From: Cold-based glaciation of Pavonis Mons, Mars: evidence for moraine deposition during glacial advance
 | Number | Ridge width | X-sectional area | Ridge spacing |
---|---|---|---|---|
Extracted from CTX stereo DEM a | ||||
 All ridges | 26 | 660 ± 480 m | 9000 ± 12,500 m2 |  |
 Non-terminal ridges | 23 | 500 ± 210 m | 5200 ± 3800 m2 |  |
Extracted from CTX image mosaic | ||||
 Prominent, non-terminal ridges | 30 |  |  | 1.7 ± 1.3 km |
 Prominent + minor, non-terminal ridges | 42 |  |  | 1.3 ± 1.1 km |