The median of slopes in 35-km windows indicate the typical roughness on 300-meter baselines. The rougher nature of the heavily cratered terrain in the Southern Hemisphere is apparent, as well as that of Valles Marineris (12S, 289E) canyon walls and the Olympus Mons (18N, 227E) aureole deposits. The Northern Lowlands are smooth, especially Amazonis Planitia (16N, 202E), a region to the west of Olympus Mons, were typical median slopes on these baselines are often smaller than 0.1 degree. A shaded relief map of the topography is overlaid is monochrome.
Name | Value | Additional Values |
---|---|---|
Target | Mars | |
System | ||
Target Type | Planet | |
Mission | Mars Global Surveyor (MGS) | Mariner |
Instrument Host | Mars Global Surveyor | |
Host Type | Orbiter | Flyby Spacecraft |
Instrument | Mars Orbiter Laser Altimeter (MOLA) | |
Detector | ||
Extra Keywords | Color, Crater, Map, Mountain | |
Acquisition Date | ||
Release Date | 2000-10-06 | |
Date in Caption | ||
Image Credit | NASA/JPL/GSFC | |
Source | photojournal.jpl.nasa.gov/catalog/PIA02808 | |
Identifier | PIA02808 |