Earth and Environment Atlas

How The Planet Works
Sign In
Text size
100%
Theme
Geological Formation

Valle Peligna

Structural and Tectonic Formations

Valle Peligna, also called Conca di Sulmona, is a plateau of about 100 square kilometers in central Abruzzo in southern Italy, in the province of L Aquila, named for the Paeligni, an Oscan speaking tribe who originally inhabited it. The plateau formed where a prehistoric lake once stood, drained roughly 300,000 years ago after seismic activity opened what is now the Popoli gorges, leaving marshland with rich soil behind. The Aterno and Sagittario rivers cross the valley, and its main towns are Sulmona, the largest, along with Raiano, Vittorito, Corfinio, Pratola Peligna, and Pacentro. This description is adapted from Wikipedia contributors under CC BY-SA 4.0; changes were made. https://creativecommons.org/licenses/by-sa/4.0/

Connections

Caused By

Erosion, Processes

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

Source Wikidata: Valle Peligna

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: Valle Peligna
In the Other Atlases

Found In

Also in Geography Atlas: where this subject is found.

Source Wikidata: Valle Peligna
Sources
Valle Peligna (Wikipedia)
Lead section
Quote, Lead section
The Valle Peligna, also known as Conca di Sulmona, is a plateau in central Abruzzo, southern Italy, included in the province of L'Aquila.
View the Source
Wikidata: Valle Peligna
Wikidata Q4008059, class allow-list match (w-wdresolver-0926)View the Source
Comments (0)
No comments yet. Be the first to share a thought.
Reader Challenges (0)
No disputes yet. Spotted an error or a better source? Open the first one.