Apennine orogeny

E557625

The Apennine orogeny is the mountain-building event responsible for forming Italy’s Apennine Mountains through the collision and complex interaction of the African and Eurasian tectonic plates.

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All labels observed (1)

Label Occurrences
Apennine orogeny canonical 4

Statements (45)

Predicate Object
instanceOf geological process
mountain-building event
orogeny
activeDuring Miocene
Pliocene
Quaternary
associatedWith Adriatic microplate NERFINISHED
Mediterranean region NERFINISHED
Tyrrhenian Sea back-arc basin NERFINISHED
extensional tectonics in the Tyrrhenian side
foreland basin development along the Adriatic side
causes earthquakes in central Italy
mountain uplift rates in the Apennines
seismic activity in the Apennines
drivenBy convergence of the African and Eurasian tectonic plates
formed Apennine Mountains NERFINISHED
geologicalAge Cenozoic
hasConsequence geomorphological evolution of the Italian Peninsula
landslide susceptibility in the Apennine region
hasEffect formation of the Apennine Mountains
hasRegion Central Apennines NERFINISHED
Northern Apennines NERFINISHED
Southern Apennines NERFINISHED
influences drainage patterns in Italy
topography of the Italian Peninsula
involvesProcess collision
crustal shortening
folding
subduction
thrust faulting
uplift
occursIn Italy NERFINISHED
partOf Alpine orogenic system NERFINISHED
relatedTo African Plate NERFINISHED
Alpine orogeny
Eurasian Plate NERFINISHED
resultsIn crustal thickening beneath the Apennines
exhumation of metamorphic rocks
formation of fold-and-thrust belts
startedIn Neogene NERFINISHED
stillActive true
studiedInDiscipline geology of Italy
structural geology
tectonics
tectonicSetting convergent plate boundary

Referenced by (4)

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

Marsili Basin linkedTo Apennine orogeny
Sabine Mountains orogeny Apennine orogeny
Tuscan-Romagnol Apennines orogeny Apennine orogeny