. 408 ISBN 978-1566706339