Mars -- the Red Planet

Key points: The mirage of Martian canals; comparison of Mars with Earth; evidence for water, search for life

Image of Mars (about 2/3 of full disk)

mars-mangala.jpg (19635 bytes)

(to left, from SEDS,  http://www.seds.org/nineplanets/nineplanets/mars.html

above, Mangala, the planet Mars, depicted as a red-skinned horseman on a white ram. from The Black Peacock, http://www.goloka.com/index.html))

For 150 years, there has been a fascination with the possibility of life on Mars.

Seasonal variations in both the size of its polar caps and brightness of mid-latitude features led to the speculation by Percival Lowell around 1900 that the poles consist of water with “canals” that provide irrigation for crops grown by an advanced civilization (An original sketch by Percival Lowell)

We now know that the polar caps are predominately CO2 and not water; the variations in mid-latitude features are due to seasonal dust storms. The infamous “canals” are the result of an optical illusion where the human brain likes to play “connect-the-dots”.

Mars Orbiter missions in late '60s and early '70s revealed a barren and cratered landscape on Mars making life as we know it on Earth unlikely. However, the areas mapped first have turned out to be the oldest, least "interesting" of the whole Martian surface!

Orbiter image of Martian surface shows barren landscape with craters

Later missions have shown much more interesting terrain. For example, Candor Chasma is a region containing many landslides, fractured blocks that were probably at the bottoms of ancient lakes, and craters partially buried by wind-blown sand. Volcanic deposits of lava are present elsewhere in the canyon. (Image from NASA and NASM, http://www.nasm.edu/ceps/etp/mars/surface/canyons.html)

 

mars_candor.jpg (91466 bytes)

This complex, in some ways earth-like, planetary surface has encouraged continued searches for life, but now on a bacterial and possibly extinct level - and also searches for water, as a necessary condition for formation of life. We will discuss these modern searches later, in the overall context of the formation of life. We now turn to the study of the planet itself.

Mars is similar to Earth in some respects:

Very different from Earth in some respects:

Mars is smaller and less dense than the earth, and as a result has much lower surface gravity. The appearance of Mars is dominated by iron oxide (rust) that gives it a reddish color.

Geology

Mars has huge shield volcanoes, like those in Hawaii (such as Mauna Kea) -- Olympus Mons shown below is larger than any mountain on Earth,

Olympus Mons Diagram showing how much bigger Olympus Mons is than Everest

The Martian volcanos grew to huge size because there are no plate motions on Mars (From U. Tenn, http://csep10.phys.utk.edu/astr161/lect/mars/surface.html) We can trace this difference from the earth to the smaller size of the planet and its inability to retain sufficient interior heat to drive plates.

Animation shows why plate motions limit the size of volcanos on Earthhirisevallemar.jpg (1073312 bytes)

 

 

 

 

 

 

 

 

The lack of plate tectonics is confirmed by a lack of marsquakes that can be detected by various Martian lander spacecraft.

Mars also has a huge canyon, Valles Marineris, visible in the whole-disk image at the top, in the view to the below left, and the artist's concept to the below right. (from NASA, http://www.units.muohio.edu/dragonfly/space/VALLES.shtml, Robert Hurt, http://homepage.mac.com/rhurt/gallery/latest.html). It is far larger than the Grand Canyon. Here is an imaginary flight over these features Caution! Large File!! en00500_1.jpg (18578 bytes) (from http://themis.asu.edu/valles_video Mars Odyssey Mission Thermal Emission Imaging System, ASU and JPL Digital Image Animation Laboratory) If you missed the movie, or want to review what you saw, look here buttonbook.jpg (10323 bytes)

valles-mar.jpg (78113 bytes) valles-marineris.jpg (59779 bytes)

The background image to the extreme right covers a small portion of the floor of Ius Chasma, one branch of the giant Valles Marineris system of canyons. The image illustrates a variety of processes that have shaped the Martian surface. There are bedrock exposures of layered materials, which could be sedimentary rocks deposited in water or from the air. Some of the bedrock has been faulted and folded, perhaps the result of large-scale forces in the crust or from a giant landslide. (from HiRise operations center, U. of Arizona: http://hiroc.lpl.arizona.edu/images/TRA/)

Martian Atmosphere

The escape velocity from the surface of Mars is less than 1/2 that on Earth. The atmosphere’s density is about 1/200th that on Earth. As we would expect given the low escape velocity, the atmospheric composition is dominated by heavier gases than for Earth -- CO2, Argon, H2O.

Martian Weather

Dust streaks left by blowing sand Martian sunset
Surface is extensively modified by winds,blowing dust. Notice streaks of dust from craters (left). Martian sunset from Mars Pathfinder (right) shows the effect of dust in the atmosphere: (http://www.spacedaily.com/news/mars-odyssey-01b.html)

Dust devils sweep across the Martian desert in this movie clip from the Mars Roversen00500_1.jpg (18578 bytes)

http://marsrovers.jpl.nasa.gov/gallery/press/spirit/20050819a.html

Thin clouds form in the atmosphere.

http://www.ucls.uchicago.edu/students/projects/martiansuntimes/

Olympus Mons with clouds
Temperature range over a Martian day is large, about 60C Chart of temperatures from Mars Pathfinder -- a Sol is a Martian day.

