Introduction to the Solar System


APAS 1110 Summer 1996

Lecture 8 -- Earth-Venus-Mars: Continued

Friday, June 14




  • Homework 4 postponed until Tue, late HW 3 accepted on Monday


  • Review of Tides

    Why do we have tides twice a day, instead of once? Why not just the side facing the moon. It works like this:
    Moon pulls on the whole Earth
    The pull is actually 'felt' by the Earth at its center
    Water on the Moon side is actually pulled more than average
    Water on the side facing away from the moon actually is pulled less than the average--The water can flow, so it bulges away.


  • SL: Mars

    Half the size of Earth
    24 hour day, same as Earth
    23 deg axial tilt, same as Earth --which means it has seasons just like Earth
    Half as much sunlight as Earth
    Very cold, -50 F on average
    But in the summer on the equator, it can get room temperature
    Has a thin CO2 atmosphere, 1/100th of the Earth's.
    Almost same composition as Venus', but 10,000 times thinner
    Has polar caps, made of water ice and dry ice (CO2)
    It has weather, with morning clouds, snow, storms, dust storms
    But no evidence for running water recently (recall surface dating with crater counting). It's all frozen out.


  • SL: Viking

    Most of what we know about comes from an incredible mission: The Viking Missions to Mars in 1976
    Two spacecraft, with two orbiters and two landers
    Perhaps the pinnacle of human exploration of the planets
    Orbiters mapped the planet, looking at some areas with 20 m resolution
    Landers photographed the surface, studied the chemistry of the soil, and also performed as weather stations measuring winds, temperatures, and atmospheric pressures
    They also had a complex set of biological experiments to look for life
    Details in the Mars Quest show in the planetarium on Monday.


  • SL: Marineris Hemisphere

    Here's what Viking saw
    Mars has two kinds of terrain, roughly divided between the Northern hemisphere and Southern hemisphere
    The northern hemisphere, which we are looking at here is smooth, relatively crater free
    It has huge shield volcanoes, sitting on a huge bump on the surface, as well as other places.
    It also has an enormous crack, the size of the US, splitting down the side of the bump
    The northern hemisphere has relatively few craters, probably wiped out by the volcanism--it is a relatively young surface, maybe 1 by old
    Notice the clouds on the morning terminator--morning fog surrounding three enormous volcanoes on the Tharsis bulge
    Light is where windblown dust has settled -- dark areas may be bedrock
    Mars is red because it the surface has oxidized iron -- rust, just like volcanic red dirt on the Earth


  • SL: Southern Hemisphere

    The southern hemisphere is much, much older, as evidenced by a lot of craters
    The entire south is higher than the volcanic plains, and we call it the highlands, just like on the moon


  • SL: Argyre

    The southern portion looks just like the moon, like a dead planet
    This is a huge basin and numerous other craters in the south
    When we sent Mariner 9 there in 1971, it flew under the south pole, and we thought Mars was just like the Moon. It was very disappointing
    But Viking changed all that


  • SL: Simulated Landing

    Since we didn't know what to expect, we surveyed possible landing sites for several months before deploying the landers
    The lander used parachute and rockets, and used the orbiter as a relay


  • SL: Simulated Lander Site

    Landers were semiautonomous, and bristling with instruments


  • SL: First Surface Photo

    You can imagine the anticipation we felt, wondering what this new place, new world looked like.
    Far more Earth like, this is even a place that could be home to humanity
    Here's what it saw
    Rock strewn desert, light sky
    The rocks are probably strewn from some distant impact crater or volcano
    If you look at the rock on the lower right, it looks vesicular
    That means it has evidence of bubbles that came out as the rock cooled
    Probably volcanic in origin


  • SL: Trench

    Viking scooped up soil with a shovel, and put it in various chambers for testing
    They tested what elements the rocks were made of -- Fe, Mg, Al --basalts
    They looked for water (1%)
    I know a researcher who discovered you can retrieve the water from this kind of soil with a microwave oven


  • SL: Lander Instrument

    One of the most incredible things the Viking Landers did was search for evidence of life
    They tried to stimulate microorganisms to do photosynthesis
    They looked for evidence that carbon was used up in metabolic activity
    And they directly measured the organic content of the soil
    What they found was that there were no organic molecules at all
    But they also found that gases were given off by the soil violently
    The soil is very chemically reactive
    But there was no life
    Later, we came to realize that the experiments were a bit naive, too restricted in what we expect from life
    Also, we may have to dig in different places to look for fossil remains of life


