Phyllosilicate-bearing Trough Latitude/longitude: -4.72 North, 137.40 East Rationale: The phyllosilicates exposed here may be lacustrine sediments. Morphology.
Mound-Skirting Unit Outcrop and Inverted Channel Latitude/longitude: -4.75 North, 137.38 East Rationale: This outcrop may be an alluvial fan or part of.
Crater Floor Stratigraphy Latitude/longitude: -4.57 North, 137.31 East Rationale: Several crater floor units are exposed in close proximity to each other.
Erosion-resistant Polygonal Ridges Latitude/longitude: -4.80 North, 137.38 East Rationale: These features are widespread in Gale crater and may be cemented.
Phyllosilicate-bearing outcrop within the Eberswalde Crater landing ellipse Latitude/longitude: -23.824 North, 326.675 East Rationale: This brecciated,
Light-Toned Ridge Latitude/longitude: -4.72 North, 137.39 East Rationale: A prominent part of the stratigraphy of the Gale mound, containing phyllosilicates.
