Mediterranean Ridge region

E62375

The Mediterranean Ridge region is a vast underwater mountain and trench system in the eastern Mediterranean Sea, notable for containing the sea’s deepest point and marking the complex boundary between the African and Eurasian tectonic plates.

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Observed surface forms (1)

Surface form Occurrences
Mediterranean plate boundary zone 1

Statements (46)

Predicate Object
instanceOf submarine mountain range
tectonic plate boundary region
associatedWith seismic activity
slow plate convergence
contains Calypso Deep
deepest point of the Mediterranean Sea
countryOffshoreFrom Cyprus
Egypt
Greece
Libya
Turkey
dominantProcess crustal shortening
sediment accretion
thrust faulting
extendsFrom south of Crete
extendsTo towards the Hellenic Arc
towards the Levant Basin
formedBy subduction of African Plate beneath Eurasian Plate
geologicalAge Cenozoic
hasFeature accretionary wedge
deep-sea trenches
fold-and-thrust belt
underwater mountain chain
hasMorphology imbricated thrust sheets
ridge-and-trough topography
locatedIn Eastern Mediterranean
surface form: eastern Mediterranean Sea
maximumDepth about 5.2 km below sea level
about 5267 m
oceanographicSetting oligotrophic deep-sea environment
partOf Hellenic subduction system
Mediterranean Sea
plateConvergenceRate on the order of a few millimeters per year
relatedTo Hellenic Arc
Ionian Sea
researchInterest accretionary prism evolution
deep-sea ecosystems
subduction dynamics
sedimentSource African continental margin
Nile
surface form: Nile River system
separates African Plate
Eurasian Plate
studiedBy marine geologists
oceanographers
seismologists
tectonicSetting convergent plate boundary
subduction zone

Referenced by (2)

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

Aegean Sea Plate partOf Mediterranean Ridge region
this entity surface form: Mediterranean plate boundary zone
Calypso Deep partOf Mediterranean Ridge region