Central Lau Spreading Center

E718598

The Central Lau Spreading Center is a major seafloor spreading ridge in the southwestern Pacific where tectonic plates diverge and new oceanic crust forms within the Lau Basin back-arc region.

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Statements (45)

Predicate Object
instanceOf back-arc spreading ridge
seafloor spreading center
associatedWith Indo-Australian Plate NERFINISHED
Pacific Plate subduction
Tonga Trench NERFINISHED
Tonga subduction zone NERFINISHED
hydrothermal vent fields
submarine volcanic edifices
crustTypeFormed oceanic crust
environment deep-sea seafloor
geologicalFeature divergent plate boundary
spreading ridge
governedBy plate divergence
hasActivity active volcanism
frequent magmatism
hydrothermal venting
hasCrustalAge young oceanic crust
hasHazard hydrothermal plume emissions
submarine volcanic activity
hasMagmatismSource decompression melting
mantle upwelling
hasMorphology axial ridge
rifted spreading axis
hasOrientation approximately north–south trending axis
hasSpreadingType asymmetric back-arc spreading
isBackArcTo Tonga volcanic arc NERFINISHED
Tonga–Kermadec arc system
isBetween Eastern Lau Spreading Center NERFINISHED
Valu Fa Ridge NERFINISHED
isSegmentOf Lau spreading ridge system NERFINISHED
linkedTo arc–back-arc magmatic system
locatedIn Lau Basin NERFINISHED
Tonga–Lau back-arc region NERFINISHED
southwestern Pacific Ocean NERFINISHED
partOf Lau Basin spreading centers NERFINISHED
Lau back-arc spreading system NERFINISHED
process formation of new oceanic crust
seafloor spreading
researchInterest back-arc basin evolution
hydrothermal systems
plate tectonics
submarine volcanism
separates tectonic plates
tectonicSetting back-arc basin
convergent margin back-arc

Referenced by (1)

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

Lau Basin contains Central Lau Spreading Center