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Mamma
Etna's countless children |
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While
many flank eruptions of Mount Etna produce sizeable pyroclastic cones
(the result of strong explosive activity), others have very low degrees
of explosivity and no pyroclastic cones of appreciable dimensions are
formed. But even these low-explosivity eruptions can produce huge amounts
of lava, as was impressively shown during the 1991-1993 eruption in the
Valle del Bove. During their initial stages, mild degassing at the eruptive
vents produces small bursts of liquid spatter that fall down immediately
next to the vents and build small edifices that are generally known as
hornitos (the Spanish word for "little ovens") or spatter cones.
A spectacular row of spatter cones was built at the eruptive fissure of
a voluminous eruption that occurred on the SSE flank of Etna in 1634-1638,
on the southern outer slope of the Valle del Bove. These are still very
well preserved, and a footpath leading up to the rim of the Valle del
Bove passes nearby. There are about 15 distinct spatter cones of different
size and shape, ranging from very small mounds about 1 m high to broad
rings of agglutinated (welded) spatter with diameters of up to 10 m and
heights of 5-8 m. |
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Copyright © Boris Behncke, "Italy's Volcanoes: The Cradle of Volcanology" |
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Page set up on 12 March 2004 |