Lord Howe Trough

E440840

Lord Howe Trough is a deep submarine basin in the Tasman Sea, separating the Lord Howe Rise from the Australian mainland and forming part of the complex tectonic structure of the southwest Pacific Ocean floor.

All labels observed (1)

Label Occurrences
Lord Howe Trough canonical 1

How this entity was disambiguated

Statements (36)

Predicate Object
instanceOf oceanic basin ⓘ
submarine trough ⓘ
adjacentTo Australian mainland ⓘ
Lord Howe Rise ⓘ
age Mesozoic–Cenozoic ⓘ
boundedBy Australian continental slope to the west ⓘ
Lord Howe Rise to the east ⓘ
linked to: Lord Howe Rise
contains thick sedimentary sequences ⓘ
countryOffshoreFrom Australia ⓘ
floorType deep-sea basin ⓘ
formedBy back-arc style extension ⓘ
continental rifting ⓘ
geologicalProvince Zealandia region ⓘ
geologicalSignificance key structure in evolution of Zealandia–Australia margin ⓘ
records rifting history of Tasman Sea ⓘ
hasFeature complex faulted morphology ⓘ
steep basin margins ⓘ
liesBetween eastern Australia and Lord Howe Rise ⓘ
locatedIn Tasman Sea ⓘ
maximumDepth over 3000 m ⓘ
namedAfter Lord Howe Island region ⓘ
linked to: Lord Howe Island
ocean Pacific Ocean ⓘ
orientation north–south ⓘ
partOf Australian plate margin ⓘ
Tasman Sea tectonic system ⓘ
linked to: Tasman Sea Basin

southwest Pacific Ocean floor ⓘ
region Southwest Pacific ⓘ
relatedTo Tasman Sea opening ⓘ
separation of Australia and Zealandia ⓘ
sedimentSource Australian continental margin ⓘ
Lord Howe Rise ⓘ
separates Australian continental margin ⓘ
Lord Howe Rise ⓘ
studiedIn marine geophysics ⓘ
plate tectonics research ⓘ
tectonicSetting extensional basin ⓘ

How these facts were elicited

Referenced by (1)

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

Lord Howe Rise → adjacentTo → Lord Howe Trough ⓘ