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.

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All labels observed (1)

Label Occurrences
Indus submarine fan canonical 1

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 Himalayan orogeny
surface form: Indian–Eurasian plate collision

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
surface form: Indus River system
records monsoon variability in South Asia
tectonic activity in the Himalayan region
sedimentSource Himalayan foreland basin
Indus River basin
surface form: Indus River catchment

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

Referenced by (1)

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

Murray Ridge region nearbyFeature Indus submarine fan