Oxia Planum

E1021661

Oxia Planum is a region on Mars characterized by ancient, clay-rich terrains that make it a prime site for investigating past habitability and the potential for preserved biosignatures.

All labels observed (1)

Label Occurrences
Oxia Planum canonical 2

How this entity was disambiguated

Statements (49)

Predicate Object
instanceOf Martian plain
geological region on Mars
characterizedBy ancient terrains
clay-rich deposits
layered sedimentary units
low-relief topography
phyllosilicate-bearing rocks
considered prime site for investigating past habitability
prime site for searching preserved biosignatures
contains Fe/Mg-smectite clays
deltaic or fan-like deposits
hydrated minerals
phyllosilicates
valley networks
coordinateSystem planetocentric
elevationRelativeToDatum low-lying region
geologicalContext transition between highlands and lowlands
hasApproximateLatitude 18°N
hasApproximateLongitude 335°E
hasEvidenceFor aqueous alteration
long-lived water activity
past habitable conditions
hasSurfaceAgeEstimate >3.8 billion years
hostMission ExoMars Rosalind Franklin rover (planned)
investigatedBy CRISM spectrometer
linked to: CRISM instrument

Mars Express
Mars Reconnaissance Orbiter
OMEGA spectrometer
liesNear Chryse Planitia
Coogoon Valles
Mawrth Vallis
locatedInQuadrangle Margaritifer Sinus quadrangle
locatedOn Mars
planetaryProtectionCategory Category IVc (for ExoMars landing)
scientificInterest astrobiology
paleoclimate reconstruction
sedimentary processes on early Mars
selectedAs landing site for ExoMars Rosalind Franklin rover
selectedBy European Space Agency
Roscosmos
selectionReason ancient Noachian-aged surface
engineering safety for landing
high abundance of phyllosilicates
potential for preservation of organic material
spectralSignature strong phyllosilicate absorption bands
surfaceType dusty
rocky
terrainAge Hesperian
Noachian

How these facts were elicited

Referenced by (2)

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