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SOLFATARA , a volcanic vent emitting vapours chiefly of sulphurous character, whence the name, from theSee also: Italian solfo (See also: sulphur)
.
The typical example is the famous Solfatara, near Puzzuoli, in the Phlegraean See also: Fields, west of Naples
.
This is an old See also: crater which has not been in active eruption since A.D
.
1198, but which is continuously exhaling heated vapours, chiefly hydrogen sulphide, sulphur dioxide and steam
.
These issue from orifices in the crust, on the walls of which are yellow incrustations of sublimed sulphur, sometimes orange-red by association with arsenic sulphide, whilst the trachytic rocks of the See also: volcano are bleached and corroded by the effluent vapours, with formation of such products as See also: gypsum and See also: alum
.
Sal ammoniac occurs among the sublimates
.
The See also: term solfatara has been extended to all dormant volcanoes of this type; and a
' volcano which has ceased to emit See also: lava or ashes but still evolves heated vapours, is said to have passed into the " solfataric stage." Examples are to be found in many. volcanic districts
.
By French geologists the term soufriere is used instead of the Italian solfatara
.
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