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The Terrestrial Planets, Part III

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Title: The Terrestrial Planets, Part III


1
The Terrestrial Planets,Part III
  • Mars

2
MARSThe God of War
3
Physical Data
  • Diameter 6,794 km (0.531 Dearth)
  • Mass 6.40x1027 g (0.107 Mearth)
  • Density 3.96 g/cm3
  • Rotation Period 24.6 hours
  • Tilt of Axis 25o
  • Surface Temperature 130-290 K

4
Physical Data
  • Orbital Semi-major Axis 1.524 AU
  • Orbital Period 1.881 years
  • Orbital Inclination 2o
  • Orbital Eccentricity 0.093
  • Surface Gravity 0.38 Earth Gravity

5
Physical Data
  • Satellites 2
  • Magnetic Field no
  • Surface Pressure 0.01 Earths Pressure

6
Mars Interior
CRUST ( aluminum silicates )
  • Relatively small core size compared to the mantle
  • Smallest core of all the terrestrial
    planets compared to the overall volume
    (9)
  • Exact composition of mantle is unknown

3393 km
1520 km
CORE ( iron iron sulfide )
MANTLE ( iron-magnesium silicates ? )
7
Mars Atmosphere
  • Clouds

Planet-wide Clouds ( from Hubble)
A Cyclonic Event
8
Mars Atmosphere
  • 95 Carbon Dioxide
  • 2.7 Nitrogen
  • 1.6 Argon
  • 0.6 Carbon Monoxide
  • 0.15 Oxygen
  • 0.03 Water Vapor (variable)

9
Mars Surface
  • Polar Caps
  • Composed of both carbon dioxide and water
  • South Polar Cap
  • Consists mainly of frozen carbon dioxide.
  • This cap never melts completely.
  • This picture shows it at its minimum size of 400
    km (249 miles).

10
Mars Surface
  • North Polar Cap
  • Consists of mainly water-ice.
  • Seasonal Changes
  • When spring begins in a hemisphere, the
    corresponding cap shrinks as the carbon dioxide
    turns directly into a gas.

11
Mars Surface
  • Polar caps change in size depending on the
    Martian seasons.

12
Mars Surface
500 km
  • Olympus Mons
  • Largest mountain (volcano) in the Solar System
  • 24 km (78,000 ft) high
  • Base is 500 km in diameter
  • Rimmed by a 6 km (20,000 ft) high cliff

13
Mars Surface
  • Valles Marineris
  • Huge canyon
  • Would stretch coast to coast across the U.S.
  • It is 4000 km (2500 miles) long and up to 6 km (4
    miles) deep

4000 km
14
Mars Surface
Flight over the Martian Terrain, including Valles
Marineris and Three Volcanos
m
15
Mars Surface
  • Viking Lander
  • Landed in Chryse Planitia on July 20, 1976
  • Took panoramic pictures of the surface
  • On-board experiments tested soil for signs of
    life. Results were inconclusive.

16
Mars Surface
Viking Photos To the right Morning ground
frost Below Panorama and Mars pink sky.

17

Mars Surface



Pathfinder Photos
Rover and Yogi Martian Sunset
18
Mars Surface
  • Water on Mars?
  • There is evidence of liquid water once flowing
    over the surface of Mars.
  • Fluvial Features
  • Created by water flowing around a crater (right).
    Probably caused by a flood.

19
Mars Surface
  • Dry Riverbeds
  • Created by slow erosion of running water.

20
Mars Surface
  • Dust Storms
  • Mars surface winds churn up surface material
  • Storm sizes range in size from small local
    dust-devils to plumes that sweep over the
    entire planet (right)

21
Mars Moons
PHOBOS
Phobos is Greek for fear Mars innermost
moon Size 27 x 21.6 x 18.8 km

Above Crater Stickney Left Image by Soviet
spacecraft Phobos 2, launched in 1988
22
Mars Moons
  • DEIMOS
  • Deimos is Greek
  • for panic
  • Smallest known moon
  • in the solar system
  • 15 x 12.2 x 11 km

Phobos and Deimos are probably captured asteroids
23
Martian Myths of Yesterday
  • Canals of Mars
  • Discovered by G.V. Schiaparelli in 1877
  • Percival Lowell (below) built an observatory in
    1894 pricipally for the study of the Martian
    canals
  • The canals are actually optical illusions


24
Martian Myths of Today
  • The Face
  • Lies in the Cydonia region, a region of
    weathered, isolated hills
  • One hill resembling a face was photograghed by
    Viking 1

Some people believe this is a monument built by a
Martian intelligence, and that other
surface features resemble pyramids, cities, and
fortresses
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