Formation of lava stalactites in the master tube of the 1792-1793 flow field, Mt Etna (Italy).

Lava tubes are often coated with spectacular lava stalactites that are thought to form by a process
of lava remelting. Here, we present results from lava stalactites collected inside a master lava tube
that fed the 1792−1793 Etna ß ank eruption, which show features rather different from their Hawaiian
or Icelandic counterparts. We analyzed three types of stalactites recognized at Mt. Etna on the
basis of their morphology, and compared their features with those of the lava ß ow hosting the tube.
Three-dimensional morphologic analyses by SEM, petrographic observations, and mineral and glass
composition measured by SEM-EDS, allowed us to infer processes and conditions of stalactite formation.
Our results indicate that in all the analyzed stalactites, the nature, abundance and composition of
phenocrysts is similar to that of the host lava ß ow. This Þ nding suggests a common mechanical origin
for different types of stalactites, caused by drainage of the tube and dripping of ß uid lava from the
roof. However, the composition of interstitial glass is signiÞ cantly different from that of the glassy
groundmass measured in historical volcanic rocks of Mt. Etna and suggests that, once stalactites solidi
Þ ed, they were affected by a process of partial melting. Partial melting involved between 12 and
25% of the bulk rock, causing the wide compositional variation and enrichment in K2O measured in
our samples.

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