Geologic map of the Elysium region of Mars
January 1, 1992
The region centered at Elysium Mons contains that second largest volcanic complex on Mars, surpassed in size by only the Tharsis complex. The Elysium region also has been a center of tectonic, fluvial, and mass-wasting activity. After degradation of ancient cratered terrain within the northern lowlands, volcanic rocks erupted from Elysium Mons, Hectas Tholus, and Albor Tholus in Elysium Planitia. The volcanic activity was associated with episodes of channel formation, faulting, and apparent volcano/ground-ice modifications of some areas. On this map sheet we portray, describe, and interpret the rich geologic history of the region.
Citation Information
| Publication Year | 1992 |
|---|---|
| Title | Geologic map of the Elysium region of Mars |
| DOI | 10.3133/i2147 |
| Authors | K. L. Tanaka, M. G. Chapman, D. H. Scott |
| Publication Type | Report |
| Publication Subtype | USGS Numbered Series |
| Series Title | IMAP |
| Series Number | 2147 |
| Index ID | i2147 |
| Record Source | USGS Publications Warehouse |
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Geologic map of the Elysium region of Mars
The region centered at Elysium Mons contains that second largest volcanic complex on Mars, surpassed in size by only the Tharsis complex. The Elysium region also has been a center of tectonic, fluvial, and mass-wasting activity. After degradation of ancient cratered terrain within the northern lowlands, volcanic rocks erupted from Elysium Mons, Hectas Tholus, and Albor Tholus in Elysium Planitia.
Related Content
Geologic map of the Elysium region of Mars
The region centered at Elysium Mons contains that second largest volcanic complex on Mars, surpassed in size by only the Tharsis complex. The Elysium region also has been a center of tectonic, fluvial, and mass-wasting activity. After degradation of ancient cratered terrain within the northern lowlands, volcanic rocks erupted from Elysium Mons, Hectas Tholus, and Albor Tholus in Elysium Planitia.