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Published byErick York Modified over 9 years ago
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A thick CO 2 atmosphere with a surface pressure 92 times that of Earth’s atmosphere hides the planet’s surface from view
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Facts about Venus * * 462 C o * *
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Venus Atmospheric Missions Mariner 10 – Fly-by in 1973 Pioneer Venus – 5 probes in 1978 Vega 1 and 2 – 2 probes in 1985 Galileo – Fly-by in 1990 Europe’s Venus Express (orbits in April 2006) Messenger (fly-bys October 2006 & June 2007)
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45 km = 100 C o Cloud Tops
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The “Greenhouse Effect” on Venus
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Carbon dioxide cycle on Earth keeps us from being like Venus But this cycle would not work if there’s no liquid water!
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Single-celled floating organisms like these foraminifera construct fragile CaCO 3 shells. When the organisms die, their shells sink to the ocean floor and form limestone deposits, thus trapping CO 2.
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Limestone deposits in today’s oceans
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Spacecraft that have studied the surface of Venus Mariner 2 – 1962 – First planetary mission Pioneer Venus – 1978 - Topography and atmospheric probes Veneras 8 – 14, 1975 – 1982 – Landers! Veneras 15 & 16, 1984 – Orbital radars Magellan – 1990 – 1994 – Orbital radar images, topography and gravity data Europe’s Venus Express, 2006
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Venera 14 Soviet Lander - 1982
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Landing Sites for Venera Spacecraft
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Venera 14 views of surface of Venus
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The surface of Venus, imaged by the Venera 14 Lander. Upper image: CO 2 atmosphere results in reddish color. Lower image: CO 2 removed. The dark rock is basalt!
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Composition of the surface rocks of Venus. The rocks are basalt!
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Magellan being launched from Space Shuttle
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Topography of Venus from the Pioneer Venus spacecraft
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The “continents” on Venus are as big or bigger than those on Earth
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Maxwell Montes over 12 km high!
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Maat Mons ~8 km high Still active?
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Sapas Mons ~400 km dia.
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Cleopatra Caldera On Lakshmi Planum
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Tectonic features: Fotla Corona S.E. of Aphrodite Terra
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Tessera rolling plains near Maxwell Montes
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Rift zones
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Stuart Crater 67 km diameter Aurelia crater 32 km diameter Unusual fluid ejecta at impact craters on Venus
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Wind streaks – fine particles moved by wind
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Isabella crater – Ejecta so hot it flows like lava
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High surface pressure may help pancake domes form
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Summary of Venus
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