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Kettle holes are relatively common features of glaciated landscapes and have been widely reported in the literature. The work reported here documents the presence of kettle holes at high altitude and low latitude in the Central Apennines (Italy) and describes the geomorphic and pedogenic processes that originated the soils infilling these depressions. The areas selected for this study were located...
Volcano flanks are usually covered by deposits of fine materials (tephra) with variable thickness originated by the explosive activity. The deposits form bedded sequences of tephra layers often alternated with paleosols. Pyroclastic successions on Etna volcano (Italy) are composed of scoria or pumice lapilli and ash deposits, representing separate eruptions, and volcanogenic sediments developed between...
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