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Geological Formation

Pietra di Bismantova

Inselbergs and Crystalline Monoliths

Pietra di Bismantova is an isolated tabletop massif in the Reggio Emilia Apennines of northern Italy, a narrow plateau roughly a kilometer long and 240 meters wide, ringed by cliffs some 300 meters high and reaching an elevation of 1,047 meters. It is built from yellowish calcarenite over a marl base, both laid down as sediment on the floor of a warm Miocene sea that once covered the area, later uplifted and left standing as a steep-sided monadnock once the softer surrounding rock wore away. The formation, believed by many scholars to have inspired a passage in Dante's Purgatorio, sits within the Tuscan-Emilian Apennine National Park.

Facts
Classification
Protected Status
National Park or Reserve 1
Connections

Caused By

Orogeny, Processes

Wikidata P31 formation-type mapped to formative process Orogeny via reviewed judgment map (earth atlas); source citation is this entity's own cited Wikidata item.

Source Wikidata: Pietra di Bismantova

In Discipline

Wikidata P31 formation-type mapped to discipline Geomorphology via reviewed judgment map (earth atlas); source citation is this entity's own cited Wikidata item.

Source Wikidata: Pietra di Bismantova
In the Other Atlases

Found In

Also in Geography Atlas: where this subject is found.

Source Wikidata: Pietra di Bismantova
Sources
1. Pietra di Bismantova (Wikipedia)
Wikipedia article lead, protection designation
Quote, Wikipedia article lead, protection designation
an elevation of 1,047 metres (3,435 ft) above sea level. It is included in the National Park of the Appennino Tosco-Emiliano.
View the Source
Wikidata: Pietra di Bismantova
Wikidata Q510076, class allow-list match (w-wdresolver-0926)View the Source
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