The Eastern Préalpes Southerners constitute a whole of the the Alps extending from the north of the Italy (Trentin-Haut-Adige) in the north of the Slovenia, while passing by the extreme south of the Austria (Carinthie).

They different from the the central Eastern Alps by their geological nature, namely that they are made up of Sedimentary rocks and not of crystalline rocks. Their tops are also less low.

The solid masses (of is in west) which constitute Préalpes Eastern Southerners are:

• Pohorje (German: Bachergebirge ) (1)

• the kamnic Alps or the Alps de Savinja (2)
• Karavanke (3)
• the Alps juliennes (4)
• the Alps de Gailtal (5)
• the carnic Alps (6)
• Préalpes carnic (7)
• Massive of the Dolomites (8)
• the Alps de Fiemme (9)
• Préalpes vicentines (10)
• Massive of Non (11)
• Massive of Brenta (12)
• Mountains around Lake Garda (13)
• Massive of Ortles (14)
• Massif of Adamello-Presanella (15)
• Massif of Sobretta-Gavia (16)

Related articles

• Geography of the Eastern Alps