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(obsolete,geology) Flowing mud associated with a volcaniceruption (especially in South America), formed when snow or a lake near a volcano is disrupted, or when rain or steam mixes with soil or ash during an eruption.
1832, Samuel Hibbert, History of the Extinct Volcanos of the Basin of Neuwied, on the Lower Rhine, page 40:
These are the principal tufas indicative of the boiling tufaceous mud, or moya, which once filled, even to an overflow, the valley of Rieden.