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Updated: Jul 12, 2026

11:34
Scattering And Absorption of Light in Planetary Regoliths
Published on: July 1, 2019
Preliminary results from the viking orbiter imaging experiment
Summary
Viking orbiter images reveal Mars surface processes like cratering and permafrost. Analysis of early Mars surface features shows evidence of fluid ejecta and atmospheric phenomena.
Area of Science:
- Planetary Science
- Geology
- Atmospheric Science
Background:
- The Viking orbiter provided early high-resolution imagery of the Martian surface.
- Previous observations from Mariner 9 established a baseline for surface changes.
Purpose of the Study:
- To analyze photographic frames from the Viking orbiter's initial 30 orbits.
- To enhance understanding of Martian surface processes and features.
Main Methods:
- Acquisition and analysis of approximately 1000 photographic frames from the Viking orbiter.
- Examination of surface features in Chryse Planitia, Cydonia, and near Capri Chasma.
- Assessment of image resolutions ranging from 100 meters to over 1 kilometer.
Main Results:
- Detailed understanding of Martian surface processes including cratering, fluvial activity, and mass-wasting.
- Identification of old surfaces, abundant channel features, and permafrost indicators.
- Evidence of fluid ejecta patterns around craters and minimal changes since Mariner 9 observations.
- Observation of atmospheric phenomena such as hazes, discrete clouds, and wave clouds.
Conclusions:
- Viking orbiter data significantly advanced the understanding of Mars' geological and atmospheric processes.
- The Martian surface exhibits ancient features, hydrological indicators, and signs of permafrost.
- Atmospheric observations contribute to the study of Mars' climate.
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