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Pioneer Venus radar results - Geology from images and altimetryAn unimodal distribution of relief for Venus was obtained from the Pioneer Venus altimetry measurements. The 'upland' rolling plains constituting 65% of the surface show dark circular lava-filled impact basins; highlands in the 8% of the area comprise Ishtar Terra and Aphrodite Terra; and the lowlands consist of crudely circular surfaces with low relief within the highlands. The complex ridge-and-trough regions east of Ishtar Terra and in the southern Aphrodite Terra may be due to large-scale crustal motions.
Document ID
19810042423
Acquisition Source
Legacy CDMS
Document Type
Reprint (Version printed in journal)
Authors
Masursky, H.
(Geological Survey Flagstaff, AZ, United States)
Eliason, E.
(Geological Survey Flagstaff, AZ, United States)
Schaber, G. G.
(U.S. Geological Survey Flagstaff, Ariz., United States)
Ford, P. G.
(Geological Survey Flagstaff, AZ, United States)
Pettengill, G. H.
(MIT Cambridge, Mass., United States)
Mcgill, G. E.
(Massachusetts, University Amherst, Mass., United States)
Schubert, G.
(California, University Los Angeles, Calif., United States)
Date Acquired
August 11, 2013
Publication Date
December 30, 1980
Publication Information
Publication: Journal of Geophysical Research
Volume: 85
Subject Category
Lunar And Planetary Exploration
Accession Number
81A26827
Funding Number(s)
CONTRACT_GRANT: NAS2-9129
CONTRACT_GRANT: NASA ORDER A-831221
CONTRACT_GRANT: NAS2-9473
Distribution Limits
Public
Copyright
Other

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