Indus submarine fan

E360263

The Indus submarine fan is one of the world’s largest deep-sea sedimentary fans, formed by sediments carried from the Indus River into the Arabian Sea.

All labels observed (1)

Label Occurrences
Indus submarine fan canonical 1

How this entity was disambiguated

Statements (47)

Predicate Object
instanceOf deep-sea sedimentary fan ⓘ
submarine fan ⓘ
age primarily Neogene to Quaternary ⓘ
associatedWith Indus River delta ⓘ
Indus submarine canyon ⓘ
composedOf clay ⓘ
sand ⓘ
silt ⓘ
terrigenous sediments ⓘ
depositedOn oceanic crust of the Arabian Sea ⓘ
drains sediment from the Hindu Kush ⓘ
sediment from the Karakoram ⓘ
sediment from the western Himalaya ⓘ
environment deep-marine ⓘ
extendsFrom Indus submarine canyon ⓘ
fedBy Indus River ⓘ
formedBy sediment transported by the Indus River ⓘ
turbidity currents ⓘ
formedDuring Cenozoic ⓘ
growthLinkedTo Indian–Eurasian plate collision ⓘ
linked to: Himalayan orogeny

erosion of the Himalaya ⓘ
uplift of the Himalaya ⓘ
hasPart channel-levee systems ⓘ
distal lobes ⓘ
levees ⓘ
overbank deposits ⓘ
submarine channels ⓘ
importantFor paleoclimate reconstruction ⓘ
paleoseismic studies ⓘ
petroleum geology ⓘ
recording Himalayan erosion history ⓘ
locatedIn Arabian Sea ⓘ
northern Indian Ocean ⓘ
oneOf largest sedimentary fans on Earth ⓘ
partOf Indus River system ⓘ
linked to: Indus River
records monsoon variability in South Asia ⓘ
tectonic activity in the Himalayan region ⓘ
sedimentSource Himalayan foreland basin ⓘ
Indus River catchment ⓘ
linked to: Indus River basin

Karakoram ranges ⓘ
linked to: Karakoram
studiedBy marine geologists ⓘ
oceanographers ⓘ
sedimentologists ⓘ
terminatesNear Owen Ridge region of the Arabian Sea ⓘ
linked to: Arabian Sea
transportProcess gravity-driven flows ⓘ
submarine mass flows ⓘ
turbidite deposition ⓘ

How these facts were elicited

Referenced by (1)

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

Murray Ridge region → nearbyFeature → Indus submarine fan ⓘ