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Mars Astronomy 311 Professor Lee Carkner Lecture 14 Mars -- The God of War  The Canals of Mars In 1877 G. Schiaparelli thought that he saw intersecting straight lines on Mars   Percival Lowell built an observatory near Flagstaff, AZ and published elaborate maps of a network of canals and oasis on Mars  Mars Facts Size: ~1/2 Earth size  Orbit: 1.5 AU  Description: Celestial Motions of Mars Mars rotates on its axis with a period of 24 1/2 hours  Mars has an orbital period of 23 months  Mars is tilted on its axis  Spacecraft to Mars Mariner 4 was the first spacecraft to visit Mars in 1964  Recent missions:   Mars Express (2003, orbiter) Mars Reconnaissance Orbiter (2006, orbiter)  Spirit and Opportunity (2003, rover) Surface Features Volcanoes -- Mars has many shield volcanoes, but they are not active today  Canyons -- Mars shows deep canyons, the result of volcanic activity stressing the crust  Craters --The northern hemisphere is less heavily cratered than the southern    Dust storms alter the Martian craters Tharsis Rise Olympus Mons Valles Marineris Cratering on Mars Mars Topological Map The Surface of Mars Mars is red due to iron oxide (rust) in the soil   Surface is covered with reddish soil and is rocky and broken Mars is cold   Mars has seasons due to the tilt of its axis Standing on Mars Mars’s Atmosphere Composition: 95% CO2, 3% N2, trace amounts of water vapor and oxygen Pressure: 0.007 atmospheres  Early Mars may have had a thicker CO2 and H2O atmosphere   Water on Mars Mars is now a very dry world   Water ice may be present in the polar ice caps (along with frozen CO2)  It is possible that water exists underground Frost on Mars Polar Ice Cap Was Mars Wet?  Surface features indicate that water once flowed freely on the Martian surface   Due to:  Global water (Many oceans, rivers, etc)?   Mars may have been warmer with a thicker atmosphere in the past   Where is the water now?    Mars may warm up periodically allowing water to form (Mars may now be in an ice age) Dried-up River Bed Past Water Erosion on Mars Life on Mars?  Mars shows evidence for liquid water and higher temperatures in the past    Viking tested soil samples but the results were inconclusive  We do have a few meteors that were blasted off the surface of Mars   AH84001 shows some features that look a little like the remains of life-forms, but evidence is not very strong Viking’s Soil Scoop Fossil Life in Martian Meteorite? Cydonia “Face” on Mars Traits of Psuedoscience Certainty  Avoidance of Occam’s Razor  Paranoia  Mars’s Interior Mars has a lower density than the other terrestrial planets (4000 compared to 5000 kg/m3)  No evidence for plate tectonics We have very little other data on Mars’s interior   Continuing Mars Exploration Phoenix, a small “scout” lander mission, to be launched 2007  Sample return?  Manned mission?  A Possible History of Mars Mars forms  Volcanism creates volcanoes and lava flows  Mars losses internal heat, crust cools  Atmosphere loses CO2, atmosphere cools  Water freezes Summary Red, dusty, thin atmosphere Mars is a medium-sized world allowing it to retain an atmosphere (unlike Mercury and the Moon), but not a thick atmosphere (like Venus and Earth) Mars shows signs of being habitable in the past, but no good evidence of life has been found Summary: Surface Mars has a red surface composed of dust, soil and rocks Mars has large volcanoes and deep chasms Dust storms often cover the surface Mars has a low density and may not have an iron core Summary: Climate Mars has a very thin atmosphere and is cold Low temperature and pressure prevent liquid water on the surface Mars must have had a thicker, warmer atmosphere in the past since there is substantial evidence for water flows Early thicker CO2 greenhouse atmosphere gradually washed out by rainfall The temperature on Mars may change over time due to orbital variations
 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
                                             
                                             
                                             
                                             
                                             
                                             
                                             
                                             
                                             
                                             
                                            