Geologic map of the Noachis Quadrangle of Mars
January 1, 1977
The Noachis quadrangle is in the ancient cratered highlands of Mars. Craters dominate the surface of the planet in this area; most are of impact origin, some are of volcanic, origin, and some are of undetermined origin. Martian craters are I general similar in morphology of lunar craters but are more degraded. Analogous morphologies and size-frequency distributions of lunar and Martian craters indicate that both populations are mostly of impact origin (McCauley and others, 1972). Martian 10 pictures of Mercury suggest similar trends on that planet, a further indication that the crating process was exogenous.
Citation Information
Publication Year | 1977 |
---|---|
Title | Geologic map of the Noachis Quadrangle of Mars |
DOI | 10.3133/i910 |
Authors | J.E. Peterson |
Publication Type | Report |
Publication Subtype | USGS Numbered Series |
Series Title | IMAP |
Series Number | 910 |
Index ID | i910 |
Record Source | USGS Publications Warehouse |
Related
Geologic map of the Noachis Quadrangle of Mars
The Noachis quadrangle is in the ancient cratered highlands of Mars. Craters dominate the surface of the planet in this area; most are of impact origin, some are of volcanic origin, and some are of undetermined origin. Impact craters in the Noachis quadrangle are classified into four groups based on their morphologic characteristics, each group representing a relative age range. Where applicable,
Related
Geologic map of the Noachis Quadrangle of Mars
The Noachis quadrangle is in the ancient cratered highlands of Mars. Craters dominate the surface of the planet in this area; most are of impact origin, some are of volcanic origin, and some are of undetermined origin. Impact craters in the Noachis quadrangle are classified into four groups based on their morphologic characteristics, each group representing a relative age range. Where applicable,