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 |
Statements (33)
| Predicate | Object |
|---|---|
| instanceOf |
Martian valley
ⓘ
paleoriver channel ⓘ valley system on Mars ⓘ |
| associatedWith |
Jezero Crater delta
ⓘ
Jezero Crater ⓘ
surface form:
Jezero Crater paleolake
|
| 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 NERFINISHED ⓘ |
| nameOrigin | Earth river in the Balkans ⓘ |
| observedBy |
Mars Global Surveyor
ⓘ
Mars Reconnaissance Orbiter ⓘ |
| partOf | Jezero Crater watershed ⓘ |
| relatedToMission |
Perseverance rover
ⓘ
surface form:
Mars 2020 Perseverance rover
|
| studiedInContextOf | NASA Perseverance rover landing site selection ⓘ |
| surfaceProcess | water-driven erosion ⓘ |
Referenced by (1)
Full triples — surface form annotated when it differs from this entity's canonical label.