Days are similar to Earth, seasons more extreme (and colder) because Mars’ orbit is more eccentric than the earth’s and Mars’ polar axis tilt is a little more than for the earth’s (25.2o as compared to Earth’s 23.5o)

Mars' southern polar cap The polar caps (we show the south one here) are frozen carbon dioxide (dry ice). They have a complex layered structure from the cycles of melting and freezing.

(Picture from Mars Global Surveyor, http://www.msss.com/mars_images/moc/4_27_00_spcap/index.html)

Although the atmosphere and weather conditions do not seem conducive to life now, perhaps the lighter gases leaked away slowly. Is it possible that Mars started with Earth-like conditions, such as flowing water? If so, did life form then?

Water on Mars -- a key to life as we know it

Valles Marineris and other geological features provide strong evidence for running water on surface in the past.

Gullies in a crater wall Probable erosion streaks on a cliff (above left) (HiRise, MRO; LPL (U Arizona), NASA)

Probable ancient river bed (Mars Express, ESA)

Gullies in a crater wall (left), from Mars Global Surveyor, http://www.msss.com/The_MOC_Shop/order_form

The walls of the Garni Crater (below) are marked by dark narrow steaks, called "recurring slope lineae" by geologists. The streaks are a few hundred meters in length (a few football fields) and almost certainly are produced by recent flows or salty water. (credit NASA/JPL/University of Arizona, HiRise spacecraft, https://www.nasa.gov/multimedia/imagegallery/iotd.html)

marslake.jpg (69511 bytes) marswater.jpg (15322 bytes)

Crater (to left; diameter about 20 miles) that appears to have been a lake in the past. It has a very smooth, flat floor with "shoreline" markings and streams bringing water in and out as indicated by the arrows. (From Cabrol & Grin, 1999 Icarus); artist's concept (above) shows how it might have looked (from Berkeley Lab, http://www.lbl.gov/Science-Articles/Archive/SB-ESD-hunting-for-martians.html

This beautiful image of the Victoria Crater is from the HIRISE camera (provided by the U. of Arizona) on the Mars Reconnaisance Orbiter. The original image can distinguish details at the scale of a few feet.  http://marsprogram.jpl.nasa.gov/mro/gallery/press/

The crater is about 800 meters (half a mile) in diameter. The distinctive scalloped shape of the rim is caused by erosion and downhill slides of crater wall material. Boulders that have fallen from the crater wall can be seen at the bottom of the crater. A striking field of sand dunes also lies on the crater floor. The Opportunity rover is perched on the rim of the crater at about the ten o'clock position. See the blow-up below for a better view of it.

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The Mars Odyssey mission has found that the planet used to have large amounts of water (using an instrument whose development was led by UA Professor Bill Boynton).

Principles of Gamma Ray Spectrometer Here is how the Odyssey experiment works:

When cosmic rays strike the surface of Mars, they can penetrate and react with the atomic nuclei trapped just below. The reaction produces gamma rays with energies characteristic of the atom that produced them. By measuring the gamma rays, we can tell what the atoms below the surface are. From Mars Odyssey home page, http://mars.jpl.nasa.gov/odyssey/

Surface map of Mars, blue shows sites of underground water The surface areas colored blue show lots of subsurface hydrogen, indicating the presence of water. Maybe they are telling us where Mars used to have oceans!

From Mars Odyssey home page, http://mars.jpl.nasa.gov/odyssey/

The Mars Phoenix mission (led by Peter Smith of the UA Planetary Sciences Department) confirmed the presence of water in Martian soil by landing on the surface, where it used this scoop to deliver Martian soil to an on-board device that heated it and analyzed the vapors it gave off. They included water that had been trapped in the soil.
These pictures taken by Phoenix show the underground frost. The spacecraft scoop has cleared away some of the surface soil. Some lumps of material can be seen to the lower left in the trench on Sol 20 (indicated with three arrows). However, they have evaporated and disappeared by Sol 24 (Sol 20 and Sol 24 are days counted since the mission started taking data).,The white material is probably carbon dioxide frost deposited over the cold Martian night.

Terraforming Mars

Terraforming, starting point Terraforming. part way through Terraforming, complete

Conditions are similar enough to Earth that some have proposed ways we might modify them to make Mars more habitable -- a process that has been named "terraforming". Basically, the proposals are based on enhancing greenhouse gases in the Martian atmosphere to raise the surface temperature. For an explanation of how it might be done, see http://www.cem.msu.edu/~cem181fp/mars/chem-intro.html, and many other web sites. It isn't clear at all that this is feasible, of course, nor that it is desirablebuttonex.jpg (1228 bytes)

Moons of Mars

Mars has two moons, Phobos and Deimos, which probably are captured asteroids and did not form with Mars.(from NASA via http://sci.esa.int/science-e/www/object/index.cfm?fobjectid=31031)

Phobos Deimos
Here is a view of the large crater on Phobos, taken by the HiRise mission.The crater is 9 km (6 miles) across; its size suggests that the impact that created it must have come close to shattering the small moon. (from APOD, http://www.brera.mi.astro.it/apod/ap080410.html

 

Test your understanding before going onbuttongrad.jpg (11232 bytes)

venusborga.jpg (21260 bytes)Mayan Venus deity, from the Borgia Codex, http://members.shaw.ca/mjfinley/4VENUS.htm

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Marduk, associated

with Jupiter by the Babylonians

http://www.livius.org/es-ez/esagila/esagila.html

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hypertext copyright.jpg (1684 bytes) G. H. Rieke

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