Pliva Vallis

E424256

Pliva Vallis is an ancient Martian valley system interpreted as a former river channel that once drained water from Jezero Crater.

All labels observed (1)

Label Occurrences
Pliva Vallis canonical 1

How this entity was disambiguated

Statements (27)

Predicate Object
instanceOf Martian valley ⓘ
ancient river channel ⓘ
associatedWith Jezero Crater delta system ⓘ
linked to: Jezero Crater
connectedTo Jezero Crater ⓘ
considered potential former outflow channel from Jezero Crater ⓘ
drainsFrom Jezero Crater ⓘ
evidenceFor ancient Martian hydrologic activity ⓘ
past surface water on Mars ⓘ
formedBy fluvial erosion ⓘ
formedIn Martian past ⓘ
hasMorphology sinuous channel ⓘ
valley network ⓘ
hasScientificInterest record of Martian surface hydrology ⓘ
record of ancient Martian climate ⓘ
interpretedAs former river channel ⓘ
locatedOn Mars ⓘ
mentionedIn Mars fluvial geomorphology studies ⓘ
observedBy Mars Global Surveyor ⓘ
Mars Reconnaissance Orbiter ⓘ
observedUsing orbital imagery ⓘ
partOf Martian fluvial systems ⓘ
planetaryBody Mars ⓘ
relevantTo astrobiology on Mars ⓘ
paleolake in Jezero Crater ⓘ
studiedInContextOf Mars 2020 Perseverance rover landing site ⓘ
surfaceFeatureOf Martian highlands and lowlands transition region ⓘ
usedAs constraint on Jezero Crater paleolake level ⓘ

How these facts were elicited

Referenced by (1)

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

Jezero Crater → hasOutflowChannel → Pliva Vallis ⓘ