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Pietra di Bismantova : ウィキペディア英語版 | Pietra di Bismantova
The Pietra di Bismantova is a geological formation in the Reggiano Apennines, in the ''comune'' of Castelnovo ne' Monti, province of Reggio Emilia, central Italy, c. 45 km from Reggio Emilia. It has the shape of a narrow, quasi-cylindrical plateau (measuring 1 km x 240 m) whose steep walls emerge c. 300 m as an isolated spur from the nearby hills. The top has an elevation of 1,047 m above sea level. It is included in the National Park of the Appennino Tosco-Emiliano. The spur is composed of yellowish calcarenite over a marl basement, all formed in the Miocene as a sea bottom. It includes fossils belonging to a tropical environment. It is surrounded by woods, mostly of hazel trees (''Corylus avellana''). The Pietra di Bismantova is mentioned by Dante Alighieri in his ''Divine Comedy'' (Purgatory, IV, 25-30). ==See also==
*Monadnock
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