Scotia Arc

E54355

The Scotia Arc is a geologically active, curved chain of undersea ridges and island arcs in the South Atlantic that forms the boundary between the South American and Antarctic tectonic plates.

Aliases (2)

Statements (47)
Predicate Object
instanceOf island arc system
submarine ridge system
tectonic feature
associatedWith active volcanism
oceanic crust deformation
seismic activity
borders Scotia Sea
extendsFrom Tierra del Fuego region
extendsTo South Sandwich Islands region
formedBy relative motion of South American Plate and Antarctic Plate
formsBoundaryBetween Antarctic Plate
South American Plate
geologicalAge Cenozoic
hasImportanceFor plate kinematic reconstructions in the South Atlantic–Antarctic region
hasMorphology arc-shaped chain of ridges and island arcs
hasPart Aurora Bank
Bruce Bank
Discovery Bank
North Scotia Ridge
Scotia Sea margins
Shackleton Fracture Zone
South Georgia microcontinent
South Orkney microcontinent
South Sandwich Arc
South Sandwich Trench
South Scotia Ridge
Terror Rise
influences Antarctic Circumpolar Current pathways
ocean circulation in the Southern Ocean
isCurved true
isGeologicallyActive true
isStudiedIn geophysics
marine geology
plate tectonics
isSubmerged mostly
locatedIn South Atlantic Ocean
near Antarctic Peninsula
Falkland Plateau
partOf Scotia Plate boundary zone
relatedTo Scotia Plate
South Sandwich Plate
separates Drake Passage region
South Atlantic Ocean basin
Weddell Sea region
tectonicSetting back-arc basin environment
convergent plate boundary
subduction zone system


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