Mount Somma caldera rim

E315336

The Mount Somma caldera rim is the semicircular mountainous ridge encircling Mount Vesuvius, formed by the remnants of an older, larger volcano that collapsed in a prehistoric eruption.

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All labels observed (1)

Label Occurrences
Mount Somma caldera rim canonical 1

Statements (40)

Predicate Object
instanceOf caldera rim
mountain ridge
volcanic landform
composition volcanic rocks
country Italy
elevationRelativeTo higher than Vesuvius crater rim in places
encircles Vesuvius
surface form: Mount Vesuvius
formedBy caldera-forming eruption
forms semicircular ridge
formsBoundaryOf Somma caldera
geologicalAge prehistoric
hasFeature eroded outer flanks
steep inner slopes
hasHighestPoint Punta Nasone
hasScientificName Somma caldera rim
hasVegetation Mediterranean scrub
woodlands
isExampleOf nested caldera-cone structure
isImportantFor geomorphological research
volcanological studies
isOlderThan current Vesuvius cone
isPartOf Vesuvius National Park
surface form: Somma-Vesuvius National Park
isRemnantOf older Somma volcano
isSeparatedFrom Vesuvius cone by Atrio del Cavallo
isTypeOf stratovolcano remnant
isVisibleFrom Metropolitan City of Naples
surface form: Naples metropolitan area
locatedIn Campania
Italy
locatedNear Naples
near Ottaviano
San Sebastiano al Vesuvio
Vesuvius
surface form: Somma Vesuviana
originatedFrom collapse of a prehistoric volcano
overlooks Gulf of Naples
surface form: Bay of Naples

Vesuvius crater
partOf Vesuvius
surface form: Mount Somma–Vesuvius volcanic complex
surrounds younger cone of Vesuvius
survived AD 79 eruption of Vesuvius
usedFor hiking
scientific excursions

Referenced by (1)

Full triples — surface form annotated when it differs from this entity's canonical label.

Vesuvius hasFeature Mount Somma caldera rim