Ross Embayment

E282079

Ross Embayment is a large, ice-filled embayment in Antarctica that forms part of the Ross Sea and is closely linked to major tectonic and glacial processes in the West Antarctic region.

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All labels observed (1)

Label Occurrences
Ross Embayment canonical 1

Statements (48)

Predicate Object
instanceOf embayment
geographical feature
glacial-tectonic system
age Cenozoic
associatedWith Ross Ice Shelf
West Antarctic Rift System
glacial processes
ice-sheet dynamics
tectonic extension
borderedBy Marie Byrd Land
Transantarctic Mountains
climateRole modulates ice discharge from West Antarctic Ice Sheet
connectedTo Southern Ocean
contains glaciomarine sediments
marine sediments
thick sedimentary sequences
countryClaim Ross Dependency
filledWith ice
formedBy crustal thinning
glacial erosion
rifting
governedBy Antarctic Treaty System
hasFeature fault-bounded troughs
subglacial basins
volcanic centers
hasIceShelf Ross Ice Shelf
hasPart Ross Ice Shelf
continental shelf
deep marine basin
iceCover permanent
importantFor ice-sheet modeling
sea-level change reconstructions
understanding Antarctic glaciation history
influences West Antarctic Ice Sheet stability
linkedTo Amundsen Sea Embayment via West Antarctic Ice Sheet
locatedIn Antarctica
West Antarctica
namedAfter James Clark Ross
near McMurdo Sound
Ross Island
oceanBasin Pacific sector of Southern Ocean
partOf Ross Sea
researchFocus ice-sheet retreat and advance cycles
tectonic-glacial interactions
studiedBy drilling programs
marine geophysics
seismic reflection surveys
tectonicSetting back-arc or rifted margin

Referenced by (1)

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