Neretva Vallis

E416934

Neretva Vallis is an ancient Martian valley system interpreted as a former river channel that once fed water into Jezero Crater, the landing site of NASA’s Perseverance rover.

All labels observed (1)

Label Occurrences
Neretva Vallis canonical 1

How this entity was disambiguated

Statements (33)

Predicate Object
instanceOf Martian valley ⓘ
paleoriver channel ⓘ
valley system on Mars ⓘ
associatedWith Jezero Crater delta ⓘ
Jezero Crater paleolake ⓘ
linked to: Jezero Crater
connectedTo Jezero Crater ⓘ
considered major inlet system to Jezero Crater ⓘ
evidenceFor ancient Martian hydrologic activity ⓘ
past surface water on Mars ⓘ
feedsInto Jezero Crater ⓘ
formedBy fluvial erosion ⓘ
geomorphologicalType branching channel system ⓘ
sinuous valley ⓘ
hasRelevanceFor reconstruction of ancient Martian drainage networks ⓘ
search for past life on Mars ⓘ
hasRole inlet valley to Jezero Crater ⓘ
hasScientificInterest Martian climate history ⓘ
astrobiology ⓘ
sedimentology ⓘ
indicates long-lived fluvial activity ⓘ
potential ancient lake in Jezero Crater ⓘ
interpretedAs former river channel ⓘ
locatedOn Mars ⓘ
mappedUsing digital elevation models ⓘ
orbital imagery ⓘ
namedAfter Neretva River ⓘ
linked to: Neretva
nameOrigin Earth river in the Balkans ⓘ
observedBy Mars Global Surveyor ⓘ
Mars Reconnaissance Orbiter ⓘ
partOf Jezero Crater watershed ⓘ
relatedToMission Mars 2020 Perseverance rover ⓘ
linked to: Perseverance rover
studiedInContextOf NASA Perseverance rover landing site selection ⓘ
surfaceProcess water-driven erosion ⓘ

How these facts were elicited

Referenced by (1)

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

Jezero Crater → hasInflowChannels → Neretva Vallis ⓘ