Catalog of Planetary Maps
#1693

Davies, Merton E. · Robinson, J. C. · Smith, Bradford A. · 6, Mariner · Team, 7 Television Experiment

National Aeronautics and Space Administration Mars Chart

Scale 1: 25 000 000

Marsmap

1970, Washington, D.C. · U.S. Army Topographic Command

1:25M
US Army Topographic Command, Washington, D.C.
Advisors: Merton E Davies, JC Robinson, Bradford A Smith and the Mariner 6 and 7 Television Experiment Team.
Nomenclature: 1958 IAU
1970
Note the handwritten notes of the Tharsis Montes.

The map was drawn by pencil and charcoal, by Charles Cross  (Morton 2002:50)

Morton O 2002 Mapping Mars. Picador, New York.

usgs_flagstaff_map_collection_16

Map provided courtesy of the USGS Flagstaff Library.

Prepared under the direction of the Department of Defense and published by the U. S. Army Topographic Command, Washington, D. C., with the advisory assistance of Merton E. Davies, J. C. Robinson, and Bradford A. Smith of the Mariner 6 and 7 Television Experiment Team.

ORIENTATION

The orientation of cardinal directions is in accordance with the resolution adopted at the 1961 Congress of the International Astronomical Union. North is at the top of the Mercator projection chart, east is at the right. Areographic longitudes increase from 0° to 360° westward on the planet’s surface.

NOMENCLATURE

Names of surface features are in accordance with the standard list of Martian names prepared by Subcommission 16 of the International Astronomical Union and adopted at the 1958 IAU Congress. A few additional feature names in common use, which are not included in the IAU list, are shown enclosed in parentheses.

CONTROL

Features of this map were positioned by a new areodetic control net derived from the Mariner 6 and 7 pictures. This net was established by the Aeronautical Chart and Information Center, St. Louis, Missouri and the Television Experimenters. This control consists of the coordinates of approximately 110 surface features and photograph coordinates of intersections of parallels and meridians at 5° intervals. The control derived from Mariner 6 near-encounter photography was designated as the basic control net and all other control has been tied to this net to produce a unified control system.

SOURCES

This map was produced from Mariner 6 and 7 photography provided by the National Aeronautics and Space Administration. The following photograph frames were used to control the compilation: far-encounter frames 6F39–49; 7F62–67, 69–77, 80–83, 85–88, 93; and near-encounter (close-up) wide angle frames 6N1–25, 7N1–31 (odd-numbered frames only). Additional photographs were used in the compilation to aid in the interpretation and portrayal of features. The coverage diagram at right shows photographic coverage by area.

TERRAIN FEATURES

The photographs from Mariners 6 and 7 confirm the finding of Mariner 4 that the surface of Mars is heavily cratered. However, in addition to this cratered terrain, two new distinctive types of terrain are visible in the Mariner 6 and 7 pictures. These have been characterized as “chaotic” terrain and “featureless” terrain (Leighton, R. B. et al., Science, October 3, 1969). Craters are of two general types: large, flat-bottomed craters and small, bowl-shaped craters. The flat-bottomed craters range in diameter from several to a few hundred kilometers, while the bowl-shaped ones are generally somewhat smaller. Cratered terrain occurs fairly generally throughout the southern hemisphere, and appears to be fairly widespread in the northern hemisphere.

Chaotic terrain, visible on portions of frames 6N6, 6N8, and 6N14, consists of a very irregular network of short ridges and depressions, generally 1 to 3 km wide and 2 to 10 km long. Very few clearly defined craters can be seen in these areas.

The area of featureless terrain revealed by the Mariner pictures is in the circular desert Hellas. No craters or other surface features can be distinguished down to the limit of resolution of the photographs, about 300 meters. Apparently some process has been operative in this region which obliterates or obscures craters and other features on a short geological time scale, or an unusual material is localized here.