West Antarctic Rift System

E58285

The West Antarctic Rift System is a major tectonic rift zone underlying much of West Antarctica, characterized by crustal extension, volcanism, and significant influence on the region’s topography and ice sheet dynamics.


Statements (48)
Predicate Object
instanceOf geological structure
intraplate rift
tectonic rift system
affects basal melting of West Antarctic Ice Sheet
ice stream flow patterns
associatedWith Amundsen Sea Embayment
Cenozoic alkaline volcanism
Marie Byrd Land
Ross Embayment
Ross Sea
Transantarctic Mountains uplift
intraplate volcanism
tectonic subsidence
characterizedBy crustal extension
normal faulting
thin continental crust
volcanism
contains Executive Committee Range
Marie Byrd Land volcanic province
Mount Erebus volcanic system vicinity
contrastsWith East Antarctic craton
discoveredBy geophysical investigations in the 20th century
extendsBeneath West Antarctic Ice Sheet
forms major part of West Antarctic tectonic province
geologicalAge Mesozoic-Cenozoic
hasCrustalThickness significantly thinned relative to East Antarctica
hasTectonicSetting extensional tectonics
heatFlow elevated relative to East Antarctica
influences West Antarctic Ice Sheet dynamics
West Antarctic topography
ice sheet basal conditions
length over 3000 kilometers (approximate)
locatedIn West Antarctica
locatedOnContinent Antarctica
orientation roughly east–west to northwest–southeast in segments
partOf West Antarctic plate region
relatedTo breakup of Gondwana
opening of the Ross Sea
separation of New Zealand from Antarctica
relevantTo Antarctic ice sheet stability studies
geodynamic modeling of Antarctica
sea-level rise projections
riftingActiveDuring Cenozoic era
riftingInitiated Mesozoic era
studiedBy aeromagnetic surveys
gravity surveys
radar sounding beneath ice
seismic tomography

Referenced by (3)

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