Corinth Rift

E397467

The Corinth Rift is an active continental rift zone in central Greece, known for its rapid extension, frequent earthquakes, and role in shaping the Gulf of Corinth region.

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All labels observed (1)

Label Occurrences
Corinth Rift canonical 1

Statements (48)

Predicate Object
instanceOf active tectonic zone
continental rift
geological structure
activityStatus active
age Quaternary activity
associatedWith Gulf of Corinth
controls morphology of the Gulf of Corinth
sedimentation in the Gulf of Corinth
country Greece
deformationStyle brittle crustal deformation
extendsBeneath Gulf of Corinth
geologicalProcess continental rifting
crustal extension
hasFaultType north-dipping normal faults
south-dipping normal faults
hasProcess earthquake clustering
fault segmentation
subsidence of the rift basin
uplift of rift shoulders
hazardType ground shaking
seismic hazard
surface faulting
influences coastal morphology of the Gulf of Corinth
landscape evolution of central Greece
isExampleOf active continental rift in the Mediterranean region
isKeySiteFor studies of continental breakup processes
studies of earthquake mechanics
knownFor dense geodetic monitoring
high strain rates
rapid extension rates
locatedIn Aegean region
central Greece
monitoredBy GPS networks
seismological networks
movementType normal faulting
partOf Hellenic subduction system
surface form: Hellenic plate boundary zone
region Gulf of Corinth
surface form: Gulf of Corinth region
relatedTo Hellenic subduction system
surface form: Hellenic subduction zone

subduction of the African Plate beneath the Eurasian Plate
seismicity frequent earthquakes
shapes Gulf of Corinth
studiedIn geodesy
neotectonics
seismology
structural geology
tectonicSetting back-arc extension
extensional
youngerThan Alpine orogeny structures in Greece

Referenced by (1)

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