Geologic map of the Cleomedes Quadrangle of the Moon
January 1, 1972
The Cleomedes quadrangle is broadly divisible into three provinces. First, the north half of Mare Crisium dominates the southern part of the area. Second, terra materials occur in concentric bands that alternate with mare or plains-forming materials in the northern part. These bands are interrupted by the crater Cleomedes whose associated materials dominate the northwest part of the map and form the third province.
Citation Information
| Publication Year | 1972 |
|---|---|
| Title | Geologic map of the Cleomedes Quadrangle of the Moon |
| DOI | 10.3133/i707 |
| Authors | C.J. Casella, A.B. Binder |
| Publication Type | Report |
| Publication Subtype | USGS Numbered Series |
| Series Title | IMAP |
| Series Number | 707 |
| Index ID | i707 |
| Record Source | USGS Publications Warehouse |
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Geologic map of the Cleomedes Quadrangle of the Moon
The Cleomedes quadrangle is broadly divisible into three provinces. First, the north half of Mare Crisium dominates the southern part of the area. Second, terra materials occur in concentric bands that alternate with mare or plains forming materials in the northern part. These bands are interrupted by the crater Cleomedes whose associated materials dominate the northwest part of the map and form t
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Geologic map of the Cleomedes Quadrangle of the Moon
The Cleomedes quadrangle is broadly divisible into three provinces. First, the north half of Mare Crisium dominates the southern part of the area. Second, terra materials occur in concentric bands that alternate with mare or plains forming materials in the northern part. These bands are interrupted by the crater Cleomedes whose associated materials dominate the northwest part of the map and form t