Geologic map of the MTM -85080 quadrangle (revised), Planum Australe region of Mars
January 9, 2023
Published geologic maps of south polar region of Mars have been based on either Mariner 9 (Condit Soderblom, 1978; Scott and Carr, 1978) or Viking Orbiter (Tanaka and Scott, 1987) images. The mapped extent of the southern layered deposits differs in many places on these maps and on our maps. These differences reflect the difficulty in accurately determining the location of the contact between the layered deposits and subjacent units. The polar layered deposit gradually thin toward their margin in many places, and the smooth surface features that characterize the layered deposits are also found on other sedimentary blankets in the south polar region (Murray and others, 1972; Sharp, 1973).
Citation Information
Publication Year | 2023 |
---|---|
Title | Geologic map of the MTM -85080 quadrangle (revised), Planum Australe region of Mars |
DOI | 10.5066/P93C78YH |
Authors | K. E. Herkenhoff, B. C. Murray |
Product Type | Data Release |
Record Source | USGS Asset Identifier Service (AIS) |
USGS Organization | Astrogeology Science Center |
Rights | This work is marked with CC0 1.0 Universal |
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Geologic map of the MTM -85080 quadrangle (revised), Planum Australe region of Mars
Published geologic maps of south polar region of Mars have been based on either Mariner 9 (Condit Soderblom, 1978; Scott and Carr, 1978) or Viking Orbiter (Tanaka and Scott, 1987) images. The mapped extent of the southern layered deposits differs in many places on these maps and on our maps. These differences reflect the difficulty in accurately determining the location of the contact between the
Related
Geologic map of the MTM -85080 quadrangle (revised), Planum Australe region of Mars
Published geologic maps of south polar region of Mars have been based on either Mariner 9 (Condit Soderblom, 1978; Scott and Carr, 1978) or Viking Orbiter (Tanaka and Scott, 1987) images. The mapped extent of the southern layered deposits differs in many places on these maps and on our maps. These differences reflect the difficulty in accurately determining the location of the contact between the