Venus Statistics General Venus Geology GLY 424/524 March 18, 2002 • • • • • • • • Mass = 80% Earth’s mass Uncompressed density = 5250 kg/m3 Equatorial radius = 6052 km Orbital period = 225 days Rotational period = 243 (backwards) Gravity = 8.82 m/s2 Mean surface temp = 482°C Mean surface pressure = 92 bars Mariner 2 • First successful Venus flyby • December 1962/January 1963 • Objectives – Atmosphere, magnetic field, charged particle environment, mass • Results – – – – – Retrograde rotation Hot, high-pressure surface CO2 atmosphere Permanent clouds No magnetic field Venera 7 • Venus Lander • August, 1970 • Returned signals for 23 minutes from surface before failing • First transmission from another planet! • Results – High surface temperature – High surface pressure Venera 4 • • • • Soviet mission October, 1967 Atmospheric probe Penetrated to ~25 km above surface – Atmosphere hot – High pressure Venera 8 • June, 1972 • Probe and lander • Returned signals for 53 minutes after landing – Confirmed high surface temps, pressures – Determined natural light suitable for photography 1 Mariner 10 Venus Mariner 10 • Slingshot around Venus to reach Mercury • February, 1974 • Confirmed opaque clouds, “chevron” pattern suggesting high-altitude winds Venera 9 Results Venera 9 • Orbiter and Lander • October, 1975 • Survived for 53 minutes after landing • Clouds 30-40 km thick with bases at 30-35 km altitude • Atmospheric constituents including HCl, HF, Br, and I • Surface pressure about 90 (Earth) atmospheres • Surface temperature 485°C • Light levels comparable to those at earth on a cloudy summer day • TV photography showing no apparent dust in the air, and fresh 30-40 cm rocks Venera 9 landing site Venera10 • • • • Lander and orbiter October, 1975 Roughly similar results as Venera 9 Max windspeed of 3.5 m/s Only image returned Horizon in corners Lander pad at center base Rocks 30-40 cm across 2 Venera 11, 12 Pioneer Venus 1 and 2 • Low resolution radar mapping of portions of Venus • Orbiters and multiprobes • Revealed apparently young, tectonically complex surface • September, 1978 • Orbiter and Landers • Instruments – – – – gas chromatograph scattered solar radiation soil composition amospheric electrical discharges • Results – lightning and thunder – highAr36/Ar40 ratio – discovery of carbon monoxide at low altitudes Venera 13 & 14 • March 1982 • Orbiters and Landers • Instruments – – – – – camera system X-ray fluorescence spectrometer screw drill and surface sampler Dynamic penetrometer seismometer Venera 13 Lander Venera 13 & 14 Results • Landed near Pheobe Regio • Images returned • XRF suggest weakly differentiated melanocratic alkaline gabbroids Venera 13 Lander: Opposite views 3 Venera 14 Lander: Opposite Views Magellan • August, 1990 • Near-global coverage in radar ~12.5 cm wavelength • Results – – – – No plate tectonics 85% covered with volcanics Anhydrous Winds slow but effective General Geology Magellan Topography • 2 crustal provinces – Plains • Presumably volcanic • Various degrees of deformation • Low-lying – Tesserae • Russian parquet wooden floors • Formed from plains or older bits of crust poking through? • Topographically above plains Synthetic Aperture Radar Magellan Radar image 4 Alpha Regio Ishtar Terra Strike-slip Fault in Ovda Regio Venera 13 Landing Site Fractured Plains 5 Eastern Aphrodite Terra Coronae Large Coronae Stages in Coronae Evolution 6 7
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