This topographical map [
http://ltpwww.gsfc.
] of the southern hemisphere of Mars [
http://antwrp.gsfc.
] was generated using data from the Mars Orbiter Laser Altimeter [
http://ltpwww.gsfc.
] (MOLA). Flying on the Mars Global Surveyor spacecraft, MOLA has bounced a laser beam off the Martian surface over 200,000,000 times producing a wealth of detailed elevation measurements. The MOLA measurements [
http://ltpwww.gsfc.
] have been color-coded so, for example, the white areas at left are the highest elevations in the southern Tharsis region [
http://ltpwww.gsfc.
] and not snow-covered peaks. These areas are more than 6 kilometers above the hypothetical Martian "sea-level". Likewise, deep blues and purples are not water oceans [
http://antwrp.gsfc.
] but correspond to the lowest elevations (more than 4 kilometers below "sea-level"), like those found within the giant Hellas impact basin at right. In fact, liquid water is not present on Mars' surface today, but may have been [
http://www.msss.com
] in the past [
http://mars.jpl.nas
]. NASA's Mars Polar Lander [
http://mars.jpl.nas
] spacecraft is scheduled to embark on an investigation [
http://mars.jpl.nas
] of the role of water in the climate history of the Red Planet. The lander is targeted to touch down [
http://www.msss.com
] within the long, thin ellipse [
http://www.msss.com
] indicated here just below the Martian South Pole today at 20:00 UTC [
http://tycho.usno.n
].
Explanation
This topographical map [
http://ltpwww.gsfc.
] of the southern hemisphere of Mars [
http://antwrp.gsfc.
] was generated using data from the Mars Orbiter Laser Altimeter [
http://ltpwww.gsfc.
] (MOLA). Flying on the Mars Global Surveyor spacecraft, MOLA has bounced a laser beam off the Martian surface over 200,000,000 times producing a wealth of detailed elevation measurements. The MOLA measurements [
http://ltpwww.gsfc.
] have been color-coded so, for example, the white areas at left are the highest elevations in the southern Tharsis region [
http://ltpwww.gsfc.
] and not snow-covered peaks. These areas are more than 6 kilometers above the hypothetical Martian "sea-level". Likewise, deep blues and purples are not water oceans [
http://antwrp.gsfc.
] but correspond to the lowest elevations (more than 4 kilometers below "sea-level"), like those found within the giant Hellas impact basin at right. In fact, liquid water is not present on Mars' surface today, but may have been [
http://www.msss.com
] in the past [
http://mars.jpl.nas
]. NASA's Mars Polar Lander [
http://mars.jpl.nas
] spacecraft is scheduled to embark on an investigation [
http://mars.jpl.nas
] of the role of water in the climate history of the Red Planet. The lander is targeted to touch down [
http://www.msss.com
] within the long, thin ellipse [
http://www.msss.com
] indicated here just below the Martian South Pole today at 20:00 UTC [
http://tycho.usno.n
].
Explanation