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Topic 5: Ken Nealson, Imre Friedmann Topic 6: Peter Ward and Donald Brownlee Bennett Ch. 9 &10 Goldsmith and Owen Ch.16-18 Suggested reading for next HW assignment:
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A brief tour of the solar system
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Mercury Planet closest to the Sun Heavily cratered, no moons, no atmosphere, has iron core 0.38 the diameter of the Earth Surface temperature ranges from 90-700K (mean=452 K) Relatively strong magnetic field (still 1% of Earth’s) MESSENGER 2004-2009
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Venus Sometimes called Earth’s “Sister planet” because similar in size. Atmosphere is primarily CO2 with small amount of Nitrogen 930 °F temperature Runaway Greenhouse effect Retrograde rotation 80% of surface is basaltic rock (lava), many volcanoes observed. Tectonics We have a 100m resolution radar map of the surface. Craters but not many larger craters or very small craters (WHY?)
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Image from Venera 13
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Mars Thin CO 2 atmosphere -60 C average surface temp Very arid with no organic molecules Huge, dormant volcanoes Evidence of past water. Surface made mostly of volcanic rocks 2 Moons: Phobos and Deimos
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Map of Mars
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Jupiter Largest planet in the solar system mass= 318 Earths, volume=1200 Earths Brown Dwarf or “failed star” Mostly Hydrogen and Helium atmosphere Powerful magnetic field and gravitational force
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Jupiter’s Inner moons
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Europa
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Tidal heating
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Saturn Mostly Hydrogen and Helium The rings are either left over chunks of colliding moons or else left over “construction material” that never made it to becoming a moon.
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Cassini-Huygens
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Titan Only moon in solar system to have a dense atmosphere. There are ORGANIC molecules in the atmosphere An atmosphere of mostly Nitrogen with Methane Surface temp = -178 C Cryovolcanism?
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Uranus and Neptune H, He, CH4 atmospheres Uranus: Lacks internal heat & so nearly featureless Axis is tilted by 90º, giving extreme seasons. Neptune: Has internal heat & an active atmosphere Has methane-rich haze which strongly absorbs red & orange light, letting blue & green light pass through.
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Pluto Really a trapped Kuiper-belt object (smaller than our Moon) Kuiper-belt (50 AU out) consists of icy planetesimals: Not all of the outer solar-system material was consumed when the gas giants formed Has one moon: Charon
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Comets Characterized by long period, heliocentric orbits Gases released include OH, CH, NH Nucleus of silicates and ice
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