|
gptkb:Eberswalde_Crater
|
channel bifurcations
|
|
gptkb:Eberswalde_Crater
|
oxbow lakes
|
|
gptkb:Eberswalde_Crater
|
sedimentary fans
|
|
gptkb:Eberswalde_Crater
|
evidence of standing water
|
|
gptkb:Eberswalde_Crater
|
evidence of habitability
|
|
gptkb:Eberswalde_Crater
|
deltaic deposits
|
|
gptkb:Eberswalde_Crater
|
potential biosignature preservation
|
|
gptkb:Eberswalde_Crater
|
layered sediments
|
|
gptkb:Eberswalde_Crater
|
evidence of delta progradation
|
|
gptkb:Eberswalde_Crater
|
meandering channels
|
|
gptkb:Eberswalde_Crater
|
evidence of ancient lake
|
|
gptkb:Eberswalde_Crater
|
potential for past life
|
|
gptkb:Eberswalde_Crater
|
evidence of hydrous minerals
|
|
gptkb:Eberswalde_Crater
|
evidence of fluvial processes
|
|
gptkb:Eberswalde_Crater
|
clay minerals
|
|
gptkb:Eberswalde_Crater
|
inverted channels
|
|
gptkb:Eberswalde_Crater
|
potential for organic material preservation
|
|
gptkb:Eberswalde_Crater
|
evidence of ancient Martian climate
|
|
gptkb:Eberswalde_Crater
|
evidence of clay formation
|
|
gptkb:Eberswalde_Crater
|
evidence of sediment transport
|