  • SL: Frost

    One lander landed N, about 50 deg latitude, and one landed nearer the equator
    The northern one saw dramatic seasons.
    This is a shot of the area around lander 2 during the morning
    A thin CO2 frost has condensed out of the atmosphere during the night
    During the day, it will quickly sublimate --directly from frost to gas


  • SL: Tharsis Volcanoes

    While the lander is doing its complex experiments, up in orbit, the orbiter is mapping the planet
    The most striking features are volcanoes, much, much bigger than Earth volcanoes
    Here are the three Tharsis volcanoes, on the big bump, shrouded in clouds
    You can see that they have calderas, or volcanic craters on the tops
    Notice the cracks, the beginning of the huge crack going SE from the Tharsis Bulge


  • SL: Olympus Mons

    The biggest volcano in the solar system
    80,000 feet high, 500 miles across
    Called Olympus Mons
    Enormous pit in the center
    Calderas are formed when the volcano finished erupting, and the magma from below withdraws. The ground collapses at the top


  • SL: Olympus 3-D

    Stereo images were taken by Viking that allows us to reconstruct the 3-D nature of the surface.
    Here you can see the miles high scarp, or cliff that surrounds Olympus Mons
    Caused by the falling away of material
    This mountain is almost exactly like the large Hawaiian shield volcanoes
    It was probably created by a huge plume of hot material from the depths of Mars


  • SL: Olympus Mons Clouds

    Because it is so high, Olympus Mons strongly influences the weather on Mars, just like mountains do here
    Here is an oblique view of the summit, encircled by clouds


  • SL: Ulysses Patera

    Because Viking orbited for 3 years, it was able to take very close looks at certain portions of the planet
    So we looked closely at the volcanoes
    Here's a volcano with a huge caldera, and some impact craters
    By counting craters around the volcanoes, we find that some may be as little as 100 my.
    If Mars is a dead planet, then the corpse is still warm
    Maybe even some hydrothermal activity (hot vents of gas) still left
    This is exciting, because there is life in hydrothermal systems on the Earth, and it looks like a good place to evolve


  • SL: Olympus Caldera

    Some of these calderas are very complex, showing evidence for multiple eruption events -- volcanoes may have lasted for a long time
    Therefore, hydrothermal systems may have lasted for a long time, allowing life to evolve
    Bu see the bottom left--evidence for something flowing


  • SL: BW River Valleys

    In fact everywhere we look, in both the old (South) and new (north) areas of Mars, we see evidence for running water in the past
    Here is a very, very old valley network
    The valleys are more common in the old regions, but there is also evidence for a large system of drainage networks from older region to newer regions


  • SL: River Valleys

    Some of the river systems clearly look like rivers, and must have carried enormous amounts of water
    We interpret this to mean that Mars was warmer in the past
    It has almost no greenhouse effect now, because the air is so thin
    But it may have had a much thicker CO2 atmosphere in the past, now sequestered at the poles or escaped from the planet
    Mars has a lower gravity, and light gases can escape easily
    Higher pressure, more greenhouse, liquid water
    Now the water is probably frozen as permafrost, or under the ground
    There is other evidence for massive climate change as well


  • SL: Flood Drainage

    But most of the intricate river networks are ancient -- 3.5 B years ago
    Recall that the solar system is 4.5 billion years old
    But there is more recent evidence of flowing water
    This is the result of a series of great floods
    You can tell that the water has moved fast, cutting deep channels
    These may have been much more recent -- maybe 1 by ago


  • SL: Chaotic Terrain

    There are places where it looks like huge amounts of ice melted suddenly and flowed out. The land collapsed in these places, creating chaotic terrain
    There are places like this on the Earth -- badlands of Eastern Washington


  • SL: Teardrop

    But there is other evidence for flowing water
    Here, you see a teardrop shape around a crater. Somehow when the crater formed (before the flood) it sort of cemented the ground, making it more resistant to erosion as the water flowed


  • SL: Rampart Craters

    Some craters have funny impact ejecta, called lobate ejecta
    It looks like the impactor hit where there was subsurface ice
    The ice melted on impact, made mud, which was flung out in these patterns


  • SL: Boundary Scarp

    Some people have even suggested that Mars may have had oceans, and that there are ancient shorelines
    This is the scarp that makes a boundary between the south and north
    you can see a crater with lobate ejecta in the center right
    Channels ending between s and n
    Sand dune fields

    VIDEO: CLIPS OF FLYING OVER MARS FROM 'FLYING BY THE PLANETS'

    6/14/96