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Mamma
Etna's countless children |
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Hikers
descending on the crest of the Northeast Rift of Etna from Monte Pizzillo
and the 1879 craters to Monte Timparossa have the chance to see numerous
older and younger crater. Among the most spectacular of these is a group
of three aligned craters surrounded by low pyroclastic rims that lie about
halfway between Monte Pizzillo and Monte Timparossa. The date of the eruption
that produced these craters is not known, but they appear quite youthful
and furthermore lie on the same trend as the 1879 fissure system, so that
it cannot be excluded that they formed during the same eruption. A low
hill (not a pyroclastic cone) near the middle crater in this cluster bears
the name Monte Cacciatore, and therefore I call these craters "the
craters of Monte Cacciatore" here. All three craters are elongate
in NNE-SSW direction (that is, the trend of the Northeast Rift) and have
very similar diameters, 100 x 130 m. |
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Copyright © Boris Behncke, "Italy's Volcanoes: The Cradle of Volcanology" |
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Page set up on 23 February 2004 |